{"pageNumber":"6866","pageRowStart":"171625","pageSize":"25","recordCount":184828,"records":[{"id":56123,"text":"ofr5867 - 1958 - Preliminary report on ground water in the Bonanza Lake area, Power and Blaine counties, Idaho","interactions":[],"lastModifiedDate":"2013-11-19T11:07:42","indexId":"ofr5867","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-67","title":"Preliminary report on ground water in the Bonanza Lake area, Power and Blaine counties, Idaho","docAbstract":"The investigation in the Bonanza Lake area of northwestern Power and southeastern Blaine Counties was made to determine the direction of ground-water movement and to ascertain the relation of the regional ground-water body to the Snake River. The surface of the area is nearly flat to gently rolling, and slopes to the west. Lake Channel, an abandoned channel of the Snake River, and a few volcanic cones modify the gentle relief. The climate is semiarid, the annual precipitation ranging from 10 to 15 inches. Most of the area is uncultivated and covered with sagebrush, the predominate vegetation. A significant amount of the area is dry farmed; about 500 to 650 acres is irrigated with ground water pumped from wells or from ponds in Lake Channel. The Bonanza area and vicinity are underlin by windblown deposits of Recent age (not shown on the geologic map); alluvium with admixed windblown material and black basalt, both also of Recent age; undifferentiated Snake River basalt, of Pliocene to Recent age; the American Falls lake beds and Cedar Butte basalt, or Pleistocene age; of the Raft Lake beds and Massacre volcanic and associated rocks, of Pliocene(?) age. The alluvium contains ground water at shallow depth, but because of its limited areal extent it is not an important aquifer, The Snake River basalt is the most important aquifer in the area and yields water to irrigation, domestic, and stock wells. Several springs discharge from the basalt into Lake Walcott. The Cedar Butte basalt is a major aquifer supplying water to a number of stock and domestic wells and to Bonanza Lake. Ground water moves southward and southwestward through the area from the Aberseen-Springfield tract on the northeast and possibly from the downstream end of American Falls Reservoir. Part of the ground water is discharged to the Snake River and Lake Walcott and part moves westward out of the area of the main ground-water body. The amount of ground water can not be determined from the data bow available. Data from dam-site borings and wells suggest the possibility that a part of the ground water in the area may be perched above the regional water table.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5867","collaboration":"Prepared for the U.S. Bureau of Reclamation","usgsCitation":"Meisler, H., 1958, Preliminary report on ground water in the Bonanza Lake area, Power and Blaine counties, Idaho: U.S. Geological Survey Open-File Report 58-67, Report: ii, 32 p.; 1 Plate: 48.05 x 28.87 inches, https://doi.org/10.3133/ofr5867.","productDescription":"Report: ii, 32 p.; 1 Plate: 48.05 x 28.87 inches","numberOfPages":"36","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":180838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1958/0067/report-thumb.jpg"},{"id":275858,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0067/report.pdf"},{"id":275859,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0067/plate-1.pdf"}],"country":"United States","state":"Idaho","city":"Blaine County;Power County","otherGeospatial":"Bonanza Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.9967,41.9948 ], [ -114.9967,43.9934 ], [ -111.9136,43.9934 ], [ -111.9136,41.9948 ], [ -114.9967,41.9948 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66caa0","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":254793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":47210,"text":"ofr582 - 1958 - Geologic map of the Dodgeville quadrangle, Wisconsin","interactions":[{"subject":{"id":47210,"text":"ofr582 - 1958 - Geologic map of the Dodgeville quadrangle, Wisconsin","indexId":"ofr582","publicationYear":"1958","noYear":false,"title":"Geologic map of the Dodgeville quadrangle, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":33636,"text":"b1123D - 1963 - Geology of the Dodgeville and Mineral Point quadrangles, Wisconsin","indexId":"b1123D","publicationYear":"1963","noYear":false,"chapter":"D","title":"Geology of the Dodgeville and Mineral Point quadrangles, Wisconsin"},"id":1}],"supersededBy":{"id":33636,"text":"b1123D - 1963 - Geology of the Dodgeville and Mineral Point quadrangles, Wisconsin","indexId":"b1123D","publicationYear":"1963","noYear":false,"title":"Geology of the Dodgeville and Mineral Point quadrangles, Wisconsin"},"lastModifiedDate":"2020-06-25T14:20:55.515253","indexId":"ofr582","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-2","title":"Geologic map of the Dodgeville quadrangle, Wisconsin","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr582","usgsCitation":"Allingham, J.W., 1958, Geologic map of the Dodgeville quadrangle, Wisconsin: U.S. Geological Survey Open-File Report 58-2, Report: 2 p.; 1 Plate: 27.72 x 33.50 inches, https://doi.org/10.3133/ofr582.","productDescription":"Report: 2 p.; 1 Plate: 27.72 x 33.50 inches","costCenters":[],"links":[{"id":375902,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1958/0002/report-thumb.jpg"},{"id":375901,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0002/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsn","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.25,\n              42.875\n            ],\n            [\n              -90.125,\n              42.875\n            ],\n            [\n              -90.125,\n              43.000\n            ],\n            [\n              -90.25,\n              43.000\n            ],\n            [\n              -90.25,\n              42.875\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6997b6","contributors":{"authors":[{"text":"Allingham, John Wing","contributorId":65466,"corporation":false,"usgs":true,"family":"Allingham","given":"John","email":"","middleInitial":"Wing","affiliations":[],"preferred":false,"id":234835,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13527,"text":"ofr5835 - 1958 - Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota","interactions":[{"subject":{"id":13527,"text":"ofr5835 - 1958 - Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota","indexId":"ofr5835","publicationYear":"1958","noYear":false,"title":"Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":33830,"text":"b1063I - 1963 - Geology of the Fanny Peak quadrangle, Wyoming-South Dakota","indexId":"b1063I","publicationYear":"1963","noYear":false,"chapter":"I","title":"Geology of the Fanny Peak quadrangle, Wyoming-South Dakota"},"id":1}],"supersededBy":{"id":33830,"text":"b1063I - 1963 - Geology of the Fanny Peak quadrangle, Wyoming-South Dakota","indexId":"b1063I","publicationYear":"1963","noYear":false,"title":"Geology of the Fanny Peak quadrangle, Wyoming-South Dakota"},"lastModifiedDate":"2025-09-30T15:43:33.691744","indexId":"ofr5835","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-35","title":"Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota","docAbstract":"<p>The Fanny Peak quadrangle is located on the west flank of the Black Hills. The exposed strata total over 4000 feet in thickness and range in age from Mississippian to late Cretaceous. Local surficial Cenozoic deposits are common.</p><p>The upper 200 to 300 feet of the Minnelusa formation is a breccia whose origin is attributed to removal of anhydrite by ground water and consequent collapse of the overlying strata. Crude bedding indicates uniform collapse; breccia pipes result from more intensive brecciation. The anhydrite probably occurred as lenses at different levels. 3recciation started after the Black Hills were uplifted and the Minnelusa was breached. Calcium sulphate in spring waters attests to present removal of anhydrite.</p><p>The Minnekahta limestone exhibits secondary structures attributed to gravity sliding. Cascade folds and slip sheets with displacements of not more than 30 feet developed in exposed beds whose dip is more than 30 degrees. Numerous intraformational folds and faults formed when beds within the limestone slid over each other. Shortening of the Ninnekahta limestone of about 200 feet per mile is estimated.</p><p>Four monoclines and associated structural terraces are interpreted as reflecting six fault blocks at depth with minimum displacement of 6000 feet. The intersecting Fanny Peak and Black Hills monoclines represent lines of major deformation. The Fanny Peak monocline passes into a near-vertical normal fault with a throw of approximately 800 feet two miles north of the quadrangle.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5835","usgsCitation":"Epstein, J., 1958, Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota: U.S. Geological Survey Open-File Report 58-35, Report: ix, 90 p.; 6 Plates: 38.14 x 30.75 inches or smaller, https://doi.org/10.3133/ofr5835.","productDescription":"Report: ix, 90 p.; 6 Plates: 38.14 x 30.75 inches or smaller","costCenters":[],"links":[{"id":145434,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1958/0035/report-thumb.jpg"},{"id":496101,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0035/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496100,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0035/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496099,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0035/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496098,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0035/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496097,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0035/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496096,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496095,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","country":"United States","state":"South Dakota, Wyoming","otherGeospatial":"Fanny Peak quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -96.17043233426008,\n              46.02219860279615\n            ],\n            [\n              -104.27866231105207,\n              46.106454434710486\n            ],\n            [\n              -104.23582820786766,\n              45.214489532361\n            ],\n            [\n              -111.27535473898402,\n              45.13085307785758\n            ],\n            [\n              -111.25098841134513,\n              40.80068970960221\n            ],\n            [\n              -103.86339300460446,\n              40.84538515481847\n            ],\n            [\n              -103.82331486730374,\n              42.75085593602702\n            ],\n            [\n              -96.14642029605193,\n              42.38559774737402\n            ],\n            [\n              -96.17043233426008,\n              46.02219860279615\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836cd","contributors":{"authors":[{"text":"Epstein, Jack Burton","contributorId":64625,"corporation":false,"usgs":true,"family":"Epstein","given":"Jack Burton","affiliations":[],"preferred":false,"id":167949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39200,"text":"pp260U - 1958 - Bikini and nearby atolls, Marshall Islands; geothermal measurements on Eniwetok and Bikini Atolls","interactions":[],"lastModifiedDate":"2012-02-02T00:09:55","indexId":"pp260U","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"260","chapter":"U","title":"Bikini and nearby atolls, Marshall Islands; geothermal measurements on Eniwetok and Bikini Atolls","language":"ENGLISH","doi":"10.3133/pp260U","usgsCitation":"Swartz, J., 1958, Bikini and nearby atolls, Marshall Islands; geothermal measurements on Eniwetok and Bikini Atolls: U.S. Geological Survey Professional Paper 260, p. 711-741, https://doi.org/10.3133/pp260U.","productDescription":"p. 711-741","costCenters":[],"links":[{"id":122148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0260u/report-thumb.jpg"},{"id":66845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0260u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db62621c","contributors":{"authors":[{"text":"Swartz, J.H.","contributorId":101721,"corporation":false,"usgs":true,"family":"Swartz","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":221126,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14561,"text":"ofr5856 - 1958 - Dissipation of the temperature effect of drilling a well in Arctic Alaska","interactions":[{"subject":{"id":14561,"text":"ofr5856 - 1958 - Dissipation of the temperature effect of drilling a well in Arctic Alaska","indexId":"ofr5856","publicationYear":"1958","noYear":false,"title":"Dissipation of the temperature effect of drilling a well in Arctic Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":47387,"text":"b1083A - 1959 - Periodic heat flow in a stratified medium with application to permafrost problems","indexId":"b1083A","publicationYear":"1959","noYear":false,"chapter":"A","title":"Periodic heat flow in a stratified medium with application to permafrost problems"},"id":1}],"supersededBy":{"id":47387,"text":"b1083A - 1959 - Periodic heat flow in a stratified medium with application to permafrost problems","indexId":"b1083A","publicationYear":"1959","noYear":false,"title":"Periodic heat flow in a stratified medium with application to permafrost problems"},"lastModifiedDate":"2012-02-02T00:06:47","indexId":"ofr5856","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-56","title":"Dissipation of the temperature effect of drilling a well in Arctic Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr5856","usgsCitation":"Lachenbruch, A.H., 1958, Dissipation of the temperature effect of drilling a well in Arctic Alaska: U.S. Geological Survey Open-File Report 58-56, 62 p. ill. ;27 cm., https://doi.org/10.3133/ofr5856.","productDescription":"62 p. ill. ;27 cm.","costCenters":[],"links":[{"id":146273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a2a0","contributors":{"authors":[{"text":"Lachenbruch, Arthur H.","contributorId":27850,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"Arthur","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":169651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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