{"pageNumber":"5985","pageRowStart":"149600","pageSize":"25","recordCount":165846,"records":[{"id":1769,"text":"wsp1499D - 1964 - Water resources of the Albany-Schenectady-Troy area, New York","interactions":[],"lastModifiedDate":"2022-12-05T21:29:48.470516","indexId":"wsp1499D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"D","title":"Water resources of the Albany-Schenectady-Troy area, New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1499D","usgsCitation":"Halberg, H.N., Hunt, O.P., and Pauszek, F.H., 1964, Water resources of the Albany-Schenectady-Troy area, New York: U.S. Geological Survey Water Supply Paper 1499, Report: v, 64 p.; 2 Plates: 18.00 × 18.83 inches and 14.00 × 13.86 inches, https://doi.org/10.3133/wsp1499D.","productDescription":"Report: v, 64 p.; 2 Plates: 18.00 × 18.83 inches and 14.00 × 13.86 inches","costCenters":[],"links":[{"id":410067,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24440.htm","linkFileType":{"id":5,"text":"html"}},{"id":26898,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26899,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26897,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499d/report-thumb.jpg"}],"country":"United States","state":"New York","city":"Albany, Schenectady, Troy","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -74.083,\n              42.917\n            ],\n            [\n              -74.083,\n              42.5\n            ],\n            [\n              -73.583,\n              42.5\n            ],\n            [\n              -73.583,\n              42.917\n            ],\n            [\n              -74.083,\n              42.917\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f064b","contributors":{"authors":[{"text":"Halberg, Henry Nicholas","contributorId":41804,"corporation":false,"usgs":true,"family":"Halberg","given":"Henry","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":144118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, O. P.","contributorId":69116,"corporation":false,"usgs":true,"family":"Hunt","given":"O.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":144120,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144119,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1768,"text":"wsp1779V - 1964 - Ground-water resources of eastern Arkansas in the vicinity of U.S. Highway 70","interactions":[],"lastModifiedDate":"2012-11-20T13:38:16","indexId":"wsp1779V","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"V","title":"Ground-water resources of eastern Arkansas in the vicinity of U.S. Highway 70","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1779V","usgsCitation":"Halberg, H.N., and Reed, J., 1964, Ground-water resources of eastern Arkansas in the vicinity of U.S. Highway 70: U.S. Geological Survey Water Supply Paper 1779, iv, 38 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1779V.","productDescription":"iv, 38 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":26893,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779v/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26894,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779v/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26895,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779v/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26896,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779v/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":263312,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779v/report-thumb.jpg"},{"id":263311,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779v/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d628","contributors":{"authors":[{"text":"Halberg, Henry Nicholas","contributorId":41804,"corporation":false,"usgs":true,"family":"Halberg","given":"Henry","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":144117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":144116,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1848,"text":"wsp1723 - 1964 - Compilation of records of surface waters of the United States, October 1950 to September 1960, part 2–A. South Atlantic slope basins, James River to Savannah River","interactions":[],"lastModifiedDate":"2022-01-28T21:56:36.571854","indexId":"wsp1723","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1723","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960, part 2–A. South Atlantic slope basins, James River to Savannah River","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1723","usgsCitation":"Hendricks, E.L., 1964, Compilation of records of surface waters of the United States, October 1950 to September 1960, part 2–A. South Atlantic slope basins, James River to Savannah River: U.S. Geological Survey Water Supply Paper 1723, Report: ix, 303 p.; 1 Plate: 28.00 × 29.00 inches, https://doi.org/10.3133/wsp1723.","productDescription":"Report: ix, 303 p.; 1 Plate: 28.00 × 29.00 inches","costCenters":[],"links":[{"id":395099,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24907.htm"},{"id":138530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1723/report-thumb.jpg"},{"id":27064,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1723/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1723/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia, North Carolina, South Carolina, Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.35302734375,\n              32\n            ],\n            [\n              -75.7,\n              32\n            ],\n            [\n              -75.7,\n              37.92686760148135\n            ],\n            [\n              -84.35302734375,\n              37.92686760148135\n            ],\n            [\n              -84.35302734375,\n              32\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a982f","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144247,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1850,"text":"wsp1729 - 1964 - Compilation of records of surface waters of the United States, October 1950 to September 1960, part 6–A. Missouri River basin above Sioux City, Iowa","interactions":[],"lastModifiedDate":"2022-01-28T22:17:29.764548","indexId":"wsp1729","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1729","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960, part 6–A. Missouri River basin above Sioux City, Iowa","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1729","usgsCitation":"Hendricks, E.L., 1964, Compilation of records of surface waters of the United States, October 1950 to September 1960, part 6–A. Missouri River basin above Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1729, Report: xii, 507 p.; 1 Plate: 39.00 × 23.50 inches, https://doi.org/10.3133/wsp1729.","productDescription":"Report: xii, 507 p.; 1 Plate: 39.00 × 23.50 inches","costCenters":[],"links":[{"id":395103,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24913.htm"},{"id":27069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1729/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27068,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1729/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1729/report-thumb.jpg"}],"country":"United States","state":"Montana, North Dakota, South Dakota","otherGeospatial":"Missouri River basin above Sioux City","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.4228515625,\n              42.52069952914966\n            ],\n            [\n              -96.50390625,\n              42.52069952914966\n            ],\n            [\n              -96.50390625,\n              48.8936153614802\n            ],\n            [\n              -113.4228515625,\n              48.8936153614802\n            ],\n            [\n              -113.4228515625,\n              42.52069952914966\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9b4f","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1851,"text":"wsp1731 - 1964 - Compilation of records of surface waters of the United States, October 1950 to September 1960, part 7. Lower Mississippi basin","interactions":[],"lastModifiedDate":"2022-01-28T22:31:44.768151","indexId":"wsp1731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1731","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960, part 7. Lower Mississippi basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1731","usgsCitation":"Hendricks, E.L., 1964, Compilation of records of surface waters of the United States, October 1950 to September 1960, part 7. Lower Mississippi basin: U.S. Geological Survey Water Supply Paper 1731, Report: xiii, 552 p.; 1 Plate: 39.79 × 30.88 inches, https://doi.org/10.3133/wsp1731.","productDescription":"Report: xiii, 552 p.; 1 Plate: 39.79 × 30.88 inches","costCenters":[],"links":[{"id":138477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1731/report-thumb.jpg"},{"id":27070,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1731/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264375,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1731/plate-1.pdf","size":"8506","linkFileType":{"id":1,"text":"pdf"}},{"id":395104,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24915.htm"}],"country":"United States","otherGeospatial":"lower Mississippi River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.501953125,\n              29.878755346037977\n            ],\n            [\n              -86.044921875,\n              29.878755346037977\n            ],\n            [\n              -86.044921875,\n              39.605688178320804\n            ],\n            [\n              -104.501953125,\n              39.605688178320804\n            ],\n            [\n              -104.501953125,\n              29.878755346037977\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a97fa","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1852,"text":"wsp1750A - 1964 - Floods of January-February 1959 in Ohio and adjacent states","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1750A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1750","chapter":"A","title":"Floods of January-February 1959 in Ohio and adjacent states","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;","doi":"10.3133/wsp1750A","isbn":"pbk","usgsCitation":"Hendricks, E.L., 1964, Floods of January-February 1959 in Ohio and adjacent states: U.S. Geological Survey Water Supply Paper 1750, v, 296 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1750A.","productDescription":"v, 296 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1750a/report-thumb.jpg"},{"id":27071,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1750a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfc63","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1853,"text":"wsp1750B - 1964 - Summary of floods in the United States during 1959","interactions":[],"lastModifiedDate":"2017-09-06T17:51:01","indexId":"wsp1750B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1750","chapter":"B","title":"Summary of floods in the United States during 1959","docAbstract":"<p>This report describes the most outstanding floods that occurred in the United States during 1959.</p><p>The floods of January-February in Ohio and adjacent States were the most outstanding floods of the year 1959 with respect to area affected, number of streams having maximum discharge of record, rare occurrence of peaks, and great amount of damage caused.</p><p>Floods in the Rock River basin in southern Wisconsin and northern Illinois during late March and early April produced maximum stages and discharges on many streams. The Rock River at Watertown, Wisc., was the highest in 40 years and Lake Mendota at Madison, Wisc., reached its maximum stage since 1916. Many towns were flooded and thousands of persons were forced from their homes.</p><p>What is possibly the greatest 24-hour rainfall ever to be noted in Iowa fell August 5-6. The resulting floods inundated an 80-block area in Fort Madison, Iowa, and caused damage estimated at $600,000 in the city. A total of 130,000 acres of land was inundated.</p><p>Major floods occurred in Texas in the upper Trinity, middle Brazos, middle Colorado, upper Guadalupe, and upper Nueces River basins in early October, following heavy general rains that covered most of Texas. The peak stage on North Bosque River near Clifton was the highest known since 1887. More than \\$1 million in damage was reported for Houston.</p><p>In addition to the 4 floods mentioned above, 22 others of lesser magnitude are considered important enough to report in this annual summary.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1750B","usgsCitation":"Hendricks, E.L., 1964, Summary of floods in the United States during 1959: U.S. Geological Survey Water Supply Paper 1750, vi, 101 p., https://doi.org/10.3133/wsp1750B.","productDescription":"vi, 101 p.","numberOfPages":"101","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":27072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1750b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1750b/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69927b","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144252,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1874,"text":"wsp1669X - 1964 - Ground-water investigations in the lower Cache la Poudre River basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1669X","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1669","chapter":"X","title":"Ground-water investigations in the lower Cache la Poudre River basin, Colorado","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669X","usgsCitation":"Hershey, L.A., and Schneider, P., 1964, Ground-water investigations in the lower Cache la Poudre River basin, Colorado: U.S. Geological Survey Water Supply Paper 1669, iv, 22 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669X.","productDescription":"iv, 22 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669x/report-thumb.jpg"},{"id":27158,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669x/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27159,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669x/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27160,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669x/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669x/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66818b","contributors":{"authors":[{"text":"Hershey, Lloyd A.","contributorId":6831,"corporation":false,"usgs":true,"family":"Hershey","given":"Lloyd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, Paul A.","contributorId":32509,"corporation":false,"usgs":true,"family":"Schneider","given":"Paul A.","affiliations":[],"preferred":false,"id":144289,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1896,"text":"wsp1620 - 1964 - Geology and ground water of the Umatilla River Basin, Oregon","interactions":[{"subject":{"id":14147,"text":"ofr5654 - 1956 - Geology and ground-water resources of the Umatilla River basin area, Oregon","indexId":"ofr5654","publicationYear":"1956","noYear":false,"title":"Geology and ground-water resources of the Umatilla River basin area, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":1896,"text":"wsp1620 - 1964 - Geology and ground water of the Umatilla River Basin, Oregon","indexId":"wsp1620","publicationYear":"1964","noYear":false,"title":"Geology and ground water of the Umatilla River Basin, Oregon"},"id":1},{"subject":{"id":55745,"text":"ofr5568 - 1955 - Geology of the Umatilla River basin area, Oregon","indexId":"ofr5568","publicationYear":"1955","noYear":false,"title":"Geology of the Umatilla River basin area, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":1896,"text":"wsp1620 - 1964 - Geology and ground water of the Umatilla River Basin, Oregon","indexId":"wsp1620","publicationYear":"1964","noYear":false,"title":"Geology and ground water of the Umatilla River Basin, Oregon"},"id":2}],"lastModifiedDate":"2017-02-03T13:40:01","indexId":"wsp1620","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1620","title":"Geology and ground water of the Umatilla River Basin, Oregon","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1620","usgsCitation":"Hogenson, G., 1964, Geology and ground water of the Umatilla River Basin, Oregon: U.S. Geological Survey Water Supply Paper 1620, v, 162 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1620.","productDescription":"v, 162 p. :ill., maps ;23 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":27187,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1620/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27186,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1620/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1620/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138420,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1620/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ffb","contributors":{"authors":[{"text":"Hogenson, G.M.","contributorId":69957,"corporation":false,"usgs":true,"family":"Hogenson","given":"G.M.","affiliations":[],"preferred":false,"id":144329,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1725,"text":"wsp1753 - 1964 - Geology and ground-water resources of the Los Alamos area, New Mexico","interactions":[],"lastModifiedDate":"2023-01-03T21:48:27.368303","indexId":"wsp1753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1753","title":"Geology and ground-water resources of the Los Alamos area, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1753","usgsCitation":"Griggs, R.L., and Hem, J.D., 1964, Geology and ground-water resources of the Los Alamos area, New Mexico: U.S. Geological Survey Water Supply Paper 1753, Report: v, 106 p.; 1 Plate: 44.00 x 37.50 inches, https://doi.org/10.3133/wsp1753.","productDescription":"Report: v, 106 p.; 1 Plate: 44.00 x 37.50 inches","costCenters":[],"links":[{"id":411298,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24928.htm","linkFileType":{"id":5,"text":"html"}},{"id":26831,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1753/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26830,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1753/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136973,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1753/report-thumb.jpg"}],"country":"United States","state":"New Mexico","city":"Los Alamos","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.46530839888855,\n              36.019941722617205\n            ],\n            [\n              -106.46530839888855,\n              35.80051769145014\n            ],\n            [\n              -106.13840393978654,\n              35.80051769145014\n            ],\n            [\n              -106.13840393978654,\n              36.019941722617205\n            ],\n            [\n              -106.46530839888855,\n              36.019941722617205\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe9d","contributors":{"authors":[{"text":"Griggs, Roy Lee","contributorId":54170,"corporation":false,"usgs":true,"family":"Griggs","given":"Roy","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":144025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":144024,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1097,"text":"wsp1669S - 1964 - Yearly variations in runoff for the conterminous United States, 1931-1960","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1669S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1669","chapter":"S","title":"Yearly variations in runoff for the conterminous United States, 1931-1960","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1669S","usgsCitation":"Busby, M., 1964, Yearly variations in runoff for the conterminous United States, 1931-1960: U.S. Geological Survey Water Supply Paper 1669, iii, 49 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669S.","productDescription":"iii, 49 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669s/report-thumb.jpg"},{"id":25827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669s/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de56d","contributors":{"authors":[{"text":"Busby, Mark W.","contributorId":83099,"corporation":false,"usgs":true,"family":"Busby","given":"Mark W.","affiliations":[],"preferred":false,"id":143172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1947,"text":"wsp1748 - 1964 - Apparatus and techniques for measuring bedload","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1748","title":"Apparatus and techniques for measuring bedload","docAbstract":"The need for accurate determinations of the total sediment discharge of particles of bedload size has prompted this investigation of available and possible measuring apparatus and procedures. The accuracy of measurements of sediment discharge made with trap-type samplers is affected by the variability of sampler efficiency, by the oscillatory variation of bedload discharge, and by sampler placement. Equations that were developed for determining total discharge from measured bedioad discharge and measured suspended-sediment discharge are simplest if the bedload apparatus measures only the true bedload. \r\n\r\nEarly bedload samplers are generally unsatisfactory. Recently developed or suggested apparatus include various improved samplers of the pressure-difference type, a pumping sampler, a magnetic sampler, acoustical instruments that measure the magnitude of the sound of particle collisions, an ultrasonic bedload sampler designed to measure and integrate electronically the concentration and velocity, and a tiltmeter designed to measure the total sediment discharge from the ground tilt that results from the passage of flow. All the pressure-difference samplers are improvements over early samplers, but none are void of the inherent shortcomings of trap-type apparatus; probably the Sphinx (Dutch) and VUV (Hungarian) samplers are the most satisfactory. The acoustical instruments are capable of measuring only the relative discharge. The ultrasonic sampler and the tiltmeter are not adequate without further development. \r\n\r\nSome new possible apparatus and means for measuring or aiding in measuring bedload discharge are small pit samplers, ultrasonic sounders, pressure transducers, and photography. A small pit sampler for measuring bedload discharge was designed to provide self-placement and portability ; however, its practicability and efficiency are undetermined. Exploratory films show that by using slowmotion photography the discharge of particles larger than about pea size can be determined provided the flow is clear; however, photography generally is not practical. Ultrasonic sounders provide continuous and accurate data on bed configuration and dune movement for use in equations that were developed for computing the bedload discharge. Computations with the equations indicate that the interpretation of the sounding data needs further study. Pressure transducers placed beneath the bed surface possibly can be used to provide information on dune movement; however, their installation would be difficult. The time required for collecting data on bed configuration and dune movement throughout a cross section could be substantially reduced by using several transducers simultaneously in conjunction with an ultrasonic sounder. A modified ultrasonic sounder that provides information on the shape and velocity of large particles and a method for determining the discharge of such particles were proposed; the method seems most feasible for particles of high sphericity.","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1748","usgsCitation":"Hubbell, D.W., 1964, Apparatus and techniques for measuring bedload: U.S. Geological Survey Water Supply Paper 1748, v, 74 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1748.","productDescription":"v, 74 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":27278,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1748/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1748/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4883e4b07f02db51824d","contributors":{"authors":[{"text":"Hubbell, David Wellington","contributorId":88330,"corporation":false,"usgs":true,"family":"Hubbell","given":"David","email":"","middleInitial":"Wellington","affiliations":[],"preferred":false,"id":144417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1952,"text":"wsp1689 - 1964 - Magnitude and frequency of floods in the United States: Part 14. Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2022-01-25T21:53:44.628933","indexId":"wsp1689","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1689","title":"Magnitude and frequency of floods in the United States: Part 14. Pacific slope basins in Oregon and lower Columbia River basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1689","usgsCitation":"Hulsing, H., and Kallio, N.A., 1964, Magnitude and frequency of floods in the United States: Part 14. Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1689, Report: xiii, 319 p.; 5 Plates: 11.00 × 22.25 inches or smaller, https://doi.org/10.3133/wsp1689.","productDescription":"Report: xiii, 319 p.; 5 Plates: 11.00 × 22.25 inches or smaller","costCenters":[],"links":[{"id":394846,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24898.htm"},{"id":27292,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1689/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27291,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27290,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27289,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27288,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27287,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1689/report-thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"lower Columbia River basin, Pacific slope basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.564,\n              42\n            ],\n            [\n              -118,\n              42\n            ],\n            [\n              -118,\n              46.667\n            ],\n            [\n              -124.564,\n              46.667\n            ],\n            [\n              -124.564,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649599","contributors":{"authors":[{"text":"Hulsing, Harry","contributorId":62200,"corporation":false,"usgs":true,"family":"Hulsing","given":"Harry","email":"","affiliations":[],"preferred":false,"id":144425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kallio, N. A.","contributorId":42833,"corporation":false,"usgs":true,"family":"Kallio","given":"N.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144424,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1958,"text":"wsp1779H - 1964 - Ground water in Cedar Rapids Division of Lower Platte River basin, Nebraska","interactions":[],"lastModifiedDate":"2022-12-30T22:01:19.587282","indexId":"wsp1779H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"H","title":"Ground water in Cedar Rapids Division of Lower Platte River basin, Nebraska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1779H","usgsCitation":"Hyland, J.B., Keech, C.F., and Rosene, P.G., 1964, Ground water in Cedar Rapids Division of Lower Platte River basin, Nebraska: U.S. Geological Survey Water Supply Paper 1779, Report: iii, 12 p.; 3 Plates: 30.00 x 30.83 inches, https://doi.org/10.3133/wsp1779H.","productDescription":"Report: iii, 12 p.; 3 Plates: 30.00 x 30.83 inches","costCenters":[],"links":[{"id":411260,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24960.htm","linkFileType":{"id":5,"text":"html"}},{"id":27310,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779h/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27309,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779h/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27308,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27311,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138559,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779h/report-thumb.jpg"}],"country":"United States","state":"Nebraska","otherGeospatial":"Cedar Rapids division of lower Platte River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -97.654,\n              41.328\n            ],\n            [\n              -98.649,\n              41.328\n            ],\n            [\n              -98.649,\n              41.817\n            ],\n            [\n              -97.654,\n              41.817\n            ],\n            [\n              -97.654,\n              41.328\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dbe9","contributors":{"authors":[{"text":"Hyland, James B.","contributorId":49340,"corporation":false,"usgs":true,"family":"Hyland","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":144436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":144434,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosene, Philip G.","contributorId":48942,"corporation":false,"usgs":true,"family":"Rosene","given":"Philip","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144435,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1960,"text":"wsp1779K - 1964 - Chemical quality of surface waters in the Brazos River basin in Texas","interactions":[],"lastModifiedDate":"2016-08-22T11:24:32","indexId":"wsp1779K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"K","title":"Chemical quality of surface waters in the Brazos River basin in Texas","docAbstract":"<p>The Brazos River basin, which makes up 15 percent of the land area of Texas, extends from the High Plains, where altitudes reach 4,200 feet and the average precipitation ranges from 15 to 20 inches a year, to the Gulf of Mexico where the annual rainfall is 45-^50 inches. Large reservoirs have been built in the Brazos River basin, but the use of the stored water has been limited because the salinity often makes the water undesirable for municipal and industrial use. However, the water is generally satisfactory for irrigation. Records for the Brazos River show that the salinity of the water was a problem even as early as 1906 and that the water more often than not failed to meet today's chemical-quality standards for a municipal supply.</p>\n<p>The salt load of the Brazos River comes from the entire basin and is the result of solution, accretion of undetermined amounts of oil-field brine, and accretion of brine from springs and seeps such as those in Salt Croton Creek which contribute about 400 tons of chloride a day.</p>\n<p>Much of the salinity of the Brazos River is due to inflow of brines above Possum Kingdom Dam. The area above Possum Kingdom Dam is about 52 percent of the total area in the Brazos River basin but contributes only about 17 percent of the total runoff; however, about 50 percent of the annual salt load comes from this part of the basin.</p>\n<p>Quality-of-water records show a wide difference in the salinity of the steams in different parts of the basin, Dissolved-solids concentrations ranged from about 100 ppm (parts per million) for flood water to 300,000 ppm for saturated brines from springs.</p>\n<p>The quality of the surface water in the Brazos River basin is discussed by areas and by stream reaches. This study indicates that the water of the Salt Fork Brazos River is too saline for most uses. The water of the Double Mountain Fork Brazos River is less saline and might be used for irrigation; however, it probably could not be used as a municipal supply or as a supply for most industries. The water of the dear Fork Brazos River is generally good but is adversely affected by brine pollution. Chemical-quality records for the Lampasas, Leon, and Navasota Rivers indicate that the water of these streams is of excellent quality; however, more data are needed to determine variations. The quality of the water in other tributaries could only be inferred from the results of miscellaneous sampling and from the&nbsp;probable effect of the underlying rocks. The weighted-average concentration of constituents in the Brazos River at Richmond indicated that inflow below Whitney Reservoir has a dilution effect on the river. For 12 of the 14 years of record, the weighted-average dissolved-solids concentration of the Brazos River at Richmond was lessi than, the 500 ppm maximum limit recommended by the U.S. Public Health Service (1961).</p>\n<p>This study indicates that water stored in Possum Kingdom and Whitney Reservoirs tends to become stratified, with the more saline water being at the greater depths. Samples collected in 1956 at Whitney Reservoir showed that the chloride concentration at the bottom was almost twice that at the surface. After a flood in June 1957, the dissolved-solids concentrations of bottom releases at Possum Kingdom were almost double those of surface releases through the spillway even though the flood volume had been more than twice the capacity of the reservoir.</p>\n<p>The quality of water in the lower main stem can be improved by control and disposal of brines in the upper basin. Also, the maximum concentrations in the water of the lower main stem can be lowered by dilution with water stored in reservoirs on tributaries that yield water of good quality.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1779K","usgsCitation":"Irelan, B., and Mendieta, H., 1964, Chemical quality of surface waters in the Brazos River basin in Texas: U.S. Geological Survey Water Supply Paper 1779, Report: vi, 70 p.; 4 Plates, https://doi.org/10.3133/wsp1779K.","productDescription":"Report: vi, 70 p.; 4 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":27313,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27314,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779k/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27315,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779k/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27316,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779k/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27317,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779k/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e32ac","contributors":{"authors":[{"text":"Irelan, Burdge","contributorId":15991,"corporation":false,"usgs":true,"family":"Irelan","given":"Burdge","email":"","affiliations":[],"preferred":false,"id":144438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mendieta, H.B.","contributorId":38965,"corporation":false,"usgs":true,"family":"Mendieta","given":"H.B.","email":"","affiliations":[],"preferred":false,"id":144439,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1106,"text":"wsp1669W - 1964 - The yield of sedimentary aquifers of the coastal plain, southeast river basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1669W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1669","chapter":"W","title":"The yield of sedimentary aquifers of the coastal plain, southeast river basins","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669W","usgsCitation":"Callahan, J.T., 1964, The yield of sedimentary aquifers of the coastal plain, southeast river basins: U.S. Geological Survey Water Supply Paper 1669, iv, 56 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669W.","productDescription":"iv, 56 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669w/report-thumb.jpg"},{"id":25841,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669w/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25842,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e816","contributors":{"authors":[{"text":"Callahan, Joseph Thomas","contributorId":45689,"corporation":false,"usgs":true,"family":"Callahan","given":"Joseph","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":143186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1969,"text":"wsp1583 - 1964 - Ground water in Fountain and Jimmy Camp Valleys, El Paso County, Colorado","interactions":[{"subject":{"id":51914,"text":"ofr5660 - 1956 - Results of pumping tests in the Widefield area, Fountain Valley, Colorado","indexId":"ofr5660","publicationYear":"1956","noYear":false,"title":"Results of pumping tests in the Widefield area, Fountain Valley, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":1969,"text":"wsp1583 - 1964 - Ground water in Fountain and Jimmy Camp Valleys, El Paso County, Colorado","indexId":"wsp1583","publicationYear":"1964","noYear":false,"title":"Ground water in Fountain and Jimmy Camp Valleys, El Paso County, Colorado"},"id":1}],"lastModifiedDate":"2022-02-22T12:23:23.211645","indexId":"wsp1583","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1583","title":"Ground water in Fountain and Jimmy Camp Valleys, El Paso County, Colorado","docAbstract":"The part of Fountain Valley considered in this report extends from Colorado Springs to the Pueblo County line. It is 23 miles long and has an area of 26 square miles. The part of Jimmy Camp Valley discussed is 11 miles long and has an area of 9 square miles. The topography is characterized by level flood plains and alluvial terraces that parallel the valley and by rather steep hills along the valley sides. The climate is semiarid, average annual precipitation being about 13 inches. Farming and stock raising are the principal occupations in the valleys; however, some of the agricultural land near Colorado Springs is being used for housing developments. \r\n\r\nThe Pierre Shale and alluvium underlie most of the area, and mesa gravel caps the shale hills adjacent to Fountain Valley. The alluvium yields water to domestic, stock, irrigation, and public-supply wells and is capable of yielding large quantities of water for intermittent periods. Several springs issue along the sides of the valley at the contact of the mesa gravel and the underlying Pierre Shale. \r\n\r\nThe water table ranges in depth from less than 10 feet along the bottom lands to about 80 feet along the sides of the valleys; the saturated thickness ranges from less than a foot to about 50 feet. \r\n\r\nThe ground-water reservoir in Fountain Valley is recharged by precipitation that falls within the area, by percolation from Fountain Creek, which originates in the Pikes Peak, Monument Valley, and Rampart Range areas, and by seepage from irrigation water. This reservoir contains about 70,000 acre-feet of ground water in storage. The ground-water reservoir in Jimmy Camp Valley is recharged from precipitation that falls within the area, by percolation from Jimmy Camp Creek during periods of streamflow, and by seepage from irrigation water. The Jimmy Camp ground-water reservoir contains about 25,000 acre-feet of water in storage. Ground water is discharged from the area by movement to the south, by evaporation and transpiration in areas of shallow water table, by seepage into Fountain and Jimmy Camp Creeks, and through wells. About 3 to 4 mgd (million gallons per day) of ground water moves through the Fountain Valley alluvium at a velocity of about 15 feet per day. About 1 mgd of ground water moves through the Jimmy Camp Valley alluvium at a velocity of about 6 feet per day. \r\n\r\nMost of the wells in the area are drilled, but a few are dug. Many large-diameter wells are used for irrigation and public supply: one of the wells","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1583","usgsCitation":"Jenkins, E., and Glover, R., 1964, Ground water in Fountain and Jimmy Camp Valleys, El Paso County, Colorado: U.S. Geological Survey Water Supply Paper 1583, v, 66 p., https://doi.org/10.3133/wsp1583.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":138289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1583/report-thumb.jpg"},{"id":27345,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1583/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396181,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24768.htm"}],"country":"United States","state":"Colorado","county":"El Paso County","otherGeospatial":"Fountain and Jimmy Camp Valleys","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.8,\n              38.625\n            ],\n            [\n              -104.625,\n              38.625\n            ],\n            [\n              -104.625,\n              38.817\n            ],\n            [\n              -104.8,\n              38.817\n            ],\n            [\n              -104.8,\n              38.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db54","contributors":{"authors":[{"text":"Jenkins, Edward D.","contributorId":17972,"corporation":false,"usgs":true,"family":"Jenkins","given":"Edward D.","affiliations":[],"preferred":false,"id":144452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glover, Robert E.","contributorId":64636,"corporation":false,"usgs":true,"family":"Glover","given":"Robert E.","affiliations":[],"preferred":false,"id":144453,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1974,"text":"wsp1779Z - 1964 - Selected bibliography on laboratory and field methods in ground-water hydrology","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1779Z","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"Z","title":"Selected bibliography on laboratory and field methods in ground-water hydrology","language":"ENGLISH","publisher":"for sale by the Supt. of Docs., U. S. Govt. Print. Off.,","doi":"10.3133/wsp1779Z","usgsCitation":"Johnson, A., 1964, Selected bibliography on laboratory and field methods in ground-water hydrology: U.S. Geological Survey Water Supply Paper 1779, iii, 21 p. ;24 cm., https://doi.org/10.3133/wsp1779Z.","productDescription":"iii, 21 p. ;24 cm.","costCenters":[],"links":[{"id":138313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779z/report-thumb.jpg"},{"id":27350,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779z/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa6c1","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":144461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1717,"text":"wsp1779T - 1964 - The effect of artesian-pressure decline on confined aquifer systems and its relation to land subsidence","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1779T","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"T","title":"The effect of artesian-pressure decline on confined aquifer systems and its relation to land subsidence","docAbstract":"Ground water in the Southwestern United States is derived chiefly from unconsolidated to semiconsolidated alluvial deposits. Where these deposits contain confined water, they may be susceptible to compaction and related land- surface subsidence, if artesian pressures are reduced. \r\n\r\nCompaction of artesian-aquifer systems can be estimated from core tests if the artesian-pressure decline is known. Compaction occurs chiefly in the finer grained deposits ; porosity decrease is greater near the top of the confined aquifer than near the bottom. \r\n\r\nBecause most of the compaction of these aquifer systems is permanent, the storage coefficient during the initial decline of artesian pressure greatly exceeds the storage coefficient during a subsequent pressure decline through the same depth range, after an intervening period of pressure recovery.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1779T","usgsCitation":"Green, J.H., 1964, The effect of artesian-pressure decline on confined aquifer systems and its relation to land subsidence: U.S. Geological Survey Water Supply Paper 1779, iii, 11 p. ;24 cm., https://doi.org/10.3133/wsp1779T.","productDescription":"iii, 11 p. ;24 cm.","costCenters":[],"links":[{"id":136939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779t/report-thumb.jpg"},{"id":26803,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779t/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6681bf","contributors":{"authors":[{"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":144009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1716,"text":"wsp1671 - 1964 - Magnitude and frequency of floods in the United States; part 1-A. North Atlantic Slope Basins, Maine to Connecticut","interactions":[],"lastModifiedDate":"2022-01-04T21:02:32.328471","indexId":"wsp1671","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1671","title":"Magnitude and frequency of floods in the United States; part 1-A. North Atlantic Slope Basins, Maine to Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey ;","doi":"10.3133/wsp1671","usgsCitation":"Green, A.R., 1964, Magnitude and frequency of floods in the United States; part 1-A. North Atlantic Slope Basins, Maine to Connecticut: U.S. Geological Survey Water Supply Paper 1671, Report: x, 260 p.; 1 Plate: 24.00 × 34.00 inches, https://doi.org/10.3133/wsp1671.","productDescription":"Report: x, 260 p.; 1 Plate: 24.00 × 34.00 inches","costCenters":[],"links":[{"id":110005,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24880.htm","linkFileType":{"id":5,"text":"html"},"description":"24880"},{"id":136938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1671/report-thumb.jpg"},{"id":26801,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1671/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1671/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, Rhode Island, Vermont","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.685302734375,\n              41.00477542222947\n            ],\n            [\n              -66.09375,\n              41.00477542222947\n            ],\n            [\n              -66.09375,\n              47.635783590864854\n            ],\n            [\n              -73.685302734375,\n              47.635783590864854\n            ],\n            [\n              -73.685302734375,\n              41.00477542222947\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495a8","contributors":{"authors":[{"text":"Green, A. Rice","contributorId":31731,"corporation":false,"usgs":true,"family":"Green","given":"A.","email":"","middleInitial":"Rice","affiliations":[],"preferred":false,"id":144008,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13,"text":"wsp1739 - 1964 - Compilation of records of surface waters of Hawaii, July 1950 to June 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1739","title":"Compilation of records of surface waters of Hawaii, July 1950 to June 1960","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1739","usgsCitation":"Hendricks, E.L., 1964, Compilation of records of surface waters of Hawaii, July 1950 to June 1960: U.S. Geological Survey Water Supply Paper 1739, vii, 136 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1739.","productDescription":"vii, 136 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1739/report-thumb.jpg"},{"id":24612,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24613,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24614,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24615,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24616,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24617,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1739/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9087","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":141816,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11,"text":"wsp1740 - 1964 - Compilation of records of surface waters of Alaska, October 1950 to September 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1740","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1740","title":"Compilation of records of surface waters of Alaska, October 1950 to September 1960","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1740","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Compilation of records of surface waters of Alaska, October 1950 to September 1960: U.S. Geological Survey Water Supply Paper 1740, vi, 86 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1740.","productDescription":"vi, 86 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":136324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1740/report-thumb.jpg"},{"id":24604,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1740/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24605,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1740/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9b76","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":527154,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1122,"text":"wsp1773 - 1964 - Geology and ground-water resources of the Anchorage area, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1773","title":"Geology and ground-water resources of the Anchorage area, Alaska","docAbstract":"The Anchorage area, at the head of Cook Inlet in south-central Alaska, \r\noccupies 150 square miles of a glaciated lowland and lies between two estuaries and the Chugach Mountains. Two military bases are in the area; \r\nAnchorage is the largest city in Alaska and the chief transportation center \r\nfor this part of the State. \r\nThe bedrock in the Anchorage area is chiefly Tertiary shale in the lowland \r\nand metamorphic rocks of Mesozoic age beneath the adjacent mountain \r\nslopes. Glacial drift which underlies nearly the entire area has an average \r\nthickness of several hundred feet and appears to include at least five sheets \r\nof deposits, two of which are exposed. The drift consists of till, outwash stream and lake deposits (sand and gravel), and estuarine (and lake) deposits \r\n(clay and silt). The stratigraphy and lateral distribution of the deposits are \r\ncomplex, but data at hand s, how that the thickest deposits, including all the \r\nestuarine and lake sediment and most of the stream-deposited sediment, \r\nare beneath the lowland away from the mountain wall, and that the deposits \r\nnear the mountains are till and subordinate outwash sediments. \r\nDeposits of sand and gravel laid down by outwash streams in channels and \r\non outwash plains are the most important aquifers, and the only \r\nones which yield large quantities of ground water from single beds. Thin \r\nlayers of sandy or gravelly material in till are also important aquifers although they yield relatively small quantities of water. Bedded sand and \r\nsilt associated with the estuarine and lake(?) clay commonly becomes unstable during drilling and pumping, and has been successfully developed in \r\nonly a few wells. Unconfined aquifers are extensive, but permeable saturated \r\nmaterial is thin in many places and water supplies available from them are \r\nsmall or undependable in those places. The most important aquifers are confined or artesian. Clay and till form the confining beds: the till is somewhat 'leaky' in many places. Near Anchorage the buried water-bearing \r\nbeds appear to be interconnected and to form a single artesian system. The \r\nwater table and piezometric surface slope from the mountain wall of the \r\nlowland toward the estuaries, and the flow of the ground water is in that \r\ndirection. The aquifers are recharged by the infiltration of precipitation \r\nat the land surface and of surface water through stream beds: near the mountains the artesian aquifers are probably recharged in part by percolation from \r\nthe water-table aquifer, and far from the mountains the water-table aquifer \r\nis probably recharged in part by upward flow from the underlying artesian \r\naquifers. In several valleys and in a few other places, in the lowland, artesian wells flow at the land surface. \r\nThe outwash sand and gravel are moderately to very permeable; most \r\nof the other water-bearing material are much less permeable. The co- efficient of transmissibility for some single beds of sandy gravel is as high \r\nas 60,000 to I00,000 gpd per ft (gallons per day per foot); for the entire \r\nsection of glacial drift at and near Anchorage it is believed to be of the \r\norder of 200,000 gpd per ft. Calculations based on this value for the total \r\nsection and on the slope of the piezometric surface indicate that in the \r\nimmediate vicinity of Anchorage about 5 million gpd flows through each \r\nmile-wide section of the drift (measured in a northeast-southwest direction, perpendicular to the direction of flow), under normal (nonpumping) conditions. Under conditions of continuous heavy pumping the slope of the piezometric surface is steepened, flow is increased, and additional recharge is induced. \r\n\r\nThe highest yield reported from a well in this area is 2.600 gpm (gallons per minute) with 35 feet of drawdown: the highest reported specific capacity is 180 gpm per ft of drawdown, for a well pumped at. 270 gpm. \r\n\r\nOnly a few wells in the area have been developed for high yields. Well screens have been used ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1773","usgsCitation":"Cederstrom, D.J., Trainer, F.W., and Waller, R.M., 1964, Geology and ground-water resources of the Anchorage area, Alaska: U.S. Geological Survey Water Supply Paper 1773, vi, 108 p. :illus., maps (1 col.) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1773.","productDescription":"vi, 108 p. :illus., maps (1 col.) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":138014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1773/report-thumb.jpg"},{"id":25887,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25888,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25889,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25890,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1773/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6855f4","contributors":{"authors":[{"text":"Cederstrom, Dagfin John","contributorId":90287,"corporation":false,"usgs":true,"family":"Cederstrom","given":"Dagfin","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":143212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trainer, Frank W.","contributorId":103655,"corporation":false,"usgs":true,"family":"Trainer","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143213,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waller, Roger Milton","contributorId":22320,"corporation":false,"usgs":true,"family":"Waller","given":"Roger","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":143211,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1989,"text":"wsp1776 - 1964 - Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water","interactions":[{"subject":{"id":52182,"text":"ofr6179 - 1961 - Basic data, ground-water resources and geology of Washington, D. C., and vicinity","indexId":"ofr6179","publicationYear":"1961","noYear":false,"title":"Basic data, ground-water resources and geology of Washington, D. C., and vicinity"},"predicate":"SUPERSEDED_BY","object":{"id":1989,"text":"wsp1776 - 1964 - Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water","indexId":"wsp1776","publicationYear":"1964","noYear":false,"title":"Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water"},"id":1}],"lastModifiedDate":"2023-11-02T21:05:20.22677","indexId":"wsp1776","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1776","title":"Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water","docAbstract":"<p>The area of this report includes 436 square miles centered about the District of Columbia. </p><p>The area contains parts of two distinctly different physiographic provinces-the Piedmont and the Coastal Plain. The Fall Line, which separates the Piedmont province on the west from the Coastal Plain Province on the east, bisects the area diagonally from northeast to southwest. Northwest of the Fall Line, deeply weathered igneous and metamorphic rocks are exposed ; to the southeast, these rocks are covered by Coastal Plain sediments; the nonconformity between crystalline rock and sediments dips southeast at an average rate of about 125 feet per mile. </p><p>The rocks of the Piedmont include: (1) schist, phyllite, and quartzite of the Wissahickon Formation; (2) altered mafic rocks such as greenstone and serpentine; (3) the Laurel Gneiss of Chapman, 1942, and the Sykesville Formation of Jonas, 1928--both probably derived from the Wissahickon ; and (4) later granitic intrusive rocks.</p><p> Lying upon this basement of hard rocks east of the Fall Line are the generally unconsolidated sediments of the Coastal Plain, which include gravel, sand, and clay, ranging in age from Cretaceous to Recent. These sediments measure only a few inches at their western extremity but thicken to 1,800 feet at the southeast corner of the mapped area. </p><p>Owing to the great diversity in the geology of the two provinces, the waterbearing characteristics of the rocks also vary greatly. In the Piedmont, ground water occurs under unconfined or water-table conditions in openings and fissures in the hard rocks or in the residual weathered blanket that overlies them. In the Coastal Plain, the shallow wells tap unconfined water, but beneath the upper clay layers the water is contained in the sand and gravel under artesian pressure and must be recovered by deep drilled wells. </p><p>Wells are of three types--drilled, bored, and dug. Drilled wells furnish a permanent water supply and are the least subject to pollution when properly constructed. Bored or dug wells allow greater storage capacity and are satisfactory for domestic supplies in some locations, but they are polluted easily. If not properly constructed or of sufficient depth, they may fail in dry weather. </p><p>Ground-water supplies for domestic use, 5 to 10 gpm (gallons per minute), are obtainable in most places. In the Piedmont, recorded yields in drilled wells range from 0.2 to 212 gpm. In the Coastal Plain, wells yield from 1 to 800 gpm. </p><p>The quality of the ground water in the report area is generally satisfactory for domestic, industrial, and irrigation use. High iron content and corrosiveness are troublesome in places. The water is soft to moderately hard--2 to 175 ppm (parts per million). Water in the Piedmont province is. dominantly the calcium and bicarbonate type; in the Coastal Plain most water is of calcium-magnesium bicarbonate type. </p><p>In the Piedmont, careful location of wells with respect to the geology (rock type and structure) and to topography usually results in higher yields and may mean the difference between success and failure. In the Coastal Plain, drilled artesian wells are not affected by topography, but the yield obtained depends upon the penetration of a water-bearing sand or gravel bed at sufficient depth. </p><p>The early settlers obtained water from the springs and streams, and later from dug wells. After Washington was established as the Capital in 1800, water was obtained from public and privately owned wells. Water was piped from some of the springs to government buildings and to private homes and business houses. In 1863 a diversion dam was completed in the Potomac above Great Falls and a conduit was built into the city to furnish a public water supply. This system with modifications has been in use ever since. A new diversion dam and pumping station at Little Falls was put into service in the summer of 1959. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1776","usgsCitation":"Johnston, P.M., Weaver, D.E., and Siu, L., 1964, Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water: U.S. Geological Survey Water Supply Paper 1776, Report: vi, 97 p.; 2 Plates: 34.50 x 26.60 inches and 21.00 x 28.60 inches, https://doi.org/10.3133/wsp1776.","productDescription":"Report: vi, 97 p.; 2 Plates: 34.50 x 26.60 inches and 21.00 x 28.60 inches","costCenters":[],"links":[{"id":422360,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16352.htm","linkFileType":{"id":5,"text":"html"}},{"id":27381,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1776/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27382,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1776/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138471,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1776/report-thumb.jpg"},{"id":27380,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1776/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"District of Columbia","city":"Washington D.C.","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-77.038598,38.791513],[-77.038898,38.800813],[-77.035798,38.814913],[-77.038098,38.815613],[-77.039098,38.821413],[-77.038098,38.828612],[-77.039199,38.832212],[-77.041199,38.833712],[-77.042599,38.833812],[-77.043499,38.833212],[-77.044899,38.834712],[-77.044999,38.838512],[-77.044489,38.839595],[-77.044199,38.840212],[-77.041699,38.840212],[-77.032798,38.841712],[-77.031698,38.850512],[-77.039299,38.864312],[-77.038899,38.865812],[-77.039099,38.868112],[-77.040599,38.871212],[-77.043299,38.874012],[-77.045399,38.875212],[-77.046599,38.874912],[-77.045599,38.873012],[-77.046299,38.871312],[-77.049099,38.870712],[-77.051299,38.873212],[-77.051099,38.875212],[-77.054099,38.879112],[-77.055199,38.880012],[-77.058254,38.880069],[-77.063499,38.888611],[-77.067299,38.899211],[-77.068199,38.899811],[-77.070099,38.900711],[-77.0822,38.901911],[-77.0902,38.904211],[-77.0937,38.905911],[-77.1012,38.911111],[-77.1034,38.912911],[-77.1063,38.919111],[-77.1134,38.925211],[-77.1166,38.928911],[-77.1179,38.932411],[-77.119857,38.93427],[-77.1199,38.934311],[-77.1045,38.94641],[-77.1007,38.94891],[-77.0915,38.95651],[-77.054299,38.98511],[-77.040999,38.99511],[-77.036299,38.99171],[-77.015598,38.97591],[-77.013798,38.97441],[-77.008298,38.97011],[-77.002636,38.965521],[-77.002498,38.96541],[-76.941519,38.918276],[-76.935096,38.913311],[-76.909395,38.892812],[-76.910795,38.891712],[-76.919295,38.885112],[-76.920195,38.884412],[-76.949696,38.861312],[-76.953696,38.858512],[-76.979497,38.837812],[-76.992697,38.828213],[-76.999997,38.821913],[-77.001397,38.821513],[-77.024392,38.80297],[-77.038598,38.791513]]]},\"properties\":{\"name\":\"District of Columbia\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685810","contributors":{"authors":[{"text":"Johnston, Paul McKelvey","contributorId":8828,"corporation":false,"usgs":true,"family":"Johnston","given":"Paul","email":"","middleInitial":"McKelvey","affiliations":[],"preferred":false,"id":144482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weaver, D. E.","contributorId":51718,"corporation":false,"usgs":true,"family":"Weaver","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":887473,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Siu, Leonard","contributorId":331349,"corporation":false,"usgs":false,"family":"Siu","given":"Leonard","email":"","affiliations":[],"preferred":false,"id":887474,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1999,"text":"wsp1651 - 1964 - Chemical quality of surface waters and sedimentation in the Saline River basin, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1651","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1651","title":"Chemical quality of surface waters and sedimentation in the Saline River basin, Kansas","docAbstract":"This report gives the results of an investigation of the sediment and dissolved minerals that are transported by the Saline River and its tributaries. The Saline River basin is in western and central Kansas; it is long and narrow and covers 3,420 square miles of rolling plains, which is broken in some places by escarpments and small areas of badlands. In the western part the uppermost bedrock consists predominantly of calcareous elastic sedimentary rocks of continental origin of Pliocene age and in most places is covered by eolian deposits of Pleistocene and Recent age. In the central part the ex posed bedrock consists predominantly of calcareous marine sedimentary rocks of Late Cretaceous age. In the eastern part the exposed bedrock consists mainly of noncalcareous continental and littoral elastic sedimentary rocks of Early Cretaceous and Permian age. Fluvial deposits are in the valleys, and eolian materials are present over much of the uplands. \r\n\r\nAverage precipitation increases rather uniformly from about 18 inches per year in the west to almost 28 inches per year in the east. Runoff is not affected by irrigation nor regulated by large structures, but it is closely related to precipitation. Average runoff increases from less than 0.2 inch per year in the west to more than 1.5 inches per year in the east. Aquifers of the flood-plain and terrace deposits and of the Cretaceous Dakota Sandstone are the major sources of ground-water accretion to the streams. In the upper reaches of the Saline River, the water is only slightly mineralized; during the period of record the specific conductance near Wakeeney never exceeded 750 micromhos per centimeter. In the lower reaches, however, the water is slightly mineralized during periods of high flow and is highly mineralized during periods of low flow; the specific conductance near Russell exceeded 1,500 micromhos per centimeter more than 80 percent of the time. Near Russell, near Wilson, and at Tescott the water is of the calcium bicarbonate type when the specific conductance is less than about 1,000 micromhos per centimeter, but it is of the sodium chloride type when the specific conductance is more than about 1,500 micromhos per centimeter. The water is off the calcium bicarbonate, sodium bicarbonate, or sodium chloride type when the conductance is between 1,000 and 1,500 micromhos per centimeter. Most of the increase in mineralization of the water is caused by inflow of highly mineralized ground water. The ground-water inflow was estimated to be 22 percent of the total streamflow at Tescott in 1948 and 60 percent in 1952. Mineralization increases and water quality deteriorates progressively downstream along nearly the entire Saline River, especially in the part of the area directly underlain by the Dakota Sandstone between the vicinities of Fairport and Wilson: sodium and chloride are the principal constituents of water contributed by the Dakota. The total percentage of the salt in the Saline River that comes from oil-field brines is considered to be small. The water in the upper Saline River is of good quality for domestic use except that it is hard; the water in the lower Saline River is of poor quality for domestic use because most of the time it is highly mineralized, is hard, and contains high concentrations of chloride and sulfate. In the upper reaches of the river, the water is of good quality for irrigation. In the lower reaches, if the water were impounded in a reservoir, it would be of good quality for irrigation during years of high flow and of very poor quality during years of low flow. The water in the lower reaches is of poor quality for industrial use because it is highly mineralized most of the tinge. Relations of suspended-sediment discharge to water discharge were used with the long-term streamflow duration curves to compute the long-term aver age suspended-sediment discharges and concentrations at five indications. Sediment discharge is closely related to runoff. S","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1651","usgsCitation":"Jordan, P.R., Jones, B., and Petri, L., 1964, Chemical quality of surface waters and sedimentation in the Saline River basin, Kansas: U.S. Geological Survey Water Supply Paper 1651, v, 90 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1651.","productDescription":"v, 90 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":110000,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24844.htm","linkFileType":{"id":5,"text":"html"},"description":"24844"},{"id":138366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1651/report-thumb.jpg"},{"id":27438,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27439,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27440,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27441,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27442,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27443,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1651/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4827e4b07f02db4e55e1","contributors":{"authors":[{"text":"Jordan, Paul Robert","contributorId":57819,"corporation":false,"usgs":true,"family":"Jordan","given":"Paul","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":144506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":144505,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, Lester R.","contributorId":19534,"corporation":false,"usgs":true,"family":"Petri","given":"Lester R.","affiliations":[],"preferred":false,"id":144504,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}