{"pageNumber":"2578","pageRowStart":"64425","pageSize":"25","recordCount":68807,"records":[{"id":38915,"text":"pp450C - 1962 - Short papers in geology and hydrology, articles 60-119","interactions":[{"subject":{"id":52301,"text":"ofr62160 - 1962 - Interbasin movement of ground water at the Nevada Test Site","indexId":"ofr62160","publicationYear":"1962","noYear":false,"title":"Interbasin movement of ground water at the Nevada Test Site"},"predicate":"SUPERSEDED_BY","object":{"id":38915,"text":"pp450C - 1962 - Short papers in geology and hydrology, articles 60-119","indexId":"pp450C","publicationYear":"1962","noYear":false,"chapter":"C","title":"Short papers in geology and hydrology, articles 60-119"},"id":1}],"lastModifiedDate":"2023-09-29T21:33:28.175908","indexId":"pp450C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"450","chapter":"C","title":"Short papers in geology and hydrology, articles 60-119","docAbstract":"<p>No abstract available.&nbsp;</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1962 (Professional Paper 450)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp450C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Short papers in geology and hydrology, articles 60-119: U.S. Geological Survey Professional Paper 450, vi, 147 p., https://doi.org/10.3133/pp450C.","productDescription":"vi, 147 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":421432,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28129.htm","linkFileType":{"id":5,"text":"html"}},{"id":252066,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0450c/report-thumb.jpg"},{"id":247697,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0450c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fc4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529893,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52286,"text":"ofr62134 - 1962 - Ground water test well D, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-134","title":"Ground water test well D, Nevada Test Site, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/ofr62134","usgsCitation":"Thordarson, W., Garber, M.S., and Walker, G., 1962, Ground water test well D, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 62-134, 53 p., https://doi.org/10.3133/ofr62134.","productDescription":"53 p.","costCenters":[],"links":[{"id":178919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d73d","contributors":{"authors":[{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":245085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garber, M. S.","contributorId":6433,"corporation":false,"usgs":true,"family":"Garber","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":245084,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walker, G.E.","contributorId":59109,"corporation":false,"usgs":true,"family":"Walker","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":245086,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":13865,"text":"ofr6253 - 1962 - Idri salt deposits, Fezzan Province, Libya","interactions":[{"subject":{"id":13865,"text":"ofr6253 - 1962 - Idri salt deposits, Fezzan Province, Libya","indexId":"ofr6253","publicationYear":"1962","noYear":false,"title":"Idri salt deposits, Fezzan Province, Libya"},"predicate":"SUPERSEDED_BY","object":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"id":1}],"supersededBy":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"lastModifiedDate":"2025-06-05T17:24:36.968591","indexId":"ofr6253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-53","title":"Idri salt deposits, Fezzan Province, Libya","docAbstract":"<p>The Idri salt deposit, located 135 kilometers west of Brack in the Shatti Valley area of the Fezzan province, United Kingdom of Libya, covers an area of about 35 square Kilometers. It is connected to the newly constructed black-top Fezzan road by about 250 kilometers of secondary road. The deposit is a salt flat that lies in a closed depression. It consists of a hard crust commonly 20 to 40 cm thick overlying 40 cm of salts and wet sand above the brine.</p><p>The origin of the deposit is attributed to the percolating waters that concentrate into a brine and then by capillary action and evaporation form a crust on the surface.</p><p>Experiments with fractional crystallization by solar evaporation in the field indicated that fairly pure table salt may be obtained in the first stage of evaporation, and a product containing about 6 percent K<sub>2</sub>0 equivalent may be recovered in the second stage.</p><p>Laboratory experiments indicate that by the dissolving of the natural crust and recrystallization by artificial heat a salt mixture containing about 7 to 10 percent potassium may be recovered.</p><p>No future geologic work is recommended for the area but it is suggested that the deposit may be worked on a small scale to recover a pure table salt and, if the conditions warrant, the residual brine may be further treated to recover potash as a by-product.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6253","usgsCitation":"Goudarzi, G.H., 1962, Idri salt deposits, Fezzan Province, Libya: U.S. Geological Survey Open-File Report 62-53, Report: 36 p.; 3 Plates: 34.63 x 20.13 inches or smaller, https://doi.org/10.3133/ofr6253.","productDescription":"Report: 36 p.; 3 Plates: 34.63 x 20.13 inches or smaller","costCenters":[],"links":[{"id":489686,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0053/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":489685,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0053/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144409,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0053/report-thumb.jpg"},{"id":489683,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":489684,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0053/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Libya","otherGeospatial":"Fezzan Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              7.38280404429841,\n              33.468752022234625\n            ],\n            [\n              7.38280404429841,\n              18.987742330336374\n            ],\n            [\n              27.39090851205833,\n              18.987742330336374\n            ],\n            [\n              27.39090851205833,\n              33.468752022234625\n            ],\n            [\n              7.38280404429841,\n              33.468752022234625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faa2e","contributors":{"authors":[{"text":"Goudarzi, Gus H.","contributorId":44923,"corporation":false,"usgs":true,"family":"Goudarzi","given":"Gus","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":168532,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22804,"text":"ofr6234 - 1962 - Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho","interactions":[],"lastModifiedDate":"2013-11-22T15:37:23","indexId":"ofr6234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-34","title":"Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho","docAbstract":"This reports evaluates the ground-water resources of about 1,000 square miles in the semiarid uplands south of the Snake River between Bruneau River and Salmon Falls Creek. The outcropping rocks are the Idavada Volcanics of Pliocene age, and the Idaho Group of Pliocene and Plieistocene age, consisting of the Banbury Basalt of middle Pliocene age and overlying predominantly sedimentary deposits of middle Pliocene through middle Pleistocene age. These rocks dip gently northward. The volcanic rocks are the best aquifers, but the yield of water from the sedimentary deposits is adequate for domestic and stock use. About 6,000 acre-feet of water is withdrawn annually from the Idavada Volcanics by 9 irrigation wells to irrigate about 3,000 acres. Only a few tends of acre-feet of water withdrawn from the other formations. The regional dip of the rocks induces weak artesian conditions in the volcanic rocks and somewhat higher artesian head in the sedimentary rocks. Estimated depth to water ranges from less than 250 feet to more than 750 feet, as shown in an accompanying map. The eastern part of the area appears to be more favorable for the development of ground water for irrigation than the western part because of better aquifers at shallower depth.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6234","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Crosthwaite, E., 1962, Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho: U.S. Geological Survey Open-File Report 62-34, Report: ii, 53 p.; 3 Plates: 32.94 x 21.57 inches and smaller, https://doi.org/10.3133/ofr6234.","productDescription":"Report: ii, 53 p.; 3 Plates: 32.94 x 21.57 inches and smaller","numberOfPages":"56","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":155706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0034/report-thumb.jpg"},{"id":52232,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52233,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52234,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52235,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Elmore County;Owyhee County;Twin Falls County","otherGeospatial":"Sailor Creek Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.4626,42.0584 ], [ -116.4626,44.1361 ], [ -112.07,44.1361 ], [ -112.07,42.0584 ], [ -116.4626,42.0584 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0c5","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":188903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57723,"text":"ofr62162 - 1962 - Surface water of Beaver Creek Basin, in South-Central Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:12:12","indexId":"ofr62162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-162","title":"Surface water of Beaver Creek Basin, in South-Central Oklahoma","docAbstract":"Annual discharge from Beaver Creek basin is estimated to have averaged 217,000 acre-feet during a 19-year base period, water years 1938-56, equivalent to an average annual runoff depth of 4.7 inches over the 857 square-mile drainage area. About 55,000 acre-feet per year comes from Little Beaver Creek basin, a tributary drainage of 195 square miles.\r\nYearly streamflow is highly variable. The discharge of Little Beaver Creek near Duncan during 13-year period of record (water years 1949-61) has ranged from 86,530 acre-feet in calendar year 1957 to 4,880 acre-feet in 1956, a ratio of almost 18 to 1.\r\n\r\nHighest runoff within a year tends to occur in the spring months of May and June, a 2-month period that, on the average, accounts for more than half of the annual discharge of Little Beaver Creek near Duncan. The average monthly runoff during record was lowest in January. Variation in daily streamflow is such that while the average discharge for the 13-year period of record was 50.1 cfs (cubic feet per second), the daily discharge was more than 6 cfs only about half of the time. There was no flow at the site 19 percent of the time during the period.\r\n\r\nSome base runoff usually exists in the headwaters of Beaver and Little Beaver Creeks, and in the lower reaches of Beaver Creek. Low flow in Cow Creek tends to be sustained by waste water from Duncan, where water use in 1961 averaged 4 million gallons per day. In the remainder of the basin, periods of no flow occur in most years.\r\n\r\nThe surface water of Beaver Creek basin is very hard but in general is usable for municipal, agricultural and industrial purposes. The chemical character of the water is predominantly a calcium, magnesium bicarbonate type of water in the lower three quarters of the basin, except in Cow Creek where oil-field brines induce a distinct sodium, calcium chloride characteristic at low and medium flows. A calcium sulfate type of water occurs in most of the northern part of the basin except in headwater areas underlain by the Rush Springs Sandstone, where quality is similar to that in the lower basin.\r\n\r\nThe report gives an estimate of the average discharge at several sites in Beaver Creek basin for a 19-year base period, October 1937 to September 1956. Duration curves of daily discharge for Little Beaver Creek near Duncan and Beaver Creek near Waurika are shown for the period of record. Monthly and annual discharge records for these gaging stations are presented. The results of 52 discharge measurements at 17 other sites in the basin are tabulated, with 5 groups being plotted as discharge profiles. Storage requirements for regulated discharge at the two gaging stations are shown.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr62162","usgsCitation":"Laine, L., and Murphy, J., 1962, Surface water of Beaver Creek Basin, in South-Central Oklahoma: U.S. Geological Survey Open-File Report 62-162, 28 p., https://doi.org/10.3133/ofr62162.","productDescription":"28 p.","costCenters":[],"links":[{"id":184243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698203","contributors":{"authors":[{"text":"Laine, L.L.","contributorId":100464,"corporation":false,"usgs":true,"family":"Laine","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":257642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murphy, J.J.","contributorId":69144,"corporation":false,"usgs":true,"family":"Murphy","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":257641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68187,"text":"ha28 - 1962 - Availability of ground water in Union and Henderson Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:42","indexId":"ha28","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"28","title":"Availability of ground water in Union and Henderson Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha28","usgsCitation":"Maxwell, B.W., and Devaul, R.W., 1962, Availability of ground water in Union and Henderson Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 28, 3 col. maps ;56 x 70 cm.  (Tow maps, scale 1:125,000, and generalized columnar sction.  Sheets 1 and 2, 22 by 27 inches; sheet 3, 20 by 27 inches), https://doi.org/10.3133/ha28.","productDescription":"3 col. maps ;56 x 70 cm.  (Tow maps, scale 1:125,000, and generalized columnar sction.  Sheets 1 and 2, 22 by 27 inches; sheet 3, 20 by 27 inches)","costCenters":[],"links":[{"id":185562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89501,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/028/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89502,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/028/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89503,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/028/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660878","contributors":{"authors":[{"text":"Maxwell, Bruce William","contributorId":67489,"corporation":false,"usgs":true,"family":"Maxwell","given":"Bruce","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Devaul, Robert Washburn","contributorId":84338,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"Washburn","affiliations":[],"preferred":false,"id":277803,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38914,"text":"pp450B - 1962 - Short papers in geology, hydrology, and topography; Articles 1-59: Geological Survey Research 1962","interactions":[],"lastModifiedDate":"2022-06-09T21:14:22.507435","indexId":"pp450B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"450","chapter":"B","title":"Short papers in geology, hydrology, and topography; Articles 1-59: Geological Survey Research 1962","docAbstract":"<p>This collection of 59 short papers on subjects in the fields of geology, hydrology, topography, and related sciences is one of a, series to be relea~ed during the year as chapters of Professional Paper 450. The papers in this chapter report on the scientific and economic&middot; results of current work by members of the Geologic, Topographic, and 'Vater Resources Division of the United States Geological Survey. Some of the pa.pers annom1ce new discoveries or present observations on problems of limited scope; other papers draw conclusions from more extensive or continuing investigations that in large part will be discussed in greater detail in reports to be published in the future.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp450B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Short papers in geology, hydrology, and topography; Articles 1-59: Geological Survey Research 1962: U.S. Geological Survey Professional Paper 450, vi, 145 p., https://doi.org/10.3133/pp450B.","productDescription":"vi, 145 p.","numberOfPages":"150","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":402035,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28123.htm","linkFileType":{"id":5,"text":"html"}},{"id":252065,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0450b/report-thumb.jpg"},{"id":247696,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0450b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fca","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529892,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52295,"text":"ofr62151 - 1962 - Ground-water conditions during 1962 at the Marine Corps Base, Twentynine Palms, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-151","title":"Ground-water conditions during 1962 at the Marine Corps Base, Twentynine Palms, California","language":"ENGLISH","doi":"10.3133/ofr62151","usgsCitation":"Weir, J.E., 1962, Ground-water conditions during 1962 at the Marine Corps Base, Twentynine Palms, California: U.S. Geological Survey Open-File Report 62-151, 42 p., https://doi.org/10.3133/ofr62151.","productDescription":"42 p.","costCenters":[],"links":[{"id":179500,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0151/report-thumb.jpg"},{"id":86785,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0151/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86786,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0151/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2af","contributors":{"authors":[{"text":"Weir, J. E. Jr.","contributorId":102476,"corporation":false,"usgs":true,"family":"Weir","given":"J.","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":245099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52219,"text":"ofr6213 - 1962 - Sources of potable water supplies for the U. S. National Park Service Recreation area, Crawford Dam and Reservoir Site, Delta County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr6213","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-13","title":"Sources of potable water supplies for the U. S. National Park Service Recreation area, Crawford Dam and Reservoir Site, Delta County, Colorado","language":"ENGLISH","doi":"10.3133/ofr6213","usgsCitation":"Broom, M., 1962, Sources of potable water supplies for the U. S. National Park Service Recreation area, Crawford Dam and Reservoir Site, Delta County, Colorado: U.S. Geological Survey Open-File Report 62-13, 15 p., https://doi.org/10.3133/ofr6213.","productDescription":"15 p.","costCenters":[],"links":[{"id":177949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e75e5","contributors":{"authors":[{"text":"Broom, M.E.","contributorId":91147,"corporation":false,"usgs":true,"family":"Broom","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":244986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3722,"text":"cir460A - 1962 - The man and the hill","interactions":[],"lastModifiedDate":"2017-03-24T15:52:55","indexId":"cir460A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"460","chapter":"A","title":"The man and the hill","docAbstract":"<p>He was sitting on a large slab of rock. As he looked at the cloud of dust hanging hazily on the horizon, the piece of antler and the block of flint he held in his hand hung as if they were suspended from their previous rapid motion. The man gazed intently across the swaying grass which rose in wave-like billows across the distant hills. What was that dust - a herd of buffalo, a band of hunters, or were coyotes chasing the antelope again? After watching for a while he started again to chip the flint with a rapid twisting motion of the bone in his right hand. The little chips of flint fell in the grass before him. </p><p>It is the same hill but the scene has changed. Seated on the same rock, holding the reins of a saddle horse, a man dressed in buckskin took the fur cap off his head and wiped his brow. He was looking intently across a brown and desolate landscape at a cloud of dust on the far horizon. Was it the hostile tribe of Indians? It could be buffalo. Nervously he kicked at the ground with the deerhide moccasin, pushing the flint chips out of the way. He wiped the dust from his long rifle. What a terrible place - no water, practically no grass, everything bare and brown. </p><p>Now at sunset, slanting across the hills green with springtime, a cowman sits on a big rock, pushes his sombrero back on his head, and looks across the valley at a large but quiet herd of stock, moving slowly as each steer walks from one lush patch of grass to another, nibbling. Suddenly he stood up. Far on the horizon some dark objects were moving. Is it the sheepmen? Could it be the stage coach from Baggs to the Sweetwater Crossing?</p><p>Same hill - a gray truck was grinding slowly toward the summit. It pulled up near a small fenced enclosure where there were some instruments painted a bright silver color. A man stepped out of the truck and turned to his younger companion, \"You've never found an arrowhead? Maybe you have never thought about it correctly. If you want to find where an Indian camped long ago, put yourself in his place. Where would he sit to chip flint? He would take some high hill above a grassy valley where the breeze would cool him and where he could look across the country, watching for game or for enemies. If I were an Indian, that's what I would do. You change the chart of the rain gage and I am going to walk up to the place where I think he might have sat.\" He walked over to the crest of the hill and, near a large slab of sandstone, started to pick up pieces of flint. </p><p>This is an oft-repeated story. A given hill is repeatedly visited, used, loved or hated, protected or marred, by successive generations of men. All these men had characteristics in common. They had a job to do, a livelihood to make; they had their own plans, their own fears, but they were in one way or another connected with the land. </p>","conferenceTitle":"UNESCO and World Meteorological Organization Symposium on Climatic Change","conferenceDate":"October 3, 1961","conferenceLocation":"Rome, Italy","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir460A","usgsCitation":"Leopold, L.B., 1962, The man and the hill: U.S. Geological Survey Circular 460, 5 p., https://doi.org/10.3133/cir460A.","productDescription":"5 p.","startPage":"1","endPage":"5","numberOfPages":"8","costCenters":[],"links":[{"id":30782,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0460a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0460a/report-thumb.jpg"}],"publicComments":"Opening address to the Symposium on Climatic Change, United Nations Educational, Scientific and Cultural Organization and World Meteorological Organization, Rome, October 1961","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64abe5","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":147483,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2231,"text":"wsp1599 - 1962 - Reconnaissance of ground-water resources in the Western Coal Field Region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1599","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":"1599","title":"Reconnaissance of ground-water resources in the Western Coal Field Region, Kentucky","docAbstract":"In the Western Coal Field region of Kentucky, water is obtained from consolidated sedimentary rocks of Mississippian and Pennsylvanian ages and from unconsolidated sediments of Cenozoic age. Pennsylvanian rocks crop out in more than 95 percent of the area and consist of shale and sandstone interbedded with some limestone and coal. The Pennsylvanian strata are divided into five formations. They are, in ascending order: the Caseyville sandstone and the Tradewater, Carbondale, Lisman, and Henshaw formations. The Anvil Rock sandstone member of the Lisman formation and the Caseyville sandstone are the only bedrock aquifers in the region that are known to yield more than 100 gpm (gallons per minute) to wells. Most bedrock wells produce enough water for a modern domestic supply, more than 500 gpd (gallons per day), and few yield so little water as to be inadequate for hand pumps and bailers, less than 100 gpd. \r\n\r\nUnconsolidated Cenozoic deposits range from latest Pliocene(?) to Recent in age and consist of clay, silt, sand, and gravel. High gravels, tentatively considered to be late Pliocene and early Pleistacene in age by McFarlan (1950, p. 125), and loess of Pleistocene age are locally exposed, but nearly all of the alluvium is of late Pleistocene and Recent ages. The alluvium along the Ohio River generally yields from a few hundred to as much as 1,000 gpm to single vertical wells and as much as several thousand gallons per minute to wells that have multiple horizontal screens. Alluvium in the tributaries of the Ohio River generally is finer grained than that of the Ohio Valley. The highest known yield from a well in the alluvium of the tributaries is 56 gpm; other wells yield enough for domestic supplies. \r\n\r\nAvailability of ground water in the region depends on the character and thickness of the aquifer penetrated, and, where the aquifer is bedrock on the depth of the water-bearing bed, and to a certain extent on the topographic situation. Most bedrock aquifers in the Western Coal Field region are sandstone and may vary greatly in thickness and composition within short distances. The region is divided into five areas of ground-water availability. Area 1 is confined to the Ohio Valley, most of which is underlain by relatively thick sections of sand and gravel that yield at least 50 gpm to most wells at depths of less than 150 feet. In area 2 most wells yield enough water for a modern domestic supply from depths of less than 300 feet. This area includes the largest part of the bedrock outcrop in the region, some of the alluvial area along the Ohio River, and much of the alluvial areas along the larger tributaries. In area 3 most wells yield enough water from depths of less than 300 feet to supply domestic needs when a hand pump is used. This area covers the bedrock parts of the region that are underlain by shale, sandy shale, and limestone, and the section where few wells are known to yield large supplies of water. In area 4 most wells fail to supply enough water for domestic use from depths of less than 300 feet, probably because they penetrate thick sections of unfractured shale or well-cemented sandstone. In area 5 the yield of wells is unpredictable, commonly because of faulting. \r\n\r\nThe water in the shallow bedrock aquifers of the region is mostly of the sodium bicarbonate or the calcium bicarbonate type. Saline water has been encountered at depths as shallow as 100 feet, but fresh water has been obtained at depths approaching 1,000 feet. Water from the bedrock is soft to moderately hard, but it may contain undesirable amounts of iron. Most water from the alluvium is of the calcium bicarbonate type and is generally harder and contains more iron than water from the bedrock.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1599","usgsCitation":"Maxwell, B.W., and Devaul, R.W., 1962, Reconnaissance of ground-water resources in the Western Coal Field Region, Kentucky: U.S. Geological Survey Water Supply Paper 1599, vi, 34 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1599.","productDescription":"vi, 34 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1599/report-thumb.jpg"},{"id":247195,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1599/plate-table_4.pdf","size":"791","linkFileType":{"id":1,"text":"pdf"}},{"id":27985,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1599/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27986,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1599/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27987,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1599/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27988,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1599/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a64e4b07f02db637b34","contributors":{"authors":[{"text":"Maxwell, Bruce William","contributorId":67489,"corporation":false,"usgs":true,"family":"Maxwell","given":"Bruce","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":144860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Devaul, Robert Washburn","contributorId":84338,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"Washburn","affiliations":[],"preferred":false,"id":144861,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52255,"text":"ofr6278 - 1962 - Development of ground water in the vicinity of Tensleep, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:11:46","indexId":"ofr6278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-78","title":"Development of ground water in the vicinity of Tensleep, Wyoming","language":"ENGLISH","doi":"10.3133/ofr6278","usgsCitation":"Lowry, M., 1962, Development of ground water in the vicinity of Tensleep, Wyoming: U.S. Geological Survey Open-File Report 62-78, 12 p., https://doi.org/10.3133/ofr6278.","productDescription":"12 p.","costCenters":[],"links":[{"id":174427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0078/report-thumb.jpg"},{"id":86772,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65ded8","contributors":{"authors":[{"text":"Lowry, M.E.","contributorId":55807,"corporation":false,"usgs":true,"family":"Lowry","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":245046,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2481,"text":"wsp1539E - 1962 - Ground-water geology and hydrology of the Maynard area, Massachusetts","interactions":[{"subject":{"id":56085,"text":"ofr5788 - 1957 - Ground-water conditions, Maynard Ordnance Test Station and vicinity, Sudbury, Massachusetts","indexId":"ofr5788","publicationYear":"1957","noYear":false,"title":"Ground-water conditions, Maynard Ordnance Test Station and vicinity, Sudbury, Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":2481,"text":"wsp1539E - 1962 - Ground-water geology and hydrology of the Maynard area, Massachusetts","indexId":"wsp1539E","publicationYear":"1962","noYear":false,"chapter":"E","title":"Ground-water geology and hydrology of the Maynard area, Massachusetts"},"id":1}],"lastModifiedDate":"2023-10-30T22:00:02.423038","indexId":"wsp1539E","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":"E","title":"Ground-water geology and hydrology of the Maynard area, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539E","usgsCitation":"Perlmutter, N., 1962, Ground-water geology and hydrology of the Maynard area, Massachusetts: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 69 p.; 4 Plates: 28.50 x 15.98 inches or smaller, https://doi.org/10.3133/wsp1539E.","productDescription":"Report: iv, 69 p.; 4 Plates: 28.50 x 15.98 inches or smaller","costCenters":[],"links":[{"id":109975,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24728.htm","linkFileType":{"id":5,"text":"html"},"description":"24728"},{"id":28574,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28573,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28572,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28571,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28575,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138765,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539e/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Maynard area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.5,\n              42.5\n            ],\n            [\n              -71.5,\n              42.375\n            ],\n            [\n              -71.38630924839453,\n              42.375\n            ],\n            [\n              -71.38630924839453,\n              42.5\n            ],\n            [\n              -71.5,\n              42.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668e19","contributors":{"authors":[{"text":"Perlmutter, Nathaniel M.","contributorId":32139,"corporation":false,"usgs":true,"family":"Perlmutter","given":"Nathaniel M.","affiliations":[],"preferred":false,"id":145266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52263,"text":"ofr6293 - 1962 - Ground water in Birch Creek Valley, Idaho","interactions":[],"lastModifiedDate":"2013-11-19T11:56:07","indexId":"ofr6293","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-93","title":"Ground water in Birch Creek Valley, Idaho","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6293","usgsCitation":"Mundorff, M., 1962, Ground water in Birch Creek Valley, Idaho: U.S. Geological Survey Open-File Report 62-93, 10 p., https://doi.org/10.3133/ofr6293.","productDescription":"10 p.","numberOfPages":"10","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":175262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Birch Creek Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.4146,43.5779 ], [ -113.4146,44.5002 ], [ -111.8974,44.5002 ], [ -111.8974,43.5779 ], [ -113.4146,43.5779 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db92","contributors":{"authors":[{"text":"Mundorff, M.J.","contributorId":48158,"corporation":false,"usgs":true,"family":"Mundorff","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":245055,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2312,"text":"wsp1586C - 1962 - Observations of tidal flow in the Delaware River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1586C","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":"1586","chapter":"C","title":"Observations of tidal flow in the Delaware River","language":"ENGLISH","publisher":"[U.S.] Govt. Print. Off.,","doi":"10.3133/wsp1586C","usgsCitation":"Miller, E.G., 1962, Observations of tidal flow in the Delaware River: U.S. Geological Survey Water Supply Paper 1586, 26 p. :illus., https://doi.org/10.3133/wsp1586C.","productDescription":"26 p. :illus.","costCenters":[],"links":[{"id":137737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1586c/report-thumb.jpg"},{"id":28142,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1586c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69649a","contributors":{"authors":[{"text":"Miller, Everett George","contributorId":100358,"corporation":false,"usgs":true,"family":"Miller","given":"Everett","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":144993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3172,"text":"wsp1496C - 1962 - Flame-photometric determination of strontium in natural water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1496C","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":"1496","chapter":"C","title":"Flame-photometric determination of strontium in natural water","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1496C","usgsCitation":"Horr, C.A., 1962, Flame-photometric determination of strontium in natural water: U.S. Geological Survey Water Supply Paper 1496, 33-53 p., https://doi.org/10.3133/wsp1496C.","productDescription":"33-53 p.","costCenters":[],"links":[{"id":138921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1496c/report-thumb.jpg"},{"id":30130,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1496c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef2e1","contributors":{"authors":[{"text":"Horr, C. Albert","contributorId":43333,"corporation":false,"usgs":true,"family":"Horr","given":"C.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":146368,"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":3180,"text":"wsp1369D - 1962 - Flow through openings in width constrictions","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1369D","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":"1369","chapter":"D","title":"Flow through openings in width constrictions","docAbstract":"A highway embankment across a stream channel may have one or several bridge openings. In 1953, the pattern of flow through a single opening was quantitatively described by C. E. Kindsvater, R. W. Carter, and H. J. Tracy. The present investigation of the flow pattern at constrictions with two to seven openings is a continuation of the earlier study. Laboratory experiments and the analysis were directed toward the development of methods for (a) computing discharge through multiple-opening constrictions, (b) apportioning a given total discharge among the several openings, and (c) predicting the backwater caused by the constriction. \r\n\r\nThe division of flow among the openings was related to the relative area of each opening, and the relative velocity in the channel immediately upstream from each opening. On the basis of this relationship, the boundaries of the flow channel approaching each opening were established. The head-discharge and backwater characteristics of each opening were then analyzed separately. It is shown that the relations developed for the constriction with a single opening are applicable to each opening of a multiple-opening constriction once the boundaries of the separate flow channels have been established.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1369D","usgsCitation":"Davidian, J., Carrigan, P., and Shen, J., 1962, Flow through openings in width constrictions: U.S. Geological Survey Water Supply Paper 1369, 154 p. :illus., maps. ;24 cm. :91-122 p., https://doi.org/10.3133/wsp1369D.","productDescription":"154 p. :illus., maps. ;24 cm. :91-122 p.","costCenters":[],"links":[{"id":139023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1369d/report-thumb.jpg"},{"id":30138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1369d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db544634","contributors":{"authors":[{"text":"Davidian, Jacob","contributorId":80245,"corporation":false,"usgs":true,"family":"Davidian","given":"Jacob","email":"","affiliations":[],"preferred":false,"id":146383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrigan, P.H. Jr.","contributorId":21935,"corporation":false,"usgs":true,"family":"Carrigan","given":"P.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":146381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shen, John","contributorId":34109,"corporation":false,"usgs":true,"family":"Shen","given":"John","email":"","affiliations":[],"preferred":false,"id":146382,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3054,"text":"wsp1702 - 1962 - Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp1702","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":"1702","title":"Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1702","usgsCitation":"Hendricks, E.L., 1962, Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River: U.S. Geological Survey Water Supply Paper 1702, xi, 567 p. ;23 cm., https://doi.org/10.3133/wsp1702.","productDescription":"xi, 567 p. ;23 cm.","costCenters":[],"links":[{"id":139335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1702/report-thumb.jpg"},{"id":29908,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1702/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6943b2","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3447,"text":"cir465 - 1962 - Floods of December 1961 in Mississippi and adjoining states","interactions":[],"lastModifiedDate":"2022-12-12T19:54:00.957179","indexId":"cir465","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"465","title":"Floods of December 1961 in Mississippi and adjoining states","docAbstract":"Widespread floods occurred over parts of Mississippi, Louisiana, and Alabama after heavy rains during December 18, 1961. A series of low-pressure systems produced as much as 19 inches of rainfall in some areas. Heavy rainfall, 7 to 11 inches, on December 10 resulted in outstanding floods on small streams in southern Mississippi and southwestern Alabama. Subsequent rains produced multiple floods on small streams and outstanding floods of prolonged duration along the Big Black, upper Pearl, and lower Tombigbee Rivers in Mississippi. \r\n\r\nAt Jackson, Miss., the Pearl River reached the highest stage known. Along the east bank, flood waters topped or breached some of the levee system protecting the Flowood industrial area, but other parts were saved by extensive reinforcement and by emergency operation of the partially completed dam 10 miles upstream. Additional heavy damage to commercial and industrial property was prevented as a result of these measures. \r\n\r\nElsewhere, damage was restricted primarily to secondary highways and bridges. Two lives were lost.","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/cir465","usgsCitation":"Shell, J.D., 1962, Floods of December 1961 in Mississippi and adjoining states: U.S. Geological Survey Circular 465, iii, 17 p., https://doi.org/10.3133/cir465.","productDescription":"iii, 17 p.","costCenters":[],"links":[{"id":410300,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23828.htm","linkFileType":{"id":5,"text":"html"}},{"id":30460,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0465/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0465/report-thumb.jpg"}],"country":"United States","state":"Alabama, Arkansas, Georgia, Louisiana, Mississippi","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -91,\n              35\n            ],\n            [\n              -91,\n              30.833\n            ],\n            [\n              -85,\n              30.933\n            ],\n            [\n              -85,\n              35\n            ],\n            [\n              -91,\n              35\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b065f","contributors":{"authors":[{"text":"Shell, James D.","contributorId":23933,"corporation":false,"usgs":true,"family":"Shell","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":146932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3197,"text":"wsp1544B - 1962 - An application of thermometry to the study of ground water","interactions":[],"lastModifiedDate":"2018-04-02T10:17:13","indexId":"wsp1544B","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":"1544","chapter":"B","title":"An application of thermometry to the study of ground water","docAbstract":"<p>Except for studies of temperature data related to ground-water developments that induce infiltration from streams, little attention has been given to the possibility of using temperature fluctuations as a tool for studying the elements of the hydrologic cycle involving ground water.</p>\n<p>The temperature of the water discharged from large installations that induce river infiltration through alluvial deposits depends primarily on the following factors: (a) the porosity of the aquifer, (b) the specific heat of the rocks or mineral grains making it up, (c) the temperature of the ground water in storage, (d) the temperature of the river water, and (e) the amount of mixing that occurs as a result of pumping. In six installations of this type, where the annual rivertemperature fluctuations ranged from 44&deg; to 52&deg;F, the average range in groundwater temperature was 22 &deg;F. The cycles of ground-water temperature lagged behind the river-temperature cycles by 1 to 5<sup>1</sup>/<sub>2</sub> months. Under the conditions that existed, the lag of the minima of the cycles was much greater than that of the maxima, largely because of variations in pumpage and of the effect of viscosity differences on the rate of flow.</p>\n<p>An experimental study was made at Worthington in southwestern Minnesota to determine whether temperature fluctuations could be used to study rates and directions of ground-water movement or to evaluate recharge conditions. Three shallow glacial-outwash aquifers were studied by measuring temperatures at approximately monthly intervals in three municipal-supply wells whose average yields were about 60 to 150 gpm (gallons per minute). Temperatures were read with an accuracy of 0.01&deg; to 0.02&deg;C, and the data were analyzed graphically and correlated in detail with lake levels, lake temperatures, precipitation, and groundwater levels.</p>\n<p>Thermographs for 2 wells, 1 completed in a semiconfined aquifer about 200 feet from Okabena Lake and the other in a water-table aquifer about 850 feet from the lake, indicate that pumping induces water to move from the lake into the aquifers. A larger percentage of cold lake water was mixed with ground water from January to March 1958 than from January to March 1959. On the assumption that the cold or warm lake water was a distinct mass, the average time required for water to move from the lake to the well 200 feet away, under the prevailing hydraulic gradient, was 2 to 4 months; and to the well 850 feet away, 5 to 7 months.</p>\n<p>The thermograph for a well 1,800 feet from the lake, completed in an artesian aquifer that is confined by relatively impervious glacial till, indicates that the till acts as an insulating medium. However, despite the apparently low permeability of the till, the thermograph suggests that the lowering of artesian pressure, which results from pumping, induces warmer water to move downward through the till.</p>\n<p>The infiltration of relatively warm spring and summer rainfall can be detected on the thermographs of all the wells.</p>\n<p>The precise measurement of fluctuations in ground-water temperature, based on monthly readings in shallow glacial-outwash aquifers (up to about 70 feet deep), is useful in the study of ground-water movement and recharge. In addition to the study of natural phenomena in the hydrologic cycle, thermometry may be used as a tool in making detailed studies of (1) the effects of inducing the infiltration of surface water, (2) artificial recharge, (3) the effects of injecting petroleum products or radioactive or other wastes into the ground, and (4) ground-water movement in mines.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1544B","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation","usgsCitation":"Schneider, R., 1962, An application of thermometry to the study of ground water: U.S. Geological Survey Water Supply Paper 1544, Document: iii, 16 p.; 2 Plates: 16 x 12 inches and 16 x 17 inches, https://doi.org/10.3133/wsp1544B.","productDescription":"Document: iii, 16 p.; 2 Plates: 16 x 12 inches and 16 x 17 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":30184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30182,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1544b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30183,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1544b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68571e","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":146417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3198,"text":"wsp1544C - 1962 - Methods of flow measurement in well bores","interactions":[],"lastModifiedDate":"2022-07-19T11:31:11.072932","indexId":"wsp1544C","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":"1544","chapter":"C","title":"Methods of flow measurement in well bores","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1544C","usgsCitation":"Patten, E., and Bennett, G.D., 1962, Methods of flow measurement in well bores: U.S. Geological Survey Water Supply Paper 1544, 28 p., https://doi.org/10.3133/wsp1544C.","productDescription":"28 p.","costCenters":[],"links":[{"id":138322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544c/report-thumb.jpg"},{"id":30185,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bd13","contributors":{"authors":[{"text":"Patten, Eugene P. Jr.","contributorId":34897,"corporation":false,"usgs":true,"family":"Patten","given":"Eugene P.","suffix":"Jr.","affiliations":[],"preferred":false,"id":146419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, Gordon D.","contributorId":18740,"corporation":false,"usgs":true,"family":"Bennett","given":"Gordon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":146418,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3200,"text":"wsp1544E - 1962 - A thermal flowmeter for measuring velocity of flow in a well","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1544E","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":"1544","chapter":"E","title":"A thermal flowmeter for measuring velocity of flow in a well","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1544E","usgsCitation":"Chapman, H.T., and Robinson, A.E., 1962, A thermal flowmeter for measuring velocity of flow in a well: U.S. Geological Survey Water Supply Paper 1544, v. :ill. ;23 cm. ;12 p., https://doi.org/10.3133/wsp1544E.","productDescription":"v. :ill. ;23 cm. ;12 p.","costCenters":[],"links":[{"id":138324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544e/report-thumb.jpg"},{"id":30187,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5bc0","contributors":{"authors":[{"text":"Chapman, Howard T.","contributorId":99821,"corporation":false,"usgs":true,"family":"Chapman","given":"Howard","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":146423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Albert E.","contributorId":81360,"corporation":false,"usgs":true,"family":"Robinson","given":"Albert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146422,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2189,"text":"wsp1460J - 1962 - Geology and ground-water resources of the Elizabethton-Johnson City area, Tennessee","interactions":[],"lastModifiedDate":"2024-05-29T20:37:40.906455","indexId":"wsp1460J","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":"1460","chapter":"J","title":"Geology and ground-water resources of the Elizabethton-Johnson City area, Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1460J","usgsCitation":"Maclay, R.W., 1962, Geology and ground-water resources of the Elizabethton-Johnson City area, Tennessee: U.S. Geological Survey Water Supply Paper 1460, iv, 48 p., https://doi.org/10.3133/wsp1460J.","productDescription":"iv, 48 p.","costCenters":[],"links":[{"id":138566,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1460j/report-thumb.jpg"},{"id":429366,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24394.htm","linkFileType":{"id":5,"text":"html"}},{"id":27829,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1460j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Tennessee","otherGeospatial":"Elizabethton-Johnson City area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.375,\n              36.474\n            ],\n            [\n              -82.375,\n              36.25\n            ],\n            [\n              -82,\n              36.25\n            ],\n            [\n              -82,\n              36.474\n            ],\n            [\n              -82.375,\n              36.474\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68552c","contributors":{"authors":[{"text":"Maclay, Robert W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22803,"text":"ofr6233 - 1962 - Ground-water reconnaissance in Round Valley, Custer County, Idaho","interactions":[],"lastModifiedDate":"2013-11-15T12:53:00","indexId":"ofr6233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-33","title":"Ground-water reconnaissance in Round Valley, Custer County, Idaho","docAbstract":"Round Valley in central Idaho contains alluvial deposits of Pleistocene and Recent age which yield adequate supplies of ground water for stock and domestic wells. The alluvial deposits are underlain by Challis Volcanics of Oligocene or Early Miocene age and a few wells obtain domestic and stock water from the basalt, iatite, andesite, and rhyolite which are the principal rocks in the Challis. Very crude estimates indicate that the average annual recharge to the alluvium and Challis Volcanics from precipitation and irrigation is 50,000 acre-feet.\n\nGeologic and well data suggest that sufficient ground water might be obtained for irrigation supplies at some places.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6233","usgsCitation":"Crosthwaite, E., 1962, Ground-water reconnaissance in Round Valley, Custer County, Idaho: U.S. Geological Survey Open-File Report 62-33, Report: 27 p.; 1 Plate: 15.46 x 14.23 inches, https://doi.org/10.3133/ofr6233.","productDescription":"Report: 27 p.; 1 Plate: 15.46 x 14.23 inches","numberOfPages":"29","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":155705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0033/report-thumb.jpg"},{"id":52230,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52231,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Custer County","otherGeospatial":"Round Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.76,44.44 ], [ -114.76,44.93 ], [ -113.77,44.93 ], [ -113.77,44.44 ], [ -114.76,44.44 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667120","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":188902,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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