{"pageNumber":"2326","pageRowStart":"58125","pageSize":"25","recordCount":68857,"records":[{"id":70180025,"text":"70180025 - 1976 - Developing a state water plan: Ground-water conditions in Utah, spring of 1976","interactions":[],"lastModifiedDate":"2017-01-23T12:58:20","indexId":"70180025","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"15","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1976","docAbstract":"<p>This report is the thirteenth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.</p><p>This report, like the others (see references, p. 16), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing water-table configuration are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>This report includes individual discussions of selected major areas of ground-water withdrawal in the State for the calendar year 1975. Water-level fluctuations, however, are described for the period spring 1975 to spring 1976. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Sumison, C., Jibson, W., Bolke, E., Mower, R.W., Herbert, L.R., Cordova, R., Jensen, V., ReMillard, M.D., Sandberg, G.W., and Bjorklund, L., 1976, Developing a state water plan: Ground-water conditions in Utah, spring of 1976: Cooperative Investigations Report 15, viii, 69 p.","productDescription":"viii, 69 p.","numberOfPages":"79","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333715,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333714,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-189"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5887248fe4b08aa8f945abfc","contributors":{"authors":[{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jibson, W.N.","contributorId":27928,"corporation":false,"usgs":true,"family":"Jibson","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":659860,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":659861,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659862,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659863,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659864,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":659865,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"ReMillard, M. D.","contributorId":38645,"corporation":false,"usgs":true,"family":"ReMillard","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":659866,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659867,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659868,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70178750,"text":"70178750 - 1976 - Geophysical prospecting for ground water in Alaska","interactions":[],"lastModifiedDate":"2016-12-06T15:53:38","indexId":"70178750","displayToPublicDate":"2016-03-17T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Geophysical prospecting for ground water in Alaska","docAbstract":"<p>[none]</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Ackermann, H.D., 1976, Geophysical prospecting for ground water in Alaska: Earthquake Information Bulletin (USGS), v. 8, no. 2, p. 18-20.","productDescription":"3 p.","startPage":"18","endPage":"20","numberOfPages":"3","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":331604,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5847dc82e4b06d80b7af6ae9","contributors":{"editors":[{"text":"Pistrang, Marvin A.","contributorId":86224,"corporation":false,"usgs":true,"family":"Pistrang","given":"Marvin A.","affiliations":[],"preferred":false,"id":655039,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Spall, Henry","contributorId":77933,"corporation":false,"usgs":true,"family":"Spall","given":"Henry","email":"","affiliations":[],"preferred":false,"id":655040,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Ackermann, Hans D.","contributorId":44539,"corporation":false,"usgs":false,"family":"Ackermann","given":"Hans","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":655038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174208,"text":"wri33 - 1976 - Water quality characteristics of six small lakes in Missouri: Mo. Dept. of Natural Resources.","interactions":[],"lastModifiedDate":"2016-08-10T11:00:35","indexId":"wri33","displayToPublicDate":"2016-02-17T02:45:00","publicationYear":"1976","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":"33","title":"Water quality characteristics of six small lakes in Missouri: Mo. Dept. of Natural Resources.","docAbstract":"<p>A study of six small lakes, representative of those in the major physiographic regions of Missouri, shows variation in physical. chemical, and biological characteristics related to their location in the Slate. For example, because of climatic differences, ice cover and winter stratification are more prevalent in northern Missouri. Summer stratification lasts about one month longer in the southern than in the northern part of the State. Because of the difference in geology. lake water in the Plains area is more mineralized than in the Ozarks. Different geology and land use generally account for more sedimentation of Plains Jakes. Lakes in the Plains area usually receive enough nutrients to be classified as mesouophic or eutrophic while those in the Ozarks receive less nutrients from natural sources and are often oligotrophic or mesotrophic. However, as seen from one of the study lakes, an oligotrophic lake can be made quite productive through the application of commercial fertilizers within the lake.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri33","collaboration":"Prepared in cooperation with Missouri Department of Natural Resources: Division of Geology and Land Survey","usgsCitation":"Barks, J.H., 1976, Water quality characteristics of six small lakes in Missouri: Mo. Dept. of Natural Resources.: U.S. Geological Survey Water-Resources Investigations Report 33, vi, 42 p., https://doi.org/10.3133/wri33.","productDescription":"vi, 42 p.","startPage":"i","endPage":"42","numberOfPages":"50","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":324632,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.545006,36.336809],[-89.605668,36.342234],[-89.615841,36.336085],[-89.620255,36.323006],[-89.611819,36.309088],[-89.578492,36.288317],[-89.554289,36.277751],[-89.539487,36.277368],[-89.534507,36.261802],[-89.539229,36.248821],[-89.562206,36.250909],[-89.577544,36.242262],[-89.602374,36.238106],[-89.642182,36.249486],[-89.678046,36.248284],[-89.695235,36.252766],[-89.705328,36.239898],[-89.69263,36.224959],[-89.607004,36.171179],[-89.591605,36.144096],[-89.59307,36.129699],[-89.601936,36.11947],[-89.666598,36.095802],[-89.678821,36.084636],[-89.688577,36.029238],[-89.706932,36.000981],[-90.37789,35.995683],[-90.351732,36.025347],[-90.34909,36.040131],[-90.339343,36.047112],[-90.333261,36.067504],[-90.320746,36.071326],[-90.320662,36.087138],[-90.29991,36.098236],[-90.294492,36.112949],[-90.266256,36.120559],[-90.235585,36.139474],[-90.231386,36.147348],[-90.23537,36.159153],[-90.220425,36.184764],[-90.21128,36.183392],[-90.188189,36.20536],[-90.152497,36.215582],[-90.14224,36.227522],[-90.126366,36.229367],[-90.130114,36.240307],[-90.118219,36.253491],[-90.114922,36.265595],[-90.086471,36.271531],[-90.06398,36.303038],[-90.081961,36.322097],[-90.074074,36.342895],[-90.077695,36.348478],[-90.066297,36.3593],[-90.064514,36.382085],[-90.078671,36.399116],[-90.138512,36.413952],[-90.134231,36.422827],[-90.143743,36.424433],[-90.143798,36.428483],[-90.134136,36.436602],[-90.137323,36.455411],[-90.141101,36.461791],[-90.155804,36.463555],[-90.152888,36.47093],[-90.142222,36.470554],[-90.143683,36.476029],[-90.158838,36.479558],[-90.159305,36.492446],[-90.152481,36.497952],[-94.617919,36.499414],[-94.617975,37.722176],[-94.607354,39.113444],[-94.589933,39.140403],[-94.591933,39.155003],[-94.608834,39.160503],[-94.640035,39.153103],[-94.662435,39.157603],[-94.663835,39.179103],[-94.680336,39.184303],[-94.714137,39.170403],[-94.741938,39.170203],[-94.763138,39.179903],[-94.781518,39.206146],[-94.811663,39.206594],[-94.831679,39.215938],[-94.835056,39.220658],[-94.825663,39.241729],[-94.831471,39.256273],[-94.84632,39.268481],[-94.887056,39.28648],[-94.905329,39.311952],[-94.910017,39.352543],[-94.88136,39.370383],[-94.879281,39.37978],[-94.885026,39.389801],[-94.901823,39.392798],[-94.92311,39.384492],[-94.942039,39.389499],[-94.946293,39.405646],[-94.972952,39.421705],[-94.982144,39.440552],[-95.0375,39.463689],[-95.045716,39.472459],[-95.052177,39.499996],[-95.082714,39.516712],[-95.109304,39.542285],[-95.113077,39.559133],[-95.103228,39.577783],[-95.089515,39.581028],[-95.064519,39.577115],[-95.049277,39.589583],[-95.046361,39.599557],[-95.055152,39.621657],[-95.053367,39.630347],[-95.027644,39.665454],[-95.018318,39.672869],[-94.984149,39.67785],[-94.971317,39.68641],[-94.971206,39.729305],[-94.965318,39.739065],[-94.948726,39.745593],[-94.902612,39.724202],[-94.875643,39.730494],[-94.862943,39.742994],[-94.860743,39.763094],[-94.869644,39.772894],[-94.912293,39.759338],[-94.934262,39.773642],[-94.935206,39.78313],[-94.929654,39.788282],[-94.884084,39.794234],[-94.875944,39.813294],[-94.878677,39.826522],[-94.886933,39.833098],[-94.916918,39.836138],[-94.942567,39.856602],[-94.928466,39.876344],[-94.929574,39.888754],[-94.95154,39.900533],[-94.986975,39.89667],[-95.00844,39.900596],[-95.024389,39.891202],[-95.027931,39.871522],[-95.037767,39.865542],[-95.085003,39.861883],[-95.128166,39.874165],[-95.140601,39.881688],[-95.143802,39.901918],[-95.149657,39.905948],[-95.179453,39.900062],[-95.199347,39.902709],[-95.206326,39.912121],[-95.20069,39.928155],[-95.204428,39.938949],[-95.250254,39.948644],[-95.269886,39.969396],[-95.302507,39.984357],[-95.315271,40.01207],[-95.356876,40.031522],[-95.387195,40.02677],[-95.40726,40.033112],[-95.416824,40.043235],[-95.42164,40.058952],[-95.409856,40.07432],[-95.407591,40.09803],[-95.394216,40.108263],[-95.39284,40.115887],[-95.398667,40.126419],[-95.428749,40.135577],[-95.436348,40.15872],[-95.460746,40.169173],[-95.479193,40.185652],[-95.482757,40.197346],[-95.469718,40.227908],[-95.477501,40.24272],[-95.490333,40.248966],[-95.521925,40.24947],[-95.552473,40.261904],[-95.556325,40.267714],[-95.550966,40.285947],[-95.562157,40.297359],[-95.581787,40.29958],[-95.610439,40.31397],[-95.642262,40.306025],[-95.657328,40.310856],[-95.653729,40.322582],[-95.625204,40.334288],[-95.623728,40.346567],[-95.641027,40.366399],[-95.643934,40.386849],[-95.659134,40.40869],[-95.65819,40.44188],[-95.693133,40.469396],[-95.699969,40.505275],[-95.661687,40.517309],[-95.652262,40.538114],[-95.655848,40.546609],[-95.671754,40.562626],[-95.678718,40.56256],[-95.694147,40.556942],[-95.69505,40.533124],[-95.708591,40.521551],[-95.722444,40.528118],[-95.75711,40.52599],[-95.769281,40.536656],[-95.763366,40.550797],[-95.773549,40.578205],[-95.765645,40.585208],[-94.632035,40.571186],[-94.080463,40.572899],[-92.689854,40.589884],[-91.729115,40.61364],[-91.716769,40.59853],[-91.686357,40.580875],[-91.690804,40.559893],[-91.681714,40.553035],[-91.6219,40.542292],[-91.618028,40.53403],[-91.621353,40.510072],[-91.590817,40.492292],[-91.574746,40.465664],[-91.52509,40.457845],[-91.524053,40.448437],[-91.533623,40.43832],[-91.519935,40.433673],[-91.526555,40.419872],[-91.522333,40.409648],[-91.498093,40.401926],[-91.489816,40.404317],[-91.484507,40.3839],[-91.465116,40.385257],[-91.465009,40.376223],[-91.452458,40.375501],[-91.441243,40.386255],[-91.419422,40.378264],[-91.444833,40.36317],[-91.46214,40.342414],[-91.492727,40.278217],[-91.490524,40.259498],[-91.505828,40.238839],[-91.505495,40.195606],[-91.512974,40.181062],[-91.508224,40.157665],[-91.510322,40.127994],[-91.489606,40.057435],[-91.494878,40.036453],[-91.465315,39.983995],[-91.41936,39.927717],[-91.41988,39.916533],[-91.443513,39.893583],[-91.446922,39.883034],[-91.436051,39.84551],[-91.377971,39.811273],[-91.361571,39.787548],[-91.370009,39.732524],[-91.3453,39.709402],[-91.27614,39.665759],[-91.229317,39.620853],[-91.181936,39.602677],[-91.174651,39.593313],[-91.168419,39.564928],[-91.153628,39.548248],[-91.100307,39.538695],[-91.079769,39.507728],[-91.064305,39.494643],[-91.059439,39.46886],[-91.03827,39.448436],[-90.993789,39.422959],[-90.940766,39.403984],[-90.928745,39.387544],[-90.904862,39.379403],[-90.893777,39.367343],[-90.8475,39.345272],[-90.816851,39.320496],[-90.793461,39.309498],[-90.751599,39.265432],[-90.72996,39.255894],[-90.717113,39.213912],[-90.707902,39.15086],[-90.686051,39.117785],[-90.681086,39.10059],[-90.681994,39.090066],[-90.712541,39.057064],[-90.71158,39.046798],[-90.678193,38.991851],[-90.675949,38.96214],[-90.657254,38.92027],[-90.639917,38.908272],[-90.625122,38.888654],[-90.583388,38.86903],[-90.555693,38.870785],[-90.500117,38.910408],[-90.486974,38.925982],[-90.482419,38.94446],[-90.472122,38.958838],[-90.440078,38.967364],[-90.395816,38.960037],[-90.309454,38.92412],[-90.250248,38.919344],[-90.109407,38.843548],[-90.123107,38.798048],[-90.166409,38.772649],[-90.176309,38.754449],[-90.20991,38.72605],[-90.20921,38.70275],[-90.18641,38.67475],[-90.181325,38.660381],[-90.17801,38.63375],[-90.18451,38.611551],[-90.196011,38.594451],[-90.222112,38.576451],[-90.260314,38.528352],[-90.285215,38.443453],[-90.295316,38.426753],[-90.349743,38.377609],[-90.368219,38.340254],[-90.373929,38.281853],[-90.353902,38.213855],[-90.331554,38.18758],[-90.290765,38.170453],[-90.274928,38.157615],[-90.243116,38.112669],[-90.218708,38.094365],[-90.17222,38.069636],[-90.158533,38.074735],[-90.130788,38.062341],[-90.126612,38.043981],[-90.11052,38.026547],[-90.08826,38.015772],[-90.059367,38.015543],[-90.051357,38.003584],[-90.03241,37.995258],[-90.00011,37.964563],[-89.978919,37.962791],[-89.942099,37.970121],[-89.933797,37.959143],[-89.925085,37.960021],[-89.932467,37.947497],[-89.959646,37.940196],[-89.974918,37.926719],[-89.952499,37.883218],[-89.923185,37.870672],[-89.901832,37.869822],[-89.844786,37.905572],[-89.799333,37.881517],[-89.796087,37.859505],[-89.786369,37.851734],[-89.782035,37.855092],[-89.739873,37.84693],[-89.71748,37.825724],[-89.669644,37.799922],[-89.660227,37.781032],[-89.667993,37.759484],[-89.665546,37.752095],[-89.64953,37.745498],[-89.617278,37.74972],[-89.612478,37.740036],[-89.596566,37.732886],[-89.583316,37.713261],[-89.516685,37.692762],[-89.51204,37.680985],[-89.517718,37.641217],[-89.478399,37.598869],[-89.47603,37.590226],[-89.486062,37.580853],[-89.519808,37.582748],[-89.521925,37.560735],[-89.517051,37.537278],[-89.475525,37.471388],[-89.439769,37.4372],[-89.421054,37.387668],[-89.432836,37.347056],[-89.489005,37.333368],[-89.511842,37.310825],[-89.51834,37.285497],[-89.489915,37.251315],[-89.470525,37.253357],[-89.458827,37.248661],[-89.467631,37.2182],[-89.456105,37.18812],[-89.42558,37.138235],[-89.37871,37.094586],[-89.375712,37.080505],[-89.384681,37.048251],[-89.362397,37.030156],[-89.322982,37.01609],[-89.29213,36.992189],[-89.278628,36.98867],[-89.263527,37.00005],[-89.257608,37.015496],[-89.260003,37.023288],[-89.304752,37.047565],[-89.310819,37.057897],[-89.30829,37.068371],[-89.259936,37.064071],[-89.25493,37.072014],[-89.234053,37.037277],[-89.200793,37.016164],[-89.192097,36.979995],[-89.185491,36.973518],[-89.170008,36.970298],[-89.125069,36.983499],[-89.109498,36.976563],[-89.099594,36.964543],[-89.100762,36.944002],[-89.117567,36.887356],[-89.131944,36.857437],[-89.137969,36.847349],[-89.1704,36.841522],[-89.178888,36.831368],[-89.179229,36.812915],[-89.171069,36.798119],[-89.155891,36.789126],[-89.12353,36.785309],[-89.116563,36.767557],[-89.126134,36.751735],[-89.166888,36.759633],[-89.184523,36.753638],[-89.197808,36.739412],[-89.19948,36.716045],[-89.169522,36.688878],[-89.169467,36.674596],[-89.15908,36.666352],[-89.197654,36.628936],[-89.202607,36.601576],[-89.217447,36.576159],[-89.236542,36.566824],[-89.258318,36.564948],[-89.278935,36.577699],[-89.326731,36.632186],[-89.365548,36.625059],[-89.375453,36.615719],[-89.382762,36.583603],[-89.41977,36.493896],[-89.448468,36.46442],[-89.464153,36.457189],[-89.486215,36.46162],[-89.494248,36.475972],[-89.465888,36.529946],[-89.467761,36.546847],[-89.479093,36.568206],[-89.500076,36.576305],[-89.542459,36.580566],[-89.566817,36.564216],[-89.571241,36.547343],[-89.560344,36.525436],[-89.519501,36.475419],[-89.523427,36.456572],[-89.543406,36.43877],[-89.545255,36.427079],[-89.509722,36.373626],[-89.519,36.3486],[-89.545006,36.336809]]]},\"properties\":{\"name\":\"Missouri\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5774f310e4b07dd077c6aecc","contributors":{"authors":[{"text":"Barks, James H.","contributorId":73569,"corporation":false,"usgs":true,"family":"Barks","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":641316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70157469,"text":"70157469 - 1976 - Ground-water resources and geology of St. Croix County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:36:02","indexId":"70157469","displayToPublicDate":"2015-02-09T08:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"32","title":"Ground-water resources and geology of St. Croix County, Wisconsin","docAbstract":"<p>The increasing need for good-quality ground water in St. Croix County, caused by a steadily increasing population, can be met from the sand-and-gravel and sandstone aquifers. As much as 15 gallons per minute (0.95 litres per second) can be obtained from wells almost everywhere in the county. Yields of more than 1,000 gallons per minute (63 litres per second) are available from glacial deposits and alluvium where there is sufficient thickness of saturated sand and gravel. The sandstone aquifer underlies the entire county and is more than 1,000 feet (300 metres) thick in the southwest near River Falls. In St. Croix County the sandstone aquifer is all bedrock younger than Precambrian age and includes, in ascending order, from oldest to youngest, sandstones of Cambrian age (in ascending order, the Mount Simon, Eau Claire, Galesville, and Franconia Sandstones, and the Trempealeau Formation); and the Prairie du Chien Group, St. Peter Sandstone, and Galena-Platteville unit (Platteville and Decorah Formations and Galena Dolomite, undifferentiated), all of Ordovician age. This aquifer is capable of yielding more than 1,000 gallons per minute (63 litres per second) to wells in much of the county and is the principal source of municipal water.</p>\n<p>The chemical quality of water from the two aquifers is similar. The water from both aquifers is hard to very hard, having a median hardness between 180 and 190 milligrams per litre. Iron and manganese are locally present in botherSome amounts (combined total exceeding 0.3 milligrams per litre). Nitrate is a minor problem in both aquifers, with median concentrations more than 10 milligrams per litre, possibly indicating some contamination of ground water by organic matter.</p>\n<p>About 3.83 million gallons per day (0.168 cubic metres per second) of ground water was pumped in the county in 1974, of which 94 percent was from the sandstone aquifer. About 44 percent of the total water pumped was for industrial and commercial use, 42 percent for residential</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared in cooperation with Wisconsin Geological and Natural History Survey","usgsCitation":"Borman, R.G., 1976, Ground-water resources and geology of St. Croix County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 32, vii, 30.","productDescription":"vii, 30","numberOfPages":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308480,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350392,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic32/"}],"country":"United States","state":"Wisconsin","county":"St. Croix County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-92.1564,45.2097],[-92.1568,45.1215],[-92.136,45.121],[-92.1364,45.0315],[-92.1356,44.9447],[-92.1367,44.8579],[-92.2584,44.8582],[-92.3752,44.8622],[-92.4969,44.8622],[-92.6193,44.8626],[-92.7411,44.862],[-92.7644,44.8622],[-92.7637,44.8647],[-92.763,44.8671],[-92.7628,44.8716],[-92.7632,44.8753],[-92.7632,44.8759],[-92.7654,44.8795],[-92.7685,44.8842],[-92.7689,44.8848],[-92.7698,44.8865],[-92.7721,44.8905],[-92.7738,44.8933],[-92.7743,44.895],[-92.775,44.8982],[-92.7729,44.901],[-92.7707,44.9023],[-92.7677,44.9036],[-92.767,44.9039],[-92.7645,44.9046],[-92.7606,44.9068],[-92.7569,44.9105],[-92.7547,44.9159],[-92.7534,44.9237],[-92.753,44.9362],[-92.753,44.9369],[-92.7523,44.9481],[-92.7526,44.9522],[-92.7527,44.9527],[-92.7547,44.9571],[-92.7593,44.9639],[-92.7643,44.9707],[-92.7646,44.9711],[-92.7652,44.9723],[-92.7672,44.9765],[-92.7686,44.9796],[-92.7688,44.9817],[-92.7694,44.9909],[-92.7683,44.9997],[-92.7682,45.0005],[-92.7677,45.0023],[-92.7657,45.0108],[-92.7639,45.0196],[-92.7639,45.0237],[-92.7645,45.0265],[-92.7664,45.0292],[-92.7683,45.0325],[-92.7707,45.0344],[-92.7741,45.037],[-92.7745,45.0373],[-92.7793,45.0397],[-92.7837,45.0421],[-92.7881,45.0453],[-92.7926,45.0481],[-92.7952,45.0499],[-92.7984,45.0531],[-92.8005,45.0567],[-92.8016,45.0597],[-92.8018,45.0634],[-92.8019,45.0647],[-92.8015,45.0668],[-92.8008,45.07],[-92.8001,45.0723],[-92.7982,45.0746],[-92.7955,45.0768],[-92.795,45.0772],[-92.7917,45.0791],[-92.7885,45.0806],[-92.7871,45.0815],[-92.7847,45.083],[-92.7803,45.0849],[-92.7743,45.0889],[-92.7689,45.0927],[-92.7624,45.0972],[-92.7596,45.0995],[-92.7591,45.0999],[-92.7548,45.1026],[-92.7513,45.1045],[-92.7472,45.1073],[-92.7467,45.1076],[-92.7446,45.11],[-92.7433,45.112],[-92.7422,45.1135],[-92.7415,45.1172],[-92.7426,45.121],[-92.7441,45.1264],[-92.7459,45.1309],[-92.7484,45.1373],[-92.749,45.1419],[-92.7489,45.1446],[-92.7484,45.1483],[-92.7473,45.1515],[-92.7475,45.1551],[-92.7483,45.1597],[-92.7472,45.1634],[-92.7475,45.1668],[-92.748,45.1698],[-92.7493,45.173],[-92.7522,45.1759],[-92.7557,45.178],[-92.7589,45.1812],[-92.7622,45.1847],[-92.7629,45.1853],[-92.764,45.1895],[-92.7637,45.1972],[-92.7632,45.2009],[-92.7619,45.2041],[-92.7603,45.2065],[-92.76,45.2069],[-92.7579,45.2097],[-92.6517,45.21],[-92.53,45.21],[-92.4063,45.2091],[-92.2839,45.2094],[-92.1564,45.2097]]]},\"properties\":{\"name\":\"Saint Croix\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ec9e4b058f706e512d7","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573255,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","interactions":[{"subject":{"id":42244,"text":"ofr76463 - 1976 - Bedrock topography map of Walworth County, Wisconsin","indexId":"ofr76463","publicationYear":"1976","noYear":false,"title":"Bedrock topography map of Walworth County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","indexId":"70047687","publicationYear":"1976","noYear":false,"title":"Ground-water resources and geology of Walworth County, Wisconsin"},"id":1},{"subject":{"id":42264,"text":"ofr76462 - 1976 - Bedrock geology map of Walworth County, Wisconsin","indexId":"ofr76462","publicationYear":"1976","noYear":false,"title":"Bedrock geology map of Walworth County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","indexId":"70047687","publicationYear":"1976","noYear":false,"title":"Ground-water resources and geology of Walworth County, Wisconsin"},"id":2},{"subject":{"id":44023,"text":"ofr76464 - 1976 - Water-table map of Walworth County, Wisconsin, 1973","indexId":"ofr76464","publicationYear":"1976","noYear":false,"title":"Water-table map of Walworth County, Wisconsin, 1973"},"predicate":"SUPERSEDED_BY","object":{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","indexId":"70047687","publicationYear":"1976","noYear":false,"title":"Ground-water resources and geology of Walworth County, Wisconsin"},"id":3},{"subject":{"id":46009,"text":"ofr76465 - 1976 - Map showing thickness of unconsolidated materials of Walworth County, Wisconsin","indexId":"ofr76465","publicationYear":"1976","noYear":false,"title":"Map showing thickness of unconsolidated materials of Walworth County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","indexId":"70047687","publicationYear":"1976","noYear":false,"title":"Ground-water resources and geology of Walworth County, Wisconsin"},"id":4}],"lastModifiedDate":"2018-01-08T19:59:35","indexId":"70047687","displayToPublicDate":"2013-01-01T13:21:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"34","title":"Ground-water resources and geology of Walworth County, Wisconsin","docAbstract":"Population growth in Walworth County, Wisconsin, requires an increasing amount of ground water. Good quality water is available from the sand-and gravel, Niagara, Galena-Platteville, and sandstone aquifers in the county. As much as 15 gallons per minute (0.95 liters per second) can be obtained from individual wells almost everywhere in the county. Well yields of 1,000 gallons per minute (63 liters per second) are available from glacial drift where it contains sufficient thickness of saturated sand and gravel. The sand-and-gravel aquifer is an important source of municipal water. Estimated well yields from most of the Niagara aquifer, a Silurian age dolomite as thick as 125 feet (38.1 meters), exceed 100 gallons per minute (6.3 liters per second). The Niagara aquifer occurs in the eastern third of the county. The Galena-Platteville aquifer, chiefly dolomite, is present in the western half of the county where it is as thick as 325 feet (99.1 meters). Estimated yields from this aquifer exceed 500 gallons per minute (32 liters per second). The sandstone aquifer underlies the entire county and ranges from less than 800 feet (240 meters) thick in the northwest corner to more than 2,200 feet (670 meters) in the east. This aquifer is capable of yielding 1,000 gallons per minute (63 liters per second) to individual wells and is a principal source of municipal water.","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared by United States Department of the Interior Geological Survey in cooperation with Wisconsin Geological and Natural History Survey","usgsCitation":"Borman, R.G., 1976, Ground-water resources and geology of Walworth County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 34, vii, 45 p.","productDescription":"vii, 45 p.","numberOfPages":"54","costCenters":[],"links":[{"id":276760,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047687.JPG"},{"id":276759,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/ic34/"}],"country":"United States","state":"Wisconsin","county":"Walworth County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.776008,42.492041 ], [ -88.776008,42.84625 ], [ -88.301522,42.84625 ], [ -88.301522,42.492041 ], [ -88.776008,42.492041 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e34e4b0b08f446198e6","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":482722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047436,"text":"70047436 - 1976 - Geology and ground-water resources of northern Mercer County, Pennsylvania","interactions":[{"subject":{"id":52599,"text":"ofr67127 - 1967 - Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania","indexId":"ofr67127","publicationYear":"1967","noYear":false,"title":"Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047436,"text":"70047436 - 1976 - Geology and ground-water resources of northern Mercer County, Pennsylvania","indexId":"70047436","publicationYear":"1976","noYear":false,"title":"Geology and ground-water resources of northern Mercer County, Pennsylvania"},"id":1},{"subject":{"id":55850,"text":"ofr68158 - 1968 - Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania","indexId":"ofr68158","publicationYear":"1968","noYear":false,"title":"Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047436,"text":"70047436 - 1976 - Geology and ground-water resources of northern Mercer County, Pennsylvania","indexId":"70047436","publicationYear":"1976","noYear":false,"title":"Geology and ground-water resources of northern Mercer County, Pennsylvania"},"id":2}],"lastModifiedDate":"2013-08-06T15:25:36","indexId":"70047436","displayToPublicDate":"2013-01-01T09:18:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"33","title":"Geology and ground-water resources of northern Mercer County, Pennsylvania","docAbstract":"The Shenango and Stoneboro 15-minute quadrangles are in northwestern Pennsylvania and are about 60 miles north of Pitts burgh. These two quadrangles comprise the following 7%-minute quadrangles: Greenville West, Greenville East, Sharpsville, Fredonia, Hadley, New Lebanon, Jackson Center, and Sandy Lake. The area covered by the two quadrangles includes the northern two thirds of Mercer County and a small amount of adjoining southern Crawford County.","language":"English","publisher":"Pennsylvania Bureau of Topographic and Geologic Survey","collaboration":"Prepared by the U. S. Geological Survey, Water Resources Division, in cooperation with the Pennsylvania Geological Survey","usgsCitation":"Schiner, G., and Kimmel, G., 1976, Geology and ground-water resources of northern Mercer County, Pennsylvania: Water Resource Report 33, 136 p.; Maps: 2 Sheets.","productDescription":"136 p.; Maps: 2 Sheets","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276094,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047436.PNG"},{"id":276093,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_016321.zip"}],"country":"United States","state":"Pennsylvania","county":"Mercer County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.518715,41.069935 ], [ -80.518715,41.490429 ], [ -79.998161,41.490429 ], [ -79.998161,41.069935 ], [ -80.518715,41.069935 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae3e4b0e21cafa49c47","contributors":{"authors":[{"text":"Schiner, G. R.","contributorId":85175,"corporation":false,"usgs":true,"family":"Schiner","given":"G. R.","affiliations":[],"preferred":false,"id":482040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimmel, G.E.","contributorId":23976,"corporation":false,"usgs":true,"family":"Kimmel","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":482039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042717,"text":"70042717 - 1976 - Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","interactions":[{"subject":{"id":15062,"text":"ofr75615 - 1975 - Digital-model analysis of the effects of water-use alternatives on spring discharges, Gooding and Jerome Counties, Idaho","indexId":"ofr75615","publicationYear":"1975","noYear":false,"title":"Digital-model analysis of the effects of water-use alternatives on spring discharges, Gooding and Jerome Counties, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70042717,"text":"70042717 - 1976 - Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","indexId":"70042717","publicationYear":"1976","noYear":false,"title":"Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho"},"id":1}],"lastModifiedDate":"2013-01-18T14:10:29","indexId":"70042717","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":301,"text":"Water Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"42","title":"Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","docAbstract":"Springs discharging from the Snake Plain aquifer contribute approximately 6,000 cubic feet per second (170 cubic metres per second) to flow in the Snake River between Milner and King Hill. Before irrigation began on the Snake River Plain north and east of the springs, total spring discharge was about 4,200 cubic feet per second (120 cubic meters per second). Increasing amounts of irrigated acreage from the early 1900's to the mid-1940's contributed more irrigation-return water to the aquifer resulting in increased discharge at the springs. Maximum discharge of about 6,800 cubic feet per second (190 cubic metres per second) occurred during the late 1940's and early 1950's. Increased use of pumped ground water for irrigation and changing irrigation practices have since resulted in a decline in spring discharge.","language":"English","publisher":"Idaho Department of Water Resources","publisherLocation":"Boise, ID","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Idaho Department of Water Resources, Statehouse, Boise, Idaho","usgsCitation":"Moreland, J.A., 1976, Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho: Water Information Bulletin 42, vi, 46 p.; ill.; maps.","productDescription":"vi, 46 p.; ill.; maps","startPage":"i","endPage":"46","numberOfPages":"53","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":265963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265962,"type":{"id":11,"text":"Document"},"url":"https://www.idwr.idaho.gov/WaterInformation/Publications/wib/wib42-water-use_alternatives.pdf"}],"country":"United States","state":"Idaho","county":"Gooding County;Jerome County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.0875,42.4981 ], [ -115.0875,43.2001 ], [ -113.9308,43.2001 ], [ -113.9308,42.4981 ], [ -115.0875,42.4981 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50fa7d53e4b061045bf9ac32","contributors":{"authors":[{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":472107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042515,"text":"70042515 - 1976 - Saline water in the Little Arkansas River Basin area, south-central Kansas","interactions":[{"subject":{"id":17647,"text":"ofr76257 - 1976 - Saline water in the Little Arkansas River Basin area, south-central Kansas","indexId":"ofr76257","publicationYear":"1976","noYear":false,"title":"Saline water in the Little Arkansas River Basin area, south-central Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":70042515,"text":"70042515 - 1976 - Saline water in the Little Arkansas River Basin area, south-central Kansas","indexId":"70042515","publicationYear":"1976","noYear":false,"title":"Saline water in the Little Arkansas River Basin area, south-central Kansas"},"id":1}],"lastModifiedDate":"2013-01-10T14:49:37","indexId":"70042515","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":243,"text":"Chemical Quality Series","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"3","title":"Saline water in the Little Arkansas River Basin area, south-central Kansas","docAbstract":"Ground water in unconsolidated deposits of Pleistocene age in part of the Little Arkansas River basin has been polluted by the influx of saline water. The source of the saline water generally is oil-field brine that leaked from disposal ponds on the land surface. Locally, pollution by saline water also has been caused by upwelling of oil-field brine injected under pressure into the \"lost-circulation zone\" of the Lower Permian Wellington Formation and, possibly, by leakage of brine from corroded or improperly cased disposal wells. Anomalously high concentrations of chloride ion in some reaches of the Little Arkansas River probably can be attributed to pollution by municipal wastes rather than from inflow of saline ground water. Hydraulic connection exists between the \"lost-circulation zone\" and unconsolidated deposits, as evidenced by the continuing development of sinkholes, by the continuing discharge of saline water through springs and seeps along the Arkansas River south of the Little Arkansas River basin and by changes in the chloride concentration in water pumped from wells in the \"lost-circulation zone.\" The hydraulic head in the \"lost-circulation zone\" is below the base of the unconsolidated deposits, and much below the potentiometric surface of the aquifer in those deposits. Any movement of water, therefore, would be downward from the \"fresh-water\" aquifer to the saline \"lost-circulation zone.\"","language":"English","publisher":"University of Kansas Publications","publisherLocation":"Lawrence, KS","collaboration":"Prepared cooperatively by the Kansas Geological Survey and the U.S. Geological Survey","usgsCitation":"Leonard, R., and Kleinschmidt, M.K., 1976, Saline water in the Little Arkansas River Basin area, south-central Kansas: Chemical Quality Series 3, iii, 24 p.; ill.; maps.","productDescription":"iii, 24 p.; ill.; maps","startPage":"i","endPage":"24","numberOfPages":"28","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":265515,"type":{"id":11,"text":"Document"},"url":"https://www.kgs.ku.edu/Publications/Bulletins/CQS3/cqs3.pdf"},{"id":265516,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Little Arkansas River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.05,37.0 ], [ -102.05,40.0 ], [ -94.59,40.0 ], [ -94.59,37.0 ], [ -102.05,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd714ae4b0b29085107974","contributors":{"authors":[{"text":"Leonard, Robert B.","contributorId":14407,"corporation":false,"usgs":true,"family":"Leonard","given":"Robert B.","affiliations":[],"preferred":false,"id":471676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kleinschmidt, Melvin K.","contributorId":32793,"corporation":false,"usgs":true,"family":"Kleinschmidt","given":"Melvin","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":471677,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042576,"text":"70042576 - 1976 - Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","interactions":[{"subject":{"id":16567,"text":"ofr75322 - 1975 - Geology and geophysics of the southern Raft River valley geothermal area, Idaho, U.S.A.","indexId":"ofr75322","publicationYear":"1975","noYear":false,"title":"Geology and geophysics of the southern Raft River valley geothermal area, Idaho, U.S.A."},"predicate":"SUPERSEDED_BY","object":{"id":70042576,"text":"70042576 - 1976 - Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","indexId":"70042576","publicationYear":"1976","noYear":false,"title":"Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA"},"id":1}],"lastModifiedDate":"2017-11-03T11:01:24","indexId":"70042576","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","docAbstract":"The Raft River valley, near the boundary of the Snake River plain with the Basin and Range province, is a north-trending late Cenozoic downwarp bounded by faults on the west, south, and east. Pleistocene alluvium and Miocene-Pliocene tuffaceous sediments, conglomerate, and felsic volcanic rocks aggregate 2 km in thickness. Large gravity, magnetic, and total field resistivity highs probably indicate a buried igneous mass that is too old to serve as a heat source. Differing seismic velocities relate to known or inferred structures and to a suspected shallow zone of warm water. Resistivity anomalies reflect differences of both composition and degree of alteration of Cenozoic rocks. Resistivity soundings show a 2 to 5 ohm·m unit with a thickness of 1 km beneath a large part of the valley, and the unit may indicate partly hot water and partly clayey sediments. Observed self-potential anomalies are believed to indicate zones where warm water rises toward the surface. Boiling wells at Bridge, Idaho are near the intersection of north-northeast normal faults which have moved as recently as the late (?) Pleistocene, and an east-northeast structure, probably a right-lateral fault. Deep circulation of ground water in this region of relatively high heat flow and upwelling along faults is the probable cause of the thermal anomaly.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Energy Research and Development Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Williams, P., Mabey, D.R., Zohdy, A.A., Ackermann, H.D., Hoover, D.B., Pierce, K.L., and Oriel, S.S., 1976, Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA, <i>in</i> Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975, v. 2, p. 1273-1282.","productDescription":"10 p.","startPage":"1273","endPage":"1282","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":265587,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Raft River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,42.0 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,42.0 ], [ -117.24,42.0 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f293f4e4b0c9e41dd3ab73","contributors":{"authors":[{"text":"Williams, Paul L.","contributorId":91086,"corporation":false,"usgs":true,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":471858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mabey, Don R.","contributorId":43741,"corporation":false,"usgs":true,"family":"Mabey","given":"Don","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":471855,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zohdy, Adel A. R.","contributorId":61799,"corporation":false,"usgs":true,"family":"Zohdy","given":"Adel","email":"","middleInitial":"A. R.","affiliations":[],"preferred":false,"id":471856,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ackermann, Hans D.","contributorId":44539,"corporation":false,"usgs":false,"family":"Ackermann","given":"Hans","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":471854,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":471857,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pierce, Kenneth L. kpierce@usgs.gov","contributorId":1609,"corporation":false,"usgs":true,"family":"Pierce","given":"Kenneth","email":"kpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":471853,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Oriel, Steven S.","contributorId":108079,"corporation":false,"usgs":true,"family":"Oriel","given":"Steven","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":471859,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70043279,"text":"70043279 - 1976 - Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah","interactions":[{"subject":{"id":13217,"text":"ofr75215 - 1975 - Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal Systems, Duchesne County, Utah","indexId":"ofr75215","publicationYear":"1975","noYear":false,"title":"Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal Systems, Duchesne County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043279,"text":"70043279 - 1976 - Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah","indexId":"70043279","publicationYear":"1976","noYear":false,"title":"Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T13:36:59","indexId":"70043279","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","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":"50","title":"Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah","docAbstract":"This report describes the study of the Rocky Point Canal system in the vicinity of Duchesne and the Grey Mountain-Pleasant Valley Canal system between Duchesne and Myton, in the Uinta Basin, Duchesne County, Utah. The Rocky Point Canal diverts from the left bank of the Duchesne River about 4 mi north of Duchesne. This canal splits into the upper Rocky Point Canal and the lower Rocky Point Canal about 5.2 mi below its head. The Grey Mountain Canal diverts from the right bank of the Duchesne River about 6 mi east of Duchesne. At a point about 7.6 mi below the head, the Pleasant Valley Canal diverts from the right bank of the Grey Mountain Canal.","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":"Cruff, R., and Hood, J.W., 1976, Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah: Technical Publication 50, vi, 53 p.","productDescription":"vi, 53 p.","numberOfPages":"64","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267164,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331874,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-280"},{"id":331875,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009c.pdf"}],"country":"United States","state":"Utah","county":"Duchesne County","otherGeospatial":"Grey Mountain-Pleasant Valley Canal System, Rocky Point Canal","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-109.9746,40.8065],[-109.9747,40.8038],[-109.9725,40.6903],[-109.9742,40.6087],[-109.9741,40.547],[-109.9737,40.4757],[-109.9737,40.4109],[-109.9742,40.3964],[-109.974,40.3819],[-109.9738,40.346],[-109.9744,40.2589],[-109.9748,40.2444],[-109.9747,40.2295],[-109.9748,40.1832],[-109.9746,40.1673],[-109.9752,40.1469],[-109.9753,40.1419],[-109.9755,40.1134],[-109.9757,40.1093],[-109.9751,40.0644],[-109.9749,40.0499],[-109.9746,39.9782],[-109.9743,39.9646],[-109.974,39.8912],[-109.9739,39.8744],[-109.9729,39.8036],[-109.9867,39.8038],[-110.0249,39.8049],[-110.0435,39.8047],[-110.0627,39.805],[-110.0818,39.8053],[-110.1004,39.8052],[-110.1076,39.8053],[-110.1381,39.8053],[-110.1567,39.8055],[-110.1734,39.8053],[-110.1908,39.8056],[-110.2112,39.8054],[-110.2471,39.8055],[-110.2656,39.8057],[-110.2854,39.806],[-110.3028,39.8058],[-110.3219,39.8056],[-110.359,39.8056],[-110.3782,39.8059],[-110.404,39.8053],[-110.4219,39.8051],[-110.4411,39.8058],[-110.4603,39.8055],[-110.4698,39.8057],[-110.4974,39.8055],[-110.5165,39.8058],[-110.5164,39.8112],[-110.535,39.8119],[-110.5529,39.8121],[-110.5721,39.8119],[-110.5912,39.8125],[-110.6595,39.8137],[-110.7451,39.8137],[-110.8559,39.8157],[-110.8574,39.8719],[-110.8569,39.9009],[-110.8887,39.9017],[-110.8881,39.937],[-110.89,40.0091],[-110.8904,40.0232],[-110.8907,40.0781],[-110.8931,40.0822],[-110.8944,40.1103],[-110.8937,40.4304],[-110.9016,40.431],[-110.9011,40.4586],[-110.9009,40.4736],[-110.9013,40.489],[-110.9019,40.5634],[-110.9001,40.6786],[-110.8929,40.6799],[-110.891,40.6821],[-110.8916,40.684],[-110.8934,40.6858],[-110.8939,40.6894],[-110.8945,40.6908],[-110.8975,40.6958],[-110.8986,40.7017],[-110.8997,40.7085],[-110.8942,40.7126],[-110.8911,40.7148],[-110.8856,40.7188],[-110.8898,40.7216],[-110.8915,40.728],[-110.8842,40.7288],[-110.8794,40.7292],[-110.8769,40.7296],[-110.8655,40.7255],[-110.8618,40.7245],[-110.8546,40.7222],[-110.8479,40.7253],[-110.8425,40.723],[-110.8353,40.7188],[-110.8298,40.7161],[-110.8208,40.7105],[-110.8184,40.7119],[-110.8043,40.7204],[-110.7878,40.7297],[-110.7829,40.7319],[-110.7804,40.7333],[-110.7755,40.7355],[-110.7615,40.7413],[-110.7548,40.743],[-110.7529,40.7448],[-110.7499,40.7457],[-110.7469,40.7448],[-110.7426,40.7443],[-110.7377,40.746],[-110.7341,40.7469],[-110.7298,40.7473],[-110.7213,40.7472],[-110.7171,40.749],[-110.7128,40.7512],[-110.7085,40.7521],[-110.7025,40.7507],[-110.6989,40.7493],[-110.694,40.7478],[-110.6886,40.7442],[-110.682,40.7414],[-110.6808,40.7414],[-110.6729,40.7404],[-110.6668,40.743],[-110.6626,40.7439],[-110.6571,40.7425],[-110.6535,40.7424],[-110.6473,40.7469],[-110.638,40.7577],[-110.6275,40.7671],[-110.6245,40.7689],[-110.6226,40.7689],[-110.6184,40.7684],[-110.6112,40.7651],[-110.607,40.7628],[-110.5998,40.7591],[-110.5845,40.7617],[-110.5779,40.7611],[-110.5694,40.7601],[-110.5603,40.7587],[-110.553,40.7631],[-110.5468,40.7671],[-110.5437,40.7716],[-110.5363,40.7747],[-110.5315,40.7733],[-110.5285,40.7714],[-110.5244,40.7669],[-110.5244,40.7659],[-110.5172,40.7622],[-110.5068,40.7658],[-110.4989,40.767],[-110.4915,40.7715],[-110.4816,40.7786],[-110.478,40.7777],[-110.4738,40.7758],[-110.469,40.7744],[-110.4647,40.7743],[-110.461,40.7765],[-110.4561,40.7792],[-110.4505,40.7841],[-110.4469,40.7832],[-110.4379,40.7808],[-110.4318,40.7825],[-110.4299,40.7839],[-110.4244,40.7874],[-110.4219,40.7897],[-110.4195,40.7906],[-110.4159,40.7887],[-110.4116,40.7873],[-110.4068,40.7868],[-110.4032,40.7854],[-110.3983,40.7853],[-110.394,40.7871],[-110.3867,40.7874],[-110.3764,40.7887],[-110.3666,40.7903],[-110.3618,40.7916],[-110.3586,40.7952],[-110.3592,40.798],[-110.3543,40.8006],[-110.3517,40.806],[-110.3516,40.8115],[-110.349,40.8178],[-110.341,40.8245],[-110.3326,40.8203],[-110.3235,40.8197],[-110.3094,40.8223],[-110.2923,40.8257],[-110.277,40.8304],[-110.2697,40.8322],[-110.2593,40.8343],[-110.2551,40.8347],[-110.2502,40.8337],[-110.243,40.8313],[-110.2375,40.8308],[-110.2315,40.8285],[-110.2243,40.8274],[-110.2218,40.827],[-110.2158,40.8273],[-110.2109,40.8282],[-110.197,40.8234],[-110.1897,40.8238],[-110.1777,40.8209],[-110.1645,40.8134],[-110.1609,40.8134],[-110.1414,40.8145],[-110.128,40.8138],[-110.1232,40.8133],[-110.119,40.8128],[-110.1123,40.8122],[-110.1099,40.8117],[-110.1087,40.8117],[-110.1027,40.8085],[-110.0991,40.8066],[-110.0899,40.8096],[-110.0832,40.8118],[-110.068,40.8116],[-110.0644,40.8106],[-110.0577,40.81],[-110.054,40.8109],[-110.0473,40.8144],[-110.0417,40.8184],[-110.0398,40.8193],[-110.0338,40.8169],[-110.0169,40.8139],[-110.0018,40.8096],[-109.9904,40.8063],[-109.9789,40.8065],[-109.9746,40.8065]]]},\"properties\":{\"name\":\"Duchesne\",\"state\":\"UT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177e05e4b0893acf3fffd0","contributors":{"authors":[{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":473275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":473276,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","interactions":[{"subject":{"id":13216,"text":"ofr74214 - 1974 - Estimating mean streamflow in the Duchesne River basin, Utah","indexId":"ofr74214","publicationYear":"1974","noYear":false,"title":"Estimating mean streamflow in the Duchesne River basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","indexId":"70042823","publicationYear":"1976","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah"},"id":1},{"subject":{"id":16124,"text":"ofr75392 - 1975 - Hydrologic reconnaissance of the Pine Valley drainage basin; Millard, Beaver, and Iron counties, Utah","indexId":"ofr75392","publicationYear":"1975","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin; Millard, Beaver, and Iron counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","indexId":"70042823","publicationYear":"1976","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah"},"id":2}],"lastModifiedDate":"2016-12-12T13:38:13","indexId":"70042823","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","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":"51","title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","docAbstract":"The Pine Valley drainage basin is an area of about 730 square miles (1,890 square kilometres) in Millard, Beaver, and Iron Counties in southwestern Utah. Total annual precipitation in the basin averages about 410,000 acre-ft (acre-feet) or 506 hm<sup>3</sup> (cubic hectometres). Less than 500 acre-ft (0.6 hm<sup>3</sup>) of runoff reaches the playa on the lowest part of the valley floor. There is no surface outflow from the basin. All streams are ephemeral except in short headwater reaches of a few streams where perennial or intermittent ground-water discharge sustains flow. Surface-water development and use in the basin are insignificant.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights.","usgsCitation":"Stephens, J.C., 1976, Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah: Technical Publication 51, iv, 38 p.","productDescription":"iv, 38 p.","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":266429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267163,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009d.pdf"},{"id":331876,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-300"}],"country":"United States","state":"Utah","county":"Beaver County, Iron County, Millard County","otherGeospatial":"Pine Valley Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.0106201171875,\n              37.96801944035648\n            ],\n            [\n              -114.0106201171875,\n              38.884619201291905\n            ],\n            [\n              -113.27728271484374,\n              38.884619201291905\n            ],\n            [\n              -113.27728271484374,\n              37.96801944035648\n            ],\n            [\n              -114.0106201171875,\n              37.96801944035648\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51026618e4b0d4f5ea817c00","contributors":{"authors":[{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":472331,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043958,"text":"70043958 - 1976 - Seepage study of canals in Beaver Valley, Beaver County, Utah","interactions":[{"subject":{"id":8473,"text":"ofr76182 - 1976 - Seepage study of canals in Beaver Valley, Beaver County, Utah","indexId":"ofr76182","publicationYear":"1976","noYear":false,"title":"Seepage study of canals in Beaver Valley, Beaver County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043958,"text":"70043958 - 1976 - Seepage study of canals in Beaver Valley, Beaver County, Utah","indexId":"70043958","publicationYear":"1976","noYear":false,"title":"Seepage study of canals in Beaver Valley, Beaver County, Utah"},"id":1}],"lastModifiedDate":"2016-12-11T10:22:58","indexId":"70043958","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","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":"52","title":"Seepage study of canals in Beaver Valley, Beaver County, Utah","docAbstract":"A study of the gains or losses of nine canals near Beaver, Utah, was made to aid in the water allocation of the canal systems. The canals included in this study are Manderfield Ditch, Last Chance Canal, Christiansen Ditch, Mammoth Canal, City Ditch, Owens Ditch, South Field Ditch, Patterson Ditch and Aberdare Canal. Four sets of seepage measurements were made during 1974, but flow was observed in all nine canals only during the set of measurements made in June. Adjustments for fluctuations in flow in the canals were made from information obtained from water-stage recorders operated at selected locations along the canals during the time of each seepage run.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Cruff, R., and Mower, R.W., 1976, Seepage study of canals in Beaver Valley, Beaver County, Utah: Technical Publication 52, iv, 45 p.","productDescription":"iv, 45 p.","numberOfPages":"50","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268160,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268159,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009e.pdf"},{"id":331877,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-320"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Aberdare Canal, Christiansen Ditch, City Ditch, Last Chance Canal, Mammoth Canal, Manderfield Ditch, Owens Ditch, Patterson Ditch, South Field Ditch","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.8,\n              38.1\n            ],\n            [\n              -112.8,\n              38.5\n            ],\n            [\n              -112.4,\n              38.5\n            ],\n            [\n              -112.4,\n              38.1\n            ],\n            [\n              -112.8,\n              38.1\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512b44bae4b0523e997a81ad","contributors":{"authors":[{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":474552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474551,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042934,"text":"70042934 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","interactions":[{"subject":{"id":14188,"text":"ofr76323 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","indexId":"ofr76323","publicationYear":"1976","noYear":false,"title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70042934,"text":"70042934 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","indexId":"70042934","publicationYear":"1976","noYear":false,"title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado"},"id":1}],"lastModifiedDate":"2016-12-12T13:40:24","indexId":"70042934","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","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":"53","title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","docAbstract":"<p>This report presents a part of the results of an investigation of the hydrology of the northern Uinta Basin area by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources. The purpose of the report is to summarize the hydraulic and geohydrologic characteristics of the aquifers in the area.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights ","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights ","usgsCitation":"Hood, J.W., 1976, Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado: Technical Publication 53, vi, 71 p.","productDescription":"vi, 71 p.","numberOfPages":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":266666,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331878,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-330"},{"id":331879,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009f.pdf"}],"country":"United States","state":"Colorado, Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,37.0 ], [ -114.0,42.0 ], [ -102.0,42.0 ], [ -102.0,37.0 ], [ -114.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd7fe4b0d965cd9f2319","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":472616,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042740,"text":"70042740 - 1976 - Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf","interactions":[{"subject":{"id":15965,"text":"ofr75566 - 1975 - Textural distribution of sea-floor sediments, South Texas Outer Continental Shelf","indexId":"ofr75566","publicationYear":"1975","noYear":false,"title":"Textural distribution of sea-floor sediments, South Texas Outer Continental Shelf"},"predicate":"SUPERSEDED_BY","object":{"id":70042740,"text":"70042740 - 1976 - Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf","indexId":"70042740","publicationYear":"1976","noYear":false,"title":"Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf"},"id":1}],"lastModifiedDate":"2016-06-08T16:39:16","indexId":"70042740","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf","docAbstract":"The general texture of sea-floor sediments along the south Texas Outer Continental Shelf was evaluated in terms of gravel, sand, silt, and clay components. The gravel component is quantitatively minor and is concentrated mainly in the southern sector; it consists, for the most part, of relict biogenic detritus dominated by molluscan shells. The sand component consists of terrigenous and biogenic detritus. Modern sand is localized along the shoreface sector, whereas palimpsest and relict sands characterize the northern and southern sectors, which are the respective locations of the ancestral Brazos-Colorado 'and Rio Grande deltas. The central sector contains an extensive modern mud blanket that appears to be migrating southward over relict deposits of the ancestral Rio Grande delta. The silt fraction is the highly dominant component of the mud blanket; silt appears to be hydraulically trapped within the shelf environment and constitutes the most abundant detrital component within the Outer Continental Shelf region. The subordinate clay component of the mud blanket is concentrated toward the shelf break and may be largely escaping into deeper water environments.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Shideler, G.L., 1976, Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf: Journal of Research of the U.S. Geological Survey, v. 4, no. 6, p. 703-713.","productDescription":"11 p.","startPage":"703","endPage":"713","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":266234,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266227,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue6/report.pdf","text":"Report","size":"20.3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","otherGeospatial":"Texas Outer Continental Shelf","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.72,25.84 ], [ -97.72,30.0 ], [ -93.52,30.0 ], [ -93.52,25.84 ], [ -97.72,25.84 ] ] ] } } ] }","volume":"4","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50ffc323e4b0ca65fed0d2b1","contributors":{"authors":[{"text":"Shideler, Gerald L.","contributorId":89137,"corporation":false,"usgs":true,"family":"Shideler","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":472134,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25234,"text":"25234 - 1976 - Water Resources of the Upper New River Basin, West Virginia","interactions":[{"subject":{"id":48283,"text":"ofr7669 - 1975 - Water resources of the Upper New River basin, West Virginia","indexId":"ofr7669","publicationYear":"1975","noYear":false,"title":"Water resources of the Upper New River basin, West Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":25234,"text":"25234 - 1976 - Water Resources of the Upper New River Basin, West Virginia","indexId":"25234","publicationYear":"1976","noYear":false,"title":"Water Resources of the Upper New River Basin, West Virginia"},"id":1}],"lastModifiedDate":"2013-07-01T15:06:18","indexId":"25234","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":286,"text":"River Basin Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"4","title":"Water Resources of the Upper New River Basin, West Virginia","language":"ENGLISH","publisher":"West Virginia Geological and Economic Survey","publisherLocation":"Morgantown, WV","collaboration":"Prepared by the United States Geological Survey in cooperation with the West Virginia Geological and Economic Survey and the West Virginia Department of Natural Resources, Division of Water Resources","usgsCitation":"Clark, W.E., Chisholm, J.L., and Frye, P.M., 1976, Water Resources of the Upper New River Basin, West Virginia: River Basin Bulletin 4, vii, 87 p.; Maps: 3 Sheets.","productDescription":"vii, 87 p.; Maps: 3 Sheets","costCenters":[],"links":[{"id":274390,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":274389,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_40242.htm"}],"scale":"250000","country":"United States","state":"West Virginia","otherGeospatial":"New River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.629,37.228 ], [ -79.629,38.739 ], [ -81.399,38.739 ], [ -81.399,37.228 ], [ -79.629,37.228 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51d2a4efe4b0ca1848338aa2","contributors":{"authors":[{"text":"Clark, William E.","contributorId":105365,"corporation":false,"usgs":true,"family":"Clark","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chisholm, James L.","contributorId":77911,"corporation":false,"usgs":true,"family":"Chisholm","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":193339,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frye, Prentis M.","contributorId":98792,"corporation":false,"usgs":true,"family":"Frye","given":"Prentis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193340,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039591,"text":"70039591 - 1976 - National Cartographic Information Center Newsletter No. 4","interactions":[],"lastModifiedDate":"2012-08-14T01:01:44","indexId":"70039591","displayToPublicDate":"2012-01-01T13:05:24","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":373,"text":"Newsletter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"4","title":"National Cartographic Information Center Newsletter No. 4","docAbstract":"Last week, the editor of this publication was told to start signing the introduction. Something to do with credit given for work done. We look at it in the unfortunate light of accountability; our days under the bushel of anonymity are over. Speaking of accountability, it's about time we gave some recognition to the Newsletter's unknowing progenitor, John Wright, of the British Directorate of Overseas Surveys. Editorially and stylistically, the NCIC Newsletter owes him a large debt. Last month we received a suggestion from a reader that the Newsletter begin consistently listing prices for new products. In the publishing business, however, there is an infallible law of inflation prices increase as soon as they appear in print. We do try to quote exact prices where possible, and as our reader suggested, ballpark figures when we have to. In nearly all cases, additional information is available either by contacting the addresses listed in the article or indexed in the back or by calling NCIC's User Services Section. Numerous bits and pieces of information make up the bulk of this issue. Among them are the possibility of the Geological Survey issuing readable indexes to available topographic maps, the development of an NCIC classification system for U.S. cartographic data, and information on the publication of prototype topographic-bathymetric maps. Lastly, here is our quarterly solicitation for suggestions, comments, criticism, notes, and information for publication. Call it your bicentennial contribution to participatory democracy.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039591","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, National Cartographic Information Center Newsletter No. 4: Newsletter 4, 12 p., https://doi.org/10.3133/70039591.","productDescription":"12 p.","numberOfPages":"14","costCenters":[{"id":409,"text":"National Cartographic Information Center","active":false,"usgs":true}],"links":[{"id":261115,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039591/report.pdf"},{"id":261116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039591/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a619ce4b0c8380cd71a77","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25184,"text":"other5 - 1976 - National Cartographic Information Center Newsletter No. 5","interactions":[],"lastModifiedDate":"2012-07-27T01:01:50","indexId":"other5","displayToPublicDate":"2012-01-01T11:52:35","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":373,"text":"Newsletter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"5","title":"National Cartographic Information Center Newsletter No. 5","docAbstract":"The profile in this issue describes the Map Section of the Geological Survey Library.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/other5","issn":"0749-5781","collaboration":"National Cartographic Information Center Newsletter No. 5, Summer/Fall 1976","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, National Cartographic Information Center Newsletter No. 5: Newsletter 5, 12 p., https://doi.org/10.3133/other5.","productDescription":"12 p.","numberOfPages":"14","costCenters":[{"id":409,"text":"National Cartographic Information Center","active":false,"usgs":true}],"links":[{"id":260317,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/25184/report.pdf"},{"id":260318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/25184/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a619de4b0c8380cd71a7d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039027,"text":"70039027 - 1976 - United States Geological Survey Annual Report, Fiscal Year 1975","interactions":[],"lastModifiedDate":"2017-05-19T18:43:48","indexId":"70039027","displayToPublicDate":"2012-01-01T11:12:54","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":345,"text":"Annual Report","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Annual Report, Fiscal Year 1975","docAbstract":"The Survey resumes the practice of annually summarizing the progress it has made in identifying the Nation's land, water, energy, and mineral resources, classifying federally owned mineral lands and waterpower sites, and in supervising the exploration and development of energy and mineral resources on Federal and Indian lands. The Annual Report for 1975 consists of five parts: * The Year in Review - a review of the issues and events which affected Survey programs and highlights of program accomplishments. * Perspectives - several short papers which address major resource issues and summarize recent advances in the earth sciences. * A description of the Survey's budget, programs, and accomplishments. * A set of statistical tables and related information which documents program trends, workloads, and accomplishments. * A compendium of Survey publications and information services available to the public. One purpose of this report is to increase public awareness and understanding of the Geological Survey's programs and, more generally, of the role of earth sciences information in helping to resolve many of the natural resource conflicts that face our society now and in the years ahead. To be useful, however, information must be available and readily accessible to those responsible for natural resource policy at the time that the decisions are made. This report emphasizes the types of information products and services provided by the Survey and tells how to obtain additional information.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039027","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, United States Geological Survey Annual Report, Fiscal Year 1975: Annual Report, vi, 194 p., https://doi.org/10.3133/70039027.","productDescription":"vi, 194 p.","numberOfPages":"203","costCenters":[],"links":[{"id":261263,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039027/report.pdf"},{"id":261264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039027/report-thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173,16.916666666666668 ], [ 173,71.83333333333333 ], [ -66.95,71.83333333333333 ], [ -66.95,16.916666666666668 ], [ 173,16.916666666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc8ee4b08c986b328cdd","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039401,"text":"70039401 - 1976 - Chart of conversion factors: From English to metric system and metric to English system","interactions":[],"lastModifiedDate":"2017-05-19T18:44:10","indexId":"70039401","displayToPublicDate":"2012-01-01T11:04:52","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Chart of conversion factors: From English to metric system and metric to English system","docAbstract":"The conversion factors in the following tables are for conversion of our customary (English) units of measurement to SI*units, and for convenience, reciprocals are shown for converting SI units back to the English system. The first table contains rule-of-thumb figures, useful for \"getting the feel\" of SI units or mental estimation. The succeeding tables contain factors accurate to 3 or more significant figures. Please refer to known reference volumes for additional accuracy, as well as for factors dealing with other scientific notation involving SI units.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039401","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Chart of conversion factors: From English to metric system and metric to English system: General Information Product, 5 p., https://doi.org/10.3133/70039401.","productDescription":"5 p.","costCenters":[],"links":[{"id":261548,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039401/report.pdf"},{"id":261549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039401/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f505e4b0c8380cd4c054","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040758,"text":"70040758 - 1976 - Floods in New York, 1973 and 1974","interactions":[],"lastModifiedDate":"2017-09-13T18:22:37","indexId":"70040758","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5495,"text":"New York State Department of Environmental Conservation Report of Investigations","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"RI-15","title":"Floods in New York, 1973 and 1974","language":"English","publisher":"New York State Department of Environmental Conservation","publisherLocation":"Albany, NY","usgsCitation":"Robison, F., Embree, W., and Dunn, B., 1976, Floods in New York, 1973 and 1974: New York State Department of Environmental Conservation Report of Investigations RI-15, 81 p.","productDescription":"81 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263192,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a61d0ce4b0d446a665c9ce","contributors":{"authors":[{"text":"Robison, F.L.","contributorId":41889,"corporation":false,"usgs":true,"family":"Robison","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":468965,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Embree, W.N.","contributorId":85143,"corporation":false,"usgs":true,"family":"Embree","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":468967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunn, Bernard","contributorId":61423,"corporation":false,"usgs":true,"family":"Dunn","given":"Bernard","email":"","affiliations":[],"preferred":false,"id":468966,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70005424,"text":"70005424 - 1976 - Water-resources investigations of the U.S. Geological Survey in the major coal and oil shale areas of Wyoming, 1975-76","interactions":[],"lastModifiedDate":"2012-02-02T00:15:57","indexId":"70005424","displayToPublicDate":"2011-09-14T18:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Water-resources investigations of the U.S. Geological Survey in the major coal and oil shale areas of Wyoming, 1975-76","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Cheyenne, Wyoming","doi":"10.3133/70005424","usgsCitation":"U.S. Geological Survey, Water Resources Division, 1976, Water-resources investigations of the U.S. Geological Survey in the major coal and oil shale areas of Wyoming, 1975-76: Open-File Report, iv, 43 p. : maps ; 27 cm., https://doi.org/10.3133/70005424.","productDescription":"iv, 43 p. : maps ; 27 cm.","costCenters":[],"links":[{"id":204358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94451,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015018204738?urlappend=%3Bseq=3"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c28"}
,{"id":70001198,"text":"70001198 - 1976 - Volcanic rocks and processes of the Mid-Atlantic Ridge rift valley near 36 ° 49′ N","interactions":[],"lastModifiedDate":"2015-06-15T10:45:18","indexId":"70001198","displayToPublicDate":"2010-09-28T23:09:33","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Volcanic rocks and processes of the Mid-Atlantic Ridge rift valley near 36 ° 49′ N","docAbstract":"<p class=\"Para\">Eighty samples of submarine basaltic lava were sampled from an 8 km segment of the floor and walls of the inner rift valley of the Mid-Atlantic Ridge during the French American Mid-Ocean Undersea Study (project Famous). The samples were collected from outcrops and talus slopes by the three submersibles: Alvin, Archimede, and Cyana at water depths of about 2600 meters.</p>\n<p class=\"Para\">The early formed mineral content of the pillow lavas' glassy margins enables classification of the rocks into 5 types: (1) olivine basalt, (2) picritic basalt, (3) plagioclase-olivine-pyroxene basalt, (4) aphyric basalt, and (5) plagioclase-rich basalt. Chemical and mineralogical study indicates that at least 4 types are directly interrelated and that types (1) and (2) are higher-temperature, primitive lavas, and types (3) and (4) are lower-temperature, differentiated lavas derived from the primitive ones by crystal-liquid differentiation. The plagioclase-rich basalts also have a chemical composition of their glass comparable to that of the most differentiated basalts (types 3 and 4) but they differ in their greater amount of early formed plagioclase (12&ndash;35%).</p>\n<p class=\"Para\">In general, the mineralogical variation across the rift valley shows an assymetrical distribution of the major basalt types. Despite the mineralogical diversity of the early formed crystals, the chemistry of the basalt glasses indicates a symmetrical and a gradual compositional change across the rift valley. Based primarily on their chemistry, the rock types 1 and 2 occupy an axial zone 1.1 km wide and make up the central volcanic hills. Differentiated lavas (types 3, 4) occupy the margins and walls of the inner rift valley and also occur near the center of the rift valley between the central hills.</p>\n<p class=\"Para\">FeO/MgO ratios of olivine and coexisting melt indicate that the average temperature of eruption was 40 &deg; C higher for the primitive melts (types 1 and 2). Aside from major elements trends, the higher temperature character of the primitive basalts is shown by their common content of chrome spinel.</p>\n<p class=\"Para\">The thickness of manganese oxide and palagonite on glassy lava provide an estimate of age. In a general fashion the relative age of the various volcanic events follow the compositional zoning observed in the explored area. Most of the youngest samples are olivine basalt of the axial hills. Most older samples occur in the margins of the rift valley (West and N.E. part of explored area) but are significantly younger than the spreading age of the crust on which they are erupted. Intermediate lava types occur mainly east of the rift valley axis and in other areas where plagioclase&mdash;olivine&mdash;pyroxene basalt and aphyric basalt are present.</p>\n<p class=\"Para\">The above relations indicate that the diverse lava types were erupted from a shallow, zoned magma chamber from fissures distributed over the width of the inner rift valley and elongate parallel to it. Differentiation was accomplished by cooling and crystallization of plagioclase, olivine, and clinopyroxene toward the margins of the chamber. The centrally located hills were built by the piling up of frequent eruption of mainly primitive lavas which also are the youngest flows. In contrast smaller and less frequent eruptions of more differentiated lavas were exposed on both sides of the rift valley axis.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF00384746","issn":"00107999","usgsCitation":"Hekinian, R., Moore, J., and Bryan, W., 1976, Volcanic rocks and processes of the Mid-Atlantic Ridge rift valley near 36 ° 49′ N: Contributions to Mineralogy and Petrology, v. 58, no. 1, p. 83-110, https://doi.org/10.1007/BF00384746.","productDescription":"28 p.","startPage":"83","endPage":"110","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":203543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":19066,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00384746"}],"volume":"58","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd905","contributors":{"authors":[{"text":"Hekinian, R.","contributorId":44273,"corporation":false,"usgs":true,"family":"Hekinian","given":"R.","email":"","affiliations":[],"preferred":false,"id":346660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":346661,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bryan, W.B.","contributorId":100412,"corporation":false,"usgs":true,"family":"Bryan","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":346662,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70001164,"text":"70001164 - 1976 - Plankton secondary productivity and biomass: Their relation to lake trophic state","interactions":[],"lastModifiedDate":"2021-03-03T14:21:09.07031","indexId":"70001164","displayToPublicDate":"2010-09-28T23:09:33","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Plankton secondary productivity and biomass: Their relation to lake trophic state","docAbstract":"<p>The biomass and production of the most important zooplankton species were followed for two years in three lakes of varying trophic status in the Lake Washington watershed. Cladocerans and copepods were of equal importance in the biomass of lakes Findley and Chester Morse (both oligotrophic), whereas, copepods were the main biomass component in Lake Sammamish (mesotrophic). Cladocerans dominated production in lakes Sammamish and Chester Morse, while in Findley Lake their productive role, like that of biomass, was equal to that of the copepods. Rotifers contributed a relatively small biomass and production.</p><p>Data from this study supported Hillbricht-Ilkowska's postulate that the energy transfer efficiency between the primary and secondary trophic levels decreases with increasing trophic state. Energy transfer efficiencies for the lakes of this study expressed as a two year mean of the ratio-secondary: primary production, were as follows: Findley Lake-0.13; Chester Morse Lake-0.08; and Lake Sammanish-0.04.</p><p>On the other hand, the hypothesis of Patalas that the secondary productivity: biomass ratio (P/B) tended to increase in proportion to the productivity of a lake, could not be supported. Lake Sammamish, the most productive of the lakes studied, had a P/B ratio of 0.03 while lakes Findley and Chester Morse had P/B ratios of 0.04.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF00019816","issn":"00188158","usgsCitation":"Pederson, G., Welch, E., and Litt, A., 1976, Plankton secondary productivity and biomass: Their relation to lake trophic state: Hydrobiologia, v. 50, no. 2, p. 129-144, https://doi.org/10.1007/BF00019816.","productDescription":"16 p.","startPage":"129","endPage":"144","costCenters":[],"links":[{"id":203615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659740","contributors":{"authors":[{"text":"Pederson, G.L.","contributorId":90781,"corporation":false,"usgs":true,"family":"Pederson","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":346649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welch, E.B.","contributorId":77279,"corporation":false,"usgs":true,"family":"Welch","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":346648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Litt, A.H.","contributorId":45437,"corporation":false,"usgs":true,"family":"Litt","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":346647,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70000759,"text":"70000759 - 1976 - Problems in shallow land disposal of solid low-level radioactive waste in the united states","interactions":[],"lastModifiedDate":"2021-04-26T13:13:12.098629","indexId":"70000759","displayToPublicDate":"2010-09-28T23:09:28","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1128,"text":"Bulletin of the International Association of Engineering Geology","active":true,"publicationSubtype":{"id":10}},"title":"Problems in shallow land disposal of solid low-level radioactive waste in the united states","docAbstract":"<p>Disposal of solid low-level wastes containing radionuclides by burial in shallow trenches was initiated during World War II at several sites as a method of protecting personnel from radiation and isolating the radionuclides from the hydrosphere and biosphere. Today, there are 11 principal shallow-land burial sites in the United States that contain a total of more than 1.4 million cubic meters of solid wastes contaminated with a wide variety of radionuclides. Criteria for burial sites have been few and generalized and have contained only minimal hydrogeologic considerations. Waste-management practices have included the burial of small quantities of long-lived radionuclides with large volumes of wastes contaminated with shorter-lived nuclides at the same site, thereby requiring an assurance of extremely long-time containment for the entire disposal site.</p><p>Studies at 4 of the 11 sites have documented the migration of radionuclides. Other sites are being studied for evidence of containment failure. Conditions at the 4 sites are summarized. In each documented instance of containment failure, ground water has probably been the medium of transport. Migrating radionuclides that have been identified include<sup>90</sup>Sr,<sup>137</sup>Cs,<sup>106</sup>Ru,<sup>239</sup>Pu,<sup>125</sup>Sb,<sup>60</sup>Co, and<sup>3</sup>H.</p><p>Shallow land burial of solid wastes containing radionuclides can be a viable practice only if a specific site satisfies adequate hydrogeologic criteria. Suggested hydrogeologic criteria and the types of hydrogeologic data necessary for an adequate evaluation of proposed burial sites are given. It is mandatory that a concomitant inventory and classification be made of the longevity, and the physical and chemical form of the waste nuclides to be buried, in order that the anticipated waste types can be matched to the containment capability of the proposed sites.</p><p>Ongoing field investigations at existing sites will provide data needed to improve containment at these sites and help develop hydrogeologic criteria for new sites. These studies have necessitated the development of special drilling, sampling, well construction, and testing techniques. A recent development in borehole geophysical techniques is downhole spectral gammaray analysis which not only locates but identifies specific radionuclides in the subsurface.</p><p>Field investigations are being supplemented by laboratory studies of the hydrochemistry of the transuranic elements, the kinetics of solid-liquid phase interactions, and the potential complexing of radionuclides with organic compounds and solvents which mobilize normally highly sorbable nuclides. Theoretical studies of digital predictive solute transport models are being implemented to assure their availability for application to problems and processes identified in the field and laboratory.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF02634782","issn":"14359529","usgsCitation":"Stevens, P.R., and DeBuchananne, G., 1976, Problems in shallow land disposal of solid low-level radioactive waste in the united states: Bulletin of the International Association of Engineering Geology, v. 13, no. 1, p. 161-171, https://doi.org/10.1007/BF02634782.","productDescription":"11 p.","startPage":"161","endPage":"171","costCenters":[],"links":[{"id":203472,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a0ca","contributors":{"authors":[{"text":"Stevens, P. R.","contributorId":90289,"corporation":false,"usgs":true,"family":"Stevens","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346519,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeBuchananne, G.D.","contributorId":91166,"corporation":false,"usgs":true,"family":"DeBuchananne","given":"G.D.","affiliations":[],"preferred":false,"id":346520,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5220853,"text":"5220853 - 1976 - The waterfowl hunter's perceptions of the waterfowl resource","interactions":[],"lastModifiedDate":"2012-02-02T00:14:47","indexId":"5220853","displayToPublicDate":"2010-06-16T12:19:17","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3638,"text":"Transactions of the North American Wildlife and Natural Resources Conference","active":true,"publicationSubtype":{"id":10}},"title":"The waterfowl hunter's perceptions of the waterfowl resource","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the North American Wildlife and Natural Resources Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Smith, R., and Roberts, R.J., 1976, The waterfowl hunter's perceptions of the waterfowl resource: Transactions of the North American Wildlife and Natural Resources Conference, v. 41, p. 183-193.","productDescription":"183-193","startPage":"183","endPage":"193","numberOfPages":"11","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62ed29","contributors":{"authors":[{"text":"Smith, R.I.","contributorId":63116,"corporation":false,"usgs":true,"family":"Smith","given":"R.I.","email":"","affiliations":[],"preferred":false,"id":332601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, R. J.","contributorId":58250,"corporation":false,"usgs":true,"family":"Roberts","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":332600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}