No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619V","usgsCitation":"Turcan, A., and Meyer, R.R., 1962, Alluvial aquifer in northeastern Louisiana — A large source of water: U.S. Geological Survey Water Supply Paper 1619, iv, 28 p., https://doi.org/10.3133/wsp1619V.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":394362,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24836.htm"},{"id":138973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619v/report-thumb.jpg"},{"id":29403,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619v/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Louisiana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.2840,\n 32.275\n ],\n [\n -90.9790,\n 32.275\n ],\n [\n -90.9790,\n 32.495\n ],\n [\n -91.2840,\n 32.495\n ],\n [\n -91.2840,\n 32.275\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6879ea","contributors":{"authors":[{"text":"Turcan, A. N.","contributorId":34114,"corporation":false,"usgs":true,"family":"Turcan","given":"A. N.","affiliations":[],"preferred":false,"id":145879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, R. R.","contributorId":20725,"corporation":false,"usgs":true,"family":"Meyer","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145878,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1370,"text":"wsp1598 - 1962 - Geology and ground-water resources of the Ahtanum Valley, Yakima County, Washington","interactions":[{"subject":{"id":43527,"text":"ofr5744 - 1957 - Geologic sections of the Ahtanum Valley, Yakima County, Washington","indexId":"ofr5744","publicationYear":"1957","noYear":false,"title":"Geologic sections of the Ahtanum Valley, Yakima County, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":1370,"text":"wsp1598 - 1962 - Geology and ground-water resources of the Ahtanum Valley, Yakima County, Washington","indexId":"wsp1598","publicationYear":"1962","noYear":false,"title":"Geology and ground-water resources of the Ahtanum Valley, Yakima County, Washington"},"id":1}],"lastModifiedDate":"2022-03-22T18:43:07.929619","indexId":"wsp1598","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1598","title":"Geology and ground-water resources of the Ahtanum Valley, Yakima County, Washington","docAbstract":"The Ahtanum Valley covers an area of about 100 square miles in an important agricultural district in central Yakima County, Wash. Because the area is semiarid, virtually all crops require irrigation. Surface-water supplies are inadequate in most of the area, and ground water is being used increasingly for irrigation. The purpose of this investigation was the collection and interpretation of data, pertaining to ground water in the area as an aid in the proper development and management of the water resources. \r\n\r\nThe occurrence and movement of ground water in the Ahtanum Valley are directly related to the geology. The valley occupies part of a structural trough (Ahtanum-Moxee subbasin) that is underlain by strongly folded flow layers of a thick sequence of the Yakima basalt. The upper part of the basalt sequence interfingers with, and is conformably overlying by, sedimentary rocks of the Ellensburg formation which are as much as 1,000 feet thick. These rocks are in turn overlying unconformably by cemented basalt gravel as much as 400 feet thick. Unconsolidated alluvial sand and gravel, as much as 30 feet thick, form the valley floor. \r\n\r\nAlthough ground water occurs in each of the rock units within the area, the Yakima basalt and the unconsolidated alluvium yield about three-fourths of the ground water currently used. Wells in the area range in depth from a few feet to more than 1,200 feet and yield from less than 1 to more than 1,030 gallons per minute. \r\n\r\nAlthough water levels in water-table wells usually are shallow--often less than 5 feet below the land surface--levels in deeper wells tapping confined water range from somewhat above the land surface (in flowing wells) to about 200 feet below. Wells drilled into aquifers in the Yakima basalt, the Ellensburg formation, and the cemented gravel usually tap confined water, and at least 12 wells in the area flow or have flowed in the past. Ground-water levels fluctuate principally in response to changes in stream levels, variations in the flow of irrigation ditches and in rates of water application, variations in local precipitation, and seasonal differences in withdrawals from wells. Annual fluctuations of levels generally are less than 10 feet except in localities of heavy pumping. Periodic measurements of water levels in two observation wells in the area indicate, locally at least, a persistent decline in artesian pressures in confined basalt aquifers, although the record is too short to show whether withdrawal by pumping has \r\nreached, or is nearing, an optimum balance with recharge. \r\n\r\nThe aquifers are recharged by precipitation, by infiltration from streams, and by ground-water underflow into the area. Ground water is discharged by seepage to streams, by evapotranspiration, by springs and seeps at the land surface, and, artificially, by withdrawal from wells. It is estimated that the seepage discharge to the Yakima River from the area studied may range from about 20,000 to 25,000 acre-feet per year. The consumptive waste of ground water by phreatophytes probably exceeds 4,000 acre-feet per year and may represent a large reclaimable source of water in the area. The annual withdrawal of ground water from wells in the area for domestic, industrial, irrigation, public, and stock supplies is estimated to be 6,300 acre-feet. The chemical quality of the ground water generally is satisfactory for most purposes, although the water from many wells is harder than is desirable for domestic use.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1598","usgsCitation":"Foxworthy, B., 1962, Geology and ground-water resources of the Ahtanum Valley, Yakima County, Washington: U.S. Geological Survey Water Supply Paper 1598, Report: v, 100 p.; 3 Plates: 28.00 × 25.00 inches or smaller, https://doi.org/10.3133/wsp1598.","productDescription":"Report: v, 100 p.; 3 Plates: 28.00 × 25.00 inches or smaller","costCenters":[],"links":[{"id":397412,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24787.htm"},{"id":26461,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1598/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26460,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1598/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26459,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1598/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26458,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1598/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1598/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Washington","county":"Yakima County","otherGeospatial":"Ahtanum Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.924,\n 46.493\n ],\n [\n -120.457,\n 46.493\n ],\n [\n -120.457,\n 46.575\n ],\n [\n -120.924,\n 46.575\n ],\n [\n -120.924,\n 46.493\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68571f","contributors":{"authors":[{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":143650,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":224,"text":"wsp1720 - 1962 - Quantity and quality of surface waters of Alaska, 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1720","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1720","title":"Quantity and quality of surface waters of Alaska, 1960","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1720","usgsCitation":"Hendricks, E.L., and Love, S.K., 1962, Quantity and quality of surface waters of Alaska, 1960: U.S. Geological Survey Water Supply Paper 1720, vi, 122 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1720.","productDescription":"vi, 122 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1720/report-thumb.jpg"},{"id":24835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1720/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64af4f","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142095,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2808,"text":"wsp1619I - 1962 - Pumping tests in the Los Alamos Canyon well field near Los Alamos, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1619I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"I","title":"Pumping tests in the Los Alamos Canyon well field near Los Alamos, New Mexico","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1619I","usgsCitation":"Theis, C., and Conover, C., 1962, Pumping tests in the Los Alamos Canyon well field near Los Alamos, New Mexico: U.S. Geological Survey Water Supply Paper 1619, iii, 24 p. :ill., maps ;24 cm. & 2 maps in pocket., https://doi.org/10.3133/wsp1619I.","productDescription":"iii, 24 p. :ill., maps ;24 cm. & 2 maps in pocket.","costCenters":[],"links":[{"id":138247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619i/report-thumb.jpg"},{"id":29310,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29311,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29312,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619i/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29313,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649504","contributors":{"authors":[{"text":"Theis, C.V.","contributorId":101641,"corporation":false,"usgs":true,"family":"Theis","given":"C.V.","email":"","affiliations":[],"preferred":false,"id":145828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conover, C.S.","contributorId":79862,"corporation":false,"usgs":true,"family":"Conover","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":145827,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2008,"text":"wsp1670 - 1962 - Water problems in the Springfield-Holyoke area, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1670","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1670","title":"Water problems in the Springfield-Holyoke area, Massachusetts","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey; for sale by the Superintendent of Documents, U.S. G.P.O.,","doi":"10.3133/wsp1670","usgsCitation":"Kammerer, J.C., and Baldwin, H.L., 1962, Water problems in the Springfield-Holyoke area, Massachusetts (Revision): U.S. Geological Survey Water Supply Paper 1670, 68 p. :ill., col. maps ;24 cm., https://doi.org/10.3133/wsp1670.","productDescription":"68 p. :ill., col. maps ;24 cm.","costCenters":[],"links":[{"id":138396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1670/report-thumb.jpg"},{"id":27453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1670/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Revision","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c4c","contributors":{"authors":[{"text":"Kammerer, John Craig","contributorId":90701,"corporation":false,"usgs":true,"family":"Kammerer","given":"John","email":"","middleInitial":"Craig","affiliations":[],"preferred":false,"id":144518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baldwin, H. L.","contributorId":104032,"corporation":false,"usgs":true,"family":"Baldwin","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1987,"text":"wsp1539S - 1962 - Water in the Coconino sandstone for the Snowflake-Hay Hollow area, Navajo County, Arizona","interactions":[],"lastModifiedDate":"2022-12-19T19:46:02.249571","indexId":"wsp1539S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1539","chapter":"S","title":"Water in the Coconino sandstone for the Snowflake-Hay Hollow area, Navajo County, Arizona","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539S","usgsCitation":"Johnson, P.W., 1962, Water in the Coconino sandstone for the Snowflake-Hay Hollow area, Navajo County, Arizona: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 46 p.; 4 Plates: 18.00 × 19.15 inches or smaller, https://doi.org/10.3133/wsp1539S.","productDescription":"Report: iv, 46 p.; 4 Plates: 18.00 × 19.15 inches or smaller","costCenters":[],"links":[{"id":27375,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539s/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27374,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539s/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27373,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539s/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109985,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24740.htm","linkFileType":{"id":5,"text":"html"},"description":"24740"},{"id":27376,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539s/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27372,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539s/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539s/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Navajo County","otherGeospatial":"Snowflake-Hay Hollow area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.846,\n 34.732\n ],\n [\n -109.846,\n 34.307\n ],\n [\n -110.272,\n 34.307\n ],\n [\n -110.272,\n 34.732\n ],\n [\n -109.846,\n 34.732\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa0d7","contributors":{"authors":[{"text":"Johnson, Phillip W.","contributorId":27422,"corporation":false,"usgs":true,"family":"Johnson","given":"Phillip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144480,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1986,"text":"wsp1475H - 1962 - Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1475H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1475","chapter":"H","title":"Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona","docAbstract":"The Chiricahua National Monument is in the eastern part of Cochise County, Ariz. The monument is about 35 miles southeast of Wilicox in the north end of the Chiricahua Mountains which border Sulphur Springs Valley on the west. The area is drained by two intermittent washes, one in Bonita and the other in Rhyolite Canyons.\r\n\r\nShake Spring is the present source of water for the monument. It ranges in rate of flow from 2 to 12 gpm (gallons per minute) and during dry periods It is not adequate to support the requirements of the monument.\r\n\r\nAmple water to meet the present and future needs of the Chiricahua National Monument is available from a combination of several sources - undeveloped springs or seeps, capture of runoff out of the canyons, and wells drilled in the alluvium.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475H","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Johnson, P.W., 1962, Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona: U.S. Geological Survey Water Supply Paper 1475, 209-216 p. & 1 map in pocket., https://doi.org/10.3133/wsp1475H.","productDescription":"209-216 p. & 1 map in pocket.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":137684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475h/report-thumb.jpg"},{"id":27370,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27371,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":12449,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/wsp/1475-H/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a98e","contributors":{"authors":[{"text":"Johnson, Phillip W.","contributorId":27422,"corporation":false,"usgs":true,"family":"Johnson","given":"Phillip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2661,"text":"wsp1663A - 1962 - Ground-water provinces of Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1663A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1663","chapter":"A","title":"Ground-water provinces of Brazil","docAbstract":"As part of a study of the status of investigations and development of ground water in Brazil, made under the auspices of the United States International Cooperation Administration and with the cooperation of the Government of Brazil, the country was divided into seven ground-water provinces. The identification and delineation of the provinces were based on the regional distribution of the dominant geologic units which are known or inferred to have distinctive water-bearing characteristics. \r\n\r\nThree of the provinces, covering most of the country, are underlain by Precambrian crystalline rocks. Three others coincide in part with four extensive sedimentary basins--the Parnaiba or Maranhfio basin and the contiguous Sao Francisco basin in the northeast and east, the Amazon basin in the north and northwest, and the Paranfi basin in the south and southwest. In addition, the narrow, discontinuous coastal plain is considered as a province. the occurrence of ground water is discussed briefly, and pertinent data are given on the more important aquifers, together with information on some existing wells. Because of the widespread distribution of crystalline rocks of low permeability, it is difficult in many areas to develop large or even adequate ground-water supplies. In general, satisfactory supplies of water are available in most of the rest of the country. Some problems include the relative deficiency of rainfall in the northeast together with the occurrence, in parts of this region, of mineralized water in the crystalline rocks. Also, there is a potential problem of excessive lowering of water levels and interference among wells in the intensively developed area of the city of Sao Paulo.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1663A","usgsCitation":"Schneider, R., 1962, Ground-water provinces of Brazil: U.S. Geological Survey Water Supply Paper 1663, 14 p. ;24 cm., https://doi.org/10.3133/wsp1663A.","productDescription":"14 p. ;24 cm.","costCenters":[],"links":[{"id":138216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1663a/report-thumb.jpg"},{"id":28997,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1663a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28998,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1663a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673f9","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":145571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1980,"text":"wsp1529 - 1962 - Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams","interactions":[{"subject":{"id":14338,"text":"ofr5756 - 1957 - Water power possibilities of Sheep Creek, Carlson Creek, Lake Dorothy and Turner Lake near Juneau, Alaska","indexId":"ofr5756","publicationYear":"1957","noYear":false,"title":"Water power possibilities of Sheep Creek, Carlson Creek, Lake Dorothy and Turner Lake near Juneau, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":1980,"text":"wsp1529 - 1962 - Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams","indexId":"wsp1529","publicationYear":"1962","noYear":false,"title":"Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1529","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1529","title":"Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1529","usgsCitation":"Johnson, F., 1962, Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams: U.S. Geological Survey Water Supply Paper 1529, v, 102 p. :illus., maps, diagr., tables. ;24 cm., https://doi.org/10.3133/wsp1529.","productDescription":"v, 102 p. :illus., maps, diagr., tables. ;24 cm.","costCenters":[],"links":[{"id":137668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1529/report-thumb.jpg"},{"id":27362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1529/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b62","contributors":{"authors":[{"text":"Johnson, Fred A.","contributorId":93863,"corporation":false,"usgs":true,"family":"Johnson","given":"Fred A.","affiliations":[],"preferred":false,"id":144472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1973,"text":"wsp1619U - 1962 - Methods of measuring soil moisture in the field","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1619U","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"U","title":"Methods of measuring soil moisture in the field","docAbstract":"For centuries, the amount of moisture in the soil has been of interest in agriculture. The subject of soil moisture is also of great importance to the hydrologist, forester, and soils engineer. \r\n\r\nMuch equipment and many methods have been developed to measure soil moisture under field conditions. This report discusses and evaluates the various methods for measurement of soil moisture and describes the equipment needed for each method. The advantages and disadvantages of each method are discussed and an extensive list of references is provided for those desiring to study the subject in more detail. \r\n\r\nThe gravimetric method is concluded to be the most satisfactory method for most problems requiring onetime moisture-content data. The radioactive method is normally best for obtaining repeated measurements of soil moisture in place. It is concluded that all methods have some limitations and that the ideal method for measurement of soil moisture under field conditions has yet to be perfected.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1619U","usgsCitation":"Johnson, A., 1962, Methods of measuring soil moisture in the field: U.S. Geological Survey Water Supply Paper 1619, iii, 25 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1619U.","productDescription":"iii, 25 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619u/report-thumb.jpg"},{"id":27349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bee4","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":144460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":181,"text":"wsp1572 - 1962 - Quality of surface waters of the United States, 1958, Parts 5 & 6, Hudson Bay and upper Mississippi River basins and Missouri River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1572","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1572","title":"Quality of surface waters of the United States, 1958, Parts 5 & 6, Hudson Bay and upper Mississippi River basins and Missouri River Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1572","usgsCitation":"Love, S.K., 1962, Quality of surface waters of the United States, 1958, Parts 5 & 6, Hudson Bay and upper Mississippi River basins and Missouri River Basin: U.S. Geological Survey Water Supply Paper 1572, ix, 365 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1572.","productDescription":"ix, 365 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1572/report-thumb.jpg"},{"id":24792,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1572/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651c18","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142052,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2517,"text":"wsp1619C - 1962 - Subsidence in the Santa Clara Valley, California: A progress report","interactions":[{"subject":{"id":46033,"text":"ofr5792 - 1957 - Map and graph showing land subsidence and ground-water level in Santa Clara Valley, California","indexId":"ofr5792","publicationYear":"1957","noYear":false,"title":"Map and graph showing land subsidence and ground-water level in Santa Clara Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":2517,"text":"wsp1619C - 1962 - Subsidence in the Santa Clara Valley, California: A progress report","indexId":"wsp1619C","publicationYear":"1962","noYear":false,"chapter":"C","title":"Subsidence in the Santa Clara Valley, California: A progress report"},"id":1}],"lastModifiedDate":"2022-05-11T18:44:50.672005","indexId":"wsp1619C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"C","title":"Subsidence in the Santa Clara Valley, California: A progress report","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619C","usgsCitation":"Poland, J.F., and Green, J.H., 1962, Subsidence in the Santa Clara Valley, California: A progress report: U.S. Geological Survey Water Supply Paper 1619, iii, 16 p., https://doi.org/10.3133/wsp1619C.","productDescription":"iii, 16 p.","costCenters":[],"links":[{"id":28717,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619c/report-thumb.jpg"},{"id":400532,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24816.htm"}],"country":"United States","state":"California","otherGeospatial":"Santa Clara Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.25,\n 37.25\n ],\n [\n -121.75,\n 37.25\n ],\n [\n -121.75,\n 37.567\n ],\n [\n -122.25,\n 37.567\n ],\n [\n -122.25,\n 37.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b5b","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, J. H.","contributorId":43312,"corporation":false,"usgs":true,"family":"Green","given":"J.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2762,"text":"wsp1585 - 1962 - Effect of irrigation on ground water in southern Canyon County, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1585","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1585","title":"Effect of irrigation on ground water in southern Canyon County, Idaho","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1585","usgsCitation":"Stevens, P.R., 1962, Effect of irrigation on ground water in southern Canyon County, Idaho: U.S. Geological Survey Water Supply Paper 1585, iv, 74 p. :maps (part fold. in pocket) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1585.","productDescription":"iv, 74 p. :maps (part fold. in pocket) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":138596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1585/report-thumb.jpg"},{"id":29191,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1585/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29192,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1585/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29193,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1585/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29194,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1585/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29195,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1585/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625600","contributors":{"authors":[{"text":"Stevens, Peter R.","contributorId":66239,"corporation":false,"usgs":true,"family":"Stevens","given":"Peter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145740,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1724,"text":"wsp1499B - 1962 - Water resources of the Tacoma area, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1499B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1499","chapter":"B","title":"Water resources of the Tacoma area, Washington","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1499B","usgsCitation":"Griffin, W.C., Sceva, J., Swenson, H.A., and Mundorff, M., 1962, Water resources of the Tacoma area, Washington: U.S. Geological Survey Water Supply Paper 1499, v, 101 p. :ill., maps (1 col.) ;24 cm., https://doi.org/10.3133/wsp1499B.","productDescription":"v, 101 p. :ill., maps (1 col.) ;24 cm.","costCenters":[],"links":[{"id":136956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499b/report-thumb.jpg"},{"id":26825,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26826,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26827,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26828,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26829,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b7e4b07f02db5cc0eb","contributors":{"authors":[{"text":"Griffin, William Colvin","contributorId":49773,"corporation":false,"usgs":true,"family":"Griffin","given":"William","email":"","middleInitial":"Colvin","affiliations":[],"preferred":false,"id":144021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sceva, J.E.","contributorId":70366,"corporation":false,"usgs":true,"family":"Sceva","given":"J.E.","affiliations":[],"preferred":false,"id":144023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swenson, H. A.","contributorId":58618,"corporation":false,"usgs":true,"family":"Swenson","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144022,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mundorff, M.J.","contributorId":48158,"corporation":false,"usgs":true,"family":"Mundorff","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":144020,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1767,"text":"wsp1499C - 1962 - Water resources of the Utica-Rome area, New York","interactions":[],"lastModifiedDate":"2021-12-13T21:17:31.346876","indexId":"wsp1499C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1499","chapter":"C","title":"Water resources of the Utica-Rome area, New York","docAbstract":"The Utica-Rome area is along the Mohawk River and New York State Erie (Barge) Canal about midway between Lake Ontario and Albany. It encompasses about 390 square miles centered around the industrial cities of Utica and Rome. The Mohawk River, its tributary West Canada Creek, and a system of reservoirs and diversions to maintain the flow in the barge-canal system, assure an ample water supply for the foreseeable needs of the area. The water from these sources is generally of good chemical quality requiring little treatment, although that from the Mohawk River is only fair and may require some treatment for sensitive industrial processes. Additional surface water is available from smaller streams in the area, particularly Oriskany and Sauquoit Creeks, but the water from these sources is hard, and has a dissolved-solids content of more than 250 ppm (parts per million). Ground water is available in moderate quantities from unconsolidated sand and gravel deposits in the river valleys and buried bedrock channels, and in small quantities from bedrock formations and less permeable unconsolidated deposits. The quality of water from sand and gravel, and bedrock ranges from good to poor. However, where necessary, the quality can be improved with treatment. \r\n\r\nThe Mohawk River is the source of the largest quantity of water in the area. The flow of the stream below Delta Dam equals or exceeds 108 mgd (million gallons per day) 90 percent of the time, and at Little Falls it equals or exceeds 560 mgd 90 percent of the time. The flow between these two points is increased by additions from Oriskany, Sauquoit, and West Canada Creeks and from many smaller tributary streams. The flow is also increased by diversions from outside the area, from the Black and Chenango Rivers and West Canada Creek for improvement of navigation in the Erie (Barge) Canal, and from West Canada and East Branch Fish Creeks for the public supplies of Utica and Rome. Much of the public-supply water eventually reaches the river by way of sewerage and industrial waste-disposal systems. The total diversion from these sources averages more than 92 mgd. An estimated 18.5 mgd is withdrawn from the Mohawk River by industry, mostly for nonconsumptive uses. \r\n\r\nFloods in the Utica-Rome area are not a frequent problem owing to the use of regulatory measures. The major streams fluctuate through a narrow range in stage and generally only a narrow strip along the streams is subject to flooding. Water-bearing sand and gravel deposits in the major river valleys are the principal sources of ground water, especially where they are recharged by infiltration from streams. The most important potential source is the deposit of sand and gravel underlying the extensive plain adjacent to the Mohawk River between Delta Reservoir and Rome. Maximum sustained yields from these deposits are not known; but moderate quantities of water, 300 gpm (gallons per minute) or less from a single well, can probably be obtained from some parts of the sand plain area, particularly in the vicinity of a buried bedrock channel that extends southwestward from Delta Reservoir. Similar quantities of ground water probably can be withdrawn from some parts of the flood plain of the Mohawk River between Rome and Frankfort and from the sand and gravel deposits filling the valley of Ninemile Creek below Holland Patent. The deposits underlying the flood plain of the Mohawk River generally are fine grained but in places contain interstratified beds of coarser sand and gravel. The most productive part of the flood plain is at the east end near Frankfort. The deposits in Ninemile Creek valley also are generally fine grained; but where they are sufficiently thick, as over a buried bedrock valley southwest of Floyd, moderate quantities of water may be obtained. \r\n\r\nSmall to moderate quantities of water (150 gpm or less from a single well) can be obtained from sand and gravel deposits in the bottoms of Oriskany and Sauquoit Creek vall","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1499C","usgsCitation":"Halberg, H., Hunt, O.P., and Pauszek, F.H., 1962, Water resources of the Utica-Rome area, New York: U.S. Geological Survey Water Supply Paper 1499, Report: iv, 46 p.; 3 Plates: 21.00 × 17.15 inches or smaller, https://doi.org/10.3133/wsp1499C.","productDescription":"Report: iv, 46 p.; 3 Plates: 21.00 × 17.15 inches or smaller","costCenters":[],"links":[{"id":26891,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26890,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26889,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499c/report-thumb.jpg"},{"id":26892,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392829,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24439.htm"}],"country":"United States","state":"New York","city":"Rome, Utica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.59417724609375,\n 43.018705515824635\n ],\n [\n -75.10528564453125,\n 43.018705515824635\n ],\n [\n -75.10528564453125,\n 43.29120116988416\n ],\n [\n -75.59417724609375,\n 43.29120116988416\n ],\n [\n -75.59417724609375,\n 43.018705515824635\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3376","contributors":{"authors":[{"text":"Halberg, Henry N.","contributorId":19929,"corporation":false,"usgs":true,"family":"Halberg","given":"Henry N.","affiliations":[],"preferred":false,"id":144113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, O. 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