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,{"id":30546,"text":"wri7687 - 1976 - Index to water resources data for Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:09:08","indexId":"wri7687","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-87","title":"Index to water resources data for Illinois","docAbstract":"This index to water resources data for Illinois includes 1,275 sites where surface-water and ground-water data were collected through December 31, 1975. The index is the first comprehensive tabulation of data collected in Illinois by the U.S. Geological Survey; data collection began in 1903. Information included are the county code, drainage area, datum, type of data available, period of record, where data are filed, and the name of the current cooperating agency. The surface-water index is listed sequentially by station number and also alphabetically by station name. Station numbers for the ground-water index are grouped by counties. The hydrologic unit index shows all sites and is listed by the respective hydrologic boundaries. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri7687","usgsCitation":"Winget, D., 1976, Index to water resources data for Illinois: U.S. Geological Survey Water-Resources Investigations Report 76-87, iii, 81 p. :tables ;28 cm., https://doi.org/10.3133/wri7687.","productDescription":"iii, 81 p. :tables ;28 cm.","costCenters":[],"links":[{"id":160723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1c51","contributors":{"authors":[{"text":"Winget, D.E.","contributorId":46138,"corporation":false,"usgs":true,"family":"Winget","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":203435,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68052,"text":"ha571 - 1976 - Teton Dam flood of June 1976, Deer Parks quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T13:46:00","indexId":"ha571","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"571","title":"Teton Dam flood of June 1976, Deer Parks quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Deer Parks quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha571","usgsCitation":"Ray, H.A., Bennett, C.M., and Records, A.W., 1976, Teton Dam flood of June 1976, Deer Parks quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 571, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha571.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186030,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89315,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/571/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Deer Parks Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.125,43.75 ], [ -112.125,43.875 ], [ -112.0,43.875 ], [ -112.0,43.75 ], [ -112.125,43.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684ab4","contributors":{"authors":[{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, C. Michael","contributorId":26761,"corporation":false,"usgs":true,"family":"Bennett","given":"C.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":277571,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Records, Andrew W.","contributorId":7366,"corporation":false,"usgs":true,"family":"Records","given":"Andrew","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277570,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68191,"text":"ha576 - 1976 - Teton Dam flood of June 1976, Woodville quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T14:16:24","indexId":"ha576","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"576","title":"Teton Dam flood of June 1976, Woodville quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Woodville quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha576","usgsCitation":"Matthai, H.F., and Ray, H.A., 1976, Teton Dam flood of June 1976, Woodville quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 576, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha576.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":185566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89519,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/576/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Woodville Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,43.375 ], [ -112.25,43.5 ], [ -112.125,43.5 ], [ -112.125,43.375 ], [ -112.25,43.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d7c","contributors":{"authors":[{"text":"Matthai, Howard F.","contributorId":106491,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":277812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277811,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21114,"text":"ofr76339 - 1976 - Neutron activation analysis in hydrology","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr76339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-339","title":"Neutron activation analysis in hydrology","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76339","usgsCitation":"Thatcher, L.L., 1976, Neutron activation analysis in hydrology: U.S. Geological Survey Open-File Report 76-339, iv, 19 leaves :ill. ;28 cm.; (56 p. - PGS), https://doi.org/10.3133/ofr76339.","productDescription":"iv, 19 leaves :ill. ;28 cm.; (56 p. - PGS)","costCenters":[],"links":[{"id":154113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697b5c","contributors":{"authors":[{"text":"Thatcher, Leland Lincoln","contributorId":73985,"corporation":false,"usgs":true,"family":"Thatcher","given":"Leland","email":"","middleInitial":"Lincoln","affiliations":[],"preferred":false,"id":183868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20929,"text":"ofr76214 - 1976 - Distribution functions for statistics derived from bivariate normal and bivariate two-parameter log-normal populations","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr76214","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-214","title":"Distribution functions for statistics derived from bivariate normal and bivariate two-parameter log-normal populations","docAbstract":"The distribution functions for hydrologic statistics that may be used to assess the significance of differences between sample means, standard deviations, coefficients of skewness, and coefficients of variations are obtained by Monte Carlo experiments. The distributions are expressed as functions of sample size, cross correlation, and skewness. In general, the distributions are more sensitive to cross correlation than to skewness. As sample size increases, however, the distributions tend to become more sensitive to skewness. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76214","usgsCitation":"Slack, J.R., Matalas, N.C., and Wallis, J.R., 1976, Distribution functions for statistics derived from bivariate normal and bivariate two-parameter log-normal populations: U.S. Geological Survey Open-File Report 76-214, 22 leaves :ill. ;28 cm., https://doi.org/10.3133/ofr76214.","productDescription":"22 leaves :ill. ;28 cm.","costCenters":[],"links":[{"id":154082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649372","contributors":{"authors":[{"text":"Slack, James Richard","contributorId":83905,"corporation":false,"usgs":true,"family":"Slack","given":"James","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":183522,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matalas, Nicholas C.","contributorId":34535,"corporation":false,"usgs":true,"family":"Matalas","given":"Nicholas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":183521,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallis, James R.","contributorId":100419,"corporation":false,"usgs":true,"family":"Wallis","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":183523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17112,"text":"ofr76313 - 1976 - Field trip to Nevada test site","interactions":[],"lastModifiedDate":"2012-02-02T00:07:18","indexId":"ofr76313","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-313","title":"Field trip to Nevada test site","docAbstract":"Two road logs guide the reader through the geologic scene from Las Vegas to Mercury and from Mercury through eight stops on the Nevada Test Site. Maps and cross sections depict the geology and hydrology of the area. Included among the tables is one showing the stratigraphic units in the southwestern Nevada volcanic field and another that lists the geologic maps covering the Nevada Test Site and vicinity. The relation of the geologic environment to nuclear-explosion effects is alluded to in brief discussions of collapse, surface subsidence, and cratering resulting from underground nuclear explosions.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76313","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Field trip to Nevada test site: U.S. Geological Survey Open-File Report 76-313, iii, 64 p. (1 folded) :ill. ;28 cm., https://doi.org/10.3133/ofr76313.","productDescription":"iii, 64 p. (1 folded) :ill. ;28 cm.","costCenters":[],"links":[{"id":150185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0313/report-thumb.jpg"},{"id":46236,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0313/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8924","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":529007,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14782,"text":"ofr75642 - 1976 - Programmable calculators; modern instruments for analyzing hydrologic data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr75642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-642","title":"Programmable calculators; modern instruments for analyzing hydrologic data","language":"ENGLISH","publisher":"United States Department of the Interior, Geological Survey,","doi":"10.3133/ofr75642","usgsCitation":"Maddy, D.V., 1976, Programmable calculators; modern instruments for analyzing hydrologic data: U.S. Geological Survey Open-File Report 75-642, 24 p. :ill. ;27 cm.; (28 p. - PGS), https://doi.org/10.3133/ofr75642.","productDescription":"24 p. :ill. ;27 cm.; (28 p. - PGS)","costCenters":[],"links":[{"id":148131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688983","contributors":{"authors":[{"text":"Maddy, David V.","contributorId":87559,"corporation":false,"usgs":true,"family":"Maddy","given":"David","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":169996,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13733,"text":"ofr76338 - 1976 - Test drilling for ground water in Hudspeth, Culberson, and Presidio Counties in westernmost Texas","interactions":[],"lastModifiedDate":"2016-08-10T16:30:19","indexId":"ofr76338","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-338","title":"Test drilling for ground water in Hudspeth, Culberson, and Presidio Counties in westernmost Texas","docAbstract":"<p>From November 1973 to October 1974, the U.S. Geological Survey drilled four deep test holes to supplement hydrologic and geophysical studies evaluating fresh ground water in the basins of westernmost Texas. For each test, samples of drill cuttings were collect&middot;ed, borehole geophysical logs were run, and water samples were collected from specific zones.</p>\n<p>The Leopold Guerra No. 1 test hole penetrated sand and gravel :o 1,100 feet (335m), and logs and water samples indicated fresh ground water to that depth. Below 1,100 feet (335m), the material probably has low permeability. The Clay Evans No. 1 test penetrated sand, gravel, and clay to 555 feet (169m), sand and thin volcanic flows to about 1,250 feet (381 m), and volcanic flows and tuffs to 2,006 feet (611 m). Logs and water samples indicated fresh ground \\vater to about 1, 250 feet (381 m); below that, permeability is probably low. The Culberson County Airport test was drilled through sand, gravel, and clay to 1,145 feet (349m), conglomerate to 1,205 feet (367m), and the Lower Cretaceous Cox Sandstone to 1,306 feet (398m). Logs and water s~mples indicated fresh water in the alluvial fill and in the Cox Sandstone to about 1,265 feet (386m); below that depth, permeability is probably low. The Davis test was drilled through clay with some thin beds of sand and gravel containing fresh water to a depth of 2,012 feet (613 m).</p>\n<p>Borehole temperature data indicated above-nonnal gradients in the Guerra and Culberson County Airport tests. Temperature gradients in the Evans and Davis tests were near normal.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76338","usgsCitation":"Gates, J.S., and White, D.E., 1976, Test drilling for ground water in Hudspeth, Culberson, and Presidio Counties in westernmost Texas: U.S. Geological Survey Open-File Report 76-338, 76 p., https://doi.org/10.3133/ofr76338.","productDescription":"76 p.","numberOfPages":"77","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":112974,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0338/report.pdf","size":"2928","linkFileType":{"id":1,"text":"pdf"}},{"id":147541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0338/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684c34","contributors":{"authors":[{"text":"Gates, Joseph Spencer","contributorId":108089,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph","email":"","middleInitial":"Spencer","affiliations":[],"preferred":false,"id":168308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Donald Edward","contributorId":84731,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":168307,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56336,"text":"wdrCT751 - 1976 - Water resources data for Connecticut, water year 1975","interactions":[],"lastModifiedDate":"2022-11-30T19:11:02.830757","indexId":"wdrCT751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"CT-75-1","title":"Water resources data for Connecticut, water year 1975","docAbstract":"<p>Water resources data for the 1975 water year for Connecticut consist of records of stage, discharge, and water quality of streams; contents and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report contains discharge records for 56 gaging stations; tidal volume for 1 gaging station; stage only records for 3 tidal-gaging stations; contents for 36 lakes and reservoirs; water quality for 16 gaging stations, 39 partial-record flow stations, 3 lakes, 2 tidal stations, and 4 wells; and water levels for 27 observation wells. Also included are data for 65 crest-stage partial-record stations and 55 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. Locations of hydrologic stations are shown on figures 1 and 2. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Connecticut.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrCT751","collaboration":"Prepared in cooperation with the State of Connecticut and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Connecticut, water year 1975: U.S. Geological Survey Water Data Report CT-75-1, xv, 366 p., https://doi.org/10.3133/wdrCT751.","productDescription":"xv, 366 p.","costCenters":[],"links":[{"id":409882,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1975/ct-75-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1975/ct-75-1/report-thumb.jpg"}],"country":"United 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,{"id":39587,"text":"pp813G - 1976 - Summary appraisals of the nation's ground-water resources – Great Basin region","interactions":[],"lastModifiedDate":"2021-12-14T21:26:13.518321","indexId":"pp813G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"G","title":"Summary appraisals of the nation's ground-water resources – Great Basin region","docAbstract":"<p>Ground-water withdrawals by wells in the Great Basin Region were about 1.1 million acre-feet (1,360 cubic hectometres) in 1970. Most of these withdrawals were from 87 of the 234 hydrographic areas in the region. Withdrawals ranged from about 1,000 acre-feet (1.2 cubic hectometres) to more than 100,000 acre-feet (123 cubic hectometres). Jordan Valley, which includes Salt Lake City, had the largest withdrawal, about 115,000 acre-feet (142 cubic hectometres).</p>\n<p>An appraisal of the regional ground-water resource indicates the region could sustain an annual net pumpage of about 2.6 million acre-feet (3,200 cubic hectometres). Larger withdrawals could be sustained if only part of the pumped water was used consumptively, if conflicts with existing surface-water rights are resolved, and if extensive treatment, artificial recharge, and reuse of water prove feasible. Ground water stored in the upper 100 feet (30 metres) of saturated deposits of the valley ground-water reservoirs is estimated to be on the order of 300 million acre-feet (370,000 cubic hectometres). Total ground-water storage probably exceeds several billion acre-feet; however, much of this could not be developed within economic feasibility expected over the next several decades.</p>\n<p>Only a few areas of the Great Basin Region have been studied in detail sufficient to enable adequate design of an areawide groundwater development. These areas already have been developed. As of 1973 data for broadly outlining the ground-water resources of the region had been obtained. However, if large-scale planned development is to become a reality, a program for obtaining adequate hydrologic and related data would be a prerequisite. Ideally, the data should be obtained in time to be available for the successively more intensive levels of planning required to implement developments.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813G","usgsCitation":"Eakin, T., Price, D., and Harrill, J., 1976, Summary appraisals of the nation's ground-water resources – Great Basin region: U.S. Geological Survey Professional Paper 813, Report: iv, 37 p.; 1 Plate: 51.25 x 31.75 inches, https://doi.org/10.3133/pp813G.","productDescription":"Report: iv, 37 p.; 1 Plate: 51.25 x 31.75 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":392890,"rank":4,"type":{"id":36,"text":"NGMDB Index 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,{"id":12574,"text":"ofr75318 - 1976 - Hydrologic data for the Idaho National Engineering Laboratory Site, Idaho, 1971 to 1973","interactions":[],"lastModifiedDate":"2012-02-02T00:06:50","indexId":"ofr75318","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-318","title":"Hydrologic data for the Idaho National Engineering Laboratory Site, Idaho, 1971 to 1973","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division ;\r\navailable from National Technical Information Service,","doi":"10.3133/ofr75318","isbn":"pbk","usgsCitation":"Barraclough, J.T., and Jensen, R.G., 1976, Hydrologic data for the Idaho National Engineering Laboratory Site, Idaho, 1971 to 1973: U.S. Geological Survey Open-File Report 75-318, ix, 52 p. :diagrs., maps ;29 cm., https://doi.org/10.3133/ofr75318.","productDescription":"ix, 52 p. :diagrs., maps ;29 cm.","costCenters":[],"links":[{"id":145887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608391","contributors":{"authors":[{"text":"Barraclough, Jack T.","contributorId":8822,"corporation":false,"usgs":true,"family":"Barraclough","given":"Jack","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":166360,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jensen, R. G.","contributorId":63799,"corporation":false,"usgs":true,"family":"Jensen","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":166361,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68057,"text":"ha572 - 1976 - Teton Dam flood of June 1976, Rigby quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T13:52:38","indexId":"ha572","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"572","title":"Teton Dam flood of June 1976, Rigby quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Rigby quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha572","usgsCitation":"Ray, H.A., and Bigelow, B.B., 1976, Teton Dam flood of June 1976, Rigby quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 572, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha572.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89320,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/572/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Rigby Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.0,43.625 ], [ -112.0,43.75 ], [ -111.875,43.75 ], [ -111.875,43.625 ], [ -112.0,43.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c404","contributors":{"authors":[{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277583,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bigelow, Bruce B.","contributorId":8180,"corporation":false,"usgs":true,"family":"Bigelow","given":"Bruce","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":277582,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61441,"text":"mf719 - 1976 - Preliminary photointerpretation map of landslide and other surficial deposits of the Mount Vaca, Vacaville, and parts of Courtland, Davis, Lake Berryessa, and Woodland 15-minute quadrangles, Napa and Solano counties, California","interactions":[],"lastModifiedDate":"2025-05-14T19:26:11.961712","indexId":"mf719","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"719","title":"Preliminary photointerpretation map of landslide and other surficial deposits of the Mount Vaca, Vacaville, and parts of Courtland, Davis, Lake Berryessa, and Woodland 15-minute quadrangles, Napa and Solano counties, California","docAbstract":"<p>This map presents preliminary information about the distribution and general character of landslides and other surficial deposits.&nbsp; When used in combination with other types of information, such as data on soils, bedrock geology, slopes, seismic response, hydrology, vegetation and climatic variation, it should be easier to arrive at sound decisions regarding the physical aspects of land use.&nbsp; The U.S. Geological Survey is studying many of these factors as part of its San Francisco Bay Regional Environment and Resources Planning Study in cooperation with the Department of Housing and Urban Development.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf719","isbn":"0607801492","usgsCitation":"Sims, J.D., and Frizzell, V.A., 1976, Preliminary photointerpretation map of landslide and other surficial deposits of the Mount Vaca, Vacaville, and parts of Courtland, Davis, Lake Berryessa, and Woodland 15-minute quadrangles, Napa and Solano counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 719, 1 Plate: 39.65 x 44.34 inches, https://doi.org/10.3133/mf719.","productDescription":"1 Plate: 39.65 x 44.34 inches","costCenters":[],"links":[{"id":360467,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0719/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179733,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0719/report-thumb.jpg"},{"id":485946,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3855.htm"}],"country":"United States","state":"California","county":"Napa County, Solano County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.25,38.75 ], [ -122.25,38.88333333333333 ], [ -121.75,38.88333333333333 ], [ -121.75,38.75 ], [ -122.25,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69659e","contributors":{"authors":[{"text":"Sims, John D.","contributorId":60202,"corporation":false,"usgs":true,"family":"Sims","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frizzell, Virgil A. Jr.","contributorId":46919,"corporation":false,"usgs":true,"family":"Frizzell","given":"Virgil","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":265649,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27728,"text":"wri76106 - 1976 - Mapping and measuring land-cover characteristics of New River Basin, Tennessee, using Landsat digital tapes","interactions":[],"lastModifiedDate":"2018-08-08T13:56:03","indexId":"wri76106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-106","title":"Mapping and measuring land-cover characteristics of New River Basin, Tennessee, using Landsat digital tapes","docAbstract":"<p>Land-cover information is needed to select subbasins within the New River basin, Tennessee, for the study of hydrologic processes and also is needed to transfer study results to other sites affected by coal mining. It was believed that data recorded by the first Earth Resources Technology Satellite (Landsat-1) could be processed to yield the needed land-cover information. This study demonstrates that digital computer processing of the spectral information contained in each picture element (pixel) of 1.1 acres (4,500 m2) can produce maps and tables of the areal extent of selected land-cover categories.</p><p>The distribution of water, rock, agricultural areas, evergreens, bare earth, hardwoods, and uncategorized areas, is portrayed on a map of the entire New River basin (1:62,500 scale) and on 15 quadrangles (1:24,000 scale). Although some categories are a mixture of land-cover types, they portray the predominant component named. Tables quantify the area of each category and indicate that agriculture covers 5 percent of the basin, evergreens cover 7 percent, bare earth covers 6 percent, three categories of hardwoods cover 81 percent, and water, rock, and uncategorized areas each cover less than 1 percent of the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76106","usgsCitation":"Hollyday, E., and Sauer, S., 1976, Mapping and measuring land-cover characteristics of New River Basin, Tennessee, using Landsat digital tapes: U.S. Geological Survey Water-Resources Investigations Report 76-106, iv, 14 p., https://doi.org/10.3133/wri76106.","productDescription":"iv, 14 p.","numberOfPages":"20","costCenters":[],"links":[{"id":356335,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0106/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0106/report-thumb.jpg"}],"country":"United States","state":"Tennessee","otherGeospatial":"New River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.8636474609375,\n              35.27925852568387\n            ],\n            [\n              -83.9630126953125,\n              35.27925852568387\n            ],\n            [\n              -83.9630126953125,\n              36.96744946416934\n            ],\n            [\n              -85.8636474609375,\n              36.96744946416934\n            ],\n            [\n              -85.8636474609375,\n              35.27925852568387\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69de82","contributors":{"authors":[{"text":"Hollyday, E. F.","contributorId":95062,"corporation":false,"usgs":true,"family":"Hollyday","given":"E. F.","affiliations":[],"preferred":false,"id":198601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sauer, S.P.","contributorId":100869,"corporation":false,"usgs":true,"family":"Sauer","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":198602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29736,"text":"wri7536 - 1976 - Flood hydrology of Butte Basin, 1973 and 1974 water years, Sacramento Valley, California: A progress report","interactions":[],"lastModifiedDate":"2019-07-16T09:00:57","indexId":"wri7536","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-36","title":"Flood hydrology of Butte Basin, 1973 and 1974 water years, Sacramento Valley, California: A progress report","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7536","usgsCitation":"Simpson, R., 1976, Flood hydrology of Butte Basin, 1973 and 1974 water years, Sacramento Valley, California: A progress report: U.S. Geological Survey Water-Resources Investigations Report 75-36, iv, 53 p., https://doi.org/10.3133/wri7536.","productDescription":"iv, 53 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":365565,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0036/report-thumb.jpg"}],"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              -121.75048828124999,\n              38.773357720269075\n            ],\n            [\n              -121.95098876953125,\n              37.99183365313853\n            ],\n            [\n              -121.66534423828125,\n              37.98750437106374\n            ],\n            [\n              -121.4923095703125,\n              38.453588708941375\n            ],\n            [\n              -121.1572265625,\n              38.659777730712534\n            ],\n            [\n              -121.46759033203125,\n              38.79690830348427\n            ],\n            [\n              -121.75048828124999,\n              38.773357720269075\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef10e","contributors":{"authors":[{"text":"Simpson, R.G.","contributorId":16016,"corporation":false,"usgs":true,"family":"Simpson","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":202036,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68055,"text":"ha573 - 1976 - Teton Dam flood of June 1976, Lewisville quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T13:58:07","indexId":"ha573","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"573","title":"Teton Dam flood of June 1976, Lewisville quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Lewisville quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha573","usgsCitation":"Ray, H.A., and Bigelow, B.B., 1976, Teton Dam flood of June 1976, Lewisville quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 573, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha573.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186033,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89318,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/573/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Lewisville Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.125,43.625 ], [ -112.125,43.75 ], [ -112.0,43.75 ], [ -112.0,43.625 ], [ -112.125,43.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684975","contributors":{"authors":[{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bigelow, Bruce B.","contributorId":8180,"corporation":false,"usgs":true,"family":"Bigelow","given":"Bruce","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":277577,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68054,"text":"ha575 - 1976 - Teton Dam flood of June 1976, Idaho Falls South quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T14:11:27","indexId":"ha575","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"575","title":"Teton Dam flood of June 1976, Idaho Falls South quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Idaho Falls South quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha575","usgsCitation":"Ray, H.A., and Matthai, H.F., 1976, Teton Dam flood of June 1976, Idaho Falls South quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 575, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha575.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89317,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/575/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Idaho Falls South Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.125,43.375 ], [ -112.125,43.5 ], [ -112.0,43.5 ], [ -112.0,43.375 ], [ -112.125,43.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843c1","contributors":{"authors":[{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matthai, Howard F.","contributorId":106491,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":277576,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27040,"text":"wri7671 - 1976 - Mathematical model of the West Bolsa Ground-water Basin, San Benito County, California","interactions":[],"lastModifiedDate":"2019-07-17T13:51:27","indexId":"wri7671","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-71","title":"Mathematical model of the West Bolsa Ground-water Basin, San Benito County, California","docAbstract":"Simulation of the West Bolsa ground-water basin hydrology in California had provided values of basin recharge and discharge and nodally distributed values of transmissivity and storage coefficient. Average net recharge from April 1945 to March 1969 was 6.2 cubic feet per second and occurred as subsurace recharge and infiltration of rain and minor streamflow. Discharge from the basin during the same period was 8.1 cubic feet per second and occurred as pumping and leakage from confined parts of the basin. Values of transmissivity used in the model generally range from 3,300 to 20,000 feet squared per day. Values of storage coefficient used in the model range from 0.0005 to 0.10. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7671","usgsCitation":"Faye, R.E., 1976, Mathematical model of the West Bolsa Ground-water Basin, San Benito County, California: U.S. Geological Survey Water-Resources Investigations Report 76-71, v, 54 p. , https://doi.org/10.3133/wri7671.","productDescription":"v, 54 p. ","costCenters":[],"links":[{"id":159013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0071/report-thumb.jpg"},{"id":365653,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Benito County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-121.6434,36.8935],[-121.6428,36.8935],[-121.6272,36.9119],[-121.6197,36.9094],[-121.6108,36.9009],[-121.5998,36.8988],[-121.5947,36.9025],[-121.5803,36.8996],[-121.5749,36.8929],[-121.571,36.8966],[-121.5623,36.8963],[-121.56,36.8968],[-121.5592,36.9063],[-121.5587,36.9095],[-121.553,36.9146],[-121.544,36.9184],[-121.5389,36.9221],[-121.5373,36.9271],[-121.5288,36.9336],[-121.5187,36.9419],[-121.5175,36.9415],[-121.5154,36.947],[-121.5115,36.9525],[-121.5128,36.9584],[-121.5049,36.9639],[-121.4987,36.9717],[-121.4903,36.9805],[-121.4869,36.9837],[-121.4713,36.9785],[-121.4678,36.979],[-121.4633,36.9818],[-121.4582,36.986],[-121.4444,36.9853],[-121.4343,36.9769],[-121.4278,36.9684],[-121.4195,36.9608],[-121.3774,36.9601],[-121.3446,36.9606],[-121.257,36.9596],[-121.2116,36.9607],[-121.2127,36.958],[-121.2143,36.9539],[-121.2234,36.947],[-121.2329,36.9364],[-121.2333,36.9287],[-121.2291,36.9206],[-121.2232,36.9152],[-121.2151,36.9144],[-121.2001,36.9142],[-121.1927,36.9143],[-121.188,36.913],[-121.1839,36.9099],[-121.1819,36.8986],[-121.1789,36.8914],[-121.1695,36.8838],[-121.1653,36.8766],[-121.1617,36.8694],[-121.1524,36.8632],[-121.1453,36.8528],[-121.1439,36.842],[-121.138,36.8361],[-121.1159,36.826],[-121.0597,36.8032],[-120.9334,36.7521],[-120.9183,36.7414],[-120.8233,36.6659],[-120.7814,36.6332],[-120.7623,36.6171],[-120.7448,36.6032],[-120.7082,36.5732],[-120.6682,36.5419],[-120.6497,36.5275],[-120.6317,36.5127],[-120.6149,36.4997],[-120.597,36.4881],[-120.5973,36.4731],[-120.5971,36.4586],[-120.5975,36.4441],[-120.5976,36.4137],[-120.5972,36.3847],[-120.5969,36.3275],[-120.6089,36.3238],[-120.6162,36.3192],[-120.6293,36.3168],[-120.6356,36.3181],[-120.6447,36.3176],[-120.6521,36.3157],[-120.6629,36.3124],[-120.6658,36.3106],[-120.6787,36.2982],[-120.6821,36.2945],[-120.6826,36.2918],[-120.6814,36.2859],[-120.675,36.2787],[-120.6732,36.2719],[-120.6799,36.266],[-120.695,36.2799],[-120.6973,36.283],[-120.71,36.2884],[-120.722,36.296],[-120.7272,36.2986],[-120.7365,36.3044],[-120.744,36.3089],[-120.7531,36.3088],[-120.7577,36.3083],[-120.7432,36.2976],[-120.732,36.2773],[-120.7198,36.262],[-120.7156,36.2506],[-120.7102,36.2353],[-120.7067,36.2267],[-120.7065,36.2172],[-120.7047,36.2118],[-120.7063,36.204],[-120.7091,36.2004],[-120.7159,36.1971],[-120.7222,36.1993],[-120.7308,36.2015],[-120.7467,36.1982],[-120.757,36.1999],[-120.7633,36.2043],[-120.7657,36.2116],[-120.7744,36.2188],[-120.7871,36.2277],[-120.7964,36.2344],[-120.8085,36.2411],[-120.8161,36.2541],[-120.8207,36.2568],[-120.8265,36.2608],[-120.8404,36.2747],[-120.8474,36.281],[-120.8561,36.2868],[-120.8642,36.2926],[-120.8762,36.2934],[-120.891,36.2914],[-120.8939,36.2977],[-120.9055,36.3044],[-120.9107,36.3088],[-120.9199,36.3115],[-120.9221,36.3096],[-120.9267,36.3082],[-120.9334,36.3004],[-120.9355,36.2949],[-120.9394,36.2881],[-120.9445,36.2835],[-120.9495,36.2785],[-120.9546,36.2752],[-120.9639,36.2828],[-120.968,36.2878],[-120.9863,36.2911],[-120.9888,36.2748],[-120.9894,36.2757],[-120.999,36.2701],[-121.012,36.2654],[-121.0257,36.2612],[-121.0247,36.2716],[-121.0242,36.2752],[-121.0328,36.2747],[-121.039,36.2719],[-121.0412,36.3231],[-121.1534,36.4155],[-121.1703,36.4275],[-121.1913,36.4454],[-121.1977,36.4503],[-121.2125,36.4714],[-121.2245,36.4717],[-121.2292,36.4752],[-121.2306,36.4888],[-121.2354,36.4983],[-121.2372,36.5014],[-121.2384,36.5041],[-121.2448,36.5063],[-121.2585,36.5061],[-121.2664,36.5033],[-121.2774,36.5049],[-121.2825,36.5044],[-121.2894,36.5065],[-121.2963,36.506],[-121.3031,36.5045],[-121.3065,36.5013],[-121.3094,36.5026],[-121.3111,36.5031],[-121.3123,36.5067],[-121.3001,36.5227],[-121.2962,36.5269],[-121.2963,36.5318],[-121.3099,36.5484],[-121.3191,36.5501],[-121.3255,36.5536],[-121.3279,36.5568],[-121.3316,36.5712],[-121.325,36.579],[-121.3217,36.5877],[-121.3226,36.5981],[-121.321,36.604],[-121.32,36.61],[-121.3288,36.618],[-121.3376,36.6256],[-121.3413,36.6368],[-121.349,36.6458],[-121.3589,36.652],[-121.3624,36.6565],[-121.3687,36.6559],[-121.371,36.6541],[-121.379,36.6535],[-121.3882,36.6543],[-121.4002,36.655],[-121.4066,36.6576],[-121.4109,36.6661],[-121.4116,36.672],[-121.4185,36.6751],[-121.4306,36.6776],[-121.4437,36.6738],[-121.4513,36.6791],[-121.4653,36.6857],[-121.4772,36.7005],[-121.4849,36.7121],[-121.4821,36.7144],[-121.4718,36.7164],[-121.465,36.7183],[-121.4542,36.7217],[-121.4491,36.7245],[-121.4608,36.732],[-121.4609,36.7379],[-121.4639,36.7433],[-121.4709,36.7459],[-121.4756,36.7522],[-121.4747,36.7581],[-121.4753,36.7594],[-121.4829,36.7652],[-121.4972,36.7627],[-121.5081,36.7621],[-121.5246,36.7768],[-121.5987,36.8385],[-121.6219,36.8463],[-121.6417,36.8731],[-121.6401,36.8786],[-121.6434,36.8935]]]},\"properties\":{\"name\":\"San Benito\",\"state\":\"CA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db60ffd7","contributors":{"authors":[{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":197453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26658,"text":"wri7683 - 1976 - Measured and simulated ground-water levels in the Franklin area, southeastern Virginia","interactions":[],"lastModifiedDate":"2019-07-17T09:48:49","indexId":"wri7683","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-83","title":"Measured and simulated ground-water levels in the Franklin area, southeastern Virginia","docAbstract":"The Lower Cretaceous aquifer is the principal source of water in Southeastern Virginia. Synoptic water-level measurements made since 1970 have been used to verify a digital model of the aquifer. Measurements made in December 1973, August and December 1974 were used to further verify the model, using updated pumpage for those periods. The close agreement of the potentiometric maps based on measured and simulated water levels indicates that the model is simulating hydrologic conditions satisfactorily. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7683","usgsCitation":"Cosner, O.J., 1976, Measured and simulated ground-water levels in the Franklin area, southeastern Virginia: U.S. Geological Survey Water-Resources Investigations Report 76-83, 5 Plates: 34.04 x 22.01 inches, https://doi.org/10.3133/wri7683.","productDescription":"5 Plates: 34.04 x 22.01 inches","costCenters":[],"links":[{"id":365655,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365654,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365656,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365657,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365658,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0083/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Franklin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.0306396484375,\n              36.608913667193676\n            ],\n            [\n              -76.7889404296875,\n              36.608913667193676\n            ],\n            [\n              -76.7889404296875,\n              36.71466899719828\n            ],\n            [\n              -77.0306396484375,\n              36.71466899719828\n            ],\n            [\n              -77.0306396484375,\n              36.608913667193676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61081f","contributors":{"authors":[{"text":"Cosner, O. J.","contributorId":19587,"corporation":false,"usgs":true,"family":"Cosner","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25467,"text":"wri7699 - 1976 - Effects of off-road vehicle use on the hydrology and landscape of arid environments in central and southern California","interactions":[],"lastModifiedDate":"2019-11-22T15:14:50","indexId":"wri7699","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-99","title":"Effects of off-road vehicle use on the hydrology and landscape of arid environments in central and southern California","docAbstract":"<p>Two widely separated sites in California used for motorcycle hill-climbing were studied to evaluate the impact on the landscape and hydrology. At Panoche Hills in central California, an area formerly used by motorcycles together with an adjacent unused area were monitored from 1971 to 1975. Observations in both areas included measurements of precipitation, runoff, soil moisture, soil bulk density, plant cover, and erosion surveys. At Dove Spring Canyon in southern California erosion was measured on a site that is currently being used for motorcycle hill-climbing. At the Panoche Hills site, the area used by motorcycles produced about eight times as much runoff as the unused area. Similarly, sediment yield from the used areas was 857 cubic meters/sq km, while the quantity of sediment from the unused area was not measurable by standard methods. At the Dove Spring Canyon site, which is still being used for hill-climbing, erosion surveys show that degradation in trails has been as much as 0.3 m in the period 1973-75. Compaction of soils and reduction of permeability appears to be the most serious hydrologic impact of motorcycle use at Panoche Hills. Increased bulk density of soils reduces depth of moisture penetration which deprives plants of moisture needed for growth. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7699","usgsCitation":"Snyder, C., Frickel, D., Hadley, R.F., and Miller, R., 1976, Effects of off-road vehicle use on the hydrology and landscape of arid environments in central and southern California: U.S. Geological Survey Water-Resources Investigations Report 76-99, iv, 45 p. , https://doi.org/10.3133/wri7699.","productDescription":"iv, 45 p. ","costCenters":[],"links":[{"id":156971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0099/report-thumb.jpg"},{"id":369494,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0099/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Dove Spring Canyon, Panoche Hills","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.14624023437499,\n              35.14237113713991\n            ],\n            [\n              -118.07556152343749,\n              35.14237113713991\n            ],\n            [\n              -118.07556152343749,\n              36.6551995018735\n            ],\n            [\n              -121.14624023437499,\n              36.6551995018735\n            ],\n            [\n              -121.14624023437499,\n              35.14237113713991\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4445","contributors":{"authors":[{"text":"Snyder, Charles T.","contributorId":53767,"corporation":false,"usgs":true,"family":"Snyder","given":"Charles T.","affiliations":[],"preferred":false,"id":193811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frickel, D. G.","contributorId":11213,"corporation":false,"usgs":true,"family":"Frickel","given":"D. G.","affiliations":[],"preferred":false,"id":193809,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":193810,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":193812,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68053,"text":"ha574 - 1976 - Teton Dam flood of June 1976, Idaho Falls North quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T14:07:43","indexId":"ha574","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"574","title":"Teton Dam flood of June 1976, Idaho Falls North quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Idaho Falls North quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha574","usgsCitation":"Ray, H.A., and Matthai, H.F., 1976, Teton Dam flood of June 1976, Idaho Falls North quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 574, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha574.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89316,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/574/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Idaho Falls North Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.125,43.5 ], [ -112.125,43.625 ], [ -112.0,43.625 ], [ -112.0,43.5 ], [ -112.125,43.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699da2","contributors":{"authors":[{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matthai, Howard F.","contributorId":106491,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":277574,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68225,"text":"ha549 - 1976 - Water resources of the Big Fork River watershed, north-central Minnesota","interactions":[{"subject":{"id":49274,"text":"ofr74126 - 1974 - Water resources of the Big Fork River watershed, north-central Minnesota","indexId":"ofr74126","publicationYear":"1974","noYear":false,"title":"Water resources of the Big Fork River watershed, north-central Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":68225,"text":"ha549 - 1976 - Water resources of the Big Fork River watershed, north-central Minnesota","indexId":"ha549","publicationYear":"1976","noYear":false,"title":"Water resources of the Big Fork River watershed, north-central Minnesota"},"id":1}],"lastModifiedDate":"2016-05-16T09:59:48","indexId":"ha549","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"549","title":"Water resources of the Big Fork River watershed, north-central Minnesota","docAbstract":"<p>The Big Fork River watershed is one of 39 watershed units designated by the Minnesota Department of Natural Resources for evaluation of the State 's water resources. Included is an appraisal of the occurrence, quantity, quality, and availability of ground and surface waters. Water resources are not intensively developed anywhere in the watershed. Most development is in the southern half, as much of the northern half is peat-covered wetlands. Essentially all water used is withdrawn from ground-water sources, mainly glacial drift, which ranges from 0 to 250 feet in thickness. Most ground water is of the calcium or sodium bicarbonated type. The degree of mineralization increases down-gradient in the flow system. Groundwater is typically very hard and high in iron and manganese. Lakes and large areas of wetlands have a natural regulating effect on streamflow. Water in streams is of the calcium bicarbonate type. The amount of mineralization at a given time reflects surficial geology, being greatest in streams draining till areas and least in streams draining peatlands. Water drained from peatlands is commonly higher in color and iron and lower in pH than water from areas of mineral soil.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha549","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Lindholm, G.F., Helgesen, J.O., and Ericson, D.W., 1976, Water resources of the Big Fork River watershed, north-central Minnesota: U.S. Geological Survey Hydrologic Atlas 549, 7 Plates: 37.5 x 52.0 inches or smaller, https://doi.org/10.3133/ha549.","productDescription":"7 Plates: 37.5 x 52.0 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":38695,"text":"pp813F - 1976 - Summary appraisals of the nation's ground-water resources–Texas-Gulf region","interactions":[],"lastModifiedDate":"2021-12-03T19:28:08.045954","indexId":"pp813F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"F","title":"Summary appraisals of the nation's ground-water resources–Texas-Gulf region","docAbstract":"<p>Ground water in the Texas-Gulf Region is a large and important resource that can provide a more significant percentage of the total water supply of the region. Total water requirements within the region are projected to rise sharply from 14 million acre-feet (17 cubic kilometres) in 1970 to nearly 26 million acre-feet (32 cubic kilometres) in 2020. About half of the water used in 1970 was ground water.</p>\n<p>An estimated total of 1.04 billion acre-feet (1,280 cubic kilometres) of recoverable water containing less than 3,000 milligrams per litre dissolved solids is stored above a depth of 400 feet (122 metres) in the aquifers of the region. In addition, part of an estimated 3.28 billion acre-feet (4,040 cubic kilometres) of water in storage below 400 feet (122 metres) is recoverable. Although not all of the ground water in storage is recoverable, a significant amount is available for development; and an enormous quantity is accessible should occasions prompt its use on a time-limited basis.</p>\n<p>The total steady-state yield (amount of water that approximates the maximum perennial replenishment from precipitation) of the region's aquifers is about 4.6 million acre-feet (5.7 cubic kilometres) annually, or about 2.3 times the ground-water usage in 1970 if the large mining draft on the High Plains is not considered as part of the total steady-state yield. Because of the large quantity of recoverable groundwater in storage, the steady-state yield can be augmented for a very long time on a \"deferred\" basis, whereby the economic use of the water that is withdrawn from storage in excess of the steady-state yield may result in a strengthened economy.</p>\n<p>An important goal in programs for meeting future water needs should be to identify the full potential of the available ground-water resources. The subsurface reservoirs may be utilized not only as sources of fresh and treatable water, but as storage facilities for other freshwater supplies and as possible sources of geothermal energy. Some saline-water reservoirs may be suitable for liquid-waste storage or disposal.</p>\n<p>Large-scale and unregulated ground-water pumping may result in hydrologic problems such as declining water levels, streamflow depletion, and land-surface subsidence; but studies on proper development of the ground-water reservoirs could provide solutions to many of the problems. Water rights and other legal concepts should be based on sound hydrologic principles to assist development of water resources in an orderly and efficient manner.</p>\n<p>Because significant amounts of ground water are available, the opportunities for expanded and conjunctive use of ground water and surface water should be considered in regional plans for water development and conservation. The complexities of water management and the difficulties of achieving an integrated system of total-water management will require additional technical information.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813F","usgsCitation":"Baker, E.T., and Wall, J.R., 1976, Summary appraisals of the nation's ground-water resources–Texas-Gulf region: U.S. Geological Survey Professional Paper 813, Report: iii, 29 p.; 3 Plates: 39.79 x 34.18 inches or smaller, https://doi.org/10.3133/pp813F.","productDescription":"Report: iii, 29 p.; 3 Plates: 39.79 x 34.18 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":392453,"rank":6,"type":{"id":36,"text":"NGMDB Index 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,{"id":68535,"text":"ha542 - 1976 - Preliminary maps showing ground-water resources in the Lower Colorado River region, Arizona, Nevada, New Mexico, and Utah","interactions":[],"lastModifiedDate":"2017-02-21T10:39:35","indexId":"ha542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"542","title":"Preliminary maps showing ground-water resources in the Lower Colorado River region, Arizona, Nevada, New Mexico, and Utah","docAbstract":"<p><span>This atlas was prepared to meet the need for information on the areal distribution, quantity, and availability of ground water in the lower Colorado River region, an area of about 140,000 square miles in parts of Arizona, Nevada, New Mexico, and Utah. The maps are necessarily generalized in places owing to the lack of sufficient data. In general the geohydrologic information pertains to large areas, and local exceptions occur. Users needing more detailed information for specific areas may address inquiries to the district chief of the U.S. Geological Survey at the addresses given in the section “Selected References.” The maps were prepared using data from previously published reports, data collected by other Federal State, and local agencies, and data from the files of the U.S. Geological Survey offices in Arizona, Nevada, New Mexico, and Utah. The report is the result of the lower Colorado River region Type I framework study made in cooperation with the U.S. Bureau of Reclamation.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha542","collaboration":"Prepared in cooperation with the U.S. Bureau of Reclamation","usgsCitation":"Brown, S., 1976, Preliminary maps showing ground-water resources in the Lower Colorado River region, Arizona, Nevada, New Mexico, and Utah: U.S. Geological Survey Hydrologic Atlas 542, 3 Sheets: 58.00 x 41.25 inches or smaller, https://doi.org/10.3133/ha542.","productDescription":"3 Sheets: 58.00 x 41.25 inches or smaller","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":186122,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90145,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/542/plate-3.pdf","text":"Sheet 3","size":"11.45 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Generalized well-production potential"},{"id":90144,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/542/plate-2.pdf","text":"Sheet 2","size":"13.86 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Generalized depth to water as of 1965"},{"id":90143,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/542/plate-1.pdf","text":"Sheet 1","size":"10.87 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Generalized geohydrologic framework"}],"scale":"1000000","country":"United States","state":"Arizona, Nevada, New Mexico, Utah","otherGeospatial":"Lower Colorado River region","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115,32 ], [ -115,39 ], [ -108,39 ], [ -108,32 ], [ -115,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6670f3","contributors":{"authors":[{"text":"Brown, S. G.","contributorId":46914,"corporation":false,"usgs":true,"family":"Brown","given":"S. G.","affiliations":[],"preferred":false,"id":278413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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