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,{"id":49281,"text":"ofr90509A - 1990 - FASPU English and metric version computer file : analytic petroleum resource appraisal microcomputer programs for play analysis using a reservoir-engineering model, Part A - Documentation","interactions":[],"lastModifiedDate":"2012-02-02T00:11:18","indexId":"ofr90509A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-509","chapter":"A","title":"FASPU English and metric version computer file : analytic petroleum resource appraisal microcomputer programs for play analysis using a reservoir-engineering model, Part A - Documentation","language":"ENGLISH","doi":"10.3133/ofr90509A","usgsCitation":"Crovelli, R.A., and Balay, R.H., 1990, FASPU English and metric version computer file : analytic petroleum resource appraisal microcomputer programs for play analysis using a reservoir-engineering model, Part A - Documentation: U.S. Geological Survey Open-File Report 90-509, i, 23 leaves : forms ; 28 cm., https://doi.org/10.3133/ofr90509A.","productDescription":"i, 23 leaves : forms ; 28 cm.","costCenters":[],"links":[{"id":176044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0509a/report-thumb.jpg"},{"id":85986,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0509a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8978","contributors":{"authors":[{"text":"Crovelli, Robert A.","contributorId":92242,"corporation":false,"usgs":true,"family":"Crovelli","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":239429,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balay, Richard H.","contributorId":10048,"corporation":false,"usgs":true,"family":"Balay","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":239428,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":49307,"text":"ofr90610A - 1990 - Earthquake Data Report, October 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr90610A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-610","chapter":"A","title":"Earthquake Data Report, October 1990","language":"ENGLISH","doi":"10.3133/ofr90610A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, Earthquake Data Report, October 1990: U.S. Geological Survey Open-File Report 90-610, 307 p., https://doi.org/10.3133/ofr90610A.","productDescription":"307 p.","costCenters":[],"links":[{"id":176116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0610a/report-thumb.jpg"},{"id":85998,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0610a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62aca0","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531873,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":26711,"text":"wri904122 - 1990 - Hydrology and land use in Grand Traverse County, Michigan","interactions":[],"lastModifiedDate":"2016-09-16T10:33:48","indexId":"wri904122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4122","title":"Hydrology and land use in Grand Traverse County, Michigan","docAbstract":"<p>Glacial deposits are the sole source of ground-water supplies in Grand Traverse County. These deposits range in thickness from 100 to 900 feet and consist of till, outwash, and materials of lacustrine and eolian origin. In some areas, the deposits fill buried valleys that are 500 feet deep. Sedimentary rocks of Paleozoic age, which underlie the glacial deposits, are mostly shale and are not used for water supply. </p><p>Of the glacial deposits, outwash and lacustrine sand are the most productive aquifers. Most domestic wells obtain water from sand and gravel at depths ranging from 50 to 150 feet and yield at least 20 gallons per minute. Irrigation, municipal, and industrial wells capable of yielding 250 gallons per minute or more are generally greater than 150 feet deep. At places in the county where moranial deposits contain large amounts of interbedded silt and clay, wells are generally deeper and yields are much lower. </p><p>Areal variations in the chemical and physical characteristics of ground and surface water are related to land use and chemical inputs to the hydrologic system. Information on fertilizer application, septic-tank discharges, animal wastes, and precipitation indicate that 40 percent of nitrogen input is from precipitation, 6 percent from septic tanks, 14 percent from animal wastes, and 40 percent from fertilizers. </p><p>Streams and lakes generally have a calcium bicarbonate-type water. The dissolved-solids concentration of streams ranged from 116 to 380 milligrams per liter, and that of lakes, from 47 to 170 milligrams per liter. Water of streams is hard to very hard; water of lakes ranges from soft to hard. The maximum total nitrogen concentration found in streams was 4.4 milligrams per liter. Water of lakes have low nitrogen concentrations; the median nitrate concentration is less than 0.01 milligrams per liter. Pesticides (Parathion and Simazine) were detected in low concentrations at six stream sites; 2,4-D was detected in low concentrations in water of two lakes. Relationships between land use and the yield of dissolved and suspended substances could not be established for most stream basins. </p><p>Calcium and bicarbonate are the principal dissolved substances in ground water. Dissolved-solids concentrations ranged from 70 to 700 milligrams per liter; the countywide mean concentration is 230 milligrams per liter. The mean nitrate concentration is 1.3 milligrams per liter; about 1.6 percent of the county's ground water has nitrate concentrations that exceed the U.S. Environmental Protection Agency's maximum drinking water level of 10 milligrams per liter. An effect of fertilizer applications on ground-water quality is evident in some parts of the county.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri904122","collaboration":"Prepared in cooperation with Grand Traverse County and the Michigan Department of Natural Resources, Geological Survey Division","usgsCitation":"Cummings, T., Gillespie, J., and Grannemann, N., 1990, Hydrology and land use in Grand Traverse County, Michigan: U.S. Geological Survey Water-Resources Investigations Report 90-4122, Document: viii, 99 p.; 3 Plates: 26.93 x 38.31 inches or smaller, https://doi.org/10.3133/wri904122.","productDescription":"Document: viii, 99 p.; 3 Plates: 26.93 x 38.31 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":123237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4122/report-thumb.jpg"},{"id":55581,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4122/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55582,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4122/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55583,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4122/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55584,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Grand Traverse County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.3317,44.8158],[-85.3363,44.512],[-85.4567,44.5116],[-85.5804,44.5116],[-85.6956,44.5124],[-85.8205,44.5117],[-85.8184,44.5988],[-85.816,44.7744],[-85.6938,44.7738],[-85.6385,44.7729],[-85.6321,44.7679],[-85.6245,44.7665],[-85.6136,44.7641],[-85.6071,44.7663],[-85.5994,44.7658],[-85.5942,44.7676],[-85.5948,44.7713],[-85.5948,44.7736],[-85.5881,44.7941],[-85.5794,44.8159],[-85.5774,44.8191],[-85.5748,44.8209],[-85.5716,44.8227],[-85.5644,44.8322],[-85.5577,44.8477],[-85.5518,44.8591],[-85.5485,44.8627],[-85.5362,44.8717],[-85.5335,44.8781],[-85.5321,44.8845],[-85.5333,44.8886],[-85.5314,44.8909],[-85.5268,44.8931],[-85.5274,44.8986],[-85.5306,44.8991],[-85.5351,44.8991],[-85.5428,44.8992],[-85.5493,44.8988],[-85.5512,44.8974],[-85.5513,44.8956],[-85.5533,44.8924],[-85.5565,44.8888],[-85.5591,44.8883],[-85.5661,44.8929],[-85.5648,44.8984],[-85.5596,44.8993],[-85.5589,44.9011],[-85.5537,44.9061],[-85.5393,44.9197],[-85.5308,44.9292],[-85.53,44.9452],[-85.526,44.9497],[-85.5199,44.9707],[-85.5173,44.9743],[-85.5108,44.9765],[-85.5004,44.9801],[-85.4952,44.986],[-85.4874,44.9901],[-85.4803,44.9909],[-85.4745,44.99],[-85.4719,44.9881],[-85.4688,44.9794],[-85.4653,44.9593],[-85.4672,44.9584],[-85.4814,44.9608],[-85.4859,44.959],[-85.4879,44.9567],[-85.4873,44.9554],[-85.4867,44.949],[-85.4861,44.9439],[-85.4875,44.9398],[-85.4875,44.9389],[-85.4895,44.9339],[-85.4922,44.9285],[-85.4928,44.9262],[-85.4916,44.9207],[-85.4898,44.9166],[-85.4885,44.9143],[-85.4918,44.912],[-85.4925,44.9075],[-85.4906,44.902],[-85.49,44.8979],[-85.4934,44.8901],[-85.4941,44.8869],[-85.4929,44.8828],[-85.4935,44.8796],[-85.4988,44.8737],[-85.495,44.866],[-85.4977,44.8591],[-85.4984,44.8578],[-85.5082,44.8464],[-85.5296,44.8384],[-85.5569,44.8135],[-85.559,44.8062],[-85.5598,44.7925],[-85.5592,44.7866],[-85.5606,44.782],[-85.5697,44.7711],[-85.5698,44.7693],[-85.5737,44.7648],[-85.5744,44.762],[-85.5738,44.7575],[-85.5649,44.7528],[-85.5559,44.7514],[-85.5341,44.7476],[-85.5283,44.7498],[-85.5217,44.7584],[-85.5068,44.7688],[-85.5067,44.7716],[-85.5053,44.7812],[-85.5097,44.7857],[-85.5077,44.7907],[-85.5071,44.793],[-85.5024,44.8017],[-85.4966,44.8057],[-85.492,44.8084],[-85.4875,44.8102],[-85.4856,44.8107],[-85.4817,44.8138],[-85.4719,44.817],[-85.4615,44.8265],[-85.4587,44.8387],[-85.4528,44.8478],[-85.4501,44.8551],[-85.4443,44.8596],[-85.3831,44.8591],[-85.3787,44.8518],[-85.3763,44.844],[-85.3706,44.8353],[-85.3624,44.8284],[-85.3572,44.827],[-85.3489,44.8265],[-85.3387,44.8227],[-85.3317,44.8158]]]},\"properties\":{\"name\":\"Grand Traverse\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f70","contributors":{"authors":[{"text":"Cummings, T. 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,{"id":67189,"text":"i1901 - 1990 - Geologic map of the Richfield 1 degree by 2 degrees Quadrangle, west-central Utah","interactions":[{"subject":{"id":11335,"text":"ofr83583 - 1983 - Geology of the Richfield Quadrangle, west-central Utah","indexId":"ofr83583","publicationYear":"1983","noYear":false,"title":"Geology of the Richfield Quadrangle, west-central Utah"},"predicate":"SUPERSEDED_BY","object":{"id":67189,"text":"i1901 - 1990 - Geologic map of the Richfield 1 degree by 2 degrees Quadrangle, west-central Utah","indexId":"i1901","publicationYear":"1990","noYear":false,"title":"Geologic map of the Richfield 1 degree by 2 degrees Quadrangle, west-central Utah"},"id":1},{"subject":{"id":42506,"text":"ofr78602 - 1978 - Preliminary geologic map of the Richfield 1? by 2? Quadrangle, Utah","indexId":"ofr78602","publicationYear":"1978","noYear":false,"title":"Preliminary geologic map of the Richfield 1? by 2? Quadrangle, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":67189,"text":"i1901 - 1990 - Geologic map of the Richfield 1 degree by 2 degrees Quadrangle, west-central Utah","indexId":"i1901","publicationYear":"1990","noYear":false,"title":"Geologic map of the Richfield 1 degree by 2 degrees Quadrangle, west-central Utah"},"id":2}],"lastModifiedDate":"2012-02-10T00:11:20","indexId":"i1901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1901","subseriesTitle":"NONE","title":"Geologic map of the Richfield 1 degree by 2 degrees Quadrangle, west-central Utah","language":"ENGLISH","doi":"10.3133/i1901","usgsCitation":"Steven, T.A., Morris, H.T., and Rowley, P.D., 1990, Geologic map of the Richfield 1 degree by 2 degrees Quadrangle, west-central Utah: U.S. Geological Survey IMAP 1901, 3 maps on 1 sheet :col. ;44 x 70 cm. and 22 x 35 cm., on sheet 105 x 140 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1901.","productDescription":"3 maps on 1 sheet :col. ;44 x 70 cm. and 22 x 35 cm., on sheet 105 x 140 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107173,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9991.htm","linkFileType":{"id":5,"text":"html"},"description":"9991"},{"id":188848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,38 ], [ -114,39 ], [ -112,39 ], [ -112,38 ], [ -114,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6912e8","contributors":{"authors":[{"text":"Steven, T. A.","contributorId":42575,"corporation":false,"usgs":true,"family":"Steven","given":"T.","middleInitial":"A.","affiliations":[],"preferred":false,"id":275740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":275739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowley, P. D.","contributorId":87551,"corporation":false,"usgs":true,"family":"Rowley","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":275741,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29020,"text":"wri894048 - 1990 - Altitude of potentiometric surface, fall 1985, and historic water-level changes in the Fort Pillow aquifer in western Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri894048","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4048","title":"Altitude of potentiometric surface, fall 1985, and historic water-level changes in the Fort Pillow aquifer in western Tennessee","docAbstract":"Recharge to the Fort Pillow aquifer of Tertiary age in Tennessee is from precipitation on the outcrop, which forms a narrow belt across western Tennessee, and by downward infiltration of water from the overlying fluvial deposits of Tertiary and Quaternary age and alluvium of Quaternary age or, where the upper confining unit is absent, from the overlying Memphis aquifer of Tertiary age. The potentiometric surface in the Fort Pillow aquifer slopes gently westward from the outcrop-recharge area, and the water moves slowly in that direction. A depression in the potentiometric surface in the Memphis area is the result of past pumping at Memphis Light, Gas and Water Division (MLGW) well fields (1924-74), and past and present pumping at an industrial well field at Memphis, and the municipal well field at West Memphis, Ark. Water levels in areas affected by pumping have declined at average rates ranging from 0.4 to 0. 9 ft/year during the period 1945-85. The greatest rate of decline was as much as 4.0 ft/year between 1945 and 1954 in an observation well in a well field of MLGW at Memphis. In 1971, MLGW ceased pumping from the Fort Pillow aquifer at this well field, and between 1972 and 1976, water levels rose about 28 ft in this well. Withdrawals from the Fort Pillow aquifer in western Tennessee in 1985 averaged about 12 million gal/day. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894048","usgsCitation":"Parks, W.S., and Carmichael, J.K., 1990, Altitude of potentiometric surface, fall 1985, and historic water-level changes in the Fort Pillow aquifer in western Tennessee: U.S. Geological Survey Water-Resources Investigations Report 89-4048, iii, 8 p. :ill. ;28 cm., https://doi.org/10.3133/wri894048.","productDescription":"iii, 8 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":2288,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri89-4048","linkFileType":{"id":5,"text":"html"}},{"id":124140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_89_4048.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689b98","contributors":{"authors":[{"text":"Parks, W. S.","contributorId":99555,"corporation":false,"usgs":true,"family":"Parks","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carmichael, J. K.","contributorId":90276,"corporation":false,"usgs":true,"family":"Carmichael","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":200801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28838,"text":"wri874200 - 1990 - Geochemistry of batch-extract waters derived from spoil material collected at the Cordero coal mine, Powder River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri874200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"87-4200","title":"Geochemistry of batch-extract waters derived from spoil material collected at the Cordero coal mine, Powder River basin, Wyoming","docAbstract":"Batch-mixing experiments to evaluate postmining water quality at the Cordero Mine were conducted by the U.S. Geological Survey during 1984 to 1985. Contact of groundwater from the spoil aquifer with fresh spoil material caused only small changes in major-element concentrations and in pH, unless sulfide oxidation or contact with soluble salts, such as epsomite, occurred. In contrast, large changes in major-element concentration resulted when water from the coal aquifer contacted the spoil material. Only three of seven reaction models considered to explain the water quality changes during the batch-mixing experiments were consistent with the thermodynamic and mineralogical data. The three models used to account for the observed water quality changes derived potassium from potassium feldspar; magnesium from chlorite or epsomite or both; sodium from cation exchange and halite; chloride from halite; silica from potassium feldspar and chlorite; sulfate from gypsum, or epsomite or both, and carbon from carbon dioxide. In general, water quality samples obtained from the batch-mixing experiments using water from the coal aquifer had smaller major-ion concentrations than the actual water quality in the spoil aquifer. These differences can be explained by the limited amount of efflorescent salt dissolution and volume of water used in the experiments. Correction ratios calculated for these experiments may be applied to batch-mixing experiments at other mines in the area, to predict postmining water quality. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports Section [distributor],","doi":"10.3133/wri874200","usgsCitation":"Naftz, D.L., 1990, Geochemistry of batch-extract waters derived from spoil material collected at the Cordero coal mine, Powder River basin, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 87-4200, vi, 58 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874200.","productDescription":"vi, 58 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4200/report-thumb.jpg"},{"id":57713,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a844c","contributors":{"authors":[{"text":"Naftz, D. L.","contributorId":40624,"corporation":false,"usgs":true,"family":"Naftz","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200487,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29025,"text":"wri884182 - 1990 - Geology and ground-water resources of the Memphis Sand in western Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri884182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-4182","title":"Geology and ground-water resources of the Memphis Sand in western Tennessee","docAbstract":"The Memphis Sand of the Claiborne Group of Tertiary age underlies approximately 7,400 square miles in western Tennessee. The formation primarily consists of a thick body of veryfine to very coarse sand that includes subordinate lenses or beds of clay and silt at various horizons. The Memphis Sand ranges from 0 to about 900 feet in thickness, but where the original thickness is preserved, it is about 400 to 900 feet thick. The Memphis Sand yields water to wells in most of the area of occurrence in western Tennessee and, where saturated, makes up the Memphis aquifer.\r\n\r\nRecharge to the Memphis aquifer is from precipitation on the outcrop, which is a broad belt across western Tennessee, or by downward infiltration of water from the overlying fluvial deposits of Tertiary(?) and Quatemary age and alluvium of Quatemary age. Long-term data from five observation wells indicate that water levels have declined at average rates rangingfrom less than 0.1 to 1.3 feet per year during the period 1928-83. The largest declines have been in the Memphis area. Water from the Memphis aquifer generally is a calcium bicarbonate type, but locally is a sodium bicarbonate or mixed type. The water contains low concentrations of most major constituents and generally is suitable for most uses. Dissolved-solids concentrations range from 19 to 333 milligrams per liter. The results from 76 aquifer tests made in the Memphis area and western Tennessee during the period 1949-62 indicate that transmissivities range from 2,700 to 53,500 feet squared per day, and storage coefficients range from 0.0001 to 0.003. The Memphis aquifer provides moderate to large quantities of water for many public and industrial water supplies in western Tennessee and small quantities to numerous domestic and farm wells. Withdrawals for public and industrial supplies in 1983 averaged about 227 million gallons per day, of which 183 million gallons per day were in the Memphis area. The Memphis aquifer has much potential for future use, particularly at places outside the Memphis area.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri884182","usgsCitation":"Parks, W.S., and Carmichael, J.K., 1990, Geology and ground-water resources of the Memphis Sand in western Tennessee: U.S. Geological Survey Water-Resources Investigations Report 88-4182, iv, 30 p. :ill. (some col.), maps ;28 cm., https://doi.org/10.3133/wri884182.","productDescription":"iv, 30 p. :ill. (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":2292,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri88-4182","linkFileType":{"id":5,"text":"html"}},{"id":123455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_88_4182.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6854ed","contributors":{"authors":[{"text":"Parks, William Scott","contributorId":52148,"corporation":false,"usgs":true,"family":"Parks","given":"William","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":200812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carmichael, J. K.","contributorId":90276,"corporation":false,"usgs":true,"family":"Carmichael","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":200813,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67119,"text":"i1926 - 1990 - Geologic map of Precambrian rocks of Neillsville-Stevens Point area, Wisconsin","interactions":[{"subject":{"id":41096,"text":"ofr78318 - 1978 - Preliminary geologic map of Precambrian rocks in part of northern Wisconsin","indexId":"ofr78318","publicationYear":"1978","noYear":false,"title":"Preliminary geologic map of Precambrian rocks in part of northern Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":67119,"text":"i1926 - 1990 - Geologic map of Precambrian rocks of Neillsville-Stevens Point area, Wisconsin","indexId":"i1926","publicationYear":"1990","noYear":false,"title":"Geologic map of Precambrian rocks of Neillsville-Stevens Point area, Wisconsin"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:03","indexId":"i1926","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1926","subseriesTitle":"NONE","title":"Geologic map of Precambrian rocks of Neillsville-Stevens Point area, Wisconsin","language":"ENGLISH","doi":"10.3133/i1926","usgsCitation":"Sims, P., 1990, Geologic map of Precambrian rocks of Neillsville-Stevens Point area, Wisconsin: U.S. Geological Survey IMAP 1926, 1 map :col. ;56 x 120 cm., on sheet 99 x 142 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1926.","productDescription":"1 map :col. ;56 x 120 cm., on sheet 99 x 142 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107184,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10004.htm","linkFileType":{"id":5,"text":"html"},"description":"10004"},{"id":189403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91,44.25 ], [ -91,44.75 ], [ -89.5,44.75 ], [ -89.5,44.25 ], [ -91,44.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2c50","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":275628,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29023,"text":"wri884181 - 1990 - Geology and ground-water resources of the Cockfield Formation in western Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri884181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-4181","title":"Geology and ground-water resources of the Cockfield Formation in western Tennessee","docAbstract":"The Cockfield Formation of the Claiborne Group of Tertiary age underlies approximately 4,000 sq mi in western Tennessee. The formation consists primarily of lenticular beds of very fine to coarse sand, silt, clay, and lignite. The Cockfield Formation has been extensively eroded, and the original thickness is preserved only in a few areas where the formation ranges from 235 to 270 ft in thickness. Recharge to the Cockfield aquifer is from precipitation on sparse outcrops or by downward infiltration of water from the overlying fluvial deposits of Tertiary and Quaternary age and alluvium of Quaternary age or, where present, the overlying Jackson Formation of Tertiary age. Data from two observation wells indicate that water levels have risen at average rates of about 0.5 and 0.7 ft/year during the period 1980-85. Water from the Cockfield aquifer is a calcium bicarbonate type that contains low concentrations of most major constituents, and generally is suitable for most uses. Dissolved-solids concentrations range from 44 to 218 mg/L. Data from two aquifer tests indicate transmissivities of 2,500 and 6 ,000 sq ft/day and storage coefficients of 0.0003 and 0.0007, respectively. The Cockfield aquifer presently provides small to moderate quantities of water for several public and industrial water supplies and small quantities to numerous domestic and farm wells. Withdrawals for public and industrial supplies in 1983 averaged about 3.3 million gal/day. (USGS)","language":"ENGLISH","publisher":"Department of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri884181","usgsCitation":"Parks, W.S., and Carmichael, J.K., 1990, Geology and ground-water resources of the Cockfield Formation in western Tennessee: U.S. Geological Survey Water-Resources Investigations Report 88-4181, iv, 17 p. :ill. (some col.), one col. map ;28 cm., https://doi.org/10.3133/wri884181.","productDescription":"iv, 17 p. :ill. (some col.), one col. map ;28 cm.","costCenters":[],"links":[{"id":2290,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri88-4181","linkFileType":{"id":5,"text":"html"}},{"id":126785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_88_4181.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685834","contributors":{"authors":[{"text":"Parks, W. S.","contributorId":99555,"corporation":false,"usgs":true,"family":"Parks","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carmichael, J. K.","contributorId":90276,"corporation":false,"usgs":true,"family":"Carmichael","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":200808,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27899,"text":"wri904086 - 1990 - Use of ground-penetrating radar for water-table mapping, Brewster and Harwich, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri904086","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4086","title":"Use of ground-penetrating radar for water-table mapping, Brewster and Harwich, Massachusetts","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor], 1992","doi":"10.3133/wri904086","usgsCitation":"Johnson, D., 1990, Use of ground-penetrating radar for water-table mapping, Brewster and Harwich, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 90-4086, v, 27 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904086.","productDescription":"v, 27 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4086/report-thumb.jpg"},{"id":56717,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4086/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56718,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4086/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604544","contributors":{"authors":[{"text":"Johnson, D.G.","contributorId":40245,"corporation":false,"usgs":true,"family":"Johnson","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":198868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28426,"text":"wri904012 - 1990 - Ground-water withdrawals, water-level changes, land-surface subsidence, and ground-water quality in Fort Bend County, Texas, 1969-87","interactions":[],"lastModifiedDate":"2016-08-16T09:40:10","indexId":"wri904012","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4012","title":"Ground-water withdrawals, water-level changes, land-surface subsidence, and ground-water quality in Fort Bend County, Texas, 1969-87","docAbstract":"<p>Fort Bend County, which has one of the fastest growing populations of all counties in the United States, is dependent entirely on ground water for public supply. Since 1969, at least 90 large-capacity wells have been drilled, of which 57 were public supply wells, 23 were irrigation wells, and 10 were industrial wells. All but seven of the new public-supply wells are located in the northeastern part of the county.</p>\n<p>The withdrawal of ground water in Fort Bend County increased from 56 million gallons per day in 1969 to 72 million gallons per day in 1982, and then decreased to 53 million gallons per day in 1986. Withdrawals for public supply increased from 4 million gallons per day in 1969 to 28 million gallons per day in 1986. Withdrawals for irrigation averaged 38 million gallons per day during 1969-82 and in 1984, but averaged 20 million gallons per day in 1983, 1985, and 1986. Withdrawals for industrial use declined from 13 million gallons per day in 1969 to 5 million gallons per day in 1986.</p>\n<p>Water levels in wells screened in the upper unit of the Chicot aquifer generally fluctuated less than 4 feet between 1968-69 and 1987. During the same period, water-level declines in wells screened in the lower unit of the Chicot aquifer ranged from less than 10 feet in most of the western part of the county to 100 feet in the northeastern corner. In the southwestern part of the county, the decline was less than 20 feet. Hydrographs of wells completed in the lower unit of the Chicot showed that water levels continued to decline from 1969 to the early 1980's. The hydrographs of wells located outside of the northeast area generally show a stabilization of water levels corresponding to the reduction in withdrawals after 1982 in Fort Bend County and in the neighboring Houston metropolitan area to the northeast.</p>\n<p>Withdrawals from the Evangeline aquifer increased from 15 percent of the total in 1969 to 50 percent in 1986. Water-level declines in wells screened in the Evangeline aquifer during the same period ranged from less than 25 feet in the northwestern part of the county to 125 feet in the northeastern part. In the southwestern one-quarter of the county, the decline was less than 50 feet.</p>\n<p>Declines in the potentiometric surfaces of the aquifers have caused compaction of clay resulting in land-surface subsidence. Between 1906 and 1978, about 65 percent of the county subsided more than 0.5 foot. Studies in the Houston area have shown that most clay compaction occurs in the Chicot aquifer and that the compressibility of the clays increases towards the coast. The total thickness of clays in the Chicot aquifer increases from less than 150 feet in the northwestern part of Fort Bend County to more than 350 feet along the eastern border. The total thickness of clay in the Evangeline aquifer increases from an average of about 700 feet in the northwest to about 1,100 feet in the east. The northeastern part of Fort Bend County is most susceptible to future subsidence because it is the area where the largest water-level declines have occurred and where the thickest, most compressible clays in the county are found.</p>\n<p>The concentrations of dissolved solids in water from wells in Fort Bend County have not changed appreciably from 1969 to 1987. The median concentrations of dissolved solids are 475 milligrams in water from wells in Fort Bend per liter in water from the upper unit of the Chicot aquifer, 337 milligrams per liter in water from the lower unit of the Chicot aquifer, and 307 milligrams per liter in water from the Evangeline aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri904012","collaboration":"Prepared in cooperation with Ford Bend County","usgsCitation":"Locke, G., 1990, Ground-water withdrawals, water-level changes, land-surface subsidence, and ground-water quality in Fort Bend County, Texas, 1969-87: U.S. Geological Survey Water-Resources Investigations Report 90-4012, v, 155 p., https://doi.org/10.3133/wri904012.","productDescription":"v, 155 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":123231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4012/report-thumb.jpg"},{"id":57229,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4012/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Fort Bend 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Bend\",\"state\":\"TX\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648727","contributors":{"authors":[{"text":"Locke, G.L.","contributorId":59065,"corporation":false,"usgs":true,"family":"Locke","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":199775,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38368,"text":"pp1515 - 1990 - The San Andreas Fault System, California","interactions":[],"lastModifiedDate":"2019-07-10T15:06:12","indexId":"pp1515","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"1515","title":"The San Andreas Fault System, California","docAbstract":"<p>Maps of northern and southern California printed on flyleaf inside front cover and on adjacent pages show faults that have had displacement within the past 2 million years. Those that have had displacement within historical time are shown in red. Bands of red tint emphasize zones of historical displacement; bands of orange tint emphasize major faults that have had Quaternary displacement before historical time. Faults are dashed where uncertain, dotted where covered by sedimentary deposits, and queried when doubtful. Arrows indicate direction of relative movement; sawteeth on upper plate of thrust fault. </p><p>These maps are reproductions, in major part, of selected plates from the \"Fault Map of California,\" published in 1975 by the California Division of Mines and Geology at a scale of 1:750,000; the State map was compiled and data interpreted by Charles W. Jennings. New data about faults, not shown on the 1975 edition, required modest revisions, primarily additions however, most of the map was left unchanged because the California Division of Mines and Geology is currently engaged in a major revision and update of the 1975 edition. Because of the reduced scale here, names of faults and places were redrafted or omitted. Faults added to the reduced map are not as precise as on the original State map, and the editor of this volume selected certain faults and omitted others. Principal regions for which new information was added are the region north of the San Francisco Bay area and the offshore regions.</p><p>Many people have contributed to the present map, but the editor is solely responsible for any errors and omissions. Among those contributing informally, but extensively, and the regions to which each contributed were G.A. Carver, onland region north of lat 40°N.; S.H. Clarke, offshore region north of Cape Mendocino; R.J. McLaughlin, onland region between lat 40°00' and 40°30' N. and long 123°30' and 124°30' W.; D.S. McCulloch offshore region between lat 35° and 40° N.; J.G. Vedder, offshore reglor south of lat 35° N.; and D.G. Herd, southern San Francisco Bay region. The Fault Evaluation Program of the California Division of Mines and Geology under the direction of E.W. Hart, provided much data about many faults. Unpublished material about the Bartlett Springs fault zone that was gathered by Geomatrix Consultants for the Pacific Gas and Electric Co. was very useful. In addition, selected publications that provided invaluable data include Bortugno (1982), Herd (1977), Herd and Helley (1977), Pampeyan and others (1981), and Yerkes and others (1980).&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1515","usgsCitation":"1990, The San Andreas Fault System, California (Version 1.0): U.S. Geological Survey Professional Paper 1515, viii, 283 p., https://doi.org/10.3133/pp1515.","productDescription":"viii, 283 p.","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":125276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_1515.jpg"},{"id":9777,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/1990/1515/","linkFileType":{"id":5,"text":"html"}},{"id":333194,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1990/1515/pp1515.pdf","text":"Report","size":"116 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"California","otherGeospatial":"San Andreas Fault","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,33 ], [ -125,43 ], [ -114,43 ], [ -114,33 ], [ -125,33 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67abf3","contributors":{"editors":[{"text":"Wallace, Robert E.","contributorId":15570,"corporation":false,"usgs":true,"family":"Wallace","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":658428,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":28997,"text":"wri904034 - 1990 - Estimation of the relative permeability distribution in fractured granitic rocks by means of vertical flow measurements in the Siblingen borehole, Switzerland","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri904034","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4034","title":"Estimation of the relative permeability distribution in fractured granitic rocks by means of vertical flow measurements in the Siblingen borehole, Switzerland","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey :\r\nBooks and Open-File Reports Sections [distributor],","doi":"10.3133/wri904034","usgsCitation":"Paillet, F.L., Hess, A., and Morin, R.H., 1990, Estimation of the relative permeability distribution in fractured granitic rocks by means of vertical flow measurements in the Siblingen borehole, Switzerland: U.S. Geological Survey Water-Resources Investigations Report 90-4034, v, 26 p. :ill. ;28 cm., https://doi.org/10.3133/wri904034.","productDescription":"v, 26 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":121502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4034/report-thumb.jpg"},{"id":57864,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4034/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb1b0","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, A.E.","contributorId":71979,"corporation":false,"usgs":true,"family":"Hess","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":200759,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morin, R. H.","contributorId":31794,"corporation":false,"usgs":true,"family":"Morin","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":200757,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3699,"text":"cir1036 - 1990 - Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings","interactions":[{"subject":{"id":70194907,"text":"70194907 - 1990 - Geohydrology of the near-surface unsaturated zone adjacent to the disposal site for low-level radioactive waste near Beatty, Nevada: A section in Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings (Circular 1036)","indexId":"70194907","publicationYear":"1990","noYear":false,"displayTitle":"Geohydrology of the near-surface unsaturated zone adjacent to the disposal site for low-level radioactive waste near Beatty, Nevada: A section in <i>Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings (Circular 1036)</i>","title":"Geohydrology of the near-surface unsaturated zone adjacent to the disposal site for low-level radioactive waste near Beatty, Nevada: A section in Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings (Circular 1036)"},"predicate":"IS_PART_OF","object":{"id":3699,"text":"cir1036 - 1990 - Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings","indexId":"cir1036","publicationYear":"1990","noYear":false,"title":"Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings"},"id":1},{"subject":{"id":70194941,"text":"70194941 - 1990 - Topic I: Induced changes in hydrology at low-level radioactive waste repository sites: A section in Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings (Circular 1036)","indexId":"70194941","publicationYear":"1990","noYear":false,"displayTitle":"Topic I: Induced changes in hydrology at low-level radioactive waste repository sites: A section in <i>Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings (Circular 1036)</i>","title":"Topic I: Induced changes in hydrology at low-level radioactive waste repository sites: A section in Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings (Circular 1036)"},"predicate":"IS_PART_OF","object":{"id":3699,"text":"cir1036 - 1990 - Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings","indexId":"cir1036","publicationYear":"1990","noYear":false,"title":"Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings"},"id":2}],"lastModifiedDate":"2018-01-29T14:44:15","indexId":"cir1036","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"1036","title":"Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings","docAbstract":"<p>In the United States, low-level radioactive waste is disposed by shallow-land burial. Low-level radioactive waste generated by non-Federal facilities has been buried at six commercially operated sites; low-level radioactive waste generated by Federal facilities has been buried at eight major and several minor Federally operated sites (fig. 1). Generally, low-level radioactive waste is somewhat imprecisely defined as waste that does not fit the definition of high-level radioactive waste and does not exceed 100 nCi/g in the concentration of transuranic elements. Most low-level radioactive waste generated by non-Federal facilities is generated at nuclear powerplants; the remainder is generated primarily at research laboratories, hospitals, industrial facilities, and universities. On the basis of half lives and concentrations of radionuclides in low-level radioactive waste, the hazard associated with burial of such waste generally lasts for about 500 years. Studies made at several of the commercially and Federally operated low-level radioactive-waste repository sites indicate that some of these sites have not provided containment of waste nor the expected protection of the environment.</p>","conferenceTitle":"Low-level radioactive-waste disposal workshop","conferenceDate":"July 11-16, 1987","conferenceLocation":"Big Bear Lake, CA","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir1036","usgsCitation":"1990, Safe disposal of radionuclides in low-level radioactive-waste repository sites; Low-level radioactive-waste disposal workshop, U.S. Geological Survey, July 11-16, 1987, Big Bear Lake, Calif., Proceedings: U.S. Geological Survey Circular 1036, ix, 125 p., https://doi.org/10.3133/cir1036.","productDescription":"ix, 125 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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,{"id":38392,"text":"pp1505D - 1990 - Coal resources of Upper Cretaceous Fruitland Formation in the Southern Ute Indian Reservation, southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:09:39","indexId":"pp1505D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"1505","chapter":"D","title":"Coal resources of Upper Cretaceous Fruitland Formation in the Southern Ute Indian Reservation, southwestern Colorado","docAbstract":"Coal resources of the Upper Cretaceous Fruitland Formation in the Southern Ute Indian Reservation are estimated to total 16 billion short tons of bituminous coal in beds 2 feet thick or more. The coal-bearing Fruitland Formation underlies about 700 square miles of the Southern Ute Indian Reservation and crops out in a roughly semicircular band around the northern edge of the structural San Juan Basin. The coal beds locally dip more than 10? to the southeast along the northwestern rim of the basin. \r\n\r\nThis estimate of coal resources is based on a study of about 500 geophysical logs, mostly of oil and gas wells. Total coal resources include 15 billion short tons of identified resources, based on data points 3 miles or less apart, and about 1 billion short tons of undiscovered or hypothetical resources, based on data points more than 3 miles apart. \r\n\r\nIn this report, the coal-bearing interval is divided into three overlapping zones: lower, middle, and upper. Coal resources were estimated by aggregate thickness for each zone. The lower zone, which is southwest of a large stratigraphic rise of the Pictured Cliffs Sandstone, contains the thickest coal beds, generally in two thick beds that locally have an aggregate thickness as much as 50 feet. The lower zone contains about 28 percent of the estimated resources; in the lower zone, 6 percent of the resources are less than 500 feet beneath the surface, 10 percent of the resources are 500-2,000 feet beneath the surface, and 84 percent are more than 2,000 feet beneath the surface. The middle zone contains 22 percent of the estimated resources; in the middle zone, only 2 percent of the resources are less than 500 feet beneath the surface, 4 percent of the resources are 500-2,000 feet beneath the surface, and 94 percent are more than 2,000 feet beneath the surface. The upper zone contains about half the estimated resources, in part because it occupies about three-fourths of the area underlain by the Fruitland Formation; in the upper zone, about 2 percent of the resources are less then 500 feet beneath the surface, 11 percent are 500-2,000 feet beneath the surface, and 87 percent are more than 2,000 feet beneath the surface. In general the coal beds are thinner in the middle and upper zones than in the lower zone. \r\n\r\nAlthough the coal on the Reservation is of comparatively high rank, coal in the Fruitland is generally characterized by high ash content. Mining on the Reservation has been restricted generally to small underground and strip mines within 200 feet of the surface along the edges of the San Juan Basin.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and Mineral Resources of the Southern Ute Indian Reservation","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp1505D","usgsCitation":"Sandberg, D.T., 1990, Coal resources of Upper Cretaceous Fruitland Formation in the Southern Ute Indian Reservation, southwestern Colorado: U.S. Geological Survey Professional Paper 1505, p. D1-D24; 3 plates in pocket, https://doi.org/10.3133/pp1505D.","productDescription":"p. D1-D24; 3 plates in pocket","costCenters":[],"links":[{"id":104668,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4912.htm","linkFileType":{"id":5,"text":"html"},"description":"4912"},{"id":125038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1505d/report-thumb.jpg"},{"id":64746,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1505d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64747,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1505d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64748,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1505d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1505d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0f97","contributors":{"authors":[{"text":"Sandberg, Dorothy T.","contributorId":19240,"corporation":false,"usgs":true,"family":"Sandberg","given":"Dorothy","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":219738,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26644,"text":"wri884209 - 1990 - Use of paleoflood investigations to improve flood-frequency analyses of plains streams in Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri884209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-4209","title":"Use of paleoflood investigations to improve flood-frequency analyses of plains streams in Wyoming","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri884209","usgsCitation":"Cooley, M.E., 1990, Use of paleoflood investigations to improve flood-frequency analyses of plains streams in Wyoming: U.S. Geological Survey Water-Resources Investigations Report 88-4209, vii, 75 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884209.","productDescription":"vii, 75 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4209/report-thumb.jpg"},{"id":55522,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4209/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685892","contributors":{"authors":[{"text":"Cooley, M. E.","contributorId":89868,"corporation":false,"usgs":true,"family":"Cooley","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":196761,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28823,"text":"wri904043 - 1990 - Hydrogeology and ground-water-quality conditions at the Emporia- Lyon County Landfill, eastern Kansas, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri904043","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4043","title":"Hydrogeology and ground-water-quality conditions at the Emporia- Lyon County Landfill, eastern Kansas, 1988","docAbstract":"Hydrogeology and water-quality conditions at the Emporia-Lyon County Landfill, eastern Kansas, were investigated from April 1988 through April 1989. Potentiometric-surface maps indicated groundwater movement from the northeast and northwest towards the landfill and then south through the landfill to the Cottonwood River. The maps indicate that during periods of low groundwater levels, groundwater flows northward in the north-west part of the landfill, which may have been induced by water withdrawal from wells north of the landfill or by water ponded in waste lagoons south and west of the landfill. Chemical analysis of water samples from monitoring wells upgradient and downgradient of the landfill indicate calcium bicarbonate to be the dominant water type. No inorganic or organic chemical concentrations exceeded Kansas or Federal primary drinking-water standards. Kansas secondary drinking-water standards were equaled or exceeded, however, in water from some or all wells for total hardness, dissolved solids, iron, and manganese. Water from one upgradient well contained larger concentrations of dissolved oxygen and nitrate, and smaller concentrations of bicarbonate, alkalinity, ammonia, arsenic, iron, and manganese as compared to all other monitoring wells. Results of this investigation indicate that groundwater quality downgradient of well MW-2 has increased concentrations of some inorganic and organic compounds. Due to the industrial nature of the area and the changing directions of groundwater flow, it is not clear what the source of these compounds might be. Long-term monitoring, additional wells, and access to nearby waste lagoons and waste-lagoon monitoring wells would help define the sources of increased inorganic and organic compounds. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904043","usgsCitation":"Myers, N.C., and Bigsby, P., 1990, Hydrogeology and ground-water-quality conditions at the Emporia- Lyon County Landfill, eastern Kansas, 1988: U.S. Geological Survey Water-Resources Investigations Report 90-4043, vi, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904043.","productDescription":"vi, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4043/report-thumb.jpg"},{"id":57683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4043/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625690","contributors":{"authors":[{"text":"Myers, N. C.","contributorId":13622,"corporation":false,"usgs":true,"family":"Myers","given":"N.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":200458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bigsby, P. R.","contributorId":54631,"corporation":false,"usgs":true,"family":"Bigsby","given":"P. R.","affiliations":[],"preferred":false,"id":200459,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28934,"text":"wri874156 - 1990 - Appraisal of the water resources of the Skunk Creek Aquifer in Minnehaha County, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri874156","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"87-4156","title":"Appraisal of the water resources of the Skunk Creek Aquifer in Minnehaha County, South Dakota","docAbstract":"The Skunk Creek aquifer, a major glacial outwash deposit in the Skunk Creek drainage basin, consists of a 30-sq-mi shallow stream connected sand and gravel aquifer in southeastern South Dakota. The aquifer thickness ranges from 1 to 74 ft. Average annual fluctuation of the water table is 2.5 ft. The water has an average dissolved-solids content of 620 mg/L and is very hard , averaging 403 mg/L calcium carbonate hardness. A numerical model was developed and calibrated under steady-state and transient conditions. The model contained 484 active nodes each representing 0.0625 sq mi. Hydraulic conductivities of the aquifer used in the model range from 10 to 400 ft/d, and average specific yield is 20%. Recharge from infiltration of precipitation was estimated to be 6 inches/yr or 24% of average annual precipitation. Maximum evapotranspiration rate was 32 inches/yr and the evapotranspiration extinction depth for the model was 5 ft. The steady-state hydrologic budget was about 11 ,000 acre-ft/yr. Recharge by precipitation was about 9,500 acre-ft and recharge from streams was about 1,100 acre-ft. Discharge by evapotranspiration was about 5,000 acre-ft and discharge to streams was about 5,700 acre-ft. A hypothetical simulation to determine maximum withdrawal under steady-state conditions resulted in a groundwater withdrawal of about 15,700 acre-ft/yr from 19 hypothetical wells pumping at a rate of 500 gal/min and 13 existing wells pumping at a combined average rate of 24 gal/min. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports, [distributor],","doi":"10.3133/wri874156","usgsCitation":"Ohland, G., 1990, Appraisal of the water resources of the Skunk Creek Aquifer in Minnehaha County, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 87-4156, v, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874156.","productDescription":"v, 54 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4156/report-thumb.jpg"},{"id":57807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4156/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a3eb","contributors":{"authors":[{"text":"Ohland, G.L.","contributorId":45749,"corporation":false,"usgs":true,"family":"Ohland","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":200643,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27536,"text":"wri904178 - 1990 - Simulation of ground-water flow and potential land subsidence, Avra Valley, Arizona","interactions":[],"lastModifiedDate":"2022-11-23T19:46:57.690056","indexId":"wri904178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4178","title":"Simulation of ground-water flow and potential land subsidence, Avra Valley, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904178","usgsCitation":"Hanson, R.T., Anderson, S.R., and Pool, D.R., 1990, Simulation of ground-water flow and potential land subsidence, Avra Valley, Arizona: U.S. Geological Survey Water-Resources Investigations Report 90-4178, v, 41 p., https://doi.org/10.3133/wri904178.","productDescription":"v, 41 p.","costCenters":[],"links":[{"id":56395,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4178/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4178/report-thumb.jpg"},{"id":409595,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47422.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona","otherGeospatial":"Avra Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.0167,\n              32\n            ],\n            [\n              -111.0167,\n              32.6439\n            ],\n            [\n              -111.5,\n              32.6439\n            ],\n            [\n              -111.5,\n              32\n            ],\n            [\n              -111.0167,\n              32\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2ae2","contributors":{"authors":[{"text":"Hanson, R. T.","contributorId":91148,"corporation":false,"usgs":true,"family":"Hanson","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":198278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, S. R.","contributorId":93518,"corporation":false,"usgs":true,"family":"Anderson","given":"S.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198277,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":49418,"text":"ofr90400E - 1990 - New information resources of the U.S. Geological Survey Library System, May 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:10:24","indexId":"ofr90400E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-400","chapter":"E","title":"New information resources of the U.S. Geological Survey Library System, May 1990","language":"ENGLISH","doi":"10.3133/ofr90400E","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, New information resources of the U.S. Geological Survey Library System, May 1990: U.S. Geological Survey Open-File Report 90-400, 66 p. ; 28 cm., https://doi.org/10.3133/ofr90400E.","productDescription":"66 p. ; 28 cm.","costCenters":[],"links":[{"id":170251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0400e/report-thumb.jpg"},{"id":86062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0400e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69766c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29026,"text":"wri904092 - 1990 - Hydrogeology and preliminary assessment of the potential for contamination of the Memphis aquifer in the Memphis area, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri904092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4092","title":"Hydrogeology and preliminary assessment of the potential for contamination of the Memphis aquifer in the Memphis area, Tennessee","docAbstract":"Detailed maps of the thickness of the\r\nJackson-upper Claibome confining unit and the\r\naltitude of the water table in the alluvium andfluvial\r\ndeposits provide much new information concerning\r\nareas where downward leakage is or may be\r\noccurringfrom the water-table aquifers to theMemphrj\r\naqutyer in the Memphis area. A detailed map\r\nof the altitude of the potentiometric surface of the\r\nMemphis aquifer and the locations of 44sites where\r\ncontaminants have been detected in the water-table\r\naquifers indicate that many of these sites are located\r\nin areas where the direction of ground-water flow in\r\nthe Memphis aquifer is toward municipal well\r\nfields. Consequently, if contaminants enter the\r\nMemphis aquifer, a hydraulic potential exists for\r\ntheir transport to those wellfields.\r\nRecently (19&S-88), volatile organic compounds\r\nwere detected in water from five municipal\r\nwells screened in the Memphis aquifer - three in the\r\nAllen well field of the Memphis Light, Gas and\r\nWater Division at Memphis and two in the west well\r\nfield at Collierville. Concentrations of seven volatile\r\norganic compounds totaled about II microgramsperliterin\r\nasamplefrom one well in theAllen\r\nwellfield at Memphis, and the concentration of one\r\ncompound was 25 micrograms per liter in a sample\r\nj?om one well at Collierville. These are the first\r\nreported occurrences of synthetic organic compounds\r\nin the Memphis aquifer andprove that the\r\nprincipal aquifer in the Memphis area is vulnerable\r\nto contamination.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904092","usgsCitation":"Parks, W.S., 1990, Hydrogeology and preliminary assessment of the potential for contamination of the Memphis aquifer in the Memphis area, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 90-4092, iv, 39 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri904092.","productDescription":"iv, 39 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":2293,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri904092/","linkFileType":{"id":5,"text":"html"}},{"id":159409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":57887,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4092/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57888,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4092/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57889,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4092/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57890,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4092/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a642b","contributors":{"authors":[{"text":"Parks, W. S.","contributorId":99555,"corporation":false,"usgs":true,"family":"Parks","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}