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,{"id":6495,"text":"pp516A - 1964 - Regional geologic implications of the gravity and magnetic fields of a part of eastern Tennessee and southern Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:53","indexId":"pp516A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"516","chapter":"A","title":"Regional geologic implications of the gravity and magnetic fields of a part of eastern Tennessee and southern Kentucky","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp516A","usgsCitation":"Watkins, J.S., 1964, Regional geologic implications of the gravity and magnetic fields of a part of eastern Tennessee and southern Kentucky: U.S. Geological Survey Professional Paper 516, p. A1-A17, https://doi.org/10.3133/pp516A.","productDescription":"p. A1-A17","costCenters":[],"links":[{"id":120743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0516a/report-thumb.jpg"},{"id":33950,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0516a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33951,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0516a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33952,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0516a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c537","contributors":{"authors":[{"text":"Watkins, Joel S.","contributorId":10788,"corporation":false,"usgs":true,"family":"Watkins","given":"Joel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":152823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2733,"text":"wsp1673 - 1964 - Magnitude and frequency of floods in the United States; part 2-A. South Atlantic slope basins, James River to Savannah River","interactions":[],"lastModifiedDate":"2022-01-07T20:41:08.645519","indexId":"wsp1673","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":"1673","title":"Magnitude and frequency of floods in the United States; 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/wsp1673","usgsCitation":"Speer, P.R., and Gamble, C.R., 1964, Magnitude and frequency of floods in the United States; part 2-A. South Atlantic slope basins, James River to Savannah River: U.S. Geological Survey Water Supply Paper 1673, Report: x, 329 p.; 3 Plates: 26.00 × 25.50 inches or smaller, https://doi.org/10.3133/wsp1673.","productDescription":"Report: x, 329 p.; 3 Plates: 26.00 × 25.50 inches or smaller","costCenters":[],"links":[{"id":29152,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1673/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29151,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1673/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29150,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1673/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29149,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1673/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1673/report-thumb.jpg"},{"id":110007,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24882.htm","linkFileType":{"id":5,"text":"html"},"description":"24882"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.5,\n              32.05\n            ],\n            [\n              -75.667,\n              32.05\n            ],\n            [\n              -75.667,\n              38.333\n            ],\n            [\n              -83.5,\n              38.333\n            ],\n            [\n              -83.5,\n              32.05\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495ce","contributors":{"authors":[{"text":"Speer, Paul R.","contributorId":24768,"corporation":false,"usgs":true,"family":"Speer","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, Charles R.","contributorId":6822,"corporation":false,"usgs":true,"family":"Gamble","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145683,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2797,"text":"wsp1608B - 1964 - Ground water in folded Cretaceous sandstone of the Bhachau area, Kutch, India, with reference to the Kandla Port water supply","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1608B","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":"1608","chapter":"B","title":"Ground water in folded Cretaceous sandstone of the Bhachau area, Kutch, India, with reference to the Kandla Port water supply","docAbstract":"This report is based on an investigation of the availability of ground-water supplies in the Bhachau area for the nearby Kandla Port and township development undertaken by the Government of India. This seaport lies on an estuary of the Gulf of Kutch in western India and in the eastern part of the State of Kutch. The fieldwork on the investigation was carried on from November 1952 through April 1953 with continuing hydrologic observations through 1954-55. The fieldwork included: geologic mapping and delimitation of the principal aquifers of the region; preparation of water-table maps; a detailed inventory of existing wells and springs; observations of significant water table fluctuations; preparation of isobicarb, isochlor and isosulf maps to show the areal distribution of ground-water salinity. \r\n\r\nThe Bhachau area includes about 116 square miles in eastern Kutch and lies in a belt of semiarid low-latitude steppes. The mean annual rainfall is about 15 inches, most of which falls from late June to late September during the southwest monsoon. The area includes a central sandy upland ranging from about 100 to 250 feet above sea level ; a northern lowland of between about 50 to 125 feet altitude that slopes north to the Great Rann of Kutch; a belt of low buttes and discontinuous ridges ranging from about 200 to 275 feet above sea level; and southern lowland which slopes in a southerly to southeasterly direction from an altitude of about 125 feet to 25 feet or less near the Gulf of Kutch. The principal streams are Kageshwar Vokra and Kara Vokra which drain north to the Great Rann and Kotwala Vokra and Dalwala Vokra which drain south toward the Gulf of Kutch. \r\n\r\nThe rocks of the Bhachau area include nonmarine and marine sediments of Mesozoic, Tertiary, and Quaternary age and volcanic rocks of late Mesozoic to early Tertiary age. The oldest rocks in the area are medium- to coarse-grained white to buff current-bedded friable sandstone with occasional partings of white silty shale of the Upper Bhuj series that has been assigned to the Early Cretaceous. The soft friable sandstone of the Upper Bhuj series constitutes the most productive ground-water reservoir in the Bhachau area. At present (1955) there are nine irrigated tracts for which water is obtained from dug wells less than 90 feet deep in the Upper Bhuj. These wells are worked by bullocks and 'motes' (leather bags) at withdrawal rates ranging from about 6,000 to 24,000imperial gallons per day; however, many existing individual wells if equipped with mechanical pumps are capable of yielding 100,000 gallons per day. The Deccan trap of Late Cretaceous to Eocene age occurs in a sequence of basaltic lava flows in the Bhachau area, but trap dikes, sills and plugs that are common in other parts of Kutch have not been observed in the area. Laterite of probable Eocene age is extensive at the top of the Deccan trap, and in places where the lava flows are thin the parent rock has been almost completely lateritized. The Deccan lava flows or the laterite, where the trap is absent, rest disconformably on the Upper Bhuj. No wells have been observed in the Deccan trap of the Bhachau area, but it is possible that locally small supplies of good water may be obtained from these rocks. \r\n\r\nThe Tertiary sediments, which are assigned to the Manchhar series of Pliocene age, generally rest on the laterite or the Deccan trap ; but where both are absent, the Manchhar rests directly on the Upper Bhuj. The Manchhar series includes massive reddish-brown gypseous clay shales, laminated gray siltstones, some limestone, mottled sandstone, and laterite trap gravel. Only meager supplies of brackish water are obtained from wells in these sediments. \r\n\r\nAlong the channels of Kotwala, Dalwala, Kageshwar, and Kara Vokras are narrow bands of unconsolidated coarse sand with fine gravel of Quaternary age. No wells were observed in these deposits, but it is possible that locally they may contain small supplies of bracki","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608B","usgsCitation":"Taylor, G., Osa, H., Mitra, A., and Sen, B., 1964, Ground water in folded Cretaceous sandstone of the Bhachau area, Kutch, India, with reference to the Kandla Port water supply: U.S. Geological Survey Water Supply Paper 1608, iv, 31 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1608B.","productDescription":"iv, 31 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608b/report-thumb.jpg"},{"id":29295,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29296,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29297,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29298,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66da12","contributors":{"authors":[{"text":"Taylor, George C.","contributorId":45693,"corporation":false,"usgs":true,"family":"Taylor","given":"George C.","affiliations":[],"preferred":false,"id":145810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osa, H.M.","contributorId":15594,"corporation":false,"usgs":true,"family":"Osa","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":145809,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitra, A.","contributorId":97077,"corporation":false,"usgs":true,"family":"Mitra","given":"A.","email":"","affiliations":[],"preferred":false,"id":145811,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sen, B.N.","contributorId":8079,"corporation":false,"usgs":true,"family":"Sen","given":"B.N.","email":"","affiliations":[],"preferred":false,"id":145808,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14992,"text":"ofr65109 - 1964 - Materials tests data, Franklin, Webster, and Nuckolls Counties, Nebraska","interactions":[],"lastModifiedDate":"2025-06-24T16:41:24.498663","indexId":"ofr65109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"65-109","title":"Materials tests data, Franklin, Webster, and Nuckolls Counties, Nebraska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65109","usgsCitation":"Miller, R.D., Van Horn, R., Dobrovolny, E., and Buck, L., 1964, Materials tests data, Franklin, Webster, and Nuckolls Counties, Nebraska: U.S. Geological Survey Open-File Report 65-109, Report: 6 p.; 3 Tables: 23.99 x 41.35 inches or smaller, https://doi.org/10.3133/ofr65109.","productDescription":"Report: 6 p.; 3 Tables: 23.99 x 41.35 inches or smaller","costCenters":[],"links":[{"id":491198,"rank":4,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1965/0109/Table-2.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"}},{"id":491199,"rank":5,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1965/0109/Table-3.pdf","text":"Table 3","linkFileType":{"id":1,"text":"pdf"}},{"id":491197,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1965/0109/Table-1.pdf","text":"Table 1","linkFileType":{"id":1,"text":"pdf"}},{"id":491196,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148775,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0109/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db60ff67","contributors":{"authors":[{"text":"Miller, Robert D.","contributorId":85168,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":170378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Horn, Richard","contributorId":52169,"corporation":false,"usgs":true,"family":"Van Horn","given":"Richard","email":"","affiliations":[],"preferred":false,"id":170377,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dobrovolny, Ernest","contributorId":45288,"corporation":false,"usgs":true,"family":"Dobrovolny","given":"Ernest","affiliations":[],"preferred":false,"id":170375,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buck, L.P.","contributorId":51306,"corporation":false,"usgs":true,"family":"Buck","given":"L.P.","email":"","affiliations":[],"preferred":false,"id":170376,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"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":2769,"text":"wsp1779P - 1964 - Geology and ground water of the Luke area, Maricopa County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1779P","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":"P","title":"Geology and ground water of the Luke area, Maricopa County, Arizona","docAbstract":"Luke Air Force Base, in the Salt River Valley in central Arizona. is within an intermontane basin--the Phoenix basin--in the Basin and Range lowlands province. The Luke area, the subject of this study, extends beyond the limits of the base. \r\n\r\nGround-water resources of the Luke area were studied to determine the possibility of developing a water supply of optimum quantity and quality to supplement the base supply. Several wells drilled for this purpose, prior to the study, either produced an inadequate supply of water or produced ware-that had a high dissolved-solids content. \r\n\r\nThe Phoenix basin is filled with unconsolidated to semiconsolidated Tertiary and Quaternary sedimentary rocks that are referred to as valley fill. Although its total thickness is unknown, 2,784 feet of valley fill--primarily consisting of clay, silt, sand, and gravel--has been penetrated. \r\n\r\nPercentage-distribution maps of fine-grained materials indicate a gross-facies pattern and a selective depositional area of the valley-fill materials. The maps also indicate that the areal distribution of fine-grained materials increases with depth. In general, the better producing wells, regardless of depth, are in areas where tee valley fill is composed of less than 60 percent fine-grained materials. The water table in the area is declining because large quantities of water are withdrawn and recharge is negligible. The decline near Luke Air Force Base during the period 1941-61 was about 150 feet. \r\n\r\nGround water was moving generally southwest in the spring of 1961. Locally, changes in the direction of movement indicate diversion toward two major depressions. \r\n\r\nThe dissolved-solids content of the ground water ranged from about 190 to 6,300 ppm. The highest concentration of dissolved solids is in water from the southern part of the area and seems to come from relatively shallow depths; wells in the northern part generally yield water of good quality. \r\n\r\nAfter a reconnaissance of the area, the U.S. Geological Survey located and supervised the drilling of two test wells--wells (B-2-1) 9bcb and (B-2-1) 5abc?on Luke Air Force Base. The quantity of water produced by the wells was adequate. The dissolved-solids content of water from the wells was low, and the overall quality of water from well (B-2-1) 5abc was good. When well (B-2-1) 9bcb was perforated between 907 and 977 feet, the water had a fluoride concentration of 4.4 ppm; however, the fluoride concentration decreased to 2.8 ppm when new perforations were cut at a shallower depth, and it was decided that dilution with other base water supplies probably would alleviate any possible fluoride problem.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1779P","usgsCitation":"Stulik, R.S., and Twenter, F.R., 1964, Geology and ground water of the Luke area, Maricopa County, Arizona: U.S. Geological Survey Water Supply Paper 1779, iv, 30 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1779P.","productDescription":"iv, 30 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779p/report-thumb.jpg"},{"id":29208,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779p/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29209,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779p/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29210,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779p/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29211,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779p/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29212,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779p/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29213,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779p/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29214,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779p/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635c47","contributors":{"authors":[{"text":"Stulik, Ronald S.","contributorId":44900,"corporation":false,"usgs":true,"family":"Stulik","given":"Ronald","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145754,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2732,"text":"wsp1676 - 1964 - Magnitude and frequency of floods in the United States. Part 3-B. Cumberland and Tennessee River basins","interactions":[],"lastModifiedDate":"2022-01-03T20:23:23.199318","indexId":"wsp1676","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":"1676","title":"Magnitude and frequency of floods in the United States. Part 3-B. Cumberland and Tennessee River basins","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1676","usgsCitation":"Speer, P.R., and Gamble, C.R., 1964, Magnitude and frequency of floods in the United States. Part 3-B. Cumberland and Tennessee River basins: U.S. Geological Survey Water Supply Paper 1676, Report: xii, 340 p.; 2 Plates: 27.00 × 18.00 inches, https://doi.org/10.3133/wsp1676.","productDescription":"Report: xii, 340 p.; 2 Plates: 27.00 × 18.00 inches","costCenters":[],"links":[{"id":393789,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24885.htm"},{"id":29148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1676/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29147,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1676/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29146,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1676/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1676/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia, Kentucky, Mississippi, North Carolina, South Carolina, Tennessee, Virginia","otherGeospatial":"Cumberland and Tennessee River basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.5,\n              34.192\n            ],\n            [\n              -81.3330,\n              34.192\n            ],\n            [\n              -81.3330,\n              37.5\n            ],\n            [\n              -88.5,\n              37.5\n            ],\n            [\n              -88.5,\n              34.192\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495dc","contributors":{"authors":[{"text":"Speer, Paul R.","contributorId":24768,"corporation":false,"usgs":true,"family":"Speer","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, C. R.","contributorId":26727,"corporation":false,"usgs":true,"family":"Gamble","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145682,"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}]}}
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,{"id":32742,"text":"pp377 - 1964 - Ore deposits of the St. Lawrence County magnetite district, northwest Adirondacks, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"pp377","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"377","title":"Ore deposits of the St. Lawrence County magnetite district, northwest Adirondacks, New York","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/pp377","usgsCitation":"Leonard, B.F., and Buddington, A.F., 1964, Ore deposits of the St. Lawrence County magnetite district, northwest Adirondacks, New York: U.S. Geological Survey Professional Paper 377, 259 p., https://doi.org/10.3133/pp377.","productDescription":"259 p.","costCenters":[],"links":[{"id":119248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0377/report-thumb.jpg"},{"id":260351,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-01.pdf"},{"id":260352,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-02.pdf"},{"id":260353,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-03.pdf"},{"id":260354,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-04.pdf"},{"id":260355,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-05.pdf"},{"id":260356,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-06.pdf"},{"id":260357,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-07.pdf"},{"id":260358,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-08.pdf"},{"id":260359,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-09.pdf"},{"id":260360,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-10.pdf"},{"id":260361,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-11.pdf"},{"id":260362,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-12.pdf"},{"id":260363,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-13.pdf"},{"id":260364,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-14.pdf"},{"id":260365,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-15.pdf"},{"id":260366,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-16.pdf"},{"id":260367,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-17.pdf"},{"id":260368,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-18.pdf"},{"id":260369,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-19.pdf"},{"id":260370,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-20.pdf"},{"id":260371,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0377/plate-21.pdf"},{"id":60658,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0377/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db69128a","contributors":{"authors":[{"text":"Leonard, B. F.","contributorId":32911,"corporation":false,"usgs":true,"family":"Leonard","given":"B.","middleInitial":"F.","affiliations":[],"preferred":false,"id":209078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buddington, A. F.","contributorId":40211,"corporation":false,"usgs":true,"family":"Buddington","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209079,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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