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Alaska","indexId":"pp539","publicationYear":"1966","noYear":false,"title":"Potential effects of Project Chariot on local water supplies, northwestern Alaska"},"id":1}],"supersededBy":{"id":6254,"text":"pp539 - 1966 - Potential effects of Project Chariot on local water supplies, northwestern Alaska","indexId":"pp539","publicationYear":"1966","noYear":false,"title":"Potential effects of Project Chariot on local water supplies, northwestern Alaska"},"lastModifiedDate":"2012-02-02T00:11:20","indexId":"ofr62103","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":"62-103","title":"Potential effects of Project Chariot on local water 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M.","contributorId":102865,"corporation":false,"usgs":true,"family":"Piper","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":245061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52239,"text":"ofr6243 - 1962 - The Precambrian geology and talc deposits of the Balmat-Edwards district, northwest Adirondack Mountains, New York","interactions":[],"lastModifiedDate":"2018-04-27T15:14:23","indexId":"ofr6243","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":"62-43","title":"The Precambrian geology and talc deposits of the Balmat-Edwards district, northwest Adirondack Mountains, New York","docAbstract":"

The Balmat-Edwards, or Gouverneur, mining district is in the Grenville Lowlands of the northwest Adirondacks, St. Lawrence County, New York. In the district, important deposits of talc and zinc and minor deposits of lead are mined from a northeast trending belt of marble. Deposits of pyrite that were prospected and mined during and before World War I occur in schists in the vicinity of Pyrites and Antwerp villages. Fifteen to 50 miles east-southeast is the St. Lawrence County magnetite district, which contains commercially important magnetite deposits.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6243","usgsCitation":"Engel, A., 1962, The Precambrian geology and talc deposits of the Balmat-Edwards district, northwest Adirondack Mountains, New York: U.S. Geological Survey Open-File Report 62-43, Part 1: xvi, 349 p.; Part 2: xliii p.; 51 plates: 36.58 x 12.56 inches or smaller, https://doi.org/10.3133/ofr6243.","productDescription":"Part 1: xvi, 349 p.; Part 2: xliii p.; 51 plates: 36.58 x 12.56 inches or smaller","costCenters":[],"links":[{"id":353803,"rank":14,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1962/0043/figure-11.pdf","text":"Figure 11","linkFileType":{"id":1,"text":"pdf"}},{"id":353804,"rank":15,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1962/0043/figure-12.pdf","text":"Figure 12","linkFileType":{"id":1,"text":"pdf"}},{"id":353805,"rank":16,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1962/0043/figure-13.pdf","text":"Figure 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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":52280,"text":"ofr62123 - 1962 - Variations in the chemical character of the water in the Englishtown formation, New Jersey","interactions":[{"subject":{"id":52280,"text":"ofr62123 - 1962 - Variations in the chemical character of the water in the Englishtown formation, New Jersey","indexId":"ofr62123","publicationYear":"1962","noYear":false,"title":"Variations in the chemical character of the water in the Englishtown formation, New Jersey"},"predicate":"SUPERSEDED_BY","object":{"id":6378,"text":"pp498B - 1965 - Variations in chemical character of water in the Englishtown Formation, New Jersey","indexId":"pp498B","publicationYear":"1965","noYear":false,"chapter":"B","title":"Variations in chemical character of water in the Englishtown Formation, New Jersey"},"id":1}],"supersededBy":{"id":6378,"text":"pp498B - 1965 - Variations in chemical character of water in the Englishtown Formation, New Jersey","indexId":"pp498B","publicationYear":"1965","noYear":false,"title":"Variations in chemical character of water in the Englishtown Formation, New Jersey"},"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62123","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":"62-123","title":"Variations in the chemical character of the water in the Englishtown formation, New Jersey","language":"ENGLISH","doi":"10.3133/ofr62123","usgsCitation":"Seaber, P., 1962, Variations in the chemical character of the water in the Englishtown formation, New Jersey: U.S. Geological Survey Open-File Report 62-123, 68 p., https://doi.org/10.3133/ofr62123.","productDescription":"68 p.","costCenters":[],"links":[{"id":178826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602986","contributors":{"authors":[{"text":"Seaber, P. R.","contributorId":53802,"corporation":false,"usgs":true,"family":"Seaber","given":"P. R.","affiliations":[],"preferred":false,"id":245076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":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":1767,"text":"wsp1499C - 1962 - Water resources of the Utica-Rome area, New York","interactions":[],"lastModifiedDate":"2021-12-13T21:17:31.346876","indexId":"wsp1499C","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":"1499","chapter":"C","title":"Water resources of the Utica-Rome area, New York","docAbstract":"The Utica-Rome area is along the Mohawk River and New York State Erie (Barge) Canal about midway between Lake Ontario and Albany. It encompasses about 390 square miles centered around the industrial cities of Utica and Rome. The Mohawk River, its tributary West Canada Creek, and a system of reservoirs and diversions to maintain the flow in the barge-canal system, assure an ample water supply for the foreseeable needs of the area. The water from these sources is generally of good chemical quality requiring little treatment, although that from the Mohawk River is only fair and may require some treatment for sensitive industrial processes. Additional surface water is available from smaller streams in the area, particularly Oriskany and Sauquoit Creeks, but the water from these sources is hard, and has a dissolved-solids content of more than 250 ppm (parts per million). Ground water is available in moderate quantities from unconsolidated sand and gravel deposits in the river valleys and buried bedrock channels, and in small quantities from bedrock formations and less permeable unconsolidated deposits. The quality of water from sand and gravel, and bedrock ranges from good to poor. However, where necessary, the quality can be improved with treatment. \r\n\r\nThe Mohawk River is the source of the largest quantity of water in the area. The flow of the stream below Delta Dam equals or exceeds 108 mgd (million gallons per day) 90 percent of the time, and at Little Falls it equals or exceeds 560 mgd 90 percent of the time. The flow between these two points is increased by additions from Oriskany, Sauquoit, and West Canada Creeks and from many smaller tributary streams. The flow is also increased by diversions from outside the area, from the Black and Chenango Rivers and West Canada Creek for improvement of navigation in the Erie (Barge) Canal, and from West Canada and East Branch Fish Creeks for the public supplies of Utica and Rome. Much of the public-supply water eventually reaches the river by way of sewerage and industrial waste-disposal systems. The total diversion from these sources averages more than 92 mgd. An estimated 18.5 mgd is withdrawn from the Mohawk River by industry, mostly for nonconsumptive uses. \r\n\r\nFloods in the Utica-Rome area are not a frequent problem owing to the use of regulatory measures. The major streams fluctuate through a narrow range in stage and generally only a narrow strip along the streams is subject to flooding. Water-bearing sand and gravel deposits in the major river valleys are the principal sources of ground water, especially where they are recharged by infiltration from streams. The most important potential source is the deposit of sand and gravel underlying the extensive plain adjacent to the Mohawk River between Delta Reservoir and Rome. Maximum sustained yields from these deposits are not known; but moderate quantities of water, 300 gpm (gallons per minute) or less from a single well, can probably be obtained from some parts of the sand plain area, particularly in the vicinity of a buried bedrock channel that extends southwestward from Delta Reservoir. Similar quantities of ground water probably can be withdrawn from some parts of the flood plain of the Mohawk River between Rome and Frankfort and from the sand and gravel deposits filling the valley of Ninemile Creek below Holland Patent. The deposits underlying the flood plain of the Mohawk River generally are fine grained but in places contain interstratified beds of coarser sand and gravel. The most productive part of the flood plain is at the east end near Frankfort. The deposits in Ninemile Creek valley also are generally fine grained; but where they are sufficiently thick, as over a buried bedrock valley southwest of Floyd, moderate quantities of water may be obtained. \r\n\r\nSmall to moderate quantities of water (150 gpm or less from a single well) can be obtained from sand and gravel deposits in the bottoms of Oriskany and Sauquoit Creek vall","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1499C","usgsCitation":"Halberg, H., Hunt, O.P., and Pauszek, F.H., 1962, Water resources of the Utica-Rome area, New York: U.S. Geological Survey Water Supply Paper 1499, Report: iv, 46 p.; 3 Plates: 21.00 × 17.15 inches or smaller, https://doi.org/10.3133/wsp1499C.","productDescription":"Report: iv, 46 p.; 3 Plates: 21.00 × 17.15 inches or smaller","costCenters":[],"links":[{"id":26891,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26890,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26889,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499c/report-thumb.jpg"},{"id":26892,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392829,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24439.htm"}],"country":"United States","state":"New York","city":"Rome, Utica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.59417724609375,\n 43.018705515824635\n ],\n [\n -75.10528564453125,\n 43.018705515824635\n ],\n [\n -75.10528564453125,\n 43.29120116988416\n ],\n [\n -75.59417724609375,\n 43.29120116988416\n ],\n [\n -75.59417724609375,\n 43.018705515824635\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3376","contributors":{"authors":[{"text":"Halberg, Henry N.","contributorId":19929,"corporation":false,"usgs":true,"family":"Halberg","given":"Henry N.","affiliations":[],"preferred":false,"id":144113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, O. P.","contributorId":69116,"corporation":false,"usgs":true,"family":"Hunt","given":"O.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":144115,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144114,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":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":52271,"text":"ofr62107 - 1962 - Hydraulic model studies--stream gaging control structure for Carrizo-Corduroy Project, Arizona","interactions":[],"lastModifiedDate":"2013-08-01T15:16:00","indexId":"ofr62107","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":"62-107","title":"Hydraulic model studies--stream gaging control structure for Carrizo-Corduroy Project, Arizona","language":"ENGLISH","doi":"10.3133/ofr62107","usgsCitation":"Richardson, E., 1962, Hydraulic model studies--stream gaging control structure for Carrizo-Corduroy Project, Arizona: U.S. Geological Survey Open-File Report 62-107, 42 p., https://doi.org/10.3133/ofr62107.","productDescription":"42 p.","costCenters":[],"links":[{"id":179396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0107/report-thumb.jpg"},{"id":275860,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0107/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a1f4","contributors":{"authors":[{"text":"Richardson, E.V.","contributorId":105697,"corporation":false,"usgs":true,"family":"Richardson","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":245066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67313,"text":"i348 - 1962 - Geology of the Albany West quadrangle, Georgia","interactions":[],"lastModifiedDate":"2013-12-17T09:46:35","indexId":"i348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"348","title":"Geology of the Albany West quadrangle, Georgia","docAbstract":"The Albany West Quadrangle is near the east edge of the Dougherty Plain of southwestern Georgia, an area of karst topography. The Ocala limestone (uppoer Eocene) underlies the quadrangle and crops out along the Flint River and its tributaries and sinkholes. Sinkholes of two ages are developed in the limestone. A gravelly argillaceous sand of Pliocene(?) age is exposed in ditches near the Flint River and in a sinkhole in the western part of the quadrangle. Reddish brown, argillaceous, older Pleistocene sand, believed to be part of a marine terrace deposit above altitude 160 feet, overlies the Pliocene(?) and is exposed in a sinkhole. River terraces are present along the Flint River at altitudes of 175 and 200 feet. Accumulations of dune sand east of the Flint River are believed to have been derived from the earliest river-terrace deposit. The quadrangle is covered by a mixture of reddish-brown, argillaceous, older Pleistocene sand, and residuum containing siliceous boulders from the Ocala limestone, which has been mapped as residuum.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i348","collaboration":"Prepared in cooperation with the Georgia Department of Mines, Mining and Geology","usgsCitation":"Wait, R.L., 1962, Geology of the Albany West quadrangle, Georgia: U.S. Geological Survey IMAP 348, Plate: 41.67 x 36.05 inches, https://doi.org/10.3133/i348.","productDescription":"Plate: 41.67 x 36.05 inches","costCenters":[],"links":[{"id":102896,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1363.htm","linkFileType":{"id":5,"text":"html"},"description":"1363"},{"id":188414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0348/report-thumb.jpg"},{"id":279956,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0348/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Georgia","county":"Dougherty County;Lee County","city":"Albany","otherGeospatial":"Dougherty Plain;Flint River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.25,31.5 ], [ -84.25,31.625 ], [ -84.125,31.625 ], [ -84.125,31.5 ], [ -84.25,31.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68361e","contributors":{"authors":[{"text":"Wait, Robert L.","contributorId":12839,"corporation":false,"usgs":true,"family":"Wait","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52272,"text":"ofr62108 - 1962 - Ground-water situation in Delaware--1962","interactions":[],"lastModifiedDate":"2012-02-02T00:11:20","indexId":"ofr62108","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":"62-108","title":"Ground-water situation in Delaware--1962","language":"ENGLISH","doi":"10.3133/ofr62108","usgsCitation":"Rima, D., 1962, Ground-water situation in Delaware--1962: U.S. Geological Survey Open-File Report 62-108, 17 p., https://doi.org/10.3133/ofr62108.","productDescription":"17 p.","costCenters":[],"links":[{"id":179397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656a53","contributors":{"authors":[{"text":"Rima, D.R.","contributorId":70845,"corporation":false,"usgs":true,"family":"Rima","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":245067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61792,"text":"gq171 - 1962 - Geology of the Ano quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"171","title":"Geology of the Ano quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq171","usgsCitation":"Stager, H.K., 1962, Geology of the Ano quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 171, 1 map., https://doi.org/10.3133/gq171.","productDescription":"1 map.","costCenters":[],"links":[{"id":102170,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_619.htm","linkFileType":{"id":5,"text":"html"},"description":"619"},{"id":248084,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0171/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":252744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0171/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.36749999999999,37 ], [ -84.36749999999999,37.1175 ], [ -84.25,37.1175 ], [ -84.25,37 ], [ -84.36749999999999,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6835fe","contributors":{"authors":[{"text":"Stager, Harold Keith","contributorId":54299,"corporation":false,"usgs":true,"family":"Stager","given":"Harold","email":"","middleInitial":"Keith","affiliations":[],"preferred":false,"id":266369,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5763,"text":"pp345 - 1962 - Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont","interactions":[{"subject":{"id":12992,"text":"ofr5147 - 1951 - Diamond-drill exploration of the Rousseau talc prospect, Cambridge, Vermont, and the Barnes Hill prospect, Waterbury, Vermont","indexId":"ofr5147","publicationYear":"1951","noYear":false,"title":"Diamond-drill exploration of the Rousseau talc prospect, Cambridge, Vermont, and the Barnes Hill prospect, Waterbury, Vermont"},"predicate":"SUPERSEDED_BY","object":{"id":5763,"text":"pp345 - 1962 - Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont","indexId":"pp345","publicationYear":"1962","noYear":false,"title":"Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont"},"id":1},{"subject":{"id":55476,"text":"ofr4530 - 1945 - Talc mines in Vermont","indexId":"ofr4530","publicationYear":"1945","noYear":false,"title":"Talc mines in Vermont"},"predicate":"SUPERSEDED_BY","object":{"id":5763,"text":"pp345 - 1962 - Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont","indexId":"pp345","publicationYear":"1962","noYear":false,"title":"Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont"},"id":2}],"lastModifiedDate":"2025-05-16T20:48:11.100437","indexId":"pp345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"345","title":"Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp345","usgsCitation":"Chidester, A., 1962, Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont: U.S. Geological Survey Professional Paper 345, Report: vii, 207 p.; 7 Plates: 17.00 x 35.00 inches or smaller, https://doi.org/10.3133/pp345.","productDescription":"Report: vii, 207 p.; 7 Plates: 17.00 x 35.00 inches or smaller","costCenters":[],"links":[{"id":122995,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0345/report-thumb.jpg"},{"id":32349,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0345/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32350,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0345/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32351,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0345/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32352,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0345/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32353,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0345/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32354,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0345/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32355,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0345/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32356,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0345/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":486130,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4341.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Vermont","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -72.825,\n 44.4056\n ],\n [\n -72.825,\n 44.2161\n ],\n [\n -72.625,\n 44.2161\n ],\n [\n -72.625,\n 44.4056\n ],\n [\n -72.825,\n 44.4056\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687342","contributors":{"authors":[{"text":"Chidester, A.H.","contributorId":42940,"corporation":false,"usgs":true,"family":"Chidester","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":151543,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63393,"text":"gq187 - 1962 - Geology of the Williamson quadrangle in Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:47","indexId":"gq187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"187","title":"Geology of the Williamson quadrangle in Kentucky","language":"ENGLISH","doi":"10.3133/gq187","usgsCitation":"Alvord, D.C., and Trent, V.A., 1962, Geology of the Williamson quadrangle in Kentucky: U.S. Geological Survey Geologic Quadrangle 187, 1 map., https://doi.org/10.3133/gq187.","productDescription":"1 map.","costCenters":[],"links":[{"id":102187,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_636.htm","linkFileType":{"id":5,"text":"html"},"description":"636"},{"id":249488,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0187/report.pdf","size":"36","linkFileType":{"id":1,"text":"pdf"}},{"id":252970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0187/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.36749999999999,37.6175 ], [ -82.36749999999999,37.75 ], [ -82.25,37.75 ], [ -82.25,37.6175 ], [ -82.36749999999999,37.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9bb","contributors":{"authors":[{"text":"Alvord, Donald Clayton","contributorId":49356,"corporation":false,"usgs":true,"family":"Alvord","given":"Donald","email":"","middleInitial":"Clayton","affiliations":[],"preferred":false,"id":268775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trent, Virgil A.","contributorId":47381,"corporation":false,"usgs":true,"family":"Trent","given":"Virgil","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":268774,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36026,"text":"b1122E - 1962 - Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky","interactions":[{"subject":{"id":55418,"text":"ofr4415 - 1944 - Preliminary notes on the geology of the Levias fault system, Crittenden County, Kentucky","indexId":"ofr4415","publicationYear":"1944","noYear":false,"title":"Preliminary notes on the geology of the Levias fault system, Crittenden County, Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":36026,"text":"b1122E - 1962 - Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky","indexId":"b1122E","publicationYear":"1962","noYear":false,"chapter":"E","title":"Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky"},"id":1}],"lastModifiedDate":"2022-07-22T18:41:11.031816","indexId":"b1122E","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":"E","title":"Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky","docAbstract":"The fault systems of the Levias-Keystone and Dike-Eaton areas, in the \r\nKentucky-Illinois fiuorspar district, are a complex northeastward-trending sys- \r\ntem and a simple northwestward-trending system of steeply dipping normal \r\nfaults, associated in part with a lamprophyre dike. Fluorspar mining started \r\nin the area about 1900 and, as of 1945, more than 200,000 tons of crude ore \r\nprobably has been mined; most of the ore was from the Levias-Keystone area. \r\nA small quantity of zinc and lead ore also is present in the Dike-Eaton area.\r\n\r\nThe deposits are localized along faults that displace fiat-lying or low-dipping \r\nlimestones, sandstones, and shales of the Meramec and Chester series of Missis- \r\nsippian age. Movement along most of the faults was principally vertical, with \r\ndisplacement as much as 600 feet. Some horizontal movement occurred along \r\nat least one fault. Geologic mapping of the surface and data from underground \r\nworkings have revealed 13 faults in an area of four-fifths of a square mile. \r\nOnly a few of these faults are known to contain economically important deposits \r\nof fiuorspar.\r\n\r\nThe most abundant vein minerals are calcite and fiuorite with subordinate \r\nquantities of sphalerite, galena, barite, and quartz. Some weathering products \r\nof sphalerite and galena are present also. The veins are dominantly calcite \r\nthat contains fiuorite lenses but in places are mainly fiuorite having lesser \r\nquantities of calcite. Sphalerite- and galena-bearing deposits are present in the Dike-Eaton area. The ore bodies mainly are the result of fissure filling and replacement of calcite by fiuorite; in addition a small amount of limestone \r\nwallrock probably has been replaced. Residual concentrations of high-grade \r\nfluorspar in the overburden above faults have yielded some so-called gravel \r\nfiuorspar. The position of the veins within the faults may be related to one \r\nor more factors such as type of wallrock, change in dip of the fault, and amount of displacement.","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/b1122E","usgsCitation":"Trace, R.D., 1962, Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky: U.S. Geological Survey Bulletin 1122, Report: iv, 26 p.; 4 Plates: 28.00 × 8.50 inches or smaller, https://doi.org/10.3133/b1122E.","productDescription":"Report: iv, 26 p.; 4 Plates: 28.00 × 8.50 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":63975,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1122e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63974,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63973,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63972,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63971,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1122e/report-thumb.jpg"},{"id":109364,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20826.htm","linkFileType":{"id":5,"text":"html"},"description":"20826"}],"country":"United States","state":"Kentucky","county":"Crittenden County","otherGeospatial":"Levias-Keystone and Dike-Eaton areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.204,\n 37.333\n ],\n [\n -88.153,\n 37.333\n ],\n [\n -88.153,\n 37.287\n ],\n [\n -88.204,\n 37.287\n ],\n [\n -88.204,\n 37.333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68663e","contributors":{"authors":[{"text":"Trace, Robert Denny","contributorId":53866,"corporation":false,"usgs":true,"family":"Trace","given":"Robert","email":"","middleInitial":"Denny","affiliations":[],"preferred":false,"id":215636,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13687,"text":"ofr6248 - 1962 - Bedrock geology of the Mount Carmel and Southington quadrangles, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr6248","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":"62-48","title":"Bedrock geology of the Mount Carmel and Southington quadrangles, Connecticut","docAbstract":"New data concerning the geologic structure, stratigraphy, petrography, origin, and ages of bedrock formations in an area of approximately 111 square miles in south-central Connecticut were obtained in the course of detailed geologic mapping from 1957 to 1960. Mapping was done at a scale of 1:24,000 on topographic base maps having a 10-foot contour interval.\r\n\r\nBedrock formations are classified in two principal categories. The first includes metasedimentary, meta-igneous, and igneous rocks of Precambrian to Devonian age, which crop out in the western parts of both quadrangles. The second includes sedimentary and igneous rocks of the Newark Group of Late Triassic age, which crop out in the eastern parts of the quadrangles. Diabase dikes, which are Late Triassic or younger in age, intruded rocks in both the western and eastern parts of the map area.\r\n\r\nRocks in the western part of the area underwent progressive regional metamorphism in Middle to Late Devonian time. The arrangement of the chlorite, garnet, biotite, staurolite, and kyanite zones here is approximately the mirror-image of metamorphic zones in Dutchess County, New York. However, garnet appeared before biotite in politic rocks in the map area, because the ration MgO/FeO is low.\r\n\r\nWaterbury Gneiss and the intrusive Woodtick Gneiss are parts of a basement complex of Precambrian age, which forms the core of the Waterbury dome. This structure is near the southern end of a line of similar domes that lie along the crest of a geanticline east of the Green Mountain anticlinorium. The Waterbury Gneiss is believed to have been metamorphosed in Precambrian time as well as in Paleozoic time. The Woodtick Gneiss also may have been metamorphosed more than once.\r\n\r\nIn Paleozoic time, sediments were deposited in geosynclines during two main cycles of sedimentation. The Straits, Southington Mountain, and Derby Hill Schists, which range in age from Cambrian to Ordovician, reflect a transition from relatively clean politic sediments to thinly layered sediments that contained rather high percentages of fine-grained volcanic debris. Metadiabase and metabasalt extrusives above Derby Hill Schist south of the map area represent more intense volcanic activity before or during the early stages of the Taconic disturbance in Late Ordovician time. Impure argillaceous, siliceous, and minor calcareous sediments of the Wepawaug Schist, which is Silurian and Devonian in age, were deposited unconformably on older rocks during renewed subsidence of a geosyncline. The Wepawaug now occupies the trough of a tight syncline, which formed before and during progressive regional metamorphism at the time of the Acadian orogeny in middle to Late Devonian time.\r\n\r\nFelsic igneous rocks were intruded into the metasedimentary formations of Paleozoic age before the climax of the latest progressive regional metamorphism. Intrusives that gave rise to the Prospect and Ansonia Gneisses were emplaced mainly in the Southington Mountain Schist, and the igneous rocks as well as the host rocks were metamorphosed in the staurolite zone. Although it is possible that these two intrusives were emplaced during the Taconic disturbance, the writer believes it more likely that the igneous rocks from which the Prospect and Ansonia Gneisses formed were emplaced during the Acadian orogeny. Woodbridge Granite, which intruded the Wepawaug Schist, is Devonian in age and undoubtedly was emplaced during the Acadian orogeny. In this area the granite is essentially unmetamorphosed, because it is in the chlorite, garnet, and biotite zones. Southwest of the map area, however, metamorphic equivalents of the Woodbridge are found in Wepawaug Schist in the staurolite zone. The Ansonia Gneiss, therefore, may be a metamorphic equivalent of the Woodbridge Granite.\r\n\r\nRocks of Late Triassic age formerly covered the entire map area, but were eroded from the western part after tilting and faulting in Late Triassic time. The New Haven Arkose of the Newark ","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6248","usgsCitation":"Fritts, C.E., 1962, Bedrock geology of the Mount Carmel and Southington quadrangles, Connecticut: U.S. Geological Survey Open-File Report 62-48, 161 p. ill., maps (some col.) ;30 cm., https://doi.org/10.3133/ofr6248.","productDescription":"161 p. ill., maps (some col.) ;30 cm.","costCenters":[],"links":[{"id":147018,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0048/report-thumb.jpg"},{"id":42237,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42238,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42239,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42240,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42241,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42242,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42243,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42244,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42245,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0048/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db63404e","contributors":{"authors":[{"text":"Fritts, Crawford Ellswroth","contributorId":102087,"corporation":false,"usgs":true,"family":"Fritts","given":"Crawford","email":"","middleInitial":"Ellswroth","affiliations":[],"preferred":false,"id":168232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":62414,"text":"gq167 - 1962 - Geology of the West Carlsbad quadrangle, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:42","indexId":"gq167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"167","title":"Geology of the West Carlsbad quadrangle, New Mexico","language":"ENGLISH","doi":"10.3133/gq167","usgsCitation":"Motts, W., 1962, Geology of the West Carlsbad quadrangle, New Mexico: U.S. Geological Survey Geologic Quadrangle 167, 1 map :col. ;44 x 37 cm. on sheet 76 x 127 cm. fold. to 30 x 24 cm., https://doi.org/10.3133/gq167.","productDescription":"1 map :col. ;44 x 37 cm. on sheet 76 x 127 cm. fold. to 30 x 24 cm.","costCenters":[],"links":[{"id":102165,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_614.htm","linkFileType":{"id":5,"text":"html"},"description":"614"},{"id":248585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0167/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":253729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0167/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.5,32.25 ], [ -104.5,32.5 ], [ 0,32.5 ], [ 0,32.25 ], [ -104.5,32.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c995","contributors":{"authors":[{"text":"Motts, Ward S.","contributorId":53032,"corporation":false,"usgs":true,"family":"Motts","given":"Ward S.","affiliations":[],"preferred":false,"id":267351,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15287,"text":"ofr6297 - 1962 - Provisional geologic map of the crystalline rocks of South Carolina","interactions":[],"lastModifiedDate":"2024-08-05T20:08:57.386446","indexId":"ofr6297","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":"62-97","title":"Provisional geologic map of the crystalline rocks of South Carolina","docAbstract":"

No abstract available. 

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