{"pageNumber":"4045","pageRowStart":"101100","pageSize":"25","recordCount":184938,"records":[{"id":19250,"text":"ofr94419 - 1994 - Geology of the Coffman 7 1/2' quadrangle, Ste. Genevieve County, Missouri","interactions":[],"lastModifiedDate":"2021-10-18T21:50:56.880269","indexId":"ofr94419","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-419","title":"Geology of the Coffman 7 1/2' quadrangle, Ste. Genevieve County, Missouri","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94419","usgsCitation":"Harrison, R., and Schultz, A., 1994, Geology of the Coffman 7 1/2' quadrangle, Ste. Genevieve County, Missouri: U.S. Geological Survey Open-File Report 94-419, Report: 6 p.; 2 Plates: 23.00 × 30.00 inches and \t21.00 × 33.00 inches, https://doi.org/10.3133/ofr94419.","productDescription":"Report: 6 p.; 2 Plates: 23.00 × 30.00 inches and \t21.00 × 33.00 inches","costCenters":[],"links":[{"id":108232,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12528.htm","linkFileType":{"id":5,"text":"html"},"description":"12528"},{"id":48710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0419/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21616,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0419/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21615,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0419/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0419/report-thumb.jpg"}],"country":"United States","state":"Missouri","county":"Ste. Genevieve County","otherGeospatial":"Coffman 7 1/2' quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.25,\n              37.75\n            ],\n            [\n              -90.125,\n              37.75\n            ],\n            [\n              -90.125,\n              37.875\n            ],\n            [\n              -90.25,\n              37.875\n            ],\n            [\n              -90.25,\n              37.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6986ad","contributors":{"authors":[{"text":"Harrison, R.W.","contributorId":32188,"corporation":false,"usgs":true,"family":"Harrison","given":"R.W.","affiliations":[],"preferred":false,"id":180559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schultz, A. P.","contributorId":106139,"corporation":false,"usgs":true,"family":"Schultz","given":"A. P.","affiliations":[],"preferred":false,"id":180560,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001548,"text":"1001548 - 1994 - Birds of an unnatural prairie","interactions":[],"lastModifiedDate":"2017-12-27T13:06:20","indexId":"1001548","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3787,"text":"Winging It","active":true,"publicationSubtype":{"id":10}},"title":"Birds of an unnatural prairie","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Winging It","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Johnson, D.H., 1994, Birds of an unnatural prairie: Winging It, v. 6, no. 6, p. 7-7.","productDescription":"1 p.","startPage":"7","endPage":"7","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db611f87","contributors":{"authors":[{"text":"Johnson, Douglas H. 0000-0002-7778-6641","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":70327,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":311236,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44745,"text":"wri934174 - 1994 - Potentiometric-surface map of the lower Wilcox aquifer in Mississippi, October through December 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:10:55","indexId":"wri934174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4174","title":"Potentiometric-surface map of the lower Wilcox aquifer in Mississippi, October through December 1988","language":"ENGLISH","doi":"10.3133/wri934174","usgsCitation":"Oakley, W.T., Burt, D.E., and Goldsmith, G.D., 1994, Potentiometric-surface map of the lower Wilcox aquifer in Mississippi, October through December 1988: U.S. Geological Survey Water-Resources Investigations Report 93-4174, 1 map ; 84 x 94 cm. on sheet 91 x 97 cm., folded in envelope 32 x 24 cm., https://doi.org/10.3133/wri934174.","productDescription":"1 map ; 84 x 94 cm. on sheet 91 x 97 cm., folded in envelope 32 x 24 cm.","costCenters":[],"links":[{"id":167989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91734,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4174/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681ecb","contributors":{"authors":[{"text":"Oakley, W. T.","contributorId":76331,"corporation":false,"usgs":true,"family":"Oakley","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":230358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burt, David E. Jr.","contributorId":31443,"corporation":false,"usgs":true,"family":"Burt","given":"David","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":230357,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goldsmith, Gala D. S.","contributorId":88420,"corporation":false,"usgs":true,"family":"Goldsmith","given":"Gala","email":"","middleInitial":"D. S.","affiliations":[],"preferred":false,"id":230359,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70197323,"text":"70197323 - 1994 - Continent-ocean transition in Alaska:  The tectonic assembly of eastern Denalia","interactions":[],"lastModifiedDate":"2023-11-16T15:45:13.360747","indexId":"70197323","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Continent-ocean transition in Alaska:  The tectonic assembly of eastern Denalia","docAbstract":"<p><span>Alaska is the eastern, subaerial part of a large subcontinent of distinctive tectonic character that serves as an isthmus between nuclear North America, with its fringing belt of allochthonous terranes, and the accreted terranes and volcanic belts that constitute northeastern Russia. Physiographically, this subcontinent, which we name Denalia, is a bulge in the continental platform in the vicinity of Alaska, the Chukotsk Peninsula, and the broad continental shelf of the Bering Sea. The bulge is convex to the south and is bounded on the east and west by constrictions in the width of the continental platform and on the north and south by the edge of the continental shelf (Fig. 1). Tectonically, Denalia is characterized by geologic youthfulness and complexity, an abundance of convergent and transcurrent faults, and absence of autochthonous cratonic rocks. It contains a profusion of lithotectonic terranes of diverse origin and age that were emplaced in late Mesozoic and Cenozoic time. In addition, it includes the superimposed Cenozoic Aleutian arc and subduction zone and the Queen Charlotte-Fairweather transform fault system. Parts of Denalia were created by pre-middle Mesozoic tectonic events, but these took place elsewhere, before the affected rocks were tectonically transported and incorporated into the landmass of Denalia. Except for a small area in the Porcupine Plateau region along the Alaska-Yukon boundary, the only Precambrian rocks that have been recognized in the subcontinent are in tectonically emplaced fragments, the largest of which is the Arctic Alaska terrane in the Brooks Range, Arctic Foothills, and Arctic Foothills.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Phanerozoic evolution of North American continent ocean transitions","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder, CO","doi":"10.1130/DNAG-COT-PEN.399","usgsCitation":"Moore, T.E., Grantz, A., and Roeske, S.M., 1994, Continent-ocean transition in Alaska:  The tectonic assembly of eastern Denalia, chap. <i>of</i> Phanerozoic evolution of North American continent ocean transitions, p. 399-441, https://doi.org/10.1130/DNAG-COT-PEN.399.","productDescription":"43 p.","startPage":"399","endPage":"441","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354536,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States, Russia","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -135,\n              75\n            ],\n            [\n              -179.9,\n              75\n            ],\n            [\n              -179.9,\n              50\n            ],\n            [\n              -135,\n              50\n            ],\n            [\n              -135,\n              75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              179.9,\n              75\n            ],\n            [\n              160,\n              75\n            ],\n            [\n              160,\n              50\n            ],\n            [\n              179.9,\n              50\n            ],\n            [\n              179.9,\n              75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b15a001e4b092d9651e228c","contributors":{"authors":[{"text":"Moore, Thomas E. 0000-0002-0878-0457 tmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-0878-0457","contributorId":1033,"corporation":false,"usgs":true,"family":"Moore","given":"Thomas","email":"tmoore@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":736649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":736650,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roeske, S. M.","contributorId":96865,"corporation":false,"usgs":false,"family":"Roeske","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":736651,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":19355,"text":"ofr93481 - 1994 - Five computer programs for testing weighted residuals and calculating linear confidence and prediction intervals on results from the ground-water parameter-estimation computer program MODFLOWP","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr93481","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-481","title":"Five computer programs for testing weighted residuals and calculating linear confidence and prediction intervals on results from the ground-water parameter-estimation computer program MODFLOWP","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr93481","usgsCitation":"Hill, M.C., 1994, Five computer programs for testing weighted residuals and calculating linear confidence and prediction intervals on results from the ground-water parameter-estimation computer program MODFLOWP: U.S. Geological Survey Open-File Report 93-481, iv, 81 p. :ill. ;28 cm., https://doi.org/10.3133/ofr93481.","productDescription":"iv, 81 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151711,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0481/report-thumb.jpg"},{"id":48831,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0481/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef367","contributors":{"authors":[{"text":"Hill, M. C.","contributorId":48993,"corporation":false,"usgs":true,"family":"Hill","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":180736,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70182170,"text":"70182170 - 1994 - Age, habitat and tide effects on feeding activity of Emperor Geese during Autumn migration","interactions":[],"lastModifiedDate":"2017-02-17T15:02:51","indexId":"70182170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Age, habitat and tide effects on feeding activity of Emperor Geese during Autumn migration","docAbstract":"<p><span>I studied feeding activity of Emperor Geese (<i>Chen canagica</i>) on the Alaska Peninsula during autumn migration, 1991. Scan samples were used to estimate the proportion of birds feeding in flocks as a measure of feeding intensity. Most geese fed during low tides and roosted during high tides. However, flocks with disproportionately more juveniles continued to feed during high tides in either blue mussel (<i>Mytilus edulis</i>) beds (during relatively low high tides) or in vegetated habitats. Feeding intensity was higher in mussel habitats than in mud/sand or vegetated habitats, and juveniles fed more than adults. Juvenile geese probably have greater nutritional needs than adults, and feeding during high tide may represent their attempt to satisfy these disproportionate demands. Vegetated habitats may be used when high value bivalve prey are unavailable due to tidal inundation.</span></p>","language":"English","publisher":"Cooper Ornithological Society","doi":"10.2307/1369062","usgsCitation":"Schmutz, J.A., 1994, Age, habitat and tide effects on feeding activity of Emperor Geese during Autumn migration: The Condor, v. 96, no. 1, p. 46-51, https://doi.org/10.2307/1369062.","productDescription":"6 p.","startPage":"46","endPage":"51","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":503115,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/condor/vol96/iss1/5","text":"External Repository"},{"id":335821,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula","volume":"96","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a819b9e4b025c46429afd6","contributors":{"authors":[{"text":"Schmutz, Joel A. 0000-0002-6516-0836 jschmutz@usgs.gov","orcid":"https://orcid.org/0000-0002-6516-0836","contributorId":1805,"corporation":false,"usgs":true,"family":"Schmutz","given":"Joel","email":"jschmutz@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":669862,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5319,"text":"fs03295 - 1994 - United States Geological Survey, programs in New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"fs03295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"032-95","title":"United States Geological Survey, programs in New York","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs03295","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1994, United States Geological Survey, programs in New York: U.S. Geological Survey Fact Sheet 032-95, [4] p. : ill., map ; 28 cm. ill., map ;, https://doi.org/10.3133/fs03295.","productDescription":"[4] p. : ill., map ; 28 cm. ill., map ;","costCenters":[],"links":[{"id":329,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/wid/html/ny.html","linkFileType":{"id":5,"text":"html"}},{"id":121404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0032/report-thumb.jpg"},{"id":32018,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0032/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60f037","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":528486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17058,"text":"ofr94229B - 1994 - Digital bedrock geologic map of the Mount Holly and Ludlow quadrangles, Vermont: Database","interactions":[],"lastModifiedDate":"2023-11-20T21:57:11.031079","indexId":"ofr94229B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-229","chapter":"B","title":"Digital bedrock geologic map of the Mount Holly and Ludlow quadrangles, Vermont: Database","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94229B","collaboration":"The USGS does not support this software or answer technical questions for the software associated with the publication.","usgsCitation":"Walsh, G.J., Ratcliffe, N.M., Dudley, J.B., and Merrifield, T., 1994, Digital bedrock geologic map of the Mount Holly and Ludlow quadrangles, Vermont: Database: U.S. Geological Survey Open-File Report 94-229, 2 Computer Disks, https://doi.org/10.3133/ofr94229B.","productDescription":"2 Computer Disks","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":277768,"rank":2,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1994/0229b/application.zip","linkFileType":{"id":6,"text":"zip"}},{"id":149641,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108219,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12480.htm","linkFileType":{"id":5,"text":"html"},"description":"12480"}],"country":"United States","state":"Vermont","otherGeospatial":"Mount Holly and Ludlow quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.875,\n              43.5\n            ],\n            [\n              -72.875,\n              43.375\n            ],\n            [\n              -72.625,\n              43.375\n            ],\n            [\n              -72.625,\n              43.5\n            ],\n            [\n              -72.875,\n              43.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b462a","contributors":{"authors":[{"text":"Walsh, Gregory J. 0000-0003-4264-8836 gwalsh@usgs.gov","orcid":"https://orcid.org/0000-0003-4264-8836","contributorId":873,"corporation":false,"usgs":true,"family":"Walsh","given":"Gregory","email":"gwalsh@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":174766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ratcliffe, Nicholas M. 0000-0002-7922-5784 nratclif@usgs.gov","orcid":"https://orcid.org/0000-0002-7922-5784","contributorId":4167,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"Nicholas","email":"nratclif@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":174767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dudley, John B.","contributorId":21175,"corporation":false,"usgs":true,"family":"Dudley","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":174768,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Merrifield, Thomas","contributorId":42982,"corporation":false,"usgs":true,"family":"Merrifield","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":174769,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29158,"text":"wri934141 - 1994 - Water resources of Hot Springs County, Wyoming","interactions":[],"lastModifiedDate":"2017-12-14T09:17:42","indexId":"wri934141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4141","title":"Water resources of Hot Springs County, Wyoming","docAbstract":"<p>The wells and springs inventoried in Hot Springs County most commonly had been completed in or issued from the Quaternary alluvium, Quaternary terrace deposits, Fort Union and Mesaverde Formations, Cody Shale, and the Frontier and Chugwater Formations. The largest discharges measured were from the Quaternary terrace deposits (400 gallons per minute) and the Phosphoria Formation (1,000 gallons per minute). Discharges from all other geologic units varied, but most wells and springs yielded 50 gallons per minute or less.</p><p>Water-quality samples collected from springs that issued from the Absaroka Volcanic Supergroup, the Bighorn Dolomite, and the Flathead Sandstone had the lowest dissolved-solids concentrations, which ranged from 58 to 265 milligrams per liter, and the least variable water types. Water from the volcanic rocks was a sodium bicarbonate type; whereas, water from the Flathead Sandstone was a calcium bicarbonate type. Water types for all the other aquifers varied from sampling site to sampling site; however, water samples from the Fort Union Formation and the Cody Shale were consistently of the sodium sulfate type. </p><p>The effect of oil- and gas-development at Hamilton Dome on thermal spring discharges at Hot Springs State Park near Thermopolis was studied. The estimated drawdown from 1918, when the Hamilton Dome oil field was discovered, to 1988 was made using drill-stem data from previous studies. Drawdown at Big Spring in the Park was estimated to be less than 3 feet on the basis of recent oil- and water-production data, previous modeling studies, and the estimated water-level drawdown of 330 feet in wells at the Hamilton Dome oil field.</p><p>Streams originating in the Plains region of the county, such as Middle Fork Owl Creek, are ephemeral or intermittent; whereas, streams originating in the mountains, such as Gooseberry Creek, are perennial. Average annual runoff across the county ranges from 0.26 inches at a representative streamflow-gaging station near Worland in the plains region to 5.4 inches in the Owl Creek Mountains and southeastern Absaroka Range.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934141","usgsCitation":"Plafcan, M., and Ogle, K.M., 1994, Water resources of Hot Springs County, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 93-4141, Report: v, 90 p.; 2 Plates: 16.50 x 26.44 inches and 25.78 x 17.71 inches, https://doi.org/10.3133/wri934141.","productDescription":"Report: v, 90 p.; 2 Plates: 16.50 x 26.44 inches and 25.78 x 17.71 inches","costCenters":[],"links":[{"id":349978,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4141/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58034,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4141/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58035,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4141/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4141/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Hot Springs County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {\n        \"stroke\": \"#555555\",\n        \"stroke-width\": 2,\n        \"stroke-opacity\": 1,\n        \"fill\": \"#555555\",\n        \"fill-opacity\": 0.5\n      },\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.36065673828125,\n              43.42898792344155\n            ],\n            [\n              -107.61383056640625,\n              43.42898792344155\n            ],\n            [\n              -107.61383056640625,\n              44.10336537791152\n            ],\n            [\n              -109.36065673828125,\n              44.10336537791152\n            ],\n            [\n              -109.36065673828125,\n              43.42898792344155\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ac70","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":201050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ogle, Kathy Muller","contributorId":8896,"corporation":false,"usgs":true,"family":"Ogle","given":"Kathy","email":"","middleInitial":"Muller","affiliations":[],"preferred":false,"id":201051,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5287,"text":"fs04995 - 1994 - United States Geological Survey, programs in Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"fs04995","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"049-95","title":"United States Geological Survey, programs in Wisconsin","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs04995","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1994, United States Geological Survey, programs in Wisconsin: U.S. Geological Survey Fact Sheet 049-95, 4 p. : ill., map ; 28 cm. ill., map ;, https://doi.org/10.3133/fs04995.","productDescription":"4 p. : ill., map ; 28 cm. ill., map ;","numberOfPages":"4","costCenters":[],"links":[{"id":268,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/wid/html/wi.html","linkFileType":{"id":5,"text":"html"}},{"id":117796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0049/report-thumb.jpg"},{"id":31990,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eef4","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":528457,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29170,"text":"wri944169 - 1994 - An interactive code (NETPATH) for modeling NET geochemical reactions along a flow PATH, version 2.0","interactions":[],"lastModifiedDate":"2020-04-12T14:27:07.34098","indexId":"wri944169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4169","title":"An interactive code (NETPATH) for modeling NET geochemical reactions along a flow PATH, version 2.0","docAbstract":"NETPATH is an interactive Fortran 77 computer program used to interpret net geochemical mass-balance reactions between an initial and final water along a hydrologic flow path. Alternatively, NETPATH computes the mixing proportions of two to five initial waters and net geochemical reactions that can account for the observed composition of a final water. The program utilizes previously defined chemical and isotopic data for waters from a hydrochemical system. For a set of mineral and (or) gas phases hypothesized to be the reactive phases in the system, NETPATH calculates the mass transfers in every possible combination of the selected phases that accounts for the observed changes in the selected chemical and (or) isotopic compositions observed along the flow path. The calculations are of use in interpreting geochemical reactions, mixing proportions, evaporation and (or) dilution of waters, and mineral mass transfer in the chemical and isotopic evolution of natural and environmental waters. Rayleigh distillation calculations are applied to each mass-balance model that satisfies the constraints to predict carbon, sulfur, nitrogen, and strontium isotopic compositions at the end point, including radiocarbon dating. DB is an interactive Fortran 77 computer program used to enter analytical data into NETPATH, and calculate the distribution of species in aqueous solution. This report describes the types of problems that can be solved, the methods used to solve problems, and the features available in the program to facilitate these solutions. Examples are presented to demonstrate most of the applications and features of NETPATH. The codes DB and NETPATH can be executed in the UNIX or DOS1 environment. This report replaces U.S. Geological Survey Water-Resources Investigations Report 91-4078, by Plummer and others, which described the original release of NETPATH, version 1.0 (dated December, 1991), and documents revisions and enhancements that are included in version 2.0.  1 The use of trade, brand or product names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944169","usgsCitation":"Plummer, N., Prestemon, E.C., and Parkhurst, D.L., 1994, An interactive code (NETPATH) for modeling NET geochemical reactions along a flow PATH, version 2.0 (Version 2.0): U.S. Geological Survey Water-Resources Investigations Report 94-4169, iv, 130 p. , https://doi.org/10.3133/wri944169.","productDescription":"iv, 130 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":124969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4169/report-thumb.jpg"},{"id":58044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4169/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 2.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684566","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":201073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prestemon, Eric C.","contributorId":45352,"corporation":false,"usgs":true,"family":"Prestemon","given":"Eric","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parkhurst, David L. 0000-0003-3348-1544 dlpark@usgs.gov","orcid":"https://orcid.org/0000-0003-3348-1544","contributorId":1088,"corporation":false,"usgs":true,"family":"Parkhurst","given":"David","email":"dlpark@usgs.gov","middleInitial":"L.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":201072,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61756,"text":"gq1751 - 1994 - Geologic map of the Giant Forest quadrangle, Tulare County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:33","indexId":"gq1751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1751","title":"Geologic map of the Giant Forest quadrangle, Tulare County, California","language":"ENGLISH","doi":"10.3133/gq1751","usgsCitation":"Sisson, T.W., and Moore, J., 1994, Geologic map of the Giant Forest quadrangle, Tulare County, California: U.S. Geological Survey Geologic Quadrangle 1751, 1 map :col. ;45 x 36 cm., on sheet 64 x 102 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1751.","productDescription":"1 map :col. ;45 x 36 cm., on sheet 64 x 102 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102061,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_476.htm","linkFileType":{"id":5,"text":"html"},"description":"476"},{"id":248053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1751/report.pdf","size":"70","linkFileType":{"id":1,"text":"pdf"}},{"id":252713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1751/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119,36.5 ], [ -119,36.75 ], [ -118.75,36.75 ], [ -118.75,36.5 ], [ -119,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635d99","contributors":{"authors":[{"text":"Sisson, Thomas W. 0000-0003-3380-6425 tsisson@usgs.gov","orcid":"https://orcid.org/0000-0003-3380-6425","contributorId":2341,"corporation":false,"usgs":true,"family":"Sisson","given":"Thomas","email":"tsisson@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":266328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, James Gregory","contributorId":73622,"corporation":false,"usgs":true,"family":"Moore","given":"James Gregory","affiliations":[],"preferred":false,"id":266329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26727,"text":"wri924083 - 1994 - Ground-water quality in the central part of the Passaic River basin, northeastern New Jersey, 1959-88","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri924083","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"92-4083","title":"Ground-water quality in the central part of the Passaic River basin, northeastern New Jersey, 1959-88","docAbstract":"Ground-water samples were collected from 71 wells screened in or open to three aquifers in the central part of the Passaic River basin during 1959-88. Water samples from aquifers in glacial sediments and aquifers in sedimentary and igneous bedrock of the Newark  Supergroup were analyzed for major ions. Most samples were analyzed for metals, nutrients, and tritium; 38 samples were analyzed for purgeable organic compounds. Calcium and bicarbonate were the predominant ions in ground water in the study area. Ground water was dilute (median dissolved-solids concentration 239 milligrams per liter) and slightly basic (median pH 7.89). Concentrations of inorganic constituents were within U.S. Environmental Protection Agency (USEPA) primary drinking-water regulations. Concentrations of benzene, tetrachloroethylene, and  trichloroethylene, however, were greater than USEPA primary drinking-water regulations in six samples. Ground-water samples from aquifers in sedimentary bedrock were enriched in barium, calcium, magnesium, strontium,and sulfate relative to samples form the other aquifers. Such ion enrichment can be attributed either to disolution of carbonate and sulfate-containing minerals or to human activities. Ground-water samples from two wells screened in glacial sediments near swamps contained sulfate in concentrations higher than the median for the aquifer. Sulfate enrichment could result from downward leaching of water enriched in sulfur from the decay of organic matter in the swamps, from the disolution of sulfate-containing minerals, or from human activities. No regional trends in the chemical composition of the ground water in the study area were identified. Sulfate concentrations in ground- water samples from the sedimentary bedrock tended to increase with decreasing altitude of the deepest opening of the well; the correlation coefficient for the ranks of sulfate  concentration and the altitude of the deepest opening of the well for 17 pairs of data is -0.690. Concentrations of tritium were greater than the detection limit in 33 of 35 ground-water samples, indicating that most ground water in the study area is more recent than 1953.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924083","usgsCitation":"Czarnik, T., and Kozinski, J., 1994, Ground-water quality in the central part of the Passaic River basin, northeastern New Jersey, 1959-88: U.S. Geological Survey Water-Resources Investigations Report 92-4083, vi, 66 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924083.","productDescription":"vi, 66 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4083/report-thumb.jpg"},{"id":55602,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4083/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db6556ad","contributors":{"authors":[{"text":"Czarnik, T.S.","contributorId":89178,"corporation":false,"usgs":true,"family":"Czarnik","given":"T.S.","email":"","affiliations":[],"preferred":false,"id":196897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kozinski, Jane","contributorId":59836,"corporation":false,"usgs":true,"family":"Kozinski","given":"Jane","email":"","affiliations":[],"preferred":false,"id":196896,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5311,"text":"fs02295 - 1994 - United States Geological Survey, programs in Michigan","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"fs02295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"022-95","title":"United States Geological Survey, programs in Michigan","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs02295","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1994, United States Geological Survey, programs in Michigan: U.S. Geological Survey Fact Sheet 022-95, 4 p. : ill. ; 28 cm. ill. ;, https://doi.org/10.3133/fs02295.","productDescription":"4 p. : ill. ; 28 cm. ill. ;","costCenters":[],"links":[{"id":321,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/wid/html/mi.html","linkFileType":{"id":5,"text":"html"}},{"id":117015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0022/report-thumb.jpg"},{"id":32010,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60f184","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":528478,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29216,"text":"wri944160 - 1994 - Estimates of percolation rates and ages of water in unsaturated sediments at two Mojave Desert sites, California-Nevada","interactions":[],"lastModifiedDate":"2019-12-08T13:32:24","indexId":"wri944160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4160","title":"Estimates of percolation rates and ages of water in unsaturated sediments at two Mojave Desert sites, California-Nevada","docAbstract":"<p>Thick unsaturated zones in arid regions increasingly are being sought for the burial of radioactive and other hazardous wastes. Estimating percolation rates of water from precipitation at proposed burial sites is important for site assessment. Chloride profiles in unsaturated sediments are used to show differences and similarities in the rates of percolation at two sites in the Mojave Desert of southern Nevada and southeastern California; the first is an existing burial site for low-level radioactive waste in the Amargosa Desert, and the second is a proposed waste-burial site in Ward Valley. The Mojave Desert is one of the most arid regions of the United States.</p><p>Chloride concentrations in pore water of unsaturated sediments peak between depths of 2 and 3 meters at both the Amargosa Desert and Ward Valley, sites; maximum chloride concentration is 9,000 milligrams per liter at the Amargosa Desert site and 15,000 milligrams per liter at the Ward Valley, site. Below a depth of 10 meters, however, chloride concentrations at the Amargosa Desert site decrease to less than 50 milligrams per liter, whereas concentrations at the Ward Valley site are greater than 2,300 milligrams per liter. Estimated age of water at a depth of 10 meters at both sites is between 16,000 and 33,000 years. Below a depth of 10 meters, estimated age of water in the sediments at the Ward Valley site is considerably older than at the Amargosa Desert site because of the greater chloride concentrations at the Ward Valley site.</p><p>The dilute chloride concentrations in the pore water below a depth of 10 meters at the Amargosa Desert site could indicate that the sediments were flushed with water in the past. The climate in the region was wetter and cooler from about 30,000 to 18,000 years ago. Perhaps increased precipitation or more frequent flooding of the Amargosa River resulted in deep percolation at the site. Downward percolation of water since that time seems limited to the upper 10 meters.</p><p>The downward percolation rate of water below a depth of 10 meters at the Amargosa Desert site, as estimated from chloride concentrations, is 0.2 centimeters per year; however, the rate is not representative of present conditions as measured water-potential and vapor-density, gradients indicate upward water flow. The rate may be representative of a period during the Pleistocene when the climate was wetter and cooler. Estimated percolation rates below a depth of 10 meters at the Ward Valley site are on the order of 3 to 5 centimeters per 1,000 years, also reflecting flow conditions during the Pleistocene.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Carson City, NV","doi":"10.3133/wri944160","usgsCitation":"Prudic, D.E., 1994, Estimates of percolation rates and ages of water in unsaturated sediments at two Mojave Desert sites, California-Nevada: U.S. Geological Survey Water-Resources Investigations Report 94-4160, iv, 19 p., https://doi.org/10.3133/wri944160.","productDescription":"iv, 19 p.","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":125019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4160/report-thumb.jpg"},{"id":58072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada","otherGeospatial":"Amargosa  Desert, Mojave Desert, Ward 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,{"id":5301,"text":"fs00995 - 1994 - United States Geological Survey, programs in Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"fs00995","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"009-95","title":"United States Geological Survey, programs in Florida","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs00995","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1994, United States Geological Survey, programs in Florida: U.S. Geological Survey Fact Sheet 009-95, [4] p. : ill., map ; 28 cm. ill., map ;, https://doi.org/10.3133/fs00995.","productDescription":"[4] p. : ill., map ; 28 cm. ill., map ;","costCenters":[],"links":[{"id":275,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/wid/html/fl.html","linkFileType":{"id":5,"text":"html"}},{"id":121275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0009/report-thumb.jpg"},{"id":32000,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f570","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":528468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61855,"text":"gq1749 - 1994 - Geologic map of the Los Pinos quadrangle, Rio Arriba and Taos Counties, New Mexico, and Conejos County, Colorado","interactions":[],"lastModifiedDate":"2022-02-01T21:22:18.030506","indexId":"gq1749","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1749","title":"Geologic map of the Los Pinos quadrangle, Rio Arriba and Taos Counties, New Mexico, and Conejos County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq1749","usgsCitation":"Thompson, R.A., and Lipman, P.W., 1994, Geologic map of the Los Pinos quadrangle, Rio Arriba and Taos Counties, New Mexico, and Conejos County, Colorado: U.S. Geological Survey Geologic Quadrangle 1749, Report: 2 p.; Plate, https://doi.org/10.3133/gq1749.","productDescription":"Report: 2 p.; Plate","costCenters":[],"links":[{"id":102784,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1234.htm","linkFileType":{"id":5,"text":"html"},"description":"1234"},{"id":252888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1749/report-thumb.jpg"},{"id":248145,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1749/report.pdf","size":"71","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Colorado, New Mexico","county":"Conejos County, Rio Arriba County, Taos County","otherGeospatial":"Los Pinos quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.125,36.875 ], [ -106.125,37 ], [ -106,37 ], [ -106,36.875 ], [ -106.125,36.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d16","contributors":{"authors":[{"text":"Thompson, Ren A. 0000-0002-3044-3043 rathomps@usgs.gov","orcid":"https://orcid.org/0000-0002-3044-3043","contributorId":1265,"corporation":false,"usgs":true,"family":"Thompson","given":"Ren","email":"rathomps@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":266458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":266459,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47168,"text":"ofr88628 - 1994 - Geologic map of the Deer Creek Church Quadrangle, Dawson County, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:04:58","indexId":"ofr88628","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-628","title":"Geologic map of the Deer Creek Church Quadrangle, Dawson County, Montana","language":"ENGLISH","doi":"10.3133/ofr88628","usgsCitation":"Colton, R.B., McGraw, J.P., and Durst, S., 1994, Geologic map of the Deer Creek Church Quadrangle, Dawson County, Montana: U.S. Geological Survey Open-File Report 88-628, 1 map :photocopy ;58 x 40 cm., on sheet 77 x 61 cm., folded to 24 x 19 cm., https://doi.org/10.3133/ofr88628.","productDescription":"1 map :photocopy ;58 x 40 cm., on sheet 77 x 61 cm., folded to 24 x 19 cm.","costCenters":[],"links":[{"id":108768,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17511.htm","linkFileType":{"id":5,"text":"html"},"description":"17511"},{"id":135766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84160,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0628/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b877","contributors":{"authors":[{"text":"Colton, Roger B.","contributorId":17967,"corporation":false,"usgs":true,"family":"Colton","given":"Roger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":234742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGraw, J. P.","contributorId":68283,"corporation":false,"usgs":true,"family":"McGraw","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":234743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Durst, S.L.","contributorId":6788,"corporation":false,"usgs":true,"family":"Durst","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":234741,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":65085,"text":"i2357 - 1994 - Geologic map of science study area 4, Chasma Boreale Region of Mars","interactions":[],"lastModifiedDate":"2023-07-06T10:53:25.801243","indexId":"i2357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"2357","title":"Geologic map of science study area 4, Chasma Boreale Region of Mars","docAbstract":"<p><span data-contrast=\"auto\">This map is one is a series of 1:500,000 scale maps initiated by the National Aeronautics and Space Administration to investigate Science Study Areas (selected area of scientific interest) on Mars (fig. 1). The Chasma Boreale region merits detailed geologic study because it contains parts of (1) the north polar ice cap, which is composed of water ice with lesser amounts of carbon dioxide; (2) the layered terrain that recorded climatic and atmospheric changes on Mars during the Amazonian Period; and (3) the enigmatic low-lying polygonal patterned terrain.</span><span data-ccp-props=\"{&quot;201341983&quot;:0,&quot;335559739&quot;:160,&quot;335559740&quot;:259}\">&nbsp;</span></p><p><span data-contrast=\"auto\">The map was compiled on a composite of three 1:500,000-scale photomosaic bases (U.S. Geological Survey, 1986a, b, c), each of which is the summer scene of a two-sheet set that includes a spring scene. (Summer scenes, acquired when the north polar ice cap is smallest, show the greatest extent of underlying materials. However, spring scenes that show more detail in specific areas were also used.) Map units (including crater materials) and contacts are generally consistent with those of Howard and others (1982), Dial (1984), and Tanaka and Scott (1987) except where revised on the basis of higher resolution Viking images. Several Viking images were computer enhanced for our mapping.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2357","usgsCitation":"Dial, A.L., and Dohm, J.M., 1994, Geologic map of science study area 4, Chasma Boreale Region of Mars: U.S. Geological Survey IMAP 2357, 1 Plate: 74.67 × 56.00 inches, https://doi.org/10.3133/i2357.","productDescription":"1 Plate: 74.67 × 56.00 inches","costCenters":[],"links":[{"id":189709,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100818,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2357/plate-1.pdf","size":"15262","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6fe","contributors":{"authors":[{"text":"Dial, A. L. Jr.","contributorId":74458,"corporation":false,"usgs":true,"family":"Dial","given":"A.","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":272636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dohm, J. M.","contributorId":102150,"corporation":false,"usgs":true,"family":"Dohm","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":272637,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61768,"text":"gq1739 - 1994 - Geologic map of the Bluemont quadrangle, Loudoun and Clarke Counties, Virginia","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"gq1739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1739","title":"Geologic map of the Bluemont quadrangle, Loudoun and Clarke Counties, Virginia","language":"ENGLISH","doi":"10.3133/gq1739","usgsCitation":"Southworth, S., 1994, Geologic map of the Bluemont quadrangle, Loudoun and Clarke Counties, Virginia: U.S. Geological Survey Geologic Quadrangle 1739, 1 map :col. ;58 x 45 cm., on sheet 104 x 137 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1739.","productDescription":"1 map :col. ;58 x 45 cm., on sheet 104 x 137 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102781,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1231.htm","linkFileType":{"id":5,"text":"html"},"description":"1231"},{"id":248063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1739/report.pdf","size":"72","linkFileType":{"id":1,"text":"pdf"}},{"id":252723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1739/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.86749999999999,39 ], [ -77.86749999999999,39.6175 ], [ -77.75,39.6175 ], [ -77.75,39 ], [ -77.86749999999999,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69dd1a","contributors":{"authors":[{"text":"Southworth, Scott","contributorId":93933,"corporation":false,"usgs":true,"family":"Southworth","given":"Scott","affiliations":[],"preferred":false,"id":266344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29082,"text":"wri934232 - 1994 - Sources and transport of sediment, nutrients, and oxygen-demanding substances in the Minnesota River basin, 1989-92","interactions":[],"lastModifiedDate":"2018-03-19T10:47:07","indexId":"wri934232","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4232","title":"Sources and transport of sediment, nutrients, and oxygen-demanding substances in the Minnesota River basin, 1989-92","docAbstract":"<p>The Minnesota River, 10 major tributaries, and 21 springs were sampled to determine the sources and transport of sediment, nutrients, and oxygen- demanding substances. The study was part of a four-year assessment of non-point source pollution in the Minnesota River Basin. Runoff from tributary watersheds was identified as the primary source of suspended sediment and nutrients in the Minnesota River mainstem. Suspended-sediment, phosphorus, and nitrate concentrations were elevated in all major tributaries during runoff, but tributaries in the south-central and eastern part of the basin produce the highest annual loading to the mainstem because of higher annual precipitation and runoff in that part of the basin. Particle-size analyses showed that most of the suspended sediment in transport consisted of silt- and clay-size material. Phosphorus enrichment was indicated throughout the mainstem by total phosphorus concentrations that ranged from 0.04 to 0.48 mg/L with a median value of 0.22 mg/L, and an interquartile range of 0.15 to 0.29 mg/L. Nitrate concentrations periodically exceeded drinking water standards in tributaries draining the south-central and eastern part of the basin. Oxygen demand was most elevated during periods of summer low flow. Correlations between levels of biochemical oxygen demand and levels of algal productivity suggest that algal biomass comprises much of the oxygen-demanding material in the mainstem. Transport of sediment, nutrients, and organic carbon within the mainstem was found to be conservative, with nearly all tributary inputs being transported downstream. Uptake and utilization of nitrate and orthophosphorus was indicated during low flow, but at normal and high flow, inputs of these constituents greatly exceeded biological utilization.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri934232","collaboration":"Prepared in cooperation with the Minnesota Pollution Control Agency and the Legislative Commission on Minnesota Resources","usgsCitation":"Payne, G.A., 1994, Sources and transport of sediment, nutrients, and oxygen-demanding substances in the Minnesota River basin, 1989-92: U.S. Geological Survey Water-Resources Investigations Report 93-4232, vii, 71 p., https://doi.org/10.3133/wri934232.","productDescription":"vii, 71 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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