{"pageNumber":"2387","pageRowStart":"59650","pageSize":"25","recordCount":68846,"records":[{"id":13684,"text":"ofr7469 - 1974 - Ground-water management, Buzzards Bay coastal streams, Massachusetts and Rhode Island","interactions":[],"lastModifiedDate":"2019-11-25T13:57:22","indexId":"ofr7469","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-69","title":"Ground-water management, Buzzards Bay coastal streams, Massachusetts and Rhode Island","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/ofr7469","usgsCitation":"Frimpter, M.H., 1974, Ground-water management, Buzzards Bay coastal streams, Massachusetts and Rhode Island: U.S. Geological Survey Open-File Report 74-69, Report: 38 p.; 1 Plate: 40.70 x 28.45 inches, https://doi.org/10.3133/ofr7469.","productDescription":"Report: 38 p.; 1 Plate: 40.70 x 28.45 inches","costCenters":[],"links":[{"id":147721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0069/report-thumb.jpg"},{"id":369558,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0069/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":369557,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0069/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts, Rhode Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.17355346679688,\n              41.445814633981904\n            ],\n            [\n              -70.47866821289062,\n              41.445814633981904\n            ],\n            [\n              -70.47866821289062,\n              42.01869237684385\n            ],\n            [\n              -71.17355346679688,\n              42.01869237684385\n            ],\n            [\n              -71.17355346679688,\n              41.445814633981904\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66748a","contributors":{"authors":[{"text":"Frimpter, Michael H.","contributorId":8074,"corporation":false,"usgs":true,"family":"Frimpter","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":168229,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30625,"text":"wri7411 - 1974 - The effect of heated water on the temperature and evaporation of Hyco Lake, North Carolina, 1966-72","interactions":[],"lastModifiedDate":"2018-10-30T09:36:05","indexId":"wri7411","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-11","title":"The effect of heated water on the temperature and evaporation of Hyco Lake, North Carolina, 1966-72","docAbstract":"<p>Three levels of thermal loading of Hyco Lake by heat from two steam-electric generators have resulted in higher temperatures and increased evaporation in the 3,750-acre (1,518 square hectometer) lake. During the winter, local temperature increases of 34°F (19°C) were sometimes observed at the surface as heated water spread out on top of the cooler, more-dense, lake water, affecting areas as large as 2,590 acres (1,048 square hectometers) with temperature increases averaging up to 12°F (6.7°C) higher than natural lake temperatures. In the summer average temperature increases at the surface seldom exceeded 6°F (3.3°C) and the maximum area affected was 2,570 acres (1,040 square hectometers).</p><p>Forced evaporation from the heated part of Hyco Lake increased in proportion to the added heat, reaching a maximum of 23.1 inches (586 millimeters) in 1970, as compared to 55.6 inches (1,412 millimeters) of natural evaporation for that year.</p><p>In 1969, over the heated area, 210,600 British thermal units per square foot per year or 2,407,510,000 joules per square meter per year of heat were added to the lake. Of this amount, about 58 percent of the heat was utilized for evaporation, 24 percent for back radiation, 8.0 percent was conducted as sensible heat from the lake, 1.0 percent was removed through outflow, and 0.04 percent was advected by the evaporated water. These percentages are fairly typical of the first three stages of thermal loading.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7411","usgsCitation":"Yonts, W., and Giese, G.L., 1974, The effect of heated water on the temperature and evaporation of Hyco Lake, North Carolina, 1966-72: U.S. Geological Survey Water-Resources Investigations Report 74-11, v, 38 p., https://doi.org/10.3133/wri7411.","productDescription":"v, 38 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":159916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0011/report-thumb.jpg"},{"id":358927,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Hyco Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.19769287109375,\n              36.376791419469725\n            ],\n            [\n              -79,\n              36.376791419469725\n            ],\n            [\n              -79,\n              36.53143297936592\n            ],\n            [\n              -79.19769287109375,\n              36.53143297936592\n            ],\n            [\n              -79.19769287109375,\n              36.376791419469725\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66766f","contributors":{"authors":[{"text":"Yonts, W.L.","contributorId":93099,"corporation":false,"usgs":true,"family":"Yonts","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":203559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giese, G. L.","contributorId":44898,"corporation":false,"usgs":true,"family":"Giese","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":203558,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30059,"text":"wri741 - 1974 - Hydrologic conditions related to subsurface and surface disposal of wastes in Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-1","title":"Hydrologic conditions related to subsurface and surface disposal of wastes in Hawaii","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/wri741","usgsCitation":"Takasaki, K., 1974, Hydrologic conditions related to subsurface and surface disposal of wastes in Hawaii: U.S. Geological Survey Water-Resources Investigations Report 74-1, 5 fold. sheets (incl. illus., maps) in envelope. ;71 x 82cm. fold. to 21 x 25cm., https://doi.org/10.3133/wri741.","productDescription":"5 fold. sheets (incl. illus., maps) in envelope. ;71 x 82cm. fold. to 21 x 25cm.","costCenters":[],"links":[{"id":159303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":58871,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0001/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58872,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0001/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58868,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0001/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58869,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0001/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58870,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0001/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fe4e","contributors":{"authors":[{"text":"Takasaki, K. J.","contributorId":44523,"corporation":false,"usgs":true,"family":"Takasaki","given":"K. J.","affiliations":[],"preferred":false,"id":202607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15441,"text":"ofr7486 - 1974 - Response of ground-water levels of flood control operations in three basins, south-eastern Florida","interactions":[],"lastModifiedDate":"2025-08-04T17:44:08.754532","indexId":"ofr7486","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-86","title":"Response of ground-water levels of flood control operations in three basins, south-eastern Florida","docAbstract":"Three basins in southeastern Florida were investigated to determine the changes in ground-water levels and canal flows that occurred in response to operation of coastal water-control structures in each canal. All three basins are underlain by the Biscayne aquifer. They are, Snapper Creek Canal basin, where the Biscayne aquifer is of high permeability; the Snake Creek Canal basin, where the aquifer is of moderate permeability; and the Pompano-Cypress Canal basin, where the aquifer is of low permeability. In each basin, drainage is a function of permeability; thus, where the permeability of the aquifer is high, drainage is excellent. The coastal water-conrol structures are intended to afford flood protection in the three basins. In general the control operation criteria for flood control in newly developing areas in southeastern Florida do not provide adequate protection from flooding because of the time required for the aquifer to respond to changes in the controls. Adequate protection would require increasing the density of secondary drainage canals, but this could achieved only by reducing the quantity of water available for recharging those segments of the Biscayne aquifer adjacent to the canals. 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,{"id":66509,"text":"i878 - 1974 - Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah","interactions":[],"lastModifiedDate":"2025-08-13T19:30:55.69324","indexId":"i878","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"878","title":"Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah","docAbstract":"<p>The Navajo and Hopi Indian reservations are located mainly in northeastern Arizona, although the Navajo Indian reservation extends into northwestern New Mexico and southeastern Utah (see location map). The area of this report coincides with the areas of the Navajo and Hopi Indian reservations except in part of New Mexico, where the areas was extended eastward to longitude 108° and southward to Interstate Highway 40 and in southeastern Utah.</p><p>This investigation was conducted by the U.S. Geological Survey at the request of the Bureau of Indian Affairs. The study was undertaken to evaluate the potential for large-scale ground-water development in the Navajo and Hope Indian Reservations. The results given in this report are intended as preliminary guidelines for the development of ground water in sufficient quantity and of suitable quality for irrigation, municipal, and industrial uses. Data are not included for areas in which less than 25 gal min<sup>-1</sup> (gallons per minute) or 95 l min<sup>-1 </sup>(litres per minute) can be developed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i878","collaboration":"Prepared in cooperation with the Bureau of Indian Affairs","usgsCitation":"McGavock, E.H., and Edmonds, R.J., 1974, Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah: U.S. Geological Survey IMAP 878, 4 Sheets: 48.74 x 34.30 inches or smaller; Cover: 9.15 x 11.92 inches, https://doi.org/10.3133/i878.","productDescription":"4 Sheets: 48.74 x 34.30 inches or smaller; Cover: 9.15 x 11.92 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":494052,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9778.htm","linkFileType":{"id":5,"text":"html"}},{"id":255953,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-2.pdf","text":"Sheet 2: Areas where wells will yield at least 200 gallons per minute","size":"18.36 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0878/report-thumb.jpg"},{"id":255956,"rank":2,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0878/report.pdf","text":"Folio Cover","size":"30 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":255955,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-4.pdf","text":"Sheet 4: Areas where wells will yield at least 25 gallons per minute","size":"14.86 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255952,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-1.pdf","text":"Sheet 1: Areas where wells will yield at least 500 gallons per minute","size":"19.92 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255954,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-3.pdf","text":"Sheet 3: Areas where wells will yield at least 75 gallons per minute","size":"17.89 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"375000","country":"United States","state":"Arizona, New Mexico, Utah","otherGeospatial":"Navajo Indian Reservations, Hopi Indian Reservations","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,35 ], [ -112,37.5 ], [ -108,37.5 ], [ -108,35 ], [ -112,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667eda","contributors":{"authors":[{"text":"McGavock, E. H.","contributorId":40679,"corporation":false,"usgs":true,"family":"McGavock","given":"E.","middleInitial":"H.","affiliations":[],"preferred":false,"id":274633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edmonds, R. J.","contributorId":78825,"corporation":false,"usgs":true,"family":"Edmonds","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":274634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26895,"text":"wri7417 - 1974 - Hydrologic analysis of the Mojave River, California, using a mathematical model","interactions":[],"lastModifiedDate":"2018-10-29T14:32:18","indexId":"wri7417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-17","title":"Hydrologic analysis of the Mojave River, California, using a mathematical model","docAbstract":"<p>The channel of the Mojave Rive'r in California is normally dry and is highly permeable over much of its length, and large quantities of water from natural floodflows in the channel infiltrate through the channel bed to the underlying ground-water body. From 1930 to 1972 only 18 floods at The Forks produced flow at Barstow, 55 miles (88 kilometres) downstream from The Forks. Peak discharges at Barstow from these floods ranged from 180 cubic feet per second (5 cubic metres per second) in 1967 to 64,300 cubic feet per second (1,820 cubic metres per second) in 1938. Total stream infiltration, primarily as ground-water recharge, ranged from 3,600 acre-feet (4.40 cubic hectometres) in 1935 to 50,400 acre-feet (62.1 cubic hectometres) in 1969 between The Forks and Victorville and from about 7,000 acre-feet (8.61 cubic hectometres) in 1935 to 128,000 acre-feet (158 cubic hectometres) in 1969 between Victorville and Barstow.</p><p>The Mojave Water Agency is considering the use of the channel of the river to convey water imported from northern California through Silverwood Reservoir (5 miles or 8 kilometres upstream from The Forks) downstream to the Barstow area. The imported water would be used to replenish aquifers underlying the Barstow area. A mathematical model was developed that simulates the advance of discharge down the initially dry channel of the Mojave River, and the model was used to evaluate the potential of the channel to move imported water downstream to Barstow.</p><p>Results of simulation by modeling indicate that the channel of the Mojave River can be used to efficiently convey imported water to Barstow only when the absorption capacity of the channel has been reduced by an antecedent flood. The volume of imported water that can reach Barstow depends on the volume and duration of the antecedent flood, on the volume of imported water released trom Silverwood Reservoir, and on the rate at which imported water is released. A release of 20,000 acre-feet (24.6 cubic hectometres) of imported water may produce at Barstow a maximum volume of imported water of 2,500, 8,000, 11,000, or 15,000 acre-feet (3.08, 9.86, 13.6, or 18.4 cubic hectometres) for a release rate of 500, 750, 1,000, or 2,000 cubic feet per second (14.2, 21.2, 28.3, or 56.8 cubic metres per second).</p><p>For planning purposes in evaluating some of the hydraulic effects of recharge on the aquifer, a simulation of the aquifer near the Barstow area using an electrical analog model showed that a combination of no pumping and a yearly recharge of 5,000 acre-feet (6.17 cubic hectometres) for 10 years could raise ground-water levels at least 10 feet (3 metres) over an area of about 10 square miles (25 square kilometres). To obtain the water-level changes due to the combined effects of pumping and recharge, the above water-level changes should be superimposed on the separate effects of pumping.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7417","usgsCitation":"Durbin, T.J., and Hardt, W.F., 1974, Hydrologic analysis of the Mojave River, California, using a mathematical model: U.S. Geological Survey Water-Resources Investigations Report 74-17, v, 50 p., https://doi.org/10.3133/wri7417.","productDescription":"v, 50 p.","costCenters":[],"links":[{"id":157467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0017/report-thumb.jpg"},{"id":358909,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0017/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Mojave River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.42187500000001,\n              34.26289150646404\n            ],\n            [\n              -117.00576782226562,\n              34.26289150646404\n            ],\n            [\n              -117.00576782226562,\n              34.91521472314689\n            ],\n            [\n              -117.42187500000001,\n              34.91521472314689\n            ],\n            [\n              -117.42187500000001,\n              34.26289150646404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611900","contributors":{"authors":[{"text":"Durbin, Timothy J.","contributorId":63373,"corporation":false,"usgs":true,"family":"Durbin","given":"Timothy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardt, W. F.","contributorId":12455,"corporation":false,"usgs":true,"family":"Hardt","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197203,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56448,"text":"wdrAR732 - 1974 - Water resources data for Arkansas, water year 1973; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:17","indexId":"wdrAR732","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-73-2","title":"Water resources data for Arkansas, water year 1973; Part 2, Water quality records","language":"ENGLISH","doi":"10.3133/wdrAR732","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for Arkansas, water year 1973; Part 2, Water quality records: U.S. Geological Survey Water Data Report AR-73-2, 247 p., https://doi.org/10.3133/wdrAR732.","productDescription":"247 p.","costCenters":[],"links":[{"id":185114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f775b","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":532629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":217,"text":"wsp2150 - 1974 - Quality of surface waters of the United States, 1969, Parts 12-16, North Pacific slope basins, Alaska, Hawaii, and other Pacific areas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp2150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"2150","title":"Quality of surface waters of the United States, 1969, Parts 12-16, North Pacific slope basins, Alaska, Hawaii, and other Pacific areas","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/wsp2150","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Quality of surface waters of the United States, 1969, Parts 12-16, North Pacific slope basins, Alaska, Hawaii, and other Pacific areas: U.S. Geological Survey Water Supply Paper 2150, xiii, 480 p. :tables ;23 cm., https://doi.org/10.3133/wsp2150.","productDescription":"xiii, 480 p. :tables ;23 cm.","costCenters":[],"links":[{"id":137370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2150/report-thumb.jpg"},{"id":24828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2150/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6518dc","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":527246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3602,"text":"cir690 - 1974 - Seismic hazards and land-use planning","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"cir690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"690","title":"Seismic hazards and land-use planning","docAbstract":"Basic earth-science data are necessary for a realistic assessment of seismic hazards and as a basis for limiting corrective land-use controls only to those areas of greatest hazard. For example, the location, character, and amount of likely displacement and activity of surface faulting can be predicted if detailed geologic maps and seismic data are available and are augmented by field studies at critical localities. Because few structures can withstand displacement of their foundations, they should be located off active fault traces, the distance varying with the character of faulting, the certainty with which fault traces are known, and the importance of the structure. Recreational activities and other nonoccupancy land uses should be considered for fault zone areas where land is under pressure for development; elsewhere, such areas should remain as open space. \r\n\r\nTwo methods of predicting ground shaking effects have applications to land-use decisions: (1) Relative earthquake effects can be related to firmness of the ground and can be used in a gross way to allocate population density in the absence of more sophisticated analyses; and (2) intensity maps, based on, (a) damage from former earthquakes, or (b) a qualitative analyses of geologic units added to a design earthquake, can be helpful both for general and specific plans. Theoretical models are used with caution to predict ground motion for critical structures to be located at specific sites with unique foundation conditions. Fully adequate methods of assessing possible shaking remain to be developed. Where land-use decisions do not reflect likely ground shaking effects, stringent building codes are needed, particularly for important structures. \r\n\r\nGround failure (landsliding, ground cracking and lurching, differential settlement, sand boils, and subsidence) commonly results from liquefaction, loss of soil strength, or compaction. Areas suspected of being most likely to fail should not be developed unless detailed site studies can demonstrate the hazard does not exist or can be overcome. Various methods can be used to reduce the high, long-term public costs that follow development of unstable ground. However, areas subject to tectonic deformation generally cannot be predicted nor can effects of such deformation be minimized. \r\n\r\nLarge water waves, such as produced by tsunamis, seiches, and dam failure or overtopping, can be anticipated in many places. Their effects can be lessened by land-use regulations similar to flood-plain zoning, restrictions on location of critical structures, and appropriate warning systems. \r\n\r\nMany local, state, and federal government agencies, universities, and private consultants may be able to assist planners by advising them of pertinent data and where those data can be obtained. Interpretation of the data for an evaluation of seismic risk commonly requires a team of planners, geologists, and soil and structural engineers.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir690","usgsCitation":"Nichols, D.R., and Buchanan-Banks, J.M., 1974, Seismic hazards and land-use planning: U.S. Geological Survey Circular 690, iv, 33 p. :ill. ;27 cm., https://doi.org/10.3133/cir690.","productDescription":"iv, 33 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":124619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1974/0690/report-thumb.jpg"},{"id":30637,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1974/0690/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a879b","contributors":{"authors":[{"text":"Nichols, Donald R.","contributorId":83129,"corporation":false,"usgs":true,"family":"Nichols","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":147239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchanan-Banks, Jane M.","contributorId":29421,"corporation":false,"usgs":true,"family":"Buchanan-Banks","given":"Jane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147238,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47191,"text":"ofr7432 - 1974 - Formation factors and their use in estimating water quality in Mississippi aquifers","interactions":[{"subject":{"id":47191,"text":"ofr7432 - 1974 - Formation factors and their use in estimating water quality in Mississippi aquifers","indexId":"ofr7432","publicationYear":"1974","noYear":false,"title":"Formation factors and their use in estimating water quality in Mississippi aquifers"},"predicate":"SUPERSEDED_BY","object":{"id":47632,"text":"wri752 - 1975 - Formation factors and their use in estimating water quality in Mississippi aquifers","indexId":"wri752","publicationYear":"1975","noYear":false,"title":"Formation factors and their use in estimating water quality in Mississippi aquifers"},"id":1}],"supersededBy":{"id":47632,"text":"wri752 - 1975 - Formation factors and their use in estimating water quality in Mississippi aquifers","indexId":"wri752","publicationYear":"1975","noYear":false,"title":"Formation factors and their use in estimating water quality in Mississippi aquifers"},"lastModifiedDate":"2013-01-17T11:41:18","indexId":"ofr7432","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-32","title":"Formation factors and their use in estimating water quality in Mississippi aquifers","language":"ENGLISH","doi":"10.3133/ofr7432","usgsCitation":"Newcome, R., 1974, Formation factors and their use in estimating water quality in Mississippi aquifers: U.S. Geological Survey Open-File Report 74-32, 1 sheet, https://doi.org/10.3133/ofr7432.","productDescription":"1 sheet","costCenters":[],"links":[{"id":135236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de086","contributors":{"authors":[{"text":"Newcome, Roy Jr.","contributorId":12443,"corporation":false,"usgs":true,"family":"Newcome","given":"Roy","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":234797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56447,"text":"wdrAR731 - 1974 - Water resources data for Arkansas, water year 1973; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"wdrAR731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-73-1","title":"Water resources data for Arkansas, water year 1973; Part 1, Surface water records","language":"ENGLISH","doi":"10.3133/wdrAR731","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for Arkansas, water year 1973; Part 1, Surface water records: U.S. Geological Survey Water Data Report AR-73-1, 137 p., https://doi.org/10.3133/wdrAR731.","productDescription":"137 p.","costCenters":[],"links":[{"id":184130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7757","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":532628,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56452,"text":"wdrAL731 - 1974 - Water resources data for Alabama, water year 1973; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:17","indexId":"wdrAL731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AL-73-1","title":"Water resources data for Alabama, water year 1973; Part 1, Surface water records","language":"ENGLISH","doi":"10.3133/wdrAL731","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for Alabama, water year 1973; Part 1, Surface water records: U.S. Geological Survey Water Data Report AL-73-1, 153 p., https://doi.org/10.3133/wdrAL731.","productDescription":"153 p.","costCenters":[],"links":[{"id":185118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f78ce","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":532633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41727,"text":"ofr7412 - 1974 - Aeromagnetic map of parts of the Cleveland and Erie 1° by 2° quadrangles, Pennsylvania","interactions":[],"lastModifiedDate":"2021-09-27T18:45:22.993482","indexId":"ofr7412","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-12","title":"Aeromagnetic map of parts of the Cleveland and Erie 1° by 2° quadrangles, Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7412","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Aeromagnetic map of parts of the Cleveland and Erie 1° by 2° quadrangles, Pennsylvania: U.S. Geological Survey Open-File Report 74-12, 1 Plate: 27.96 × 36.68 inches, https://doi.org/10.3133/ofr7412.","productDescription":"1 Plate: 27.96 × 36.68 inches","costCenters":[],"links":[{"id":168265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389825,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14999.htm"},{"id":79439,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0012/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Pennsylvania","otherGeospatial":"Cleveland and Erie 1° by 2° quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.6290,\n              41.362\n            ],\n            [\n              -80,\n              41.362\n            ],\n            [\n              -80,\n              42.169\n            ],\n            [\n              -80.6290,\n              42.169\n            ],\n            [\n              -80.6290,\n              41.362\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69772e","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":530590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68394,"text":"ha506 - 1974 - Hydrology and water resources of the Deerfield River basin, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:11:27","indexId":"ha506","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"506","title":"Hydrology and water resources of the Deerfield River basin, Massachusetts","language":"ENGLISH","doi":"10.3133/ha506","usgsCitation":"Gay, F.B., Toler, L., and Hansen, B.P., 1974, Hydrology and water resources of the Deerfield River basin, Massachusetts: U.S. Geological Survey Hydrologic Atlas 506, 8 col. maps on 2 sheets ;113 x 87 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha506.","productDescription":"8 col. maps on 2 sheets ;113 x 87 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":185700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89894,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/506/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89895,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/506/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,41.08416666666667 ], [ -77.5,41.166666666666664 ], [ -77.36749999999999,41.166666666666664 ], [ -77.36749999999999,41.08416666666667 ], [ -77.5,41.08416666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604d08","contributors":{"authors":[{"text":"Gay, Frederick B.","contributorId":102052,"corporation":false,"usgs":true,"family":"Gay","given":"Frederick","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":278143,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toler, L.G.","contributorId":98710,"corporation":false,"usgs":true,"family":"Toler","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":278142,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hansen, Bruce P.","contributorId":90727,"corporation":false,"usgs":true,"family":"Hansen","given":"Bruce","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":278141,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11835,"text":"ofr74360 - 1974 - Aeromagnetic map of the New Madrid region, Missouri-Kentucky-Arkansas-Tennessee","interactions":[],"lastModifiedDate":"2023-01-06T20:30:32.722352","indexId":"ofr74360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-360","title":"Aeromagnetic map of the New Madrid region, Missouri-Kentucky-Arkansas-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74360","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Aeromagnetic map of the New Madrid region, Missouri-Kentucky-Arkansas-Tennessee: U.S. Geological Survey Open-File Report 74-360, 1 Plate: 48.00 x 42.00 inches, https://doi.org/10.3133/ofr74360.","productDescription":"1 Plate: 48.00 x 42.00 inches","costCenters":[],"links":[{"id":145801,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411517,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15057.htm","linkFileType":{"id":5,"text":"html"}},{"id":95033,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0360/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Arkansas, Kentucky, Missouri, Tennessee","otherGeospatial":"New Madrid region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -90.5,\n              37\n            ],\n            [\n              -90.5,\n              36.083\n            ],\n            [\n              -89,\n              36.083\n            ],\n            [\n              -89,\n              37\n            ],\n            [\n              -90.5,\n              37\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cc8","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":528904,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42048,"text":"ofr74206 - 1974 - Aeromagnetic map of Frederick County, Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"ofr74206","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-206","title":"Aeromagnetic map of Frederick County, Maryland","language":"ENGLISH","doi":"10.3133/ofr74206","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Aeromagnetic map of Frederick County, Maryland: U.S. Geological Survey Open-File Report 74-206, 1 map; scale = 1:62500, https://doi.org/10.3133/ofr74206.","productDescription":"1 map; scale = 1:62500","costCenters":[],"links":[{"id":136609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98779,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0206/plate-1.pdf","size":"9418","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698232","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":530798,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":212,"text":"wsp2142 - 1974 - Quality of surface waters of the United States, 1969, Part 2, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp2142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"2142","title":"Quality of surface waters of the United States, 1969, Part 2, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2142","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Quality of surface waters of the United States, 1969, Part 2, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 2142, x, 625 p. ;23 cm., https://doi.org/10.3133/wsp2142.","productDescription":"x, 625 p. ;23 cm.","costCenters":[],"links":[{"id":136029,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2142/report-thumb.jpg"},{"id":24823,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db65190b","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":527241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41581,"text":"ofr74326 - 1974 - Availability and use of ground water on north coast of Long Island Sound, western Long Island Sound","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"ofr74326","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-326","title":"Availability and use of ground water on north coast of Long Island Sound, western Long Island Sound","language":"ENGLISH","doi":"10.3133/ofr74326","usgsCitation":"Melvin, R., and Haeni, F., 1974, Availability and use of ground water on north coast of Long Island Sound, western Long Island Sound: U.S. Geological Survey Open-File Report 74-326, 1 map, https://doi.org/10.3133/ofr74326.","productDescription":"1 map","costCenters":[],"links":[{"id":172951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79314,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0326/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667fd3","contributors":{"authors":[{"text":"Melvin, R.L.","contributorId":50497,"corporation":false,"usgs":true,"family":"Melvin","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":225250,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":225251,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2673,"text":"wsp2031 - 1974 - Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp2031","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"2031","title":"Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York","docAbstract":"An investigation of recharge basins on Long Island was made by the U.S. Geological Survey in cooperation with the New York State Department of Environmental Conservation, Nassau County Department of Public Works, Suffolk County Department of Environmental Control, and Suffolk County Water Authority. The major objectives of the study were to (1) catalog basic physical data on the recharge basins in use on Long Island, (2) measure quality and quantity of precipitation and inflow, (3) measure infiltration rates at selected recharge basins, and (4) evaluate regional effects of recharge basins on the hydrologic system of Long Island. The area of study consists of Nassau and Suffolk Counties -- about 1,370 square miles -- in eastern Long Island, N.Y. \r\n\r\nRecharge basins, numbering more than 2,100 on Long Island in 1969, are open pits in moderately to highly permeable sand and gravel deposits. These pits are used to dispose of storm runoff from residential, industrial, and commercial areas, and from highways, by infiltration of the water through the bottom and sides of the basins. \r\n\r\nThe hydrology of three recharge basins on Long Island -- Westbury, Syosset, and Deer Park basins -- was studied. The precipitation-inflow relation showed that the average percentages of precipitation flowing into each basin were roughly equivalent to the average percentages of impervious areas in the total drainage areas of the basins. Average percentages of precipitation flowing into the basins as direct runoff were 12 percent at the Westbury basin, 10 percent at the Syosset basin, and 7 percent at the Deer Park basin. Numerous open-bottomed storm-water catch basins at Syosset and Deer Park reduced the proportion of inflow to those basins, as compared with the Westbury basin, which has only a few open-bottomed catch basins. \r\n\r\nInflow hydrographs for each basin typify the usual urban runoff hydrograph -- steeply rising and falling limbs, sharp peaks, and short time bases. Unit hydrographs for the Westbury and the Syosset basins are not expected to change; however, the unit hydrograph for the Deer Park basin is expected to broaden somewhat as a result of additional future house construction within the drainage area. \r\n\r\nInfiltration rates averaged 0.9 fph (feet per hour) for 63 storms between July 1967 and May 1970 at the Westbury recharge basin, 0.8 fph for 22 storms from July 1969 to September 1970 at the Syosset recharge basin, and 0.2 fph for 24 storms from March to September 1970 at the Deer Park recharge basin. Low infiltration rates at Deer Park resulted mainly from (1) a high percentage of eroded silt, clay, and organic debris washed in from construction sites in the drainage area, which partly filled the interstices of the natural deposits, and (2) a lack of a well-developed plant-root system on the floor of the younger basin, which would have kept the soil zone more permeable. \r\n\r\nThe apparent rate of movement of storm water through the unsaturated zone below each basin averaged 5.5 fph at Westbury, 3.7 fph at Syosset, and 3.1 fph at Deer Park. The rates of movement for storms during the warm months (April through October) were slightly higher than average, probably because the recharging water was warmer than it was during the rest of the year, and therefore, was slightly less viscous.\r\n\r\nOn the average, a 1-inch rainfall resulted in a peak rise of the water table directly below each basin of 0.5 foot; a 2-inch rainfall resulted in a peak rise of about 2 feet. The mound commonly dissipated within 1 to 4 days at Westbury, 7 days to more than 15 days at Syosset, and 1 to 3 days at Deer Park, depending on the magnitude of the peak buildup. \r\n\r\nAverage annual ground-water recharge was estimated to be 6.4 acre-feet at the Westbury recharge basin, 10.3 acre-feet at the Syosset recharge basin, and 29.6 acre-feet at the Deer Park recharge basin. \r\n\r\nChemical composition of precipitation at Westbury, Syosset, and Deer Park drainage areas was similar: ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2031","usgsCitation":"Seaburn, G., and Aronson, D.A., 1974, Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York: U.S. Geological Survey Water Supply Paper 2031, vi, 66 p. :ill. (1 fold. in pocket) ;23 cm., https://doi.org/10.3133/wsp2031.","productDescription":"vi, 66 p. :ill. (1 fold. in pocket) ;23 cm.","costCenters":[],"links":[{"id":138260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2031/report-thumb.jpg"},{"id":247234,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2031/plate-1.pdf","size":"1142","linkFileType":{"id":1,"text":"pdf"}},{"id":29023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ede49","contributors":{"authors":[{"text":"Seaburn, G.E.","contributorId":42193,"corporation":false,"usgs":true,"family":"Seaburn","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":145593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aronson, D. A.","contributorId":20308,"corporation":false,"usgs":true,"family":"Aronson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28784,"text":"wri749 - 1974 - Seawater intrusion, ground-water pumpage, ground-water yield, and artificial recharge of the Pajaro Valley area, Santa Cruz and Monterey Counties, California","interactions":[],"lastModifiedDate":"2018-10-31T13:56:49","indexId":"wri749","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-9","title":"Seawater intrusion, ground-water pumpage, ground-water yield, and artificial recharge of the Pajaro Valley area, Santa Cruz and Monterey Counties, California","docAbstract":"<p>The Pajaro Valley area, California, covering about 120 square miles (310 km<sup>2</sup>), extends from the southern part of Santa Cruz County to several miles south of the county line into Monterey County. It borders the Pacific Ocean on the west and the Santa Cruz Mountains on the east. The city of Watsonville is the largest center of population.</p><p>Seawater intrusion is occurring in the Pajaro Valley area from several miles north to several miles south of the mouth of the Pajaro River and in a small area about 4 miles (6.5 km) north of the river. The intrusion extends inland about 1 mile (1.6 km). Two water-bearing zones are being intruded--the depth intervals 100-200 feet (30-60 m) and 300-600 feet (90-180 m).</p><p>Ground-water pumpage averaged 49,100 acre-feet per year (60.6 hm<sup>3</sup>/yr) for the 9-year period 1963-71. The long-term ground-water yield of the Pajaro Valley is about 44,000 acre-feet per year (54.3 hm<sup>3</sup>/yr). Artificial recharge can be effected through modified streambeds at infiltration rates as high as 3 feet per day (0.9 m/d). Injection wells may have recharge capabilities of as much as 500 gallons per minute (1.9 m<sup>3</sup>/min).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri749","usgsCitation":"Muir, K.S., 1974, Seawater intrusion, ground-water pumpage, ground-water yield, and artificial recharge of the Pajaro Valley area, Santa Cruz and Monterey Counties, California: U.S. Geological Survey Water-Resources Investigations Report 74-9, iv, 31 p., https://doi.org/10.3133/wri749.","productDescription":"iv, 31 p.","costCenters":[],"links":[{"id":159106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0009/report-thumb.jpg"},{"id":359035,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Monterey County, Santa Cruz County","otherGeospatial":"Pajaro Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.85760498046875,\n              36.8333\n            ],\n            [\n              -121.7833,\n              36.8333\n            ],\n            [\n              -121.7833,\n              36.9167\n            ],\n            [\n              -121.85760498046875,\n              36.9167\n            ],\n            [\n              -121.85760498046875,\n              36.8333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc2c4","contributors":{"authors":[{"text":"Muir, K. S.","contributorId":53764,"corporation":false,"usgs":true,"family":"Muir","given":"K.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200390,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28989,"text":"wri7345 - 1974 - Base and thickness of the Post-Eocene continental deposits in the Sacramento Valley, California","interactions":[],"lastModifiedDate":"2018-10-29T13:43:43","indexId":"wri7345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-45","title":"Base and thickness of the Post-Eocene continental deposits in the Sacramento Valley, California","docAbstract":"<p>The Sacramento Valley, which forms most of the northern one-third of the Central Valley, is a broad structural trough. The study area comprises the valley floor and some of the foothills of the Sierra Nevada and the Coast Ranges, a total area of about 6,000 square miles.</p><p>Beneath most places in the valley, the base of the post-Eocene continental deposits is equivalent to the base of the Tehama Formation of Pliocene age, which in some places at least may be of late Oligocene and early Miocene age. The deposits consist of intercalated beds of gravel, sand, silt, clay, tuff, conglomerate, sandstone, siltstone, and claystone. And beneath large areas along the eastern side of the valley the deposits consist of basaltic and andesitic mudflows, tuff, tuff breccias, volcanic sandstones and conglomerates, and sand and gravel, as well as overlying nonvolcanic sediments. They contain most of the fresh ground water in the valley.</p><p>The structure of the base of the continental deposits is that of a large northward-trending syncline whose trend is interrupted only by the Sutter Buttes. In the subsurface, faulting has occurred mostly within the basal part of the deposits. Beneath the northeastern part of the valley, along the Chico monocline, faulting has occurred through probably the total thickness of the deposits.</p><p>The deposits range in thickness from zero near the margins of the valley to about 3,500 feet beneath the south-central part of the valley. The thickest sections occur along the axis of the syncline, but near Sutter Buttes the deposits are thinner than at any other locale near the central part of the valley.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7345","usgsCitation":"Page, R.W., 1974, Base and thickness of the Post-Eocene continental deposits in the Sacramento Valley, California: U.S. Geological Survey Water-Resources Investigations Report 73-45, iii, 16 p., https://doi.org/10.3133/wri7345.","productDescription":"iii, 16 p.","costCenters":[],"links":[{"id":439031,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9XQ1CQF","text":"USGS data release","linkHelpText":"Digital subsurface data from previously published maps of the base and thickness of post-Eocene continental deposits in the Sacramento Valley, California"},{"id":158885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0045/report-thumb.jpg"},{"id":358896,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Sacramento Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.904052734375,\n              38.013476231041935\n            ],\n            [\n              -120.70678710937499,\n              38.013476231041935\n            ],\n            [\n              -120.70678710937499,\n              40.64730356252251\n            ],\n            [\n              -122.904052734375,\n              40.64730356252251\n            ],\n            [\n              -122.904052734375,\n              38.013476231041935\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6492b6","contributors":{"authors":[{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200745,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28648,"text":"wri7429 - 1974 - Preconstruction assessment of biological quality of the Chena and Little Chena Rivers in the vicinity of the Chena Lakes Flood Control Project near Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2019-11-25T14:14:27","indexId":"wri7429","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-29","title":"Preconstruction assessment of biological quality of the Chena and Little Chena Rivers in the vicinity of the Chena Lakes Flood Control Project near Fairbanks, Alaska","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7429","usgsCitation":"McCoy, G.A., 1974, Preconstruction assessment of biological quality of the Chena and Little Chena Rivers in the vicinity of the Chena Lakes Flood Control Project near Fairbanks, Alaska: U.S. Geological Survey Water-Resources Investigations Report 74-29, 84 p. , https://doi.org/10.3133/wri7429.","productDescription":"84 p. ","costCenters":[],"links":[{"id":158294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0029/report-thumb.jpg"},{"id":369561,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","city":"Fairbanks","otherGeospatial":"Chena, Little Chena Rivers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.98583984375,\n              64.7747105865518\n            ],\n            [\n              -147.60269165039062,\n              64.7747105865518\n            ],\n            [\n              -147.60269165039062,\n              64.86819106223713\n            ],\n            [\n              -147.98583984375,\n              64.86819106223713\n            ],\n            [\n              -147.98583984375,\n              64.7747105865518\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680478","contributors":{"authors":[{"text":"McCoy, George A.","contributorId":20300,"corporation":false,"usgs":true,"family":"McCoy","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200169,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14210,"text":"ofr7465 - 1974 - Soft-water zone in the Chicot Aquifer, Bayou Teche area, Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:51","indexId":"ofr7465","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-65","title":"Soft-water zone in the Chicot Aquifer, Bayou Teche area, Louisiana","docAbstract":"Test drilling in the vicinity of Bayou Teche in St. Martin Parish in southern Louisiana has disclosed a zone of soft water in the basal unit of the Chicot aquifer; the Chicot aquifer system blankets all southwestern Louisiana. Fresh water, which is defined as containing 250 milligrams per liter chloride or less, in the Chicot aquifer is characteristically hard and high in iron concentration; in this area the hardness is generally 200-300 milligrams per liter. The soft-water zone, containing water with a hardness of less than 60 milligrams per liter, is anomalous and occurs in an area where the basal part of the aquifer is separated from the main body of the aquifer by a thick clay layer. The zone has been mapped in parts of St. Martin and adjoining Lafayette Parishes.\r\n\r\nAlthough the exact areal extent of the zone cannot be determined with available data, it appears to be sufficiently large that the soft water should prove to be an important asset to the area. The water could be used by itself or mixed with either hard or slightly salty water (more than 250 milligrams per liter chloride) to provide a blend that would require little or no treatment for most purposes. Because of the proximity of salty water in much of the area, careful planning and monitoring will be necessary to maintain the soft-water zone as a dependable supply of usable water. The soft water appears to be an exhaustible supply; however, its useful life as a resource can be maximized by proper management.","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr7465","usgsCitation":"Hosman, R., 1974, Soft-water zone in the Chicot Aquifer, Bayou Teche area, Louisiana: U.S. Geological Survey Open-File Report 74-65, iii, 20 leaves :ill ;29 cm.; (31 p., 5 sheets - PGS), https://doi.org/10.3133/ofr7465.","productDescription":"iii, 20 leaves :ill ;29 cm.; (31 p., 5 sheets - PGS)","costCenters":[],"links":[{"id":147341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0065/report-thumb.jpg"},{"id":42888,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42889,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42890,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42891,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42892,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42893,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42894,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42895,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42896,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42897,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0065/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42898,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5edce0","contributors":{"authors":[{"text":"Hosman, R. L.","contributorId":42978,"corporation":false,"usgs":true,"family":"Hosman","given":"R.","middleInitial":"L.","affiliations":[],"preferred":false,"id":169087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28777,"text":"wri7333 - 1974 - Temperature and chemical data for selected thermal wells and springs in southeastern California","interactions":[],"lastModifiedDate":"2021-03-04T00:29:06.938136","indexId":"wri7333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-33","title":"Temperature and chemical data for selected thermal wells and springs in southeastern California","docAbstract":"<p><span>This report lists data on temperature and chemical quality for 95 wells </span><span>or springs in southeastern California that contain water in excess of </span><span>38</span><span>°</span><span>C (Celsius) or 100</span><span>°</span><span>F (Fahrenheit). The highest temperature listed is </span><span>280</span><span>°</span><span>C (536</span><span>°</span><span>F). </span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7333","usgsCitation":"Moyle, W.R., 1974, Temperature and chemical data for selected thermal wells and springs in southeastern California: U.S. Geological Survey Water-Resources Investigations Report 73-33, Report: iii, 12 p.; 1 Plate: 26.20 x 22.90 inches, https://doi.org/10.3133/wri7333.","productDescription":"Report: iii, 12 p.; 1 Plate: 26.20 x 22.90 inches","costCenters":[],"links":[{"id":383803,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/wri/1973/0033/figure-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383802,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159584,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0033/report-thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.0703125,\n              33.687781758439364\n            ],\n            [\n              -114.08203125,\n              33.687781758439364\n            ],\n            [\n              -114.08203125,\n              36.63316209558658\n            ],\n            [\n              -117.0703125,\n              36.63316209558658\n            ],\n            [\n              -117.0703125,\n              33.687781758439364\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685806","contributors":{"authors":[{"text":"Moyle, W. R. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200378,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14209,"text":"ofr74271 - 1974 - Geothermal systems of northern Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:51","indexId":"ofr74271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-271","title":"Geothermal systems of northern Nevada","docAbstract":"Hot springs are numerous and nearly uniformly distributed in northern Nevada. Most occur on the flanks of basins, along Basin and Range (late Miocene to Holocene) faults, while some occur in the inner parts of the basins. Surface temperatures of the springs range from slightly above ambient to, boiling; some springs are superheated. Maximum subsurface water temperatures calculated on the basis of quartz solubility range as high as 252?C, although most are below 190?C. Flows range from a trickle to several hundred liters per minute. \r\n\r\nThe Nevada geothermal systems differ markedly from the power-producing system at The Geysers, Calif., and from those areas with a high potential, for power production (e.g., Yellowstone Park, Wyo.; Jemez Mountains, N. Mex.). These other systems are associated with Quaternary felsic volcanic rocks and probably derive their heat from cooling magma rather high in the crust. In northern Nevada, however, felsic volcanic rocks are virtually all older than 10 million years, and. analogous magmatic heat sources are, therefore, probably lacking. \r\n\r\nNevada is part of an area of much higher average heat flow than the rest of the United States. In north-central Nevada, geothermal gradients are as great as 64?C per kilometer in bedrock and even higher in basin fill. The high gradients probably result from a combination of thin crust and high temperature upper mantle. \r\n\r\nWe suggest that the geothermal systems of northern Nevada result from circulation of meteoric waters along Basin and Range faults and that their temperature chiefly depends upon (1) depth of circulation and (2) the geothermal gradient near the faults.","language":"ENGLISH","publisher":"U.S. Geological Survey?,","doi":"10.3133/ofr74271","usgsCitation":"Hose, R.K., and Taylor, B.E., 1974, Geothermal systems of northern Nevada: U.S. Geological Survey Open-File Report 74-271, 27 leaves :maps ;28 cm.; (31 p. - PGS), https://doi.org/10.3133/ofr74271.","productDescription":"27 leaves :maps ;28 cm.; (31 p. - PGS)","costCenters":[],"links":[{"id":147320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0271/report-thumb.jpg"},{"id":42887,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0271/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a118","contributors":{"authors":[{"text":"Hose, Richard Kenneth","contributorId":23915,"corporation":false,"usgs":true,"family":"Hose","given":"Richard","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":169085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Bruce Edward","contributorId":88748,"corporation":false,"usgs":true,"family":"Taylor","given":"Bruce","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":169086,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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