{"pageNumber":"348","pageRowStart":"8675","pageSize":"25","recordCount":10961,"records":[{"id":59341,"text":"mf1568B - 1984 - Aeromagnetic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino counties, Arizona","interactions":[],"lastModifiedDate":"2016-08-22T10:25:00","indexId":"mf1568B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1568","chapter":"B","title":"Aeromagnetic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino counties, Arizona","docAbstract":"<p>The aeromagnetic map of the Fossil Springs Roadless Area was compiled from data collected in 1980 by Airmag Surveys, Inc., for the U.S. Geological Survey. Total magnetic intensity measurements were made along east-west flight lines about 0.5 mi apart and flown at an average altitude of 1,000 ft above the ground surface. A regional magnetic field (the International Geomagnetic Reference Field, 1975, updated to months flown) was removed from the data and a constant of 50,800 gammas was added to the adjusted total field intensity values.</p>\n<p>The roadless area includes the upper part of Fossil Creek and its northeastern tributaries in Sandrock Canyon and Calf Pen Canyon. The extremely rugged canyon of Fossil Creek is in several places more than 1,500 ft deep. Elevation of the canyon floor ranges from 4,600 ft near the mouth of Calf Pen Canyon to 3,500 ft at the southwest end of the area. Peaks and ridges on the uplands bordering the canyons range in elevation from 5,300 ft west of Fossil Springs to 6,900 ft in the northeastern part of the area. Maximum topographic relief along these uplands is less than 200 ft.</p>\n<p>The Fossil Springs Roadless Area is underlain by more than 3,000 ft of Paleozoic rocks consisting mostly of sandstone, shale, dolomite, and limestone. West of Fossil Springs and along most of the border of the area, these rocks are generally overlain by late Tertiary volcanic rocks, mainly basaltic lavas and pyroclastic deposits. Quaternary alluvial, colluvial, landslide, and travertine deposits overlie large parts of the country rock in the canyons. In the southwestern part of the area, the volcanic rocks are more than 2,000 ft thick. Along the northwest and northeast margins, these rocks are 300-400 ft thick.</p>\n<p>The prevailing dip of the Paleozoic strata is low to the north or northeast. The dominant homoclinal structure is interrupted by several fault blocks, in which the strata dip westward or southward. All the faults are high-angle normal faults and have displacements commonly ranging from about 50 to 400 ft. Although fault relations are obscure within the volcanic sequence, many faults seem to displace the volcanic rocks less than the underlying Paleozoic rocks. The volcanic rocks, which rest unconformably on the Paleozoic strata, are flat lying in the northern part of the map area, but west of Fossil Springs they dip gently southwestward. The ancestral Mogollon Rim, a north-northwest-trending escarpment of Paleozoic rocks now concealed by Tertiary volcanic rocks lies near Fossil Springs (Twenter, 1962).</p>\n<p>The magnetic anomalies and patterns on the aeromagnetic map reflect variations of magnetization in the underlying rocks. Basaltic rocks contain moderate amounts of magnetic minerals, mainly magnetite, and possess strong intensities of magnetization. The more silicic volcanic rocks have much lower magnetization intensities. Sedimentary rocks contain little or no magnetite and are virtually nonmagnetic.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1568B","usgsCitation":"Davis, W.E., and Weir, G.W., 1984, Aeromagnetic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino counties, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1568, Plate: 43.52 x 29.85 inches, https://doi.org/10.3133/mf1568B.","productDescription":"Plate: 43.52 x 29.85 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1568B.JPG"},{"id":327211,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1568-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Arizona","county":"Coconino County, Gila County, Yavapai County","otherGeospatial":"Fossil Springs Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.66666666666667,34.3675 ], [ -111.66666666666667,34.5 ], [ -111.45083333333334,34.5 ], [ -111.45083333333334,34.3675 ], [ -111.66666666666667,34.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6966c3","contributors":{"authors":[{"text":"Davis, W. E.","contributorId":100844,"corporation":false,"usgs":true,"family":"Davis","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":261819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weir, G. W.","contributorId":107290,"corporation":false,"usgs":true,"family":"Weir","given":"G.","middleInitial":"W.","affiliations":[],"preferred":false,"id":261820,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29589,"text":"wri834237 - 1984 - Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80","interactions":[],"lastModifiedDate":"2018-04-02T10:23:19","indexId":"wri834237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4237","title":"Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80","docAbstract":"<p>The ground-water system in the Twin Cities Metropolitan Area includes five aquifers; two of these aquifers the Prairie du Chien-Jordan and the Mount Simon-Hinckley supply about 80 percent and 10 percent, respectively, of the ground water pumped for public supply. Water levels and changes in water levels in these two aquifers differ greatly in the Twin Cities Metropolitan Area. The Mississippi, Minnesota, and St. Croix Rivers are in hydraulic connection with and influence the pattern of flow in the upper aquifer, the Prairie du Chien-Jordan. Water generally flows toward these streams from water-level highs northeast, northwest, and south of Minneapolis and St. Paul. Consequently, heavy pumping has caused only localized cones of depression in the potentiometric surface of this aquifer. In contrast, the Mount Simon-Hinckley, which has only a slight hydraulic connection to the streams, is greatly influenced by pumping. Pumping in the urban centers of Minneapolis and St. Paul has caused a large cone of depression in the Mount Simon-Hinckley potentiometric surface. During 1971, the measurable cone was centered in eastcentral Hennepin County, was about 25 miles in diameter, and was as much as 150 feet deep at its center.</p>\n<p>Between 1971 and 1980, average water levels in the Prairie du Chien-Jordan aquifer changed less than 5 feet in most of the study area, but rose or declined as much as 25 feet locally in response to pumpage and recharge. During this period, seasonal declines of water levels from winter to summer lessened, and the area where these declines exceeded 10 feet decreased.</p>\n<p>In contrast, between 1971 and 1980, average water levels in the Mount Simon-Hinckley aquifer rose as much as 60 feet in the center of the cone of depression in response to decreased pumping. Also, the measurable cone of depression contracted from about 25 miles to about 15 miles in diameter. However, because of increased summer pumping due to below-average precipitation during 1980, seasonal water levels declined much more and over a wider area during 1980 than in 1971.</p>\n<p>Water-level data suggest that (1) little variation in annual pumpage between 1971 and 1980 from the Prairie du Chien-Jordan aquifer produced generally stable water levels in that aquifer, (2) decreased annual pumpage from the Mount Simon-Hinckley aquifer from 1971 to 1980 caused water levels in that aquifer to rise, and (3) a greater seasonal component of pumpage from the Mount Simon-Hinckley aquifer than from the Prairie du Chien-Jordan produced larger and more widespread seasonal water-level declines in the Mount Simon-Hinckley than in the Prairie du Chien-Jordan, particularly during dry years.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri834237","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities and Minnesota Department of Natural Resources","usgsCitation":"Schoenberg, M., 1984, Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80: U.S. Geological Survey Water-Resources Investigations Report 83-4237, Document: iv, 23 p.; 2 Plates: 34.56 x 30.51 inches and 34.60 x 30.78 inches, https://doi.org/10.3133/wri834237.","productDescription":"Document: iv, 23 p.; 2 Plates: 34.56 x 30.51 inches and 34.60 x 30.78 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":159735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4237/report-thumb.jpg"},{"id":58417,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4237/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58418,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4237/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58419,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4237/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cities Metropolitan Area","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.5093,45.4163],[-93.1289,45.4153],[-93.0186,45.4131],[-93.0188,45.2984],[-92.7894,45.297],[-92.7439,45.2963],[-92.7516,45.2935],[-92.7551,45.2927],[-92.7583,45.2904],[-92.7597,45.2872],[-92.7604,45.2845],[-92.7591,45.2794],[-92.7559,45.2739],[-92.7527,45.2694],[-92.7515,45.2657],[-92.7526,45.2626],[-92.7535,45.2584],[-92.7561,45.2541],[-92.7575,45.2502],[-92.7569,45.2443],[-92.7557,45.2397],[-92.7553,45.2356],[-92.7538,45.2305],[-92.7536,45.2276],[-92.7521,45.2236],[-92.752,45.2196],[-92.7527,45.2168],[-92.7546,45.2136],[-92.7573,45.2107],[-92.7603,45.2065],[-92.7619,45.2041],[-92.7632,45.2009],[-92.7637,45.1972],[-92.764,45.1895],[-92.7629,45.1853],[-92.7557,45.178],[-92.7522,45.1759],[-92.7493,45.173],[-92.748,45.1698],[-92.7472,45.1634],[-92.7483,45.1597],[-92.7475,45.1551],[-92.7473,45.1515],[-92.7484,45.1483],[-92.749,45.1419],[-92.7484,45.1373],[-92.7441,45.1264],[-92.7415,45.1172],[-92.7422,45.1135],[-92.7446,45.11],[-92.7467,45.1076],[-92.7513,45.1045],[-92.7591,45.0999],[-92.7624,45.0972],[-92.7803,45.0849],[-92.7847,45.083],[-92.7885,45.0806],[-92.7917,45.0791],[-92.795,45.0772],[-92.7982,45.0746],[-92.8001,45.0723],[-92.8019,45.0647],[-92.8016,45.0597],[-92.8005,45.0567],[-92.7984,45.0531],[-92.7952,45.0499],[-92.7926,45.0481],[-92.7881,45.0453],[-92.7837,45.0421],[-92.7745,45.0373],[-92.7707,45.0344],[-92.7683,45.0325],[-92.7645,45.0265],[-92.7639,45.0237],[-92.7639,45.0196],[-92.7682,45.0005],[-92.7694,44.9909],[-92.7686,44.9796],[-92.7646,44.9711],[-92.7547,44.9571],[-92.7527,44.9527],[-92.7523,44.9481],[-92.753,44.9369],[-92.7534,44.9237],[-92.7547,44.9159],[-92.7569,44.9105],[-92.7606,44.9068],[-92.7645,44.9046],[-92.767,44.9039],[-92.7707,44.9023],[-92.7729,44.901],[-92.775,44.8982],[-92.7738,44.8933],[-92.7689,44.8848],[-92.7632,44.8759],[-92.7628,44.8716],[-92.763,44.8671],[-92.7644,44.8622],[-92.7682,44.8554],[-92.7683,44.853],[-92.7671,44.8494],[-92.7652,44.8462],[-92.7646,44.8423],[-92.7644,44.8382],[-92.766,44.8308],[-92.7679,44.8265],[-92.7719,44.8211],[-92.7751,44.8161],[-92.7784,44.8125],[-92.7801,44.8095],[-92.781,44.8056],[-92.7823,44.8029],[-92.783,44.7966],[-92.7858,44.7893],[-92.7909,44.7842],[-92.7993,44.7765],[-92.802,44.7729],[-92.8046,44.7683],[-92.8059,44.7624],[-92.8073,44.7524],[-92.8061,44.7483],[-92.8054,44.7473],[-92.8022,44.7446],[-92.7901,44.7381],[-92.7805,44.7344],[-92.7722,44.7317],[-92.7658,44.7289],[-92.7569,44.7234],[-92.7536,44.7226],[-92.7471,44.7204],[-92.7415,44.7192],[-92.7339,44.7157],[-92.737,44.658],[-92.7386,44.6329],[-92.7957,44.6305],[-92.7915,44.5452],[-92.9165,44.5449],[-92.9179,44.5221],[-92.9218,44.518],[-92.9282,44.5158],[-92.9321,44.513],[-92.941,44.5149],[-92.9449,44.5131],[-92.9494,44.5104],[-92.9584,44.514],[-92.9634,44.5177],[-92.975,44.5159],[-92.9827,44.5173],[-92.991,44.5215],[-93.0057,44.5197],[-93.0121,44.5175],[-93.0166,44.5166],[-93.0275,44.5198],[-93.0301,44.5148],[-93.0346,44.5148],[-93.039,44.5171],[-93.0406,44.4729],[-93.2826,44.473],[-93.2798,44.546],[-93.5259,44.5466],[-93.9091,44.5446],[-93.9117,44.5492],[-93.9078,44.5528],[-93.9027,44.5524],[-93.9008,44.5492],[-93.8956,44.5483],[-93.8937,44.5515],[-93.8963,44.5561],[-93.9008,44.5606],[-93.8996,44.5647],[-93.8957,44.5675],[-93.8958,44.5711],[-93.8996,44.5743],[-93.8958,44.5775],[-93.8939,44.5807],[-93.8959,44.5871],[-93.8991,44.5903],[-93.8908,44.5962],[-93.8857,44.5967],[-93.8838,44.6012],[-93.878,44.6013],[-93.878,44.6077],[-93.8716,44.6063],[-93.8658,44.6063],[-93.8569,44.6168],[-93.8563,44.6218],[-93.8505,44.6219],[-93.8447,44.6201],[-93.8422,44.6233],[-93.8358,44.6242],[-93.8319,44.6251],[-93.8217,44.6297],[-93.8031,44.6366],[-93.7999,44.6361],[-93.7967,44.6343],[-93.7935,44.6311],[-93.7883,44.632],[-93.78,44.6362],[-93.7768,44.6385],[-93.7729,44.6366],[-93.7723,44.6325],[-93.7691,44.6312],[-93.7665,44.6362],[-93.7685,44.6417],[-93.7686,44.675],[-93.8887,44.6756],[-93.8902,44.7185],[-94.0104,44.719],[-94.0085,44.8947],[-94.0136,44.8951],[-94.0117,44.9796],[-93.7692,44.9789],[-93.7702,45.0734],[-93.7663,45.077],[-93.7631,45.0839],[-93.7534,45.0853],[-93.7399,45.0894],[-93.7341,45.0922],[-93.7322,45.0963],[-93.7257,45.1022],[-93.7225,45.11],[-93.72,45.1205],[-93.7155,45.1269],[-93.7019,45.1374],[-93.6852,45.1489],[-93.6793,45.1525],[-93.6716,45.1562],[-93.6574,45.1585],[-93.6554,45.1599],[-93.6529,45.1631],[-93.6503,45.169],[-93.6516,45.1841],[-93.6549,45.1905],[-93.6555,45.1969],[-93.6562,45.201],[-93.6471,45.2079],[-93.6387,45.2074],[-93.6361,45.206],[-93.6329,45.2056],[-93.6258,45.2092],[-93.6167,45.2115],[-93.6096,45.2111],[-93.6031,45.2111],[-93.5967,45.2134],[-93.5857,45.2189],[-93.5792,45.2189],[-93.5734,45.2202],[-93.5676,45.2225],[-93.5617,45.2289],[-93.554,45.2298],[-93.5462,45.2289],[-93.5371,45.2294],[-93.5332,45.2317],[-93.5197,45.2417],[-93.5158,45.2458],[-93.5138,45.2454],[-93.5093,45.4163]]]},\"properties\":{\"name\":\"Anoka\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9e31","contributors":{"authors":[{"text":"Schoenberg, Michael","contributorId":22802,"corporation":false,"usgs":true,"family":"Schoenberg","given":"Michael","affiliations":[],"preferred":false,"id":201771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27544,"text":"wri834208 - 1984 - Chemical and biological quality of streams at the Indiana Dunes National Lakeshore, Indiana, 1978-80","interactions":[],"lastModifiedDate":"2016-05-25T11:32:26","indexId":"wri834208","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4208","title":"Chemical and biological quality of streams at the Indiana Dunes National Lakeshore, Indiana, 1978-80","docAbstract":"<p>A variety of land uses affects water quality of streams at the Indiana Dunes National Lakeshore. Discharge from storm sewers and runoff from roads contributed lead, zinc, and chlorinated hydrocarbons (chlordane, DOT, ODD, DDE, and PCB's) to all streams except Derby ditch. In addition, the Little Calumet River received ammonia from industrial discharges, and organic materials, nitrogen, phosphorus, and fecal coliform from wastewater-treatment-plant and combinedsanitary- and storm-sewer discharges. As a result, water at some sites in the lower reaches of the Little Calumet River contained dissolved-ammonium-nitrogen concentrations exceeding 0.10 milligram per liter, dissolved-oxygen concentrations less than 3.0 milligrams per liter, and fecal coliform populations exceeding 2,000 colonies per 100 milliliters.</p>\n<p>Seepage from two landfills may have caused the concentration of dissolved solids in the west Grand Calumet River lagoon to exceed that in the east lagoon. Ammonium concentrations in the west lagoon ranged from 13 to 16 milligrams per liter as nitrogen.</p>\n<p>Pesticides used in agricultural areas were the major source of DOT, ODD, DDE, and dieldrin on streambed materials. Runoff from residential areas was a major source of nitrate, organic materials, and chlordane in Derby ditch and Dunes Creek.</p>\n<p>Wetland drainage contributed significant amounts of organic materials to streams and at times increased concentrations of dissolved sulfate and iron. Dissolved-iron concentrations correlated with dissolved-organic-carbon concentrations in yellow-brown water of Kintzele and Derby ditches.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri834208","collaboration":"National Park Service","usgsCitation":"Hardy, M.A., 1984, Chemical and biological quality of streams at the Indiana Dunes National Lakeshore, Indiana, 1978-80: U.S. Geological Survey Water-Resources Investigations Report 83-4208, viii, 95 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834208.","productDescription":"viii, 95 p. :ill., maps ;28 cm.","startPage":"1","endPage":"95","numberOfPages":"105","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":123388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4208/report-thumb.jpg"},{"id":56400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4208/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","otherGeospatial":"Indiana Dunes National Lakeshore","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.28869438171387,\n              41.621923034123846\n            ],\n            [\n              -87.26963996887207,\n              41.621730547188456\n            ],\n            [\n              -87.26912498474121,\n              41.60806250618307\n            ],\n            [\n              -87.24603652954102,\n              41.608511736657555\n            ],\n            [\n              -87.24303245544434,\n              41.609859409312534\n            ],\n            [\n              -87.24311828613281,\n              41.61306804041503\n            ],\n            [\n              -87.23959922790527,\n              41.61313221140915\n            ],\n            [\n              -87.23779678344727,\n              41.61396642852365\n            ],\n            [\n              -87.23367691040039,\n              41.61441561788573\n            ],\n            [\n              -87.23221778869629,\n              41.61249049859493\n            ],\n            [\n              -87.2306728363037,\n              41.61531398722544\n            ],\n            [\n              -87.2303295135498,\n              41.61614817612265\n            ],\n            [\n              -87.22672462463377,\n              41.61499314246908\n            ],\n            [\n              -87.22346305847167,\n              41.618329849922084\n            ],\n            [\n              -87.22466468811035,\n              41.62558017672615\n            ],\n            [\n              -87.17668533325195,\n              41.63578058345409\n            ],\n            [\n              -87.17471122741699,\n              41.62301378257129\n            ],\n            [\n              -87.17968940734863,\n              41.62275713753768\n            ],\n            [\n              -87.18063354492188,\n              41.621923034123846\n            ],\n            [\n              -87.1805477142334,\n              41.61807318624671\n            ],\n            [\n              -87.18818664550781,\n              41.616725685192804\n            ],\n            [\n              -87.1889591217041,\n              41.61634067972058\n            ],\n            [\n              -87.18844413757324,\n              41.61364557706411\n            ],\n            [\n              -87.18973159790039,\n              41.61358140658068\n            ],\n            [\n              -87.19127655029297,\n              41.60799833014563\n            ],\n            [\n              -87.19874382019043,\n              41.605174521299304\n            ],\n            [\n              -87.19951629638672,\n              41.60645808609603\n            ],\n            [\n              -87.20681190490723,\n              41.607677449000946\n            ],\n            [\n              -87.2068977355957,\n              41.60273567783677\n            ],\n            [\n              -87.21256256103516,\n              41.59978327031246\n            ],\n            [\n              -87.21359252929686,\n              41.603698390215456\n            ],\n            [\n              -87.22123146057129,\n              41.60286404031713\n            ],\n            [\n              -87.22294807434082,\n              41.600040006763784\n            ],\n            [\n              -87.23161697387695,\n              41.600681843423565\n            ],\n            [\n              -87.23153114318848,\n              41.59644560350027\n            ],\n            [\n              -87.25247383117676,\n              41.59792190049485\n            ],\n            [\n              -87.25273132324217,\n              41.60061766004485\n            ],\n            [\n              -87.25496292114258,\n              41.60074602673845\n            ],\n            [\n              -87.2548770904541,\n              41.60382675078074\n            ],\n            [\n              -87.27805137634276,\n              41.60389093096761\n            ],\n            [\n              -87.27865219116211,\n              41.59914142471562\n            ],\n            [\n              -87.34139442443848,\n              41.605880485097465\n            ],\n            [\n              -87.32903480529784,\n              41.60645808609603\n            ],\n            [\n              -87.31126785278319,\n              41.60594466324155\n            ],\n            [\n              -87.30174064636229,\n              41.609153489052005\n            ],\n            [\n              -87.28517532348633,\n              41.609602711929725\n            ],\n            [\n              -87.28526115417479,\n              41.61640484745891\n            ],\n            [\n              -87.28963851928711,\n              41.616854019839494\n            ],\n            [\n              -87.29006767272949,\n              41.62205135842823\n            ],\n            [\n              -87.28869438171387,\n              41.621923034123846\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcbb8","contributors":{"authors":[{"text":"Hardy, M. A.","contributorId":54223,"corporation":false,"usgs":true,"family":"Hardy","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1089,"text":"wsp2215 - 1984 - Availability and quality of water from the Dakota aquifer, northwest Iowa","interactions":[{"subject":{"id":8110,"text":"ofr82264 - 1982 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"ofr82264","publicationYear":"1982","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"predicate":"SUPERSEDED_BY","object":{"id":1089,"text":"wsp2215 - 1984 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"wsp2215","publicationYear":"1984","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"id":1}],"lastModifiedDate":"2016-03-02T15:59:06","indexId":"wsp2215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2215","title":"Availability and quality of water from the Dakota aquifer, northwest Iowa","docAbstract":"<p>The Dakota aquifer in northwest Iowa consists of sandstones in the Dakota Formation. It underlies most of the study area and is the most extensive source of ground water in the area. Individual sandstone beds are from less than 10 to more than 150 feet thick. The cumulative thickness of sandstone is more than 200 feet throughout much of the area. The aquifer is confined by overlying Cretaceous limestone and shale, Quaternary glacial deposits and loess. The underlying confining material is shale of the Dakota Formation, undifferentiated Paleozoic age rocks, or Precambrian crystalline rock.</p>\n<p>Water flows through the aquifer from the northcentral part of the study area to the east, south and southwest. Recharge is dominantly by infiltration from the land surface through the confining materials. Discharge is to underlying Paleozoic aquifers and to the alluvium and glacial outwash deposits along the Missouri and Big Sioux Rivers in the southwest part of the area. Flow components toward bedrock valleys may reflect discharge to Quaternary sand and gravel deposits in these valleys.</p>\n<p>Pumping tests conducted in the study area indicate a narrow\" range of hydraulic conductivities of the Dakota aquifer, from 37 to 50 feet per day. Consequently, an average hydraulic conductivity of 40 feet per day was used to estimate the potential yield to wells completed in the aquifer. Yields of more than 250 gallons per minute can be expected throughout much of the study area and more than 1,000 gallons per minute could be produced in some areas.</p>\n<p>The quality of water from the Dakota is a calcium, magnesium, sulfate type. It is generally suitable for irrigation purposes, based on comparisons of sodium adsorption ratios and electrical conductivities. In some areas the aquifer has water with high salinity hazard that may restrict its use to irrigation of only well-drained types of soil. The concentration of radium-226 and other radionuclides exceeds recommended limits at several sites.</p>\n<p>The quality of water pumped from the aquifer may be altered by induced leakage from the underlying aquifers in Paleozoic age rocks if withdrawals reverse the pattern of natural flow from the Dakota into the Paleozoic aquifers. Evidence for such a reversal exists in the area around the city of LeMars.</p>","language":"English","publisher":"U. S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wsp2215","collaboration":"Prepared in cooperation with the Iowa Geological Survey","usgsCitation":"Burkart, M.R., 1984, Availability and quality of water from the Dakota aquifer, northwest Iowa: U.S. Geological Survey Water Supply Paper 2215, iv, 65 p.: ill., maps; 28 cm.; 8 plates in pocket, https://doi.org/10.3133/wsp2215.","productDescription":"iv, 65 p.: ill., maps; 28 cm.; 8 plates in pocket","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":25816,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2215/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25817,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2215/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25809,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2215/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25810,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2215/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25811,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2215/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25812,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2215/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25813,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2215/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25814,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2215/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25815,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2215/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2215/report-thumb.jpg"}],"country":"United States","state":"Iowa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.50439453125,\n              42.27730877423709\n            ],\n            [\n              -94.52636718749999,\n              43.50075243569041\n            ],\n            [\n              -96.591796875,\n              43.50872101129684\n            ],\n            [\n              -96.558837890625,\n              43.37311218382002\n            ],\n            [\n              -96.558837890625,\n              43.31718491566708\n            ],\n            [\n              -96.61376953125,\n              43.31718491566708\n            ],\n            [\n              -96.61376953125,\n              43.22118973298753\n            ],\n            [\n              -96.536865234375,\n              43.22118973298753\n            ],\n            [\n              -96.51489257812499,\n              43.14909399920127\n            ],\n            [\n              -96.50390625,\n              43.06086137134326\n            ],\n            [\n              -96.558837890625,\n              43.04480541304369\n            ],\n            [\n              -96.558837890625,\n              42.98857645832184\n            ],\n            [\n              -96.558837890625,\n              42.908160071960566\n            ],\n            [\n              -96.624755859375,\n              42.81152174509788\n            ],\n            [\n              -96.6357421875,\n              42.71473218539458\n            ],\n            [\n              -96.50390625,\n              42.60970621339408\n            ],\n            [\n              -96.43798828125,\n              42.48830197960227\n            ],\n            [\n              -96.40502929687499,\n              42.35854391749705\n            ],\n            [\n              -96.317138671875,\n              42.30169032824452\n            ],\n            [\n              -96.3720703125,\n              42.19596877629178\n            ],\n            [\n              -94.50439453125,\n              42.27730877423709\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db62681a","contributors":{"authors":[{"text":"Burkart, M. R.","contributorId":42190,"corporation":false,"usgs":true,"family":"Burkart","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38561,"text":"pp1295 - 1984 - Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age","interactions":[{"subject":{"id":49319,"text":"ofr77544 - 1977 - Seismic refraction time-distance curves, Carolina, Hope Valley, and Kingston quadrangles, Rhode Island","indexId":"ofr77544","publicationYear":"1977","noYear":false,"title":"Seismic refraction time-distance curves, Carolina, Hope Valley, and Kingston quadrangles, Rhode Island"},"predicate":"SUPERSEDED_BY","object":{"id":38561,"text":"pp1295 - 1984 - Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age","indexId":"pp1295","publicationYear":"1984","noYear":false,"title":"Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age"},"id":1}],"lastModifiedDate":"2022-12-21T20:09:55.708609","indexId":"pp1295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1295","title":"Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age","docAbstract":"The Glastonbury dome is a long, narrow structure trending approximately 70 km north-northeast through Connecticut and Massachusetts along the west side of the Bronson Hill anticlinorium. Structurally and stratigraphically the dome is analogous to the Oliverian domes of New Hampshire. It is cored by Glastonbury Gneiss and is mantled by Ammonoosuc Volcanics and Partridge Formation (or their equivalents) of Ordovician age. The Glastonbury Gneiss intrudes the Ammonoosuc and, thereby, establishes the relative age of the two units. Monson Gneiss, which unconformably underlies the Ammonoosuc Volcanics in the Monson anticline to the east, is not in contact with Glastonbury Gneiss except near Stafford Springs, Conn., where the contact may be gradational. In some places, Monson Gneiss shows evidence of plastic flow and potential anatexis. The northern part of the Glastonbury Gneiss typically is leucocratic, granoblastic, relatively potassium-poor gneiss that appears homogeneous in outcrop, but proves to be chemically and modally inhomogeneous over short distances, as shown by variation diagrams and REE plots. The gneiss straddles the compositional fields of trondhjemite, tonalite, and granodiorite, and partly overlaps that of Monson Gneiss. The southern part of the Glastonbury Gneiss is consistently more potassic than the northern, having compositions ranging from granite to granodiorite. All of the Glastonbury Gneiss show pervasive, strong foliation, deformation, and local shearing related to the Acadian orogeny. \r\n\r\nField relations, textures, and chemistry of the northern part of the Glastonbury suggest an origin by anatexis of the premetamorphic Monson sequence at temperatures of about 690 DC to 750 DC and pressures of <3kbars. The southern part of the Glastonbury appears to have been generated contemporaneously but not comagmatically from calcalkaline crust. U-Pb zircon ages for both the northern and southern bodies are slightly discordant with 207PbfosPb ages of 445 to 467 m.y. At first these results seem to contradict the known stratigraphic position of the Glastonbury relative to the Monson, which yields distinctly younger zircon 207PbfosPb ages of 428 to 440 m.y. However, this apparent discrepancy in the radiometric ages-younger Monson, older Glastonbury-could be resolved by postulating either (1) a small component of old inherited zircon in the Glastonbury or (2) preferential metamorphic overprinting of the zircon in the Monson. In any case, the isotopic age discrepancy is not so large as to render the proposed Monson anatectic model implausible. Rb-Sr whole-rock data show a large amount of scatter on an isochron diagram and hence do not permit a reliable estimate of age. This condition may reflect inhomogeneities in the initial 87S r /8SS r ratio or may have been also induced by later Acadian or Alleghanian metamorphism. \r\n\r\nAn early Silurian to Middle Ordovician age of the Glastonbury Gneiss gives evidence of higher heat flow and more extensive plutonism in the Taconic than has generally been recognized. With certain qualifications, the Glastonbury and associated volcanic rocks are compatible with recent plate-tectonic models involving the Bronson Hill anticlinorium.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1295","usgsCitation":"Leo, G.W., Zartman, R., and Brookins, D.G., 1984, Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age (Supercedes OFR 77-544): U.S. Geological Survey Professional Paper 1295, iv, 45 p., https://doi.org/10.3133/pp1295.","productDescription":"iv, 45 p.","costCenters":[],"links":[{"id":410878,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74531.htm","linkFileType":{"id":5,"text":"html"}},{"id":65330,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1295/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1295/report-thumb.jpg"}],"country":"United States","state":"Connecticut,  Massachusetts","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.25,\n              42.25\n            ],\n            [\n              -72.625,\n              42.25\n            ],\n            [\n              -72.625,\n              41.5772\n            ],\n            [\n              -72.25,\n              41.5772\n            ],\n            [\n              -72.25,\n              42.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Supercedes OFR 77-544","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abee4b07f02db674deb","contributors":{"authors":[{"text":"Leo, G. W.","contributorId":102899,"corporation":false,"usgs":true,"family":"Leo","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":220069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":220067,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brookins, D. G.","contributorId":93963,"corporation":false,"usgs":true,"family":"Brookins","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":220068,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57285,"text":"wdrOR831 - 1984 - Water resources data, Oregon water year 1983, volume 1: Eastern Oregon","interactions":[],"lastModifiedDate":"2020-06-11T15:20:28.431567","indexId":"wdrOR831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OR-83-1","title":"Water resources data, Oregon water year 1983, volume 1: Eastern Oregon","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrOR831","usgsCitation":"Hubbard, L., Parks, T., and Weiss, D., 1984, Water resources data, Oregon water year 1983, volume 1: Eastern Oregon: U.S. Geological Survey Water Data Report OR-83-1, 202 p., https://doi.org/10.3133/wdrOR831.","productDescription":"202 p.","costCenters":[],"links":[{"id":375169,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/or-83-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/or-83-1/report-thumb.jpg"}],"country":"United States","state":"Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.81640624999999,\n              45.66012730272194\n            ],\n            [\n              -122.14599609375001,\n              43.83452678223682\n            ],\n            [\n              -122.49755859375,\n              42.13082130188811\n            ],\n            [\n              -122.34374999999999,\n              42.00032514831621\n            ],\n            [\n              -117.09228515624999,\n              42.032974332441405\n            ],\n            [\n              -117.04833984375001,\n              44.18220395771566\n            ],\n            [\n              -117.18017578125,\n              44.4808302785626\n            ],\n            [\n              -116.82861328125001,\n              44.94924926661153\n            ],\n            [\n              -116.54296874999999,\n              45.767522962149876\n            ],\n            [\n              -116.98242187499999,\n              45.9511496866914\n            ],\n            [\n              -119.02587890624999,\n              45.96642454131025\n            ],\n            [\n              -120.52001953124999,\n              45.67548217560647\n            ],\n            [\n              -121.81640624999999,\n              45.66012730272194\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faf3f","contributors":{"authors":[{"text":"Hubbard, L.L.","contributorId":81513,"corporation":false,"usgs":true,"family":"Hubbard","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":256576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parks, T.D.","contributorId":17257,"corporation":false,"usgs":true,"family":"Parks","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":256574,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiss, D.L.","contributorId":68812,"corporation":false,"usgs":true,"family":"Weiss","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":256575,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7583,"text":"ofr84695 - 1984 - Twenty-two measured sections of Cretaceous-lower Tertiary rocks, eastern North Slope, Alaska","interactions":[],"lastModifiedDate":"2022-10-12T18:19:04.521099","indexId":"ofr84695","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-695","title":"Twenty-two measured sections of Cretaceous-lower Tertiary rocks, eastern North Slope, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84695","usgsCitation":"Molenaar, C.M., Kirk, A.R., Magoon, L.B., and Huffman, A., 1984, Twenty-two measured sections of Cretaceous-lower Tertiary rocks, eastern North Slope, Alaska: U.S. Geological Survey Open-File Report 84-695, Report: i 19 p.; 4 Plates: 7.61 × 17.61 inches or smaller, https://doi.org/10.3133/ofr84695.","productDescription":"Report: i 19 p.; 4 Plates: 7.61 × 17.61 inches or smaller","costCenters":[],"links":[{"id":35067,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0695/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35066,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0695/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35065,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0695/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0695/report-thumb.jpg"},{"id":408223,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13528.htm","linkFileType":{"id":5,"text":"html"}},{"id":35069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0695/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35068,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0695/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"eastern North Slope","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.333,\n              69\n            ],\n            [\n              -144,\n              69\n            ],\n            [\n              -144,\n              69.75\n            ],\n            [\n              -149.333,\n              69.75\n            ],\n            [\n              -149.333,\n              69\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623c84","contributors":{"authors":[{"text":"Molenaar, C. M.","contributorId":77904,"corporation":false,"usgs":false,"family":"Molenaar","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156226,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirk, A. R.","contributorId":34911,"corporation":false,"usgs":true,"family":"Kirk","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":156223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Magoon, L. B.","contributorId":44531,"corporation":false,"usgs":true,"family":"Magoon","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":156224,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Huffman, A. C.","contributorId":55422,"corporation":false,"usgs":true,"family":"Huffman","given":"A. C.","affiliations":[],"preferred":false,"id":156225,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38647,"text":"pp1151D - 1984 - Stratigraphy and structure of the western Kentucky fluorspar district","interactions":[],"lastModifiedDate":"2012-02-02T00:09:58","indexId":"pp1151D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1151","chapter":"D","title":"Stratigraphy and structure of the western Kentucky fluorspar district","docAbstract":"The western Kentucky fluorspar district is part of the larger Illinois-Kentucky fluorspar district, the largest producer of fluorspar in the United States. This report is based largely on data gathered from 1960 to 1974 during the U.S. Geological Survey-Kentucky Geological Survey cooperative geologic mapping program of Kentucky. It deals chiefly with the stratigraphy and structure of the district and, to a lesser extent, with the fluorspar-zinc-lead-barite deposits. \r\n\r\nSedimentary rocks exposed in the district range in age from Early Mississippian (Osagean) to Quaternary. Most rocks exposed at the surface are Mississippian in age; two-thirds are marine fossiliferous limestones, and the remainder are shales, siltstones, and sandstones. Osagean deep-water marine silty limestone and chert are present at the surface in the southwestern corner of the district. Meramecian marine limestone is exposed at the surface in about half the area. Chesterian marine and fluvial to fluviodeltaic clastic sedimentary rocks and marine limestone underlie about one-third of the area. The total sequence of Mississippian rocks is about 3,000 ft thick. \r\n\r\nPennsylvanian rocks are dominantly fluvial clastic sedimentary rocks that change upward into younger fluviodeltaic strata. Pennsylvanian strata of Morrowan and Atokan age are locally thicker than 600 ft along the eastern and southeastern margin and in the major grabens of the district where they have been preserved from erosion. \r\n\r\nCretaceous and Tertiary sediments of the Mississippi embayment truncate Paleozoic formations in and near the southwestern corner of the district and are preserved mostly as erosional outliers. The deposits are Gulfian nonmarine gravels, sands, and clays as much as 170 ft thick and upper Pliocene fluvial continental deposits as thick as 45 ft. Pleistocene loess deposits mantle the upland surface of the district, and Quaternary fluvial and fluviolacustrine deposits are common and widespread along the Ohio and Cumberland Rivers and their major tributaries. \r\n\r\nMany mafic dikes and a few mafic sills are present. The mafic rocks are mostly altered mica peridotites or lamprophyres that are composed of carbonate minerals, serpentine, chlorite, and biotite and contain some hornblende, pyroxene, and olivine. Most of the dikes are in a north-north west-trending belt 6 to 8 mi wide and strike N. 20 0 -30 0 W. The dikes dip from 80 0 to 90 0 and are commonly 5 to 10 ft wide. Radioisotopic study indicates that the dikes are Early Permian in age. \r\n\r\nThe district is just southeast of the intersection of the east-trending Rough Creek-Shawneetown and northeast-trending New Madrid fault systems. The district's principal structural features are a northwest-trending domal anticline, the Tolu Arch, and a series of steeply dipping to nearly vertical normal faults and fault zones that trend dominantly northeastward and divide the area into elongated northeast-trending grabens and horsts. Formation of these grabens and horsts was one of the major tectonic events in the district. Vertical displacement may be as much as 3,000 ft but commonly ranges from a few feet to a few hundred feet; no substantial horizontal movement is believed to have taken place. Many cross faults having only a few feet of displacement trend northwestward and are occupied at places by mafic dikes. Faulting was mostly post-Early Permian to pre-middle Cretaceous in age. \r\n\r\nMany theories have been advanced to explain the structural history of the district. A generally acceptable overall hypothesis that would account for all the structural complexities, however, is still lacking. Useful structural data, such as the structural differences between the grabens and the horsts, have been obtained, however, from the recently completed geologic mapping. Mapping also has more clearly shown the alinement of the Tolu Arch, the belt of dikes, and an unusually deep graben (the Griffith Bluff graben); this alinement suggests that possibl","language":"ENGLISH","doi":"10.3133/pp1151D","usgsCitation":"Trace, R.D., and Amos, D., 1984, Stratigraphy and structure of the western Kentucky fluorspar district: U.S. Geological Survey Professional Paper 1151, p. D1-D41; 1 plate in pocket, https://doi.org/10.3133/pp1151D.","productDescription":"p. D1-D41; 1 plate in pocket","costCenters":[],"links":[{"id":119900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1151d/report-thumb.jpg"},{"id":65478,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1151d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65479,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1151d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a7fee","contributors":{"authors":[{"text":"Trace, R. D.","contributorId":47004,"corporation":false,"usgs":true,"family":"Trace","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":220215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Amos, D.H.","contributorId":75600,"corporation":false,"usgs":true,"family":"Amos","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":220216,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11641,"text":"ofr83948 - 1984 - Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States","interactions":[{"subject":{"id":11641,"text":"ofr83948 - 1984 - Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States","indexId":"ofr83948","publicationYear":"1984","noYear":false,"title":"Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States"},"predicate":"SUPERSEDED_BY","object":{"id":2967,"text":"wsp2276 - 1986 - Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States","indexId":"wsp2276","publicationYear":"1986","noYear":false,"title":"Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States"},"id":1}],"supersededBy":{"id":2967,"text":"wsp2276 - 1986 - Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States","indexId":"wsp2276","publicationYear":"1986","noYear":false,"title":"Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States"},"lastModifiedDate":"2021-01-26T20:35:22.176536","indexId":"ofr83948","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-948","title":"Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83948","usgsCitation":"Wetzel, K.L., and Bettandorff, J., 1984, Techniques for estimating streamflow characteristics in the Eastern and Interior coal provinces of the United States: U.S. Geological Survey Open-File Report 83-948, Report: v, 95 p.; 2 Plates: 28.99 x 28.04 inches and 27.71 x 28.21 inches, https://doi.org/10.3133/ofr83948.","productDescription":"Report: v, 95 p.; 2 Plates: 28.99 x 28.04 inches and 27.71 x 28.21 inches","costCenters":[],"links":[{"id":145105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0948/report-thumb.jpg"},{"id":382613,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0948/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382615,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0948/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382614,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0948/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a4a","contributors":{"authors":[{"text":"Wetzel, K. L.","contributorId":14418,"corporation":false,"usgs":true,"family":"Wetzel","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163490,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bettandorff, J.M.","contributorId":67499,"corporation":false,"usgs":true,"family":"Bettandorff","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":163491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8094,"text":"ofr8465 - 1984 - Floods in south-central Oklahoma and north-central Texas, October 1981","interactions":[],"lastModifiedDate":"2017-06-14T14:30:00","indexId":"ofr8465","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-65","title":"Floods in south-central Oklahoma and north-central Texas, October 1981","docAbstract":"<p>Heavy rains fell over south-central Oklahoma and north-central Texas during October 11-14, 1981, causing record flooding in both States. Six lives were lost, many people were temporarily left homeless, and damages amounted to nearly $115 million. The maximum rainfall of 23 inches occurred 5 miles north of Clyde, Texas, in about 34 hours.</p>\n<p>Flood discharges along the East Fork Little Wichita River in Texas and along the Blue River, Clear Boggy Creek, and part of Muddy Boggy Creek in Oklahoma in the Red River basin exceeded those previously known. The Red River near Gainesville, Texas, had a record stage. Severe flooding also occurred along the West Fork and Elm Fork Trinity Rivers in Texas. The Brazos River experienced record flooding along tributaries in Abilene and Breckenridge, Texas, and the Brazos River near Glen Rose had a record stage that was almost 1.5 feet higher than any previous flood.</p>\n<p>Substantial reductions in peak stages and discharges on the West Fork Trinity River downstream from Eagle Mountain Reservoir were attained as a result of reservoir storage. All floodwater on the Elm Fork Trinity River was contained by reservoir storage thus preventing a potentially devastating flood downstream on the Trinity River. Maximum stages and discharges and/or contents were recorded during and after this major flood at 83 gaging stations, crest-stage stations, reservoir stations, and a miscellaneous site.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8465","usgsCitation":"Buckner, H.D., and Kurklin, J.K., 1984, Floods in south-central Oklahoma and north-central Texas, October 1981: U.S. Geological Survey Open-File Report 84-65, v, 112 p., https://doi.org/10.3133/ofr8465.","productDescription":"v, 112 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":141339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0065/report-thumb.jpg"},{"id":35693,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0065/report.pdf","text":"Report","size":"3.67 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oklahoma, Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.17431640625,\n              36.049098959065645\n            ],\n            [\n              -101.14013671875,\n              32.879587173066305\n            ],\n            [\n              -99.931640625,\n              31.42866311735861\n            ],\n            [\n              -94.98779296875,\n              34.831841149828655\n            ],\n            [\n              -96.17431640625,\n              36.049098959065645\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b118c","contributors":{"authors":[{"text":"Buckner, Harold D.","contributorId":173633,"corporation":false,"usgs":false,"family":"Buckner","given":"Harold","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurklin, Joanne K.","contributorId":173634,"corporation":false,"usgs":false,"family":"Kurklin","given":"Joanne","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":157136,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38532,"text":"pp1312 - 1984 - The Richmond and Greenwich slices of the Hamburg klippe in eastern Pennsylvania — Stratigraphy, sedimentology, structure, and plate tectonic implications","interactions":[],"lastModifiedDate":"2022-09-12T21:48:12.293122","indexId":"pp1312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1312","title":"The Richmond and Greenwich slices of the Hamburg klippe in eastern Pennsylvania — Stratigraphy, sedimentology, structure, and plate tectonic implications","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1312","usgsCitation":"Lash, G.G., and Drake, A.A., 1984, The Richmond and Greenwich slices of the Hamburg klippe in eastern Pennsylvania — Stratigraphy, sedimentology, structure, and plate tectonic implications: U.S. Geological Survey Professional Paper 1312, 40 p., https://doi.org/10.3133/pp1312.","productDescription":"40 p.","costCenters":[],"links":[{"id":406568,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74325.htm","linkFileType":{"id":5,"text":"html"}},{"id":65295,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1312/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1312/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Richmond and Greenwich slices of the Hamburg klippe","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.0519,\n              40.4614\n            ],\n            [\n              -75.6978,\n              40.4614\n            ],\n            [\n              -75.6978,\n              40.6889\n            ],\n            [\n              -76.0519,\n              40.6889\n            ],\n            [\n              -76.0519,\n              40.4614\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67acbe","contributors":{"authors":[{"text":"Lash, G. G.","contributorId":60648,"corporation":false,"usgs":true,"family":"Lash","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":220010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drake, Avery A. Jr.","contributorId":81090,"corporation":false,"usgs":true,"family":"Drake","given":"Avery","suffix":"Jr.","middleInitial":"A.","affiliations":[],"preferred":false,"id":220011,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34758,"text":"b1558D - 1984 - White clays of Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T12:23:48","indexId":"b1558D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1558","chapter":"D","title":"White clays of Pennsylvania","docAbstract":"<p>The white clays of Pennsylvania are composed chiefly of kaolinite and various amounts of illite. Most of the white clays are silty and a few are sandy. Quartz or chert is the only nonclay mineral in the whitest material; goethite is also present in the colored samples high in iron. The average alumina content is slightly more than 20 percent in samples from three clay pits and less than 15 percent in samples from five clay pits. The white clay deposits are found in eastern, south-central, and central Pennsylvania. They occur in rocks of the Appalachian basin that range in age from Cambrian to Devonian; however, their age of formation is Cretaceous or later. Some of the deposits are the result of katamorphic alteration, and some are the result of weathered material being transported and deposited in sinkaoles or caverns. The presence of alunite in one deposit suggests the possibility that the clay may be the result of both katamorphic and hydrothermal alteration.</p>","largerWorkTitle":"Contributions to the geology of mineral deposits","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1558D","usgsCitation":"Hosterman, J.W., 1984, White clays of Pennsylvania: U.S. Geological Survey Bulletin 1558, iv, 38 p., https://doi.org/10.3133/b1558D.","productDescription":"iv, 38 p.","startPage":"D1","endPage":"D38","costCenters":[],"links":[{"id":62632,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1558d/report.pdf","text":"Report","size":"4.23 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":165880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1558d/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"Blair County, Centre County, Cumberland County, Huntingdon County, Lancaster County, Monroe County, York County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-78.2587,40.2971],[-78.2906,40.2448],[-78.4353,40.3009],[-78.4429,40.2778],[-78.4449,40.2519],[-78.4497,40.2451],[-78.5057,40.2868],[-78.622,40.3253],[-78.6037,40.3477],[-78.5587,40.3675],[-78.5547,40.422],[-78.5592,40.4437],[-78.5421,40.4734],[-78.5408,40.5042],[-78.511,40.5353],[-78.4743,40.5514],[-78.4411,40.5975],[-78.4468,40.6242],[-78.4405,40.6442],[-78.4266,40.6475],[-78.4102,40.6431],[-78.3511,40.722],[-78.3739,40.7472],[-78.3746,40.7567],[-78.3541,40.77],[-78.3381,40.7973],[-78.3169,40.8075],[-78.3019,40.8225],[-78.3021,40.8343],[-78.2883,40.8498],[-78.2676,40.8477],[-78.2476,40.8569],[-78.2466,40.8714],[-78.2381,40.8733],[-78.2478,40.8764],[-78.2418,40.8814],[-78.2333,40.8792],[-78.2284,40.8824],[-78.2213,40.8915],[-78.2281,40.9028],[-78.2214,40.9096],[-78.1857,40.9212],[-78.1706,40.9362],[-78.1561,40.9431],[-78.1598,40.9531],[-78.1677,40.953],[-78.1684,40.9589],[-78.1483,40.9568],[-78.1452,40.9486],[-78.1368,40.965],[-78.1326,40.9641],[-78.1324,40.9482],[-78.1202,40.9442],[-78.0789,40.9566],[-78.0796,40.963],[-78.0894,40.9707],[-78.0822,40.9839],[-78.0853,40.9934],[-78.0689,40.9984],[-78.0634,40.9953],[-78.0635,41.003],[-78.0556,41.0085],[-78.0593,41.0139],[-78.0672,41.0148],[-78.0673,41.022],[-78.0783,41.0329],[-78.0565,41.0393],[-78.0614,41.0457],[-78.059,41.0529],[-78.07,41.0524],[-78.0731,41.0592],[-78.0877,41.0596],[-78.0853,41.0682],[-78.0957,41.0741],[-78.0927,41.0777],[-78.1107,41.1135],[-78.1077,41.1189],[-78.0986,41.1213],[-78.09,41.1172],[-78.084,41.1268],[-78.0675,41.1246],[-78.0694,41.1309],[-78.0572,41.1328],[-78.0536,41.1446],[-78.0408,41.1478],[-78.0372,41.1533],[-78.0153,41.1534],[-78.0103,41.1448],[-78.0024,41.1462],[-77.9964,41.1648],[-77.9885,41.163],[-77.9843,41.1703],[-77.9739,41.1731],[-77.9729,41.2035],[-77.9595,41.2176],[-77.9369,41.2104],[-77.9376,41.224],[-77.9205,41.2291],[-77.9108,41.2441],[-77.8968,41.2537],[-77.8934,41.177],[-77.8055,41.1804],[-77.7454,41.1093],[-77.729,41.1129],[-77.7168,41.108],[-77.7052,41.1148],[-77.6948,41.1098],[-77.6643,41.1094],[-77.6576,41.1022],[-77.6326,41.0954],[-77.5948,41.0741],[-77.5698,41.0668],[-77.5631,41.0591],[-77.5801,41.0496],[-77.5082,40.963],[-77.3317,40.9887],[-77.1427,41.0441],[-77.2032,40.993],[-77.2796,40.9097],[-77.3594,40.8486],[-77.3788,40.8454],[-77.5938,40.7611],[-77.6526,40.7438],[-77.6817,40.7297],[-77.6743,40.7183],[-77.698,40.707],[-77.6979,40.697],[-77.7058,40.6938],[-77.7015,40.6807],[-77.6852,40.6861],[-77.6827,40.683],[-77.7498,40.6343],[-77.7753,40.6243],[-77.8277,40.572],[-77.8385,40.5479],[-77.8165,40.5004],[-77.8934,40.4262],[-77.8958,40.4185],[-77.8891,40.3954],[-77.8697,40.3937],[-77.8727,40.3846],[-77.8599,40.3687],[-77.8437,40.3697],[-77.8213,40.3625],[-77.8111,40.3698],[-77.7634,40.3694],[-77.7502,40.3785],[-77.7022,40.2662],[-77.7208,40.2534],[-77.77,40.2016],[-77.8632,40.064],[-77.9223,40.1037],[-78.0813,40.1362],[-78.1932,40.1973],[-78.2386,40.2252],[-78.2587,40.2971]]],[[[-77.1386,40.0718],[-77.1814,40.0324],[-77.3022,40.015],[-77.4019,39.9933],[-77.4703,39.9444],[-77.4529,39.9725],[-77.4811,39.9925],[-77.5033,40.0147],[-77.5219,40.0505],[-77.5418,40.0736],[-77.546,40.0913],[-77.5598,40.0976],[-77.5634,40.1217],[-77.5821,40.1348],[-77.5917,40.1362],[-77.5941,40.1439],[-77.6104,40.1588],[-77.6183,40.1778],[-77.5936,40.1915],[-77.5617,40.2169],[-77.534,40.2223],[-77.4099,40.2971],[-77.3677,40.3157],[-77.3586,40.3152],[-77.3586,40.3089],[-77.4057,40.2794],[-77.4208,40.2654],[-77.4202,40.259],[-77.4118,40.2572],[-77.3907,40.2631],[-77.3303,40.2934],[-77.3243,40.2902],[-77.3304,40.278],[-77.3111,40.2698],[-77.2357,40.2869],[-77.0898,40.3028],[-77.0138,40.3048],[-76.954,40.3155],[-76.9159,40.3298],[-76.9136,40.318],[-76.9234,40.294],[-76.9068,40.2658],[-76.8614,40.2266],[-76.8379,40.2202],[-76.8285,40.2042],[-76.8002,40.2],[-76.7535,40.1757],[-76.7488,40.1675],[-76.7455,40.1353],[-76.7234,40.122],[-76.696,40.1549],[-76.6791,40.1503],[-76.6645,40.1652],[-76.6459,40.1669],[-76.6174,40.1812],[-76.6089,40.1902],[-76.5733,40.1954],[-76.4372,40.2387],[-76.3134,40.2567],[-76.1514,40.3158],[-75.8757,40.1371],[-75.9412,40.1093],[-75.935,40.0394],[-75.9869,39.9675],[-75.992,39.9544],[-75.9875,39.9399],[-75.9805,39.9334],[-75.9968,39.9282],[-75.9961,39.9028],[-75.9885,39.895],[-75.9912,39.8801],[-75.9877,39.8732],[-75.9932,39.8697],[-76.0015,39.8738],[-76.0091,39.8544],[-76.0211,39.8537],[-76.0191,39.8337],[-76.032,39.8207],[-76.0303,39.813],[-76.0506,39.7846],[-76.0615,39.7789],[-76.066,39.7644],[-76.0841,39.7592],[-76.0909,39.7452],[-76.1011,39.7449],[-76.0959,39.7362],[-76.0996,39.7285],[-76.1104,39.7268],[-76.1115,39.735],[-76.1198,39.7364],[-76.1188,39.726],[-76.1337,39.728],[-76.1392,39.7223],[-76.9998,39.7197],[-77.0002,39.8314],[-76.9888,39.8359],[-76.9815,39.8477],[-76.9581,39.8567],[-76.9652,39.8721],[-76.9771,39.8749],[-76.9848,39.9007],[-76.972,39.9161],[-76.9731,39.932],[-76.9683,39.936],[-77.023,40.0165],[-77.0619,40.0243],[-77.0984,40.0612],[-77.1386,40.0718]]],[[[-75.3273,41.2377],[-75.1276,41.2536],[-75.1561,41.1516],[-75.0764,41.1419],[-75.0267,41.082],[-75.0025,41.0924],[-74.9939,41.094],[-74.9854,41.0888],[-74.9676,41.0971],[-74.9659,41.0939],[-74.9804,41.0806],[-75.0121,41.067],[-75.0265,41.0416],[-75.035,41.0358],[-75.0671,41.0195],[-75.1073,41.0063],[-75.1309,40.9918],[-75.138,40.9761],[-75.1208,40.9662],[-75.1542,40.9496],[-75.1738,40.9477],[-75.1856,40.9384],[-75.2157,40.9312],[-75.2258,40.9182],[-75.2426,40.9081],[-75.2374,40.8989],[-75.2614,40.888],[-75.2877,40.8639],[-75.3239,40.8546],[-75.3842,40.8293],[-75.4757,40.8135],[-75.4866,40.8382],[-75.5663,40.9461],[-75.5343,40.9596],[-75.5389,40.967],[-75.4963,40.9894],[-75.5676,41.0523],[-75.5745,41.0678],[-75.6015,41.0863],[-75.6043,41.095],[-75.6121,41.0974],[-75.6185,41.1093],[-75.6428,41.1146],[-75.6474,41.1233],[-75.6437,41.1278],[-75.6333,41.1254],[-75.6234,41.1316],[-75.6263,41.138],[-75.6114,41.1473],[-75.6125,41.1514],[-75.604,41.1517],[-75.5967,41.1721],[-75.5764,41.179],[-75.5685,41.1984],[-75.5542,41.2086],[-75.5409,41.2257],[-75.5286,41.2273],[-75.516,41.2207],[-75.5083,41.2324],[-75.3794,41.2326],[-75.3273,41.2377]]]]},\"properties\":{\"name\":\"Blair\",\"state\":\"PA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e491c","contributors":{"authors":[{"text":"Hosterman, John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":213529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56207,"text":"wdrNY831 - 1984 - Water resources data, New York, water year 1983, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2020-11-23T19:12:34.38152","indexId":"wdrNY831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-83-1","title":"Water resources data, New York, water year 1983, volume 1, eastern New York, excluding Long Island","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY831","usgsCitation":"Lumia, R., Archer, R., Burke, P.M., and Dalton, F., 1984, Water resources data, New York, water year 1983, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report NY-83-1, viii, 240 p., https://doi.org/10.3133/wdrNY831.","productDescription":"viii, 240 p.","costCenters":[],"links":[{"id":380709,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/ny-83-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/ny-83-1/report-thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-74.04086,40.700117],[-74.037998,40.698995],[-74.044451,40.688445],[-74.046359,40.689175],[-74.04086,40.700117]]],[[[-74.144428,40.53516],[-74.177986,40.519603],[-74.182157,40.520634],[-74.199923,40.511729],[-74.210474,40.509448],[-74.219787,40.502603],[-74.23324,40.501299],[-74.246688,40.496103],[-74.250188,40.496703],[-74.254588,40.502303],[-74.256088,40.507903],[-74.252702,40.513895],[-74.242888,40.520903],[-74.241732,40.531273],[-74.247808,40.543396],[-74.229002,40.555041],[-74.216997,40.554991],[-74.210887,40.560902],[-74.204054,40.589336],[-74.19682,40.597037],[-74.195407,40.601806],[-74.196096,40.616169],[-74.200994,40.616906],[-74.201812,40.619507],[-74.20058,40.631448],[-74.1894,40.642121],[-74.180191,40.645521],[-74.174085,40.645109],[-74.170187,40.642201],[-74.152973,40.638886],[-74.120186,40.642201],[-74.086485,40.648601],[-74.075884,40.648101],[-74.0697,40.641216],[-74.067598,40.623865],[-74.053125,40.603678],[-74.059184,40.593502],[-74.111471,40.546908],[-74.121672,40.542691],[-74.137241,40.530076],[-74.144428,40.53516]]],[[[-72.132225,41.104387],[-72.128352,41.108131],[-72.126704,41.115139],[-72.084207,41.101524],[-72.081167,41.09394],[-72.086975,41.058292],[-72.0972,41.054884],[-72.097136,41.075844],[-72.1064,41.088883],[-72.12056,41.093171],[-72.139233,41.092451],[-72.141921,41.094371],[-72.142929,41.097811],[-72.140737,41.100835],[-72.132225,41.104387]]],[[[-71.943563,41.286675],[-71.926802,41.290122],[-71.935259,41.280579],[-71.978926,41.265002],[-72.002461,41.252867],[-72.036846,41.249794],[-72.029438,41.26309],[-72.018926,41.274114],[-72.006872,41.27348],[-71.991117,41.281331],[-71.980061,41.280291],[-71.943563,41.286675]]],[[[-73.767176,40.886299],[-73.766276,40.881099],[-73.770876,40.879299],[-73.775276,40.882199],[-73.770576,40.888399],[-73.767176,40.886299]]],[[[-73.773361,40.859449],[-73.770552,40.86033],[-73.766333,40.857317],[-73.766032,40.844961],[-73.769648,40.84466],[-73.773038,40.848125],[-73.773361,40.859449]]],[[[-74.027392,44.995765],[-73.874597,45.001223],[-73.639718,45.003464],[-73.343124,45.01084],[-73.354633,44.987352],[-73.350218,44.976222],[-73.338734,44.965886],[-73.338979,44.917681],[-73.353657,44.907346],[-73.35808,44.901325],[-73.369103,44.86668],[-73.379822,44.857037],[-73.381359,44.845021],[-73.379452,44.83801],[-73.375345,44.836307],[-73.369647,44.829136],[-73.354945,44.8215],[-73.335443,44.804602],[-73.333154,44.788759],[-73.335713,44.782086],[-73.347072,44.772988],[-73.354361,44.755296],[-73.365561,44.741786],[-73.36556,44.700297],[-73.361323,44.695369],[-73.365297,44.687546],[-73.370142,44.684853],[-73.367209,44.678513],[-73.371089,44.67753],[-73.37272,44.668739],[-73.369669,44.663478],[-73.379074,44.656772],[-73.378014,44.653846],[-73.383157,44.645764],[-73.378561,44.641475],[-73.386783,44.636369],[-73.386497,44.626924],[-73.390231,44.618353],[-73.382932,44.612184],[-73.376849,44.599598],[-73.376806,44.595455],[-73.381848,44.589316],[-73.375666,44.582038],[-73.374389,44.575455],[-73.356788,44.557918],[-73.338751,44.548046],[-73.3393,44.544477],[-73.331595,44.535924],[-73.329458,44.529203],[-73.322026,44.525289],[-73.320836,44.513631],[-73.306707,44.500334],[-73.304418,44.485739],[-73.298939,44.471304],[-73.300114,44.454711],[-73.293613,44.440559],[-73.296031,44.428339],[-73.310491,44.402601],[-73.315016,44.388513],[-73.333575,44.372288],[-73.334939,44.364441],[-73.334637,44.356877],[-73.323997,44.333842],[-73.324229,44.310023],[-73.312299,44.280025],[-73.311025,44.27424],[-73.312852,44.265346],[-73.323596,44.243897],[-73.329322,44.244504],[-73.34323,44.238049],[-73.342312,44.234531],[-73.349889,44.230356],[-73.362013,44.208545],[-73.382252,44.197178],[-73.383987,44.193158],[-73.390583,44.190886],[-73.389658,44.181249],[-73.396892,44.173846],[-73.395399,44.166903],[-73.398728,44.162248],[-73.402381,44.145856],[-73.415761,44.132826],[-73.411316,44.112686],[-73.416319,44.099422],[-73.429239,44.079414],[-73.43774,44.045006],[-73.42312,44.032759],[-73.410776,44.026944],[-73.407739,44.021312],[-73.405977,44.011485],[-73.412613,43.97998],[-73.406823,43.967317],[-73.405525,43.948813],[-73.408589,43.932933],[-73.395878,43.903044],[-73.383491,43.890951],[-73.374051,43.875563],[-73.382046,43.855008],[-73.372462,43.846266],[-73.373688,43.84261],[-73.388389,43.832404],[-73.392492,43.820779],[-73.380804,43.810951],[-73.376361,43.798766],[-73.357547,43.785933],[-73.354758,43.776721],[-73.350593,43.771939],[-73.369725,43.744274],[-73.370612,43.725329],[-73.385883,43.711336],[-73.395517,43.696831],[-73.404739,43.690213],[-73.404126,43.681339],[-73.415513,43.65245],[-73.426463,43.642598],[-73.42791,43.634428],[-73.417668,43.621687],[-73.423708,43.612356],[-73.421616,43.603023],[-73.431229,43.588285],[-73.428636,43.583994],[-73.420378,43.581489],[-73.405629,43.571179],[-73.395767,43.568087],[-73.383369,43.57677],[-73.383446,43.596778],[-73.372469,43.604848],[-73.376036,43.612596],[-73.369933,43.619093],[-73.371889,43.624489],[-73.347621,43.622509],[-73.342181,43.62607],[-73.323893,43.627629],[-73.310606,43.624114],[-73.306234,43.628018],[-73.302076,43.624364],[-73.300285,43.610806],[-73.292232,43.60255],[-73.292801,43.593861],[-73.296924,43.587323],[-73.292364,43.585104],[-73.294621,43.57897],[-73.284912,43.579272],[-73.279726,43.574241],[-73.26938,43.571973],[-73.258631,43.564949],[-73.248641,43.553857],[-73.250132,43.543429],[-73.246585,43.541855],[-73.24139,43.532345],[-73.247698,43.523173],[-73.256493,43.259249],[-73.26978,43.035923],[-73.278673,42.83341],[-73.285388,42.834093],[-73.287063,42.82014],[-73.28375,42.813864],[-73.290944,42.80192],[-73.276421,42.746019],[-73.264957,42.74594],[-73.508142,42.086257],[-73.496879,42.049675],[-73.487314,42.049638],[-73.489615,42.000092],[-73.521041,41.619773],[-73.550961,41.295422],[-73.482709,41.21276],[-73.727775,41.100696],[-73.654671,41.011697],[-73.659372,40.999497],[-73.659671,40.987909],[-73.655972,40.979597],[-73.662072,40.966198],[-73.664472,40.967198],[-73.678073,40.962798],[-73.686473,40.945198],[-73.721739,40.932037],[-73.756776,40.912599],[-73.781338,40.885447],[-73.784803,40.878528],[-73.788786,40.858485],[-73.78806,40.854131],[-73.782174,40.847358],[-73.781206,40.838891],[-73.783867,40.836795],[-73.785399,40.838004],[-73.791044,40.846552],[-73.789512,40.85139],[-73.793785,40.855583],[-73.799543,40.848027],[-73.806914,40.849501],[-73.81281,40.846737],[-73.815205,40.831075],[-73.804518,40.818546],[-73.797332,40.815597],[-73.781369,40.794907],[-73.776032,40.795275],[-73.768431,40.800704],[-73.754032,40.820941],[-73.7544,40.826837],[-73.728275,40.8529],[-73.726675,40.8568],[-73.729575,40.8665],[-73.713674,40.870099],[-73.675573,40.856999],[-73.655872,40.863899],[-73.654372,40.878199],[-73.633771,40.898198],[-73.617571,40.897898],[-73.569969,40.915398],[-73.566169,40.915798],[-73.548068,40.908698],[-73.519267,40.914298],[-73.514999,40.912821],[-73.499941,40.918166],[-73.491765,40.942097],[-73.485365,40.946397],[-73.463708,40.937697],[-73.437509,40.934985],[-73.429863,40.929797],[-73.428836,40.921506],[-73.406074,40.920235],[-73.402963,40.925097],[-73.403462,40.942197],[-73.400862,40.953997],[-73.392862,40.955297],[-73.374462,40.937597],[-73.365961,40.931697],[-73.352761,40.926697],[-73.345561,40.925297],[-73.344161,40.927297],[-73.33136,40.929597],[-73.295061,40.924497],[-73.229285,40.905121],[-73.148994,40.928898],[-73.146242,40.935074],[-73.144673,40.955842],[-73.140785,40.966178],[-73.110368,40.971938],[-73.081582,40.973058],[-73.043701,40.962185],[-73.040445,40.964498],[-72.995931,40.966498],[-72.88825,40.962962],[-72.826057,40.969794],[-72.774104,40.965314],[-72.760031,40.975334],[-72.714425,40.985596],[-72.689341,40.989776],[-72.665018,40.987496],[-72.585327,40.997587],[-72.565406,41.009508],[-72.560974,41.015444],[-72.549853,41.019844],[-72.521548,41.037652],[-72.477306,41.052212],[-72.460778,41.067012],[-72.445242,41.086116],[-72.417945,41.087955],[-72.397,41.096307],[-72.356087,41.133635],[-72.322381,41.140664],[-72.291109,41.155874],[-72.278789,41.158722],[-72.2681,41.154146],[-72.245348,41.161217],[-72.238211,41.15949],[-72.237731,41.156434],[-72.253572,41.137138],[-72.265124,41.128482],[-72.300374,41.112274],[-72.300044,41.132059],[-72.306381,41.13784],[-72.318146,41.137134],[-72.32663,41.132162],[-72.335271,41.120274],[-72.335177,41.106917],[-72.317238,41.088659],[-72.297718,41.081042],[-72.280373,41.080402],[-72.276709,41.076722],[-72.283093,41.067874],[-72.273657,41.051533],[-72.260515,41.042065],[-72.229364,41.044355],[-72.201859,41.032275],[-72.190563,41.032579],[-72.183266,41.035619],[-72.174882,41.046147],[-72.162898,41.053187],[-72.153857,41.051859],[-72.137297,41.039684],[-72.135137,41.031284],[-72.137409,41.023908],[-72.116368,40.999796],[-72.10216,40.991509],[-72.095456,40.991349],[-72.083039,40.996453],[-72.076175,41.009093],[-72.061448,41.009442],[-72.057934,41.004789],[-72.051585,41.006437],[-72.049526,41.009697],[-72.051928,41.020506],[-72.047468,41.022565],[-72.035792,41.020759],[-72.015013,41.028348],[-71.99926,41.039669],[-71.96704,41.047772],[-71.961078,41.054277],[-71.959595,41.071237],[-71.93825,41.077413],[-71.899256,41.080837],[-71.889543,41.075701],[-71.869558,41.075046],[-71.86447,41.076918],[-71.857494,41.073558],[-71.856214,41.070598],[-71.87391,41.052278],[-71.903736,41.040166],[-71.935689,41.034182],[-72.029357,40.999909],[-72.114448,40.972085],[-72.39585,40.86666],[-72.469996,40.84274],[-72.753112,40.763571],[-72.768152,40.761587],[-72.863164,40.732962],[-73.054963,40.666371],[-73.20844,40.630884],[-73.262106,40.621476],[-73.306396,40.620756],[-73.319257,40.635795],[-73.351465,40.6305],[-73.391967,40.617501],[-73.450369,40.603501],[-73.562372,40.583703],[-73.610873,40.587703],[-73.646674,40.582804],[-73.754776,40.584404],[-73.753349,40.59056],[-73.774928,40.590759],[-73.834408,40.577201],[-73.878906,40.560888],[-73.934512,40.545175],[-73.932729,40.560266],[-73.935686,40.564914],[-73.95005,40.573363],[-73.991346,40.57035],[-74.002056,40.570623],[-74.012022,40.574528],[-74.012996,40.578169],[-74.001591,40.590684],[-74.003281,40.595754],[-74.010926,40.600789],[-74.032856,40.604421],[-74.03959,40.612934],[-74.042412,40.624847],[-74.038336,40.637074],[-74.032066,40.646479],[-74.018272,40.659019],[-74.020467,40.67877],[-74.024827,40.687007],[-74.01849,40.695457],[-74.0168,40.701794],[-74.019526,40.706985],[-74.024543,40.709436],[-74.013784,40.756601],[-73.963182,40.8269],[-73.953982,40.848],[-73.929006,40.889578],[-73.896479,40.981697],[-73.893979,40.997197],[-73.90501,40.997591],[-74.18239,41.121595],[-74.301994,41.172594],[-74.457584,41.248225],[-74.696398,41.357339],[-74.689767,41.361558],[-74.691129,41.367324],[-74.708458,41.378901],[-74.715979,41.392584],[-74.73364,41.396975],[-74.740963,41.40512],[-74.741086,41.411413],[-74.734731,41.422699],[-74.738455,41.430641],[-74.743821,41.430635],[-74.758587,41.423287],[-74.773239,41.426352],[-74.790417,41.42166],[-74.795396,41.42398],[-74.801225,41.4381],[-74.807582,41.442847],[-74.817995,41.440505],[-74.826031,41.431736],[-74.830671,41.430503],[-74.836915,41.431625],[-74.858578,41.444427],[-74.888691,41.438259],[-74.893913,41.43893],[-74.896399,41.442179],[-74.889075,41.451245],[-74.890358,41.455324],[-74.906887,41.461131],[-74.909181,41.472436],[-74.912517,41.475605],[-74.924092,41.477138],[-74.932585,41.482323],[-74.941798,41.483542],[-74.95826,41.476396],[-74.983341,41.480894],[-74.985595,41.485863],[-74.982168,41.498486],[-74.984372,41.506611],[-74.987645,41.508738],[-75.003151,41.508101],[-75.000911,41.519292],[-75.00385,41.524052],[-75.014919,41.531399],[-75.024206,41.534018],[-75.024798,41.539801],[-75.016144,41.544246],[-75.018524,41.551802],[-75.027343,41.563541],[-75.04049,41.569688],[-75.04676,41.583258],[-75.060012,41.590813],[-75.074613,41.605711],[-75.071667,41.609501],[-75.059725,41.610801],[-75.061675,41.615468],[-75.060098,41.617482],[-75.05385,41.618655],[-75.048385,41.615986],[-75.044224,41.617978],[-75.043562,41.62364],[-75.048658,41.633781],[-75.04992,41.662556],[-75.059332,41.67232],[-75.051285,41.679961],[-75.052736,41.688393],[-75.059829,41.699716],[-75.06883,41.708161],[-75.06663,41.712588],[-75.052226,41.711396],[-75.049862,41.713309],[-75.054818,41.735168],[-75.053431,41.752538],[-75.060759,41.764638],[-75.075942,41.771518],[-75.095451,41.768366],[-75.10099,41.769121],[-75.10464,41.774203],[-75.101463,41.787941],[-75.092876,41.796386],[-75.076889,41.798509],[-75.072168,41.808327],[-75.072172,41.813732],[-75.078063,41.815112],[-75.089484,41.811576],[-75.100024,41.818347],[-75.113334,41.822782],[-75.115147,41.827285],[-75.113369,41.840698],[-75.115598,41.844638],[-75.130983,41.845145],[-75.140241,41.852078],[-75.152898,41.848564],[-75.161541,41.849836],[-75.168733,41.859258],[-75.168053,41.867043],[-75.170565,41.871608],[-75.176633,41.872371],[-75.185254,41.85993],[-75.194382,41.867287],[-75.204002,41.869867],[-75.21497,41.867449],[-75.223734,41.857456],[-75.231612,41.859459],[-75.241134,41.867118],[-75.251197,41.86204],[-75.260527,41.8638],[-75.263815,41.870757],[-75.257564,41.877108],[-75.260623,41.883783],[-75.271292,41.88736],[-75.272778,41.897112],[-75.267773,41.901971],[-75.267562,41.907054],[-75.276552,41.922208],[-75.279094,41.938917],[-75.289383,41.942891],[-75.293713,41.954593],[-75.300409,41.953871],[-75.301233,41.9489],[-75.303966,41.948216],[-75.312817,41.950182],[-75.318168,41.954236],[-75.32004,41.960867],[-75.329318,41.968232],[-75.342204,41.972872],[-75.337602,41.9867],[-75.341125,41.992772],[-75.359579,41.999445],[-76.343722,41.998346],[-76.920784,42.001774],[-77.124693,41.999395],[-77.83203,41.998524],[-78.12473,42.000452],[-78.874759,41.997559],[-79.761374,41.999067],[-79.761951,42.26986],[-79.717825,42.284711],[-79.645358,42.315631],[-79.546262,42.363417],[-79.474794,42.404291],[-79.453533,42.411157],[-79.429119,42.42838],[-79.405458,42.453281],[-79.381943,42.466491],[-79.351989,42.48892],[-79.331483,42.489076],[-79.31774,42.499884],[-79.283364,42.511228],[-79.264624,42.523159],[-79.242889,42.531757],[-79.193232,42.545881],[-79.148723,42.553672],[-79.138569,42.564462],[-79.12963,42.589824],[-79.121921,42.594234],[-79.113713,42.605994],[-79.111361,42.613358],[-79.078761,42.640058],[-79.073261,42.639958],[-79.06376,42.644758],[-79.062261,42.668358],[-79.04886,42.689158],[-79.01886,42.701558],[-78.991159,42.705358],[-78.944158,42.731958],[-78.918157,42.737258],[-78.868556,42.770258],[-78.853455,42.783958],[-78.851355,42.791758],[-78.856456,42.800258],[-78.859356,42.800658],[-78.863656,42.813058],[-78.865656,42.826758],[-78.860445,42.83511],[-78.859456,42.841358],[-78.865592,42.852358],[-78.872227,42.853306],[-78.882557,42.867258],[-78.891655,42.884845],[-78.912458,42.886557],[-78.905758,42.899957],[-78.905659,42.923357],[-78.909159,42.933257],[-78.918859,42.946857],[-78.93236,42.955857],[-78.961761,42.957756],[-78.975062,42.968756],[-79.011563,42.985256],[-79.019964,42.994756],[-79.02092,43.014287],[-79.011764,43.028956],[-79.005164,43.047056],[-79.00545,43.057231],[-79.01053,43.064389],[-79.074467,43.077855],[-79.074678,43.083141],[-79.064754,43.093205],[-79.060281,43.105086],[-79.062518,43.120182],[-79.060206,43.124799],[-79.044066,43.138055],[-79.042366,43.143655],[-79.046567,43.162355],[-79.053067,43.173655],[-79.050744,43.197417],[-79.055868,43.238554],[-79.061388,43.251349],[-79.070469,43.262454],[-79.019848,43.273686],[-78.971866,43.281254],[-78.836261,43.318455],[-78.777759,43.327055],[-78.747158,43.334555],[-78.696856,43.341255],[-78.634346,43.357624],[-78.547395,43.369541],[-78.488857,43.374763],[-78.473099,43.370812],[-78.370221,43.376505],[-78.358711,43.373988],[-78.233609,43.36907],[-78.145195,43.37551],[-78.104509,43.375628],[-78.023609,43.366575],[-77.995591,43.365293],[-77.976438,43.369159],[-77.965238,43.368059],[-77.922736,43.35696],[-77.904836,43.35696],[-77.875335,43.34966],[-77.797381,43.339857],[-77.760231,43.341161],[-77.756931,43.337361],[-77.714129,43.323561],[-77.701429,43.308261],[-77.660359,43.282998],[-77.628315,43.271303],[-77.577223,43.243263],[-77.551022,43.235763],[-77.534184,43.234569],[-77.50092,43.250363],[-77.476642,43.254522],[-77.436831,43.265701],[-77.414516,43.269263],[-77.391015,43.276363],[-77.341092,43.280661],[-77.314619,43.28103],[-77.303979,43.27815],[-77.264177,43.277363],[-77.214058,43.284114],[-77.173088,43.281509],[-77.143416,43.287561],[-77.130429,43.285635],[-77.111866,43.287945],[-77.067295,43.280937],[-77.033875,43.271218],[-76.999691,43.271456],[-76.988445,43.2745],[-76.958402,43.270005],[-76.952174,43.270692],[-76.904288,43.291816],[-76.877397,43.292926],[-76.854976,43.298443],[-76.841675,43.305399],[-76.794708,43.309632],[-76.769025,43.318452],[-76.731039,43.343421],[-76.69836,43.344436],[-76.684856,43.352691],[-76.669624,43.366526],[-76.630774,43.413356],[-76.607093,43.423374],[-76.562826,43.448537],[-76.53181,43.460299],[-76.521999,43.468617],[-76.515882,43.471136],[-76.506858,43.469127],[-76.486962,43.47535],[-76.472498,43.492781],[-76.437473,43.509213],[-76.417581,43.521285],[-76.368849,43.525822],[-76.345492,43.513437],[-76.297103,43.51287],[-76.259858,43.524728],[-76.235834,43.529256],[-76.228701,43.532987],[-76.217958,43.545156],[-76.209853,43.560136],[-76.203473,43.574978],[-76.199138,43.600454],[-76.196596,43.649761],[-76.205436,43.718751],[-76.213205,43.753513],[-76.229268,43.804135],[-76.250135,43.825713],[-76.266977,43.838046],[-76.283307,43.843923],[-76.284481,43.850968],[-76.28272,43.858601],[-76.261584,43.873278],[-76.243384,43.877975],[-76.227485,43.875061],[-76.219313,43.86682],[-76.202257,43.864898],[-76.158249,43.887542],[-76.145506,43.888681],[-76.133267,43.892975],[-76.127285,43.897889],[-76.125023,43.912773],[-76.133697,43.940356],[-76.134296,43.954726],[-76.139086,43.962111],[-76.146072,43.964705],[-76.169802,43.962202],[-76.184874,43.971128],[-76.22805,43.982737],[-76.244439,43.975803],[-76.264294,43.978009],[-76.268706,43.980846],[-76.266733,43.995578],[-76.269672,44.001148],[-76.281928,44.009177],[-76.296755,44.013307],[-76.298962,44.017719],[-76.300222,44.022762],[-76.296986,44.045455],[-76.300532,44.057188],[-76.360306,44.070907],[-76.360798,44.087644],[-76.366972,44.100409],[-76.363835,44.111696],[-76.355679,44.133258],[-76.312647,44.199044],[-76.286547,44.203773],[-76.245487,44.203669],[-76.206777,44.214543],[-76.191328,44.221244],[-76.164265,44.239603],[-76.161833,44.280777],[-76.130884,44.296635],[-76.118136,44.29485],[-76.111931,44.298031],[-76.097351,44.299547],[-76.045228,44.331724],[-76.000998,44.347534],[-75.978281,44.34688],[-75.970185,44.342835],[-75.94954,44.349129],[-75.929465,44.359603],[-75.922247,44.36568],[-75.912985,44.368084],[-75.871496,44.394839],[-75.82083,44.432244],[-75.807778,44.471644],[-75.76623,44.515851],[-75.662381,44.591934],[-75.618364,44.619637],[-75.505903,44.705081],[-75.477642,44.720224],[-75.423943,44.756329],[-75.413885,44.76889],[-75.397007,44.773471],[-75.387371,44.78003],[-75.372347,44.78311],[-75.346527,44.805563],[-75.333744,44.806378],[-75.306487,44.826144],[-75.30763,44.836813],[-75.26825,44.855119],[-75.255517,44.857651],[-75.241303,44.866958],[-75.228635,44.8679],[-75.218548,44.87554],[-75.203012,44.877548],[-75.142958,44.900237],[-75.133977,44.911838],[-75.105162,44.921193],[-75.096659,44.927067],[-75.066245,44.930174],[-75.059966,44.93457],[-75.027125,44.946568],[-75.005155,44.958402],[-74.999655,44.965921],[-74.99927,44.971638],[-74.992756,44.977449],[-74.972463,44.983402],[-74.907956,44.983359],[-74.900733,44.992754],[-74.887837,45.000046],[-74.861927,45.002771],[-74.834669,45.014683],[-74.826578,45.01585],[-74.799434,45.009132],[-74.793148,45.004647],[-74.768749,45.003893],[-74.760215,44.994946],[-74.74464,44.990577],[-74.731301,44.990422],[-74.722574,44.998062],[-74.702018,45.003322],[-74.683973,44.99969],[-74.667338,45.001648],[-74.661478,44.999592],[-74.45753,44.997032],[-74.335184,44.991905],[-74.146814,44.9915],[-74.027392,44.995765]]]]},\"properties\":{\"name\":\"New York\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0e31","contributors":{"authors":[{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":254931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Archer, R.J.","contributorId":55069,"corporation":false,"usgs":true,"family":"Archer","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":254933,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burke, P. M.","contributorId":8478,"corporation":false,"usgs":true,"family":"Burke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":254932,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dalton, F.N.","contributorId":58283,"corporation":false,"usgs":true,"family":"Dalton","given":"F.N.","email":"","affiliations":[],"preferred":false,"id":254934,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":30297,"text":"wri844180 - 1984 - Quality of water in the alluvial aquifer, American Bottoms, East St. Louis, Illinois","interactions":[],"lastModifiedDate":"2022-02-07T21:25:16.629118","indexId":"wri844180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4180","title":"Quality of water in the alluvial aquifer, American Bottoms, East St. Louis, Illinois","docAbstract":"<p>Ground-water levels in the American Bottoms regions around East St. Louis, Illinois, have risen several feet since the early 1970's. Artificial dewatering of the aquifer by increased pumping is being investigated by the U.S. Army Corps of Engineers to alleviate economic and health concerns resulting from elevated ground-water levels. A ground-water quality evaluation is necessary for selecting a feasible dewatering scheme. Analyses of water samples from 63 wells show that except for iron, manganese, and dissolved solids, constituent concentrations do not exceed Illinois water-quality standards. The waters are primarily of the calcium-magnesium-bicarbonate type with some calcium-sulfate type water. Iron concentrations ranged from less than 3 to 82,000 micrograms per liter, manganese from 5 to 5,300 micrograms per liter, and dissolved solids from 140 to 3,000 milligrams per liter. These constituent concentrations exceed Illinois ' public water supply, effluent, and general water-quality standards in most samples and analysis indicates the concentrations are representative of the ambient water quality. Concentrations of nitrite + nitrate nitrogen fluoride, zinc, lead, and sulfate also exceeded Illinois water-quality standards in a few samples. Concentrations of organic pesticides, polychlorinated biphenyls, and polychlorinated naphthalenes were below analytical detection limits.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844180","usgsCitation":"Voelker, D.C., 1984, Quality of water in the alluvial aquifer, American Bottoms, East St. Louis, Illinois: U.S. Geological Survey Water-Resources Investigations Report 84-4180, v, 51 p., https://doi.org/10.3133/wri844180.","productDescription":"v, 51 p.","costCenters":[],"links":[{"id":395572,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36048.htm"},{"id":159756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4180/report-thumb.jpg"},{"id":59086,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois","city":"East St. Louis","otherGeospatial":"American Bottoms","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.283,\n              38.5\n            ],\n            [\n              -89.967,\n              38.5\n            ],\n            [\n              -89.967,\n              38.917\n            ],\n            [\n              -90.283,\n              38.917\n            ],\n            [\n              -90.283,\n              38.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6515f7","contributors":{"authors":[{"text":"Voelker, David C. dvoelker@usgs.gov","contributorId":278,"corporation":false,"usgs":true,"family":"Voelker","given":"David","email":"dvoelker@usgs.gov","middleInitial":"C.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28212,"text":"wri844200 - 1984 - Sediment yields in eastern Montana; summary of data and proposed techniques for estimating sediment yields from small, ungaged watersheds","interactions":[],"lastModifiedDate":"2021-11-22T21:47:23.420128","indexId":"wri844200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4200","title":"Sediment yields in eastern Montana; summary of data and proposed techniques for estimating sediment yields from small, ungaged watersheds","docAbstract":"Sediment-yield data for 121 sites in eastern Montana have been compiled from results of studies conducted by various Federal, State, and private agencies. Methods used to determine mean annual sediment yields included reservoir sedimentation surveys, suspended-sediment sampling in streams, and estimates of gross erosion and indirect estimation based on physical characteristics of the basin. Multiple-regression equations were developed and evaluated for their adequacy in estimating mean annual sediment yields from small, ungaged watersheds in eastern Montana. Sediment yields determined from reservoir surveys were used as the dependent variable because they were considered the most representative of long-term yields. Independent variables consisted of basin characteristics which could be measured from maps or obtained from published sources. Consequently, equations developed in this study do not require onsite data. Evaluation of equations indicated that the best prediction capability was obtained when reservoir basins were segregated into classes of similar vegetation/soil complex. The predictive capability of regression equations developed for each of three classes of vegetation/soil complex, as indicated by the coefficient of determination (R2), ranged from 0.59 to 0.96. Corresponding standard errors ranged from 95 to 20 percent. The equations are applicable for small drainage basins of 2 square miles or less within the study area. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844200","usgsCitation":"Lambing, J., 1984, Sediment yields in eastern Montana; summary of data and proposed techniques for estimating sediment yields from small, ungaged watersheds: U.S. Geological Survey Water-Resources Investigations Report 84-4200, iv, 45 p., https://doi.org/10.3133/wri844200.","productDescription":"iv, 45 p.","costCenters":[],"links":[{"id":392019,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36060.htm"},{"id":57046,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4200/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4200/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108,\n              45\n            ],\n            [\n              -104.054,\n              45\n            ],\n            [\n              -104.054,\n              48.197\n            ],\n            [\n              -108,\n              48.197\n            ],\n            [\n              -108,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbeea","contributors":{"authors":[{"text":"Lambing, J. H.","contributorId":100860,"corporation":false,"usgs":true,"family":"Lambing","given":"J. H.","affiliations":[],"preferred":false,"id":199405,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59359,"text":"mf1699 - 1984 - Map showing recomputed hypocenters of earthquakes in the eastern and central United States and adjacent Canada, 1925-1980","interactions":[],"lastModifiedDate":"2019-06-13T17:35:47","indexId":"mf1699","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1699","title":"Map showing recomputed hypocenters of earthquakes in the eastern and central United States and adjacent Canada, 1925-1980","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1699","usgsCitation":"Dewey, J.W., and Gordon, D., 1984, Map showing recomputed hypocenters of earthquakes in the eastern and central United States and adjacent Canada, 1925-1980: U.S. Geological Survey Miscellaneous Field Studies Map 1699, 1 Plate: 53.63 x 41.59 inches, https://doi.org/10.3133/mf1699.","productDescription":"1 Plate: 53.63 x 41.59 inches","costCenters":[],"links":[{"id":182742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1699/report-thumb.jpg"},{"id":364284,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1699/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108,27 ], [ -108,48 ], [ -66,48 ], [ -66,27 ], [ -108,27 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6602fa","contributors":{"authors":[{"text":"Dewey, J. W.","contributorId":31008,"corporation":false,"usgs":true,"family":"Dewey","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":261860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, D.W.","contributorId":104132,"corporation":false,"usgs":true,"family":"Gordon","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":261861,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27398,"text":"wri844114 - 1984 - Hydrogeology and effects of tailings basins on the hydrology of Sands Plain, Marquette County, Michigan","interactions":[],"lastModifiedDate":"2016-09-29T14:42:11","indexId":"wri844114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4114","title":"Hydrogeology and effects of tailings basins on the hydrology of Sands Plain, Marquette County, Michigan","docAbstract":"<p>Sands Plain, a 225-square mile area, is near the Marquette iron-mining district in Michigan's Upper Peninsula. Gribben Basin, a settling basin for disposal of waste rock particles from iron-ore concentration, is in the western part. Because Sands Plain is near iron-ore deposits, but not underlain by them, parts of the area are being considered as sites for additional tailings basins. </p><p>Glacial deposits, as much as 500 feet thick, comprise the principal aquifer. Most ground water flows through the glacial deposits and discharges in a series of nearly parallel tributaries to the Chocolay River which flows into Lake Superior. Ninety-five percent of the discharge of these streams is ground-water runoff. The aquifer is recharged by precipitation at an average rate of 15 inches per year and by streamflow losses from the upper reaches of Goose Lake Outlet at an average rate of 2 inches per year. </p><p>Precipitation collected at two sites had mean pH values of 4.0; rates of deposition of sulfate and total dissolved nitrogen were estimated to be 17.4 and 5.8 pounds per acre per year, respectively. Dissolved-solids concentrations in water from streams ranged from 82 to 143 milligrams per liter; sulfate ranged from 4.2 to 10 milligrams per liter. Calcium and bicarbonate were the principal dissolved substances. Highest dissolved-solids concentrations in water from wells in glacial deposits were found in a major buried valley east of Goose Lake Outlet. These concentrations ranged from 14 to 246 milligrams per liter; sulfate concentrations ranged from 0.9 to 53 milligrams per liter. Because of the high ground-water component of streamflow, mean concentrations of total nitrogen and trace metals in surface water do not differ significantly from mean concentrations in ground water. </p><p>A two-dimensional digital model of ground-water flow was used to simulate water levels and ground-water runoff under steady-state and transient conditions Predictive simulations with the steady-state model were made to determine the effects of continued operation of Gribben tailings basin and construction and operation of four hypothetical tailings basins. Operation of Gribben Basin has decreased the average rate of ground-water flow to Goose Lake Outlet by 0.9 to 1.6 cubic feet per second but has increased the average rate of groundwater flow to Warner Creek by about 0.2 cubic foot per second. Continued filling of the tailings basin to its design capacity is expected to cause a slight increase in leakage from the basin to Goose Lake Outlet.</p><p>Four hypothetical tailings basins, comprising a total of 11 square miles, were simulated by successively adding one more basin to the previous basin configuration. Net ground-water flow to streams was reduced by the simulated basins. The magnitude of these reductions depends on engineering decisions about the method of basin construction and a better understanding of the hydraulic properties of the materials used to seal the basin perimeters. The maximum total reduction in ground-water runoff due to construction and operation of 11 square miles of tailings basins is about 18 cubic feet per second compared to flow simulated by a steady-state simulation without tailings basins. If bottom sealing, rather than slurry wall construction, is used for one of the hypothetical basins, the total maximum reduction is 7.5 cubic feet per second. Under some assumed conditions, leakage from the tailings basins may slightly increase ground-water flow to Goose Lake Outlet and Warner Creek. The maximum probable leakage from all tailings basins is about 7 cubic feet per second; the minimum probable leakage is about 0.7 cubic foot per second.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri844114","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Grannemann, N., 1984, Hydrogeology and effects of tailings basins on the hydrology of Sands Plain, Marquette County, Michigan: U.S. Geological Survey Water-Resources Investigations Report 84-4114, Document: vi, 98 p.; Plate: 22.07 x 17.25 inches, https://doi.org/10.3133/wri844114.","productDescription":"Document: vi, 98 p.; Plate: 22.07 x 17.25 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":56258,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4114/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4114/report-thumb.jpg"},{"id":56257,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4114/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Marquette County","otherGeospatial":"Sands Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.625,\n              46.5\n            ],\n            [\n              -87.233333,\n              46.5\n            ],\n            [\n              -87.233333,\n              46.316667\n            ],\n            [\n              -87.466667,\n              46.316667\n            ],\n            [\n              -87.466667,\n              46.366667\n            ],\n            [\n              -87.516667,\n              46.391667\n            ],\n            [\n              -87.625,\n              46.391667\n            ],\n            [\n              -87.625,\n              46.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6277f2","contributors":{"authors":[{"text":"Grannemann, N.G.","contributorId":11221,"corporation":false,"usgs":true,"family":"Grannemann","given":"N.G.","affiliations":[],"preferred":false,"id":198048,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40338,"text":"ofr84587 - 1984 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":40338,"text":"ofr84587 - 1984 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"ofr84587","publicationYear":"1984","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":63495,"text":"gp969 - 1986 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"gp969","publicationYear":"1986","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"id":1}],"supersededBy":{"id":63495,"text":"gp969 - 1986 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"gp969","publicationYear":"1986","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"lastModifiedDate":"2024-01-22T21:06:48.839996","indexId":"ofr84587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-587","title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","docAbstract":"<p>This report is one in a series resulting from the U.S. Geological Survey's Snake River Plain RASA (Regional Aquifer System Analysis) study that began in October 1979.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84587","usgsCitation":"Whitehead, R., 1984, Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 84-587, Report: 1 p.; 1 Plate: 54.96 x 35.97 inches, https://doi.org/10.3133/ofr84587.","productDescription":"Report: 1 p.; 1 Plate: 54.96 x 35.97 inches","costCenters":[],"links":[{"id":424703,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0587/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424702,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0587/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135467,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0587/report-thumb.jpg"}],"scale":"500000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.79353516529073,\n              44.75814253835162\n            ],\n            [\n              -119.79353516529073,\n              42.00600446943071\n            ],\n            [\n              -111.1325958997702,\n              42.00600446943071\n            ],\n            [\n              -111.1325958997702,\n              44.75814253835162\n            ],\n            [\n              -119.79353516529073,\n              44.75814253835162\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9722","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":223291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25971,"text":"wri844194 - 1984 - Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota","interactions":[],"lastModifiedDate":"2018-02-14T15:41:55","indexId":"wri844194","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4194","title":"Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota","docAbstract":"<p>The investigation of the water resources of the Dickinson lignite area, an area of about 500 square miles, was undertaken to define the hydrologic system of the area and to project probable effects of coal mining on the system.</p><p>Aquifers occur in sandstone beds in: the Fox Hills Sandstone and the lower Hell Creek Formation of Cretaceous age, the upper Hell Creek Formation of Cretaceous age and the lower Ludlow Member of the Fort Union Formation of Tertiary age, and the upper Ludlow and lower Tongue River Members of the Fort Union Formation of Tertiary age. Aquifers also occur in the sandstone and lignite lenses in the upper Tongue River Member and the Sentinel Butte Member of the Fort Union Formation. </p><p>Depths to the Fox Hills-lower Hell Creek aquifer system range from about 1,300 to 1,710 feet. Well yields range from 18 to 100 gallons per minute. The water is soft and is a sodium bicarbonate type. Dissolvedsolids concentrations in samples collected from the aquifer system ranged from 1,230 to 1,690 milligrams per liter.</p><p>Depths to the upper Hell Creek-lower Ludlow aquifer system range from about 720 to 1,040 feet. Well yields generally are less than 30 gallons per minute but may be as much as 150 gallons per minute. The water is soft and a sodium bicarbonate type. Dissolved-solids concentrations in samples collected from the aquifer system ranged from 1,010 to 1,450 milligrams per liter.</p><p>Depths to the upper Ludlow-lower Tongue River aquifer system range from about 440 to 713 feet. Well yields may range from about 1 to 100 gallons per minute. The water generally is soft and a sodium bicarbonate type but may be moderately hard and a sulfate type in the southwestern part of the area. Dissolved-solids concentrations in samples collected from the aquifer system ranged from 995 to 1,990 milligrams per liter. </p><p>Depths to the upper Tongue River-Sentinel Butte aquifer system range from near land surface to about 530 feet below land surface. Well yields generally range from about 1 to 185 gallons per minute. Yields from the lignite parts of the system range from about 2 to 60 gallons per minute. The water generally is a sodium bicarbonate type, but locally sulfate is the dominant anion. Dissolved-solids concentrations in samples collected from the aquifer system generally ranged from 574 to 2,720 milligrams per liter.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844194","usgsCitation":"Armstrong, C.A., 1984, Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 84-4194, Report: v, 35 p.; Plate: 22.55 x 19.31 inches, https://doi.org/10.3133/wri844194.","productDescription":"Report: v, 35 p.; Plate: 22.55 x 19.31 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":123870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4194/report-thumb.jpg"},{"id":54717,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4194/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54718,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4194/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","county":"Hettinger County, Stark County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa3b1","contributors":{"authors":[{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58829,"text":"mf1712 - 1984 - Estimated maximum regional seismic intensities associated with an ensemble of great earthquakes that might occur along the New Madrid seismic zone, east-central United States","interactions":[],"lastModifiedDate":"2019-06-13T17:34:38","indexId":"mf1712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1712","title":"Estimated maximum regional seismic intensities associated with an ensemble of great earthquakes that might occur along the New Madrid seismic zone, east-central United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1712","usgsCitation":"Algermissen, S.T., and Hopper, M.G., 1984, Estimated maximum regional seismic intensities associated with an ensemble of great earthquakes that might occur along the New Madrid seismic zone, east-central United States: U.S. Geological Survey Miscellaneous Field Studies Map 1712, 1 Plate: 28.71 x 23.19 inches, https://doi.org/10.3133/mf1712.","productDescription":"1 Plate: 28.71 x 23.19 inches","costCenters":[],"links":[{"id":364288,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1712/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1712/report-thumb.jpg"}],"scale":"7400000","country":"United States","otherGeospatial":"New Madrid seismic zone","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95,30 ], [ -95,45 ], [ -80,45 ], [ -80,30 ], [ -95,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a12a","contributors":{"authors":[{"text":"Algermissen, S. T.","contributorId":39790,"corporation":false,"usgs":true,"family":"Algermissen","given":"S.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":260918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hopper, M. G.","contributorId":39389,"corporation":false,"usgs":true,"family":"Hopper","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":260917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4261,"text":"cir927 - 1984 - The Conterminous United States Mineral Appraisal Program; background information to accompany folio of geologic, geochemical, geophysical, and mineral resources maps of the Walker Lake 1 degree x 2 degrees Quadrangle, California and Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:44","indexId":"cir927","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"927","title":"The Conterminous United States Mineral Appraisal Program; background information to accompany folio of geologic, geochemical, geophysical, and mineral resources maps of the Walker Lake 1 degree x 2 degrees Quadrangle, California and Nevada","docAbstract":"The Walker Lake 1? by 2? quadrangle in eastern California and western Nevada was studied by an interdisciplinary research team to appraise its mineral resources. The appraisal is based on geological, geochemical, and geophysical field and laboratory investigations, the results of which are published as a folio of maps, figures, and tables, with accompanying discussions. This circular provides background information on the investigations and integrates the information presented in the folio. The selected bibliography lists selected references to the geology, geochemistry, geophysics, and mineral deposits of the Walker Lake 1? by 2? quadrangle.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir927","usgsCitation":"Stewart, J.H., Chaffee, M., Dohrenwend, J.C., John, D., Kistler, R.W., Kleinhampl, F.J., Menzie, W., Plouff, D., Rowan, L.C., and Silberling, N.J., 1984, The Conterminous United States Mineral Appraisal Program; background information to accompany folio of geologic, geochemical, geophysical, and mineral resources maps of the Walker Lake 1 degree x 2 degrees Quadrangle, California and Nevada: U.S. Geological Survey Circular 927, iii, 22 p. :ill., map ; 26 cm., https://doi.org/10.3133/cir927.","productDescription":"iii, 22 p. :ill., map ; 26 cm.","costCenters":[],"links":[{"id":124870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0927/report-thumb.jpg"},{"id":31373,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0927/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ecac","contributors":{"authors":[{"text":"Stewart, John Harris","contributorId":63790,"corporation":false,"usgs":true,"family":"Stewart","given":"John","email":"","middleInitial":"Harris","affiliations":[],"preferred":false,"id":148599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chaffee, M.A.","contributorId":108049,"corporation":false,"usgs":true,"family":"Chaffee","given":"M.A.","affiliations":[],"preferred":false,"id":148603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dohrenwend, J. C.","contributorId":40960,"corporation":false,"usgs":true,"family":"Dohrenwend","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":148596,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"John, D. A.","contributorId":43748,"corporation":false,"usgs":true,"family":"John","given":"D. A.","affiliations":[],"preferred":false,"id":148597,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kistler, R. W.","contributorId":36112,"corporation":false,"usgs":true,"family":"Kistler","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148594,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kleinhampl, F. J.","contributorId":64650,"corporation":false,"usgs":true,"family":"Kleinhampl","given":"F.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":148600,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Menzie, W. D.","contributorId":52916,"corporation":false,"usgs":true,"family":"Menzie","given":"W. D.","affiliations":[],"preferred":false,"id":148598,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":148601,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rowan, L. C.","contributorId":40584,"corporation":false,"usgs":true,"family":"Rowan","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":148595,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Silberling, Norman J.","contributorId":102438,"corporation":false,"usgs":true,"family":"Silberling","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":148602,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":30317,"text":"wri844267 - 1984 - Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983","interactions":[],"lastModifiedDate":"2022-01-10T20:59:45.500688","indexId":"wri844267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4267","title":"Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983","docAbstract":"<p>Yucca Mountain, Nevada, is one of several sites under consideration for construction of the first repository for high-level nuclear waste. The climate is arid; few perennial streams are present in the region. Flash floods occasionally occur. The site is underlain by at least 1,800 meters of volcanic tuffs of Tertiary age; limestones and dolomites of Paleozoic age underlie much of the surrounding region, and, together with alluvial deposits, comprise the major aquifers. Yucca Mountain is in the Alkali Flat-Furnace Creek Ranch ground-water subbasin, which is part of the Death Valley ground-water basin. Discharge occurs at Alkali Flat almost entirely by evapotranspiration, and at Furnace Creek Ranch from small springs and seeps. Beneath Yucca Mountain, depth to water ranges from about 460 to 700 meters; the rock under consideration for construction of the repository is in the unsaturated zone. Rate of recharge at Yucca Mountain is small, perhaps much less than 5 millimeters per year. Within the saturated zone, water movement is principally along fractures. The hydraulic gradient is small east (downgradient) of Yucca Mountain, and increases to the north and west. Lack of effective-porosity data presently precludes accurate calculation of flow velocity and travel times.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844267","usgsCitation":"Waddell, R.K., Robison, J.H., and Blankennagel, R., 1984, Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983: U.S. Geological Survey Water-Resources Investigations Report 84-4267, vi, 72 p., https://doi.org/10.3133/wri844267.","productDescription":"vi, 72 p.","costCenters":[],"links":[{"id":394133,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36112.htm"},{"id":59109,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4267/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4267/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Yucca Mountain and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118,\n              35.833\n            ],\n            [\n              -114.5670,\n              35.833\n            ],\n            [\n              -114.5670,\n              38.466\n            ],\n            [\n              -118,\n              38.466\n            ],\n            [\n              -118,\n              35.833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604816","contributors":{"authors":[{"text":"Waddell, R. K.","contributorId":25560,"corporation":false,"usgs":true,"family":"Waddell","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":203045,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robison, J. H.","contributorId":60183,"corporation":false,"usgs":true,"family":"Robison","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":203046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blankennagel, R. K.","contributorId":65078,"corporation":false,"usgs":true,"family":"Blankennagel","given":"R. K.","affiliations":[],"preferred":false,"id":203047,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26366,"text":"wri834190 - 1984 - Impact of development on availability and quality of ground water in eastern Nassau County, Florida, and southeastern Camden County, Georgia","interactions":[],"lastModifiedDate":"2017-01-24T09:27:23","indexId":"wri834190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4190","title":"Impact of development on availability and quality of ground water in eastern Nassau County, Florida, and southeastern Camden County, Georgia","docAbstract":"The primary sources of water in the area are from the surficial and Floridan aquifers. The surficial aquifer, consisting of thin permeable zones of sand, shell, and limestone, provides limited water supplies (10-50 gallons per minute). Its estimated transmissivity ranges from less than 100 to 10,000 feet squared per day. Its water is generally of acceptable quality for most uses, except near the coast. The Floridan aquifer consists of three zones of permeable limestone and dolomite separated by semiconfining beds of hard, massive dolomite and limestone, all of which are confined by leaky confining beds. The upper and middle zones, about 530-1,000 feet and 1,200-1,700 feet below land surface, respectively, have transmissivities ranging from 20,000-50,000 and 40,000-60,000 feet squared per day, respectively. The lower zone, about 2,000-2,100 feet below land surface contains very saline water. Water in the upper zone contains chloride concentrations generally ranging from 20-40 milligrams per liter. In Fernandina Beach, water from a few wells tapping this zone has relatively high chloride concentrations (190 milligrams per liter), probably due to upward migration of saline water from deeper zones through uncased or improperly-plugged well bores and not by lateral intrusion. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834190","usgsCitation":"Brown, D., 1984, Impact of development on availability and quality of ground water in eastern Nassau County, Florida, and southeastern Camden County, Georgia: U.S. Geological Survey Water-Resources Investigations Report 83-4190, vi, 133 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834190.","productDescription":"vi, 133 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":122964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4190/report-thumb.jpg"},{"id":55160,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4190/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida, Georgia","county":"Camden County, Nassau County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.4853515625,\n              29.964452850852005\n            ],\n            [\n              -82.4853515625,\n              31.942839972853083\n            ],\n            [\n              -81.024169921875,\n              31.942839972853083\n            ],\n            [\n              -81.024169921875,\n              29.964452850852005\n            ],\n            [\n              -82.4853515625,\n              29.964452850852005\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6f9f","contributors":{"authors":[{"text":"Brown, D.P.","contributorId":95881,"corporation":false,"usgs":true,"family":"Brown","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":196265,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38513,"text":"pp1342 - 1984 - The evolution of the southern California uplift, 1955 through 1976","interactions":[],"lastModifiedDate":"2017-04-25T15:11:50","indexId":"pp1342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1342","title":"The evolution of the southern California uplift, 1955 through 1976","docAbstract":"<p>The southern California uplift culminated in 1974 as a 150- km-wide crustal swell that extended about 600 km eastward and east-southeastward from Point Arguello to the Colorado River and Salton Sea, respectively; it was characterized by remarkably uniform height changes between 1959 and 1974 of 0.30-0.35 m over at least half of its 60,000-70,000 km<sup>2</sup> area. At its zenith, the uplift included virtually the entire Transverse Ranges geologic province and parts of the Coast Ranges, San Joaquin Valley, Sierra Nevada, Basin and Range, Mojave Desert, Peninsular Ranges, and Salton Trough provinces. The alinement of the western part of the uplift closely paralleled the east-trending Transverse Ranges, whereas the southern flank of the eastern lobe roughly coincided with the west-northwest-trending San Andreas fault. The position and configuration of the uplift associate it with a singularly complex section of the boundary between the North American and Pacific plates that has certainly sustained major modification during the past 5 million years and probably during the past 1 million years. </p><p>Surface deformation can be categorized as tectonic or nontectonic. Nontectonic vertical displacements associated with the activities of man have overwhelmed natural compaction and areally significant soil expansion in the southern California area. Because tectonic displacements are implicitly defined as those that cannot be otherwise explained, those vertical movements that can be reasonably attributed to artificial processes have been subtracted from our reconstructed configurations of the uplift. Hence this reconstruction has necessarily included the assembly and evaluation of an enormous volume of data on oil-field operations, changes in ground-water levels, and measured subsidence (or rebound) associated with changes in the underground fluid regimen. </p><p>Measured changes in height at various stages in the evolution of the uplift have been based chiefly on first-order levelings carried out between 1953 and 1976. Exceptions to this generalization consist largely of the results of pre-1953 surveys through the western Transverse Ranges and the eastern Mojave Desert. Errors in measured height differences derive from blunders, systematic survey errors, random survey errors, improperly formulated orthometric corrections, and intrasurvey movement; the last of these has created the most serious problems encountered in our reconstruction of the basic data. A variety of independent tests indicate that survey error associated with the utilized levelings was generally small and fell largely within the predicted random-error range. Moreover, the redundancy and coherence displayed by the entire data set provide convincing evidence of survey accuracy and the virtual absence of height- and slope-dependent error in particular. </p><p>Our reconstructions of the changing configuration of the uplift derive chiefly from comparisons among sequentially developed observed elevations along the same route. Most of the observed elevations from which the vertical displacements were computed have been reconstructed with respect to bench mark Tidal 8, San Pedro, as invariant in height. Because the San Pedro tide station has been characterized by a history of modest relative uplift, vertical displacements referred to this station are biased slightly toward the appearance of subsidence. Where the observed elevations cannot be conveniently tied to Tidal 8, they have been referred to secondary control points whose history with respect to Tidal 8 can be independently established. Each of the lines of observed elevation changes provides, accordingly, a section athwart or along the axis of the uplift from which the changes in the configuration of the uplift can be roughly generalized. Because relatively few surveys were run in 1955, which we choose as a representative temporal datum, we have commonly incorporated the results of earlier or of somewhat later levelings as the equivalents of 1955 surveys. Although this procedure introduces a certain subjectivity, the probable equivalence between the results of these earlier or later surveys with those that would have been obtained had this leveling been carried out in 1955, usually can be independently tested. Wherever the calculated vertical displacements are based on comparisons between the results of levelings over different routes, the observed elevations have been orthometrically corrected to agree with those that would have been produced had each of these surveys been along the same route. </p><p>The growth of the southern California uplift consisted of two well-defined spasms of positive movement, the second of which was closely followed by partial collapse. Our reconstruction, although it clearly errs in detail, indicates that the uplift, together with marginal and apparently ephemeral tectonic subsidence, nucleated in the west-central Transverse Ranges near Ozena, sometime between the spring of 1959 and the spring of 1960. The uplift expanded rapidly eastward (and probably westward as well), and by the fall of 1961 much of the Transverse Ranges and the Mojave Desert at least as far east as Twentynine Palms had risen by as much as 0.25 m. Between 1962 and 1972 the area included by the initially developed (1959-61) uplift sustained additional but clearly decelerating uplift accompanied locally by oscillatory displacements. Between 1972/ 73 and 1974 a second crustal spasm extended the uplift eastward to the Colorado River and elevated much of the eastern Mojave Desert by values that equaled or exceeded those developed within the western lobe. Between 1974 and 1976, at least the central part of the uplift sustained partial collapse that nowhere amounted to less than 50 percent of the cumulative uplift since 1959. Whether this collapse affected the entire uplift is conjectural, but we now recognize well-defined evidence of major down-to-the-north tilting that must have occurred within the eastern part of the uplift at some time between 1974 and 1976. </p><p>Accumulating evidence indicates that nearly all the area included with the southern California uplift underwent similar uplift and partial collapse during the early part of the 20th century. Thus we infer that the recent uplift represents but a single event in an ongoing, more or less cyclic deformational process characterized by a period of about 50 years. Even though less than two full cycles are expressed in the geodetic&nbsp;record, the cumulative rate of uplift near the center of the recent uplift probably has averaged about 5 mm/yr, a value that is roughly consistent with the uplift rates that have been deduced for the late Quaternary emergent marine terraces along the south flank of the Transverse Ranges. </p><p>Although the evolution of the recent uplift is relatively well defined, its correlation with the regional seismicity is poorly defined. A comparison between the occurrence of southern California earthquakes of magnitude ≥4 during the period 1932 to 1976 with the 1974 configuration of the uplift demonstrates the existence of (1) relatively aseismic areas within the western lobe of the uplift (in the western Transverse Ranges), in the central part of the uplift (in the western Mojave Desert), and along an east-trending zone that extends into the eastern Mojave athwart the south flank of the uplift (north of the Salton Sea) and (2) localized concentrations of seismic activity along the flanks of the uplift. Moreover, 9 of the 10 largest earthquakes recorded within or around the area of the southern California uplift during the period 1932 to 1976 (the 1933 Long Beach, the 1941 Santa Barbara, the 1946 Walker Pass, the 1947 Manix, the 1948 Desert Hot Springs, and the four major 1952 Kern County shocks) occurred before the inception of the uplift in 1959 or 1960. </p><p>The area embraced by the southern California uplift has been identified with geodetically defined horizontal strain, part of which may have accumulated as a major north-south contractional event that roughly coincided with the first spasm of uplift. Nonetheless, continuing contractional strain associated with regionally developed partial collapse argues that the uplift cannot be fully explained simply as the vertical expression of continuing north-south compression. Consideration of the two well-defined historical episodes of uplift and partial collapse indicate that the southern California uplift may be the product of decoupling and viscous flow beneath the seismogenic zone, presumably driven by continuing motion between the irregularly margined plates south of the great bend of the San Andreas fault. Because the magnitude of the maximum uplift associated with each episode was approximately the same, there may be some threshold value above which collapse (viscous flow) may ensue; the absence of total collapse may be a function of precollapse strain hardening within the postulated subseismogenic viscoelastic layer.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1342","usgsCitation":"Castle, R.O., Elliot, M.R., Church, J.P., and Wood, S.H., 1984, The evolution of the southern California uplift, 1955 through 1976: U.S. Geological Survey Professional Paper 1342, Report: vii, 136 p.; 16 Plates: 48 x 50.5 inches or less, https://doi.org/10.3133/pp1342.","productDescription":"Report: vii, 136 p.; 16 Plates: 48 x 50.5 inches or less","costCenters":[],"links":[{"id":65240,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-07.pdf","text":"Plate 7","size":"973.46 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 7"},{"id":65241,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-09.pdf","text":"Plate 9","size":"1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 9"},{"id":65242,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-10.pdf","text":"Plate 10","size":"1.28 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 10"},{"id":65239,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-06.pdf","text":"Plate 6","size":"915.38 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 6"},{"id":65243,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-11.pdf","text":"Plate 11","size":"1.22 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 11"},{"id":65244,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-12.pdf","text":"Plate 12","size":"1.2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 12"},{"id":119174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1342/report-thumb.jpg"},{"id":65245,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-13.pdf","text":"Plate 13","size":"1.22 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 13"},{"id":65247,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-15.pdf","text":"Plate 15","size":"1.41 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 15"},{"id":65248,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-16.pdf","text":"Plate 16","size":"2.63 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 16"},{"id":65246,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-14.pdf","text":"Plate 14","size":"751.57 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 14"},{"id":65249,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1342/report.pdf","text":"Report","size":"4.85 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":65235,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-01.pdf","text":"Plate 1","size":"3.66 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":65236,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-02.pdf","text":"Plate 2","size":"3.68 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":65237,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-03.pdf","text":"Plate 3","size":"4.53 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":65238,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-05.pdf","text":"Plate 5","size":"1.57 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 5"},{"id":104605,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4807.htm","linkFileType":{"id":5,"text":"html"},"description":"4807"},{"id":264148,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-08_b.pdf","text":"Plate 8B","size":"4.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 8B"},{"id":264147,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-08_a.pdf","text":"Plate 8A","size":"1.75 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 8A"},{"id":340353,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-04.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.6,\n              38\n            ],\n            [\n              -122.6,\n              37.75334401310656\n            ],\n            [\n              -122.6,\n              37.58811876638322\n            ],\n            [\n              -122.618408203125,\n              37.24782120155428\n            ],\n            [\n              -122.354736328125,\n              36.97622678464096\n            ],\n            [\n              -122.15698242187499,\n              36.86204269508728\n            ],\n            [\n              -121.9921875,\n              36.79169061907076\n            ],\n            [\n              -122.091064453125,\n              36.62434536776987\n            ],\n            [\n              -122.025146484375,\n              36.2354121683998\n            ],\n            [\n              -121.77246093750001,\n              36.05798104702501\n            ],\n            [\n              -121.56372070312499,\n              35.93354064249312\n            ],\n            [\n              -121.33300781249999,\n              35.6126508187567\n            ],\n            [\n              -121.014404296875,\n              35.37113502280101\n            ],\n            [\n              -120.84960937499999,\n              35.05698043137265\n            ],\n            [\n              -120.77270507812499,\n              34.77771580360469\n            ],\n            [\n              -120.728759765625,\n              34.52466147177172\n            ],\n            [\n              -120.59692382812499,\n              34.30714385628804\n            ],\n            [\n              -120.32226562500001,\n              34.298068350990825\n            ],\n            [\n              -119.827880859375,\n              34.30714385628804\n            ],\n            [\n              -119.5751953125,\n              34.279914398549934\n            ],\n            [\n              -119.300537109375,\n              34.05265942137599\n            ],\n            [\n              -119.00390625,\n              33.88865750124075\n            ],\n            [\n              -118.531494140625,\n              33.715201644740844\n            ],\n            [\n              -118.267822265625,\n              33.6420625047537\n            ],\n            [\n              -117.94921874999999,\n              33.55055114384406\n            ],\n            [\n              -117.71850585937501,\n              33.43144133557529\n            ],\n            [\n              -117.49877929687499,\n              33.22030778968541\n            ],\n            [\n              -117.32299804687499,\n              32.9257074887604\n            ],\n            [\n              -117.27630615234374,\n              32.66018807572586\n            ],\n            [\n              -117.12524414062501,\n              32.54681317351514\n            ],\n            [\n              -114.75219726562499,\n              32.722598604044066\n            ],\n            [\n              -114.55718994140625,\n              32.71797709835758\n            ],\n            [\n              -114.49951171875,\n              32.78265637602964\n            ],\n            [\n              -114.42260742187499,\n              32.90726224488304\n            ],\n            [\n              -114.47753906249999,\n              33.054716488042736\n            ],\n            [\n              -114.6533203125,\n              33.091541548655215\n            ],\n            [\n              -114.66705322265625,\n              33.22720064403191\n            ],\n            [\n              -114.66156005859376,\n              33.38787959704519\n            ],\n            [\n              -114.554443359375,\n              33.46810795527896\n            ],\n            [\n              -114.54345703125,\n              33.61461929233378\n            ],\n            [\n              -114.49951171875,\n              33.710632271492095\n            ],\n            [\n              -114.53247070312499,\n              33.80653802509606\n            ],\n            [\n              -114.521484375,\n              33.970697997361626\n            ],\n            [\n              -114.4171142578125,\n              34.016241889667015\n            ],\n            [\n              -114.34844970703125,\n              34.08906131584994\n            ],\n            [\n              -114.18090820312499,\n              34.19135773925218\n            ],\n            [\n              -114.114990234375,\n              34.24813554589752\n            ],\n            [\n              -114.136962890625,\n              34.352506668675936\n            ],\n            [\n              -114.312744140625,\n              34.43409789359469\n            ],\n            [\n              -114.43359375,\n              34.58799745550482\n            ],\n            [\n              -114.510498046875,\n              34.71452466170392\n            ],\n            [\n              -114.5654296875,\n              34.82282272723702\n            ],\n            [\n              -114.67529296874999,\n              34.912962495216966\n            ],\n            [\n              -114.63134765625001,\n              35.000753578642396\n            ],\n            [\n              -116.56768798828125,\n              36.52067329034796\n            ],\n            [\n              -118.5369873046875,\n              38\n            ],\n            [\n              -122.6,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dc34","contributors":{"authors":[{"text":"Castle, Robert O.","contributorId":22741,"corporation":false,"usgs":true,"family":"Castle","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":219969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliot, Michael R.","contributorId":189355,"corporation":false,"usgs":true,"family":"Elliot","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Church, Jack P.","contributorId":6480,"corporation":false,"usgs":true,"family":"Church","given":"Jack","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":219966,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wood, Spencer H. 0000-0002-5794-2619","orcid":"https://orcid.org/0000-0002-5794-2619","contributorId":16111,"corporation":false,"usgs":false,"family":"Wood","given":"Spencer","email":"","middleInitial":"H.","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":219968,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29841,"text":"wri844251 - 1984 - Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"wri844251","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4251","title":"Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York","docAbstract":"Aldicarb, a toxic oxime-carbamate pesticide that was believed incapable of reaching ground water, was used in potato-farming areas of eastern Suffolk County, New York during 1975-80. In 1979, aldicarb was found in substantial concentrations in ground water throughout the area. The New York State Department of Health set a limit of 7 micrograms per liter for aldicarb in drinking water. Extensive ground-water sampling into 1980 showed widespread contamination ranging from small amounts to as much as 515 micrograms per liter. In 1980, the U.S. Environmental Protection Agency banned the use of aldicarb on Long Island at the manufacturer 's request. A 1982 sampling study found aldicarb to have penetrated to about 40 feet below the water table in concentrations ranging from below detection limit to 239 micrograms per liter. Despite reputed toxicity, no instance of aldicarb poisoning on Long Island has been documented. The excessive aldicarb concentrations in the ground water of eastern Long Island may persist for decades; the duration has not been precisely determined and remains under investigation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844251","usgsCitation":"Soren, J., and Stelz, W., 1984, Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 84-4251, vi, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844251.","productDescription":"vi, 40 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4251/report-thumb.jpg"},{"id":58648,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4251/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4251/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688006","contributors":{"authors":[{"text":"Soren, Julian","contributorId":54184,"corporation":false,"usgs":true,"family":"Soren","given":"Julian","email":"","affiliations":[],"preferred":false,"id":202224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stelz, W. G.","contributorId":72837,"corporation":false,"usgs":true,"family":"Stelz","given":"W. G.","affiliations":[],"preferred":false,"id":202225,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}