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,{"id":52296,"text":"ofr62152 - 1962 - Ground-water inventory for 1961, Edwards Air Force Base, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-152","title":"Ground-water inventory for 1961, Edwards Air Force Base, California","language":"ENGLISH","doi":"10.3133/ofr62152","usgsCitation":"Weir, J.E., 1962, Ground-water inventory for 1961, Edwards Air Force Base, California: U.S. Geological Survey Open-File Report 62-152, 54 p., https://doi.org/10.3133/ofr62152.","productDescription":"54 p.","costCenters":[],"links":[{"id":179501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0152/report-thumb.jpg"},{"id":86787,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0152/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86788,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0152/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668caa","contributors":{"authors":[{"text":"Weir, J. E. Jr.","contributorId":102476,"corporation":false,"usgs":true,"family":"Weir","given":"J.","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":245100,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52298,"text":"ofr62154 - 1962 - Surface waters of Elk Creek basin in southwestern Oklahoma","interactions":[{"subject":{"id":52298,"text":"ofr62154 - 1962 - Surface waters of Elk Creek basin in southwestern Oklahoma","indexId":"ofr62154","publicationYear":"1962","noYear":false,"title":"Surface waters of Elk Creek basin in southwestern Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":52374,"text":"ofr63138 - 1963 - Surface waters of Elk Creek basin in southwestern Oklahoma","indexId":"ofr63138","publicationYear":"1963","noYear":false,"title":"Surface waters of Elk Creek basin in southwestern Oklahoma"},"id":1}],"supersededBy":{"id":52374,"text":"ofr63138 - 1963 - Surface waters of Elk Creek basin in southwestern Oklahoma","indexId":"ofr63138","publicationYear":"1963","noYear":false,"title":"Surface waters of Elk Creek basin in southwestern Oklahoma"},"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-154","title":"Surface waters of Elk Creek basin in southwestern Oklahoma","language":"ENGLISH","doi":"10.3133/ofr62154","usgsCitation":"Westfall, A., 1962, Surface waters of Elk Creek basin in southwestern Oklahoma: U.S. Geological Survey Open-File Report 62-154, 18 p., https://doi.org/10.3133/ofr62154.","productDescription":"18 p.","costCenters":[],"links":[{"id":179582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691230","contributors":{"authors":[{"text":"Westfall, A.O.","contributorId":85225,"corporation":false,"usgs":true,"family":"Westfall","given":"A.O.","email":"","affiliations":[],"preferred":false,"id":245102,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52299,"text":"ofr62155 - 1962 - Surface waters of Otter Creek basin in southwestern Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-155","title":"Surface waters of Otter Creek basin in southwestern Oklahoma","docAbstract":"Otter Creek had an average annual discharge at the gaging station of 22 cfs (cubic feet per second) or 15,900 acre-feet per year from a drainage area of 132 square miles during a selected 19-year base period, water-years 1938-56.\r\nThe maximum yearly runoff was 43,410 acre-feet for water-year 1957. The maximum monthly runoff was 24,090 acre-feet in May 1957.\r\n\r\nOtter Creek has extended periods of no flow except for about the last 5 miles near the mouth. The most severe droughts occurred in 1938-41 and 1952-56. Periods of no flow have extended as long as 363 days and have exceeded 300 days many times.\r\n\r\nThe usable storage required to provide a regulated discharge equal to about half the average discharge at the gaging station at Snyder Lake during the most deficient period was determined to be 18,000 acre-feet.\r\n\r\nMiscellaneous measurements made at selected sites show that there is no sustained base flow in any of the tributaries and none in the mainstem except for about the last 5 miles near the mouth. A group of measurements made in September 1961, when there was ground-water outflow in all of the main tributaries except Horse Creek, shows that most of the ground-water outflow in the upper part of the basin comes from the tributaries that originate in the Wichita Mountains. Considerable base runoff occurs in the lower part of the basin from large alluvial and terrace deposits.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr62155","usgsCitation":"Westfall, A., 1962, Surface waters of Otter Creek basin in southwestern Oklahoma: U.S. Geological Survey Open-File Report 62-155, 37 p., https://doi.org/10.3133/ofr62155.","productDescription":"37 p.","costCenters":[],"links":[{"id":179583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69795e","contributors":{"authors":[{"text":"Westfall, A.O.","contributorId":85225,"corporation":false,"usgs":true,"family":"Westfall","given":"A.O.","email":"","affiliations":[],"preferred":false,"id":245103,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52229,"text":"ofr6229 - 1962 - Ground-water investigations of the Project Gnome area, Eddy and Lea Counties, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr6229","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-29","title":"Ground-water investigations of the Project Gnome area, Eddy and Lea Counties, New Mexico","docAbstract":"The U.S. Atomic Energy Commission, through the Office of Test Operations, Albuquerque Operations Office, plans to detonate a nuclear device in a massive salt bed 1,200 feet beneath the land surface. The project, known as Project Gnome, is an element of the Plowshare program--a study of peacetime applications of nuclear fission. The location of the proposed underground shot is in a sparsely-populated area in southeastern Eddy County, N. Mex., east of the Pecos River and about 25 miles southeast of the city of Carlsbad. The area is arid to Semiarid and ground water is a vital factor in the economic utilization of the land, which is primarily used for stock raising. An investigation of the Project Gnome site and surrounding area for the purposes of evaluating the ground-water resources and the possible effect upon them from the detonation of the nuclear shot was desired by the Commission. This report describes work done by the U.S. Geological Survey on behalf of the Commission and presents results of the investigation of the ground-water resources and geology of the area. \r\n\r\nThe most intensive investigations were made within a 15-mile radius of the site of Project Gnome and mainly on the east side of the Pecos River. The total area of study of over 1,200 square miles includes parts of Eddy and Lea Counties, N. Mex. \r\n\r\nThe Project Gnome site is in the sedimentary Delaware Basin. It is underlain by about 18,000 feet of sedimentary rocks ranging in age from Ordovician to Recent. Upper Permian evaporitic rocks, which contain the principal source of potash available in the United States, are worked in nearby mines. The potash minerals are found in a massive salt bed about 1,400 feet thick in the Salado Formation of Permian age. The land surface of the area is covered mostly by a wind-blown sand and caliche; however, rocks of the Rustler Formation of Permian age and younger rocks of Permian, Triassic, Pleistocene(?) and Recent age crop out at several localities. Solution by ground water of salt at the top of the Salado Formation and of anhydrite within the Rustler Formation has removed thick sections of these rocks. A subsequent lowering of the land surface and differential collapse of the Rustler has formed many sinkholes and has created a karst topography over much of the western part of the area. \r\n\r\nGround water is obtained from rocks of Permian, Triassic, Tertiary, and Quaternary age in the general region. However, the only aquifer at the Gnome site is the Culebra Dolomite Member of the Rustler Formation of Permian age. The aquifer is about 500 feet beneath the surface at the site and is about 30 feet thick. An aquifer, immediately above the top of the salt, contains a brine solution in Nash Draw, a few miles west of the Gnome site. This aquifer discharges into the Pecos River and is a major source of contamination of the river water. No potable water is known to be present in the area below the top of the salt of the Salado Formation. \r\n\r\nThe ground water in the area is generally under artesian pressure. The general direction of ground-water movement is toward the Pecos River both east and west of the river. At the Gnome site the artesian head of the water in the Culebra Dolomite Member is about 7.5 feet. The water moves westward through the aquifer at a rate of about ? foot per day. The most widespread utilization of ground water east of the river is for stock use. Irrigation usage west of the Pecos River accounts for the largest withdrawal of water. Wells range in depth from a few tens of feet to nearly 800 feet. Water levels range from a few feet to about 500 feet below the surface. A test well at the Gnome site drawing water from the Culebra Dolomite Member was pumped at a rate of 100 gpm (gallons per minute); however, most wells east of the river yield only a few gpm. Irrigation wells west of the river yield as much as 3,500 gpm. \r\n\r\nMost of the water in the area is highly mineralized and is suitable only for use by livest","language":"ENGLISH","doi":"10.3133/ofr6229","usgsCitation":"Cooper, J., 1962, Ground-water investigations of the Project Gnome area, Eddy and Lea Counties, New Mexico: U.S. Geological Survey Open-File Report 62-29, 67 p., https://doi.org/10.3133/ofr6229.","productDescription":"67 p.","costCenters":[],"links":[{"id":177171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0029/report-thumb.jpg"},{"id":86746,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0029/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86747,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0029/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86748,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0029/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86749,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0029/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86750,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0029/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698629","contributors":{"authors":[{"text":"Cooper, J.B.","contributorId":92316,"corporation":false,"usgs":true,"family":"Cooper","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":245000,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52237,"text":"ofr6241 - 1962 - Interim geological investigations in the U12e.04 tunnel, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:46","indexId":"ofr6241","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-41","title":"Interim geological investigations in the U12e.04 tunnel, Nevada Test Site, Nye County, Nevada","docAbstract":"The Ul2e.04 tunnel is a part of the Ul2e tunnel system, which has been driven southwestward beneath Rainier Mesa in the northern part of the Nevada Test Site. The Ul2e.04 tunnel was driven about S. 15? W. in zeolitic tuff of subunits E and F of Tunnel Bed W near the top of the lower member of the Indian Trail Formation (upper Miocene or lower Pliocene). Dolomite of Paleozoic age lies about 915 feet below the end of the tunnel; vertical cover over the end of the tunnel to the surface of Rainier Mesa is about 1,390 feet. The tuffs in the tunnel strike almost north-south and dip to the west. There are several normal northwest-trending faults with vertical to steep dips and small displacements. The predominant joint set strikes northwest and dips mostly vertically or steeply to the northeast. \r\n\r\nPetrographically and chemically the tuffs in the U12e.04 tunnel are similar to other tuffs of the Indian Trail Formation from the Nevada Test Site, The tuffs in the tunnel have an average porosity of 38.6 percent, dry bulk density of 1.46 g/cc (grams per cubic centimeter), grain density of 2.38 g/cc, water content of 20.7 percent by weight. \r\n\r\nShore hardness of 25.1, and unconfined compressive strength of 4,400 psi (pounds per square inch). Separately, the tuffs from the chamber at the end of the tunnel have an average porosity of 36.8 percent, dry bulk density of 1.51 g/cc, grain density of 2.38 g/cc, water content of 20.0 percent by weight, Shore hardness of 27.2 and unconfined compressive strength of 4,500 psi. \r\n\r\nAn NX-size cored hole was drilled from the surface of Rainier Mesa into the Ul2e.04 chamber.","language":"ENGLISH","doi":"10.3133/ofr6241","usgsCitation":"Emerick, W., Dickey, D., and McKeown, F.A., 1962, Interim geological investigations in the U12e.04 tunnel, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 62-41, 27 p., https://doi.org/10.3133/ofr6241.","productDescription":"27 p.","costCenters":[],"links":[{"id":175097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0041/report-thumb.jpg"},{"id":86759,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86760,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0041/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86761,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d482","contributors":{"authors":[{"text":"Emerick, W.L.","contributorId":64668,"corporation":false,"usgs":true,"family":"Emerick","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":245018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickey, D.D.","contributorId":15612,"corporation":false,"usgs":true,"family":"Dickey","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":245017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":245019,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52278,"text":"ofr62118 - 1962 - Progress report on streamflow investigations in Suffolk County, Long Island, New York, 1953-57","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-118","title":"Progress report on streamflow investigations in Suffolk County, Long Island, New York, 1953-57","language":"ENGLISH","doi":"10.3133/ofr62118","usgsCitation":"Sawyer, R., 1962, Progress report on streamflow investigations in Suffolk County, Long Island, New York, 1953-57: U.S. Geological Survey Open-File Report 62-118, 159 p., https://doi.org/10.3133/ofr62118.","productDescription":"159 p.","costCenters":[],"links":[{"id":178824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de92","contributors":{"authors":[{"text":"Sawyer, R.M.","contributorId":55074,"corporation":false,"usgs":true,"family":"Sawyer","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":245073,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52279,"text":"ofr62121 - 1962 - Portrayal of drainage and vegetation on topographic maps","interactions":[],"lastModifiedDate":"2025-06-05T17:18:03.062958","indexId":"ofr62121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-121","title":"Portrayal of drainage and vegetation on topographic maps","docAbstract":"<p>Accurate measurements of drainage networks are necessary for studies in many scientific disciplines, especially hydrology. To this end, topographic maps must show accurate classification as well as a consistent pattern of the stream network.</p><p>A recent study in Georgia has developed two photo-interpretive keys which permit accurate drainage classification during the normal stereo-compilation procedures in map-making. The study was made in the Tired Creek basin in the Coastal Plain, and in the Yellow River basin in the Piedmont Province.</p><p>In the Tired Creek basin, the perennial stream channels were associated with blackgum swamps which showed as a characteristic pattern on the aerial photographs of the area. Although the areas were classed as evergreen forest on specially-compiled vegetation maps without field checking, the classification was relatively consistent, indicating that the perennial channels could be identified accurately within the basin.</p><p>In the Yellow River basin origins of perennial flow were found in valleys having concave-upward profiles. Valleys with convex-upward profiles remained ephemeral up to their juncture with a larger stream. Field checks indicated better than 80 percent accuracy in delineating these points of origin of perennial flow through stereoscopic viewing of the aerial photographs of the area. Vegetative difference above and below the origins of perennial flow were to subtle to be readily discerned on the photographs. Errors in classifying vegetation on special maps were attributed mainly to inexperience and to faulty criteria for for classification.</p><p>Proposals are presented to improve portrayal of both drainage and vegetation on topographic maps. The proposed drainage criteria suggest portrayal of all perennial streams as well as ephemeral drainage below the first branching. The proposed vegetation criteria suggest classification of forest and shrubs, with further sub-division of distinctive patterns of vegetation easily recognized on the aerial photographs.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr62121","usgsCitation":"Schneider, W., and Goodlett, J.C., 1962, Portrayal of drainage and vegetation on topographic maps: U.S. Geological Survey Open-File Report 62-121, 63 p., https://doi.org/10.3133/ofr62121.","productDescription":"63 p.","costCenters":[],"links":[{"id":489702,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0121/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178825,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0121/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696f11","contributors":{"authors":[{"text":"Schneider, W.J.","contributorId":32963,"corporation":false,"usgs":true,"family":"Schneider","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":245074,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodlett, J. C.","contributorId":98771,"corporation":false,"usgs":true,"family":"Goodlett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":245075,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52230,"text":"ofr6230 - 1962 - Road log from Carlsbad, New Mexico, to Project Gnome site","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr6230","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-30","title":"Road log from Carlsbad, New Mexico, to Project Gnome site","language":"ENGLISH","doi":"10.3133/ofr6230","usgsCitation":"Cooper, J., 1962, Road log from Carlsbad, New Mexico, to Project Gnome site: U.S. Geological Survey Open-File Report 62-30, 10 p., https://doi.org/10.3133/ofr6230.","productDescription":"10 p.","costCenters":[],"links":[{"id":100140,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0030/report.pdf","size":"864","linkFileType":{"id":1,"text":"pdf"}},{"id":177172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0030/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a10e4b07f02db5ff2ae","contributors":{"authors":[{"text":"Cooper, J.B.","contributorId":92316,"corporation":false,"usgs":true,"family":"Cooper","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":245001,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52231,"text":"ofr6231 - 1962 - Test holes drilled in support of ground-water investigations, Project Gnome, Eddy County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr6231","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-31","title":"Test holes drilled in support of ground-water investigations, Project Gnome, Eddy County, New Mexico","docAbstract":"Project Gnome is a proposed underground nuclear shot to be detonated within a massive salt bed in Eddy County, N. Mex. Potable and neat potable ground water is present in rocks above the salt and is being studied in relation to this nuclear event. This report presents details of two test holes which were drilled to determine ground-water conditions in the near vicinity of the shot point.\r\n\r\nA well-defined aquifer is present at the site of USGS test hole 1, about 1,000 feet south of the access shaft to the underground shot point. Water with 75 feet of artesian pressure head is contained in the Culebra dolomite member of the Rustler formation. The dolomite aquifer is 32 feet thick and its top lies at a depth of 517 feet below land surface. The aquifer yielded 100 gpm (gallons per minute) with a drawdown of 40 feet during a pumping period of 24 hours. Water was not found in rocks above or below the Culebra dolomite.\r\n\r\nAt the site of USGS test hole 2, about 2 miles southwest of the access shaft no distinctive aquifer exists. About one-half gpm was yielded to the well from the rocks between the Culebra dolomite and the top of the salt. Water could not be detected in the Culebra dolomite or overlying rocks.\r\n\r\nThe report contains drawdown and recovery curves of yield tests, drilling-time charts, and electric logs. The data are given in tables; they include summaries of hole construction, sample description logs, water measurements, drilling-time logs, and water analyses.","language":"ENGLISH","doi":"10.3133/ofr6231","usgsCitation":"Cooper, J., 1962, Test holes drilled in support of ground-water investigations, Project Gnome, Eddy County, New Mexico: U.S. Geological Survey Open-File Report 62-31, 116 p., https://doi.org/10.3133/ofr6231.","productDescription":"116 p.","costCenters":[],"links":[{"id":177173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0031/report-thumb.jpg"},{"id":86752,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0031/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86753,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0031/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86754,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0031/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86755,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0031/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86756,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0031/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86757,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0031/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86758,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684d41","contributors":{"authors":[{"text":"Cooper, J.B.","contributorId":92316,"corporation":false,"usgs":true,"family":"Cooper","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":245002,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47104,"text":"ofr6214 - 1962 - Geologic map of the Chandalar quadrangle, Alaska","interactions":[{"subject":{"id":47104,"text":"ofr6214 - 1962 - Geologic map of the Chandalar quadrangle, Alaska","indexId":"ofr6214","publicationYear":"1962","noYear":false,"title":"Geologic map of the Chandalar quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":64817,"text":"i375 - 1964 - Geologic map and section of the Chandalar quadrangle, Alaska","indexId":"i375","publicationYear":"1964","noYear":false,"title":"Geologic map and section of the Chandalar quadrangle, Alaska"},"id":1}],"supersededBy":{"id":64817,"text":"i375 - 1964 - Geologic map and section of the Chandalar quadrangle, Alaska","indexId":"i375","publicationYear":"1964","noYear":false,"title":"Geologic map and section of the Chandalar quadrangle, Alaska"},"lastModifiedDate":"2012-02-02T00:10:47","indexId":"ofr6214","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-14","title":"Geologic map of the Chandalar quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/ofr6214","usgsCitation":"Brosge, W.P., and Reiser, H.N., 1962, Geologic map of the Chandalar quadrangle, Alaska: U.S. Geological Survey Open-File Report 62-14, 1 map, https://doi.org/10.3133/ofr6214.","productDescription":"1 map","costCenters":[],"links":[{"id":111582,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10673","linkFileType":{"id":5,"text":"html"}},{"id":172052,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69cf88","contributors":{"authors":[{"text":"Brosge, William Peters","contributorId":40191,"corporation":false,"usgs":true,"family":"Brosge","given":"William","email":"","middleInitial":"Peters","affiliations":[],"preferred":false,"id":234634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiser, H. N.","contributorId":13199,"corporation":false,"usgs":true,"family":"Reiser","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":234633,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35472,"text":"b1122F - 1962 - Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources","interactions":[],"lastModifiedDate":"2021-12-23T19:56:45.980641","indexId":"b1122F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1122","chapter":"F","title":"Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources","docAbstract":"The Haldeman and Wrigley 7th-minute quadrangles are near the western edge of the eastern Kentucky coal field and cover an area of approximately 117 square miles in parts of Carter, Rowan, Elliott, and Morgan Counties, Ky. The rocks exposed in the two quadrangles are of Early and Late Mississippian and Early and Middle Pennsylvanian age. The Mississippian rocks are composed of the thick Brodhead formation, which consists of siltstone and shale, and eleven thin marine limestone and shale formations, having an aggregate thickness of about 150 feet. The Lee and Breathitt formations, of Pennsylvanian age, consist of sandstone, siltstone, and shale; they also contain thin beds of coal and several beds of underclay, including the economically important Olive Hill clay bed of Crider, 1913. Pennsylvanian rocks include beds of both continental and marine origin. The eleven thin Mississippian formations and the upper-most part of the thick Brodhead formation are truncated by a prominent unconformity on which rocks of Pennsylvanian age rest. The rocks occupy a region of gentle dips between the Cincinnati arch and the Appalachian Mountains.\r\n\r\nRefractory clay deposits are in the Olive Hill clay bed, which occurs in the \r\nlower part of the Lee formation. The Olive Hill clay bed is discontinuous and \r\nconsists of a series of irregularly shaped lenses. The bed is approximately \r\ntwo-thirds semifiint clay and one-third flint clay, and it contains minor amounts of plastic clay. Some of the flint clay is nearly pure kaolinite, but the semi flint and plastic clay consists of mixtures of kaolinite, illite, and mixed-layer clay minerals. The structure of the kaolinite ranges from highly crystalline to very poorly crystalline 'fireclay' type. The degree of crystallinity of the kaolinite and the hardness of the clay vary inversely with the amount of illite and mixed-layer clay minerals present. The nearly pure kaolinite is believed to have formed by the removal of alkalies and some silica fram mixtures of kaolinite, illite, and mixed-layer clays by leaching in swamps to the deposition of the beds overlying the clay. The refractory properties of the clay vary directly with the purity of the kaolinite, and refractoriness decreases as the proportions of illite and mixed-layer clays increase. Certain nonclay minerals, chiefly siderite, pyrite, and iron oxide-bearing minerals, also act as fiuxes, reducing the refractory properties of the clay. The entire resources of clay in the Olive Hill clay bed are roughly and tentatively estimated to include 105,000,000 tons in the Haldeman quadrangle and 175,000,000 tons in the Wrigley quadrangle. Much of this clay is of poor quality and the amount that is better than the minimum requirements for use in refractories is probably about 30,000,000 tons. Only a fraction of this tonnage is suitable for superheat-duty products.\r\n\r\nLimestone is the only nonmetallic mineral resource other than refractory clay \r\nthat has been developed in the two quadrangles, but 1arge amounts of shale \r\nsuitable for use in making lightweight aggregate and structural clay products \r\nmay also be present. Most of the limestone, which is quarried. in both quadrangles, is used for road-metal, concrete aggregate, and agriculture stone, but some of the limestone is of the quality that would be suitable for other uses. Virtually all the Mississippian Beech Creek limestone of Malott, 1919 which is as much as 18 feet thick, consists of high-calcium limestone. Shale beds that appear most favoralble for making lightweight aggregate are in the shale facies of the Lee formation of Pennsylvanian age. Shale that is probably suitable for structural clay products is present in the shale flacles of the Lee formation and in the Muldraugh formation of Mississippian age.\r\n\r\nSeveral dry holes have been drilled in search for oil and gas within the area \r\nof the two quadrangles. Though no commercial production was ever attained, one well furnished a supply of gas f","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology (1960)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1122F","usgsCitation":"Patterson, S.H., Hosterman, J.W., and Huddle, J.W., 1962, Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources: U.S. Geological Survey Bulletin 1122, Report: vi, 113 p.; 8 Plates: 28 x 18 inches or smaller, https://doi.org/10.3133/b1122F.","productDescription":"Report: vi, 113 p.; 8 Plates: 28 x 18 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":109365,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20827.htm","linkFileType":{"id":5,"text":"html"},"description":"20827"},{"id":63375,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63374,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63373,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63372,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63371,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1122f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63370,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63369,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63368,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1122f/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Haldeman and Wrigley quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.375,\n              38.25\n            ],\n            [\n              -83.25,\n              38.25\n            ],\n            [\n              -83.25,\n              38.0\n            ],\n            [\n              -83.375,\n              38.0\n            ],\n            [\n              -83.375,\n              38.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6863e2","contributors":{"authors":[{"text":"Patterson, Sam H.","contributorId":62996,"corporation":false,"usgs":true,"family":"Patterson","given":"Sam","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hosterman, John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":214697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huddle, John Warfield","contributorId":23932,"corporation":false,"usgs":true,"family":"Huddle","given":"John","email":"","middleInitial":"Warfield","affiliations":[],"preferred":false,"id":214696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":59791,"text":"mf247 - 1962 - Preliminary geologic map of the Nome C-1 quadrangle, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:13","indexId":"mf247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"247","title":"Preliminary geologic map of the Nome C-1 quadrangle, Seward Peninsula, Alaska","language":"ENGLISH","doi":"10.3133/mf247","usgsCitation":"Hummel, C., 1962, Preliminary geologic map of the Nome C-1 quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 247, 1 map ;44 x 39 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf247.","productDescription":"1 map ;44 x 39 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104026,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2663.htm","linkFileType":{"id":5,"text":"html"},"description":"2663"},{"id":184549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165.5,64.5 ], [ -165.5,64.75 ], [ -165,64.75 ], [ -165,64.5 ], [ -165.5,64.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67af2d","contributors":{"authors":[{"text":"Hummel, C. H.","contributorId":29065,"corporation":false,"usgs":true,"family":"Hummel","given":"C. H.","affiliations":[],"preferred":false,"id":262599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35479,"text":"b1148 - 1962 - Summary of rock salt deposits in the United States as possible storage sites for radioactive waste materials","interactions":[{"subject":{"id":56172,"text":"ofr5995 - 1959 - Summary of rock salt deposits in the United States as possible disposal sites for radioactive waste","indexId":"ofr5995","publicationYear":"1959","noYear":false,"title":"Summary of rock salt deposits in the United States as possible disposal sites for radioactive waste"},"predicate":"SUPERSEDED_BY","object":{"id":35479,"text":"b1148 - 1962 - Summary of rock salt deposits in the United States as possible storage sites for radioactive waste materials","indexId":"b1148","publicationYear":"1962","noYear":false,"title":"Summary of rock salt deposits in the United States as possible storage sites for radioactive waste materials"},"id":1}],"lastModifiedDate":"2025-05-15T14:20:04.620399","indexId":"b1148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1148","title":"Summary of rock salt deposits in the United States as possible storage sites for radioactive waste materials","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1148","usgsCitation":"Pierce, W.G., and Rich, E.I., 1962, Summary of rock salt deposits in the United States as possible storage sites for radioactive waste materials: U.S. Geological Survey Bulletin 1148, 91 p., https://doi.org/10.3133/b1148.","productDescription":"91 p.","costCenters":[],"links":[{"id":485956,"rank":10,"type":{"id":36,"text":"NGMDB Index 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,{"id":46930,"text":"ofr6289 - 1962 - Geologic map of the Mammoth mine area, Tintic district, Utah","interactions":[{"subject":{"id":46930,"text":"ofr6289 - 1962 - Geologic map of the Mammoth mine area, Tintic district, Utah","indexId":"ofr6289","publicationYear":"1962","noYear":false,"title":"Geologic map of the Mammoth mine area, Tintic district, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":6190,"text":"pp1024 - 1979 - General geology and mines of the East Tintic mining district, Utah and Juab counties, Utah, with sections on the geology of the Burgin mine and the geology of the Trixie mine","indexId":"pp1024","publicationYear":"1979","noYear":false,"title":"General geology and mines of the East Tintic mining district, Utah and Juab counties, Utah, with sections on the geology of the Burgin mine and the geology of the Trixie mine"},"id":1}],"supersededBy":{"id":6190,"text":"pp1024 - 1979 - General geology and mines of the East Tintic mining district, Utah and Juab counties, Utah, with sections on the geology of the Burgin mine and the geology of the Trixie mine","indexId":"pp1024","publicationYear":"1979","noYear":false,"title":"General geology and mines of the East Tintic mining district, Utah and Juab counties, Utah, with sections on the geology of the Burgin mine and the geology of the Trixie mine"},"lastModifiedDate":"2025-09-25T19:14:45.838778","indexId":"ofr6289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-89","title":"Geologic map of the Mammoth mine area, Tintic district, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6289","usgsCitation":"Morris, H.T., 1962, Geologic map of the Mammoth mine area, Tintic district, Utah: U.S. Geological Survey Open-File Report 62-89, 1 Plate: 17.96 x 13.19 inches, https://doi.org/10.3133/ofr6289.","productDescription":"1 Plate: 17.96 x 13.19 inches","costCenters":[],"links":[{"id":369488,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0089/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170858,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0089/report-thumb.jpg"},{"id":496174,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8034.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"Mammoth mine area, Tintic district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.19512939453125,\n              39.87391156801293\n            ],\n            [\n              -112.027587890625,\n              39.87391156801293\n            ],\n            [\n              -112.027587890625,\n              39.98132938627215\n            ],\n            [\n              -112.19512939453125,\n              39.98132938627215\n            ],\n            [\n              -112.19512939453125,\n              39.87391156801293\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c20","contributors":{"authors":[{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":234350,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22552,"text":"ofr6210 - 1962 - Relation of surface and ground water in the Souris River Valley near Minot, North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:59","indexId":"ofr6210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-10","title":"Relation of surface and ground water in the Souris River Valley near Minot, North Dakota","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr6210","issn":"0094-9140","usgsCitation":"Bradley, E., 1962, Relation of surface and ground water in the Souris River Valley near Minot, North Dakota: U.S. Geological Survey Open-File Report 62-10, 12 p., [1] leaf of plates :map ;28 cm., https://doi.org/10.3133/ofr6210.","productDescription":"12 p., [1] leaf of plates :map ;28 cm.","costCenters":[],"links":[{"id":155002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634a33","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":188454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35183,"text":"b1099B - 1962 - Uranium-bearing coal in the eastern part of the Red Desert area, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:33","indexId":"b1099B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1099","chapter":"B","title":"Uranium-bearing coal in the eastern part of the Red Desert area, Wyoming","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1099B","usgsCitation":"Masursky, H., 1962, Uranium-bearing coal in the eastern part of the Red Desert area, Wyoming: U.S. Geological Survey Bulletin 1099, p. B1-B152, ill. ;24 cm., https://doi.org/10.3133/b1099B.","productDescription":"p. B1-B152, ill. ;24 cm.","costCenters":[],"links":[{"id":109329,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20785.htm","linkFileType":{"id":5,"text":"html"},"description":"20785"},{"id":165932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1099b/report-thumb.jpg"},{"id":63055,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63056,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63057,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63058,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63059,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63060,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63061,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63062,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63063,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63064,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1099b/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1099b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60530c","contributors":{"authors":[{"text":"Masursky, Harold","contributorId":94304,"corporation":false,"usgs":true,"family":"Masursky","given":"Harold","email":"","affiliations":[],"preferred":false,"id":214215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1045,"text":"wsp1594B - 1962 - Experiments in water spreading at Newark, Delaware","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1594B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1594","chapter":"B","title":"Experiments in water spreading at Newark, Delaware","docAbstract":"Two experiments in water spreading were made at Newark, Del., to evaluate the prospects of using excess storm runoff to recharge the shallow water-table aquifer which serves the community. Water was diverted from 1 of the city's 3 production wells and released into an infiltration ditch near the municipal well field. \r\n\r\nAlthough slightly more than 65,000 cubic feet of water (nearly 500,000 gallons ) was spread in the infiltration ditch and allowed to seep into the subsurface, there was no indication that any appreciable amount of water reached the producing aquifer. Instead, a perched zone of saturation was created by the presence of an impermeable or slightly permeable bed above the water table. So effective is this barrier to the downward movement of water that within a period of less than 1 day, the apex of the perched zone rose about 10 feet to the level of the bottom of the infiltration ditch. As more water was added, the mound of saturation spread laterally. \r\n\r\nOn the basis of these experiments, it appears that the principal aquifer at Newark, Del., would not be benefited by spreading water in shallow infiltration ditches or basins. However, the absorptive capacity of the unsaturated materials which occur at a shallow depth, is sufficient to permit the disposal of large volumes of storm runoff.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1594B","usgsCitation":"Boggess, D.H., and Rima, D.R., 1962, Experiments in water spreading at Newark, Delaware: U.S. Geological Survey Water Supply Paper 1594, 15 p. :illus., map., https://doi.org/10.3133/wsp1594B.","productDescription":"15 p. :illus., map.","costCenters":[],"links":[{"id":137901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1594b/report-thumb.jpg"},{"id":25708,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1594b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25709,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1594b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c21","contributors":{"authors":[{"text":"Boggess, Durward Haye","contributorId":102049,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"Haye","affiliations":[],"preferred":false,"id":143085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rima, Donald Robert","contributorId":99535,"corporation":false,"usgs":true,"family":"Rima","given":"Donald","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":143084,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1333,"text":"wsp1536E - 1962 - Theory of aquifer tests","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1536E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1536","chapter":"E","title":"Theory of aquifer tests","docAbstract":"The development of water supplies from wells was placed on a rational basis with Darcy's development of the law governing the movement of fluids through sands and with Dupuit's application of that law to the problem of radial flow toward a pumped well. As field experience increased, confidence in the applicability of quantitative methods was gained and interest in developing solutions for more complex hydrologic problems was stimulated. An important milestone was Theis' development in 1935 of a solution for the nonsteady flow of ground water, which enabled hydrologists for the first time to predict future changes in ground-water levels resulting from pumping or recharging of wells. In the quarter century since, quantitative ground-water hydrology has been enlarging so rapidly as to discourage the preparation of comprehensive textbooks. \r\n\r\nThis report surveys developments in fluid mechanics that apply to groundwater hydrology. It emphasizes concepts and principles, and the delineation of limits of applicability of mathematical models for analysis of flow systems in the field. It stresses the importance of the geologic variable and its role in governing the flow regimen. \r\n\r\nThe report discusses the origin, occurrence, and motion of underground water in relation to the development of terminology and analytic expressions for selected flow systems. It describes the underlying assumptions necessary for mathematical treatment of these flow systems, with particular reference to the way in which the assumptions limit the validity of the treatment.","language":"ENGLISH","publisher":"U.S. Government Print. Office,","doi":"10.3133/wsp1536E","usgsCitation":"Ferris, J., Knowles, D., Brown, R.H., and Stallman, R., 1962, Theory of aquifer tests: U.S. Geological Survey Water Supply Paper 1536, vii, 105 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1536E.","productDescription":"vii, 105 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":12,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wsp1536-E","linkFileType":{"id":5,"text":"html"}},{"id":137382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd475","contributors":{"authors":[{"text":"Ferris, J.G.","contributorId":12453,"corporation":false,"usgs":true,"family":"Ferris","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":143577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knowles, D.B.","contributorId":83898,"corporation":false,"usgs":true,"family":"Knowles","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":143580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143578,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stallman, R.H.","contributorId":55800,"corporation":false,"usgs":true,"family":"Stallman","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":143579,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":33983,"text":"b1141I - 1962 - Character and history of the Upper Ohio River valley","interactions":[],"lastModifiedDate":"2012-02-02T00:09:26","indexId":"b1141I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1141","chapter":"I","title":"Character and history of the Upper Ohio River valley","language":"ENGLISH","publisher":"U.S. Govt. Print. Off. ; For sale by the Supt. of Docs.,","doi":"10.3133/b1141I","usgsCitation":"Carlston, C.W., 1962, Character and history of the Upper Ohio River valley: U.S. Geological Survey Bulletin 1141, iii, 10 p. :ill., map ;23 cm., https://doi.org/10.3133/b1141I.","productDescription":"iii, 10 p. :ill., map ;23 cm.","costCenters":[],"links":[{"id":96218,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1141i/report.pdf","size":"666","linkFileType":{"id":1,"text":"pdf"}},{"id":164146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1141i/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5925","contributors":{"authors":[{"text":"Carlston, Charles William","contributorId":95871,"corporation":false,"usgs":true,"family":"Carlston","given":"Charles","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":212279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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