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,{"id":23511,"text":"ofr7520 - 1974 - Simulated water-level changes resulting from proposed changes in ground-water pumping in the Houston area, Texas","interactions":[],"lastModifiedDate":"2016-08-10T16:17:28","indexId":"ofr7520","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":"75-20","title":"Simulated water-level changes resulting from proposed changes in ground-water pumping in the Houston area, Texas","docAbstract":"<p>The need for additional water supplies in the Houston area prompted construction of Lake Livingston on the Trinity River in Polk and San Jacinto Counties, about 60 miles (96 km) northeast of Houston, as a source of surface water for municipal supply, industrial use, and irrigation. &nbsp;Water from the Lake Livingston will become available to users in the Houston area early in 1976.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7520","issn":"0094-9140","usgsCitation":"Jorgensen, D.G., and Gabrysch, R., 1974, Simulated water-level changes resulting from proposed changes in ground-water pumping in the Houston area, Texas: U.S. Geological Survey Open-File Report 75-20, 3 Plates: 22.02 x 17.67 inches or smaller, https://doi.org/10.3133/ofr7520.","productDescription":"3 Plates: 22.02 x 17.67 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":155643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr7520.PNG"},{"id":52799,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0020/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52800,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0020/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52801,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0020/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649366","contributors":{"authors":[{"text":"Jorgensen, Donald G.","contributorId":19537,"corporation":false,"usgs":true,"family":"Jorgensen","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":190230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":190231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44065,"text":"ofr74180 - 1974 - Water resources of the Little Fork River watershed, northeastern Minnesota","interactions":[{"subject":{"id":44065,"text":"ofr74180 - 1974 - Water resources of the Little Fork River watershed, northeastern Minnesota","indexId":"ofr74180","publicationYear":"1974","noYear":false,"title":"Water resources of the Little Fork River watershed, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":68333,"text":"ha551 - 1976 - Water resources of the Little Fork River watershed, northeastern Minnesota","indexId":"ha551","publicationYear":"1976","noYear":false,"title":"Water resources of the Little Fork River watershed, northeastern Minnesota"},"id":1}],"supersededBy":{"id":68333,"text":"ha551 - 1976 - Water resources of the Little Fork River watershed, northeastern Minnesota","indexId":"ha551","publicationYear":"1976","noYear":false,"title":"Water resources of the Little Fork River watershed, northeastern Minnesota"},"lastModifiedDate":"2012-02-02T00:10:31","indexId":"ofr74180","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":"74-180","title":"Water resources of the Little Fork River watershed, northeastern Minnesota","language":"ENGLISH","doi":"10.3133/ofr74180","issn":"ma","usgsCitation":"Helgesen, J.O., Lindholm, G.F., and Ericson, D., 1974, Water resources of the Little Fork River watershed, northeastern Minnesota: U.S. Geological Survey Open-File Report 74-180, 1 map on 2 sheets., https://doi.org/10.3133/ofr74180.","productDescription":"1 map on 2 sheets.","costCenters":[],"links":[{"id":173574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602cf7","contributors":{"authors":[{"text":"Helgesen, J. O.","contributorId":62600,"corporation":false,"usgs":true,"family":"Helgesen","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":229095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindholm, G. F.","contributorId":88763,"corporation":false,"usgs":true,"family":"Lindholm","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229097,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ericson, D.W.","contributorId":80295,"corporation":false,"usgs":true,"family":"Ericson","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":229096,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26622,"text":"wri748 - 1974 - Low-flow characteristics of streams in the Willapa Bay drainages, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"wri748","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":"74-8","title":"Low-flow characteristics of streams in the Willapa Bay drainages, Washington","language":"ENGLISH","publisher":"U. S. Geological Survey, Water Resources Division,","doi":"10.3133/wri748","usgsCitation":"Collings, M.R., and Hidaka, F.T., 1974, Low-flow characteristics of streams in the Willapa Bay drainages, Washington: U.S. Geological Survey Water-Resources Investigations Report 74-8, iii, 16 p. :ill., folded map ;27 cm., https://doi.org/10.3133/wri748.","productDescription":"iii, 16 p. :ill., folded map ;27 cm.","costCenters":[],"links":[{"id":157207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648701","contributors":{"authors":[{"text":"Collings, Michael R.","contributorId":48570,"corporation":false,"usgs":true,"family":"Collings","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hidaka, Frank T.","contributorId":107316,"corporation":false,"usgs":true,"family":"Hidaka","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":196728,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44059,"text":"ofr741131 - 1974 - Water-quality and geohydrologic data at two sanitary landfill sites near Anchorage, Alaska","interactions":[{"subject":{"id":44059,"text":"ofr741131 - 1974 - Water-quality and geohydrologic data at two sanitary landfill sites near Anchorage, Alaska","indexId":"ofr741131","publicationYear":"1974","noYear":false,"title":"Water-quality and geohydrologic data at two sanitary landfill sites near Anchorage, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70046278,"text":"70046278 - 1975 - Ground-water quality beneath solid-waste disposal sites at anchorage, Alaska","indexId":"70046278","publicationYear":"1975","noYear":false,"title":"Ground-water quality beneath solid-waste disposal sites at anchorage, Alaska"},"id":1}],"supersededBy":{"id":70046278,"text":"70046278 - 1975 - Ground-water quality beneath solid-waste disposal sites at anchorage, Alaska","indexId":"70046278","publicationYear":"1975","noYear":false,"title":"Ground-water quality beneath solid-waste disposal sites at anchorage, Alaska"},"lastModifiedDate":"2023-03-21T16:53:23.110176","indexId":"ofr741131","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":"74-1131","title":"Water-quality and geohydrologic data at two sanitary landfill sites near Anchorage, Alaska","docAbstract":"<p>Water-quality and geohydrologic data were collected at two sanitary landfill (solid-waste disposal) sites near Anchorage, Alaska. The study was undertaken by the U.S. Geological Survey in cooperation with the Greater Anchorage Area Borough and the U.S. Air Force. The purpose of the study was to evaluate the environmental effects of solid-waste disposal on the ground-water system and establish criteria for selecting future landfill sites. This report is a compilation of the data collected through August 1973.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741131","issn":"ma","collaboration":"Prepared in cooperation with the Greater Anchorage Area Borough and the U.S. Air Force","usgsCitation":"Zenone, C., and Donaldson, D., 1974, Water-quality and geohydrologic data at two sanitary landfill sites near Anchorage, Alaska: U.S. Geological Survey Open-File Report 74-1131, 1 Plate: 28.66 x 22.90 inches, https://doi.org/10.3133/ofr741131.","productDescription":"1 Plate: 28.66 x 22.90 inches","costCenters":[],"links":[{"id":173471,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1131/report-thumb.jpg"},{"id":414446,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1131/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -150.01694914400582,\n              61.279268443968306\n            ],\n            [\n              -150.01694914400582,\n              61.089052430070325\n            ],\n            [\n              -149.66615469214776,\n              61.089052430070325\n            ],\n            [\n              -149.66615469214776,\n              61.279268443968306\n            ],\n            [\n              -150.01694914400582,\n              61.279268443968306\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7290","contributors":{"authors":[{"text":"Zenone, Chester","contributorId":8094,"corporation":false,"usgs":true,"family":"Zenone","given":"Chester","email":"","affiliations":[],"preferred":false,"id":229076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donaldson, D.E.","contributorId":51829,"corporation":false,"usgs":true,"family":"Donaldson","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":229077,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67920,"text":"ha504 - 1974 - Water resources of the coastal drainage basins of Southeastern Massachusetts: Weir River, Hingham to Jones River, Kingston","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha504","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":"504","title":"Water resources of the coastal drainage basins of Southeastern Massachusetts: Weir River, Hingham to Jones River, Kingston","language":"ENGLISH","doi":"10.3133/ha504","usgsCitation":"Williams, J.R., and Tasker, G.D., 1974, Water resources of the coastal drainage basins of Southeastern Massachusetts: Weir River, Hingham to Jones River, Kingston: U.S. Geological Survey Hydrologic Atlas 504, 2 col. maps ;87-113 x 107-146 cm., https://doi.org/10.3133/ha504.","productDescription":"2 col. maps ;87-113 x 107-146 cm.","costCenters":[],"links":[{"id":189451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89114,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/504/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89115,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/504/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -70.95083333333334,41.950833333333335 ], [ -70.95083333333334,42.266666666666666 ], [ -70.58416666666666,42.266666666666666 ], [ -70.58416666666666,41.950833333333335 ], [ -70.95083333333334,41.950833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0240","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":277324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":95035,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":277323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69507,"text":"hu16 - 1974 - Hydrologic Unit Map -- 1974, Kansas","interactions":[],"lastModifiedDate":"2014-07-16T12:49:12","indexId":"hu16","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"16","subseriesTitle":"Kansas 1974","title":"Hydrologic Unit Map -- 1974, Kansas","language":"ENGLISH","doi":"10.3133/hu16","isbn":"060776774X","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Hydrologic Unit Map -- 1974, Kansas: U.S. Geological Survey Hydrologic Unit 16, col. map 72 x 149 cm. fold. in envelope 30 x 24 cm.; An overprint of the 1:500,000-scale state base map. Shows counties, location, and names of all cities and towns and most of the smaller settlements, railroads, and township and range lines in black; water features in blue; hydrologic boundaries and codes in red; county codes in green. No contours. Sheet 31 by 60 inches., https://doi.org/10.3133/hu16.","productDescription":"col. map 72 x 149 cm. fold. in envelope 30 x 24 cm.; An overprint of the 1:500,000-scale state base map. Shows counties, location, and names of all cities and towns and most of the smaller settlements, railroads, and township and range lines in black; water features in blue; hydrologic boundaries and codes in red; county codes in green. No contours. Sheet 31 by 60 inches.","costCenters":[],"links":[{"id":191405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/hu/16/report-thumb.jpg"},{"id":290286,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/hu/16/plate-1.pdf"}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6143ff","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":534602,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38692,"text":"pp813A - 1974 - Summary appraisals of the nation's ground-water resources – Ohio region","interactions":[],"lastModifiedDate":"2021-12-14T22:00:26.316554","indexId":"pp813A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"813","chapter":"A","title":"Summary appraisals of the nation's ground-water resources – Ohio region","docAbstract":"<p>Ground water in the Ohio Region is a large, important, and manageable resource that should have a significant role in regional water development.</p>\n<p>On the basis of a comparison of ground-water withdrawals with estimated ground-water recharge, it appears that the ground-water resources of the Ohio Region probably will not be used at full potential under existing development plans. Annual ground-water use (1960) by municipalities and rural residents was about 1,000 million gallons per day. Average annual regional ground-water recharge is about 35,000 million gallons per day. Therefore, base-year (1960) municipal and rural ground-water use is only about 3 percent of recharge. Annual regionwide ground-water use (1965) by industry also is only about 3 percent of recharge.</p>\n<p>Not all ground water in storage is recoverable for development, but estimates of the amounts that can be obtained from storage, under specified conditions, are calculated to show the magnitude of water that is available. Total potable ground water available from storage in the outwash and alluvial aquifers in the Ohio River valley and the subbasins is about 23,000 billion gallons. This about four times the floodcontrol storage of all Ohio Region Corps of Engineers reservoirs constructed, under construction, or in advance planning as of July 1965. Approximately 85,000 billion gallons of potable ground water is available from storage in the region in aquifers other than the outwash and alluvial aquifers. This is about 20 percent of estimated storage in Lake Ontario.</p>\n<p>About 5 percent of the region has ground-water resources capable of supplying more than local needs. For example, under certain specified conditions the excess of ground-water recharge over base-year (1960) ground-water use is available for 22 million additional people in the Wabash subbasin; for 4, 1.5, and 12 million additional people, respectively, in the Miami, lower Scioto, and Allegheny subbasins; for 5 million additional people in the Ohio River valley; or for equivalent quantities of water supply for industrial or a~ricultural expansion or other use. A reasonable assumption is that much of the available ground water in these areas can be pumped and transported to reasonably distant points of need.</p>\n<p>The Wabash and White subbasins probably have the highest potential of all Ohio River subbasins for additional ground-water development. About 30,000 billion gallons, or about 28 percent of the total potable ground water available from storage in the Ohio Region, is in storage in these subbasins. Estimated average annual ground-water recharge in the Wabash and White subbasins is 7,300 million gallons per day. Annual ground-water use (1960) by municipalities and rural residents of the subbasins of about 220 million gallons per day is only about 3 percent of estimated annual ground-water recharge and only about 0.3 percent of the potable ground water in storage in the subbasins. Also, many high-yield aquifers are present and offer excellent reservoir-manipulation possibilities in conjunction with existing and planned surface reservoirs.</p>\n<p>Practically all areas of high population density in the Ohio Region have the potential for development of ground-water resources. The Indianapolis, Ind., area probably has the highest potential.</p>\n<p>Assuming that future population growth will be heaviest in the areas paralleling the interstate highway system, much of the increased water demand associated with these growth areas can be supplied by ground water. The areas of population growth in Indiana and southwestern and south-central Ohio are especially well situated in terms of potential ground-water supplies.</p>\n<p>Underground space in the Ohio Region, consisting of natural pore spaces and fractures in rocks and sediments, can be considered a regional resource in the sense that it can be included in regional water-pollution control or waste-disposal plans. Much of this space is already occupied by ground water or other fluids which must be displaced for any alternate use. There is a potential for underground waste storage in practically the entire Ohio Region.</p>\n<p>Rapid advance of techniques in ground-water hydrology during recent years has provided methods which the hydrologist can use for evaluating planned ground-water development. Therefore, the manager can resolve the inherent problems that historically have bred caution when this part of our total water resource was considered for development.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813A","usgsCitation":"Bloyd, R.M., 1974, Summary appraisals of the nation's ground-water resources – Ohio region: U.S. Geological Survey Professional Paper 813, iv, 41 p., https://doi.org/10.3133/pp813A.","productDescription":"iv, 41 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":392900,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5056.htm"},{"id":65541,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813a/report.pdf","text":"Report","size":"11.87 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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":31067,"text":"cir691B - 1974 - Expectable Earthquakes and their ground motions in the Van Norman Reservoirs Area","interactions":[],"lastModifiedDate":"2012-02-02T00:09:08","indexId":"cir691B","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":"691","chapter":"B","title":"Expectable Earthquakes and their ground motions in the Van Norman Reservoirs Area","docAbstract":"The upper and lower Van Norman dams, in northwesternmost San Fernando Valley about 20 mi (32 km) northwest of downtown Los Angeles, were severely damaged during the 1971 San Fernando earthquake. An investigation of the geologic-seismologic setting of the Van Norman area indicates that an earthquake of at least M 7.7 may be expected in the Van Norman area. The expectable transitory effects in the Van Norman area of such an earthquake are as follows: peak horizontal acceleration of at least 1.15 g, peak velocity of displacement of 4.43 ft/sec (135 cm/sec), peak displacement of 2.3 ft (70 cm), and duration of shaking at accelerations greater than 0.05 g, 40 sec. A great earthquake (M 8+) on the San Andreas fault, 25 mi distant, also is expectable. Transitory effects in the Van Norman area from such an earthquake are estimated as follows: peak horizontal acceleration of 0.5 g, peak velocity of 1.97 ft/sec (60 cm/sec), displacement of 1.31 ft (40 cm), and duration of shaking at accelerations greater than 0.05 g, 80 sec. \r\n\r\nThe permanent effects of the expectable local earthquake could include simultaneous fault movement at the lower damsite, the upper damsite, and the site proposed for a replacement dam halfway between the upper and lower dams. The maximum differential displacements due to such movements are estimated at 16.4 ft (5 m) at the lower damsite and about 9.6 ft (2.93 m) at the upper and proposed damsites. \r\n\r\nThe 1971 San Fernando earthquake (M 6?) was accompanied by the most intense ground motions ever recorded instrumentally for a natural earthquake. At the lower Van Norman dam, horizontal accelerations exceeded 0.6 g, and shaking greater than 0.25 g lasted for about 13 see; at Pacoima dam, 6 mi (10 km) northeast of the lower dam, high-frequency peak horizontal accelerations of 1.25 g were recorded in two directions, and shaking greater than 0.25 g lasted for about 7 sec. \r\n\r\nPermanent effects of the earthquake include slope failures in the embankments of the upper and lower Van Norman dams, rupturing of the ground surface by faulting along parts of the zone of old faults that extends easterly through the reservoir area and across the northern part of the valley, folding or arching of the ground surface, and differential horizontal displacement of the terrane north and south of the fault zone. \r\n\r\nAlthough a zone of old faults extends through the reservoir area, the 1971 surface ruptures apparently did not; however, arching and horizontal displacements caused small relative displacements of the abutment areas of each of the three damsites. The 1971 arching coincided with preexisting topographic highs, and the surface ruptures coincided with eroded fault scarps and a buried ground-water impediment formed by pre-1971 faulting in young valley fill. This coincidence with evidence of past deformation indicates that the 1971 deformations were the result of a continuing geologic process that is expected to produce similar deformations during future events. \r\n\r\nThe 1971 San Fernando earthquake probably was not the largest that has occurred in this area during the last approximately 200 years, as indicated by a buried fault like scarp about 200 years old that is higher than, and aligned with, 1971 fault scarps. In addition, the San Fernando zone of 1971 ruptures is part of a regional tectonic system that includes the San Andreas and associated faults; one of these, the White Wolf fault north of the San Andreas, is symmetrical in structural attitude with the San Fernando zone and ruptured the ground surface during the 1952 Kern County earthquake (M 7.7). Other large earthquakes associated with surface rupturing on faults of this system include the 1857 Fort Tejon earthquake (M 8+) and possibly the 1852 Big Pine earthquake. Several other historic earthquakes in this general area are not known to be associated with surface ruptures, but were large enough to cause damage in the northern San Fernando Valley. \r\n\r\nThe Van Norman rese","language":"ENGLISH","doi":"10.3133/cir691B","usgsCitation":"Wesson, R.L., Page, R., Boore, D., and Yerkes, R.F., 1974, Expectable Earthquakes and their ground motions in the Van Norman Reservoirs Area: U.S. Geological Survey Circular 691, B9 p., https://doi.org/10.3133/cir691B.","productDescription":"B9 p.","costCenters":[],"links":[{"id":254943,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1974/0691b/report.pdf","size":"751","linkFileType":{"id":1,"text":"pdf"}},{"id":254944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1974/0691b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f93b4","contributors":{"authors":[{"text":"Wesson, R. L.","contributorId":51752,"corporation":false,"usgs":true,"family":"Wesson","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":204823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, R.A.","contributorId":40197,"corporation":false,"usgs":true,"family":"Page","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":204822,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":204824,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":204821,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68173,"text":"ha517 - 1974 - Ground water in Gray County, southwestern Kansas","interactions":[],"lastModifiedDate":"2017-02-13T16:27:34","indexId":"ha517","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":"517","title":"Ground water in Gray County, southwestern Kansas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha517","usgsCitation":"McGovern, H.E., and Long, W., 1974, Ground water in Gray County, southwestern Kansas: U.S. Geological Survey Hydrologic Atlas 517, 2 Sheets: 31.5 x 29.0 in., https://doi.org/10.3133/ha517.","productDescription":"2 Sheets: 31.5 x 29.0 in.","costCenters":[],"links":[{"id":186051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89481,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/517/plate-1.pdf","text":"Sheet 1 of 2","linkFileType":{"id":1,"text":"pdf"}},{"id":89482,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/517/plate-2.pdf","text":"Sheet 2 of 2","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Kansas","county":"Gray County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-100.2272,37.915],[-100.2275,37.8284],[-100.2164,37.8281],[-100.217,37.4758],[-100.652,37.4757],[-100.6526,37.7364],[-100.6507,37.8285],[-100.6641,37.8296],[-100.6638,38.0005],[-100.2269,38.0007],[-100.2272,37.915]]]},\"properties\":{\"name\":\"Gray\",\"state\":\"KS\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db60","contributors":{"authors":[{"text":"McGovern, Harold E.","contributorId":9634,"corporation":false,"usgs":true,"family":"McGovern","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, W.A.","contributorId":46619,"corporation":false,"usgs":true,"family":"Long","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":277775,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14686,"text":"ofr7439 - 1974 - Hydrology of the Dismal Swamp, Virginia-North Carolina","interactions":[],"lastModifiedDate":"2023-11-23T00:04:19.391593","indexId":"ofr7439","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":"74-39","title":"Hydrology of the Dismal Swamp, Virginia-North Carolina","docAbstract":"<p>The Dismal Swamp, on the border between eastern Virginia and North Carolina is one of the few remaining large (approximately 210,000 acres) areas of wet wilderness in the eastern United States. There has been much speculation concerning the hydrologic conditions that led to the formation of the swamp.</p><p>Oaks and Coch (1973) recently completed a detailed investigation of the geology and morphology of the area. An analysis of their geology and the pollen work of Whitehead (1972) has lead the authors to the following hypothesis concerning the hydrologic conditions that led to the formation of the peat in the swamp.</p><p>A permeable sand facies of the Norfolk Formation underlies Dismal Swamp. This facies was originally completely covered by the Sand Bridge Formation, which is a confining layer, and underlain by the impermeable Yorktown Formation. Movement of water eastward within the Norfolk Formation from the outcrop area on the top of the Suffolk Scarp was further restricted by a less permeable facies of the Norfolk east of the swamp; thereby creating an artesian head within the permeable sand facies of the Norfolk Formation.</p><p>Erosion during the Pleistocene age breached the Sand Bridge confining layer and allowed upward seepage of water along the shallow stream valleys. This seepage, combined with the abundant rainfall and naturally sluggish surface drainage, may have been sufficient to trigger the formation of peat along stream valleys about 9,000 years ago. The peat further inhibited surface drainage, which in turn, accelerated the accumulation of peat until the interfluve areas were covered. The present role of the Norfolk Formation in the hydrology of the swamp is not clear, but it is considered to be one of the most important aspects of the hydrology to be studied in future investigations.</p><p>Surface inflow is from small streams draining from the west. The flow of these streams varies widely, being generally less in the summer than in winter. Outflow is primarily through the Feeder Ditch-Dismal Swamp Canal system, which discharges at South Mills and Deep Creek locks.</p><p>Rates and direction of surface flow within the swamp are partly controlled by gates on many of the ditches. Inadequately controlled ditches penetrating the Norfolk Formation plus withdrawal of water from wells along Suffolk Scarp have altered the flow of ground water under the swamp. These modifications and the loss of water through the Dismal Swamp Canal have probably resulted in a generally drier swamp as indicated by changes in the vegetation. It is feasible to preserve Dismal Swamp, but more detailed studies of the hydrology are needed to aid in future management.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7439","usgsCitation":"Lichtler, W.F., and Walker, P.N., 1974, Hydrology of the Dismal Swamp, Virginia-North Carolina: U.S. Geological Survey Open-File Report 74-39, v, 50 p., https://doi.org/10.3133/ofr7439.","productDescription":"v, 50 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":148364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0039/report-thumb.jpg"},{"id":422873,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"Dismal Swamp","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    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36.644181586865905\n            ],\n            [\n              -76.56457901000977,\n              36.651618852404475\n            ],\n            [\n              -76.56097412109375,\n              36.65464864356238\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ea6","contributors":{"authors":[{"text":"Lichtler, William Francis","contributorId":58284,"corporation":false,"usgs":true,"family":"Lichtler","given":"William","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":169846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, Patrick Neil","contributorId":47800,"corporation":false,"usgs":true,"family":"Walker","given":"Patrick","email":"","middleInitial":"Neil","affiliations":[],"preferred":false,"id":169845,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66499,"text":"i766M - 1974 - Map showing the thickness of loosely packed sediments and the depth to bedrock in the Sugar House quadrangle, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2022-12-12T21:02:14.211744","indexId":"i766M","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":"766","chapter":"M","title":"Map showing the thickness of loosely packed sediments and the depth to bedrock in the Sugar House quadrangle, Salt Lake County, Utah","docAbstract":"<p>This map provides information on the location and distribution of three general types of geologic materials in part of Salt Lake County, including the southeastern part of Salt Lake City, Utah. These materials have different physical properties that are pertinent to comprehensive planning and zoning, land-use studies, and engineering usage. The map should be of use in preliminary studies to determine the depth to different &nbsp;general types of foundation material and to determine the potential for settlement of the ground surface during major earthquakes, which could result in damage to waterlines, gaslines, large buildings, and other major engineering structures.</p><p>The lines on the map are generalized. Lines showing the thickness of loosely packed sediments are based on drillers’ logs of 27 water wells in and near the 35-square-mile part of the quadrangle west of the mountains – less than one data point for each square mile. Lines showing the depth to bedrock are based on indirect geophysical data, and the data points are more widely scattered. The map may be useful as a general guide in planning, but investigations by qualified specialists should be made for detailed evaluations of specific areas.</p><p>references to other reports of possible interest to the reader are included at the end of this text.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i766M","usgsCitation":"McGregor, E.E., Van Horn, R., and Arnow, T., 1974, Map showing the thickness of loosely packed sediments and the depth to bedrock in the Sugar House quadrangle, Salt Lake County, Utah: U.S. Geological Survey IMAP 766, Cover : 1 p.; 1 Plate: 40.53 x 27.68 inches, https://doi.org/10.3133/i766M.","productDescription":"Cover : 1 p.; 1 Plate: 40.53 x 27.68 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":410314,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9532.htm","linkFileType":{"id":5,"text":"html"}},{"id":255945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0766m/report-thumb.jpg"},{"id":255943,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0766m/plate-1.pdf","text":"Map I-766-M","linkFileType":{"id":1,"text":"pdf"}},{"id":255944,"rank":1,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0766m/report.pdf","text":"Folio Cover","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Utah","county":"Salt Lake County","otherGeospatial":"Sugar House quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.875,40.625 ], [ -111.875,40.75 ], [ -111.75,40.75 ], [ -111.75,40.625 ], [ -111.875,40.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a25c5","contributors":{"authors":[{"text":"McGregor, Edward E.","contributorId":95886,"corporation":false,"usgs":true,"family":"McGregor","given":"Edward","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":274616,"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":274617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":274618,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66723,"text":"i844K - 1974 - Map showing ground-water velocities in the uppermost saturated alluvial deposits of the Tucson area, Arizona","interactions":[],"lastModifiedDate":"2025-08-08T19:30:02.646568","indexId":"i844K","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":"844","subseriesTitle":"NONE","chapter":"K","title":"Map showing ground-water velocities in the uppermost saturated alluvial deposits of the Tucson area, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i844K","usgsCitation":"Osterkamp, W.R., 1974, Map showing ground-water velocities in the uppermost saturated alluvial deposits of the Tucson area, Arizona: U.S. Geological Survey IMAP 844, 1 Plate: 34.93 x 26.42 inches, https://doi.org/10.3133/i844K.","productDescription":"1 Plate: 34.93 x 26.42 inches","costCenters":[],"links":[{"id":255460,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0844k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255461,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0844k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255462,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0844k/report-thumb.jpg"},{"id":493895,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9683.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Arizona","city":"Tucson","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.083,\n              32.75\n            ],\n            [\n              -112.083,\n              31.333\n            ],\n            [\n              -110.483,\n              31.333\n            ],\n            [\n              -110.483,\n              32.75\n            ],\n            [\n              -112.083,\n              32.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ccb","contributors":{"authors":[{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":274965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68064,"text":"ha487 - 1974 - Water in the Great Basin region; Idaho, Nevada, Utah, and Wyoming","interactions":[],"lastModifiedDate":"2022-12-01T20:26:08.272857","indexId":"ha487","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":"487","title":"Water in the Great Basin region; Idaho, Nevada, Utah, and Wyoming","docAbstract":"<p>The Great Basin Region is defined to include the drainage of the Great Basin physiographic section (Fennman, 1931) in Idaho, Nevada, Utah, and Wyoming. In October 1966, the President’s Water Resources Council requested that a comprehensive framework study be made in the Great Basin Region under the leadership of the Pacific Southwest Interagency Committee. The study, which included evaluation of the water resources of the region and guidelines for future study and development, was completed June 30, 1971. Results of the study received limited distribution.</p><p>The purpose of this atlas is to make available to the public the hydrologic data (including a general appraisal) that were compiled for the comprehensive framework study. Most of the work was done by a water-resources work group consisting of members from several Federal and State agencies under the chairmanship of Thomas E. Eakin of the U.S. Geological Survey. This atlas contains some data not included in the framework study.</p><p>The data presented herein are reconnaissance in nature and should be used with discretion. The maps are highly generalized and are intended only to illustrate the regional distribution of the supply and general chemical quality of the water. Sources of more detailed information on the hydrology of specific parts of the Great Basin region are listed in the selected references.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha487","collaboration":"Prepared in cooperation with the states of Idaho, Nevada, Utah, and Wyoming","usgsCitation":"Price, D., and Eakin, T., 1974, Water in the Great Basin region; Idaho, Nevada, Utah, and Wyoming: U.S. Geological Survey Hydrologic Atlas 487, 3 Plates: 47.0 x 40.0 inches or smaller, https://doi.org/10.3133/ha487.","productDescription":"3 Plates: 47.0 x 40.0 inches or smaller","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":91819,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/487/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Ground Water"},{"id":185540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89331,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/487/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Surface Water"},{"id":89330,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/487/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Physical Setting"},{"id":409947,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15876.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"2000000","country":"United States","state":"Idaho, Nevada, Utah, Wyoming","otherGeospatial":"Great Basin region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              35\n            ],\n            [\n              -110.5,\n              35\n            ],\n            [\n              -110.5,\n             43\n            ],\n            [\n              -120,\n              43\n            ],\n            [\n              -120,\n              35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9de8","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":277591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eakin, Thomas E.","contributorId":95449,"corporation":false,"usgs":true,"family":"Eakin","given":"Thomas E.","affiliations":[],"preferred":false,"id":277592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67309,"text":"i766N - 1974 - Map showing flood and surface water information in the Sugar House quadrangle, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2017-02-16T15:58:10","indexId":"i766N","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":"766","chapter":"N","title":"Map showing flood and surface water information in the Sugar House quadrangle, Salt Lake County, Utah","docAbstract":"<p>In the past man has built on land that might be covered by floodwaters, with little consideration of the consequences. The result has been disastrous to those in the path of floodwaters and has cost the loss of thousands of lives and untold billions of dollars in property damage in the United States. Salt Lake County, of which the Sugar House quadrangle is a part, has had many floods in the past and can be expected to have more in the future. Construction has taken place in filled or dried-up marshes and lakes, in spring areas, and even in stream channels. Lack of prior knowledge of these and other forms of surface water (water at the surface of the ground) can increase construction and maintenance costs significantly.</p><p>The map shows the area that probably will be covered by floods at least once in every 100 years on the long-term average (unit IRF, intermediate regional flood), the area that probably will be covered by floods from the worst possible combination of very wet weather and high streamflow reasonably expected of the area (unit SPF, standard project flood), the mapped extent of streamflow by channel shifting or flooding in the past 5,000 years (unit fa), and the probable maximum extent of damaging flash floods and mudflows from small valleys in the Wasatch Range. The map also shows the location of water at the surface of the ground: lakes, streams, springs, weep holes, canals, and reservoirs. Lakes and marshes that existed within the past 100 years, but now are drained, filled, or dried up, are also shown.</p><p>The following examples show that the presence of water can be desirable or undesirable, depending on how the water occurs. Floods, the most spectacular form of surface water, may result in great property damage and loss of life. Lakes normally are beneficial, in that they may support plant growth and provide habitats for fish and other wildlife, provide water for livestock, and can be used for recreation. Springs may or may not be desirable: they may provide a source of water for domestic or stock use but are undesirable if they appear in a foundation excavation for a building. Thus, the location of areas that may be affected by floods and other surface water is important to people concerned with land-use planning, zoning, and legislation, and with the environment in which we must live.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i766N","usgsCitation":"Van Horn, R., and Fields, F., 1974, Map showing flood and surface water information in the Sugar House quadrangle, Salt Lake County, Utah: U.S. Geological Survey IMAP 766, Map: 34.24 x 27.76 inches; Cover: 9.20 x 11.82 inches, https://doi.org/10.3133/i766N.","productDescription":"Map: 34.24 x 27.76 inches; Cover: 9.20 x 11.82 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":256347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0766n/report-thumb.jpg"},{"id":256345,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0766n/plate-1.pdf","text":"Map I-766-N","size":"6.49 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":256346,"rank":300,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0766n/report.pdf","text":"Folio Cover","size":"29 KB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Utah","county":"Salt Lake County","otherGeospatial":"Sugar House quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.86749999999999,40.6175 ], [ -111.86749999999999,40.75 ], [ -111.75,40.75 ], [ -111.75,40.6175 ], [ -111.86749999999999,40.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687df0","contributors":{"authors":[{"text":"Van Horn, Richard","contributorId":52169,"corporation":false,"usgs":true,"family":"Van Horn","given":"Richard","email":"","affiliations":[],"preferred":false,"id":275962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fields, F.K.","contributorId":90826,"corporation":false,"usgs":true,"family":"Fields","given":"F.K.","email":"","affiliations":[],"preferred":false,"id":275963,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66738,"text":"i844L - 1974 - Map showing chemical quality of ground water for public supply in the Tucson area, Arizona","interactions":[],"lastModifiedDate":"2025-08-08T19:33:17.493292","indexId":"i844L","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":"844","chapter":"L","title":"Map showing chemical quality of ground water for public supply in the Tucson area, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i844L","usgsCitation":"Osterkamp, W.R., and Laney, R., 1974, Map showing chemical quality of ground water for public supply in the Tucson area, Arizona: U.S. Geological Survey IMAP 844, 1 Plate: 34.68 x 26.81 inches, https://doi.org/10.3133/i844L.","productDescription":"1 Plate: 34.68 x 26.81 inches","costCenters":[],"links":[{"id":493896,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9684.htm","linkFileType":{"id":5,"text":"html"}},{"id":256056,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0844l/report-thumb.jpg"},{"id":256055,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0844l/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256054,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0844l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona","city":"Tucson","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.083,\n              32.75\n            ],\n            [\n              -112.083,\n              31.333\n            ],\n            [\n              -110.483,\n              31.333\n            ],\n            [\n              -110.483,\n              32.75\n            ],\n            [\n              -112.083,\n              32.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659b6b","contributors":{"authors":[{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":274995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laney, R. L.","contributorId":83889,"corporation":false,"usgs":true,"family":"Laney","given":"R. L.","affiliations":[],"preferred":false,"id":274996,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37214,"text":"rp115 - 1974 - Population ecology of the mallard: II. Breeding habitat conditions, size of the breeding populations, and production indices","interactions":[],"lastModifiedDate":"2016-11-09T13:42:16","indexId":"rp115","displayToPublicDate":"1991-08-16T07:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"115","title":"Population ecology of the mallard: II. Breeding habitat conditions, size of the breeding populations, and production indices","docAbstract":"<p><span>This report, the second in a series on a comprehensive analysis of mallard population data, provides information on mallard breeding habitat, the size and distribution of breeding populations, and indices to production. The information in this report is primarily the result of large-scale aerial surveys conducted during May and July, 1955-73. The history of the conflict in resource utilization between agriculturalists and wildlife conservation interests in the primary waterfowl breeding grounds is reviewed. The numbers of ponds present during the breeding season and the midsummer period and the effects of precipitation and temperature on the number of ponds present are analyzed in detail. No significant cycles in precipitation were detected and it appears that precipitation is primarily influenced by substantial seasonal and random components. Annual estimates (1955-73) of the number of mallards in surveyed and unsurveyed breeding areas provided estimates of the size and geographic distribution of breeding mallards in North America. The estimated size of the mallard breeding population in North America has ranged from a high of 14.4 million in 1958 to a low of 7.1 million in 1965. Generally, the mallard breeding population began to decline after the 1958 peak until 1962, and remained below 10 million birds until 1970. The decline and subsequent low level of the mallard population between 1959 and 1969 .generally coincided with a period of poor habitat conditions on the major breeding grounds. The density of mallards was highest in the </span><i>Prairie-Parkland Area</i><span> with an average of nearly 19.2 birds per square mile. The proportion of the continental mallard breeding population in the </span><i>Prairie-Parkland Area</i><span> ranged from 30% in 1962 to a high of 600/0 in 1956. The geographic distribution of breeding mallards throughout North America was significantly related to the number of May ponds in the </span><i>Prairie-Parkland Area</i><span>. Estimates of midsummer habitat conditions and indices to production from the July Production Survey were studied in detail. Several indices relating to production showed marked declines from west to east in the </span><i>Prairie-Parkland Area</i><span>, these are: (1) density of breeding mallards (per square mile and per May pond), (2) brood density (per square mile and per July pond), (3) average brood size (all species combined), and (4) brood survival from class II to class III. An index to late nesting and renesting efforts was highest during years when midsummer water conditions were good. Production rates of many ducks breeding in North America appear to be regulated by both density-dependent and density-independent factors. Spacing of birds in the </span><i>Prairie-Parkland Area</i><span> appeared to be a key factor in the density-dependent regulation of the population. The spacing mechanism, in conjunction with habitat conditions, influenced some birds to overfly the primary breeding grounds into less favorable habitats to the north and northwest where the production rate may be suppressed. The production rate of waterfowl in the </span><i>Prairie Parkland Area</i><span> seems to be independent of density (after emigration has taken place) because the production index appears to be a linear function of the number of breeding birds in the area. Similarly, the production rate of waterfowl in northern Saskatchewan and northern Manitoba appeared to be independent of density. Production indices in these northern areas appear to be a linear function of the size of the breeding population. Thus, the density and distribution of breeding ducks is probably regulated through a spacing mechanism that is at least partially dependent on measurable environmental factors. The result is a density-dependent process operating to ultimately effect the production and production rate of breeding ducks on a continent-wide basis. Continental production, and therefore the size of the fall population, is probably partially regulated by the number of birds that are distributed north and northwest into environments less favorable for successful reproduction. Thus, spacing of the birds in the </span><i>Prairie-Parkland Area</i><span> and the movement of a fraction of the birds out of the prime breeding areas may be key factors in the density-dependent regulation of the total mallard population.</span></p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Pospahala, R.S., Anderson, D.R., and Henny, C.J., 1974, Population ecology of the mallard: II. Breeding habitat conditions, size of the breeding populations, and production indices: Resource Publication 115, iv, 73 p.","productDescription":"iv, 73 p.","numberOfPages":"78","costCenters":[],"links":[{"id":193124,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683ef2","contributors":{"authors":[{"text":"Pospahala, Richard S.","contributorId":11677,"corporation":false,"usgs":true,"family":"Pospahala","given":"Richard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":511196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, David R.","contributorId":92722,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":511197,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henny, Charles J. 0000-0001-7474-350X hennyc@usgs.gov","orcid":"https://orcid.org/0000-0001-7474-350X","contributorId":3461,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"hennyc@usgs.gov","middleInitial":"J.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":511195,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112317,"text":"70112317 - 1974 - Optical data processing and projected applications of the ERTS-1 imagery covering the 1973 Mississippi River Valley floods","interactions":[],"lastModifiedDate":"2017-01-18T15:18:21","indexId":"70112317","displayToPublicDate":"1990-06-12T14:39:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Optical data processing and projected applications of the ERTS-1 imagery covering the 1973 Mississippi River Valley floods","docAbstract":"<p>Flooding along the Mississippi River and some of its tributaries was detected by the multispectral scanner (MSS) on the Earth Resources Technology Satellite (ERTS-1) on at least three orbits during the spring of 1973. The ERTS data provided the first opportunity for mapping the regional extent of flooding at the time of the imagery. Special optical data processing techniques were used to produce a variety of multispectral color composites enhancing flood-plain details. One of these, a 2-color composite of near infrared bands 6 and 7, was enlarged and registered to 1:250,000-scale topographic maps and used as the basis for preparation of flood image maps. Two specially filtered 3-color composites of MSS bands 5, 6, and 7 and 4, 5, and 7 were prepared to aid in the interpretation of the data. The extent of the flooding was vividly depicted on a single image by 2-color temporal composites produced on the additive-color viewer using band 7 flood data superimposed on pre-flood band 7 images. On May 24, when the floodwaters at St. Louis receded to bankfull stage, imagery was again obtained by ERTS. Analysis of temporal data composites of the pre-flood and post-flood band 7 images indicate that changes in surface reflectance characteristics caused by the flooding can be delineated, thus making it possible to map the overall area flooded without the necessity of a real-time system to track and image the peak flood waves. Regional planning and disaster relief agencies such as the Corps of Engineers, Office of Emergency Preparedness, Soil Conservation Service, interstate river basin commissions and state agencies, as well as private lending and insurance institutions, have indicated strong potential applications for ERTS image-maps of flood-prone areas.</p>","language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","doi":"10.1111/j.1752-1688.1974.tb00622.x","usgsCitation":"Deutsch, M., and Ruggles, F., 1974, Optical data processing and projected applications of the ERTS-1 imagery covering the 1973 Mississippi River Valley floods: Water Resources Bulletin, v. 10, no. 5, p. 1023-1039, https://doi.org/10.1111/j.1752-1688.1974.tb00622.x.","productDescription":"17 p.","startPage":"1023","endPage":"1039","numberOfPages":"17","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288529,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1974.tb00622.x"},{"id":288530,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Mississippi River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.25,29.15 ], [ -95.25,47.5 ], [ -89.09,47.5 ], [ -89.09,29.15 ], [ -95.25,29.15 ] ] ] } } ] }","volume":"10","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"539acc0ce4b0e83db6d08f9a","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":494663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggles, Fred","contributorId":26973,"corporation":false,"usgs":true,"family":"Ruggles","given":"Fred","email":"","affiliations":[],"preferred":false,"id":494662,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70112316,"text":"70112316 - 1974 - Survey of remote sensing applications","interactions":[],"lastModifiedDate":"2022-03-30T18:10:11.452276","indexId":"70112316","displayToPublicDate":"1990-06-12T14:35:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3726,"text":"Water Well Journal","active":true,"publicationSubtype":{"id":10}},"title":"Survey of remote sensing applications","docAbstract":"<p>Data from the first earth resources technology satellite (ERTS) as well as from NASA and other aircraft, contain much of the information indicative of the distribution of groundwater and the extent of its utilization. Thermal infrared imagery from aircraft is particularly valuable in studying groundwater discharge to the sea and other surface water bodies. Color infrared photography from aircraft and space is also used to locate areas of potential groundwater development. Anomalies in vegetation, soils, moisture, and their pattern of distribution may be indicative of underlying groundwater conditions. Remote sensing may be used directly or indirectly to identify stream reaches for test holes or production wells. Similarly, location of submarine springs increase effectiveness of groundwater exploration in the coastal zone.</p>","language":"English","publisher":"National Water Well Association","publisherLocation":"Columbus, OH","usgsCitation":"Deutsch, M., 1974, Survey of remote sensing applications: Water Well Journal, v. 28, no. 7, p. 35-38.","productDescription":"4 p.","startPage":"35","endPage":"38","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288528,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc18e4b0e83db6d0900b","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":494661,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039203,"text":"70039203 - 1974 - EROS: A space program for Earth resources","interactions":[],"lastModifiedDate":"2017-06-05T21:55:56","indexId":"70039203","displayToPublicDate":"1976-01-01T12:01:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"EROS: A space program for Earth resources","docAbstract":"The EROS Program, administered by the U. S. Geological Survey, works with representatives of departmental bureaus and offices to coordinate research and application of remote-sensing technology to the day to-day operations of the department. Most of the research and applications have been made possible by the experimental data acquisition systems of the National Aeronautics and Space Administration (NASA). In particular, the EROS Program uses data from the Earth Resources Technology Satellite (ERTS), from the Earth Resources Experiment Package (EREP) of Skylab, and from NASA's Aircraft Program.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039203","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, EROS: A space program for Earth resources: General Information Product, 3 p. (7 columns), https://doi.org/10.3133/70039203.","productDescription":"3 p. (7 columns)","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":261372,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039203/report.pdf"},{"id":261373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039203/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0466e4b0c8380cd50966","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":535241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232498,"text":"70232498 - 1974 - Preliminary findings of a leachate study on two landfills in Suffolk County, New York","interactions":[],"lastModifiedDate":"2022-07-05T16:39:06.331896","indexId":"70232498","displayToPublicDate":"1975-05-01T11:20:07","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary findings of a leachate study on two landfills in Suffolk County, New York","docAbstract":"<p>Plumes of leachate-enriched ground water extend 10,600 and 5,000 ft (3,200 and 1,500 m) downgradient from landfills in the towns of Babylon and Islip, respectively, and extend vertically beneath the landfills to the base of the upper glacial aquifer, whose thickness ranges from 71 to 77 ft (22-24 m) at the Babylon site and is 170 ft (52 m) at the Islip site. The Babylon and Islip landfills were started in 1947 and 1933, respectively. The quantities of ground water in the plumes are 2X10<sup>9</sup> gal (8X10<sup>6</sup> m<sup>3</sup>) at Babylon and 1X10<sup>9</sup> gal (4X10<sup>6</sup> m<sup>3</sup>) at Islip. Differences in quantity of water in the plumes and length of the plumes may result partly from a slower rate of refuse accumulation at Islip than at Babylon; however, the rate of travel for the front of the Islip plume is considerably less than the prevailing groundwater velocity would indicate. Distance traveled by the front of the Islip plume was roughly one-third the distance indicated by the calculated minimum ground-water velocity and may result from greater vertical travel distance in the upper glacial aquifer at Islip. Concentrations of HCO<sub>3</sub><sup>-</sup>, Cl<sup>-</sup>, and SO<sub>4</sub><sup>-</sup><sup>2</sup> in the leachate-enriched ground water are higher than those in ambient ground water. Concentrations of Fe and Mn in the plumes are as much as 400,000 <i><span>μ</span></i>g/1 and 200,000 <i><span>μ</span></i>g/1, but concentrations of other metals, including Zn (220 <i><span>μ</span></i>g/1), do not exceed the U.S. Public Health Service drinking-water standards. The concentration of NH<sub>4</sub><sup>+</sup>, the predominant nitrogen species in plume water, is usually more than 10 percent of the total cations in plume water and is greater than NH<sub>4</sub><sup>+</sup> concentrations in ambient ground water; concentrations of NO<sub>3</sub><sup>-</sup> in plume water are less than those in ambient ground water at Babylon and at some locations in Islip.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Kimmel, G.E., and Braids, O.C., 1974, Preliminary findings of a leachate study on two landfills in Suffolk County, New York: Journal of Research of the U.S. Geological Survey, v. 3, no. 3, p. 273-280.","productDescription":"8 p.","startPage":"273","endPage":"280","costCenters":[],"links":[{"id":402980,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402979,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue3/report.pdf","size":"19104 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Suffolk 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,{"id":70207476,"text":"70207476 - 1974 - Red Sea geochemistry","interactions":[],"lastModifiedDate":"2019-12-19T18:26:08","indexId":"70207476","displayToPublicDate":"1974-12-31T18:17:09","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Red Sea geochemistry","docAbstract":"<p>The Red Sea drillings reveal a number of new facets of the hot-brine-metalliferous system and other geochemical aspects of the sea, its sediments, and its past history as follows: </p><p>1) Dark shales rich in organic material, and containing enhanced Mo and V concentrations, are characteristic of Plio-Pleistocene strata in the Red Sea. Values as high as 1500 ppm V and 500 ppm Mo were obtained in sediments containing up to 8 percent organic carbon. </p><p>2) Metalliferous sediments in the hot brine deep (Site 226) are similar in composition in both solids and interstitial water to previously analyzed sediments. However, one site (228) well south of the known hot-brine deeps shows zinc mineralization reaching 5 percent Zn in late Miocene shale-anhydrite breccias. </p><p>3) Pore fluid studies show that near-saturated (NaCl) brines having similar total salt concentration to the hot-brine fluids are associated with Miocene evaporites at Sites 225, 227, and 228. However, their chemical and isotopic composition precludes such fluids being part of the \"hot brine plumbing system.\" Hydrogen and oxygen isotope studies demonstrate that fluids trapped between and among the evaporitic rocks have a strong meteoric water component, presumed to have entered the rocks during or shortly after formation in shallow evaporating pans. The composition of pore fluid at Site 227 suggests the presence of late-stage evaporite minerals of the tachyhydrite CaMg<sub>2</sub>Cl<sub>6</sub> • 12H<sub>2</sub>O series in the in situ rocks. </p><p>4) Diffusivity measurements show that the pre-Miocene strata permit dissolved salt or gas diffusion to the extent of from 1/2 to about 1/10 the rate in free solution. However, in anhydrites diffusivity is reduced more than 100-fold, and no diffusion could be detected through halite rock. The rates applied to interstitial salt gradients at Site 225 suggest that less than 1 meter of rock salt is removed per million years by diffusion processes. The diffusion of salt can already be detected a few meters below the sediment-water interface, and based on the interstitial water studies, one can affirm the presence of salt at depth at Sites 228, 230, and possibly 229, where rock salt was not encountered by the drill. </p><p>5) Isotopic measurements on leads show that both leads from Site 228 and the hot brine deep (Site 226) require input from igneous or volcanic sources (e.g., volcanic ash). Elsewhere, however, leads of sedimentary-pelagic origin are noted. </p><p>6) Isotopic and other evidence indicates that the long-distance transport of subterranean brines advocated by Craig (1969) is unlikely. Instead, it is proposed that the source of the hot brines is subevaporite clastic or other aquifers of early to middle Miocene age that have been disrupted by rifting. These discharge in the deeps by virtue of hydrodynamic continuity with heavy brines at higher positions on the nearby flanks of the Red Sea. In this case, the waters might be fossil (middle Miocene) Red Sea waters of relatively normal salinity that have acquired greater salt concentration by diffusion from overlying late Miocene evaporites. The model is consistent with the isolated nature of the brine deeps and suggests that flow might have been enhanced by increased hydraulic gradients during periods of lowered Red Sea levels. </p><p>7) Interstitial water evidence indicates that Pleistocene lowerings of sea level did not cause evaporative conditions leading to actual gypsum or other evaporite deposition in the deeper water zones, as has been postulated. This in turn suggests that sill depths were greater than have been assumed.</p>","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.23.138.1974","usgsCitation":"Manheim, F.T., 1974, Red Sea geochemistry: Initial reports of the Deep Sea Drilling Project, v. 23, p. 975-998, https://doi.org/10.2973/dsdp.proc.23.138.1974.","productDescription":"24 p.","startPage":"975","endPage":"998","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488224,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2973/dsdp.proc.23.138.1974","text":"Publisher Index Page"},{"id":370535,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Red Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      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,{"id":70207475,"text":"70207475 - 1974 - Interstitial water studies on small core samples, leg 23 (Red Sea)","interactions":[],"lastModifiedDate":"2019-12-20T07:07:40","indexId":"70207475","displayToPublicDate":"1974-12-31T18:11:48","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, leg 23 (Red Sea)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.23.135.1974","usgsCitation":"Manheim, F.T., Waterman, L., Woo, C.C., and Sayles, F., 1974, Interstitial water studies on small core samples, leg 23 (Red Sea): Initial reports of the Deep Sea Drilling Project, v. 23, p. 955-967, 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