{"pageNumber":"1750","pageRowStart":"43725","pageSize":"25","recordCount":46595,"records":[{"id":68497,"text":"ha558 - 1976 - Water resources of northwestern Wyoming","interactions":[{"subject":{"id":13186,"text":"ofr75409 - 1975 - Water resources of northwestern Wyoming","indexId":"ofr75409","publicationYear":"1975","noYear":false,"title":"Water resources of northwestern Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":68497,"text":"ha558 - 1976 - Water resources of northwestern Wyoming","indexId":"ha558","publicationYear":"1976","noYear":false,"title":"Water resources of northwestern Wyoming"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:31","indexId":"ha558","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":"558","title":"Water resources of northwestern Wyoming","docAbstract":"This 3-sheet map report describes the hydrologic conditions in northwestern Wyoming. The increasing number of tourists and residents and the shifting of overnight accommodations for tourists from Yellowstone and Grand Teton National Parks to nearby areas may result in the need for development of additional water supplies in northwestern Wyoming. Hydrologic data have been collected from wells, springs, streams, and lakes in northwestern Wyoming and are given in maps, tables, and graphs. Using streamflow and water-table data, the transmissivity of a segment of an aquifer in alluvium and glacial outwash in Jackson Hole was estimated to be 30,000 feet squared per day (2,800 meters squared per day). Water in the study area is used for irrigation and for public, domestic, and commercial supplies. (Woodard-USGS)","language":"ENGLISH","doi":"10.3133/ha558","usgsCitation":"Cox, E.R., 1976, Water resources of northwestern Wyoming: U.S. Geological Survey Hydrologic Atlas 558, 5 col. maps on 3 sheets ;102 x 76 cm. or smaller fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha558.","productDescription":"5 col. maps on 3 sheets ;102 x 76 cm. or smaller fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":185978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90056,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/558/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90057,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/558/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90058,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/558/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.08333333333333,43 ], [ -111.08333333333333,45 ], [ -109.83333333333333,45 ], [ -109.83333333333333,43 ], [ -111.08333333333333,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d2e4b07f02db547f12","contributors":{"authors":[{"text":"Cox, Edward Riley","contributorId":40966,"corporation":false,"usgs":true,"family":"Cox","given":"Edward","email":"","middleInitial":"Riley","affiliations":[],"preferred":false,"id":278329,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68434,"text":"ha556 - 1976 - Water resources of the Rainy Lake watershed, northeastern Minnesota","interactions":[{"subject":{"id":44066,"text":"ofr754 - 1975 - Water resources of the Rainy Lake watershed, northeastern Minnesota","indexId":"ofr754","publicationYear":"1975","noYear":false,"title":"Water resources of the Rainy Lake watershed, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":68434,"text":"ha556 - 1976 - Water resources of the Rainy Lake watershed, northeastern Minnesota","indexId":"ha556","publicationYear":"1976","noYear":false,"title":"Water resources of the Rainy Lake watershed, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2016-05-09T09:08:50","indexId":"ha556","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":"556","title":"Water resources of the Rainy Lake watershed, northeastern Minnesota","docAbstract":"<p>The watershed includes 1,481 lakes that are 10 acres (4 square hectometers) or larger (Minnesota Division of Waters, Soils, and Minerals, 1968). The area of these lakes total about 435,000 acres (176,000 hm<sup>2</sup>) or 15 percent of the watershed. Most of the lakes are smaller than 250 acres (101 hm<sup>2</sup>) (graph); data pertaining to selected large lakes are given in the table below.</p>\n<p>More than 60 percent of the lakes larger than 10 acres (4 hm<sup>2</sup>) are in the BWCA. The primitive character of the BWCA is maintained in accordance with the Wilderness Act of September 3, 1964. Most lakes not in the BWCA were assigned a Public Waters Classification by the Minnesota Department of Natural Resources, based upon the suitability of the lake for future shoreland development (unpublished data from the Minnesota Department of Natural Resources). &ldquo;Natural environment&rdquo; is most restrictive and &ldquo;general development&rdquo; least restrictive with respect to development standards. About 80 percent of lakes classified in the watershed have been designated &ldquo;natural environment.&rdquo;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ha556","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Ericson, D.W., Lindholm, G.F., and Helgesen, J.O., 1976, Water resources of the Rainy Lake watershed, northeastern Minnesota: U.S. Geological Survey Hydrologic Atlas 556, 2 Plates: 55.73 x 34.50 inches, https://doi.org/10.3133/ha556.","productDescription":"2 Plates: 55.73 x 34.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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F.","contributorId":18374,"corporation":false,"usgs":true,"family":"Lindholm","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":278204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Helgesen, John O.","contributorId":101630,"corporation":false,"usgs":true,"family":"Helgesen","given":"John","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":278206,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68296,"text":"ha581 - 1976 - Teton Dam flood of June 1976, Pingree quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T14:41:37","indexId":"ha581","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":"581","title":"Teton Dam flood of June 1976, Pingree 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 Pingree quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha581","usgsCitation":"Hubbard, L.L., and Bartells, J.H., 1976, Teton Dam flood of June 1976, Pingree quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 581, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha581.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89723,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/581/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Pingree Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.625,43.0 ], [ -112.625,43.125 ], [ -112.5,43.125 ], [ -112.5,43.0 ], [ -112.625,43.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683c78","contributors":{"authors":[{"text":"Hubbard, Larry L.","contributorId":91492,"corporation":false,"usgs":true,"family":"Hubbard","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartells, John H.","contributorId":54240,"corporation":false,"usgs":true,"family":"Bartells","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68295,"text":"ha580 - 1976 - Teton Dam flood of June 1976, Moreland quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T14:37:56","indexId":"ha580","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":"580","title":"Teton Dam flood of June 1976, Moreland 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 aea 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 Moreland quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha580","usgsCitation":"Hubbard, L.L., and Bartells, J.H., 1976, Teton Dam flood of June 1976, Moreland quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 580, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha580.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89722,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/580/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Moreland Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.5,43.125 ], [ -112.5,43.25 ], [ -112.375,43.25 ], [ -112.375,43.125 ], [ -112.5,43.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68417b","contributors":{"authors":[{"text":"Hubbard, Larry L.","contributorId":91492,"corporation":false,"usgs":true,"family":"Hubbard","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartells, John H.","contributorId":54240,"corporation":false,"usgs":true,"family":"Bartells","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277980,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68294,"text":"ha577 - 1976 - Teton Dam flood of June 1976, Firth quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T14:20:50","indexId":"ha577","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":"577","title":"Teton Dam flood of June 1976, Firth 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 Firth quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha577","usgsCitation":"Hubbard, L.L., and Bartells, J.H., 1976, Teton Dam flood of June 1976, Firth quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 577, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha577.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89721,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/577/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Firth Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,43.25 ], [ -112.25,43.375 ], [ -112.125,43.375 ], [ -112.125,43.25 ], [ -112.25,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843a4","contributors":{"authors":[{"text":"Hubbard, Larry L.","contributorId":91492,"corporation":false,"usgs":true,"family":"Hubbard","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277979,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartells, John H.","contributorId":54240,"corporation":false,"usgs":true,"family":"Bartells","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277978,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67965,"text":"ha567 - 1976 - Teton Dam flood of June 1976, Parker quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T12:57:40","indexId":"ha567","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":"567","title":"Teton Dam flood of June 1976, Parker quadrangle, Idaho","docAbstract":"The failure of 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 Parker quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha567","usgsCitation":"Thomas, C.A., and Ray, H.A., 1976, Teton Dam flood of June 1976, Parker quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 567, 1 map :col. ;58 x 50 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha567.","productDescription":"1 map :col. ;58 x 50 cm., folded in envelope 30 x 24 cm.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":185734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89194,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/567/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American datum","country":"United States","state":"Idaho","otherGeospatial":"Henrys Fork;Teton River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.904167,43.875 ], [ -111.904167,44.0 ], [ -111.75,44.0 ], [ -111.75,43.875 ], [ -111.904167,43.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683c3d","contributors":{"authors":[{"text":"Thomas, Cecil Albert","contributorId":64228,"corporation":false,"usgs":true,"family":"Thomas","given":"Cecil","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":277411,"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":277412,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68210,"text":"ha512 - 1976 - Water resources of the Bighorn basin, northwestern Wyoming","interactions":[],"lastModifiedDate":"2022-10-05T18:41:49.200429","indexId":"ha512","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":"512","title":"Water resources of the Bighorn basin, northwestern Wyoming","docAbstract":"<p>This 2-sheet map report includes the part of the Bighorn Basin and adjacent mountains in northwestern Wyoming. Water-bearing properties of the geologic units are summarized. The hydrogeologic map illustrates the distribution of wells in the different units and gives basic data on the yields of wells, depth of wells, depth to water, and dissolved solids and conductance of the water. Aquifers capable of yielding more than 1,000 gpm (gallons per minute) underlie the area everywhere, except in the mountains on the periphery of the basin. In 1970, approximately 29,500 of the 40,475 people living in the Bighorn Basin were served by municipal water supplies. The municipal supply for about 6,300 of these people was from ground water. The natural flows of streams in the Bighorn Basin differ greatly due to a wide range in the meteorologic, topographic, and geologic conditions of the basin. The station locations and the average discharge per square mile are shown on the map and give an indication of the geographic variation of basin yields. The maximum instantaneous discharge that has occurred at each station during its period of record is shown. Most of the runoff in the basin is from snowmelt in the mountains.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha512","usgsCitation":"Lowry, M.E., Lowham, H., and Lines, G.C., 1976, Water resources of the Bighorn basin, northwestern Wyoming: U.S. Geological Survey Hydrologic Atlas 512, 2 Plates: 58.00 × 41.00 inches and 51.00 × 37.50 inches, https://doi.org/10.3133/ha512.","productDescription":"2 Plates: 58.00 × 41.00 inches and 51.00 × 37.50 inches","costCenters":[],"links":[{"id":185624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":407984,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15902.htm","linkFileType":{"id":5,"text":"html"}},{"id":89555,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/512/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89556,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/512/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Wyoming","otherGeospatial":"Big Horn basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.11,\n              43.459\n            ],\n            [\n              -107.1,\n              43.459\n            ],\n            [\n              -107.1,\n              45\n            ],\n            [\n              -110.11,\n              45\n            ],\n            [\n              -110.11,\n              43.459\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699976","contributors":{"authors":[{"text":"Lowry, Marlin E.","contributorId":52552,"corporation":false,"usgs":true,"family":"Lowry","given":"Marlin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":277844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277845,"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":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":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":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":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":9036,"text":"ofr76549 - 1976 - Hydrologic studies of the U.S. Geological Survey related to coal development on Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr76549","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":"76-549","title":"Hydrologic studies of the U.S. Geological Survey related to coal development on Colorado","docAbstract":"This report summarizes the hydrologic studies related to coal development being conducted by the U.S. Geological Survey in the State of Colorado. The objective of the hydrologic data-acquisition program is to collect surface-water quality and quantity data and ground-water level records. These data are needed to define predevelopment conditions and to monitor the effects of construction and operation of coal mines and waste-disposal areas. Data-acquisition activities related to coal development in Colorado have concentrated on the Yampa River basin. A description of the hydrologic data-acquisition activities, including parameters collected and frequency of collection, precedes the summaries of the three interpretive studies currently in progress. Each study summary consists of the project title, definition of the problem being studied, objective of the study, approach of the study, and when known, the schedule for completion of the study and proposed report products resulting from the study. (Woodard-USGS)","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr76549","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Hydrologic studies of the U.S. Geological Survey related to coal development on Colorado: U.S. Geological Survey Open-File Report 76-549, iv, 22 p. :maps ;28 cm., https://doi.org/10.3133/ofr76549.","productDescription":"iv, 22 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605283","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":528883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9981,"text":"ofr76846 - 1976 - Stability of highwalls in surface coal mines, western Powder Ridge Basin, Wyoming and Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr76846","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":"76-846","title":"Stability of highwalls in surface coal mines, western Powder Ridge Basin, Wyoming and Montana","docAbstract":"Preliminary results from the first part of a two-part investigation of the stability of highwalls in open-pit coal mines in the Fort Union Formation of the western Powder River Basin of Wyoming and Montana indicate that these highwalls are subject to time-dependent deformation. Field investigations and laboratory physical-properties tests of coal and overburden rocks suggest that several factors influence highwall stability. Some of these factors are rebound of overconsolidated rocks, desiccation, water, orientation and spacing of fractures, and strength and deformation properties. Factors of safety for a typical highwall in the study area (calculated by the finite-element method) may be less than 1.0 when open fractures are present and the highwall has degraded. Although it is concluded that most open-pit mines in the Fort Union Formation within the study area have generally stable highwalls, these highwalls do deteriorate and become progressively less stable. Because of this, postmining failures are common and could be critical if mining were delayed and then resumed after a period of several months. \r\n\r\nThe second part of the investigation will utilize field measurements of rock-mass properties and instrumentation of actively mined highwalls to obtain data for comparison with the results of the initial investigation. Because the height of highwalls will increase as the more shallow coal is exhausted, these data will also be used to predict the behavior of slopes higher than those presently found in the western Powder River Basin.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76846","usgsCitation":"Lee, F.T., Smith, W.K., and Savage, W.Z., 1976, Stability of highwalls in surface coal mines, western Powder Ridge Basin, Wyoming and Montana: U.S. Geological Survey Open-File Report 76-846, iv, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr76846.","productDescription":"iv, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0846/report-thumb.jpg"},{"id":37780,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0846/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37781,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0846/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ebf","contributors":{"authors":[{"text":"Lee, Fitzhugh T.","contributorId":82272,"corporation":false,"usgs":true,"family":"Lee","given":"Fitzhugh","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":160612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, William K.","contributorId":23544,"corporation":false,"usgs":true,"family":"Smith","given":"William","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":160611,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Savage, William Z.","contributorId":107686,"corporation":false,"usgs":true,"family":"Savage","given":"William","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":160613,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10137,"text":"ofr76627 - 1976 - Progress report on geology of the Edwards aquifer, San Antonio area, Texas, and preliminary interpretation of borehole geophysical and laboratory data on carbonate rocks","interactions":[],"lastModifiedDate":"2021-12-30T19:19:42.107241","indexId":"ofr76627","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":"76-627","title":"Progress report on geology of the Edwards aquifer, San Antonio area, Texas, and preliminary interpretation of borehole geophysical and laboratory data on carbonate rocks","docAbstract":"<p>This report describes the geology and porosity of the rocks of the Edwards aquifer, with particular attention to the eastern half of the San Antonio area. The data were obtained from geologic and geophysical studies of nine cored test holes, from laboratory analyses of samples of the aquifer materials, and from recent stratigraphic studies by other investigators. </p><p>The Georgetown Formation and the Edwards Group or their equivalent stratigraphic units are extensively exposed in central Texas and they occur in the subsurface throughout southern Texas. They consist of a complex sequence of carbonate rocks deposited during Early Cretaceous time under different depositional conditions. Within the study area, the thickness of the carbonate rocks ranges from less than 400 feet (122 m) in the eastern part of the area to more than 600 feet (183 m) in the southwestern part. </p><p>The depositional environments significantly affected the texture and the composition of the sediments. The Maverick Basin in the southwestern part of the study area was a euxinic basin surrounded by a barrier rudistid reef. Fine-grained carbonates and some associated evaporites occur within this basin. The San Marcos Platform in the eastern part of the study area was intermittently submerged by a transgressing continental sea. Much of the sediments are extensively reworked and burrowed by marine organisms. Several thick sequences of dolomites, evaporites, and associated collapsed deposits occur on the San Marcos Platform. The carbonates of the San Marcos Platform are extensively dissolved within the fresh-water zone. Much of the dissolution is selective of beds containing evaporites or porous dolomites. </p><p>The dominant structural feature of the study area is a broad homocline that extends from nearly flat-lying beds on the Edwards Plateau to steeply dipping beds of the deep subsurface of the Gulf Coastal Plain. The homocline is interrupted by the Balcones Fault Zone, which is a zone of normal faults that extend across the study area. The intensity and complexity of faulting increases eastward as part of a progression from gentle flexures in the southwestern part of the study area to a complex pattern of tilted fault blocks on the San Marcos Platform. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76627","collaboration":"Prepared in cooperation with the San Antonio City Water Board and the Texas Water Development Board","usgsCitation":"Maclay, R.W., and Small, T.A., 1976, Progress report on geology of the Edwards aquifer, San Antonio area, Texas, and preliminary interpretation of borehole geophysical and laboratory data on carbonate rocks: U.S. Geological Survey Open-File Report 76-627, Report: 63 p.; 17 Figures: 17.77 x 11.94 inches or smaller, https://doi.org/10.3133/ofr76627.","productDescription":"Report: 63 p.; 17 Figures: 17.77 x 11.94 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":143618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0627/report-thumb.jpg"},{"id":393688,"rank":17,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-15.pdf","text":"Figure 15","linkFileType":{"id":1,"text":"pdf"}},{"id":393690,"rank":19,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-17.pdf","text":"Figure 17","linkFileType":{"id":1,"text":"pdf"}},{"id":393685,"rank":14,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-12.pdf","text":"Figure 12","linkFileType":{"id":1,"text":"pdf"}},{"id":393684,"rank":13,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-11.pdf","text":"Figure 11","linkFileType":{"id":1,"text":"pdf"}},{"id":393681,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-8.pdf","text":"Figure 8","linkFileType":{"id":1,"text":"pdf"}},{"id":393689,"rank":18,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-16.pdf","text":"Figure 16","linkFileType":{"id":1,"text":"pdf"}},{"id":393687,"rank":16,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-14.pdf","text":"Figure 14","linkFileType":{"id":1,"text":"pdf"}},{"id":393679,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}},{"id":393682,"rank":11,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-9.pdf","text":"Figure 9","linkFileType":{"id":1,"text":"pdf"}},{"id":393683,"rank":12,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-10.pdf","text":"Figure 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2","linkFileType":{"id":1,"text":"pdf"}},{"id":393677,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":393674,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1976/0627/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":393673,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0627/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Edwards aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -100.634765625,\n              28.825425374477224\n            ],\n            [\n              -97.44873046875,\n              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,{"id":10164,"text":"ofr76783 - 1976 - Chemical composition data and calculated aquifer temperature for selected wells and springs of Honey Lake Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr76783","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":"76-783","title":"Chemical composition data and calculated aquifer temperature for selected wells and springs of Honey Lake Valley, California","docAbstract":"Major element, minor element, and gas composition data are tabulated for 15 springs and wells in Honey Lake Valley, California. Wendel and Amedee hot springs issue Na-S04-C1 waters at boiling or near boiling temperatures; the remaining springs and wells issue Na-HC03 waters at temperatures ranging from 14 to 33 deg C. Gases escaping from the hot springs are principally nitrogen with minor amounts of methane. The geothermometers calculated from the chemical data are also tabulated for each spring. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76783","usgsCitation":"Mariner, R.H., Presser, T.S., and Evans, W.C., 1976, Chemical composition data and calculated aquifer temperature for selected wells and springs of Honey Lake Valley, California: U.S. Geological Survey Open-File Report 76-783, 10 leaves :map ;27 cm., https://doi.org/10.3133/ofr76783.","productDescription":"10 leaves :map ;27 cm.","costCenters":[],"links":[{"id":144137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e4114","contributors":{"authors":[{"text":"Mariner, Robert H.","contributorId":81075,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":160918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":160919,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Evans, William C.","contributorId":104903,"corporation":false,"usgs":true,"family":"Evans","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160920,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10029,"text":"ofr76874 - 1976 - Shallow sedimentary framework of Georges Bank","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr76874","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":"76-874","title":"Shallow sedimentary framework of Georges Bank","docAbstract":"Two thousand nine hundred kilometers of minisparker data were collected on Georges Bank by the United States Geological Survey during October of 1975. Several sedimentary features have been observed in the data, The bank is recognized as a compound feature resulting from erosion of Tertiary coastal-plain strata followed by deposition of an extensive sediment wedge on the western flank of the cuesta. Marine planation (probably Late Pleistocene) truncated this bank morphology producing an erosion surface roughly paralleling the present sea floor. The truncated bank surface is blanketed by a veneer of complex Late Pleistocene drift which masks underlying features and is being reworked by modern processes. Present bank morphology is inferred-to be arather recent development. \r\n\r\nA proper understanding of the significance of complex bank sediments with respect to the potential geologic hazards of drilling or placement of bottom. supported structures necessitates a more detailed seismic reflection program, in conjunction with geotechnical analysis of core-samples.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76874","usgsCitation":"Lewis, R.S., and Sylwester, R., 1976, Shallow sedimentary framework of Georges Bank: U.S. Geological Survey Open-File Report 76-874, 11 [i.e. 22] leaves :ill. (4 fold.) maps ;36 cm.; (14 p. - PGS), https://doi.org/10.3133/ofr76874.","productDescription":"11 [i.e. 22] leaves :ill. (4 fold.) maps ;36 cm.; (14 p. - PGS)","costCenters":[],"links":[{"id":143902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0874/report-thumb.jpg"},{"id":37870,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0874/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37871,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0874/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37872,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0874/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37873,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0874/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0874/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699f2b","contributors":{"authors":[{"text":"Lewis, R. S.","contributorId":19951,"corporation":false,"usgs":true,"family":"Lewis","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":160698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sylwester, R. E.","contributorId":34137,"corporation":false,"usgs":true,"family":"Sylwester","given":"R. E.","affiliations":[],"preferred":false,"id":160699,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8115,"text":"ofr76851 - 1976 - Chemical analysis and statistical data for water samples collected in Colorado, New Mexico, and Arizona as part of a study of surface-water and stream-sediment sampling techniques used in uranium exploration","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr76851","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":"76-851","title":"Chemical analysis and statistical data for water samples collected in Colorado, New Mexico, and Arizona as part of a study of surface-water and stream-sediment sampling techniques used in uranium exploration","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76851","usgsCitation":"Burnside, S.S., and Wenrich-Verbeek, K.J., 1976, Chemical analysis and statistical data for water samples collected in Colorado, New Mexico, and Arizona as part of a study of surface-water and stream-sediment sampling techniques used in uranium exploration: U.S. Geological Survey Open-File Report 76-851, i, 314 p. :1 map ;29 cm., https://doi.org/10.3133/ofr76851.","productDescription":"i, 314 p. :1 map ;29 cm.","costCenters":[],"links":[{"id":140648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0851/report-thumb.jpg"},{"id":112904,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0851/report.pdf","size":"9829","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4953","contributors":{"authors":[{"text":"Burnside, Sylvia S.","contributorId":101257,"corporation":false,"usgs":true,"family":"Burnside","given":"Sylvia","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":157175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wenrich-Verbeek, Karen J.","contributorId":101662,"corporation":false,"usgs":true,"family":"Wenrich-Verbeek","given":"Karen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157176,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4724,"text":"twri07C1 - 1976 - Finite difference model for aquifer simulation in two dimensions with results of numerical experiments","interactions":[{"subject":{"id":56027,"text":"ofr70211 - 1970 - A program to simulate and aquifer using alternating direction implicit-iterative procedure","indexId":"ofr70211","publicationYear":"1970","noYear":false,"title":"A program to simulate and aquifer using alternating direction implicit-iterative procedure"},"predicate":"SUPERSEDED_BY","object":{"id":4724,"text":"twri07C1 - 1976 - Finite difference model for aquifer simulation in two dimensions with results of numerical experiments","indexId":"twri07C1","publicationYear":"1976","noYear":false,"title":"Finite difference model for aquifer simulation in two dimensions with results of numerical experiments"},"id":1}],"lastModifiedDate":"2021-04-05T15:32:12.694992","indexId":"twri07C1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"07-C1","title":"Finite difference model for aquifer simulation in two dimensions with results of numerical experiments","docAbstract":"<p>The model will simulate ground-water flow in an artesian aquifer, a water-table aquifer, or a combined artesian and water-table aquifer. The aquifer may be heterogeneous and anisotropic and have irregular boundaries. The source term in the flow equation may include well discharge, constant recharge, leakage from confining beds in which the effects of storage are considered, and evapotranspiration as a linear function of depth to water. </p><p>The theoretical development includes presentation of the appropriate flow equations and derivation of the finite-difference approximations (written for a variable grid). The documentation emphasizes the numerical techniques that can be used for solving the simultaneous equations and describes the results of numerical experiments using these techniques. Of the three numerical techniques available in the model, the strongly implicit procedure, in general, requires less computer time and has fewer numerical difficulties than do the iterative alternating direction implicit procedure and line successive overrelaxation (which includes a two-dimensional correction procedure to accelerate convergence). </p><p>The documentation includes a flow chart, program listing, an example simulation, and sections on designing an aquifer model and requirements for data input. It illustrates how model results can be presented on the line printer and pen plotters with a program that utilizes the graphical display software available from the Geological Survey Computer Center Division. In addition the model includes options for reading input data from a disk and writing intermediate results on a disk.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/twri07C1","issn":"0565-596X","usgsCitation":"Trescott, P.C., Pinder, G.F., and Larson, S.P., 1976, Finite difference model for aquifer simulation in two dimensions with results of numerical experiments (Revision -1976): U.S. Geological Survey Techniques of Water-Resources Investigations 07-C1, vi, 116 p., https://doi.org/10.3133/twri07C1.","productDescription":"vi, 116 p.","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":384872,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/twri7-c1/html/pdf/TWRI_7-C1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":352,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri7-c1/","linkFileType":{"id":5,"text":"html"}}],"edition":"Revision -1976","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f46b3","contributors":{"authors":[{"text":"Trescott, Peter C.","contributorId":21533,"corporation":false,"usgs":true,"family":"Trescott","given":"Peter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":149685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pinder, George Francis","contributorId":99964,"corporation":false,"usgs":true,"family":"Pinder","given":"George","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":149687,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, S. P.","contributorId":34903,"corporation":false,"usgs":true,"family":"Larson","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":149686,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9082,"text":"ofr76824 - 1976 - Spectrographic and chemical analyses of geochemical samples from the McCarthy Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2024-03-06T19:50:52.45123","indexId":"ofr76824","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":"76-824","title":"Spectrographic and chemical analyses of geochemical samples from the McCarthy Quadrangle, Alaska","docAbstract":"<p>As an integral part of the Alaskan Mineral Resource Assessment Program, a geochemical reconnaissance survey was conducted in the McCarthy quadrangle during the summer of 1974. The investigation consisted of geochemical sampling, multielement chemical and spectrographic analyses, compilation of new and existing geochemical data, statistical evaluation of the total data set, and the generation of element distribution and abundance maps. The purpose of the survey was to define areas in the quadrangle that contain anomalous concentrations of metallic and nonmetallic elements. These studies are fundamental to a comprehensive evaluation of the mineral resource potential of the area and to assist in the discovery of additional economic mineral deposits.</p><p>The first-large scale geochemical sampling and analytical surveys were initiated in the McCarthy quadrangle in the early 1960's with the inception of the Wrangell Mountain project by the U.S. Geological Survey. Since that time, levels of activity in geochemical sampling in the quadrangle have fluctuated. Each year, many geochemical samples have been collected concomitantly with geologic mapping, and was culminated under the Alaskan Minerals Resource Assessment Program 1974.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76824","usgsCitation":"O’Leary, R.M., McDanal, S.K., Day, G.W., McDougal, C., and Robinson, K., 1976, Spectrographic and chemical analyses of geochemical samples from the McCarthy Quadrangle, Alaska: U.S. Geological Survey Open-File Report 76-824, 806 p., https://doi.org/10.3133/ofr76824.","productDescription":"806 p.","costCenters":[],"links":[{"id":426387,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0824/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142712,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0824/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"McCarthy Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -144.0,61.0 ], [ -144.0,62.0 ], [ -141.0,62.0 ], [ -141.0,61.0 ], [ -144.0,61.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e17","contributors":{"authors":[{"text":"O’Leary, Richard M.","contributorId":19936,"corporation":false,"usgs":true,"family":"O’Leary","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDanal, Steven K.","contributorId":294767,"corporation":false,"usgs":false,"family":"McDanal","given":"Steven","email":"","middleInitial":"K.","affiliations":[{"id":36625,"text":"Emeritus","active":true,"usgs":false}],"preferred":false,"id":159022,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Day, Gordon W.","contributorId":21520,"corporation":false,"usgs":true,"family":"Day","given":"Gordon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159020,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDougal, Christine","contributorId":62608,"corporation":false,"usgs":true,"family":"McDougal","given":"Christine","email":"","affiliations":[],"preferred":false,"id":159019,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":159021,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":9085,"text":"ofr76700G - 1976 - Station location map and audio-magnetotelluric and telluric data for Wendel-Amedee Known Geothermal Resource Area, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr76700G","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":"76-700","chapter":"G","title":"Station location map and audio-magnetotelluric and telluric data for Wendel-Amedee Known Geothermal Resource Area, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76700G","usgsCitation":"O’Donnell, J.E., Long, C.L., Senterfit, R.M., Brougham, G., Martinez, R., and Christopherson, K.R., 1976, Station location map and audio-magnetotelluric and telluric data for Wendel-Amedee Known Geothermal Resource Area, California: U.S. Geological Survey Open-File Report 76-700, 4 leaves :ill., map ;28 cm., https://doi.org/10.3133/ofr76700G.","productDescription":"4 leaves :ill., map ;28 cm.","costCenters":[],"links":[{"id":142727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699eb3","contributors":{"authors":[{"text":"O’Donnell, James E.","contributorId":96260,"corporation":false,"usgs":true,"family":"O’Donnell","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Senterfit, R. Michael","contributorId":10791,"corporation":false,"usgs":true,"family":"Senterfit","given":"R.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":159032,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brougham, G.W.","contributorId":8104,"corporation":false,"usgs":true,"family":"Brougham","given":"G.W.","affiliations":[],"preferred":false,"id":159031,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Martinez, R.J.","contributorId":19167,"corporation":false,"usgs":true,"family":"Martinez","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":159034,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Christopherson, K. R.","contributorId":11607,"corporation":false,"usgs":true,"family":"Christopherson","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":159033,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":8484,"text":"ofr76704 - 1976 - Low-flow characteristics of streams on the Kitsap Peninsula and selected adjacent islands, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr76704","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":"76-704","title":"Low-flow characteristics of streams on the Kitsap Peninsula and selected adjacent islands, Washington","docAbstract":"Low-flow-frequency data are tabulated for 90 streamflow sites on the Kitsap Peninsula and adjacent islands, Washington. Also listed are data for 56 additional sites which have insufficient measurements for frequency analysis but which have been observed having no flow at least once during the low-flow period. The streams drain relatively small basins; only three streams have drainage areas greater than 20.0 square miles, and only nine other streams have drainage areas greater than 10.0 square miles. Mean annual precipitation during the period 1931-60 ranged from about 25 inches near Hansville to about 70 inches near Tahuya. Low-flow-frequency curves plotted from records of streamflow at eight long-term gaging stations were used to determine data for low-flow durations of 7, 30, 60, 90, and 183 days. Regression techniques then were used to estimate low flows with frequencies up to 20 years for stations with less than 10 years of record and for miscellaneous sites where discharge measurements have been made. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76704","usgsCitation":"Cummans, J., 1976, Low-flow characteristics of streams on the Kitsap Peninsula and selected adjacent islands, Washington: U.S. Geological Survey Open-File Report 76-704, 43 leaves in various foliations :ill., maps (1 fold.) ;29 cm.; (39 p., 1 sheet, scale 1:250,000 - PGS), https://doi.org/10.3133/ofr76704.","productDescription":"43 leaves in various foliations :ill., maps (1 fold.) ;29 cm.; (39 p., 1 sheet, scale 1:250,000 - PGS)","costCenters":[],"links":[{"id":141642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0704/report-thumb.jpg"},{"id":36056,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0704/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36057,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0704/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36058,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648713","contributors":{"authors":[{"text":"Cummans, J. E.","contributorId":24767,"corporation":false,"usgs":true,"family":"Cummans","given":"J. E.","affiliations":[],"preferred":false,"id":157796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10403,"text":"ofr76673 - 1976 - Effects of drain wells on the ground-water quality of the western Snake Plain Aquifer, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr76673","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":"76-673","title":"Effects of drain wells on the ground-water quality of the western Snake Plain Aquifer, Idaho","docAbstract":"Approximately 3,100 drain wells injects irrigation waste water, urban runoff, septic-tank effluent, and industrial waste water into the Snake Plain aquifer in Minidoka, Gooding, Jerome, and Lincoln Counties, Idaho. About 29,000 acre-feet of irrigation waste water, 100 acre-feet of urban runoff, 400 acre-feet of septic-tank effluent, and 1,000 acre-feet of industrial waste water are injected annually. The quality of irrigation waste water is highly variable, depending upon its source, method and rate of application, amount of fertilizer added, and other factors. The quality of urban runoff water is generally much better than irrigation waste water. Septic-tank effluent is relatively high in nutrient concentrations. Chloride concentrations also are high, and bacterial concentrations are exceedingly high. The only industrial waste water sampled during this study had been used for cooling. No chemical changes were noted, but temperature was significantly increased. The data indicate that drain-well inflow does move appreciable distances through the aquifer and can be detected in downgradient wells. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76673","usgsCitation":"Moreland, J.A., Seitz, H.R., and LaSala, A.M., 1976, Effects of drain wells on the ground-water quality of the western Snake Plain Aquifer, Idaho: U.S. Geological Survey Open-File Report 76-673, 81 leaves :maps (3 fold.) ;28 cm.; (83 p., 1 sheet, scale 1:31,680 - PGS), https://doi.org/10.3133/ofr76673.","productDescription":"81 leaves :maps (3 fold.) ;28 cm.; (83 p., 1 sheet, scale 1:31,680 - PGS)","costCenters":[],"links":[{"id":143815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0673/report-thumb.jpg"},{"id":38249,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38250,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38251,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38252,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38253,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38254,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38255,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38256,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38257,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38258,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0673/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"31680","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615c2c","contributors":{"authors":[{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seitz, Harold R.","contributorId":61814,"corporation":false,"usgs":true,"family":"Seitz","given":"Harold","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161329,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"LaSala, Albert Mario","contributorId":74754,"corporation":false,"usgs":true,"family":"LaSala","given":"Albert","email":"","middleInitial":"Mario","affiliations":[],"preferred":false,"id":161330,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8218,"text":"ofr76619 - 1976 - Records of wells and water quality for the Garber-Wellington Aquifer, northern Oklahoma and southern Logan Counties, Oklahoma","interactions":[],"lastModifiedDate":"2018-08-08T13:53:34","indexId":"ofr76619","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":"76-619","title":"Records of wells and water quality for the Garber-Wellington Aquifer, northern Oklahoma and southern Logan Counties, Oklahoma","docAbstract":"<p>The U.S. Geological Survey has collected data on Oklahoma's ground-water resources since 1934. Most of these data were collected as part of specific ground-water studies conducted in cooperation with various Federal, State, and local agencies. </p><p>In 1972, at the request of the U.S. Bureau of Reclamation, the Geological Survey undertook a study of the Garber-Wellington aquifer in northern Oklahoma and southern Logan Counties. As a part of this project, records of about 120 wells were collected and 12 samples of ground water from the aquifer were analyzed in the laboratories of the Geological Survey; these records are included in this report. In addition, records of about 302 wells and analyses of 60 water samples were taken from a report by Wood and Burton (1966) and from the files of the Geological Survey. </p><p>Also included in this report are selected references for those desiring more information on the area's ground-water resources. </p><p>The stratigraphic nomenclature and age determinations used in this report are those accepted by the Oklahoma Geological Survey and do not necessarily agree with those of the U.S. Geological Survey. </p><p>Acknowledgment is extended to the many hundred of individuals who have provided the data compiled in this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76619","usgsCitation":"Carr, J.E., and Havens, J., 1976, Records of wells and water quality for the Garber-Wellington Aquifer, northern Oklahoma and southern Logan Counties, Oklahoma: U.S. Geological Survey Open-File Report 76-619, iii, 32 p., https://doi.org/10.3133/ofr76619.","productDescription":"iii, 32 p.","numberOfPages":"39","costCenters":[],"links":[{"id":356334,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0619/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0619/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","county":"Logan County, Oklahoma County","otherGeospatial":"Garber-Wellington Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.68905639648438,\n              35.45619556834375\n            ],\n            [\n              -97.13012695312499,\n              35.45619556834375\n            ],\n            [\n              -97.13012695312499,\n              36.01467140204727\n            ],\n            [\n              -97.68905639648438,\n              36.01467140204727\n            ],\n            [\n              -97.68905639648438,\n              35.45619556834375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf86","contributors":{"authors":[{"text":"Carr, Jerry E.","contributorId":47758,"corporation":false,"usgs":true,"family":"Carr","given":"Jerry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Havens, John S.","contributorId":13949,"corporation":false,"usgs":true,"family":"Havens","given":"John S.","affiliations":[],"preferred":false,"id":157361,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3811,"text":"cir715D - 1976 - Hydrologic analysis and river-quality data programs","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir715D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"715","chapter":"D","title":"Hydrologic analysis and river-quality data programs","docAbstract":"For nearly half a century the Willamette River in Oregon experienced severe dissolved-oxygen problems related to large loads of organically rich waste waters from industries and municipalities. Since the mid-1950 's dissolved oxygen quality has gradually improved owing to low-flow augmentation, the achievement of basinwide secondary treatment, and the use of other waste-management practices. As a result, summer dissolved-oxygen levels have increased, salmon runs have returned, and the overall effort is widely regarded as a singular water-quality success. To document the improved dissolved-oxygen regimen, the U.S. Geological Survey conducted intensive studies of the Willamette during the summer low-flow seasons of 1973 and 1974. During each summer the mean daily dissolved-oxygen levels were found to be higher than 5 milligrams per liter throughout the river. Because of the basinwide secondary treatment, carbonaceous deoxygenation rates were low. In addition, almost half of the biochemical oxygen demand entering the Willamette was from diffuse (nonpoint) sources rather than outfalls. These results indicated that point-source biochemical oxygen demand was no longer the primary cause of dissolved-oxygen depletion. Instead, the major causes of deoxygenation were nitrification in a shallow ' surface active ' reach below Salem and an anomalous oxygen demand (believed to be primarily of benthal origin) in Portland Harbor. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/cir715D","usgsCitation":"Hines, W.G., Rickert, D.A., and McKenzie, S.W., 1976, Hydrologic analysis and river-quality data programs: U.S. Geological Survey Circular 715, v, p D1-D20,  ill., map ;28 cm. , https://doi.org/10.3133/cir715D.","productDescription":"v, p D1-D20,  ill., map ;28 cm. ","costCenters":[],"links":[{"id":123895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1976/0715d/report-thumb.jpg"},{"id":30881,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1976/0715d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611bfa","contributors":{"authors":[{"text":"Hines, Walter G.","contributorId":100360,"corporation":false,"usgs":true,"family":"Hines","given":"Walter","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":147649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rickert, David A.","contributorId":80247,"corporation":false,"usgs":true,"family":"Rickert","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, Stuart W.","contributorId":27841,"corporation":false,"usgs":true,"family":"McKenzie","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147647,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}