{"pageNumber":"301","pageRowStart":"7500","pageSize":"25","recordCount":10961,"records":[{"id":67980,"text":"ha734 - 1995 - Watershed characterization for precipitation-runoff modeling system, north fork, American River and east fork, Carson River watersheds, California","interactions":[],"lastModifiedDate":"2015-10-28T11:29:03","indexId":"ha734","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"734","title":"Watershed characterization for precipitation-runoff modeling system, north fork, American River and east fork, Carson River watersheds, California","docAbstract":"<p>As part of its Global Change Hydrology Program, the U.S. Geological Survey (USGS) is investigating the potential effects of climate change on the water resources of several river basins in the United States. The American River Basin in California represents the windward slope of the north-central Sierra Nevada, and the California part of the Carson River Basin, most of which is in Nevada, represents the leeward slope. Parts of the American River and Carson River Basins&mdash;the North Fork American River and East Fork Carson River watersheds, both in California&mdash;were studied to determine the sensitivity of water resources to potential climate change. The water resources of both basins are derived primarily from snowmelt. A geographic information system (GIS) data base has been created to facilitate paired-basin analysis. The GIS data base incorporates (1) land-surface data, which include elevation, land use and land cover, soil type, and geology; (2) hydrologic data, such as stream networks and streamflow-gaging stations; and (3) climatic data, such as snow-course, snow-telemetry, radiosonde, and meteorological data. Precipitation-runoff models were developed and calibrated for the North Fork watershed within the American River Basin and for the East Fork watershed within the Carson River Basin. (These watersheds were selected to represent the climatic and physiographic variability of the two larger basins.) Synthesized climate scenarios then were used in the model to predict potential effects of climate change.</p>","language":"ENGLISH","doi":"10.3133/ha734","usgsCitation":"Smith, J.L., and Reece, B.D., 1995, Watershed characterization for precipitation-runoff modeling system, north fork, American River and east fork, Carson River watersheds, California: U.S. Geological Survey Hydrologic Atlas 734, 1 maps on 1 sheet :col ;11 x 14 cm. and 11 x 10 cm., on sheet 109 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha734.","productDescription":"1 maps on 1 sheet :col ;11 x 14 cm. and 11 x 10 cm., on sheet 109 x 104 cm., folded in envelope 30 x 24 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":252271,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/734/report-thumb.jpg"},{"id":251445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/734/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":251446,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/734/plate-1.pdf","size":"11336","linkFileType":{"id":1,"text":"pdf"}}],"scale":"545000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.91666666666667,38.35 ], [ -119.91666666666667,38.75 ], [ -119.58333333333333,38.75 ], [ -119.58333333333333,38.35 ], [ -119.91666666666667,38.35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b3b","contributors":{"authors":[{"text":"Smith, J. LaRue jlsmith@usgs.gov","contributorId":1863,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"jlsmith@usgs.gov","middleInitial":"LaRue","affiliations":[],"preferred":true,"id":277442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reece, Brian D. bdreece@usgs.gov","contributorId":2129,"corporation":false,"usgs":true,"family":"Reece","given":"Brian","email":"bdreece@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":277443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68110,"text":"ha730M - 1995 - Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","interactions":[{"subject":{"id":68110,"text":"ha730M - 1995 - Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","indexId":"ha730M","publicationYear":"1995","noYear":false,"chapter":"M","title":"Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont"},"predicate":"IS_PART_OF","object":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"id":1}],"isPartOf":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"lastModifiedDate":"2017-05-30T15:37:02","indexId":"ha730M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"730","chapter":"M","title":"Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","docAbstract":"<p>The State of New York and the six New England States of Maine, Vermont, New Hampshire, Massachusetts, Connecticut, and Rhode Island compose Segment 12 of this Atlas (fig. 1). The seven States have a total land area of about 116,000 square miles (table 1); all but a small area in southwestern New York has been glaciated. </p><p>Population in the States of Segment 12 totals about 30,408,000 (table 1) and is concentrated in southern and eastern Massachusetts, Connecticut, Rhode Island, and especially New York (fig. 1). The northern part of the segment and the mountainous areas of New York and much of New Hampshire, Vermont, and Maine are sparsely populated. </p><p>The percentage of population supplied from ground-water sources during 1980 was 54 to 60 percent in Maine, New Hampshire, and Vermont (table 1). Nearly all rural, domestic, and small-community water systems obtain water from wells that are, in comparison with other sources, the safest and the least expensive to install and maintain. Where water demand is great-in the urban areas of New York, Connecticut, Massachusetts, and Rhode Island-sophisticated reservoir, pipeline, and purification systems are economically feasible and are needed to meet demands. Surface water is the principal source of supply in these four States, and ground water was used to supply only 24 to 35 percent of their population during 1980 (table 1).</p>","largerWorkTitle":"Ground Water Atlas of the United States","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha730M","isbn":"0607868732","usgsCitation":"Olcott, P.G., 1995, Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont: U.S. Geological Survey Hydrologic Atlas 730, 28 p., https://doi.org/10.3133/ha730M.","productDescription":"28 p.","startPage":"M1","endPage":"M28","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":11490,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ha/ha730/ch_m/index.html","linkFileType":{"id":5,"text":"html"}},{"id":186515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/730m/report-thumb.jpg"},{"id":115251,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/730m/report.pdf","text":"Report","size":"56.57 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-71.860513,41.320248],[-71.886302,41.33641],[-71.945652,41.337799],[-71.988153,41.320577],[-72.084487,41.319634],[-72.11182,41.299098],[-72.184122,41.323997],[-72.212924,41.291365],[-72.248161,41.299488],[-72.261487,41.282926],[-72.333894,41.282916],[-72.386629,41.261798],[-72.398688,41.278172],[-72.451925,41.278885],[-72.546833,41.250718],[-72.583336,41.271698],[-72.617237,41.271998],[-72.671673,41.267151],[-72.69547,41.244948],[-72.754444,41.266913],[-72.895445,41.243697],[-72.916827,41.282033],[-73.013465,41.205479],[-73.054947,41.208468],[-73.07761,41.195176],[-73.108352,41.153718],[-73.130253,41.146797],[-73.177774,41.166697],[-73.235058,41.143996],[-73.262358,41.117496],[-73.286759,41.127896],[-73.372296,41.10402],[-73.435063,41.056696],[-73.468239,41.051347],[-73.477364,41.035997],[-73.493327,41.048173],[-73.516903,41.038738],[-73.528866,41.016397],[-73.535338,41.03192],[-73.570068,41.001597],[-73.595699,41.015995],[-73.643478,41.002171],[-73.683273,40.948998],[-73.756776,40.912599],[-73.784803,40.878528],[-73.781206,40.838891],[-73.793785,40.855583],[-73.81281,40.846737],[-73.811889,40.825363],[-73.781369,40.794907],[-73.728275,40.8529],[-73.730675,40.8654],[-73.675573,40.856999],[-73.633771,40.898198],[-73.499941,40.918166],[-73.485365,40.946397],[-73.406074,40.920235],[-73.392862,40.955297],[-73.352761,40.926697],[-73.229285,40.905121],[-73.148994,40.928898],[-73.140785,40.966178],[-73.110368,40.971938],[-72.774104,40.965314],[-72.714425,40.985596],[-72.585327,40.997587],[-72.477306,41.052212],[-72.445242,41.086116],[-72.397,41.096307],[-72.356087,41.133635],[-72.278789,41.158722],[-72.238211,41.15949],[-72.300374,41.112274],[-72.306381,41.13784],[-72.32663,41.132162],[-72.335177,41.106917],[-72.317238,41.088659],[-72.280373,41.080402],[-72.260515,41.042065],[-72.190563,41.032579],[-72.153857,41.051859],[-72.10216,40.991509],[-71.96704,41.047772],[-71.959595,41.071237],[-71.857494,41.073558],[-71.903736,41.040166],[-72.39585,40.86666],[-73.054963,40.666371],[-73.262106,40.621476],[-73.306396,40.620756],[-73.319257,40.635795],[-73.562372,40.583703],[-73.774928,40.590759],[-73.934512,40.545175],[-73.95005,40.573363],[-74.00903,40.572846],[-74.001591,40.590684],[-74.032856,40.604421],[-74.042412,40.624847],[-74.018272,40.659019],[-74.013784,40.756601],[-73.929006,40.889578],[-73.893979,40.997197],[-74.694914,41.357423],[-74.691129,41.367324],[-74.740963,41.40512],[-74.736688,41.429228],[-74.790417,41.42166],[-74.805655,41.442101],[-74.834635,41.430796],[-74.8542,41.443166],[-74.888691,41.438259],[-74.917282,41.477041],[-74.981652,41.479945],[-74.984372,41.506611],[-75.003706,41.511118],[-75.023018,41.533147],[-75.018524,41.551802],[-75.074613,41.605711],[-75.043562,41.62364],[-75.052736,41.688393],[-75.067278,41.705434],[-75.052226,41.711396],[-75.053431,41.752538],[-75.10464,41.774203],[-75.074409,41.815088],[-75.113334,41.822782],[-75.114399,41.843583],[-75.161541,41.849836],[-75.174574,41.87266],[-75.183937,41.860515],[-75.257825,41.862154],[-75.279094,41.938917],[-75.318168,41.954236],[-75.342204,41.972872],[-75.341125,41.992772],[-75.359579,41.999445],[-79.761374,41.999067],[-79.761951,42.26986],[-79.453533,42.411157],[-79.351989,42.48892],[-79.148723,42.553672],[-79.111361,42.613358],[-79.06376,42.644758],[-79.04886,42.689158],[-78.918157,42.737258],[-78.853455,42.783958],[-78.865592,42.852358],[-78.891655,42.884845],[-78.912458,42.886557],[-78.905659,42.923357],[-78.918859,42.946857],[-79.019964,42.994756],[-79.01053,43.064389],[-79.074467,43.077855],[-79.042366,43.143655],[-79.070469,43.262454],[-78.634346,43.357624],[-78.370221,43.376505],[-77.976438,43.369159],[-77.760231,43.341161],[-77.551022,43.235763],[-77.341092,43.280661],[-77.111866,43.287945],[-76.958402,43.270005],[-76.69836,43.344436],[-76.630774,43.413356],[-76.486962,43.47535],[-76.417581,43.521285],[-76.297103,43.51287],[-76.228701,43.532987],[-76.199138,43.600454],[-76.205436,43.718751],[-76.229268,43.804135],[-76.283307,43.843923],[-76.28272,43.858601],[-76.243384,43.877975],[-76.202257,43.864898],[-76.133267,43.892975],[-76.125023,43.912773],[-76.139086,43.962111],[-76.22805,43.982737],[-76.264294,43.978009],[-76.269672,44.001148],[-76.296755,44.013307],[-76.300532,44.057188],[-76.360306,44.070907],[-76.363835,44.111696],[-76.312647,44.199044],[-76.206777,44.214543],[-76.164265,44.239603],[-76.161833,44.280777],[-76.000998,44.347534],[-75.970185,44.342835],[-75.912985,44.368084],[-75.82083,44.432244],[-75.807778,44.471644],[-75.76623,44.515851],[-75.413885,44.76889],[-75.333744,44.806378],[-75.283136,44.849156],[-75.027125,44.946568],[-74.992756,44.977449],[-74.907956,44.983359],[-74.826578,45.01585],[-74.731301,44.990422],[-74.702018,45.003322],[-74.146814,44.9915],[-73.059685,45.015869],[-72.310073,45.003822],[-71.502487,45.013367],[-71.497917,45.070589],[-71.427208,45.127364],[-71.437216,45.142333],[-71.39781,45.203553],[-71.443882,45.235462],[-71.38317,45.234904],[-71.357253,45.253336],[-71.362831,45.267617],[-71.284396,45.302434],[-71.231572,45.253472],[-71.13943,45.242958],[-71.097772,45.301906],[-71.00905,45.319022],[-71.004848,45.345419],[-70.921435,45.313867],[-70.912111,45.296197],[-70.9217,45.279445],[-70.892822,45.239172],[-70.84443,45.234513],[-70.848554,45.263325],[-70.807058,45.322464],[-70.819828,45.340109],[-70.802648,45.364933],[-70.826033,45.398408],[-70.798677,45.424146],[-70.755567,45.428361],[-70.712286,45.390611],[-70.634661,45.383608],[-70.635498,45.427817],[-70.717047,45.487732],[-70.723167,45.507606],[-70.688214,45.563981],[-70.5584,45.666671],[-70.525831,45.666551],[-70.469869,45.701639],[-70.400404,45.719834],[-70.383552,45.734869],[-70.417641,45.79377],[-70.253704,45.902981],[-70.263315,45.920152],[-70.24092,45.939095],[-70.252963,45.955234],[-70.31297,45.961856],[-70.309725,45.98021],[-70.287754,45.99182],[-70.317629,46.01908],[-70.278169,46.059671],[-70.306734,46.061344],[-70.284554,46.098713],[-70.254021,46.0996],[-70.239566,46.142762],[-70.292736,46.191599],[-70.248421,46.267072],[-70.205719,46.299865],[-70.208733,46.328961],[-70.191412,46.348072],[-70.141164,46.362669],[-70.096286,46.40943],[-70.057061,46.415036],[-69.997086,46.69523],[-69.22442,47.459686],[-69.082508,47.423976],[-69.043947,47.427634],[-69.050367,47.259821],[-68.90524,47.180919],[-68.717867,47.240919],[-68.607906,47.247497],[-68.582984,47.285493],[-68.507432,47.296636],[-68.448844,47.282547],[-68.376829,47.28852],[-68.380334,47.340242],[-68.329879,47.36023],[-68.234604,47.355035],[-68.15515,47.32542],[-68.137059,47.296068],[-67.955669,47.199542],[-67.883844,47.105834],[-67.789761,47.065744],[-67.781095,45.943032],[-67.750422,45.917898],[-67.803318,45.883718],[-67.796514,45.859961],[-67.755068,45.82367],[-67.806598,45.794723],[-67.806308,45.755405],[-67.781892,45.731189],[-67.809833,45.729274],[-67.803148,45.696127],[-67.817892,45.693705],[-67.720401,45.662522],[-67.729908,45.689012],[-67.64581,45.613597],[-67.631762,45.621409],[-67.499444,45.587014],[-67.455406,45.604665],[-67.429716,45.583773],[-67.420976,45.550029],[-67.435044,45.528783],[-67.416416,45.503515],[-67.462882,45.508691],[-67.503157,45.485367],[-67.473366,45.425328],[-67.418747,45.37726],[-67.460554,45.300379],[-67.489464,45.282653],[-67.404629,45.159926],[-67.345585,45.126392],[-67.298209,45.146672],[-67.283619,45.192022],[-67.227324,45.163652],[-67.161247,45.162879],[-67.090786,45.068721],[-67.117688,45.05673],[-67.082074,45.029608],[-67.033474,44.939923],[-66.984466,44.912557],[-66.990351,44.882551],[-66.978142,44.856963],[-66.996523,44.844654],[-66.986318,44.820657],[-66.950569,44.814539],[-67.02615,44.768199],[-67.062239,44.769543],[-67.073439,44.741957],[-67.098931,44.741311],[-67.103957,44.717444],[-67.155119,44.66944],[-67.213025,44.63922],[-67.24726,44.641664],[-67.293403,44.599265],[-67.32297,44.609394],[-67.293665,44.634316],[-67.309627,44.659316],[-67.299176,44.705705],[-67.308538,44.707454],[-67.376742,44.681852],[-67.363158,44.631825],[-67.386605,44.626974],[-67.405492,44.594236],[-67.428367,44.609136],[-67.457747,44.598014],[-67.505804,44.636837],[-67.551133,44.621938],[-67.575056,44.560659],[-67.568159,44.531117],[-67.648506,44.525403],[-67.685861,44.537155],[-67.71419,44.495238],[-67.733986,44.496252],[-67.753854,44.543661],[-67.774001,44.547438],[-67.781556,44.520577],[-67.79726,44.520685],[-67.808837,44.544081],[-67.839896,44.558771],[-67.856684,44.523934],[-67.851648,44.484901],[-67.868774,44.465272],[-67.855108,44.419434],[-67.887323,44.433066],[-67.899571,44.394078],[-67.92132,44.433066],[-67.931453,44.411848],[-67.955737,44.416278],[-67.978876,44.387034],[-68.006102,44.409562],[-68.049334,44.33073],[-68.067047,44.335692],[-68.077873,44.373047],[-68.11229,44.401588],[-68.117746,44.475038],[-68.194554,44.47189],[-68.189937,44.484901],[-68.213861,44.492456],[-68.224354,44.464335],[-68.261708,44.484062],[-68.299063,44.437893],[-68.247438,44.433276],[-68.249956,44.417747],[-68.184532,44.369145],[-68.173608,44.328397],[-68.233435,44.288578],[-68.289409,44.283858],[-68.290818,44.247673],[-68.317588,44.225101],[-68.401268,44.252244],[-68.430946,44.298624],[-68.398035,44.376191],[-68.360318,44.389674],[-68.3791,44.430049],[-68.427874,44.3968],[-68.429648,44.439136],[-68.455095,44.447498],[-68.461072,44.378504],[-68.483317,44.388157],[-68.472824,44.404106],[-68.480379,44.432647],[-68.529905,44.39907],[-68.565161,44.39907],[-68.545434,44.355],[-68.566936,44.317603],[-68.538595,44.299902],[-68.519516,44.265046],[-68.525302,44.227554],[-68.733004,44.328388],[-68.762021,44.329597],[-68.795063,44.30786],[-68.827197,44.31216],[-68.814811,44.362194],[-68.821767,44.40894],[-68.783679,44.473879],[-68.880271,44.428112],[-68.897104,44.450643],[-68.927452,44.448039],[-68.990767,44.415033],[-68.948164,44.355882],[-68.954465,44.32405],[-68.979005,44.296327],[-69.003682,44.294582],[-69.005071,44.274071],[-69.040193,44.233673],[-69.054546,44.171542],[-69.077776,44.165043],[-69.080331,44.117824],[-69.100863,44.104529],[-69.092,44.085734],[-69.056303,44.095162],[-69.031878,44.079036],[-69.048917,44.062506],[-69.064299,44.069911],[-69.073767,44.046135],[-69.125738,44.019623],[-69.124475,44.007419],[-69.170345,43.995637],[-69.214205,43.935583],[-69.259838,43.921427],[-69.280498,43.95744],[-69.31427,43.942951],[-69.305176,43.956676],[-69.331411,43.974311],[-69.398455,43.971804],[-69.423324,43.915507],[-69.483498,43.88028],[-69.50329,43.837673],[-69.514889,43.831298],[-69.520301,43.868498],[-69.543912,43.881615],[-69.552606,43.841347],[-69.575466,43.841972],[-69.588551,43.81836],[-69.604179,43.813551],[-69.594705,43.858878],[-69.621086,43.826814],[-69.634932,43.845907],[-69.649798,43.836287],[-69.653337,43.79103],[-69.705838,43.823024],[-69.719723,43.786685],[-69.752801,43.75594],[-69.780097,43.755397],[-69.835323,43.721125],[-69.838689,43.70514],[-69.851297,43.703581],[-69.868673,43.742701],[-69.862155,43.758962],[-69.884066,43.778035],[-69.953246,43.768806],[-70.001645,43.717666],[-69.998793,43.740385],[-70.041351,43.738053],[-69.99821,43.798684],[-70.026193,43.822587],[-70.002874,43.848239],[-70.009869,43.859315],[-70.064671,43.813259],[-70.107229,43.809178],[-70.176023,43.76079],[-70.172525,43.773615],[-70.190014,43.771866],[-70.215666,43.707737],[-70.254144,43.676839],[-70.211204,43.625765],[-70.217087,43.596717],[-70.196911,43.565146],[-70.244331,43.551849],[-70.272497,43.562616],[-70.361214,43.52919],[-70.385615,43.487031],[-70.380233,43.46423],[-70.349684,43.442032],[-70.39089,43.402607],[-70.421282,43.395777],[-70.460717,43.34325],[-70.517695,43.344037],[-70.553854,43.321886],[-70.593907,43.249295],[-70.575787,43.221859],[-70.638355,43.114182],[-70.673114,43.070314],[-70.703818,43.059825],[-70.704696,43.070989],[-70.718936,43.03235],[-70.810069,42.909549],[-70.817731,42.850613],[-70.80522,42.781798],[-70.770453,42.704824],[-70.778552,42.69852],[-70.689402,42.653319],[-70.630077,42.692699],[-70.623815,42.665481],[-70.595474,42.660336],[-70.591469,42.639821],[-70.61842,42.62864],[-70.654727,42.582234],[-70.675747,42.594669],[-70.698574,42.577393],[-70.871382,42.546404],[-70.866279,42.522617],[-70.831091,42.503596],[-70.835991,42.490496],[-70.857791,42.490296],[-70.894292,42.460896],[-70.934993,42.457896],[-70.933155,42.437833],[-70.901992,42.420297],[-70.936393,42.418097],[-70.943612,42.452092],[-70.96047,42.446166],[-70.990595,42.407098],[-70.953022,42.343973],[-70.998253,42.352788],[-71.01568,42.326019],[-70.98909,42.267449],[-70.910941,42.265412],[-70.895778,42.292436],[-70.915588,42.302463],[-70.882764,42.30886],[-70.851093,42.26827],[-70.770964,42.249197],[-70.722269,42.207959],[-70.714301,42.168783],[-70.63848,42.081579],[-70.643208,42.050821],[-70.66936,42.037116],[-70.670934,42.007786],[-70.695809,42.013346],[-70.710034,41.999544],[-70.662476,41.960592],[-70.616491,41.940204],[-70.583572,41.950007],[-70.552941,41.929641],[-70.525567,41.85873],[-70.54103,41.815754],[-70.471552,41.761563],[-70.290957,41.734312],[-70.263654,41.714115],[-70.189254,41.751982],[-70.024734,41.787364],[-70.003842,41.80852],[-70.000188,41.886938],[-70.024335,41.89882],[-70.030537,41.929154],[-70.044995,41.930049],[-70.065671,41.911658],[-70.064084,41.878924],[-70.095595,42.032832],[-70.155415,42.062409],[-70.186816,42.05045],[-70.186295,42.021308],[-70.196693,42.022429],[-70.245385,42.063733],[-70.189305,42.082337],[-70.058531,42.040363],[-69.986085,41.949597],[-69.935952,41.809422],[-69.928261,41.6917],[-69.967869,41.627503],[-69.988215,41.554704],[-70.004136,41.54212],[-70.016584,41.550772],[-69.994357,41.576846],[-69.973153,41.646963],[-70.007011,41.671579],[-70.191061,41.645259],[-70.265424,41.609333],[-70.28132,41.635125],[-70.351634,41.634687],[-70.379151,41.611361],[-70.437246,41.605329],[-70.485571,41.554244],[-70.633607,41.538254],[-70.79027,41.446339],[-70.948431,41.409193],[-70.928165,41.431265],[-70.906011,41.425708],[-70.802186,41.460864],[-70.658659,41.543385],[-70.64204,41.583066],[-70.652449,41.60521],[-70.640003,41.624616],[-70.652614,41.637829],[-70.638695,41.649427],[-70.646308,41.678433],[-70.661475,41.681756],[-70.623652,41.707398],[-70.718739,41.73574],[-70.728933,41.723433],[-70.719575,41.685002],[-70.755347,41.694326],[-70.765463,41.641575],[-70.809118,41.656437],[-70.816351,41.645995],[-70.800215,41.631753],[-70.810279,41.624873],[-70.852518,41.626919],[-70.852551,41.588526],[-70.887643,41.632422],[-70.913202,41.619266],[-70.899981,41.593504],[-70.927172,41.611253],[-70.931338,41.5842],[-70.946911,41.581089],[-70.931545,41.540169],[-71.035514,41.499047],[-71.085663,41.509292],[-71.136867,41.493942],[-71.19302,41.457931],[-71.213563,41.545818],[-71.212417,41.61829],[-71.240709,41.619225],[-71.227989,41.528297],[-71.24071,41.474872],[-71.285639,41.487805],[-71.304394,41.454502],[-71.337695,41.448902],[-71.362743,41.460379],[-71.316519,41.47756],[-71.330831,41.518364],[-71.288376,41.573274],[-71.271862,41.623986],[-71.212136,41.641945],[-71.19564,41.67509],[-71.224798,41.710498],[-71.25956,41.642595],[-71.280366,41.672575],[-71.299159,41.649531],[-71.306095,41.672575],[-71.291217,41.702666],[-71.31482,41.723808],[-71.350057,41.727835],[-71.37791,41.666646],[-71.445923,41.691144],[-71.444468,41.664409],[-71.409302,41.662643],[-71.40377,41.589321],[-71.447712,41.5804],[-71.414825,41.523126],[-71.417621,41.477934],[-71.483295,41.371722],[-71.555381,41.373316],[-71.857432,41.306318],[-71.860513,41.320248]]],[[[-70.59628,41.471905],[-70.567356,41.471208],[-70.547567,41.415831],[-70.506984,41.400242],[-70.501306,41.385391],[-70.450431,41.420703],[-70.451084,41.348161],[-70.709826,41.341723],[-70.747541,41.329952],[-70.775665,41.300982],[-70.838777,41.347209],[-70.774974,41.349176],[-70.686881,41.441334],[-70.603555,41.482384],[-70.59628,41.471905]]],[[[-70.092142,41.297741],[-70.031332,41.339332],[-70.030924,41.367453],[-70.049564,41.3879],[-70.033514,41.385816],[-69.960181,41.264546],[-70.001586,41.239353],[-70.118669,41.242351],[-70.256164,41.288123],[-70.275526,41.310464],[-70.229541,41.290171],[-70.092142,41.297741]]],[[[-70.152589,43.746794],[-70.145911,43.772119],[-70.128271,43.774009],[-70.152589,43.746794]]],[[[-70.171245,43.663498],[-70.205934,43.633633],[-70.188047,43.673762],[-70.171245,43.663498]]],[[[-70.186213,43.682655],[-70.21313,43.662973],[-70.201893,43.685483],[-70.186213,43.682655]]],[[[-70.163884,43.692404],[-70.135563,43.700658],[-70.168227,43.675136],[-70.163884,43.692404]]],[[[-70.087621,43.699913],[-70.115908,43.682978],[-70.095727,43.709278],[-70.087621,43.699913]]],[[[-70.119671,43.748621],[-70.097318,43.757292],[-70.124136,43.70832],[-70.138711,43.727559],[-70.119671,43.748621]]],[[[-68.499465,44.12419],[-68.491521,44.109833],[-68.51706,44.10341],[-68.511266,44.125082],[-68.499465,44.12419]]],[[[-68.358388,44.125082],[-68.330716,44.110598],[-68.365176,44.101464],[-68.376593,44.112207],[-68.358388,44.125082]]],[[[-68.453236,44.189998],[-68.416434,44.187047],[-68.384903,44.154955],[-68.438518,44.11618],[-68.456813,44.145268],[-68.502096,44.152388],[-68.453236,44.189998]]],[[[-68.680773,44.279242],[-68.623554,44.255622],[-68.605906,44.230772],[-68.624994,44.197637],[-68.618872,44.18107],[-68.681899,44.138212],[-68.720435,44.169185],[-68.722956,44.219607],[-68.680458,44.262105],[-68.680773,44.279242]]],[[[-68.355279,44.199096],[-68.31606,44.200244],[-68.347416,44.169459],[-68.378872,44.184222],[-68.355279,44.199096]]],[[[-68.472831,44.219767],[-68.453843,44.201683],[-68.48452,44.202886],[-68.482726,44.227058],[-68.472831,44.219767]]],[[[-68.792139,44.237819],[-68.769833,44.222787],[-68.780055,44.203129],[-68.829593,44.21689],[-68.839422,44.236547],[-68.792139,44.237819]]],[[[-68.23638,44.266254],[-68.211329,44.257074],[-68.23713,44.25343],[-68.248913,44.235443],[-68.274427,44.237099],[-68.274719,44.258675],[-68.23638,44.266254]]],[[[-68.498637,44.369686],[-68.478785,44.319563],[-68.489641,44.313705],[-68.530394,44.333583],[-68.518573,44.381022],[-68.501364,44.382281],[-68.498637,44.369686]]],[[[-68.618212,44.012367],[-68.635315,44.018886],[-68.652881,44.003845],[-68.661594,44.075837],[-68.6181,44.096706],[-68.584074,44.070578],[-68.618212,44.012367]]],[[[-68.785601,44.053503],[-68.818441,44.032046],[-68.889717,44.032516],[-68.913406,44.08519],[-68.907812,44.105518],[-68.943105,44.10973],[-68.935327,44.13038],[-68.825067,44.186338],[-68.818423,44.160978],[-68.780693,44.143274],[-68.820515,44.130198],[-68.772639,44.078439],[-68.785601,44.053503]]],[[[-67.619761,44.519754],[-67.582113,44.513459],[-67.590627,44.49415],[-67.562651,44.472104],[-67.574206,44.45173],[-67.588346,44.449754],[-67.619761,44.519754]]],[[[-68.942826,44.281073],[-68.919301,44.309872],[-68.90353,44.378613],[-68.868444,44.38144],[-68.860649,44.364425],[-68.896587,44.321986],[-68.88746,44.303094],[-68.916872,44.242866],[-68.95189,44.218719],[-68.965264,44.259332],[-68.942826,44.281073]]],[[[-74.144428,40.53516],[-74.219787,40.502603],[-74.254588,40.502303],[-74.247808,40.543396],[-74.210887,40.560902],[-74.1894,40.642121],[-74.075884,40.648101],[-74.059184,40.593502],[-74.144428,40.53516]]],[[[-72.132225,41.104387],[-72.126704,41.115139],[-72.084207,41.101524],[-72.086975,41.058292],[-72.095711,41.05402],[-72.103152,41.086484],[-72.139233,41.092451],[-72.132225,41.104387]]],[[[-71.943563,41.286675],[-71.926802,41.290122],[-72.036846,41.249794],[-72.023422,41.270994],[-71.943563,41.286675]]],[[[-71.383586,41.464782],[-71.399568,41.448596],[-71.373618,41.573214],[-71.359868,41.556308],[-71.360403,41.483121],[-71.383586,41.464782]]],[[[-71.3312,41.580318],[-71.325877,41.623988],[-71.366165,41.66098],[-71.338696,41.658782],[-71.342514,41.644791],[-71.30555,41.622523],[-71.307381,41.597984],[-71.3312,41.580318]]],[[[-71.58955,41.196557],[-71.576661,41.224434],[-71.561093,41.224207],[-71.565752,41.184373],[-71.547051,41.153684],[-71.611706,41.153239],[-71.58955,41.196557]]]]},\"properties\":{\"name\":\"Connecticut\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4289","contributors":{"authors":[{"text":"Olcott, Perry G.","contributorId":17249,"corporation":false,"usgs":true,"family":"Olcott","given":"Perry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221641,"text":"70221641 - 1994 - Geologic, hydrologic, and water-quality data for a multi-aquifer system in Coastal Plain sediments near Millers Pond, Burke County, Georgia, 1992-93","interactions":[],"lastModifiedDate":"2021-06-25T21:35:21.121506","indexId":"70221641","displayToPublicDate":"2021-06-25T16:28:05","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5595,"text":"Georgia Geologic Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"96","title":"Geologic, hydrologic, and water-quality data for a multi-aquifer system in Coastal Plain sediments near Millers Pond, Burke County, Georgia, 1992-93","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Georgia Geologic Survey","usgsCitation":"Clarke, J.S., Falls, W.F., Edwards, L.E., Frederiksen, N.O., Bybell, L.M., Gibson, T.G., and Litwin, R.J., 1994, Geologic, hydrologic, and water-quality data for a multi-aquifer system in Coastal Plain sediments near Millers Pond, Burke County, Georgia, 1992-93: Georgia Geologic Survey Information Circular 96, v, 34 p.","productDescription":"v, 34 p.","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":386762,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","county":"Burke County","otherGeospatial":"Miller's Pond","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.9854736328125,\n              33.19301824551205\n            ],\n            [\n              -81.84711456298828,\n              33.19301824551205\n            ],\n            [\n              -81.84711456298828,\n              33.296673231834106\n            ],\n            [\n              -81.9854736328125,\n              33.296673231834106\n            ],\n            [\n              -81.9854736328125,\n              33.19301824551205\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Clarke, John S. jsclarke@usgs.gov","contributorId":400,"corporation":false,"usgs":true,"family":"Clarke","given":"John","email":"jsclarke@usgs.gov","middleInitial":"S.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":818315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Falls, William F.","contributorId":260648,"corporation":false,"usgs":false,"family":"Falls","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":818316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":818317,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frederiksen, Norman O.","contributorId":50880,"corporation":false,"usgs":true,"family":"Frederiksen","given":"Norman","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":818318,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818319,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gibson, Thomas G.","contributorId":25180,"corporation":false,"usgs":true,"family":"Gibson","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":818320,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Litwin, Ronald J. 0000-0002-8661-1296 rlitwin@usgs.gov","orcid":"https://orcid.org/0000-0002-8661-1296","contributorId":2478,"corporation":false,"usgs":true,"family":"Litwin","given":"Ronald","email":"rlitwin@usgs.gov","middleInitial":"J.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":818321,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70179033,"text":"70179033 - 1994 - Ground-water hydrology of Ogden Valley and surrounding area, eastern Weber County, UT, and simulation of ground-water flow in the Valley-fill aquifer system","interactions":[],"lastModifiedDate":"2016-12-13T15:32:36","indexId":"70179033","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"99","title":"Ground-water hydrology of Ogden Valley and surrounding area, eastern Weber County, UT, and simulation of ground-water flow in the Valley-fill aquifer system","docAbstract":"<p>The ground-water resources in Ogden Valley, eastern Weber County, Utah, were the subject of a study to provide a better understanding of the hydrologic system in the valley and to estimate the hydrologic effects of future ground-water development. The study area included the drainage basin of the Ogden River upstream from Pineview Reservoir dam and the drainage basin of Wheeler Creek. Ogden Valley and the surrounding area are underlain by rocks that range in age from Precambrian to Quaternary.</p><p>The consolidated rocks that transmit and yield the most water in the area surrounding Ogden Valley are the Paleozoic carbonate rocks and the Wasatch Formation of Tertiary age. Much of the recharge to the consolidated rocks is from snowmelt that infiltrates the Wasatch Formation, which underlies a large part of the study area. Discharge from the consolidated rocks is by streams, evapotranspiration, springs, subsurface outflow, and pumping from wells. Water in the consolidated rocks is a calcium bicarbonate type and has a dissolved-solids concentration of less than 250 milligrams per liter.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Avery, C., 1994, Ground-water hydrology of Ogden Valley and surrounding area, eastern Weber County, UT, and simulation of ground-water flow in the Valley-fill aquifer system: Technical Publication 99, vi, 84 p.","productDescription":"vi, 84 p.","numberOfPages":"93","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332079,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332077,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-450"},{"id":332078,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/y920/y9200007.pdf"}],"country":"United States","state":"Utah","county":"Weber County","otherGeospatial":"Ogden Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.5102,41.4242],[-111.5017,41.4133],[-111.4974,41.4092],[-111.4901,41.4069],[-111.4834,41.4042],[-111.4797,41.4028],[-111.4773,41.4019],[-111.4748,41.4005],[-111.4718,41.3968],[-111.4749,41.3932],[-111.475,41.3851],[-111.467,41.38],[-111.4591,41.3764],[-111.4524,41.3745],[-111.4457,41.3722],[-111.4402,41.3727],[-111.4334,41.3708],[-111.4267,41.3685],[-111.4243,41.3649],[-111.4188,41.3621],[-111.4262,41.3594],[-111.425,41.3513],[-111.4251,41.3472],[-111.4263,41.344],[-111.4312,41.3431],[-111.4331,41.3418],[-111.4386,41.3382],[-111.4399,41.3264],[-111.4418,41.3227],[-111.4473,41.3155],[-111.4437,41.3078],[-111.4407,41.3028],[-111.4383,41.296],[-111.4408,41.2928],[-111.4451,41.286],[-111.4433,41.2815],[-111.4483,41.2756],[-111.4562,41.2733],[-111.4655,41.2634],[-111.4698,41.2566],[-111.4766,41.2512],[-111.4925,41.2422],[-111.4962,41.2327],[-111.5097,41.2318],[-111.5158,41.2323],[-111.5213,41.2318],[-111.5268,41.2341],[-111.5396,41.2401],[-111.5481,41.2392],[-111.5671,41.2402],[-111.5744,41.2397],[-111.5811,41.2407],[-111.589,41.2416],[-111.6044,41.2326],[-111.6068,41.2253],[-111.6087,41.2158],[-111.6131,41.2081],[-111.6192,41.2059],[-111.6357,41.1996],[-111.6443,41.1928],[-111.665,41.1869],[-111.6791,41.1815],[-111.6913,41.1834],[-111.7035,41.1825],[-111.7139,41.188],[-111.7437,41.2062],[-111.7449,41.2134],[-111.7498,41.2153],[-111.7535,41.2148],[-111.7547,41.2116],[-111.7596,41.2094],[-111.773,41.2194],[-111.798,41.2158],[-111.8048,41.214],[-111.8091,41.2081],[-111.8152,41.2045],[-111.8262,41.2036],[-111.8384,41.1991],[-111.8555,41.1986],[-111.8628,41.1909],[-111.8714,41.1887],[-111.8659,41.1819],[-111.8745,41.1692],[-111.8683,41.1651],[-111.8568,41.1578],[-111.8513,41.1533],[-111.8556,41.1474],[-111.8538,41.141],[-111.8574,41.136],[-111.8885,41.1351],[-111.8983,41.1342],[-111.9111,41.1338],[-111.9288,41.1329],[-111.9471,41.1375],[-111.9581,41.1465],[-111.9703,41.1511],[-111.9837,41.1515],[-111.9941,41.1515],[-111.9943,41.3502],[-111.9916,41.3539],[-111.9773,41.3588],[-111.9693,41.3639],[-111.9622,41.3653],[-111.9648,41.3681],[-111.9741,41.3768],[-111.9736,41.3814],[-111.9754,41.3849],[-111.9668,41.3935],[-111.967,41.3974],[-111.9664,41.4097],[-111.9702,41.414],[-111.9711,41.4202],[-111.9622,41.4257],[-111.9566,41.4341],[-111.9501,41.427],[-111.9356,41.4163],[-111.935,41.4162],[-111.9176,41.4117],[-111.9138,41.4147],[-111.9065,41.4176],[-111.8947,41.4201],[-111.893,41.4206],[-111.8847,41.4255],[-111.8836,41.4265],[-111.8708,41.4214],[-111.881,41.4148],[-111.8754,41.4106],[-111.8757,41.4056],[-111.8683,41.3987],[-111.864,41.398],[-111.8557,41.3947],[-111.8441,41.3919],[-111.8337,41.3874],[-111.8171,41.3896],[-111.8116,41.3869],[-111.7975,41.3901],[-111.792,41.391],[-111.7865,41.3873],[-111.7829,41.3814],[-111.7761,41.3769],[-111.759,41.3682],[-111.7523,41.3691],[-111.7351,41.3759],[-111.7249,41.3764],[-111.7268,41.3857],[-111.7058,41.4051],[-111.7062,41.4133],[-111.7185,41.4155],[-111.7238,41.4234],[-111.7215,41.4276],[-111.7073,41.4252],[-111.6957,41.417],[-111.6885,41.4187],[-111.6785,41.4273],[-111.6661,41.4285],[-111.6512,41.4072],[-111.6448,41.4055],[-111.6402,41.4146],[-111.6239,41.4184],[-111.6187,41.4218],[-111.6117,41.4217],[-111.599,41.4208],[-111.5852,41.4179],[-111.5751,41.4277],[-111.5624,41.4233],[-111.5537,41.4242],[-111.5499,41.4141],[-111.5413,41.406],[-111.5377,41.4111],[-111.531,41.4142],[-111.5182,41.4172],[-111.5172,41.4214],[-111.5102,41.4242]]]},\"properties\":{\"name\":\"Weber\",\"state\":\"UT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585116bde4b08138bf1abd5e","contributors":{"authors":[{"text":"Avery, Charles","contributorId":70739,"corporation":false,"usgs":true,"family":"Avery","given":"Charles","affiliations":[],"preferred":false,"id":655828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038750,"text":"70038750 - 1994 - New uranium-series ages of the Waimanalo Limestone, Oahu, Hawaii: implications for sea level during the last interglacial period","interactions":[],"lastModifiedDate":"2012-07-04T01:02:11","indexId":"70038750","displayToPublicDate":"2012-01-01T14:01:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"New uranium-series ages of the Waimanalo Limestone, Oahu, Hawaii: implications for sea level during the last interglacial period","docAbstract":"The Waimanalo Formation (limestone) of Oahu has been correlated with the last interglacial period based on U-series dating of corals by T.-L. Ku and colleagues. The limestone consists of growth-position corals and overlying coral conglomerate. An apparent bimodal distribution of ages for the growth-position corals (mean age = 133 ka) and the overlying coral conglomerate (mean age = 119 ka) has been interpreted to represent two distinct high stands of sea that occurred within the last interglacial period. Both growth-position corals and overlying, conglomerate coral occur in an outcrop east of Kaena Point and consist mainly of Pocillopora and Porites. U-seriesages of growth-position corals that show closed-system conditions are 120 &plusmn; 3 ka and 127 &plusmn; 4 ka; overlying conglomerate corals have U-seriesages that range from 120 &plusmn; 3 ka to 138 &plusmn; 4 ka. At Kahe Point, conglomerate corals have ages of 120 &plusmn; 3 ka and 134 &plusmn; 4 ka. These data show that the growth position corals are not systematically older than the conglomerate corals; thus, there is no evidence for two distinct high stands of sea. Waimanalo deposits at Kahe Point and Mokapu Point (new U-seriesages of 134 &plusmn; 4 ka and 127 &plusmn; 3 ka) have beach deposits as high as 12.5 m and, at Mokapu Point, growth-position corals as high as 8.5 m. A last-interglacial sea-level stand of +8.5 to +12.5 m conflicts with estimates of +6 m from a number of tectonically stable coastlines and islands in the western Atlantic Ocean. We infer, therefore, that Oahu may be undergoing uplift at a low rate. This uplift may be due to compensatory lithospheric flexure, because the island of Hawaii has been subsiding throughout much of the Quaternary from volcanic loading. Because of this possible uplift, Oahu and islands like it elsewhere in the Pacific cannot be used as reference points for sealevel during the last interglacial period.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0025-3227(94)90091-4","usgsCitation":"Muhs, D., and Szabo, B.J., 1994, New uranium-series ages of the Waimanalo Limestone, Oahu, Hawaii: implications for sea level during the last interglacial period: Marine Geology, v. 118, no. 3-4, p. 315-326, https://doi.org/10.1016/0025-3227(94)90091-4.","productDescription":"12 p.","startPage":"315","endPage":"326","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":257722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257692,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-3227(94)90091-4","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawai'i","otherGeospatial":"O'ahu;Waimanalo Limestone","volume":"118","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6620e4b0c8380cd72d20","contributors":{"authors":[{"text":"Muhs, D.R. 0000-0001-7449-251X","orcid":"https://orcid.org/0000-0001-7449-251X","contributorId":61460,"corporation":false,"usgs":true,"family":"Muhs","given":"D.R.","affiliations":[],"preferred":false,"id":464860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szabo, Barney J.","contributorId":6848,"corporation":false,"usgs":true,"family":"Szabo","given":"Barney","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":464859,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5222772,"text":"5222772 - 1994 - Reproductive success of barn swallows nesting near a selenium-contaminated lake in east Texas, USA","interactions":[],"lastModifiedDate":"2020-01-27T09:55:40","indexId":"5222772","displayToPublicDate":"2010-06-16T12:17:48","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1555,"text":"Environmental Pollution","active":true,"publicationSubtype":{"id":10}},"title":"Reproductive success of barn swallows nesting near a selenium-contaminated lake in east Texas, USA","docAbstract":"<p><span>Reproductive success and contaminant levels in 1986 and 1987 were compared between Barn Swallows nesting at selenium-contaminated Martin Lake, Texas, USA, and swallows nesting at a reference site. Nests were initiated about the same time or earlier at Martin Lake than at the reference site and clutch size was similar between the two locations. Nest success was significantly higher at Martin Lake than at the reference site and no embryo or chick deformities were documented. Selenium concentrations in 14 of 20 eggs from Martin Lake were above background (&gt; 3 ppm, dry weight); two of 20 eggs contained &gt; 5 ppm, a concentration associated with a 20% embryo mortality/deformity rate in some bird species. Selenium concentrations in the kidneys of adult swallows were higher at Martin Lake (mean = 14 ppm dry weight) than at the reference site (5·8 ppm). DDE, the only detected organochlorine compound, was in two of 10 eggs from Martin Lake; these concentrations were below those associated with chronic poisoning and reproductive problems. The maximum mercury concentration in livers of adult Barn Swallows (0·83 ppm, dry weight) was within the range for background levels (&gt;5 ppm).</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0269-7491(94)90070-1","usgsCitation":"King, K.A., Custer, T., and Weaver, D., 1994, Reproductive success of barn swallows nesting near a selenium-contaminated lake in east Texas, USA: Environmental Pollution, v. 84, no. 1, p. 53-58, https://doi.org/10.1016/0269-7491(94)90070-1.","productDescription":"6 p.","startPage":"53","endPage":"58","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Martin Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.6255874633789,\n              32.17619366706981\n            ],\n            [\n              -94.52499389648438,\n              32.17619366706981\n            ],\n            [\n              -94.52499389648438,\n              32.28568142693891\n            ],\n            [\n              -94.6255874633789,\n              32.28568142693891\n            ],\n            [\n              -94.6255874633789,\n              32.17619366706981\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"84","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c797","contributors":{"authors":[{"text":"King, Kirk A.","contributorId":9203,"corporation":false,"usgs":true,"family":"King","given":"Kirk","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":337101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":337103,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weaver, D.A.","contributorId":33284,"corporation":false,"usgs":true,"family":"Weaver","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":337102,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017861,"text":"70017861 - 1994 - Comparison of drier- to wetter-interval estuarine roof facies in the Eastern and Western Interior coal basins, USA","interactions":[],"lastModifiedDate":"2025-06-04T15:59:45.994554","indexId":"70017861","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of drier- to wetter-interval estuarine roof facies in the Eastern and Western Interior coal basins, USA","docAbstract":"<p>Many of the Carboniferous coals in the eastern interior of the US are associated with siliciclastic roof facies that were deposited within a fluvio-estuarine transition. These facies include a variety of rhythmites, some of which exhibit tidal cycles. Drier-interval coals (Westphalian B-C, Stephanian) tend to be more laterally restricted and more commonly are associated with paleovalleys. Conversely, wetter-interval coals (Westphalian D) are very widespread and are not restricted to paleovalleys. Throughout the Lake Carboniferous, wet paleoclimates associated with these coals lead to valley incision during sea-level lowstand when large tropical rivers downcut older sediments deposited during previous sea-level highstands. During subsequent rise of sea level, these fluvial valleys were flooded and converted to estuaries where tidal ranges and sedimentation rates were significantly amplified. Based on modern analogs and interpretation of many examples of Carboniferous tidal rhythmites, the localized depositional rates in these settings are exceptionally high. The estuaries became sediment sinks, trapping sediment that is pumped in from both fluvial and marine sources. As a result, sedimentation readily keeps pace with rising baselevel. Extensive intertidal flats and shallow subtidal flats are created and prograde over the valley-confined mires. Thick tidal cycles and upright trees (some with attached foliage) record rapid burial of mires. This model is supported with examples of roof facies from the Westphalian B-C of the Eastern Interior Basin, and the Stephanian of the Western Interior Basin. In these areas facies within each cycle range from well-developed, extensive paleosols and coals, to widespread marine shales or limestones. Variations in both sea level and climate resulted in a complex history of valley fill during which coals could be developed at any time (except during widespread flooding). Minable, low-sulfur and low-ash coals occur, but the coals are relatively thin and discontinuous. Conversely, the Westphalian D coals are very widespread and significant peat accumulations were not confined to paleovalleys. Nonetheless, the lowest sulfur coals are related to rapid deposition of roof facies that occurred within the paleovalley whereas high-sulfur coals were formed in areas of lower sedimentation rate of roof facies that occurred beyond the confines of the paleovalley.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(94)90009-4","issn":"00310182","usgsCitation":"Archer, A., Feldman, H.R., Kvale, E., and Lanier, W.P., 1994, Comparison of drier- to wetter-interval estuarine roof facies in the Eastern and Western Interior coal basins, USA: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 106, no. 1-4, p. 171-185, https://doi.org/10.1016/0031-0182(94)90009-4.","productDescription":"15 p.","startPage":"171","endPage":"185","costCenters":[],"links":[{"id":228490,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Illinois, Indiana, Iowa, Kansas, Kentucky, Missouri, Oklahoma","otherGeospatial":"Eastern and Western Interior coal basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -96.65983661812253,\n              36.32189849509018\n            ],\n            [\n              -86.2378733316447,\n              36.32189849509018\n            ],\n            [\n              -86.2378733316447,\n              41.84957669831883\n            ],\n            [\n              -96.65983661812253,\n              41.84957669831883\n            ],\n            [\n              -96.65983661812253,\n              36.32189849509018\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"106","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f85de4b0c8380cd4d057","contributors":{"authors":[{"text":"Archer, A.W.","contributorId":8620,"corporation":false,"usgs":true,"family":"Archer","given":"A.W.","affiliations":[],"preferred":false,"id":377779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feldman, H. R.","contributorId":29581,"corporation":false,"usgs":true,"family":"Feldman","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":377781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kvale, E.P.","contributorId":76076,"corporation":false,"usgs":true,"family":"Kvale","given":"E.P.","affiliations":[],"preferred":false,"id":377782,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lanier, William P.","contributorId":73672,"corporation":false,"usgs":true,"family":"Lanier","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":377780,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70017806,"text":"70017806 - 1994 - Paleoecology of the Fire Clay coal bed in a portion of the Eastern Kentucky Coal Field","interactions":[],"lastModifiedDate":"2025-06-04T16:12:32.694052","indexId":"70017806","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Paleoecology of the Fire Clay coal bed in a portion of the Eastern Kentucky Coal Field","docAbstract":"<p><span>Vertically continuous increment samples of the Fire Clay coal bed (mid-Middle Pennsylvanian, late Westphalian B), collected from a portion of the Central Appalachian Basin, were studied palynologically, petrographically and geochemically in order to partially reconstruct the paleoecology and processes associated with peat formation in the ancient Fire Clay paleomire. Results indicate that four compositional groups can be identified. They are: (1) a&nbsp;</span><i>Lycospora</i><span>—vitrinite dominant group, characterized by high percentages of&nbsp;</span><i>Lycospora</i><span>&nbsp;and vitrinite macerals and generally low, but variable ash yields and sulfur contents; (2) a mixed palynoflora-high vitrinite group that petrographically is similar to group 1 except that it contains a more diverse palynoflora; (3) a mixed palynoflora-moderate/low vitrinite group characterized by various admixtures of lycopsid, fern and calamite miospores, increased percentages of liptinite and inertinite macerals, and low ash yields and sulfur contents; and (4) a mixed palynoflora-high ash yield group characterized by high percentages of small lycopsid, fern, and occasionally calamite and cordaite miospores, high liptinite and inertinite contents, high ash yields, and moderate to high sulfur contents.</span></p><p><span>The Fire Clay coal bed contains a distinctive flint clay parting of probable volcanic origin that naturally divides the bed into two benches. These two benches, (upper and lower), are highly disparte in occurrence, appearance and composition. In the study area the lower bench generally is thin (&lt; 0.5 m), laterally discontinuous and mainly composed of dull (mainly durain) coal lithotypes. Ash yields typically are high; sulfur contents generally are moderate to high. Compositional group 4, the mixed palynoflora—high ash yield group defines all of the increments examined from the lower bench.</span></p><p><span>In contrast, the upper bench is thick (&gt; 0.75 m), laterally continous and mainly comprised of bright (mainly clarain) coal lithotypes. Overall ash yields and sulfur contents for this bench are generally low, although vertical variation is apparent. All of the compositional groups occur in the upper bench; in some columns, notably those that are thick and uninterrupted by clastic partings, groups 1 and 4 often occupy basal coal layers and groups 2 and 3 occur in higher layers. Other columns, especially those taken in areas of thin (&lt; 0.5 m) Fire Clay coal, are dominated by groups 1 and 4.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(94)90015-9","issn":"00310182","usgsCitation":"Eble, C., Hower, J., and Andrews, W., 1994, Paleoecology of the Fire Clay coal bed in a portion of the Eastern Kentucky Coal Field: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 106, no. 1-4, p. 287-305, https://doi.org/10.1016/0031-0182(94)90015-9.","productDescription":"19 p.","startPage":"287","endPage":"305","costCenters":[],"links":[{"id":228443,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Eastern Kentucky Coal Field","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -84.70905950279405,\n              37.89289150405992\n            ],\n            [\n              -84.70905950279405,\n              36.7856367797942\n            ],\n            [\n              -82.8101079120946,\n              36.7856367797942\n            ],\n            [\n              -82.8101079120946,\n              37.89289150405992\n            ],\n            [\n              -84.70905950279405,\n              37.89289150405992\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"106","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a73dbe4b0c8380cd772b2","contributors":{"authors":[{"text":"Eble, C.F.","contributorId":35346,"corporation":false,"usgs":true,"family":"Eble","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":377617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hower, J.C.","contributorId":100541,"corporation":false,"usgs":true,"family":"Hower","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":377619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andrews, W.M. Jr.","contributorId":38303,"corporation":false,"usgs":true,"family":"Andrews","given":"W.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":377618,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017617,"text":"70017617 - 1994 - 40Ar/39Ar thermochronologic constraints on the tectonothermal evolution of the northern East Humboldt Range metamorphic core complex, Nevada","interactions":[],"lastModifiedDate":"2025-08-15T15:35:26.949489","indexId":"70017617","displayToPublicDate":"2003-04-02T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"40Ar/39Ar thermochronologic constraints on the tectonothermal evolution of the northern East Humboldt Range metamorphic core complex, Nevada","docAbstract":"<p><span>The northern East Humboldt Range (NEHR) of northeastern Nevada exposes a suite of complexly deformed migmatitic, upper amphibolite-facies rocks in the footwall of the Ruby Mountains-East Humboldt Range (RM-EHR) detachment fault. New&nbsp;</span><sup>40</sup><span>Ar/</span><sup>39</sup><span>Ar data on hornblende, muscovite, biotite, and potassium feldspar help constrain the kinematic and thermal evolution of this terrain during Tertiary extensional exhumation. Hornblende samples from relatively high structural levels yield discordant age spectra that suggest initial cooling during early Tertiary time (63–49 Ma). When coupled with petrological constraints indicating a strongly decompressional&nbsp;</span><i>P-T-t</i><span>&nbsp;path above 550°C, the hornblende data suggest that exhumation of the RM-EHR may have initiated in early Tertiary time, approximately coincident with the initial phases of unroofing in the Wood Hills immediately to the east and with the end of thrusting in the late Mesozoic to early Tertiary Sevier orogenic belt of eastern Nevada and western Utah. This temporal coincidence suggests that gravitational collapse of tectonically thickened crust in the internal zone of the Sevier belt could have driven the initial phases of unroofing.</span></p><p><span>Thermal history during the final stage of exhumation of the NEHR is constrained by discordant hornblende cooling ages of 36-29 Ma from deep structural levels and biotite, muscovite, and potassium feldspar cooling ages of 27-21 Ma from a range of structural levels. Comparison of muscovite, biotite, and potassium feldspar cooling ages with previously published fission-track cooling ages implies very rapid cooling rates at temperatures below the closure temperature for muscovite (270°–350°C), but time gaps of &gt; 7 m.y. between hornblende and mica cooling ages suggest that cooling at higher temperatures was more gradual. In addition, comparison of <sup>40</sup>Ar<sup>39</sup>Ar</span><span>&nbsp;mica cooling ages with previously published fission-track apatite cooling ages suggests pronounced thermal gradients between the NEHR and adjacent areas during latest Oligocene to earliest Miocene time. Such thermal gradients could be readily explained if the RM-EHR detachment fault dipped &gt; 30° between the 300°C and 100°C isotherms. Finally, <sup>40</sup>Ar<sup>39</sup>Ar</span><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"&lt;math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;&gt;&lt;msup&gt;&lt;mi&gt;&lt;/mi&gt;&lt;mn&gt;40&lt;/mn&gt;&lt;/msup&gt;&lt;mtext&gt;Ar&lt;/mtext&gt;&lt;msup&gt;&lt;mi&gt;&lt;/mi&gt;&lt;mn&gt;39&lt;/mn&gt;&lt;/msup&gt;&lt;mtext&gt;Ar&lt;/mtext&gt;&lt;/math&gt;\"></span><span>&nbsp;biotite cooling ages increase southward through the East Humboldt Range, compatible with northward extrapolation of a previously recognized pattern of WNW-younging biotite cooling ages from the Ruby Mountains. A simple model involving the propagation of footwall uplift in the direction of tectonic transport beneath an initially listric normal fault can explain the principle features of the Oligocène to Miocene thermochronologic data set for the RM-EHR.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(94)90067-1","issn":"00401951","usgsCitation":"McGrew, A.J., and Snee, L., 1994, 40Ar/39Ar thermochronologic constraints on the tectonothermal evolution of the northern East Humboldt Range metamorphic core complex, Nevada: Tectonophysics, v. 238, no. 1-4, p. 425-450, https://doi.org/10.1016/0040-1951(94)90067-1.","productDescription":"26 p.","startPage":"425","endPage":"450","costCenters":[],"links":[{"id":228938,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"northern East Humboldt Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.76321666030387,\n              42.01049898902764\n            ],\n            [\n              -117.76321666030387,\n              40.617836167615025\n            ],\n            [\n              -114.58273019606733,\n              40.617836167615025\n            ],\n            [\n              -114.58273019606733,\n              42.01049898902764\n            ],\n            [\n              -117.76321666030387,\n              42.01049898902764\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"238","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e268e4b0c8380cd45b61","contributors":{"authors":[{"text":"McGrew, Allen J.","contributorId":147302,"corporation":false,"usgs":false,"family":"McGrew","given":"Allen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":377034,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snee, Lawrence W.","contributorId":81534,"corporation":false,"usgs":true,"family":"Snee","given":"Lawrence W.","affiliations":[],"preferred":false,"id":377035,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33086,"text":"wri944026 - 1994 - Multiple flow processes accompanying a dam-break flood in a small upland watershed, Centralia, Washington","interactions":[],"lastModifiedDate":"2014-06-09T13:56:56","indexId":"wri944026","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4026","title":"Multiple flow processes accompanying a dam-break flood in a small upland watershed, Centralia, Washington","docAbstract":"On October 5, 1991, following 35 consecutive days of dry weather, a 105-meter long, 37-meter wide, 5.2-meter deep concrete-lined watersupply reservoir on a hillside in the eastern edge of Centralia, Washington, suddenly failed, sending 13,250 cubic meters of water rushing down a small, steep tributary channel into the city. Two houses were destroyed, several others damaged, mud and debris were deposited in streets, on lawns, and in basements over four city blocks, and 400 people were evacuated. The cause of failure is believed to have been a sliding failure along a weak seam or joint in the siltstone bedrock beneath the reservoir, possibly triggered by increased seepage into the rock foundation through continued deterioration of concrete panel seams, and a slight rise (0.6 meters) in the pool elevation. A second adjacent reservoir containing 18,900 cubic meters of water also drained, but far more slowly, when a 41-cm diameter connecting pipe was broken by the landslide. The maximum discharge resulting from the dam-failure was about 71 cubic meters per second. A reconstructed hydrograph based on the known reservoir volume and calculated peak discharge indicates the flood duration was about 6.2 minutes. Sedimentologic evidence, high-water mark distribution, and landforms preserved in the valley floor indicate that the dam failure flood consisted of two flow phases: an initial debris flow that deposited coarse bouldery sediment along the slope-area reach as it lost volume, followed soon after by a water-flood that achieved a stage about one-half meter higher than the debris flow. The Centralia dam failure is one of three constructed dams destroyed by rapid foundation failure that defines the upper limits of an envelope curve of peak flood discharge as a function of potential energy for failed constructed dams worldwide.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944026","usgsCitation":"Costa, J.E., 1994, Multiple flow processes accompanying a dam-break flood in a small upland watershed, Centralia, Washington: U.S. Geological Survey Water-Resources Investigations Report 94-4026, iv, 24 p., https://doi.org/10.3133/wri944026.","productDescription":"iv, 24 p.","numberOfPages":"24","onlineOnly":"Y","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":163267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri944026.jpg"},{"id":3287,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1994/4026/","linkFileType":{"id":5,"text":"html"}},{"id":288177,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4026/pdf/WRI-94-4026.pdf"}],"country":"United States","state":"Washington","city":"Centralia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.0,45.708333 ], [ -123.0,45.75 ], [ -122.916667,45.75 ], [ -122.916667,45.708333 ], [ -123.0,45.708333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b489a","contributors":{"authors":[{"text":"Costa, John E.","contributorId":105743,"corporation":false,"usgs":true,"family":"Costa","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":209859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6820,"text":"fs07094 - 1994 - Nitrate in ground water in the western Lake Michigan drainage basin, Wisconsin and Michigan","interactions":[],"lastModifiedDate":"2015-09-29T10:07:35","indexId":"fs07094","displayToPublicDate":"1996-10-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"070-94","title":"Nitrate in ground water in the western Lake Michigan drainage basin, Wisconsin and Michigan","docAbstract":"<p>In 1991, the U.S. Geological Survey began the nationwide implementation of the National Water-Quality Assessment (NAWQA) Program. The long-term goals of the NAWQA Program are to describe the status and trends in the quality of a large, representative part of the Nation's surface- and ground-water resources and to provide a sound, scientific understanding of the primary natural and human factors that affect the quality of these resources. The program (as currently planned) consists of 60 study-unit investigations that include parts of most major river basins and aquifer systems in the country. The Western Lake Michigan Drainage Basin encompasses a 20,000-square-mile area in eastern Wisconsin and the Upper Peninsula of Michigan that drains to Lake Michigan and Green Bay (fig. 1).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs07094","usgsCitation":"Saad, D.A., 1994, Nitrate in ground water in the western Lake Michigan drainage basin, Wisconsin and Michigan: U.S. Geological Survey Fact Sheet 070-94, 2 p., https://doi.org/10.3133/fs07094.","productDescription":"2 p.","numberOfPages":"2","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":34158,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1994/0070/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":836,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wi.water.usgs.gov/pubs/FS-070-94/","linkFileType":{"id":5,"text":"html"}},{"id":118350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1994/0070/report-thumb.jpg"}],"country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.68212890625,\n              45.75219336063106\n            ],\n            [\n              -86.748046875,\n              46.255846818480336\n            ],\n            [\n              -87.69287109375,\n              46.65697731621612\n            ],\n            [\n              -88.099365234375,\n              46.7774927637683\n            ],\n            [\n              -88.29711914062499,\n              46.807579571992385\n            ],\n            [\n              -88.96728515624999,\n              45.29034662473615\n            ],\n            [\n              -89.912109375,\n              43.810747313446996\n            ],\n            [\n              -89.84619140625,\n              43.02071359427862\n            ],\n            [\n              -89.417724609375,\n              42.512601715736665\n            ],\n            [\n              -87.78076171875,\n              42.50450285299051\n            ],\n            [\n              -87.56103515625,\n              42.53689200787317\n            ],\n            [\n              -86.561279296875,\n              45.49094569262732\n            ],\n            [\n              -86.68212890625,\n              45.75219336063106\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697415","contributors":{"authors":[{"text":"Saad, David A. dasaad@usgs.gov","contributorId":121,"corporation":false,"usgs":true,"family":"Saad","given":"David","email":"dasaad@usgs.gov","middleInitial":"A.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31722,"text":"ofr9346 - 1994 - Physical characteristics of stream subbasins in the Lac qui Parle River basin, southwestern Minnesota and eastern South Dakota","interactions":[],"lastModifiedDate":"2018-03-19T09:57:27","indexId":"ofr9346","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-46","title":"Physical characteristics of stream subbasins in the Lac qui Parle River basin, southwestern Minnesota and eastern South Dakota","docAbstract":"<p>Data describing the physical characteristics of stream subbasins upstream from selected points on streams in the Lac qui Parle River basin, located in southwestern Minnesota and eastern South Dakota, are presented in this report. The physical charac- teristics are the drainage area of the subbasin, the percentage area of the subbasin covered only by lakes, the percentage area of the subbasin covered by both lakes and wetlands, the main-channel length. and the main-channel slope. The points on the stream include outlets of subbasins of at least 5 square miles, outfalls of sewage treatment plants, and locations of U.S. Geological Survey low-flow, high-flow, and continuous-record gaging stations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr9346","collaboration":"Prepared in cooperation with Minnesota Department of Transportation and U.S. Army Corps of Engineers","usgsCitation":"Lorenz, D., Sanocki, C., and Winterstein, T.A., 1994, Physical characteristics of stream subbasins in the Lac qui Parle River basin, southwestern Minnesota and eastern South Dakota: U.S. Geological Survey Open-File Report 93-46, Document: 12 p.; Plate: 24.58 x 27.92 inches, https://doi.org/10.3133/ofr9346.","productDescription":"Document: 12 p.; Plate: 24.58 x 27.92 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":59946,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1993/0046/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59947,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0046/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0046/report-thumb.jpg"}],"country":"United States","state":"Minnesota, South Dakota","otherGeospatial":"Lac qui Parle River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.60140991210938,\n              44.883120442385646\n            ],\n            [\n              -96.60209655761719,\n              44.8709561282265\n            ],\n            [\n              -96.60552978515625,\n              44.8490538825394\n            ],\n            [\n              -96.62269592285156,\n              44.84954068962715\n            ],\n            [\n              -96.64878845214844,\n              44.86365630540611\n            ],\n            [\n              -96.67213439941406,\n              44.859762688042736\n            ],\n            [\n              -96.68655395507811,\n              44.84954068962715\n            ],\n            [\n              -96.70783996582031,\n              44.836395454104796\n            ],\n            [\n              -96.70921325683592,\n              44.82860426955568\n            ],\n            [\n              -96.69479370117188,\n              44.82227315654819\n            ],\n            [\n              -96.6851806640625,\n              44.81350585216505\n            ],\n            [\n              -96.6851806640625,\n              44.80376283939001\n            ],\n            [\n              -96.68380737304688,\n              44.79158175909386\n            ],\n            [\n              -96.66664123535156,\n              44.7832971556697\n            ],\n            [\n              -96.66664123535156,\n              44.77647364827334\n            ],\n            [\n              -96.65565490722656,\n              44.762336674810996\n            ],\n            [\n              -96.64672851562499,\n              44.76038647589176\n            ],\n            [\n              -96.624755859375,\n              44.761361583580005\n            ],\n            [\n              -96.61308288574219,\n              44.76087403179304\n            ],\n            [\n              -96.61376953125,\n              44.75599828763615\n            ],\n            [\n              -96.61239624023438,\n              44.74331942733374\n            ],\n            [\n              -96.60758972167967,\n              44.733564565295495\n            ],\n            [\n              -96.62338256835936,\n              44.73014997478245\n            ],\n            [\n              -96.63986206054686,\n              44.724295922018655\n            ],\n            [\n              -96.65634155273438,\n              44.715513732021336\n            ],\n            [\n              -96.67076110839842,\n              44.706730209005684\n            ],\n            [\n              -96.67694091796875,\n              44.69404054463804\n            ],\n            [\n              -96.6741943359375,\n              44.67890692528533\n            ],\n            [\n              -96.66938781738281,\n              44.65888542068506\n            ],\n            [\n              -96.67900085449219,\n              44.65204722540161\n            ],\n            [\n              -96.69136047363281,\n              44.642276976185045\n            ],\n            [\n              -96.70303344726562,\n              44.63592543171159\n            ],\n            [\n              -96.6851806640625,\n              44.61491152351938\n            ],\n            [\n              -96.67762756347656,\n              44.600735057768546\n            ],\n            [\n              -96.65977478027344,\n              44.58851118961441\n            ],\n            [\n              -96.6522216796875,\n              44.574817404670306\n            ],\n            [\n              -96.63917541503905,\n              44.56063115575429\n            ],\n            [\n              -96.63299560546875,\n              44.55133484083592\n            ],\n            [\n              -96.61445617675781,\n              44.53812173329457\n            ],\n            [\n              -96.60827636718749,\n              44.5278427984555\n            ],\n            [\n              -96.60415649414062,\n              44.520989167323734\n            ],\n            [\n              -96.591796875,\n              44.5058104003897\n            ],\n            [\n              -96.58149719238281,\n              44.49258696288604\n            ],\n            [\n              -96.56707763671875,\n              44.482789890501586\n            ],\n            [\n              -96.55815124511719,\n              44.47152122299265\n            ],\n            [\n              -96.54373168945312,\n              44.46711115202032\n            ],\n            [\n              -96.52587890625,\n              44.46368086644984\n            ],\n            [\n              -96.50321960449219,\n              44.459270203098846\n            ],\n            [\n              -96.48124694824219,\n              44.457309801319305\n            ],\n            [\n              -96.46957397460938,\n              44.45534933372025\n            ],\n            [\n              -96.45034790039062,\n              44.46172061276446\n            ],\n            [\n              -96.42837524414061,\n              44.46809119658819\n            ],\n            [\n              -96.40983581542969,\n              44.473481147578276\n            ],\n            [\n              -96.38511657714844,\n              44.481320187718026\n            ],\n            [\n              -96.3720703125,\n              44.48719877670763\n            ],\n            [\n              -96.37413024902342,\n              44.49748488200713\n            ],\n            [\n              -96.35353088378906,\n              44.49944393446856\n            ],\n            [\n              -96.34185791015625,\n              44.50042343601631\n            ],\n            [\n              -96.34735107421875,\n              44.51021754644924\n            ],\n            [\n              -96.3507843017578,\n              44.51903083890047\n            ],\n            [\n              -96.35284423828125,\n              44.536653425107495\n            ],\n            [\n              -96.34872436523438,\n              44.54252643570382\n            ],\n            [\n              -96.33636474609375,\n              44.548888195335756\n            ],\n            [\n              -96.32057189941406,\n              44.543994595789485\n            ],\n            [\n              -96.31370544433594,\n              44.54154764174371\n            ],\n            [\n              -96.30958557128906,\n              44.54105823859276\n            ],\n            [\n              -96.30958557128906,\n              44.55084551996381\n            ],\n            [\n              -96.2958526611328,\n              44.561120394347185\n            ],\n            [\n              -96.30477905273438,\n              44.57188260255312\n            ],\n            [\n              -96.31645202636719,\n              44.581664700316146\n            ],\n            [\n              -96.31919860839842,\n              44.589000193709055\n            ],\n            [\n              -96.31164550781249,\n              44.59780156391225\n            ],\n            [\n              -96.29722595214844,\n              44.6036684035188\n            ],\n            [\n              -96.29379272460938,\n              44.61491152351938\n            ],\n            [\n              -96.28829956054686,\n              44.62468638055057\n            ],\n            [\n              -96.28555297851562,\n              44.63592543171159\n            ],\n            [\n              -96.27937316894531,\n              44.65107027453459\n            ],\n            [\n              -96.26564025878905,\n              44.65986223989897\n            ],\n            [\n              -96.24984741210936,\n              44.66914120165374\n            ],\n            [\n              -96.23680114746094,\n              44.67890692528533\n            ],\n            [\n              -96.23199462890625,\n              44.68574195264856\n            ],\n            [\n              -96.22718811035156,\n              44.69501677140782\n            ],\n            [\n              -96.1962890625,\n              44.700873786431515\n            ],\n            [\n              -96.17980957031249,\n              44.708194222078845\n            ],\n            [\n              -96.1688232421875,\n              44.725759490752225\n            ],\n            [\n              -96.15303039550781,\n              44.733564565295495\n            ],\n            [\n              -96.141357421875,\n              44.74185630294231\n            ],\n            [\n              -96.11869812011719,\n              44.74234401518707\n            ],\n            [\n              -96.10359191894531,\n              44.745757885700236\n            ],\n            [\n              -96.10702514648438,\n              44.75404787477275\n            ],\n            [\n              -96.11114501953125,\n              44.76184913125266\n            ],\n            [\n              -96.12487792968749,\n              44.77939810733011\n            ],\n            [\n              -96.1358642578125,\n              44.787195940691554\n            ],\n            [\n              -96.11732482910155,\n              44.790607161582656\n            ],\n            [\n              -96.10084533691405,\n              44.79255634014767\n            ],\n            [\n              -96.09260559082031,\n              44.782809789027425\n            ],\n            [\n              -96.08505249023438,\n              44.77842330410185\n            ],\n            [\n              -96.07681274414062,\n              44.78475923091046\n            ],\n            [\n              -96.05552673339844,\n              44.78768327030475\n            ],\n            [\n              -96.04522705078125,\n              44.78183504339988\n            ],\n            [\n              -96.04454040527344,\n              44.77354904110061\n            ],\n            [\n              -96.03355407714844,\n              44.766724381691816\n            ],\n            [\n              -96.00677490234375,\n              44.75404787477275\n            ],\n            [\n              -95.99578857421875,\n              44.74380712723563\n            ],\n            [\n              -95.99235534667967,\n              44.72771085813059\n            ],\n            [\n              -95.97793579101562,\n              44.73454012555639\n            ],\n            [\n              -95.96694946289062,\n              44.750634493861064\n            ],\n            [\n              -95.95458984375,\n              44.762336674810996\n            ],\n            [\n              -95.94154357910156,\n              44.77306159217168\n            ],\n            [\n              -95.94085693359375,\n              44.79158175909386\n            ],\n            [\n              -95.92781066894531,\n              44.810095984897416\n            ],\n            [\n              -95.9271240234375,\n              44.824708282300236\n            ],\n            [\n              -95.91339111328125,\n              44.861709529639704\n            ],\n            [\n              -95.88729858398438,\n              44.89576860124879\n            ],\n            [\n              -95.8721923828125,\n              44.90160527494205\n            ],\n            [\n              -95.86395263671875,\n              44.92883525162427\n            ],\n            [\n              -95.85365295410156,\n              44.9439034403902\n            ],\n            [\n              -95.85365295410156,\n              44.95410867661361\n            ],\n            [\n              -95.86669921875,\n              44.97597092998747\n            ],\n            [\n              -95.86669921875,\n              44.99539704952344\n            ],\n            [\n              -95.86395263671875,\n              45.00996231899567\n            ],\n            [\n              -95.88180541992188,\n              45.026465147868635\n            ],\n            [\n              -95.89622497558594,\n              45.02792105147572\n            ],\n            [\n              -95.90858459472656,\n              45.03228854011639\n            ],\n            [\n              -95.93673706054688,\n              45.04635929200553\n            ],\n            [\n              -95.94566345214842,\n              45.05751639340642\n            ],\n            [\n              -95.9607696533203,\n              45.07158094070473\n            ],\n            [\n              -95.97793579101562,\n              45.09048987614683\n            ],\n            [\n              -96.01364135742188,\n              45.08515722028692\n            ],\n            [\n              -96.04179382324219,\n              45.089520339384066\n            ],\n            [\n              -96.06239318847655,\n              45.08273312122762\n            ],\n            [\n              -96.09054565429688,\n              45.0555761842945\n            ],\n            [\n              -96.11320495605469,\n              45.06382161837364\n            ],\n            [\n              -96.1358642578125,\n              45.089035564831036\n            ],\n            [\n              -96.15715026855469,\n              45.09097463835656\n            ],\n            [\n              -96.18324279785156,\n              45.08176345280282\n            ],\n            [\n              -96.19010925292969,\n              45.088550786163566\n            ],\n            [\n              -96.19422912597656,\n              45.093398387688694\n            ],\n            [\n              -96.21070861816405,\n              45.0938831252118\n            ],\n            [\n              -96.23954772949219,\n              45.097760877277096\n            ],\n            [\n              -96.28555297851562,\n              45.10551559143666\n            ],\n            [\n              -96.30409240722655,\n              45.1069694830803\n            ],\n            [\n              -96.30821228027344,\n              45.090005109822684\n            ],\n            [\n              -96.31919860839842,\n              45.086126831109596\n            ],\n            [\n              -96.3336181640625,\n              45.09145939645188\n            ],\n            [\n              -96.35284423828125,\n              45.10260769705975\n            ],\n            [\n              -96.36795043945312,\n              45.12053735276008\n            ],\n            [\n              -96.37344360351562,\n              45.10939255353115\n            ],\n            [\n              -96.39541625976562,\n              45.104061662763144\n            ],\n            [\n              -96.39610290527344,\n              45.09582203415993\n            ],\n            [\n              -96.40159606933594,\n              45.07594509664094\n            ],\n            [\n              -96.40159606933594,\n              45.06285162902221\n            ],\n            [\n              -96.40846252441406,\n              45.05363590935139\n            ],\n            [\n              -96.43730163574219,\n              45.044903857446165\n            ],\n            [\n              -96.45858764648438,\n              45.042478050891546\n            ],\n            [\n              -96.50390625,\n              45.034229539203075\n            ],\n            [\n              -96.53617858886719,\n              45.02695045318546\n            ],\n            [\n              -96.56227111816406,\n              45.02597983843737\n            ],\n            [\n              -96.57257080078125,\n              45.02064116313934\n            ],\n            [\n              -96.58493041992186,\n              45.00462215014995\n            ],\n            [\n              -96.60964965820312,\n              44.987627391684704\n            ],\n            [\n              -96.62544250488281,\n              44.97451370563986\n            ],\n            [\n              -96.64672851562499,\n              44.96285457777543\n            ],\n            [\n              -96.65428161621094,\n              44.94681940731859\n            ],\n            [\n              -96.65565490722656,\n              44.932724194996155\n            ],\n            [\n              -96.65428161621094,\n              44.92154277306035\n            ],\n            [\n              -96.63986206054686,\n              44.90549606158295\n            ],\n            [\n              -96.62406921386717,\n              44.89430934025077\n            ],\n            [\n              -96.60140991210938,\n              44.883120442385646\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685baf","contributors":{"authors":[{"text":"Lorenz, D. L.","contributorId":10776,"corporation":false,"usgs":true,"family":"Lorenz","given":"D. L.","affiliations":[],"preferred":false,"id":206810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanocki, C. A.","contributorId":92305,"corporation":false,"usgs":true,"family":"Sanocki","given":"C. A.","affiliations":[],"preferred":false,"id":206812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winterstein, Thomas A.","contributorId":25971,"corporation":false,"usgs":true,"family":"Winterstein","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":206811,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20230,"text":"ofr94116 - 1994 - Storm-tide elevations produced by Hurricane Andrew along the southern Florida coasts, August 24, 1992","interactions":[],"lastModifiedDate":"2019-12-27T12:19:18","indexId":"ofr94116","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-116","title":"Storm-tide elevations produced by Hurricane Andrew along the southern Florida coasts, August 24, 1992","docAbstract":"<p>On August 24, 1992, Hurricane Andrew crossed southern peninsular Florida. The combined effects of storm surge from the hurricane and astronomical tide, referred to as storm tide, caused flooding over a large part of southern Florida. Subsequent to the flooding, many high-water marks were identified, described, and surveyed along the south- eastern coast of Florida (Miami to Key Largo) and at selected areas along the southwestern coast of Florida (Flamingo to Goodland). Descriptions of these 336 high-water makrs are presented in tabular form in this report and their locations are plotted on nineteen 7.5-minute topographic quadrangle maps. For the southeastern coast, north-south profiles of the high-water makrs along the outher and inner barrier islands and the western shoreline of Biscayne Bay are presented. Average storm-tide elevations (relative to sea level) ranged from 4 to 6 feet in northern Biscayne Bay, were as much as 17 feet on the western shoreline near the center of the bay and ranged from 3 to 6 feet in southern Biscayne Bay and Barnes Sound. Storm-tide elevations along the southwestern coast ranged from 4 to 5 feet at Flamingo and 5 to 7 feet at Goodland in the Ten Thousand Islands area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tallahassee, FL","doi":"10.3133/ofr94116","collaboration":"Prepared in cooperation with the Federal Emergency Management Agency","usgsCitation":"Murray, M.H., 1994, Storm-tide elevations produced by Hurricane Andrew along the southern Florida coasts, August 24, 1992: U.S. Geological Survey Open-File Report 94-116, Report: iv, 27 p.; 19 Plates: 24.40 x 28.27 inches or smaller, https://doi.org/10.3133/ofr94116.","productDescription":"Report: iv, 27 p.; 19 Plates: 24.40 x 28.27 inches or smaller","numberOfPages":"31","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":321984,"rank":306,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"}},{"id":321985,"rank":307,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"}},{"id":321986,"rank":308,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"}},{"id":49773,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0116/report-thumb.jpg"},{"id":321980,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":321979,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":321981,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":321982,"rank":304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":321983,"rank":305,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"}},{"id":321987,"rank":309,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-9.pdf","text":"Plate 9","linkFileType":{"id":1,"text":"pdf"}},{"id":321988,"rank":310,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-10.pdf","text":"Plate 10","linkFileType":{"id":1,"text":"pdf"}},{"id":321996,"rank":318,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-18.pdf","text":"Plate 18","linkFileType":{"id":1,"text":"pdf"}},{"id":321989,"rank":311,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-11.pdf","text":"Plate 11","linkFileType":{"id":1,"text":"pdf"}},{"id":321997,"rank":319,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-19.pdf","text":"Plate 19","linkFileType":{"id":1,"text":"pdf"}},{"id":321990,"rank":312,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-12.pdf","text":"Plate 12","linkFileType":{"id":1,"text":"pdf"}},{"id":321991,"rank":313,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-13.pdf","text":"Plate 13","linkFileType":{"id":1,"text":"pdf"}},{"id":321992,"rank":314,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-14.pdf","text":"Plate 14","linkFileType":{"id":1,"text":"pdf"}},{"id":321993,"rank":315,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-15.pdf","text":"Plate 15","linkFileType":{"id":1,"text":"pdf"}},{"id":321994,"rank":316,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-16.pdf","text":"Plate 16","linkFileType":{"id":1,"text":"pdf"}},{"id":321995,"rank":317,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0116/plate-17.pdf","text":"Plate 17","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Collier County, Dade County, Monroe County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.97448730468749,\n              25.055745117015316\n            ],\n            [\n              -79.94750976562499,\n              25.055745117015316\n            ],\n            [\n              -79.94750976562499,\n              26.342652809380578\n            ],\n            [\n              -81.97448730468749,\n              26.342652809380578\n            ],\n            [\n              -81.97448730468749,\n              25.055745117015316\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1720","contributors":{"authors":[{"text":"Murray, Mitchell H.","contributorId":23131,"corporation":false,"usgs":true,"family":"Murray","given":"Mitchell","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":182289,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29562,"text":"wri944213 - 1994 - Sources of trends in water-quality data for selected streams in Texas, 1975-89 water years","interactions":[],"lastModifiedDate":"2016-08-16T14:32:49","indexId":"wri944213","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4213","title":"Sources of trends in water-quality data for selected streams in Texas, 1975-89 water years","docAbstract":"<p>Sources of trends in water-quality data for selected streams in Texas for the 1975-89 water years were investigated in this study. The investigation of sources was confined to distinct geographic patterns in the trend indicators for one constituent or for a group of related constituents.</p>\n<p>The probable source of trend patterns in nutrients and measures of oxygen in the Trinity River Basin was changes in the wastewater treatment facilities in the Dallas-Fort Worth metropolitan area. A pattern of increased concentrations of inorganic constituents in the upper Colorado River Basin resulted from emergency releases of water from the Natural Darn Lake, a salinity control structure. Trend patterns in inorganic constituents in the Rio Grande Basin were a result of increasing concentrations in the Pecos River and, to a lesser extent, the Rio Grande above the Amistad Reservoir, combined with the effects of reservoir regulation. A pattern of increasing concentrations of organic plus ammonia nitrogen and ammonia nitrogen was detected for the 1975-86 water years for stations with low concentrations (generally less than 5 milligrams per liter) of these nitrogen species. The trends were no longer evident when the period of trend analysis was extended to the 1989 water year. A positive bias in the data caused by the addition of mercuric chloride tablets to preserve nutrient samples during 1980-86 was the probable source of this trend pattern. A pattern of increasing concentrations in dissolved sulfate in the eastern part of the State was a result of a positive bias in the analytical results of a turbidimetric method of sulfate analysis. The source of a statewide pattern of increased pH in streams could not be identified.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri944213","usgsCitation":"Schertz, T., Wells, F., and Ohe, D., 1994, Sources of trends in water-quality data for selected streams in Texas, 1975-89 water years: U.S. Geological Survey Water-Resources Investigations Report 94-4213, v, 49 p., https://doi.org/10.3133/wri944213.","productDescription":"v, 49 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":160468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4213/report-thumb.jpg"},{"id":58390,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4213/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-97.240849,26.411504],[-97.276425,26.521729],[-97.31073,26.556558],[-97.345822,26.700589],[-97.370438,26.723896],[-97.368343,26.795649],[-97.387459,26.820789],[-97.390078,27.156512],[-97.359963,27.304732],[-97.361796,27.359988],[-97.317277,27.46369],[-97.236882,27.598293],[-97.231383,27.632336],[-97.214099,27.631551],[-97.200743,27.650144],[-97.203474,27.684533],[-97.103326,27.789068],[-97.098874,27.82285],[-97.134489,27.825206],[-97.056713,27.842294],[-96.985745,27.954048],[-96.967807,28.020041],[-96.952618,28.01644],[-96.906004,28.076147],[-96.886233,28.084396],[-96.879424,28.131402],[-96.84538,28.108881],[-96.83003,28.111842],[-96.81042,28.126034],[-96.816443,28.174808],[-96.791958,28.188687],[-96.703838,28.198246],[-96.702659,28.211208],[-96.662462,28.227314],[-96.651856,28.251275],[-96.592934,28.296972],[-96.450998,28.337039],[-96.403206,28.371475],[-96.397846,28.343513],[-96.4137,28.327343],[-96.547774,28.270798],[-96.694666,28.18212],[-96.849624,28.064939],[-96.966996,27.950531],[-97.166682,27.676583],[-97.30447,27.407734],[-97.350398,27.268105],[-97.370941,27.161166],[-97.37913,27.047996],[-97.370731,26.909706],[-97.333028,26.736479],[-97.194644,26.306513],[-97.154271,26.066841],[-97.169842,26.077853],[-97.194458,26.27164],[-97.240849,26.411504]]],[[[-94.886539,29.510724],[-94.894747,29.52697],[-94.87675,29.507922],[-94.886539,29.510724]]],[[[-97.868235,26.056656],[-97.88653,26.066339],[-97.967358,26.051718],[-97.981335,26.067182],[-98.028759,26.06647],[-98.039239,26.041275],[-98.070021,26.047992],[-98.084755,26.070808],[-98.091038,26.059169],[-98.105505,26.067537],[-98.146622,26.049412],[-98.177897,26.074672],[-98.197046,26.056153],[-98.220673,26.076467],[-98.248806,26.073101],[-98.264514,26.085507],[-98.277218,26.098802],[-98.265698,26.12037],[-98.296195,26.120321],[-98.302979,26.11005],[-98.323828,26.121249],[-98.336837,26.166432],[-98.354645,26.15304],[-98.386694,26.157872],[-98.404433,26.182564],[-98.442536,26.199151],[-98.450976,26.219904],[-98.496684,26.212853],[-98.543852,26.234492],[-98.576188,26.235221],[-98.599154,26.257612],[-98.669397,26.23632],[-98.681167,26.26271],[-98.745272,26.303096],[-98.755242,26.3251],[-98.789822,26.331575],[-98.807348,26.369421],[-98.890965,26.357569],[-98.921277,26.381426],[-98.950186,26.380303],[-98.967587,26.398266],[-99.008003,26.395459],[-99.032316,26.412082],[-99.082002,26.39651],[-99.110855,26.426278],[-99.091635,26.476977],[-99.127782,26.525199],[-99.166742,26.536079],[-99.178064,26.620547],[-99.209948,26.693938],[-99.208907,26.724761],[-99.240023,26.745851],[-99.242444,26.788262],[-99.268613,26.843213],[-99.295146,26.86544],[-99.316753,26.865831],[-99.3289,26.879761],[-99.324684,26.915973],[-99.379149,26.93449],[-99.393748,26.96073],[-99.377312,26.973819],[-99.415476,27.01724],[-99.42938,27.010833],[-99.446524,27.023008],[-99.452316,27.062669],[-99.429209,27.090982],[-99.442123,27.106839],[-99.426348,27.176262],[-99.441549,27.24992],[-99.463309,27.268437],[-99.492407,27.264118],[-99.494604,27.303542],[-99.536443,27.312538],[-99.504837,27.338289],[-99.487521,27.412396],[-99.495104,27.451518],[-99.480419,27.481596],[-99.497519,27.500496],[-99.52582,27.496696],[-99.515978,27.572131],[-99.55495,27.614454],[-99.580006,27.602251],[-99.578099,27.619196],[-99.594038,27.638573],[-99.638929,27.626758],[-99.665948,27.635968],[-99.668942,27.659974],[-99.711511,27.658365],[-99.77074,27.732134],[-99.796342,27.735586],[-99.813086,27.773952],[-99.835127,27.762881],[-99.850877,27.793974],[-99.877677,27.799427],[-99.876003,27.837968],[-99.904385,27.875284],[-99.895828,27.904178],[-99.937142,27.940537],[-99.931812,27.980967],[-99.991447,27.99456],[-100.017914,28.064787],[-100.053123,28.08473],[-100.083393,28.144035],[-100.208059,28.190383],[-100.22363,28.235224],[-100.2462,28.234092],[-100.289384,28.273491],[-100.286471,28.312296],[-100.341869,28.384953],[-100.349586,28.402604],[-100.337797,28.44296],[-100.368288,28.477196],[-100.333814,28.499252],[-100.38886,28.515748],[-100.411414,28.551899],[-100.398385,28.584884],[-100.44732,28.609325],[-100.445529,28.637144],[-100.495863,28.658569],[-100.510055,28.690723],[-100.507613,28.740599],[-100.533017,28.76328],[-100.53583,28.805888],[-100.547324,28.825817],[-100.57051,28.826317],[-100.602054,28.901944],[-100.640568,28.914212],[-100.651512,28.943432],[-100.645894,28.986421],[-100.674656,29.099777],[-100.772649,29.168492],[-100.767059,29.195287],[-100.785521,29.228137],[-100.795681,29.22773],[-100.797671,29.246943],[-100.876049,29.279585],[-100.886842,29.307848],[-100.948972,29.347246],[-101.004207,29.364772],[-101.060151,29.458661],[-101.151877,29.477005],[-101.173821,29.514566],[-101.254895,29.520342],[-101.242023,29.592512],[-101.259127,29.607284],[-101.307332,29.587847],[-101.311219,29.648491],[-101.361756,29.657821],[-101.415402,29.756561],[-101.441059,29.753451],[-101.475269,29.780663],[-101.522695,29.759671],[-101.546797,29.796991],[-101.582562,29.771334],[-101.625958,29.771063],[-101.646418,29.754304],[-101.662453,29.77128],[-101.706636,29.762737],[-101.852604,29.801895],[-101.922585,29.790161],[-101.974548,29.810276],[-101.987539,29.801057],[-102.034759,29.804028],[-102.050044,29.78507],[-102.115682,29.79239],[-102.159601,29.814356],[-102.181894,29.846034],[-102.227553,29.843534],[-102.315389,29.87992],[-102.364542,29.845387],[-102.386678,29.76688],[-102.508313,29.783219],[-102.513381,29.76576],[-102.539417,29.751629],[-102.559343,29.760377],[-102.630151,29.734315],[-102.670971,29.741954],[-102.698347,29.695591],[-102.693466,29.676507],[-102.742031,29.632142],[-102.739991,29.599041],[-102.768341,29.594734],[-102.771429,29.548546],[-102.808692,29.522319],[-102.807327,29.494009],[-102.832539,29.433109],[-102.824564,29.399558],[-102.843021,29.357988],[-102.879534,29.353327],[-102.888328,29.291947],[-102.906296,29.260011],[-102.871347,29.241625],[-102.866846,29.225015],[-102.890064,29.208814],[-102.915866,29.215878],[-102.917805,29.190697],[-102.944911,29.18882],[-102.953475,29.176308],[-102.989432,29.183174],[-103.015028,29.12577],[-103.035683,29.103029],[-103.074407,29.088534],[-103.100266,29.0577],[-103.113922,28.988547],[-103.156646,28.972831],[-103.227801,28.991532],[-103.239109,28.981651],[-103.260308,28.989731],[-103.28119,28.982138],[-103.341463,29.041224],[-103.355428,29.021529],[-103.427754,29.042334],[-103.471265,29.073115],[-103.503236,29.11911],[-103.524613,29.120998],[-103.523384,29.133389],[-103.558679,29.154962],[-103.645635,29.159286],[-103.71377,29.185008],[-103.816642,29.270927],[-103.975235,29.296017],[-104.038282,29.320156],[-104.106467,29.373127],[-104.166563,29.399352],[-104.233487,29.492734],[-104.318074,29.527938],[-104.334811,29.519463],[-104.381041,29.543406],[-104.399591,29.572319],[-104.507568,29.639624],[-104.539761,29.676074],[-104.565688,29.770462],[-104.679772,29.924659],[-104.679661,29.975272],[-104.706874,30.050685],[-104.685003,30.085643],[-104.695366,30.13213],[-104.687296,30.179464],[-104.713166,30.237957],[-104.733822,30.261221],[-104.749664,30.26126],[-104.761634,30.301148],[-104.809794,30.334926],[-104.824314,30.370466],[-104.859521,30.390413],[-104.85242,30.418792],[-104.876787,30.511004],[-104.924796,30.604832],[-104.967167,30.608107],[-105.002057,30.680972],[-105.062334,30.686303],[-105.113816,30.746001],[-105.152362,30.751452],[-105.195144,30.792138],[-105.255416,30.797029],[-105.287238,30.822206],[-105.314863,30.816961],[-105.360672,30.847384],[-105.394242,30.852979],[-105.399609,30.888941],[-105.533088,30.984859],[-105.55743,30.990229],[-105.60333,31.082625],[-105.64189,31.098322],[-105.646731,31.113908],[-105.709491,31.136375],[-105.742678,31.164897],[-105.773257,31.166897],[-105.779725,31.191283],[-105.869353,31.288634],[-105.938452,31.318735],[-105.953943,31.364749],[-106.004926,31.392458],[-106.080258,31.398702],[-106.203969,31.465378],[-106.246203,31.541153],[-106.280811,31.562062],[-106.303536,31.620413],[-106.378039,31.72831],[-106.451541,31.764808],[-106.484642,31.747809],[-106.542097,31.802146],[-106.602727,31.825024],[-106.605845,31.846305],[-106.635926,31.866235],[-106.629197,31.883717],[-106.645296,31.894859],[-106.614346,31.918003],[-106.623933,31.925335],[-106.614702,31.956],[-106.622819,31.952891],[-106.618745,31.966955],[-106.638186,31.97682],[-106.618486,32.000495],[-103.064423,32.000518],[-103.064625,32.999899],[-103.043531,34.018014],[-103.041924,36.500439],[-100.003762,36.499699],[-100.000381,34.560509],[-99.929334,34.576714],[-99.825325,34.497596],[-99.754248,34.421289],[-99.696462,34.381036],[-99.665992,34.374185],[-99.600026,34.374688],[-99.569696,34.418418],[-99.499875,34.409608],[-99.430995,34.373414],[-99.399603,34.375079],[-99.394956,34.442099],[-99.381011,34.456936],[-99.358795,34.455863],[-99.318363,34.408296],[-99.289922,34.414731],[-99.264167,34.405149],[-99.25898,34.391243],[-99.273958,34.38756],[-99.242945,34.372668],[-99.233274,34.344101],[-99.210716,34.336304],[-99.211648,34.292232],[-99.19457,34.272424],[-99.189511,34.214312],[-99.159016,34.20888],[-99.130609,34.219408],[-99.126567,34.203004],[-99.079535,34.211518],[-99.048792,34.198209],[-99.013075,34.203222],[-98.990852,34.221633],[-98.974132,34.203566],[-98.952513,34.21265],[-98.909349,34.177499],[-98.872922,34.166584],[-98.868116,34.149635],[-98.8579,34.159627],[-98.812954,34.158444],[-98.749291,34.124238],[-98.735471,34.135208],[-98.696518,34.133521],[-98.648073,34.164441],[-98.603978,34.160249],[-98.577136,34.148962],[-98.486328,34.062598],[-98.414426,34.085074],[-98.384381,34.146317],[-98.367494,34.156191],[-98.16912,34.114171],[-98.114506,34.154727],[-98.09066,34.12198],[-98.120208,34.072127],[-98.099096,34.048639],[-98.104022,34.036233],[-98.088203,34.005481],[-98.027672,33.993357],[-97.978243,34.005387],[-97.947572,33.991053],[-97.974173,33.942832],[-97.955511,33.938186],[-97.957155,33.914454],[-97.983552,33.904002],[-97.967777,33.88243],[-97.877387,33.850236],[-97.834333,33.857671],[-97.784657,33.890632],[-97.783717,33.91056],[-97.76377,33.914241],[-97.762768,33.934396],[-97.725289,33.941045],[-97.69311,33.983699],[-97.671772,33.99137],[-97.589598,33.953554],[-97.589254,33.903922],[-97.551541,33.897947],[-97.50096,33.919643],[-97.460376,33.903948],[-97.451469,33.87093],[-97.462857,33.841772],[-97.426493,33.819398],[-97.365507,33.823763],[-97.33294,33.87444],[-97.315913,33.865838],[-97.299245,33.880175],[-97.256625,33.863286],[-97.24618,33.900344],[-97.210921,33.916064],[-97.179609,33.89225],[-97.166629,33.847311],[-97.203514,33.821825],[-97.205431,33.801488],[-97.172192,33.737545],[-97.126102,33.716941],[-97.086195,33.743933],[-97.087999,33.808747],[-97.058623,33.818752],[-97.052209,33.841737],[-97.023899,33.844213],[-96.985567,33.886522],[-96.996183,33.941728],[-96.979415,33.956178],[-96.973807,33.935697],[-96.9163,33.957798],[-96.875281,33.860505],[-96.85609,33.84749],[-96.837413,33.871349],[-96.794276,33.868886],[-96.761588,33.824406],[-96.704457,33.835021],[-96.667187,33.91694],[-96.630117,33.895422],[-96.592948,33.895616],[-96.590112,33.880665],[-96.625399,33.856542],[-96.623155,33.841483],[-96.572937,33.819098],[-96.523863,33.818114],[-96.502286,33.77346],[-96.422643,33.776041],[-96.348306,33.686379],[-96.309964,33.710489],[-96.294867,33.764771],[-96.277269,33.769735],[-96.220521,33.74739],[-96.178059,33.760518],[-96.162757,33.788769],[-96.178964,33.810553],[-96.150765,33.816987],[-96.15163,33.831946],[-96.138905,33.839159],[-96.09936,33.83047],[-96.101349,33.845721],[-96.005296,33.845505],[-95.991487,33.866869],[-95.951609,33.857017],[-95.936132,33.886826],[-95.831948,33.835161],[-95.821666,33.856633],[-95.805149,33.861304],[-95.776255,33.845145],[-95.75431,33.853992],[-95.761916,33.883402],[-95.747335,33.895756],[-95.696962,33.885218],[-95.669978,33.905844],[-95.636978,33.906613],[-95.599678,33.934247],[-95.556915,33.92702],[-95.545197,33.880294],[-95.515302,33.891142],[-95.492028,33.874822],[-95.461499,33.883686],[-95.464211,33.873372],[-95.44737,33.86885],[-95.339122,33.868873],[-95.334523,33.885788],[-95.283445,33.877746],[-95.280351,33.896751],[-95.255747,33.902939],[-95.252906,33.933648],[-95.219358,33.961567],[-95.121184,33.931307],[-95.093929,33.895963],[-95.061065,33.895292],[-95.049025,33.86409],[-95.008376,33.866089],[-94.983303,33.851354],[-94.976208,33.859847],[-94.948716,33.818023],[-94.91945,33.810176],[-94.919614,33.786305],[-94.879218,33.764912],[-94.8693,33.745871],[-94.830804,33.740068],[-94.817427,33.752172],[-94.798634,33.744527],[-94.775064,33.755038],[-94.762961,33.731787],[-94.742576,33.727009],[-94.732384,33.700254],[-94.714865,33.707261],[-94.710725,33.691654],[-94.684792,33.684353],[-94.659167,33.692138],[-94.646113,33.6693],[-94.57962,33.677623],[-94.520725,33.616567],[-94.491503,33.625115],[-94.485875,33.637867],[-94.448637,33.642766],[-94.468086,33.599436],[-94.430039,33.591124],[-94.413155,33.569368],[-94.378076,33.577019],[-94.397398,33.562314],[-94.389515,33.546778],[-94.355945,33.54318],[-94.345513,33.567313],[-94.309582,33.551673],[-94.289129,33.582144],[-94.280849,33.577187],[-94.290901,33.558872],[-94.27909,33.557026],[-94.245932,33.589114],[-94.237975,33.577757],[-94.250197,33.556765],[-94.226392,33.552912],[-94.205634,33.567229],[-94.193248,33.556154],[-94.192483,33.570425],[-94.217408,33.57926],[-94.183913,33.594682],[-94.152626,33.575923],[-94.146048,33.581975],[-94.14852,33.565678],[-94.136864,33.571],[-94.128658,33.550952],[-94.088943,33.575322],[-94.061283,33.568805],[-94.055663,33.561887],[-94.073744,33.558285],[-94.06548,33.550909],[-94.04604,33.551321],[-94.04272,31.999265],[-94.018664,31.990843],[-93.971712,31.920384],[-93.923929,31.88985],[-93.904766,31.890599],[-93.874761,31.821661],[-93.827451,31.777741],[-93.830647,31.745811],[-93.802694,31.697783],[-93.826462,31.666919],[-93.816838,31.622509],[-93.838057,31.606795],[-93.834924,31.586211],[-93.798087,31.534044],[-93.743376,31.525196],[-93.725925,31.504092],[-93.74987,31.475276],[-93.70093,31.437784],[-93.704879,31.410881],[-93.674117,31.397681],[-93.665052,31.363886],[-93.687851,31.309835],[-93.642516,31.269508],[-93.620343,31.271025],[-93.598828,31.174679],[-93.588503,31.165581],[-93.535097,31.185614],[-93.551693,31.097258],[-93.52301,31.065241],[-93.516943,31.032584],[-93.539526,31.008498],[-93.566017,31.004567],[-93.571906,30.987614],[-93.526245,30.939411],[-93.567788,30.888302],[-93.554057,30.824941],[-93.561666,30.807739],[-93.584265,30.796663],[-93.592828,30.763986],[-93.619129,30.742002],[-93.611192,30.718053],[-93.629904,30.67994],[-93.6831,30.640763],[-93.684329,30.592586],[-93.727844,30.57407],[-93.729195,30.544842],[-93.740253,30.539569],[-93.714322,30.518562],[-93.697828,30.443838],[-93.757654,30.390423],[-93.765822,30.333318],[-93.708645,30.288317],[-93.705083,30.242752],[-93.720946,30.209852],[-93.688212,30.141376],[-93.701252,30.137376],[-93.702436,30.112721],[-93.732485,30.088914],[-93.70082,30.056274],[-93.720805,30.053043],[-93.739734,30.023987],[-93.786935,29.99058],[-93.838374,29.882855],[-93.927992,29.80964],[-93.926504,29.78956],[-93.89847,29.771577],[-93.891637,29.744618],[-93.873941,29.73777],[-93.837971,29.690619],[-93.866981,29.673085],[-94.001406,29.681486],[-94.132577,29.646217],[-94.594853,29.467903],[-94.694158,29.415632],[-94.731047,29.369141],[-94.778691,29.361483],[-94.783131,29.375642],[-94.766848,29.393489],[-94.6724,29.476843],[-94.608557,29.483345],[-94.566674,29.531988],[-94.532348,29.5178],[-94.495025,29.525031],[-94.503429,29.54325],[-94.522421,29.545672],[-94.553988,29.573882],[-94.740699,29.525858],[-94.783296,29.535314],[-94.78954,29.546494],[-94.755237,29.562782],[-94.708741,29.625226],[-94.693154,29.694453],[-94.695317,29.723052],[-94.735271,29.785433],[-94.816085,29.75671],[-94.851108,29.721373],[-94.872551,29.67125],[-94.893107,29.661336],[-94.915413,29.656614],[-94.936089,29.692704],[-94.965963,29.70033],[-95.015636,29.639457],[-94.982936,29.60167],[-95.016889,29.548303],[-94.981916,29.511141],[-94.909898,29.49691],[-94.930861,29.450504],[-94.8908,29.433432],[-94.893994,29.30817],[-94.921593,29.281556],[-94.952526,29.290122],[-95.099101,29.173529],[-95.151925,29.151162],[-95.16525,29.113566],[-95.136221,29.084537],[-94.879239,29.285839],[-94.824953,29.306005],[-94.822307,29.344254],[-94.810696,29.353435],[-94.784895,29.335535],[-94.72253,29.331446],[-95.081773,29.111222],[-95.38239,28.866348],[-95.439594,28.859022],[-95.812504,28.664942],[-96.220376,28.491966],[-96.378616,28.383909],[-96.37596,28.401682],[-96.335119,28.437795],[-96.223825,28.495067],[-96.21505,28.509679],[-95.98616,28.606319],[-95.978526,28.650594],[-95.996338,28.658736],[-96.006516,28.648049],[-96.047737,28.649067],[-96.221784,28.580364],[-96.233998,28.596649],[-96.212624,28.622604],[-96.230944,28.641433],[-96.192267,28.687744],[-96.19583,28.69894],[-96.222802,28.698431],[-96.287942,28.683164],[-96.304227,28.671459],[-96.303718,28.644996],[-96.373439,28.626675],[-96.487943,28.569677],[-96.485907,28.607845],[-96.510844,28.61497],[-96.499648,28.635835],[-96.563262,28.644487],[-96.572931,28.667897],[-96.561226,28.696395],[-96.584091,28.722798],[-96.664534,28.696904],[-96.61059,28.638889],[-96.61975,28.627693],[-96.611099,28.585962],[-96.565297,28.5824],[-96.561226,28.570695],[-96.526111,28.557972],[-96.505755,28.525911],[-96.402446,28.449066],[-96.59176,28.357462],[-96.672677,28.335579],[-96.705247,28.348811],[-96.710336,28.406827],[-96.772209,28.408074],[-96.794554,28.365688],[-96.791761,28.31217],[-96.809573,28.290287],[-96.787181,28.255681],[-96.800413,28.224128],[-96.934765,28.123873],[-96.962755,28.123365],[-97.027014,28.148408],[-97.021303,28.1841],[-97.037008,28.185528],[-97.153601,28.13318],[-97.214039,28.087494],[-97.21535,28.076575],[-97.176444,28.059892],[-97.137421,28.057037],[-97.025693,28.11216],[-97.035528,28.084688],[-97.025859,28.041939],[-97.129168,27.919801],[-97.186709,27.825453],[-97.219738,27.823939],[-97.250797,27.876035],[-97.272253,27.881427],[-97.379042,27.837867],[-97.393291,27.782905],[-97.368355,27.741683],[-97.316446,27.712676],[-97.253955,27.696696],[-97.296598,27.613947],[-97.294054,27.5941],[-97.321535,27.571199],[-97.401942,27.335574],[-97.508304,27.275014],[-97.532223,27.278577],[-97.544437,27.284175],[-97.498126,27.308602],[-97.502706,27.322343],[-97.483877,27.338628],[-97.48693,27.358984],[-97.501688,27.366618],[-97.609068,27.285193],[-97.63146,27.28621],[-97.640111,27.270943],[-97.628916,27.242953],[-97.54291,27.229213],[-97.42408,27.264073],[-97.443673,27.116235],[-97.45665,27.099695],[-97.495836,27.094098],[-97.477515,27.066108],[-97.48693,27.057711],[-97.486676,27.03481],[-97.473444,27.02285],[-97.478533,26.999186],[-97.555378,26.99028],[-97.555378,26.93888],[-97.540874,26.90631],[-97.563266,26.842188],[-97.509831,26.803511],[-97.468609,26.740915],[-97.445708,26.609362],[-97.416955,26.553637],[-97.441383,26.455418],[-97.41721,26.44982],[-97.42179,26.417249],[-97.382485,26.411326],[-97.369627,26.394603],[-97.388965,26.36585],[-97.387947,26.330481],[-97.358176,26.356435],[-97.335275,26.355672],[-97.336802,26.331753],[-97.352833,26.318521],[-97.343927,26.267376],[-97.311866,26.273737],[-97.307031,26.253126],[-97.32128,26.236078],[-97.296598,26.200709],[-97.306776,26.159487],[-97.282094,26.120301],[-97.294054,26.11394],[-97.270898,26.086459],[-97.199651,26.077044],[-97.195071,26.04193],[-97.224842,26.027426],[-97.219244,25.996128],[-97.208557,25.991802],[-97.167208,26.007069],[-97.162628,26.023482],[-97.18273,26.053126],[-97.152009,26.062108],[-97.146294,25.955606],[-97.276707,25.952147],[-97.277163,25.935438],[-97.350398,25.925241],[-97.37443,25.907444],[-97.360082,25.868874],[-97.372864,25.840117],[-97.422636,25.840378],[-97.445113,25.850026],[-97.454727,25.879337],[-97.521762,25.886458],[-97.546421,25.934077],[-97.582565,25.937857],[-97.583044,25.955443],[-97.598043,25.957556],[-97.643708,26.016943],[-97.758838,26.032131],[-97.789823,26.04246],[-97.801344,26.060017],[-97.868235,26.056656]]]]},\"properties\":{\"name\":\"Texas\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4880e4b07f02db515f0d","contributors":{"authors":[{"text":"Schertz, T. L.","contributorId":65841,"corporation":false,"usgs":true,"family":"Schertz","given":"T. L.","affiliations":[],"preferred":false,"id":201722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, F.C.","contributorId":25158,"corporation":false,"usgs":true,"family":"Wells","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":201721,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ohe, D.J.","contributorId":100896,"corporation":false,"usgs":true,"family":"Ohe","given":"D.J.","affiliations":[],"preferred":false,"id":201723,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26066,"text":"wri944039 - 1994 - Geologic history and hydrogeologic setting of the Edwards-Trinity aquifer system, west-central Texas","interactions":[],"lastModifiedDate":"2016-08-16T14:08:36","indexId":"wri944039","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4039","title":"Geologic history and hydrogeologic setting of the Edwards-Trinity aquifer system, west-central Texas","docAbstract":"<p>The Edwards-Trinity aquifer system underlies about 42,000 square miles of west-central Texas. Nearly flat-lying, mostly Comanche (Lower Cretaceous) strata of the aquifer system thin northwestward atop massive pre-Cretaceous rocks that are comparatively impermeable and structurally complex. From predominately terrigenous clastic sediments in the east and fluvialdeltaic (terrestrial) deposits in the west, the rocks of early Trinitian age grade upward into supratidal evaporitic and dolomitic strata, intertidal limestone and dolostone, and shallow-marine, openshelf, and reefal strata of late Trinitian, Fredericksburgian, and Washitan age. A thick, downfaulted remnant of mostly open-marine strata of Eaglefordian through Navarroan age composes a small, southeastern part of the aquifer system.</p>\n<p>The Trinity Group was deposited atop a rolling peneplain of pre-Cretaceous rocks during three predominately transgressive cycles of sedimentation that encroached upon the Llano uplift. The Fredericksburg and Washita Groups were deposited above the Trinity Group mostly in the lee of the Stuart City reef trend, a shelf margin ridge that sheltered depositional environments in the study area. The Washita Group subsequently was covered with thick, mostly fine-grained Gulf strata.</p>\n<p>During late Oligocene through early Miocene time, large-scale normal faulting formed the Balcones fault zone, where the Cretaceous strata were downfaulted, intensively fractured, and differentially rotated within a series of northeasttrending fault blocks. In addition to fracturing the rocks in the fault zone and extending the depth of freshwater diagenesis, the faulting vertically displaced the terrain, which steepened hydraulic gradients and maintained relatively high flow velocities near the surface. A shallow regime of dynamic ground-water flow evolved that promoted dissolution and enhanced the transmissivity of the Edwards Group in the Balcones fault zone. Cementation, recrystallization, and mineral replacement caused by deeper, comparatively sluggish ground-water circulation combined to diminish the transmissivity of the underlying Trinity Group, as well as most Cretaceous strata in the Hill Country, Edwards-Plateau, and Trans-Pecos.</p>\n<p>The Trinity, Fredericksburg, and Washita strata compose a regional aquifer system of three aquifers, whose water-transmitting characteristics generally are continuous in the lateral direction, and two hydraulically tight confining units. The aquifers are the Edwards aquifer in the Balcones fault zone, the Trinity aquifer in the Balcones fault zone and Hill Country, and the Edwards-Trinity aquifer in the Edwards Plateau and Trans-Pecos. The Navarro-Del Rio confining unit overlies the subcrop of the Edwards aquifer, and the Hammett confining unit lies within the updip, basal part of the Trinity aquifer and a small southeastern fringe of the Edwards-Trinity aquifer. The confining units are mostly calcareous mudstone, siltstone, and shale of low-energy terrigenous and openshelf marine depositional environments. The aquifers mainly result from fractures, joint cavities, and porosity caused by the dissolution of evaporites and unstable carbonate constituents.&nbsp;</p>\n<p>Because the diagenetic effects of cementation, recrystallization, and mineral replacement diminish the hydraulic conductivity of most rocks composing the Trinity and Edwards-Trinity aquifers, transmissivity values average less than 10,000 feet squared per day over more than 90 percent of the study area. However, the effects of tectonic fractures and dissolution in the Balcones fault zone cause transmissivity values to average about 750,000 feet squared per day in the Edwards aquifer, which occupies less than 10 percent of the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri944039","usgsCitation":"Barker, R., Bush, P.W., and Baker, E., 1994, Geologic history and hydrogeologic setting of the Edwards-Trinity aquifer system, west-central Texas: U.S. Geological Survey Water-Resources Investigations Report 94-4039, iv, 51 p., https://doi.org/10.3133/wri944039.","productDescription":"iv, 51 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":122736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4039/report-thumb.jpg"},{"id":54843,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Edwards-Trinity aquifer system","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c717","contributors":{"authors":[{"text":"Barker, R.A.","contributorId":28952,"corporation":false,"usgs":true,"family":"Barker","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":195741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, P. W.","contributorId":14826,"corporation":false,"usgs":true,"family":"Bush","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baker, E.T.","contributorId":11584,"corporation":false,"usgs":true,"family":"Baker","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":195739,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17501,"text":"ofr953 - 1994 - Preliminary analysis of integrated stratigraphic data from the South Venice corehole, Sarasota County, Florida","interactions":[],"lastModifiedDate":"2020-03-27T07:02:41","indexId":"ofr953","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-3","title":"Preliminary analysis of integrated stratigraphic data from the South Venice corehole, Sarasota County, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr953","usgsCitation":"Brewster-Wingard, G.L., Weedman, S., Scott, T., Edwards, L.E., and Green, R., 1994, Preliminary analysis of integrated stratigraphic data from the South Venice corehole, Sarasota County, Florida: U.S. Geological Survey Open-File Report 95-3, 129 p., https://doi.org/10.3133/ofr953.","productDescription":"129 p.","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":149121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0003/report-thumb.jpg"},{"id":46652,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida ","county":"Sarasota County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.6611328125,\n              27.19112839142226\n            ],\n            [\n              -82.2821044921875,\n              27.19112839142226\n            ],\n            [\n              -82.2821044921875,\n              27.464413510962768\n            ],\n            [\n              -82.6611328125,\n              27.464413510962768\n            ],\n            [\n              -82.6611328125,\n              27.19112839142226\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acae4b07f02db67cd65","contributors":{"authors":[{"text":"Brewster-Wingard, G. Lynn","contributorId":17626,"corporation":false,"usgs":true,"family":"Brewster-Wingard","given":"G.","email":"","middleInitial":"Lynn","affiliations":[],"preferred":false,"id":176612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weedman, S.D.","contributorId":23961,"corporation":false,"usgs":true,"family":"Weedman","given":"S.D.","affiliations":[],"preferred":false,"id":176614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, T.M.","contributorId":66694,"corporation":false,"usgs":true,"family":"Scott","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":176615,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":176611,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Green, R.C.","contributorId":22373,"corporation":false,"usgs":true,"family":"Green","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":176613,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":19077,"text":"ofr94708 - 1994 - Paleogene stratigraphy of the Solomons Island, Maryland, corehole","interactions":[],"lastModifiedDate":"2022-01-11T16:31:22.972084","indexId":"ofr94708","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-708","title":"Paleogene stratigraphy of the Solomons Island, Maryland, corehole","docAbstract":"<p>The Solomons Island corehole was drilled in the hope of obtaining a continuous and more nearly complete section of upper Paleocene and lower Eocene strata than are found in the discontinuous and fragmentary sections in the outcrop belt to the west. Consultation with Harry Hansen (Maryland Geological Survey) on possible drilling sites that were within the limits of our equipment and funding led to the selection of Solomons Island. A strong factor in this selection was the stratigraphic information available from the nearby Lexington Park well (Hansen and Wilson, 1984). As anticipated, all Paleogene units previously reported in the Maryland and Virginia Coastal Plain, except for the upper Eocene Chickahominy Formation and the upper Oligocene Old Church Formation, were penetrated at Solomons Island. The upper part of the Solomons Island corehole also penetrated the Calvert Formation of Miocene age and the younger Lowland Deposit. Gibson and Andrews (1994) described the lithology and biostratigraphy of these Miocene sediments. This paper describes the lithologies of the Lower Cretaceous, Paleocene, and Eocene strata that were recovered from the Solomons Island corehole and gives a brief biostratigraphic and paleoenvironmental summary of the beds penetrated there. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94708","usgsCitation":"Gibson, T.G., and Bybell, L.M., 1994, Paleogene stratigraphy of the Solomons Island, Maryland, corehole: U.S. Geological Survey Open-File Report 94-708, ii, 39 p., https://doi.org/10.3133/ofr94708.","productDescription":"ii, 39 p.","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":151105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0708/report-thumb.jpg"},{"id":394191,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0708/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland","otherGeospatial":"Solomons Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.607421875,\n              36.89719446989036\n            ],\n            [\n              -74.50927734375,\n              36.89719446989036\n            ],\n            [\n              -74.50927734375,\n              39.74943369178247\n            ],\n            [\n              -77.607421875,\n              39.74943369178247\n            ],\n            [\n              -77.607421875,\n              36.89719446989036\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689cad","contributors":{"authors":[{"text":"Gibson, Thomas G.","contributorId":25180,"corporation":false,"usgs":true,"family":"Gibson","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":180273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":180272,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29693,"text":"wri944231 - 1994 - Contributing recharge areas to water-supply wells at Wright-Patterson Air Force Base, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri944231","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4231","title":"Contributing recharge areas to water-supply wells at Wright-Patterson Air Force Base, Ohio","docAbstract":"Wright-Patterson Air Force Base, in southwestern Ohio, has operated three well fields--Area B, Skeel Road, and the East Well Fields--to supply potable water for consumption and use for base activities. To protect these well fields from contamination and to comply with the Ohio Wellhead Protection Plan, the Base is developing a wellhead-protection program for the well fields.\r\n\r\nA three-dimensional, steady-state ground-water-flow model was developed in 1993 to simulate heads in (1) the buried-valley aquifer system that is tapped by the two active well fields, and in (2) an upland bedrock aquifer that may supply water to the wells. An advective particle-tracking algorithm that requires estimated porosities and simulated heads was used to estimate ground-water-flow pathlines and traveltimes to the active well fields. Contributing recharge areas (CRA's)--areas on the water table that contribute water to a well or well field--were generated for 1-, 5-, and 10-year traveltimes.\r\n\r\nResults from the simulation and subsequent particle tracking indicate that the CRA's for the Skeel Road Well Fields are oval and extend north- ward, toward the Mad River, as pumping at the well field increases. The sizes of the 1-, 5-, and 10-year CRA's of Skeel Road Well Field, under maximum pumping conditions, are approximately 0.5, 1.5 and 3.2 square miles, respectively. The CRA's for the Area B Well Field extend to the north, up the Mad River Valley; as pumping increases at the well field, the CRA's extend up the Mad River Valley under Huffman Dam. The sizes of the 1-, 5-, and 10-year CRA's of Area B Well Field, under maximum pumping conditions, are approximately 0.1, 0.5, and 0.9 square miles, respectively. The CRA's for the East Well Field are affected by nearby streams under average pumping conditions. The sizes of the 1-, 5-, and 10-year CRA's of the East Well Field, under maximum pumping conditions, are approximately 0.2, 1.2, and 2.4 square miles, respectively. However, as pumping increases at the East Well Field, the ground-water-flow model develops numerical instabilities which limit the usefulness of the CRA's.\r\n\r\nSensitivity analyses show that variation of horizontal hydraulic conductivity and porosity in the upland bedrock does not affect the CRA's of the Skeel Road Well Field but does have a slight affect on the CRA's of the Area B Well Field. Uncertainties in horizontal hydraulic conductivity and porosity of the valley-train deposits have the largest affect on the size and shape of the CRA's of the Skeel Road Well Field. The position and size of the CRA's of Area B are probably also controlled by induced infiltration from the nearby Mad River and by pumping at the Rohrer's Island Well Field. However, uncertainty in riverbed conductance, which affects induced infiltration, does not significantly affect the size and shape of these CRA's.\r\n\r\nPumping centers not included in the ground-water-flow model do not appreciably affect the CRA's of the Area B and Skeel Road Well Fields under normal pumping. The pumping centers, located near Huffman Dam, will probably limit the northern extent of teh CRA's of Area B Well Field under greater than normal pumping conditions. The CRA's of the East Well Field will propagate farther to the northeast and southwest as a result of the increased pumping-related stress to the aquifer system.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944231","usgsCitation":"Sheets, R.A., 1994, Contributing recharge areas to water-supply wells at Wright-Patterson Air Force Base, Ohio: U.S. Geological Survey Water-Resources Investigations Report 94-4231, iv, 35 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944231.","productDescription":"iv, 35 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4231/report-thumb.jpg"},{"id":58516,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4231/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6296f5","contributors":{"authors":[{"text":"Sheets, R. A.","contributorId":43381,"corporation":false,"usgs":true,"family":"Sheets","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201961,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30199,"text":"wri944226 - 1994 - Effects of water-control structures on hydrologic and water-quality characteristics in selected agricultural drainage canals in eastern North Carolina","interactions":[],"lastModifiedDate":"2017-01-27T11:11:24","indexId":"wri944226","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4226","title":"Effects of water-control structures on hydrologic and water-quality characteristics in selected agricultural drainage canals in eastern North Carolina","docAbstract":"November of water into and out of tidally affected canals in eastern North Carolina was documented before and after the installation of water-control structures. Water levels in five of the canals downstream from the water-control structures were controlled primarily by water-level fluctuations in estuarine receiving waters. Water-control structures also altered upstream water levels in all canals. Water levels were lowered upstream from tide gates, but increased upstream from flashboard risers. Both types of water-control structures attenuated the release of runoff following rainfall events, but in slightly different ways. Tide gates appeared to reduce peak discharge rates associated with rainfall, and flashboard risers lengthened the duration of runoff release.\r\n\r\nTide gates had no apparent effect on pH, dissolved oxygen, suspended-sediment, or total phosphorus concentrations downstream from the structures. Specific conductance measured from composite samples collected with automatic samples increased downstream of tide gates after installation. Median concentrations of nitrite plus nitrate nitrogen were near the minimum detection level throughout the study; however, the number of observations of concentrations exceeding 0.1 milligram per liter dropped significantly after tide gates were installed. Following tide-gate installation, instantaneous loadings of nitrite plus nitrate nitrogen were significantly reduced at one test site, but this reduction was not observed at the other test site. Loadings of other nutrient species and suspended sediment did not change at the tide-gate test sites after tide-gate installation.\r\n\r\nSpecific conductance was lower in the Beaufort County canals than in the Hyde County canals. Although there was a slight increase in median values at the flashboard-riser sites, the mean and maximum values declined substantially downstream from the risers following installation. This decline of specific conductance in the canals occurred despite a large increase of specific conductance in the tidal creek.\r\n\r\nFlashboard risers had no significant effect on concentrations of dissolved oxygen, suspended sediment, total ammonia plus organic nitrogen, or phosphorus. Maximum concentrations of ammonia nitrogen were smaller at both test sites after riser installation. In addition, concentrations of nitrite plus nitrate nitrogen exceeding 1.0 milligram per liter rarely occurred at the flashboard-riser test sites following installation of the risers. Median loadings of nitrite plus nitrate nitrogen and total nitrogen decreased at one riser test site following flashboard-riser installation.\r\n\r\nTide gates and flashboard risers were associated with reductions in concentrations and export of nitrite plus nitrate nitrogen; however, these changes should be interpreted cautiously because reductions were not observed consistently at every site. The hydrology and baseline water-quality characteristics of the two study areas differ, making comparisons of the effectiveness of the two types of water-control structures difficult to interpret.\r\n\r\nThe effects of water-control structures on the hydrology of the drainage canals are more meaningful than the changes in water quality. Tide gates and flashboard risers altered the hydrologic characteristics of the drainage canals and created an environment favorable for nutrient loss or transformation. Both structures retained agricultural drainage upstream, which increased potential storage for infiltration and reduced the potential for surface runoff, sediment, and nutrient transport, and higher peak outflow rates.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nESIC, Open-File Reports Section [distributor],","doi":"10.3133/wri944226","usgsCitation":"Treece, M., and Jaynes, M., 1994, Effects of water-control structures on hydrologic and water-quality characteristics in selected agricultural drainage canals in eastern North Carolina: U.S. Geological Survey Water-Resources Investigations Report 94-4226, v, 62 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944226.","productDescription":"v, 62 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":124243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4226/report-thumb.jpg"},{"id":58989,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4226/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.32452392578125,\n              35.02324896091336\n            ],\n            [\n              -77.32452392578125,\n              35.86456960744962\n            ],\n            [\n              -76.0198974609375,\n              35.86456960744962\n            ],\n            [\n              -76.0198974609375,\n              35.02324896091336\n            ],\n            [\n              -77.32452392578125,\n              35.02324896091336\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684035","contributors":{"authors":[{"text":"Treece, M.W. Jr.","contributorId":60255,"corporation":false,"usgs":true,"family":"Treece","given":"M.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":202850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaynes, M.L.","contributorId":45736,"corporation":false,"usgs":true,"family":"Jaynes","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":202849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17461,"text":"ofr94653 - 1994 - Palynomorph biostratigraphy of Eocene samples from the Sagavanirktok Formation at Franklin Bluffs, North Slope of Alaska","interactions":[],"lastModifiedDate":"2020-03-27T07:03:53","indexId":"ofr94653","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-653","title":"Palynomorph biostratigraphy of Eocene samples from the Sagavanirktok Formation at Franklin Bluffs, North Slope of Alaska","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94653","usgsCitation":"Frederiksen, N.O., Edwards, L.E., Fouch, T.D., Carter, L.D., and Collett, T.S., 1994, Palynomorph biostratigraphy of Eocene samples from the Sagavanirktok Formation at Franklin Bluffs, North Slope of Alaska: U.S. Geological Survey Open-File Report 94-653, 32 p. , https://doi.org/10.3133/ofr94653.","productDescription":"32 p. ","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":150516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0653/report-thumb.jpg"},{"id":46615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0653/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"North Slope","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -164.5751953125,\n              68.98992503056704\n            ],\n            [\n              -141.15234374999997,\n              68.98992503056704\n            ],\n            [\n              -141.15234374999997,\n              71.5944122077672\n            ],\n            [\n              -164.5751953125,\n              71.5944122077672\n            ],\n            [\n              -164.5751953125,\n              68.98992503056704\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689462","contributors":{"authors":[{"text":"Frederiksen, Norman O.","contributorId":50880,"corporation":false,"usgs":true,"family":"Frederiksen","given":"Norman","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":176481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":176480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fouch, T. D.","contributorId":68333,"corporation":false,"usgs":true,"family":"Fouch","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":176482,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carter, L. D.","contributorId":87959,"corporation":false,"usgs":true,"family":"Carter","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":176484,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Collett, T. S. 0000-0002-7598-4708","orcid":"https://orcid.org/0000-0002-7598-4708","contributorId":86342,"corporation":false,"usgs":true,"family":"Collett","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":176483,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":28180,"text":"wri934039 - 1994 - Simulations of flow in the Edwards-Trinity aquifer system and contiguous hydraulically connected units, west-central Texas","interactions":[],"lastModifiedDate":"2022-12-15T22:51:23.899979","indexId":"wri934039","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4039","title":"Simulations of flow in the Edwards-Trinity aquifer system and contiguous hydraulically connected units, west-central Texas","docAbstract":"<p>The Edwards-Trinity aquifer system is currently (1993) being studied as part of the Regional Aquifer-Systems Analysis program. A major goal of the project is to understand and describe the regional ground-water flow system. A finite-element model for simulating two-dimensional steady-state ground-water flow was applied to the major aquifers of the Edwards-Trinity aquifer system and contiguous hydraulically connected units for the winter of 1974-75 and for the predevelopment conditions. The major aquifers are the Edwards-Trinity in the western semiarid part of the study area, the Trinity in the eastern subhumid part of the study area, and the Edwards in the southeastern part of the study area. The Edwards-Trinity, upper part of the Trinity, and part of the Edwards aquifers are shallow and unconfined over most of the study area. Regional ground-water flow is toward the perennial streams for the Edwards-Trinity and Trinity aquifers, as indicated by the observed and simulated potentiometric surfaces.</p>\n<p>The transmissivity values used in the simulations were within estimated ranges and generally are: 1,000 to 10,000 ft<sup>2</sup>/d (feet squared per day) for the Edwards-Trinity and Trinity aquifers; 100,000 to greater than 1 million ft<sup>2</sup>/d for the Edwards aquifer; and less than 500 to 10,000 ft<sup>2</sup>/d in contiguous hydraulically connected units. Simulated flow through the Edwards-Trinity aquifer system and contiguous hydraulically connected units is about 3 million acre-feet per year. Estimates of areally distributed recharge from the simulations range from 0.1 to 1 inch per year for the Edwards-Trinity aquifer and increase to 4 inches per year for the Trinity aquifer. Recharge to the Edwards aquifer occurs along streambeds that cross outcropped high-permeability rocks of the Edwards Group through joints and faults. Many of the streams are diverted completely underground during periods of no precipitation. The movement of a substantial quantity of water (about 400 cubic feet per second) from the Trinity and Edwards-Trinity aquifers into the Edwards aquifer was simulated. Results of the simulations indicate that anisotropy strongly influences flow in the Edwards aquifer. In the San Antonio and Austin areas, the Edwards aquifer is the most active part of the ground-water flow system with one-third of ground-water discharge occurring in 5 percent of the modeled area for both simulations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri934039","usgsCitation":"Kuniansky, E., and Holligan, K.Q., 1994, Simulations of flow in the Edwards-Trinity aquifer system and contiguous hydraulically connected units, west-central Texas: U.S. Geological Survey Water-Resources Investigations Report 93-4039, Document: iv, 40 p.; 3 Plates: 38.00 × 26.50 inches, https://doi.org/10.3133/wri934039.","productDescription":"Document: iv, 40 p.; 3 Plates: 38.00 × 26.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":410601,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47767.htm","linkFileType":{"id":5,"text":"html"}},{"id":57019,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57018,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4039/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57017,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4039/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57016,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4039/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Edwards-Trinity aquifer system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.2125,\n              32.4833\n            ],\n            [\n              -104.2125,\n              29.05\n            ],\n            [\n              -97.45,\n              29.05\n            ],\n            [\n              -97.45,\n              32.4833\n            ],\n            [\n              -104.2125,\n              32.4833\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1c32","contributors":{"authors":[{"text":"Kuniansky, E. L.","contributorId":82342,"corporation":false,"usgs":true,"family":"Kuniansky","given":"E. L.","affiliations":[],"preferred":false,"id":199344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holligan, K. Q.","contributorId":104536,"corporation":false,"usgs":true,"family":"Holligan","given":"K.","email":"","middleInitial":"Q.","affiliations":[],"preferred":false,"id":199345,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26884,"text":"wri944157 - 1994 - Water-level changes in the High Plains aquifer — Predevelopment to 1993","interactions":[],"lastModifiedDate":"2021-12-15T22:27:50.035672","indexId":"wri944157","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4157","title":"Water-level changes in the High Plains aquifer — Predevelopment to 1993","docAbstract":"Water-level change in the High Plains aquifer underlying parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming results from differences in recharge from precipitation and ground-water withdrawals for irrigation. From the beginning of irrigation development (1940) to 1980, water levels declined in several areas, and exceeded 100 feet in parts of the Central and Southern High Plains. From 1980 to 1993, water-level declines continued in these same areas, but at a smaller annual rate. This smaller rate of decline was associated with above-normal precipitation during 1981-93 and a decrease in ground-water application rates. Declines exceeding 20 feet from 1980 to 1993 were common in areas of intense irrigation development in the Central and Southern High Plains. In the Northern High Plains, water levels declined 10 to 20 feet from 1980 to 1993 in parts of northeastern Colorado, northwestern Kansas, southwestern Nebraska, and the Nebraska Panhandle. Water-level rises exceeding 20 feet, however, occurred in the Southern High Plains of Texas. Also, rises of 10 to 20 feet occurred in parts of southeastern and south-central Nebraska. The average area-weighted water level rose 0.21 foot from 1992 to 1993 in association was well-above normal precipitation in 1992. Water-level declines, however, continued in the intensively irrigated areas of the Central High Plains. Declines also' continued in the northern part of the Southern High Plains in spite of well-above normal precipitation. Water-level rises from 1992 to 1993 was widespread in eastern and southern Nebraska, northwestern and south-central Kansas, and in the southern two-thirds of the Southern High Plains of Texas in association with well-above normal precipitation in 1992. These rises exceeded 3 feet.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944157","usgsCitation":"Dugan, J.T., and Cox, D.A., 1994, Water-level changes in the High Plains aquifer — Predevelopment to 1993: U.S. Geological Survey Water-Resources Investigations Report 94-4157, vi, 60 p., https://doi.org/10.3133/wri944157.","productDescription":"vi, 60 p.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":392981,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48036.htm"},{"id":55775,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4157/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4157/report-thumb.jpg"}],"country":"United States","state":"Colorado, Kansas, Nebraska, New Mexico, Oklahoma, Texas, Wyoming","otherGeospatial":"High Plains aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.8203125,\n              31.353636941500987\n            ],\n            [\n              -95.361328125,\n              31.353636941500987\n            ],\n            [\n              -95.361328125,\n              43.5\n            ],\n            [\n              -105.8203125,\n              43.5\n            ],\n            [\n              -105.8203125,\n              31.353636941500987\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489988","contributors":{"authors":[{"text":"Dugan, J. T.","contributorId":67890,"corporation":false,"usgs":true,"family":"Dugan","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":197181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cox, D. A.","contributorId":105766,"corporation":false,"usgs":true,"family":"Cox","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":197182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67934,"text":"ha730H - 1994 - Ground Water Atlas of the United States: Segment 7, Idaho, Oregon, Washington","interactions":[{"subject":{"id":67934,"text":"ha730H - 1994 - Ground Water Atlas of the United States: Segment 7, Idaho, Oregon, Washington","indexId":"ha730H","publicationYear":"1994","noYear":false,"chapter":"H","title":"Ground Water Atlas of the United States: Segment 7, Idaho, Oregon, Washington"},"predicate":"IS_PART_OF","object":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"id":1}],"isPartOf":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"lastModifiedDate":"2017-05-30T15:43:48","indexId":"ha730H","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"730","chapter":"H","title":"Ground Water Atlas of the United States: Segment 7, Idaho, Oregon, Washington","docAbstract":"<p>The States of Idaho, Oregon, and Washington, which total 248,730 square miles, compose Segment 7 of this Atlas. The area is geologically and topographically diverse and contains a wealth of scenic beauty, natural resources, and ground and surface water that generally are suitable for all uses. Most of the area of Segment 7 is drained by the Columbia River, its tributaries, and other streams that discharge to the Pacific Ocean. Exceptions are those streams that flow to closed basins in southeastern Oregon and northern Nevada and to the Great Salt Lake in northern Utah. The Columbia River is one of the largest rivers in the Nation. The downstream reach of the Columbia River forms most of the border between Oregon and Washington. In 1990, Idaho, Oregon, and Washington had populations of 1.0 million, 2.8 million, and 4.9 million, respectively. The more densely populated parts are in lowland areas and stream valleys. Many of the mountains, the deserts, and the upland areas of Idaho, Oregon, and Washington lack major population centers. Large areas of Idaho and Oregon are uninhabited and are mostly public land (fig. 1) where extensive ground-water development is restricted. </p><p>Surface water is abundant in Idaho, Oregon, and Washington, though not always available when and where needed. In some places, surface water provides much of the water used for public-supply, domestic and commercial, agricultural (primarily irrigation and livestock watering), and industrial purposes. In arid parts of Segment 7, however, surface water has long been fully appropriated, chiefly for irrigation. Ground water is used when and where surface-water supplies are lacking. </p><p>Ground water is commonly available to shallow wells that are completed in unconsolidated-deposit aquifers that consist primarily of sand and gravel but contain variable quantities of clay and silt. Many large-yield public-supply and irrigation wells and thousands of domestic wells are completed in these types of aquifers, generally in areas of privately owned land (fig. 1). In many places, deeper wells produce water from underlying volcanic rocks, usually basalt. </p><p>Most irrigation (fig. 2) is on lowlands next to streams and on adjacent terraces. Generally, lowlands within a few miles of a main stream are irrigated with surface water diverted by gravity flow from the main stream or a reservoir and distributed through a system of canals and ditches. In some areas, water is pumped to irrigate lands farther from the stream at a higher altitude. Along the Snake and Columbia Rivers, large pumping systems withdraw billions of gallons of water per day from the rivers to irrigate adjacent uplands that are more than 500 feet higher than the rivers. Elsewhere, irrigation water is obtained from large-capacity wells, where depth to water might exceed 500 feet below land surface. </p><p>Aquifers in Idaho, Oregon, and Washington, as in most other States, differ considerably in thickness and permeability, and well yields differ accordingly. Ground-water levels in a few areas have declined as a result of withdrawals by wells. State governments have taken steps to alleviate declines in some areas by enacting programs that either limit the number of additional wells that can be completed in a particular aquifer (Ground-Water Management Area) or prevent further ground-water development (Critical Ground-Water Area). </p><p>Segment 7 includes some of the driest parts of the Nation, as well as some of the wettest. Average annual precipitation (1951-80) ranges from less than 10 inches in arid parts of Idaho, Oregon, and Washington to more than 80 inches in the western parts of Oregon and Washington (fig. 3). Most storms generally move eastward through the area. The eastward-moving air absorbs the moisture that evaporates from the Pacific Ocean. As this air encounters the fronts of mountain ranges, it rises, cools, and condenses. Accordingly, the western sides of the mountain ranges receive the most precipitation. Much of the annual precipitation moves directly to streams as overland runoff. Some of the precipitation is returned to the atmosphere by evapotranspiration, which is the combination of evaporation from the surface and transpiration from the plants. A small part of the precipitation infiltrates the soil and percolates downward to recharge underlying aquifers. </p><p>Average annual runoff ( 1951-80) in the segment varies considerably (fig. 4), and the distribution of the runoff generally parallels that of precipitation. In the arid and the semiarid parts of Segment 7, most precipitation replenishes soil moisture, evaporates, or is transpired by vegetation. Little is left to maintain streamflow or to recharge aquifers. In the wetter parts, much of the precipitation runs off the land surface to maintain streamflow, and because evaporation is usually less in wetter areas, more water is available to recharge aquifers. Precipitation that falls as snow generally does not become runoff until spring thaws begin. Reservoirs constructed on major streams to mitigate flooding and to store water for irrigation, hydroelectric-power generation, and recreation also affect the timing of runoff. The runoff is stored and subsequently released during drier periods to maintain downstream flow.</p>","largerWorkTitle":"Ground Water Atlas of the United States","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha730H","isbn":"060776757X","usgsCitation":"Whitehead, R., 1994, Ground Water Atlas of the United States: Segment 7, Idaho, Oregon, Washington: U.S. Geological Survey Hydrologic Atlas 730, 31 p., https://doi.org/10.3133/ha730H.","productDescription":"31 p.","startPage":"H1","endPage":"H31","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":11485,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ha/ha730/ch_h/index.html","linkFileType":{"id":5,"text":"html"}},{"id":115244,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/730h/report.pdf","text":"Report","size":"65.98 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":187797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/730h/report-thumb.jpg"}],"country":"United States","state":"Idaho, Oregon, Washington","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-111.044156,43.020052],[-111.046689,42.001567],[-113.893261,41.988057],[-114.831077,42.002207],[-121.035195,41.993323],[-123.145959,42.009247],[-123.656998,41.995137],[-124.211605,41.99846],[-124.270464,42.045553],[-124.299649,42.051736],[-124.356229,42.114952],[-124.361009,42.180752],[-124.383633,42.22716],[-124.410982,42.250547],[-124.410556,42.307431],[-124.429288,42.331746],[-124.424863,42.395426],[-124.434882,42.434916],[-124.390664,42.566593],[-124.401177,42.627192],[-124.413119,42.657934],[-124.45074,42.675798],[-124.473864,42.732671],[-124.491679,42.741789],[-124.510017,42.734746],[-124.552441,42.840568],[-124.456918,43.000315],[-124.434451,43.115986],[-124.401726,43.184896],[-124.38246,43.270167],[-124.402814,43.305872],[-124.373037,43.338953],[-124.341587,43.351337],[-124.315012,43.388389],[-124.233534,43.55713],[-124.168392,43.808903],[-124.142704,43.958182],[-124.111054,44.235071],[-124.1152,44.286486],[-124.084401,44.415611],[-124.071706,44.423662],[-124.084429,44.486927],[-124.067251,44.60804],[-124.082326,44.608861],[-124.065202,44.622445],[-124.058281,44.658866],[-124.070394,44.683514],[-124.059077,44.737656],[-124.075473,44.771403],[-124.074066,44.798107],[-124.025136,44.928175],[-124.004598,45.044959],[-124.017991,45.049808],[-124.015851,45.064759],[-123.989529,45.094045],[-123.975425,45.145476],[-123.964169,45.317026],[-123.972899,45.33689],[-124.007756,45.336813],[-123.973398,45.354791],[-123.965728,45.386242],[-123.960557,45.430778],[-123.976544,45.489733],[-123.957568,45.510399],[-123.939005,45.661923],[-123.943121,45.727031],[-123.982578,45.761815],[-123.969459,45.782371],[-123.962736,45.869974],[-123.96763,45.907807],[-123.993703,45.946431],[-123.969991,45.969139],[-123.941831,45.97566],[-123.927891,46.009564],[-123.933366,46.071672],[-123.974124,46.168798],[-124.024305,46.229256],[-124.001998,46.237316],[-123.987196,46.211521],[-123.950148,46.204097],[-123.9042,46.169293],[-123.854801,46.157342],[-123.841521,46.169824],[-123.863347,46.18235],[-123.838801,46.192211],[-123.636474,46.214359],[-123.625219,46.233868],[-123.605487,46.2393],[-123.586205,46.228654],[-123.548194,46.248245],[-123.547659,46.259109],[-123.669501,46.266832],[-123.680574,46.296025],[-123.700764,46.305278],[-123.75956,46.275073],[-123.806139,46.283588],[-123.875525,46.239787],[-123.909306,46.245491],[-123.985204,46.309039],[-124.020551,46.315737],[-124.044018,46.275925],[-124.080671,46.267239],[-124.057425,46.409315],[-124.069583,46.630651],[-124.048444,46.645827],[-124.035874,46.630822],[-124.052708,46.622796],[-124.023566,46.582559],[-124.026032,46.462978],[-123.990615,46.463019],[-123.988386,46.497008],[-123.97083,46.47537],[-123.943667,46.477197],[-123.894254,46.537028],[-123.928861,46.588875],[-123.955556,46.60357],[-123.960642,46.636364],[-123.921913,46.650262],[-123.923269,46.672708],[-123.851356,46.70256],[-123.84621,46.716795],[-123.893054,46.750204],[-123.929073,46.725278],[-123.968564,46.736106],[-123.979655,46.724658],[-123.966886,46.705184],[-124.003458,46.702337],[-124.092176,46.741624],[-124.108078,46.836388],[-124.138225,46.905534],[-124.117712,46.91238],[-124.093392,46.901168],[-124.089286,46.867716],[-124.073113,46.861493],[-124.055085,46.870429],[-124.049279,46.891253],[-123.985082,46.921916],[-123.86018,46.948556],[-123.898245,46.971927],[-124.012218,46.985176],[-124.019727,46.991189],[-124.005248,47.003915],[-124.026345,47.030187],[-124.122057,47.04165],[-124.151288,47.021112],[-124.124386,46.94387],[-124.180111,46.926357],[-124.169113,46.994508],[-124.182802,47.134041],[-124.236349,47.287287],[-124.271193,47.305025],[-124.299943,47.34836],[-124.319379,47.355559],[-124.355955,47.545698],[-124.425195,47.738434],[-124.453927,47.765334],[-124.471687,47.766907],[-124.489737,47.816988],[-124.539927,47.836967],[-124.562363,47.866216],[-124.625512,47.887963],[-124.645442,47.935338],[-124.672427,47.964414],[-124.696542,48.069274],[-124.688602,48.092466],[-124.731746,48.169997],[-124.696111,48.198599],[-124.6909,48.212617],[-124.705031,48.238774],[-124.684677,48.255228],[-124.65894,48.331057],[-124.731828,48.381157],[-124.653243,48.390691],[-124.631108,48.376522],[-124.599278,48.381035],[-124.395593,48.288772],[-124.361351,48.287582],[-124.272017,48.25441],[-124.238582,48.262471],[-124.101773,48.216883],[-124.107215,48.200082],[-124.050734,48.177747],[-123.981032,48.164761],[-123.858821,48.154273],[-123.672445,48.162715],[-123.628819,48.139279],[-123.590839,48.134949],[-123.551131,48.151382],[-123.507235,48.131807],[-123.440128,48.142014],[-123.441972,48.124259],[-123.424668,48.118065],[-123.332699,48.11297],[-123.239129,48.118217],[-123.133445,48.177276],[-123.143229,48.156633],[-123.06621,48.120469],[-123.038727,48.081138],[-122.929095,48.096244],[-122.917942,48.091535],[-122.927975,48.06665],[-122.877641,48.047025],[-122.849273,48.053808],[-122.878255,48.076072],[-122.882013,48.100779],[-122.833173,48.134406],[-122.760448,48.14324],[-122.748911,48.117026],[-122.801399,48.087561],[-122.766648,48.04429],[-122.74229,48.049324],[-122.739271,48.069153],[-122.747389,48.070795],[-122.733257,48.091232],[-122.68724,48.101662],[-122.69222,48.087081],[-122.669868,48.017217],[-122.723374,48.008095],[-122.718082,47.987739],[-122.683223,47.972226],[-122.681924,47.936415],[-122.651063,47.920985],[-122.646494,47.894771],[-122.610341,47.887343],[-122.63636,47.866186],[-122.69376,47.868002],[-122.683742,47.838773],[-122.748061,47.800546],[-122.758498,47.746036],[-122.781682,47.70392],[-122.811929,47.679861],[-122.832139,47.695511],[-122.790619,47.792597],[-122.812616,47.840029],[-122.820178,47.835904],[-122.815027,47.807493],[-122.845612,47.777474],[-122.896524,47.674838],[-122.97244,47.6149],[-123.106486,47.45817],[-123.15598,47.355745],[-123.140169,47.347496],[-123.111298,47.362619],[-123.120234,47.39149],[-122.967284,47.585685],[-122.856611,47.649615],[-122.754186,47.671612],[-122.740159,47.736228],[-122.714801,47.768176],[-122.690562,47.778372],[-122.684085,47.798574],[-122.608105,47.856728],[-122.573672,47.857582],[-122.588235,47.912923],[-122.616701,47.925139],[-122.617022,47.938987],[-122.603861,47.940478],[-122.592184,47.922519],[-122.549072,47.919072],[-122.513986,47.880807],[-122.506122,47.831745],[-122.482529,47.815511],[-122.495458,47.786692],[-122.470333,47.757109],[-122.488491,47.743605],[-122.554454,47.745704],[-122.543161,47.710941],[-122.504604,47.699136],[-122.518277,47.65132],[-122.493205,47.635122],[-122.49824,47.598242],[-122.483805,47.586721],[-122.543118,47.556326],[-122.547207,47.528257],[-122.494882,47.510265],[-122.530514,47.469041],[-122.531889,47.428827],[-122.551136,47.394456],[-122.537044,47.375896],[-122.573739,47.318419],[-122.550134,47.290496],[-122.589454,47.227618],[-122.611464,47.2181],[-122.692426,47.280026],[-122.671256,47.343774],[-122.634823,47.370583],[-122.639126,47.377822],[-122.725738,47.33047],[-122.749621,47.276408],[-122.641802,47.205013],[-122.711997,47.127681],[-122.771619,47.167109],[-122.832799,47.243412],[-122.799025,47.289306],[-122.803688,47.355071],[-122.821868,47.363069],[-122.822344,47.319763],[-122.863732,47.270221],[-122.838298,47.208353],[-122.858735,47.167955],[-122.814238,47.179482],[-122.775056,47.123114],[-122.721437,47.103179],[-122.67813,47.103866],[-122.631987,47.140589],[-122.614855,47.169143],[-122.590829,47.178107],[-122.527586,47.291531],[-122.547747,47.316403],[-122.4442,47.266723],[-122.409199,47.288556],[-122.444635,47.300421],[-122.423535,47.319121],[-122.324833,47.348521],[-122.328434,47.400621],[-122.348035,47.415921],[-122.355135,47.441921],[-122.383136,47.450521],[-122.368036,47.459221],[-122.365236,47.48842],[-122.396538,47.51522],[-122.398338,47.55012],[-122.421139,47.57602],[-122.387139,47.59572],[-122.358238,47.58482],[-122.339513,47.599113],[-122.367819,47.624213],[-122.414645,47.639766],[-122.429841,47.658919],[-122.37314,47.729219],[-122.397043,47.779719],[-122.394944,47.803318],[-122.339944,47.846718],[-122.307048,47.949117],[-122.230046,47.970917],[-122.224979,48.016626],[-122.343241,48.097631],[-122.363842,48.12393],[-122.370253,48.164809],[-122.362044,48.187568],[-122.395499,48.228551],[-122.449605,48.232598],[-122.441731,48.211776],[-122.478535,48.188087],[-122.479008,48.175703],[-122.442383,48.130841],[-122.379481,48.087384],[-122.363107,48.054546],[-122.4675,48.130353],[-122.486736,48.12095],[-122.512031,48.133931],[-122.53722,48.183745],[-122.530996,48.249821],[-122.480925,48.251706],[-122.466803,48.269604],[-122.406516,48.25183],[-122.371693,48.287839],[-122.408718,48.326413],[-122.533452,48.383409],[-122.554536,48.40604],[-122.557298,48.444438],[-122.649839,48.408526],[-122.678928,48.439466],[-122.654844,48.454087],[-122.657753,48.47294],[-122.689121,48.476849],[-122.700603,48.457632],[-122.710362,48.461584],[-122.712981,48.47879],[-122.684521,48.509123],[-122.606961,48.522152],[-122.568071,48.50821],[-122.537355,48.466749],[-122.500721,48.460887],[-122.471832,48.470724],[-122.498463,48.556206],[-122.534719,48.574246],[-122.495904,48.575927],[-122.482406,48.559653],[-122.44456,48.570115],[-122.425271,48.599522],[-122.500308,48.656163],[-122.519172,48.713095],[-122.490401,48.751128],[-122.535803,48.776128],[-122.596844,48.771492],[-122.637146,48.735708],[-122.612562,48.714932],[-122.605733,48.701066],[-122.615169,48.693839],[-122.673472,48.733082],[-122.645743,48.781538],[-122.680246,48.80275],[-122.693683,48.804475],[-122.703106,48.786321],[-122.7112,48.79146],[-122.717073,48.84719],[-122.793175,48.892927],[-122.751289,48.911239],[-122.746596,48.930731],[-122.766096,48.941955],[-122.787539,48.931702],[-122.818232,48.939062],[-122.817226,48.95597],[-122.796887,48.975026],[-122.756318,48.996881],[-116.049193,49.000912],[-116.04885,47.977186],[-116.030751,47.973349],[-115.906409,47.846261],[-115.881522,47.849672],[-115.852291,47.827991],[-115.835365,47.760957],[-115.824597,47.752154],[-115.803917,47.75848],[-115.780441,47.743447],[-115.776219,47.719818],[-115.72377,47.696671],[-115.73627,47.654762],[-115.694284,47.62346],[-115.689404,47.595402],[-115.734674,47.567401],[-115.747263,47.543197],[-115.717024,47.532693],[-115.686704,47.485596],[-115.655272,47.477944],[-115.654318,47.468077],[-115.671188,47.45439],[-115.718247,47.45316],[-115.731348,47.433381],[-115.657681,47.400651],[-115.644341,47.381826],[-115.609492,47.380799],[-115.556318,47.353076],[-115.51186,47.295219],[-115.428359,47.278722],[-115.410685,47.264228],[-115.326903,47.255912],[-115.29211,47.209861],[-115.300805,47.19393],[-115.261885,47.181742],[-115.243707,47.150347],[-115.200547,47.139154],[-115.140375,47.093013],[-115.107132,47.049041],[-115.087806,47.045519],[-115.049538,46.970774],[-115.001274,46.971901],[-114.963978,46.932889],[-114.929997,46.919625],[-114.931058,46.882108],[-114.947413,46.859324],[-114.928615,46.854815],[-114.920459,46.827697],[-114.888146,46.808573],[-114.864342,46.813858],[-114.829117,46.782503],[-114.79004,46.778729],[-114.765106,46.758153],[-114.788656,46.714033],[-114.76689,46.696901],[-114.713516,46.715138],[-114.699008,46.740223],[-114.649388,46.73289],[-114.620859,46.707415],[-114.623198,46.691511],[-114.641745,46.679286],[-114.635713,46.659375],[-114.595213,46.633456],[-114.547321,46.644485],[-114.466902,46.631695],[-114.424424,46.660648],[-114.360709,46.669059],[-114.320665,46.646963],[-114.348733,46.533792],[-114.342072,46.519679],[-114.35874,46.505306],[-114.403019,46.498675],[-114.376413,46.442983],[-114.384756,46.411784],[-114.422458,46.387097],[-114.411592,46.366688],[-114.413758,46.335945],[-114.431708,46.310744],[-114.425587,46.287899],[-114.470479,46.26732],[-114.445497,46.220227],[-114.445928,46.173933],[-114.472643,46.162202],[-114.514706,46.167726],[-114.527096,46.146218],[-114.5213,46.125287],[-114.474415,46.112515],[-114.460049,46.097104],[-114.468529,46.062484],[-114.493418,46.03717],[-114.470965,45.995742],[-114.425843,45.984984],[-114.403712,45.967049],[-114.431328,45.938023],[-114.387166,45.889164],[-114.409477,45.85164],[-114.44868,45.858891],[-114.509303,45.845531],[-114.512973,45.828825],[-114.562509,45.779927],[-114.495421,45.703321],[-114.507645,45.658949],[-114.561046,45.639906],[-114.538132,45.606834],[-114.559038,45.565706],[-114.460542,45.561283],[-114.456764,45.543983],[-114.415804,45.509753],[-114.36852,45.492716],[-114.360719,45.474116],[-114.333218,45.459316],[-114.270717,45.486116],[-114.247824,45.524283],[-114.248121,45.545877],[-114.192802,45.536596],[-114.180043,45.551432],[-114.135249,45.557465],[-114.122322,45.58426],[-114.086584,45.59118],[-114.067619,45.627706],[-114.018731,45.648616],[-114.019315,45.692937],[-113.986656,45.704564],[-113.93422,45.682232],[-113.898883,45.644167],[-113.904691,45.622007],[-113.861404,45.62366],[-113.806729,45.602146],[-113.803261,45.584193],[-113.834555,45.520729],[-113.766022,45.520621],[-113.759986,45.480735],[-113.78416,45.454946],[-113.764591,45.431403],[-113.765203,45.410601],[-113.734402,45.392353],[-113.738729,45.329741],[-113.689359,45.28355],[-113.684946,45.253706],[-113.599506,45.191114],[-113.57467,45.128411],[-113.554744,45.112901],[-113.513342,45.115225],[-113.506638,45.107288],[-113.520134,45.093033],[-113.485278,45.063519],[-113.45197,45.059247],[-113.437726,45.006967],[-113.446884,44.998545],[-113.443782,44.95989],[-113.498745,44.942314],[-113.455071,44.865424],[-113.356062,44.819798],[-113.3461,44.800611],[-113.354763,44.795468],[-113.341704,44.784853],[-113.247166,44.82295],[-113.131453,44.772837],[-113.134824,44.752763],[-113.102138,44.729027],[-113.098064,44.697477],[-113.06776,44.679474],[-113.068306,44.656374],[-113.049349,44.62938],[-113.083819,44.60222],[-113.019777,44.528505],[-113.020917,44.493827],[-113.003544,44.450814],[-112.951146,44.416699],[-112.886041,44.395874],[-112.855395,44.359975],[-112.814156,44.377198],[-112.812608,44.392275],[-112.836034,44.422653],[-112.781294,44.484888],[-112.71911,44.504344],[-112.664485,44.48645],[-112.541989,44.483971],[-112.50031,44.463051],[-112.473207,44.480027],[-112.387389,44.448058],[-112.358926,44.48628],[-112.35421,44.535638],[-112.319198,44.53911],[-112.286187,44.568472],[-112.242785,44.568091],[-112.221698,44.543519],[-112.183937,44.533067],[-112.136454,44.539911],[-112.106755,44.520829],[-112.069011,44.537104],[-112.036943,44.530323],[-112.032707,44.546642],[-111.980833,44.536682],[-111.947941,44.556776],[-111.870504,44.564033],[-111.821488,44.509286],[-111.715474,44.543543],[-111.704218,44.560205],[-111.617348,44.549467],[-111.591768,44.561502],[-111.471682,44.540824],[-111.469185,44.552044],[-111.519126,44.582916],[-111.525764,44.604883],[-111.473178,44.665479],[-111.468833,44.679335],[-111.484898,44.687578],[-111.486019,44.707654],[-111.438793,44.720546],[-111.414271,44.710741],[-111.385005,44.755128],[-111.355768,44.727602],[-111.323669,44.724474],[-111.26875,44.668279],[-111.276956,44.655626],[-111.25268,44.651092],[-111.224161,44.623402],[-111.225208,44.581006],[-111.189617,44.571062],[-111.143557,44.535732],[-111.122654,44.493659],[-111.048974,44.474072],[-111.044156,43.020052]]],[[[-122.519535,48.288314],[-122.551793,48.281512],[-122.584086,48.297987],[-122.618466,48.294159],[-122.623779,48.269431],[-122.652639,48.265081],[-122.668385,48.223967],[-122.63126,48.220686],[-122.588138,48.18594],[-122.558205,48.119579],[-122.571615,48.105113],[-122.54512,48.05255],[-122.516314,48.057181],[-122.511081,48.075301],[-122.525422,48.096537],[-122.513276,48.097538],[-122.491104,48.094242],[-122.431266,48.045001],[-122.376259,48.034457],[-122.373263,48.000791],[-122.353611,47.981433],[-122.349597,47.958796],[-122.380497,47.904023],[-122.431035,47.914732],[-122.445519,47.930226],[-122.446682,47.963155],[-122.47266,47.988449],[-122.546824,47.967215],[-122.542924,47.996404],[-122.607342,48.030992],[-122.593621,48.0472],[-122.614028,48.072788],[-122.598301,48.110616],[-122.609568,48.15186],[-122.633167,48.163281],[-122.679556,48.155113],[-122.693084,48.181509],[-122.770045,48.224395],[-122.72259,48.304268],[-122.673731,48.354683],[-122.664659,48.401508],[-122.634991,48.404244],[-122.637892,48.395681],[-122.60198,48.409907],[-122.585038,48.395166],[-122.585162,48.353304],[-122.506568,48.310041],[-122.519535,48.288314]]],[[[-122.474684,47.511068],[-122.452399,47.503471],[-122.460442,47.493764],[-122.433385,47.46643],[-122.437656,47.407424],[-122.373628,47.388718],[-122.437809,47.365606],[-122.453997,47.343337],[-122.51885,47.33332],[-122.528128,47.345542],[-122.517797,47.368678],[-122.526733,47.398581],[-122.514703,47.414048],[-122.513328,47.449106],[-122.482739,47.483133],[-122.474684,47.511068]]],[[[-122.695907,48.737273],[-122.663259,48.697077],[-122.618225,48.670721],[-122.609576,48.645018],[-122.673538,48.680809],[-122.691795,48.711498],[-122.718833,48.716818],[-122.715709,48.748672],[-122.695907,48.737273]]],[[[-123.035393,49.002154],[-123.021459,48.977299],[-123.083834,48.976139],[-123.090546,49.001976],[-123.035393,49.002154]]],[[[-122.800217,48.60169],[-122.801096,48.585425],[-122.771206,48.562426],[-122.788503,48.530393],[-122.779124,48.508911],[-122.816332,48.487841],[-122.81973,48.458843],[-122.802509,48.433098],[-122.812208,48.422326],[-122.874135,48.418196],[-122.893646,48.422655],[-122.889016,48.435947],[-122.928004,48.439966],[-122.91646,48.453263],[-122.926901,48.460874],[-122.962009,48.451161],[-123.039156,48.460003],[-123.119451,48.492576],[-123.163234,48.529544],[-123.173061,48.579086],[-123.203026,48.596178],[-123.178425,48.622115],[-123.107362,48.622451],[-123.102074,48.604035],[-123.048403,48.569216],[-122.987296,48.561895],[-122.995026,48.578162],[-123.034101,48.591767],[-123.024902,48.594484],[-123.048652,48.621002],[-122.941316,48.702904],[-122.894599,48.71503],[-122.743049,48.661991],[-122.809622,48.619035],[-122.800217,48.60169]]],[[[-123.197953,48.68466],[-123.14799,48.668001],[-123.106165,48.633473],[-123.237148,48.683466],[-123.197953,48.68466]]],[[[-123.025486,48.717966],[-123.009787,48.722291],[-123.005086,48.694342],[-123.021215,48.681416],[-123.042337,48.675663],[-123.035672,48.68535],[-123.047058,48.695772],[-123.070427,48.699971],[-123.025486,48.717966]]],[[[-122.649405,48.588457],[-122.583985,48.551534],[-122.572967,48.529028],[-122.599948,48.536904],[-122.649256,48.528769],[-122.649405,48.588457]]],[[[-122.714512,48.60878],[-122.670638,48.568812],[-122.68944,48.543903],[-122.717278,48.539739],[-122.73944,48.573893],[-122.714512,48.60878]]],[[[-122.699266,48.621115],[-122.674173,48.629944],[-122.657016,48.609891],[-122.699266,48.621115]]]]},\"properties\":{\"name\":\"Idaho\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dd74","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":277350,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19236,"text":"ofr9368 - 1994 - Flood data for the Sacramento River and Butte Basin, Sacramento Valley, California, 1980-90","interactions":[],"lastModifiedDate":"2022-12-23T22:45:23.536219","indexId":"ofr9368","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-68","title":"Flood data for the Sacramento River and Butte Basin, Sacramento Valley, California, 1980-90","docAbstract":"Floodflows and peak states of floods were measured and channel cross sections were surveyed at sites along the Sacramento River and in Butte Basin, Sacramento Valley, California, during 1980-90 to document magnitudes of flooding and channel changes. The study reach extends from rivermile 200 near Hamilton City to rivermile 134 near Meridian. Data were collected for each flood at about 70 sites that include streamf-flow gages, crest-stage gages, bridges and road overflows on State Highway 162 east of Butte City, and locations of historical high- water marks. Six cross sections of the river between rivermiles 193.7 near Big Chico Creek and 183.3 near Ordbend were surveyed annually during calendar years 1981-84, and 1986-90. Floodflows (peak flow 157,000 cubic feet per second) almost equaled the design flow capacity of the river at Butte City on March 2, 1983, when the peak stage of 93.0 feet was 5 feet below the top of the levee. This was the largest flood recorded at Butte City during 1980- 90. The most recent flood occurred February 18-19, 1986, when the peak stage in the river at Butte City was 92.0 feet and the peak flow was 145,000 cubic feet per second.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9368","usgsCitation":"Harmon, J.G., 1994, Flood data for the Sacramento River and Butte Basin, Sacramento Valley, California, 1980-90: U.S. Geological Survey Open-File Report 93-68, iv, 30 p., https://doi.org/10.3133/ofr9368.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":411041,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12616.htm","linkFileType":{"id":5,"text":"html"}},{"id":48693,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151747,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0068/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sacramento River and Butte Basin, Sacramento Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.10488521812019,\n              39.76166300897259\n            ],\n            [\n              -122.10488521812019,\n              39.112698933014286\n            ],\n            [\n              -121.57970543046218,\n              39.112698933014286\n            ],\n            [\n              -121.57970543046218,\n              39.76166300897259\n            ],\n            [\n              -122.10488521812019,\n              39.76166300897259\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7db","contributors":{"authors":[{"text":"Harmon, Jerry G.","contributorId":30220,"corporation":false,"usgs":true,"family":"Harmon","given":"Jerry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":180539,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5083,"text":"fs03194 - 1994 - National Water-Quality Assessment Program— Eastern Iowa basins","interactions":[],"lastModifiedDate":"2024-09-13T13:16:22.584519","indexId":"fs03194","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"031-94","title":"National Water-Quality Assessment Program— Eastern Iowa basins","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs03194","usgsCitation":"Kalkhoff, S.J., 1994, National Water-Quality Assessment Program— Eastern Iowa basins: U.S. Geological Survey Fact Sheet 031-94, 2 p., https://doi.org/10.3133/fs03194.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":433734,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/031-94/fs94-031.pdf","text":"Report","size":"758 kB","linkFileType":{"id":1,"text":"pdf"}},{"id":117348,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/031-94/coverthb.jpg"}],"country":"United States","state":"Iowa","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.217706,43.50055],[-91.216035,43.481142],[-91.233367,43.455168],[-91.200359,43.412701],[-91.198953,43.389835],[-91.21477,43.365874],[-91.20662,43.352524],[-91.132813,43.32803],[-91.107237,43.313645],[-91.07371,43.274746],[-91.071698,43.261014],[-91.058644,43.257679],[-91.066398,43.239293],[-91.12217,43.197255],[-91.1462,43.152405],[-91.1562,43.142945],[-91.175253,43.134665],[-91.179457,43.067427],[-91.156562,42.978226],[-91.14543,42.958211],[-91.14988,42.941955],[-91.1438,42.922877],[-91.146177,42.90985],[-91.100565,42.883078],[-91.097656,42.859871],[-91.091837,42.851225],[-91.09406,42.830813],[-91.078665,42.827678],[-91.069549,42.769628],[-91.060261,42.761847],[-91.065783,42.753387],[-91.056297,42.747341],[-91.051275,42.737001],[-91.035418,42.73734],[-91.026786,42.724228],[-91.000128,42.716189],[-90.977735,42.696816],[-90.949213,42.685573],[-90.923634,42.6855],[-90.88743,42.67247],[-90.731132,42.643437],[-90.706303,42.634169],[-90.692031,42.610366],[-90.686975,42.591774],[-90.661527,42.567999],[-90.654127,42.5499],[-90.643927,42.540401],[-90.636927,42.513202],[-90.655927,42.491703],[-90.654027,42.478503],[-90.624328,42.458904],[-90.567968,42.440389],[-90.560439,42.432897],[-90.555018,42.416138],[-90.477279,42.383794],[-90.462619,42.367253],[-90.443874,42.355218],[-90.416535,42.325109],[-90.430884,42.27823],[-90.419326,42.254467],[-90.400653,42.239293],[-90.391108,42.225473],[-90.356964,42.205445],[-90.328273,42.201047],[-90.282173,42.178846],[-90.234919,42.165431],[-90.209479,42.15268],[-90.197342,42.128163],[-90.167533,42.122475],[-90.161159,42.106372],[-90.168358,42.075779],[-90.164485,42.042105],[-90.151579,42.030633],[-90.140061,42.003252],[-90.146225,41.981329],[-90.164135,41.956178],[-90.163847,41.944934],[-90.152659,41.933058],[-90.153584,41.906614],[-90.181401,41.844647],[-90.181973,41.80707],[-90.278633,41.767358],[-90.310708,41.742214],[-90.317668,41.72269],[-90.313435,41.698082],[-90.334525,41.679559],[-90.343452,41.646959],[-90.339528,41.598633],[-90.343228,41.587833],[-90.41283,41.565333],[-90.461432,41.523533],[-90.500633,41.518033],[-90.540935,41.526133],[-90.591037,41.512832],[-90.602137,41.506032],[-90.605937,41.494232],[-90.655839,41.462132],[-90.750142,41.449632],[-90.846558,41.455141],[-90.930016,41.421404],[-90.979815,41.434321],[-91.027787,41.423603],[-91.043988,41.415897],[-91.05101,41.387556],[-91.06652,41.365246],[-91.074841,41.305578],[-91.092034,41.286911],[-91.114186,41.250029],[-91.113648,41.241401],[-91.07298,41.207151],[-91.041536,41.166138],[-91.027214,41.163373],[-91.007586,41.166183],[-90.99496,41.160624],[-90.946627,41.096632],[-90.949383,41.072711],[-90.942253,41.034702],[-90.945949,41.006495],[-90.958142,40.979767],[-90.952233,40.954047],[-90.965344,40.921633],[-91.009536,40.900565],[-91.021562,40.884021],[-91.044653,40.868356],[-91.05643,40.848387],[-91.092993,40.821079],[-91.097649,40.805575],[-91.091703,40.779708],[-91.110424,40.745528],[-91.115735,40.725168],[-91.11194,40.697018],[-91.123928,40.669152],[-91.185428,40.638071],[-91.253074,40.637962],[-91.306524,40.626231],[-91.339719,40.613488],[-91.359873,40.601805],[-91.379752,40.57445],[-91.401482,40.559458],[-91.406373,40.551831],[-91.404125,40.539127],[-91.384531,40.530948],[-91.369059,40.512532],[-91.364211,40.500043],[-91.364915,40.484168],[-91.381769,40.442555],[-91.372554,40.4012],[-91.381958,40.387632],[-91.419422,40.378264],[-91.441243,40.386255],[-91.452458,40.375501],[-91.463895,40.375659],[-91.465116,40.385257],[-91.484507,40.3839],[-91.490977,40.393484],[-91.487829,40.403866],[-91.498093,40.401926],[-91.522333,40.409648],[-91.527057,40.416689],[-91.519012,40.431298],[-91.529132,40.434272],[-91.533548,40.440804],[-91.523271,40.450061],[-91.526155,40.458625],[-91.552691,40.458769],[-91.574746,40.465664],[-91.590817,40.492292],[-91.621353,40.510072],[-91.618028,40.53403],[-91.6219,40.542292],[-91.6887,40.55739],[-91.691557,40.564867],[-91.686357,40.580875],[-91.716769,40.59853],[-91.729115,40.61364],[-92.686693,40.589809],[-94.294813,40.571341],[-94.632032,40.571186],[-95.765645,40.585208],[-95.753148,40.59284],[-95.748626,40.603355],[-95.768926,40.621264],[-95.776251,40.647463],[-95.795489,40.662384],[-95.822913,40.66724],[-95.842801,40.677496],[-95.852615,40.702262],[-95.883178,40.717579],[-95.888907,40.731855],[-95.879027,40.753081],[-95.84662,40.768619],[-95.835232,40.779151],[-95.834523,40.787778],[-95.845342,40.811324],[-95.837186,40.835347],[-95.847084,40.854174],[-95.847785,40.864328],[-95.838735,40.872191],[-95.815933,40.879846],[-95.809474,40.891228],[-95.813458,40.901693],[-95.836438,40.921642],[-95.839743,40.93278],[-95.829074,40.975688],[-95.838908,40.986484],[-95.867286,41.001599],[-95.869486,41.009399],[-95.859918,41.025403],[-95.859654,41.035695],[-95.882415,41.060411],[-95.862587,41.088399],[-95.865888,41.117898],[-95.882088,41.143998],[-95.883489,41.154898],[-95.871912,41.168122],[-95.846188,41.166698],[-95.841288,41.174998],[-95.856788,41.187098],[-95.90969,41.184398],[-95.91829,41.186698],[-95.92599,41.195698],[-95.924891,41.211198],[-95.910891,41.231798],[-95.921891,41.264598],[-95.913991,41.271398],[-95.928691,41.281398],[-95.927491,41.298397],[-95.90589,41.300897],[-95.90429,41.293497],[-95.912491,41.279498],[-95.90249,41.273398],[-95.87689,41.285097],[-95.871489,41.295797],[-95.883089,41.316697],[-95.92569,41.322197],[-95.946891,41.334096],[-95.956691,41.345496],[-95.954891,41.351796],[-95.93549,41.360596],[-95.92879,41.370096],[-95.93689,41.396387],[-95.929721,41.411331],[-95.933169,41.42943],[-95.919865,41.447922],[-95.922529,41.455766],[-95.936801,41.46519],[-95.962329,41.46281],[-96.011757,41.476212],[-96.019542,41.486617],[-95.997903,41.504789],[-95.992599,41.514174],[-95.999529,41.538679],[-96.005079,41.544004],[-96.019686,41.545743],[-96.027289,41.541081],[-96.034305,41.512853],[-96.040701,41.507076],[-96.05369,41.508859],[-96.07307,41.525052],[-96.08822,41.530595],[-96.09409,41.539265],[-96.093613,41.558271],[-96.081152,41.577289],[-96.085771,41.585746],[-96.109387,41.596871],[-96.117558,41.609999],[-96.116233,41.621574],[-96.100701,41.635507],[-96.095046,41.647365],[-96.099837,41.66103],[-96.120983,41.677861],[-96.121401,41.688522],[-96.111968,41.697773],[-96.082429,41.698159],[-96.073063,41.705004],[-96.079682,41.717962],[-96.10261,41.728016],[-96.106425,41.73789],[-96.102772,41.746339],[-96.079915,41.757895],[-96.077543,41.777824],[-96.064537,41.793002],[-96.075548,41.807811],[-96.107592,41.820685],[-96.110246,41.84885],[-96.142045,41.868865],[-96.148826,41.888132],[-96.161756,41.90182],[-96.160767,41.908044],[-96.136743,41.920826],[-96.144583,41.941544],[-96.133318,41.955732],[-96.1289,41.969727],[-96.141228,41.978063],[-96.156538,41.980137],[-96.184243,41.976696],[-96.192141,41.984461],[-96.183568,41.999987],[-96.194556,42.008662],[-96.215225,42.006701],[-96.223896,41.995456],[-96.236487,41.996428],[-96.241932,42.006965],[-96.223611,42.022652],[-96.223822,42.033346],[-96.238392,42.041088],[-96.261132,42.038974],[-96.271427,42.044988],[-96.279342,42.07028],[-96.267636,42.096177],[-96.2689,42.11359],[-96.279203,42.12348],[-96.310085,42.132523],[-96.319528,42.146647],[-96.342395,42.160491],[-96.349688,42.172043],[-96.348066,42.194747],[-96.35987,42.210545],[-96.358141,42.214088],[-96.336323,42.218922],[-96.323723,42.229887],[-96.330004,42.240224],[-96.328905,42.254734],[-96.336003,42.264806],[-96.365792,42.285875],[-96.369212,42.308344],[-96.375307,42.318339],[-96.407998,42.337408],[-96.417786,42.351449],[-96.417093,42.361443],[-96.408436,42.376092],[-96.41498,42.393442],[-96.413609,42.407894],[-96.387608,42.432494],[-96.380707,42.446394],[-96.385407,42.473094],[-96.396107,42.484095],[-96.409408,42.487595],[-96.474409,42.491895],[-96.476909,42.497795],[-96.473339,42.503537],[-96.477454,42.509589],[-96.490089,42.512441],[-96.49297,42.517282],[-96.479909,42.524195],[-96.476952,42.556079],[-96.498041,42.558153],[-96.498709,42.57087],[-96.489328,42.5708],[-96.485796,42.575001],[-96.49545,42.579474],[-96.494777,42.585741],[-96.499885,42.588539],[-96.509468,42.61273],[-96.517048,42.615343],[-96.525671,42.609312],[-96.531604,42.615148],[-96.518542,42.62035],[-96.516338,42.630435],[-96.537881,42.646446],[-96.542366,42.660736],[-96.559281,42.657903],[-96.556461,42.663939],[-96.566684,42.675942],[-96.576381,42.671302],[-96.575299,42.682665],[-96.596405,42.688514],[-96.59908,42.697296],[-96.61017,42.694568],[-96.629625,42.705102],[-96.624446,42.714294],[-96.624704,42.725497],[-96.631931,42.725086],[-96.638621,42.734921],[-96.630485,42.750378],[-96.620548,42.753534],[-96.620272,42.757124],[-96.632212,42.761512],[-96.633168,42.768325],[-96.61949,42.784034],[-96.604559,42.783034],[-96.595283,42.792982],[-96.590757,42.808255],[-96.596008,42.815044],[-96.585699,42.818041],[-96.577937,42.827645],[-96.581604,42.837521],[-96.571353,42.837155],[-96.565605,42.830434],[-96.560572,42.839373],[-96.552092,42.836057],[-96.549513,42.839143],[-96.554709,42.846142],[-96.545502,42.849956],[-96.54146,42.857682],[-96.550439,42.863171],[-96.549659,42.870281],[-96.537851,42.878475],[-96.540396,42.888877],[-96.526563,42.893755],[-96.542847,42.903737],[-96.537354,42.908791],[-96.541689,42.922576],[-96.525536,42.935511],[-96.516203,42.933769],[-96.52012,42.938183],[-96.500308,42.959391],[-96.505028,42.970844],[-96.515922,42.972886],[-96.520773,42.980385],[-96.512237,42.985937],[-96.509986,42.995126],[-96.49782,42.998143],[-96.49167,43.009707],[-96.499187,43.019213],[-96.510995,43.024701],[-96.509146,43.03668],[-96.518431,43.042068],[-96.510256,43.049917],[-96.490365,43.050789],[-96.476905,43.062383],[-96.463094,43.062981],[-96.458201,43.067554],[-96.454188,43.083379],[-96.462636,43.089614],[-96.460516,43.09494],[-96.436589,43.120842],[-96.450361,43.142237],[-96.458854,43.143356],[-96.466537,43.150281],[-96.464896,43.182034],[-96.473834,43.189804],[-96.470781,43.205099],[-96.475571,43.221054],[-96.496454,43.223652],[-96.519273,43.21769],[-96.535741,43.22764],[-96.56044,43.224219],[-96.568505,43.231554],[-96.571194,43.238961],[-96.552963,43.247281],[-96.552591,43.257769],[-96.582904,43.26769],[-96.586317,43.274319],[-96.577588,43.2788],[-96.580346,43.298204],[-96.553087,43.29286],[-96.530392,43.300034],[-96.526004,43.309999],[-96.534913,43.336473],[-96.524289,43.347214],[-96.527345,43.368109],[-96.521323,43.374607],[-96.521572,43.38564],[-96.524044,43.394762],[-96.529152,43.397735],[-96.537116,43.395063],[-96.573579,43.419228],[-96.569628,43.427527],[-96.575181,43.431756],[-96.592905,43.43317],[-96.602608,43.449649],[-96.600039,43.45708],[-96.584603,43.46961],[-96.586364,43.478251],[-96.580997,43.481384],[-96.590452,43.494298],[-96.598396,43.495074],[-96.598929,43.500441],[-91.217706,43.50055]]]},\"properties\":{\"name\":\"Iowa\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698528","contributors":{"authors":[{"text":"Kalkhoff, Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":150389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}