This map is part of a folio of maps of the Lewiston 1° x 2° quadrangle, Maine, New Hampshire, and Vermont, and part of the Sherbrooke 1° x 2° quadrangle, Maine, New Hampshire, and Vermont, United States, and Quebec, Canada, prepared under the Conterminous United States Mineral Assessment Program (CUSMAP). Adjacent areas in Quebec are shown, in order to illustrate the geologic continuity between northwestern Maine and northern Vermont and New Hampshire. Other results of the project are contained in reports by Nowlan and others (1990a,b,c; stream sediment geochemistry), and Cox (1990; potential tin resources related to the White Mountain Plutonic-Volcanic Suite), Bothner and others (in press; complete Bouguer gravity and aeromagnetic maps), Moench and Boudette (in press, geologic synthesis and mineral occurrence map), and Moench (in press; metallic mineral resources).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1898D","usgsCitation":"Moench, R.H., Boone, G., Bothner, W.A., Boudette, E., Hatch, N.L., Hussey, A.M., and Marvinney, R., 1995, Geologic map of the Sherbrooke-Lewiston area, Maine, New Hampshire, and Vermont, United States, and Quebec, Canada: U.S. Geological Survey IMAP 1898, Report: 56 p.; 2 Plates: 56.8 x 41.5 inches and 47.56 x 31.00 inches, https://doi.org/10.3133/i1898D.","productDescription":"Report: 56 p.; 2 Plates: 56.8 x 41.5 inches and 47.56 x 31.00 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":260890,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1898d/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":107171,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9989.htm","linkFileType":{"id":5,"text":"html"},"description":"9989"},{"id":187750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i1898D.jpg"},{"id":260891,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1898d/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":308522,"rank":901,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1898d/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"Canada, United States","state":"Maine, New Hampshire, Vermont, Quebec","otherGeospatial":"Sherbrooke-Lewiston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72,44 ], [ -72,46 ], [ -70,46 ], [ -70,44 ], [ -72,44 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68bb01","contributors":{"authors":[{"text":"Moench, R. H.","contributorId":8853,"corporation":false,"usgs":true,"family":"Moench","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":276318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boone, G.M.","contributorId":52179,"corporation":false,"usgs":true,"family":"Boone","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":276320,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bothner, Wallace A.","contributorId":80270,"corporation":false,"usgs":true,"family":"Bothner","given":"Wallace","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":276323,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boudette, E. L.","contributorId":77150,"corporation":false,"usgs":true,"family":"Boudette","given":"E. L.","affiliations":[],"preferred":false,"id":276322,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hatch, N. L. Jr.","contributorId":58663,"corporation":false,"usgs":true,"family":"Hatch","given":"N.","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":276321,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hussey, A. M. III","contributorId":85663,"corporation":false,"usgs":true,"family":"Hussey","given":"A.","suffix":"III","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":276324,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Marvinney, R.G.","contributorId":26023,"corporation":false,"usgs":true,"family":"Marvinney","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":276319,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":29218,"text":"wri954174 - 1995 - Results of hypothetical ground-water pumping in Carson Valley, a river-dominated basin in Douglas County, Nevada, and Alpine County, California","interactions":[],"lastModifiedDate":"2019-11-14T12:52:18","indexId":"wri954174","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"95-4174","title":"Results of hypothetical ground-water pumping in Carson Valley, a river-dominated basin in Douglas County, Nevada, and Alpine County, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri954174","usgsCitation":"Prudic, D.E., and Wood, J., 1995, Results of hypothetical ground-water pumping in Carson Valley, a river-dominated basin in Douglas County, Nevada, and Alpine County, California: U.S. Geological Survey Water-Resources Investigations Report 95-4174, iv, 29 p., https://doi.org/10.3133/wri954174.","productDescription":"iv, 29 p.","costCenters":[],"links":[{"id":369211,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4174/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4174/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","county":"Alpine County, Douglas County","otherGeospatial":"Carson Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.74411010742186,\n 38.688725613296725\n ],\n [\n -119.45846557617186,\n 38.688725613296725\n ],\n [\n -119.45846557617186,\n 39.12153746241925\n ],\n [\n -119.74411010742186,\n 39.12153746241925\n ],\n [\n -119.74411010742186,\n 38.688725613296725\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fa5f","contributors":{"authors":[{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":201162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, J.L.","contributorId":75958,"corporation":false,"usgs":true,"family":"Wood","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":201163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":22364,"text":"ofr95309 - 1995 - Estimated water withdrawals and use in Illinois, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:51","indexId":"ofr95309","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-309","title":"Estimated water withdrawals and use in Illinois, 1988","docAbstract":"The total amount of water withdrawn in Illinois during 1988 was about 18,756 million gallons per day (Mgal/d). About 1,170 Mgal/d, or 37 percent, of the total water withdrawn in Illinois, excluding withdrawals for thermoelectric-power generation, was ground water; about 1,998 Mgal/d of surface water was withdrawn and used, excluding withdrawals for thermoelectric-power generation. About 25 Mgal/d of the total ground water withdrawn was saline. Seventy-five percent of the total surface water, excluding withdrawals for thermoelectric-power generation, was withdrawn by public-supply facilities. Self-supplied industrial withdrawals were the next largest use of surface water. Thirty-nine percent of the total ground water was withdrawn by public-supply facilities. Irrigation was the next largest use of ground water. Sixty-two percent of the total water withdrawn, excluding thermoelectric withdrawals, in Illinois during 1988 was for public-supply facilities. Self-supplied withdrawals by industries and for irrigation were the next largest uses of water in Illinois during 1988.\r\nThe total water withdrawn for thermoelectric-power generation was about 15,589 Mgal/d. Water withdrawn and delivered from public-supply facilities in Illinois during 1988 totaled about 1,956 Mgal/d. Surface water and ground water were the sources for about 1,495 and 462 Mgal/d, respectively, of the withdrawals for public supply. The total water obtained from Lake Michigan for public-water supply was about 1,214 Mgal/d. About 122 Mgal/d was withdrawn for self-supplied domestic purposes. Total self-supplied withdrawals and deliveries from public-water facilities for commercial use were about 654 Mgal/d. About 159 Mgal/d was self-supplied by the commercial establishments. Total irrigation water withdrawals were about 302 Mgal/d. Although irrigated acreage in Illinois has increased from 265,036 acres in 1986 to 281,370 acres in 1988, the most significant factor for the increased irrigation water use was the drought conditions throughout the entire State. Total estimated livestock withdrawals were about 56 Mgal/d. Total self-supplied withdrawals and deliveries from public-supply facilities for industrial purposes were about 743 Mgal/d. About 480 Mgal/d was self-supplied withdrawals by industrial facilities. A total of about 94 Mgal/d was withdrawn during mining activities. A total of about 34 Mgal/d was withdrawn during mining from ground-water sources; about 25 Mgal/d of the ground water withdrawn was saline.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nMay be purchased from U.S. Geological Survey-ESIC, Open-File Reports Section,","doi":"10.3133/ofr95309","issn":"0094-9140","usgsCitation":"Avery, C., 1995, Estimated water withdrawals and use in Illinois, 1988: U.S. Geological Survey Open-File Report 95-309, iv, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95309.","productDescription":"iv, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0309/report-thumb.jpg"},{"id":51772,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0309/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc33","contributors":{"authors":[{"text":"Avery, C.F.","contributorId":67543,"corporation":false,"usgs":true,"family":"Avery","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":188107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18494,"text":"ofr95490 - 1995 - High-precision temperature logging at GISP2, Greenland, May 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr95490","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-490","title":"High-precision temperature logging at GISP2, Greenland, May 1992","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95490","usgsCitation":"Clow, G., Saltus, R.W., and Waddington, E., 1995, High-precision temperature logging at GISP2, Greenland, May 1992: U.S. Geological Survey Open-File Report 95-490, 24 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95490.","productDescription":"24 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0490/report-thumb.jpg"},{"id":19347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0490/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fb9c","contributors":{"authors":[{"text":"Clow, G.D.","contributorId":46112,"corporation":false,"usgs":true,"family":"Clow","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":179234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saltus, R. W.","contributorId":85588,"corporation":false,"usgs":true,"family":"Saltus","given":"R.","middleInitial":"W.","affiliations":[],"preferred":false,"id":179235,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waddington, E.D.","contributorId":36161,"corporation":false,"usgs":true,"family":"Waddington","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":179233,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19863,"text":"ofr95351 - 1995 - Selected hydrologic data for urban watersheds in South Carolina, 1983-90","interactions":[],"lastModifiedDate":"2017-01-04T12:43:06","indexId":"ofr95351","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-351","title":"Selected hydrologic data for urban watersheds in South Carolina, 1983-90","docAbstract":"Rainfall and streamflow data were collected at 23 gaging stations located in urban watersheds in South Carolina from 1983-90. The site selection process and the instrumentation used to collect the data are described. A compilation of rainfall and streamflow data in graphic and tabular form for seven selected events at each gaging station are presented. A gaging-station description and a listing of certain streamflow and basin characteristics also are included.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95351","usgsCitation":"Logan, S., Eckenwiler, M., and Bohman, L.R., 1995, Selected hydrologic data for urban watersheds in South Carolina, 1983-90: U.S. Geological Survey Open-File Report 95-351, xviii, 434 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr95351.","productDescription":"xviii, 434 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":152748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0351/report-thumb.jpg"},{"id":49372,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0351/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Depth to water is 400 to 500 feet below land surface in the northern part of Rathdrum Prairie, 100 to 200 feet below land surface at the Idaho-Washington State line, and 0 to 250 feet below land surface in the Spokane area. Depth to water in the intermontane valleys in east-central Idaho is least (usually less than 50 feet) near streams and increases toward valley margins where mountain-front alluvial fans have formed. Depths to water shown in the Moscow-Lewiston-Grangeville area in Idaho are limited to point data at individual wells because most of the water levels measured were not representative of levels in the uppermost aquifer but of levels in deeper aquifers.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944087","usgsCitation":"Berenbrock, C.E., Bassick, M.D., Rogers, T.L., and Garcia, S.P., 1995, Depth to water, 1991, in the Rathdrum Prairie, Idaho; Spokane River valley, Washington; Moscow-Lewiston-Grangeville area, Idaho; and selected intermontane valleys, east-central Idaho: U.S. Geological Survey Water-Resources Investigations Report 94-4087, Report: 1 p.; 2 Plates: 30.06 x 27.02 inches and 24.84 x 35.03 inches, https://doi.org/10.3133/wri944087.","productDescription":"Report: 1 p.; 2 Plates: 30.06 x 27.02 inches and 24.84 x 35.03 inches","costCenters":[],"links":[{"id":411312,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47980.htm","linkFileType":{"id":5,"text":"html"}},{"id":258700,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4087/report-thumb.jpg"},{"id":258699,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":258698,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4087/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":258697,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115.13714126200279,\n 48.279709292533\n ],\n [\n -119,\n 48.279709292533\n ],\n [\n -119,\n 46.390549134745584\n ],\n [\n -115.13714126200279,\n 46.390549134745584\n ],\n [\n -115.13714126200279,\n 48.279709292533\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab1e4b07f02db66dea4","contributors":{"authors":[{"text":"Berenbrock, Charles E. ceberenb@usgs.gov","contributorId":857,"corporation":false,"usgs":true,"family":"Berenbrock","given":"Charles","email":"ceberenb@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":230301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bassick, M. 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B.","contributorId":74408,"corporation":false,"usgs":true,"family":"Kotlyar","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":181375,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludington, S. D.","contributorId":80682,"corporation":false,"usgs":true,"family":"Ludington","given":"S.","middleInitial":"D.","affiliations":[],"preferred":false,"id":181376,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mosier, D.L.","contributorId":21965,"corporation":false,"usgs":true,"family":"Mosier","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":181374,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":67491,"text":"i2499 - 1995 - Geologic map of the Ontonagon and part of the Wakefield 30' x 60' quadrangles, Michigan","interactions":[],"lastModifiedDate":"2012-02-10T00:11:31","indexId":"i2499","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"2499","subseriesTitle":"NONE","title":"Geologic map of the Ontonagon and part of the Wakefield 30' x 60' quadrangles, Michigan","language":"ENGLISH","doi":"10.3133/i2499","usgsCitation":"Cannon, W., Nicholson, S.W., Woodruff, L.G., Hedgman, C.A., and Schulz, K.J., 1995, Geologic map of the Ontonagon and part of the Wakefield 30' x 60' quadrangles, Michigan: U.S. Geological Survey IMAP 2499, 1 map :col. ;70 x 77 cm., on sheet 105 x 145 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2499.","productDescription":"1 map :col. ;70 x 77 cm., on sheet 105 x 145 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107442,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10301.htm","linkFileType":{"id":5,"text":"html"},"description":"10301"},{"id":186480,"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\": [ [ [ -90,46.3675 ], [ -90,47 ], [ -89,47 ], [ -89,46.3675 ], [ -90,46.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db692b35","contributors":{"authors":[{"text":"Cannon, W.F. 0000-0002-2699-8118","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":70382,"corporation":false,"usgs":true,"family":"Cannon","given":"W.F.","affiliations":[],"preferred":false,"id":276371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nicholson, S. W.","contributorId":79504,"corporation":false,"usgs":true,"family":"Nicholson","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":276373,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodruff, L. G.","contributorId":46999,"corporation":false,"usgs":true,"family":"Woodruff","given":"L.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":276370,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hedgman, C. A.","contributorId":82795,"corporation":false,"usgs":true,"family":"Hedgman","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":276374,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schulz, K. J.","contributorId":79131,"corporation":false,"usgs":true,"family":"Schulz","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":276372,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":28415,"text":"wri954156 - 1995 - Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona, 1992-93","interactions":[],"lastModifiedDate":"2019-08-26T10:17:46","indexId":"wri954156","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"95-4156","title":"Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona, 1992-93","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri954156","usgsCitation":"Littin, G.R., and Monroe, S.A., 1995, Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona, 1992-93: U.S. Geological Survey Water-Resources Investigations Report 95-4156, iv, 37 p., https://doi.org/10.3133/wri954156.","productDescription":"iv, 37 p.","costCenters":[],"links":[{"id":159282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4156/report-thumb.jpg"},{"id":366898,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4156/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","otherGeospatial":"Black Mesa","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.08781433105467,\n 34.37914588074335\n ],\n [\n -110.0665283203125,\n 34.37914588074335\n ],\n [\n -110.0665283203125,\n 34.412574601595\n ],\n [\n -110.08781433105467,\n 34.412574601595\n ],\n [\n -110.08781433105467,\n 34.37914588074335\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614a46","contributors":{"authors":[{"text":"Littin, G. R.","contributorId":95924,"corporation":false,"usgs":true,"family":"Littin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Monroe, S. A.","contributorId":90346,"corporation":false,"usgs":true,"family":"Monroe","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199756,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28245,"text":"wri934069 - 1995 - Hydrology and the effects of selected agricultural best-management practices in the Bald Eagle Creek watershed, York County, Pennsylvania, prior to and during nutrient management: Water-quality study for the Chesapeake Bay Program","interactions":[],"lastModifiedDate":"2023-04-13T20:41:43.614521","indexId":"wri934069","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"93-4069","title":"Hydrology and the effects of selected agricultural best-management practices in the Bald Eagle Creek watershed, York County, Pennsylvania, prior to and during nutrient management: Water-quality study for the Chesapeake Bay Program","docAbstract":"The U.S. Geological Survey, in cooperation with the Susquehanna River Basin Commission and the Pennsylvania Department of Environmental Resources, conducted a study as part of the U.S. Environmental Protection Agency's Chesapeake Bay Program to determine the effects of nutrient management of surface-water quality by reducing animal units in a 0.43-square-mile agricultural watershed in York County. The study was conducted primarily from October 1985 through September 1990 prior to and during the implementation of nutrient-management practices designed to reduce nutrient and sediment discharges. Intermittent sampling continued until August 1991.
The Bald Eagle Creek Basin is underlain by schist and quartzite. About 87 percent of the watershed is cropland and pasture. Nearly 33 percent of the cropland was planted in corn prior to nutrient management, whereas 22 percent of the cropland was planted in corn during the nutrient-management phase. The animal population was reduced by 49 percent during nutrient management. Average annual applications of nitrogen and phosphorus from manure to cropland were reduced by 3,940 pounds (39 percent) and 910 pounds (46 percent), respectively, during nutrient management. A total of 94,560 pounds of nitrogen (538 pounds per acre) and 26,400 pounds of phosphorus (150 pounds per acre) were applied to the cropland as commercial fertilizer and manure during the 5-year study.
Core samples from the top 4 feet of soil were collected prior to and during nutrient management and analyzed from concentrations of nitrogen and phosphorus. The average amount of nitrate nitrogen in the soil ranged from 36 to 135 pounds per acre, and soluble phosphorus ranged from 0.39 to 2.5 pounds per acre, prior to nutrient management. During nutrient management, nitrate nitrogen in the soil ranged from 21 to 291 pounds per acre and soluble phosphorus ranged from 0.73 to 1.7 pounds per acre. Precipitation was about 18 percent below normal and streamflow was about 35 percent below normal prior to nutrient management, whereas precipitation was 4 percent above normal and streamflow was 3 percent below normal during the first 2 years of nutrient management. Eighty-four percent of the 20.44 inches of streamflow was base flow prior to nutrient management and 54 percent of the 31.14 inches of streamflow was base flow during the first 2 years of the nutrient-management phase. About 31 percent of the measured precipitation during the first 4 years of the study was discharged as surface water; the remaining 69 percent was removed as evapotranspiration or remained in ground-water storage.
Median concentrations of total nitrogen and dissolved nitrate plus nitrite in base flow increased from 4.9 and 4.1 milligrams per liter as nitrogen, respectively, prior to nutrient management to 5.8 and 5.0 milligrams per liter, respectively, during nutrient management. Median concentrations of ammonia nitrogen and organic nitrogen did not change significantly in base flow. Median concentrations of total and dissolved phosphorus in base flow did not change significantly and were 0.05 and 0.03 milligrams per liter as phosphorus, respectively, prior to the management phase, and 0.05 and 0.04 milligrams per liter, respectively, during the management phase.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934069","usgsCitation":"Langland, M.J., and Fishel, D.K., 1995, Hydrology and the effects of selected agricultural best-management practices in the Bald Eagle Creek watershed, York County, Pennsylvania, prior to and during nutrient management: Water-quality study for the Chesapeake Bay Program: U.S. Geological Survey Water-Resources Investigations Report 93-4069, vii, 72 p., https://doi.org/10.3133/wri934069.","productDescription":"vii, 72 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":415733,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47791.htm","linkFileType":{"id":5,"text":"html"}},{"id":57072,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4069/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119030,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4069/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"York County","otherGeospatial":"Bald Eagle Creek watershed","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.4794,\n 39.7567\n ],\n [\n -76.4794,\n 39.7436\n ],\n [\n -76.4639,\n 39.7436\n ],\n [\n -76.4639,\n 39.7567\n ],\n [\n -76.4794,\n 39.7567\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e836","contributors":{"authors":[{"text":"Langland, Michael J. 0000-0002-8350-8779 langland@usgs.gov","orcid":"https://orcid.org/0000-0002-8350-8779","contributorId":2347,"corporation":false,"usgs":true,"family":"Langland","given":"Michael","email":"langland@usgs.gov","middleInitial":"J.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":199460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishel, David K.","contributorId":34967,"corporation":false,"usgs":true,"family":"Fishel","given":"David","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":199461,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28532,"text":"wri954186 - 1995 - Geology and hydrology of the Edwards Aquifer in the San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-16T15:35:48","indexId":"wri954186","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"95-4186","title":"Geology and hydrology of the Edwards Aquifer in the San Antonio area, Texas","docAbstract":"The Edwards aquifer, which is the sole source of water for the city of San Antonio, is one of the most permeable and productive carbonate aquifers in the United States. The aquifer is composed of extensively faulted, fractured, and cavernous limestone and dolomite of Early Cretaceous age lying within the Balcones fault zone a series of normal en echelon strike faults that separate the Edwards Plateau from the Gulf Coastal Plain in south Texas. Along segments of some faults, the entire thickness of the aquifer is displaced vertically, and these faults then act as barriers to downdip ground-water flow.
\nThe large porosity and exceptional permeability of the unconfined part of the Edwards aquifer result from the dissolution of limestone by circulating ground water and development of a cavernous network along fractures. The large porosity and permeability of the freshwater part of the confined Edwards aquifer result primarily from dedolomitization. The small permeability of the saline-water part of the confined aquifer is caused by the limited interconnection between the pores in the rock matrix and by the lack of substantial dissolution along fractures.
\nThe large transmissivity of the Edwards aquifer is indicated by the hundreds of highyielding wells, small hydraulic gradients, and large spring discharges. The determined transmissivity throughout most of the confined freshwater aquifer ranges from 430,000 to 2,200,000 feet squared per day; the determined transmissivity of the unconfined aquifer generally is less than 430,000 feet squared per day. Faulting causes the aquifer to be highly anisotropic, and simulation indicates anisotropy ratios ranging from 0.0:1 to 1:1.
\nThe ground-water-flow system of the Edwards aquifer includes several components. These include a catchment area on the Edwards Plateau where the unconfined aquifer receives direct recharge, an area of confining beds crossed by streams draining the Edwards Plateau, a major recharge area within the Balcones fault zone where streams lose flow directly into the unconfined Edwards aquifer, and the confined Edwards aquifer that consists of the freshwater and salinewater zones.
\nWater entering the Edwards aquifer in the Balcones fault zone moves downdip in a generally southeasterly direction into the confined parts of the aquifer. In the confined aquifer, flow is toward the east and northeast under low hydraulic gradients through fractured, highly transmissive limestone and ultimately discharges at large springs and wells. All of the base flow and some of the storm runoff of streams crossing the recharge area infiltrates to the unconfined aquifer. On the basis of streamflow losses, the average annual recharge for 1934-88 was 635,500 acre-feet.
\nFreshwater discharges from the Edwards aquifer primarily from wells, springs, and seeps. Beginning in 1968, annual discharge from the aquifer has consistently exceeded average annual recharge largely because of a doubling of well pumpage. However, total springflow also increased because of greater-than-average recharge during most years since the late 1960's.
\nThe total volume of circulating freshwater in the Edwards aquifer is about 45 million acrefeet. Long-term hydrographs at San Antonio indicate no net decline in ground-water levels during 1911-87; thus, there was no net loss of water from storage in the freshwater zone of the Edwards aquifer during that long-term period, assuming the San Antonio hydrograph represents the entire aquifer. However, short-term changes in water levels result largely from the variability of precipitation as indicated by severe declines during the drought of the late 1940's to middle 1950's and by rises to record highs during the abnormally wet years in the 1970's and 1980's.
\nThe principal components of the groundwater budget (recharge, springflow, and pumpage) have varied greatly over 55 years (1934-88) of pertinent hydrologic records. Annual recharge varied from about 44,000 to 2,000,000 acre-feet. Annual springflow varied from about 70,000 acrefeet to about 580,000 acre-feet. Pumpage increased from about 100,000 acre-feet annually in the early 1930's to more than 500,000 acre-feet annually during some years in the 1980's. However, the average annual recharge of 635,500 acrefeet is about equal to the sum of the average annual springflow (359,500 acre-feet) and average annual pumpage (273,000 acre-feet), indicating no longterm decrease in ground-water storage because of springflow and pumpage.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri954186","collaboration":"Prepared in cooperation with the San Antonio Water System","usgsCitation":"Maclay, R.W., 1995, Geology and hydrology of the Edwards Aquifer in the San Antonio area, Texas: U.S. Geological Survey Water-Resources Investigations Report 95-4186, Document: v, 64 p.; 12 Plates: 28.00 x 19.39 inches or smaller, https://doi.org/10.3133/wri954186.","productDescription":"Document: v, 64 p.; 12 Plates: 28.00 x 19.39 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":57339,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57340,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57341,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57342,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4186/report-thumb.jpg"},{"id":57343,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57344,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57345,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57346,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4186/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57335,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57336,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57337,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57338,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Edwards Aquifer","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db68527d","contributors":{"authors":[{"text":"Maclay, Robert W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31893,"text":"ofr95554 - 1995 - Preliminary Geologic Map of the Big Pine Mountain Quadrangle, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:08","indexId":"ofr95554","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-554","title":"Preliminary Geologic Map of the Big Pine Mountain Quadrangle, California","docAbstract":"Reconnaissance geologic mapping of the San Rafael Primitive Area (now the San Rafael Wilderness) by Gower and others (1966) and Vedder an others (1967) showed s number of stratigraphic and structural ambiguities. To help resolve some of those problems, additional field work was done on parts of the Big Pine Moutain quadrangle during short intervals in 1981 and 1984, and 1990-1994.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95554","usgsCitation":"Vedder, J.G., McLean, H., and Stanley, R., 1995, Preliminary Geologic Map of the Big Pine Mountain Quadrangle, California (Version 1.0): U.S. Geological Survey Open-File Report 95-554, Map Sheet: 42 x 28 inches, https://doi.org/10.3133/ofr95554.","productDescription":"Map Sheet: 42 x 28 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":108951,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18509.htm","linkFileType":{"id":5,"text":"html"},"description":"18509"},{"id":160246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12728,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-554/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.75,34.6175 ], [ -119.75,34.75 ], [ -119.61749999999999,34.75 ], [ -119.61749999999999,34.6175 ], [ -119.75,34.6175 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc25","contributors":{"authors":[{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":207181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McLean, Hugh","contributorId":73977,"corporation":false,"usgs":true,"family":"McLean","given":"Hugh","affiliations":[],"preferred":false,"id":207179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stanley, R. G. 0000-0001-6192-8783","orcid":"https://orcid.org/0000-0001-6192-8783","contributorId":77123,"corporation":false,"usgs":true,"family":"Stanley","given":"R. G.","affiliations":[],"preferred":false,"id":207180,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20829,"text":"ofr94714W - 1995 - Hydrogeology of, ground-water withdrawals from, and saltwater intrusion in the shallow aquifer system of Cape May County, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr94714W","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"94-714","chapter":"W","title":"Hydrogeology of, ground-water withdrawals from, and saltwater intrusion in the shallow aquifer system of Cape May County, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94714W","usgsCitation":"Schuster, P.F., and Hill, M.C., 1995, Hydrogeology of, ground-water withdrawals from, and saltwater intrusion in the shallow aquifer system of Cape May County, New Jersey: U.S. Geological Survey Open-File Report 94-714, 40 p, https://doi.org/10.3133/ofr94714W.","productDescription":"40 p","costCenters":[],"links":[{"id":153163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0714w/report-thumb.jpg"},{"id":50425,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0714w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614920","contributors":{"authors":[{"text":"Schuster, Paul F. 0000-0002-8314-1372 pschuste@usgs.gov","orcid":"https://orcid.org/0000-0002-8314-1372","contributorId":1360,"corporation":false,"usgs":true,"family":"Schuster","given":"Paul","email":"pschuste@usgs.gov","middleInitial":"F.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":183323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, Mary Catherine","contributorId":53400,"corporation":false,"usgs":true,"family":"Hill","given":"Mary","email":"","middleInitial":"Catherine","affiliations":[],"preferred":false,"id":183324,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21152,"text":"ofr95295 - 1995 - Exploring storm surge","interactions":[],"lastModifiedDate":"2023-12-01T20:35:45.049609","indexId":"ofr95295","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-295","title":"Exploring storm surge","docAbstract":"This video provides a thorough discussion of storm surge, one of the most dangerous elements of hurricanes and major storms. This video illustrates basic storm surge principles, shows actual footage of storm surge damage and relates high-water level data collection by the U.S. Geological Survey to the task of recreating the storm surge event.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95295","usgsCitation":"Tihansky, A., and Duerr, A.D., 1995, Exploring storm surge: U.S. Geological Survey Open-File Report 95-295, 1 Videocassette: 14 minutes; 1 Transcript: 17 p., https://doi.org/10.3133/ofr95295.","productDescription":"1 Videocassette: 14 minutes; 1 Transcript: 17 p.","costCenters":[],"links":[{"id":422398,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0295/video","text":"Video","linkFileType":{"id":5,"text":"html"}},{"id":153533,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0295/coverthb.jpg"},{"id":422402,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0295/ofr19950295_cover.pdf","text":"Cover","size":"3.25 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":50743,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0295/ofr19950295_transcript.pdf","text":"Transcript","size":"60 B","linkFileType":{"id":1,"text":"pdf"}}],"contact":"Director, Caribbean-Florida Water Science Center
U.S. Geological Survey
4446 Pet Lane, Suite 108
Lutz, FL 33559
New heat-capacity measurements are reported for four rock types; Westerly granite from Bradford, RI, andesite from Lake County, OR, peridotite from Sonoma County, CA, and basalt from the Columbia River Group. Measurements were made on powders of the rocks in the temperature range of 340 to about 1000 K.
\nOur measured heat-capacity values for rocks and other measurements of heat capacity or heat content of rocks found in the literature have been compared with estimated rock heat capacities calculated from the summation of heat capacities of both minerals and oxide components. The validity of calculating the heat content or heat capacity of rocks to better than about ± 3% from its mineral or chemical composition is well demonstrated by the data presented here.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95622","usgsCitation":"Robertson, E.C., and Hemingway, B.S., 1995, Estimating heat capacity and heat content of rocks: U.S. Geological Survey Open-File Report 95-622, 38 p., https://doi.org/10.3133/ofr95622.","productDescription":"38 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":154016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0622/report-thumb.jpg"},{"id":19370,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0622/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc964","contributors":{"authors":[{"text":"Robertson, Eugene C.","contributorId":71139,"corporation":false,"usgs":true,"family":"Robertson","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":183024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hemingway, Bruch S.","contributorId":19542,"corporation":false,"usgs":true,"family":"Hemingway","given":"Bruch","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":183023,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":22043,"text":"ofr95259A - 1995 - Preliminary map of peak horizontal ground acceleration for the Hanshin-Awaji earthquake of January 17, 1995, Japan","interactions":[],"lastModifiedDate":"2018-05-02T10:33:40","indexId":"ofr95259A","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-259","chapter":"A","title":"Preliminary map of peak horizontal ground acceleration for the Hanshin-Awaji earthquake of January 17, 1995, Japan","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95259A","issn":"0094-9140","usgsCitation":"Wentworth, C.M., Borcherdt, R.D., and Mark, R.K., 1995, Preliminary map of peak horizontal ground acceleration for the Hanshin-Awaji earthquake of January 17, 1995, Japan: U.S. Geological Survey Open-File Report 95-259, map, https://doi.org/10.3133/ofr95259A.","productDescription":"map","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":51503,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0259a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0259a/report-thumb.jpg"},{"id":1209,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://quake.wr.usgs.gov/recent/reports/kobe/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d79f","contributors":{"authors":[{"text":"Wentworth, Carl M. 0000-0003-2569-569X cwent@usgs.gov","orcid":"https://orcid.org/0000-0003-2569-569X","contributorId":1178,"corporation":false,"usgs":true,"family":"Wentworth","given":"Carl","email":"cwent@usgs.gov","middleInitial":"M.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":186824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":186825,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mark, R. K.","contributorId":32159,"corporation":false,"usgs":true,"family":"Mark","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":186826,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":33259,"text":"b2124 - 1995 - Geology and mineral deposits of the Venezuelan Guayana Shield","interactions":[],"lastModifiedDate":"2018-10-23T18:04:13","indexId":"b2124","displayToPublicDate":"1996-02-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2124","title":"Geology and mineral deposits of the Venezuelan Guayana Shield","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b2124","usgsCitation":"Garcia, A., and Stoeser, J.W., 1995, Geology and mineral deposits of the Venezuelan Guayana Shield: U.S. Geological Survey Bulletin 2124, 1 v. (various pagings) :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/b2124.","productDescription":"1 v. (various pagings) :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":160989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2124/report-thumb.jpg"},{"id":61034,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2124/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46d9","contributors":{"editors":[{"text":"Sidder, Gary B.","contributorId":29486,"corporation":false,"usgs":true,"family":"Sidder","given":"Gary","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":749531,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Garcia, A.E.","contributorId":57512,"corporation":false,"usgs":true,"family":"Garcia","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":210288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoeser, J. 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I1-I41, https://doi.org/10.3133/b00I.","productDescription":"p. I1-I41","costCenters":[],"links":[{"id":60884,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2000i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2000i/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dbcb","contributors":{"authors":[{"text":"Hansley, P. L.","contributorId":82299,"corporation":false,"usgs":true,"family":"Hansley","given":"P. L.","affiliations":[],"preferred":false,"id":209879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2581,"text":"wsp2445 - 1995 - Effect of seasonal and long-term changes in stress on sources of water to wells","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp2445","displayToPublicDate":"1996-02-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2445","title":"Effect of seasonal and long-term changes in stress on sources of water to wells","docAbstract":"The source of water to wells is ultimately the location where the water flowing to a well enters the boundary surface of the ground-water system . In ground-water systems that receive most of their water from areal recharge, the location of the water entering the system is at the water table . The area contributing recharge to a discharging well is the surface area that defines the location of the water entering the groundwater system. Water entering the system at the water table flows to the well and is eventually discharged from the well. Many State agencies are currently (1994) developing wellhead-protection programs. The thrust of some of these programs is to protect water supplies by determining the areas contributing recharge to water-supply wells and by specifying regulations to minimize the opportunity for contamination of the recharge water by activities at the land surface. In the analyses of ground-water flow systems, steady-state average conditions are frequently used to simplify the problem and make a solution tractable. Recharge is usually cyclic in nature, however, having seasonal cycles and longer term climatic cycles. A hypothetical system is quantitatively analyzed to show that, in many cases, these cyclic changes in the recharge rates apparently do not significantly affect the location and size of the areas contributing recharge to wells. The ratio of the mean travel time to the length of the cyclic stress period appears to indicate whether the transient effects of the cyclic stress must be explicitly represented in the analysis of contributing areas to wells. For the cases examined, if the ratio of the mean travel time to the period of the cyclic stress was much greater than one, then the transient area contributing recharge to wells was similar to the area calculated using an average steady-state condition. Noncyclic long-term transient changes in water use, however, and cyclic stresses on systems with ratios less than 1 can and do affect the location and size of the areas contributing recharge to wells.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2445","usgsCitation":"Reilly, T.E., and Pollock, D.W., 1995, Effect of seasonal and long-term changes in stress on sources of water to wells: U.S. Geological Survey Water Supply Paper 2445, iv, 25 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2445.","productDescription":"iv, 25 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":32,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wsp2445/","linkFileType":{"id":5,"text":"html"}},{"id":138164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a3e4b07f02db49638f","contributors":{"authors":[{"text":"Reilly, Thomas E. tereilly@usgs.gov","contributorId":1660,"corporation":false,"usgs":true,"family":"Reilly","given":"Thomas","email":"tereilly@usgs.gov","middleInitial":"E.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":145435,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollock, David W. dwpolloc@usgs.gov","contributorId":4248,"corporation":false,"usgs":true,"family":"Pollock","given":"David","email":"dwpolloc@usgs.gov","middleInitial":"W.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":145436,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}