{"pageNumber":"354","pageRowStart":"8825","pageSize":"25","recordCount":11004,"records":[{"id":3568,"text":"cir760 - 1983 - Petroleum geology and resources of southeastern Mexico, northern Guatemala, and Belize","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"760","title":"Petroleum geology and resources of southeastern Mexico, northern Guatemala, and Belize","docAbstract":"Petroleum deposits in southeastern Mexico and Guatemala occur in two main basinal provinces, the Gulf Coast Tertiary basin area, which includes the Reforma and offshore Campeche Mesozoic fields, and the Peten basin of eastern Chiapas State (Mexico) and Guatemala. Gas production is mainly from Tertiary sandstone reservoirs of Miocene age. Major oil production, in order of importance, is from Cretaceous, Paleocene, and Jurassic carbonate reservoirs in the Reforma and offshore Campeche areas. Several small oil fields have been discovered in Cretaceous carbonate reservoirs in west-central Guatemala, and one major discovery has been reported in northwestern Guatemala. Small- to medium-sized oil accumulations also occur in Miocene sandstone reservoirs on salt structures in the Isthmus Saline basin of western Tabasco State, Mexico. Almost all important production is in salt structure traps or on domes and anticlines that may be related to deep-seated salt structures. Some minor oil production has occurred in Cretaceous carbonate reservoirs in a buried overthrust belt along the west flank of the Veracruz basin. \r\n\r\nThe sedimentary cover of Paleozoic through Tertiary rocks ranges in thickness from about 6,000 m (20,000 ft) to as much as 12,000 m (40,000 ft) or more in most of the region. Paleozoic marine carbonate and clastic rocks 1,000 to 2,000 m (3,300 to 6,500 ft) thick overlie the metamorphic and igneous basement in part of the region; Triassic through Middle Jurassic red beds and evaporite deposits, including halite, apparently are present throughout the region, deposited in part in a Triassic graben system. Upper Jurassic (Oxfordian) through Cretaceous rocks make up the bulk of the Mesozoic regional carbonate bank complex, which dominates most of the area. Tertiary marine and continental clastic rocks, some of deep water origin, 3,000 to 10,000 m (10,000 to 35,000 ft) thick, are present in the coastal plain Tertiary basins. These beds grade eastward into a carbonate sequence that overlies the Mesozoic carbonate complex on the Yucatan platform. \r\n\r\nDuring the past 10 years, about 50 large oil fields were discovered in the Reforma and offshore Campeche areas. Oil is produced from intensely microfractured Cretaceous, Paleocene, and Upper Jurassic dolomite reservoirs on blockfaulted salt swells or domes. Most fields are located in the \r\n\r\nMesozoic carbonate-bank margin and forebank talus (Tamabra) facies, which passes through the offshore Campeche and onshore Reforma areas. Oil source rocks are believed to be organic-rich shales and shaly carbonate rocks of latest Jurassic and possibly Early Cretaceous age. At least six of the Mesozoic discoveries are giant or supergiant fields. The largest is the Cantarell complex (about 8 billion to 10 billion barrels (BB)) in the offshore Campeche area and the Bermudez complex (about 8 BB) in the Reforma onshore area. Oil columns are unusually large (from 50 m to as much as 1,000 m, or 160 ft to 3,300 ft). Production rates are extremely high, averaging at least 3,000 to 5,000 barrels of oil per day (bo/d); some wells produce more than 20,000 bo/d, particularly in the offshore Campeche area, where 30,000- to 60,000-bo/d wells are reported. \r\n\r\nTertiary basin fields produce primarily from Miocene sandstone reservoirs. About 50 of these are oil fields ranging from 1 million barrels (MMB) to 200 MMB in size, located on faulted salt structures in the Isthmus Saline basin. Another 30 are gas or gas-condensate fields of a few billion cubic feet to 3 trillion to 4 trillion cubic feet (Tcf) located on salt structures or probable salt structures in the Macuspana, Comalcalco, Isthmus Saline, and Veracruz basins. Source rocks for the gas are believed to be carbonaceous shales interbedded with the sandstone reservoir bodies. \r\nIdentified reserves in the southeastern Mexico-Guatemala \r\narea, almost all in the Mesozoic fields, are about 53 BB of oil, \r\n3 BB of natural gas liquids, and 65 Tcf of gas. The estimat","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir760","usgsCitation":"Peterson, J.A., 1983, Petroleum geology and resources of southeastern Mexico, northern Guatemala, and Belize: U.S. Geological Survey Circular 760, vi, 44 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir760.","productDescription":"vi, 44 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":123013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0760/report-thumb.jpg"},{"id":30596,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0760/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e8e","contributors":{"authors":[{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147168,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11987,"text":"ofr83710 - 1983 - Comparative anatomy of epithermal precious- and base-metal districts hosted by volcanic rocks: A talk presented at the GAC/MSC/GGU Joint Annual Meeting, May 11-13, 1983, Victoria, British Columbia","interactions":[],"lastModifiedDate":"2018-10-22T08:47:25","indexId":"ofr83710","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-710","title":"Comparative anatomy of epithermal precious- and base-metal districts hosted by volcanic rocks: A talk presented at the GAC/MSC/GGU Joint Annual Meeting, May 11-13, 1983, Victoria, British Columbia","docAbstract":"<p>In order to distinguish dissimilar from similar features of epithermal districts, lithotectonic, mineralogical and geochemical traits are compiled for 15 such districts. The districts occur in structurally complex settings associated with silicic to intermediate volcanics. Affiliation with subduction environments on a continental scale and caldera settings on a regional scale is common but is not demonstrable for all districts. Most deposits formed near the end of major volcanism, but some formed considerably later. Paleodepth to the top of the ore is 300-600m for most districts, although Au-rich districts appear to be shallower. The lateral extent of the ore zone is highly variable and far exceeds the limited vertical range (300-800m). Most ore was deposited from dominantly meteoric fluids ranging in temperature from 220&deg;-290&deg;C. Salinities ranged from 0-13 wt% NaCl equiv., and typical values were 1-3 wt%. Although noted for eight deposits, boiling is clearly associated with precious-metal deposition in only two deposits. Four districts, typified by Goldfield, Nev., are characterized by a highly sulfidized mineral assemblage, advanced argillic alteration, and ore deposition closely following emplacement of the host rock. The remaining eleven districts highlight a second, discrete type of deposit. They contain adularia, exhibit sericitic &plusmn; argillic alteration, and were mineralized significantly after emplacement of the host rock. The latter category includes two subgroups: Ag- and base-metal-rich deposits (e.g., Creede, Colo.), and Au-rich, base-metal-poor deposits (e.g., Round Mtn., Nev.).</p>","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83710","usgsCitation":"Heald-Wetlaufer, P., Hayba, D.O., Foley, N.K., and Goss, J., 1983, Comparative anatomy of epithermal precious- and base-metal districts hosted by volcanic rocks: A talk presented at the GAC/MSC/GGU Joint Annual Meeting, May 11-13, 1983, Victoria, British Columbia: U.S. Geological Survey Open-File Report 83-710, 20 p., https://doi.org/10.3133/ofr83710.","productDescription":"20 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":145580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0710/report-thumb.jpg"},{"id":39981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0710/report.pdf","text":"Report","size":"1.00 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"Mexico, Peru, United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -101.3,\n              21\n            ],\n            [\n              -101.3,\n              21.1\n            ],\n            [\n              -101.2,\n              21.1\n            ],\n            [\n              -101.2,\n              21\n            ],\n            [\n              -101.3,\n              21\n   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dhayba@usgs.gov","orcid":"https://orcid.org/0000-0003-4092-1894","contributorId":396,"corporation":false,"usgs":true,"family":"Hayba","given":"Daniel","email":"dhayba@usgs.gov","middleInitial":"O.","affiliations":[],"preferred":true,"id":164539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foley, Nora K. 0000-0003-0124-3509 nfoley@usgs.gov","orcid":"https://orcid.org/0000-0003-0124-3509","contributorId":4010,"corporation":false,"usgs":true,"family":"Foley","given":"Nora","email":"nfoley@usgs.gov","middleInitial":"K.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":164537,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Goss, J.A.","contributorId":62222,"corporation":false,"usgs":true,"family":"Goss","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":164540,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":11729,"text":"ofr83747 - 1983 - Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California","interactions":[],"lastModifiedDate":"2022-09-23T20:16:56.047888","indexId":"ofr83747","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-747","title":"Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California","docAbstract":"Hydration-rind ages based on hydration-rind thicknesses of obsidian and an assumed hydration rate of 5 microns /1000 yrs have been determined for the 26 exposed Mono domes and coulees. Hydration-rind thickness data give good estimates of relative age differences between the domes, but determination of absolute ages will depend upon calibration to radiometric ages. \r\n\r\nThe first extrusion of highly differentiated, sparsely porphyritic rhyolite occurred an estimated 32,000 to 40,000 yrs ago and consists of a small dome at the northwest end of the contiguous chain. The next major extrusive event occurred about 24,000 yrs ago and is represented by two domes and a major tephra. About 10,000 yrs ago the frequency of eruptive activity increases and rhyolite lave was extruded at an average rate of 0.2 km3/1000 yrs; periods of dormancy ranging in length from 300 to 2000 yrs. About 2000 to 3000 yrs ago the rate of extrusion increased dramatically to 0.8 km3/1000 yrs beginning with the eruption of the South Coulee and its associated tephra. At the same time, the nature of erupted magma changed from sparsely porphyritic (3 to 10 per cent sanidine) to aphyric rhyolite. All eruptions since 2000 radiocarbon yrs BP have produced magma that is aphyric but is of the same chemical composition as the earlier porphyritic magma. Volumes of porphyritic and aphyric extrusives, each of which includes volumes of lava and volumes of pumiceous pyroclastics reduced for porosity, are nearly equal and together total about 4 km3. Projecting the recent rate of extrusion over the time since the last major eruption, 1185 radiocarbon yrs ago suggests that a future eruption in the Mono Chain could release as much as 1 km 3 of magma. The recent increase in extrusion rate and the contemporaneous change in the nature of the magma are attributed to an event in the magma chamber that allowed the release of hotter, more fluid, crystal-free magma. The young age for the beginning of rhyolite volcanism from the mono magma chamber suggests that rhyolite magma may have been emplaced in the shallow crust as recently as 32,000 to 40,000 yrs ago. Calculations by Lachenbruch et al. (1976, Jour. Geophys. Research, v. 81, p. 769-784) that a thermal disturbance at this age would have propagated upward by solid conduction only 4 km and offer an explanation for the lack of a heat-flow anomaly and surface indications of hydrothermal activity over the Mono magma chamber and its associated ring-fracture system. This report also contains new information on the age and chemistry of volcanics on the Mono Lake island, the Inyo domes, and tephras within the Long Valley Caldera. \r\n\r\nA newly discovered rhyolite tuff ring of late Quaternary age in the Toowa volcanic field of the southern Sierra Nevada is briefly described for it represents a new area that should be examined for potential as a geothermal area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83747","usgsCitation":"Wood, S.H., 1983, Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California: U.S. Geological Survey Open-File Report 83-747, vii, 76 p., https://doi.org/10.3133/ofr83747.","productDescription":"vii, 76 p.","costCenters":[],"links":[{"id":407293,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14207.htm","linkFileType":{"id":5,"text":"html"}},{"id":143964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0747/report-thumb.jpg"},{"id":39615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0747/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Long Valley and Mono Basin geothermal area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.129,\n              37.681\n            ],\n            [\n              -118.922,\n              37.681\n            ],\n            [\n              -118.922,\n              38.046\n            ],\n            [\n              -119.129,\n              38.046\n            ],\n            [\n              -119.129,\n              37.681\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e073f","contributors":{"authors":[{"text":"Wood, S. 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,{"id":5797,"text":"pp1253 - 1983 - Stratigraphy and paleontology of Mid-Cretaceous rocks in Minnesota and contiguous areas","interactions":[],"lastModifiedDate":"2024-11-18T19:11:49.604403","indexId":"pp1253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1253","title":"Stratigraphy and paleontology of Mid-Cretaceous rocks in Minnesota and contiguous areas","docAbstract":"PART A: Molluscan fossils are locally abundant at outcrops of Upper Cretaceous rocks in eastern North and South Dakota, northeastern Nebraska, northwestern Iowa, and western and northern Minnesota. Other Cretaceous mollusks have been found in the glacial deposits in Minnesota, Iowa, and Illinois. \r\n\r\nThe oldest well dated marine mollusks are of earliest late Cenomanian age and occur in northwestern Iowa. Mollusks of marginal marine \r\nand nonmarine environments in northwestern Iowa and south-central Minnesota are probably of slightly younger late Cenomanian age. The youngest mollusks treated in this report are bivalves of Santonian age found in the Niobrara Formation in eastern North and South Dakota. \r\n\r\nThe collections indicate the presence or former presence of the following ammonite zones in the northeastern part of the Western Interior seaway: \r\n\r\nSantonian: Scaphites depressus-Clioscaphites choteauensis \r\n\r\nConiacian: Scaphites uentrocosus; Scaphites preuentricosus \r\n\r\nTuronian: Scaphites coruensis; Scaphites whitfieldi; Prionocyclus hyatti; Subprionocyclus percarinatus; Collignoniceras woollgari; Watinoceras coloradoense \r\n\r\nCenomanian: Dunueganoceras albertense; Dunueganoceras pondi\r\n\r\nPART B: Sedimentary rocks of early Late Cretaceous age occur in the eastern parts of North Dakota, South Dakota, and Nebraska, and in Minnesota and western Iowa. They are generally included in, from oldest to youngest, the Dakota Formation, Graneros Shale, Greenhorn Formation, Carlile Shale, and Niobrara Formation. However, in eastern North Dakota, they are also assigned to, in ascending order, the Belle Fourche Shale, Greenhorn Formation, Carlile Shale, and Niobrara Formation. The Graneros Shale and laterally equivalent strata in the Belle Fourche Shale grade eastward into the Coleraine Formation of northeastern Minnesota and probably into the Windrow Formation of southeastern Minnesota. Cretaceous beds locally overlie rocks of Precambrian, Paleozoic, and Jurassic ages, and they are generally overlain by glacial drift and alluvium of Quaternary age. In Minnesota and adjoining areas, formations of mid-Cretaceous age commonly overlap the dissected surface of Precambrian rocks. The thickness of the lower Upper Cretaceous sequence ranges from about 223 m in eastern North Dakota and about 200 m in northeastern Nebraska to a featheredge in Minnesota and Iowa. \r\n\r\nThese lower Upper Cretaceous formations are composed mainly of shale, siltstone, sandstone, and limestone units of marine and nonmarine origin and were deposited near the eastern shore of a transgressing and regressing epicontinental sea in Cenomanian Turonian Coniacian. and Santonian time. During the late Cenoanian, the strandline was in Minnesota and was oriented generally northnortheast. Interpretations of the depositional environments of the strata and of fossils from outcrops and from clasts in glacial drift indicate that the Cretaceous seaway extended from this region northeastward across Canada to Greenland in the Turonian Coniacian, and Santonian. \r\n\r\nThe Cretaceous formations are deformed into broad, shallow synclines in eastern North and South Dakota and in northeastern Nebraska. A west-trending anticline, the Sioux uplift, separates the synclines in southeastern South Dakota. Sparse evidence of minor faulting in the formations exists in northeastern South Dakota, along the strike of a major southwest-trending zone of tectonism in the Precambrian basement rocks. The structural relief in the region, on the top of the Greenhorn Formation, is at least 250 m between eastern North Dakota and northeastern Minnesota, and at least 200 m between northeastern Nebraska and northwestern Iowa. \r\n\r\nA comparison of the Cretaceous stratigraphy of the Minnesota region and of areas in Wyoming indicates that some marine transgressions and regressions were synchronous in the two regions. The transgression during Greenhorn time, the regression during early Carlile time, and the transgression dur","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1253","usgsCitation":"Cobban, W.A., and Merewether, E., 1983, Stratigraphy and paleontology of Mid-Cretaceous rocks in Minnesota and contiguous areas: U.S. Geological Survey Professional Paper 1253, iv, 52 p., https://doi.org/10.3133/pp1253.","productDescription":"iv, 52 p.","costCenters":[],"links":[{"id":402556,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74506.htm","text":"Molluscan fossil record from the northeastern part of the Upper Cretaceous seaway, Western Interior","linkFileType":{"id":5,"text":"html"}},{"id":117719,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1253/report-thumb.jpg"},{"id":32482,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1253/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464249,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74507.htm","text":"Lower Upper Cretaceous strata in Minnesota and adjacent areas -- time-stratigraphic correlations and structural attitudes","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Iowa, Minnesota, Nebraska, North Dakota, South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.0859375,\n              41.902277040963696\n            ],\n            [\n              -94.921875,\n              42.09822241118974\n            ],\n            [\n              -90.703125,\n              43.51668853502906\n            ],\n            [\n              -92.63671875,\n              45.213003555993964\n            ],\n            [\n              -91.845703125,\n              46.86019101567027\n            ],\n            [\n              -89.56054687499999,\n              48.10743118848039\n            ],\n            [\n              -93.779296875,\n              48.69096039092549\n            ],\n            [\n              -94.921875,\n              48.922499263758255\n            ],\n            [\n              -94.74609375,\n              49.32512199104001\n            ],\n            [\n              -95.44921875,\n              49.15296965617042\n            ],\n            [\n              -99.140625,\n              48.980216985374994\n            ],\n            [\n              -98.0859375,\n              41.902277040963696\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a6e","contributors":{"authors":[{"text":"Cobban, William Aubrey","contributorId":78317,"corporation":false,"usgs":true,"family":"Cobban","given":"William","email":"","middleInitial":"Aubrey","affiliations":[],"preferred":false,"id":151598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merewether, E.A.","contributorId":32517,"corporation":false,"usgs":true,"family":"Merewether","given":"E.A.","affiliations":[],"preferred":false,"id":151597,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23793,"text":"ofr83207 - 1983 - Summary of water withdrawals in the United States, 1950-80","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr83207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-207","title":"Summary of water withdrawals in the United States, 1950-80","docAbstract":"Estimated use of water in the United States increased from 180 bgd (billion gallons per day) in 1950 to 450 bgd in 1980. During this same time population increased from about 150 million to about 230 million. Data on consumptive use are not available for the first decade of the period; however, from 1960 to 1980, consumptive use increased from 61 bgd to 100 bgd. \r\n\r\nFrom 1950 to 1980, fresh surface-water withdrawals increased from 140 bgd to 290 bgd and fresh ground-water withdrawals increased from 34 bgd to 88 bgd. Withdrawals of saline surface water increased from 10 bgd in 1950 to 71 bgd in 1980. In 1980, 91 percent of the saline surface water withdrawn was used in thermoelectric power plants. \r\n\r\nWithdrawals of water for domestic purposes nationwide increased from 16 bgd in 1960 to 25 bgd in 1980. The Northeastern States still are the largest users of water for domestic purposes; however, domestic withdrawals in that region declined from 9.6 bgd in 1975 to 8.8 bgd in 1980. Population in that region also showed a slight decline from 1970 to 1980. \r\n\r\nIrrigation withdrawals nationwide increased from 89 bgd in 1950 to 150 bgd in 1980. The Western States continue to be the largest user of irrigation water, 136 bgd in 1980. Irrigation accounted for 81 percent of the total consumptive use for the Nation in 1980. \r\n\r\nIndustrial withdrawals (exclusive of thermoelectric power generation) increased from 44 bgd in 1960 to about 56 bgd in 1980. The Northeast Region continues to withdraw the largest amount of water for industrial purposes, although withdrawals declined steadily from 33 bgd in 1965 to 27 bgd in 1980. \r\n\r\nTotal withdrawals for thermoelectric power generation increased from about 99 bgd in 1960 to about 210 bgd in 1980. During that period, saline surface water withdrawals increased from 26 bgd to 71 bgd. Thermoelectric plants accounted for 84 percent of saline surface water withdrawals in 1960 compared to 91 percent in 1980. Withdrawals for thermoelectric power generation continue to be the largest in the Northeast, ll3 bgd in 1980, where many of the major industrial and population centers are located. \r\n\r\nAgriculture (nonirrigation) water withdrawals nationwide increased from 1.6 bgd in 1960 to about 2.2 bgd in 1980. Withdrawals for this purpose in 1980 were about evenly divided between the West and East.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83207","issn":"0094-9140","usgsCitation":"Mann, W., Solley, W.B., and Chase, E.B., 1983, Summary of water withdrawals in the United States, 1950-80: U.S. Geological Survey Open-File Report 83-207, 22 p. ill., 1 map ;28 cm., https://doi.org/10.3133/ofr83207.","productDescription":"22 p. ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":156847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0207/report-thumb.jpg"},{"id":53015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4881e4b07f02db51670d","contributors":{"authors":[{"text":"Mann, William B.","contributorId":21985,"corporation":false,"usgs":true,"family":"Mann","given":"William B.","affiliations":[],"preferred":false,"id":190735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solley, Wayne B.","contributorId":61409,"corporation":false,"usgs":true,"family":"Solley","given":"Wayne","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7195,"text":"ofr83186 - 1983 - Geology report for proposed oil and gas lease sale No. 90; continental margin off the southeastern United States","interactions":[],"lastModifiedDate":"2022-12-01T20:16:31.213544","indexId":"ofr83186","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-186","title":"Geology report for proposed oil and gas lease sale No. 90; continental margin off the southeastern United States","docAbstract":"<p>This report summarizes our general knowledge of the geology and petroleum potential, as well as potential problems and hazards associated with development of petroleum resources, within the area proposed for nominations for lease sale number 90. This area includes the U.S. eastern continental margin from Raleigh Bay, just south of Cape Hatteras, to southern Florida, including the upper Continental Slope and inner Blake Plateau. The area for possible sales for lease sale number 90, as well as the area for lease sale number 78 and the previous areas leased are shown in figure 1; physiographic features of the region are shown in figure 2. </p><p>Six exploration wells have been drilled within the proposed lease area (figs. 3 and 4), but no commercial discoveries have been made. All six wells were drilled on the Continental Shelf. No commercial production has been obtained onshore in the region. The areas already drilled have thin sedimentary rock sections, and the deeper strata are dominantly of continental facies. Petroleum formation may have been hindered by a lack of organic material and lack of sufficient burial for thermal maturation. However, analyses of drilling and seismic profiling data presented here indicate that a much thicker section of sedimentary rocks containing a much higher proportion of marine deposits, exists seaward of the Continental Shelf. These geologic conditions imply that the basins farther offshore may be more favorable environments for generating petroleum.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83186","usgsCitation":"Dillon, W.P., 1983, Geology report for proposed oil and gas lease sale No. 90; continental margin off the southeastern United States: U.S. Geological Survey Open-File Report 83-186, Report: 125 p.; 2 Plates: 8.10 x 10.88 inches and 10.80 x 13.29 inches, https://doi.org/10.3133/ofr83186.","productDescription":"Report: 125 p.; 2 Plates: 8.10 x 10.88 inches and 10.80 x 13.29 inches","costCenters":[{"id":132,"text":"Atlantic Marine Geology","active":false,"usgs":true}],"links":[{"id":34584,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0186/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":34583,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0186/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":34585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0186/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":409945,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13929.htm","linkFileType":{"id":5,"text":"html"}},{"id":140159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0186/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.50357992821841,\n              29.56282563875409\n            ],\n            [\n              -76.99516298385373,\n              29.56282563875409\n            ],\n            [\n              -76.99516298385373,\n              34.177210082895485\n            ],\n            [\n              -81.50357992821841,\n              34.177210082895485\n            ],\n            [\n              -81.50357992821841,\n              29.56282563875409\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6e5","contributors":{"authors":[{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":154708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7237,"text":"ofr82679 - 1983 - Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia","interactions":[],"lastModifiedDate":"2024-09-24T18:08:13.417331","indexId":"ofr82679","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-679","title":"Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82679","usgsCitation":"May, V., 1983, Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia: U.S. Geological Survey Open-File Report 82-679, vi, 92 p., https://doi.org/10.3133/ofr82679.","productDescription":"vi, 92 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":94755,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0679/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":462210,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13802.htm","linkFileType":{"id":5,"text":"html"}},{"id":139837,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0679/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia, Tennessee","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.15478515625,\n              34.38877925439021\n            ],\n            [\n              -86.15478515625,\n              35.8356283888737\n            ],\n            [\n              -84.869384765625,\n              35.8356283888737\n            ],\n            [\n              -84.869384765625,\n              34.38877925439021\n            ],\n            [\n              -86.15478515625,\n              34.38877925439021\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604430","contributors":{"authors":[{"text":"May, V.J.","contributorId":71539,"corporation":false,"usgs":true,"family":"May","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":154863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44178,"text":"ofr83593 - 1983 - Multichannel seismic-reflection profiles collected in 1979 in the eastern Pacific Ocean off the California coast, south of Pt. Conception","interactions":[],"lastModifiedDate":"2021-11-30T19:16:03.016894","indexId":"ofr83593","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-593","title":"Multichannel seismic-reflection profiles collected in 1979 in the eastern Pacific Ocean off the California coast, south of Pt. Conception","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83593","usgsCitation":"Mann, D.M., and Crouch, J.K., 1983, Multichannel seismic-reflection profiles collected in 1979 in the eastern Pacific Ocean off the California coast, south of Pt. Conception: U.S. Geological Survey Open-File Report 83-593, Report: 3  p.; 1 Plate: 40.54 × 28.58 inches, https://doi.org/10.3133/ofr83593.","productDescription":"Report: 3  p.; 1 Plate: 40.54 × 28.58 inches","costCenters":[],"links":[{"id":392251,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14120.htm"},{"id":81573,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0593/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81574,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0593/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0593/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Pacific Ocean, Point Conception","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.167,\n              31.167\n            ],\n            [\n              -117.833,\n              31.167\n            ],\n            [\n              -117.833,\n              33.667\n            ],\n            [\n              -120.167,\n              33.667\n            ],\n            [\n              -120.167,\n              31.167\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b02","contributors":{"authors":[{"text":"Mann, Dennis M.","contributorId":50528,"corporation":false,"usgs":true,"family":"Mann","given":"Dennis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":229286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crouch, James K.","contributorId":56645,"corporation":false,"usgs":true,"family":"Crouch","given":"James","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":229287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25009,"text":"pp1241E - 1983 - Correlation chart for Precambrian rocks of the Eastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"pp1241E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1241","chapter":"E","title":"Correlation chart for Precambrian rocks of the Eastern United States","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1241E","usgsCitation":"Rankin, D., Stern, T.W., McLelland, J., Zartman, R., and Odom, A., 1983, Correlation chart for Precambrian rocks of the Eastern United States: U.S. Geological Survey Professional Paper 1241, 33 p.;  1 plate in pocket, https://doi.org/10.3133/pp1241E.","productDescription":"33 p.;  1 plate in pocket","costCenters":[],"links":[{"id":104579,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4764.htm","linkFileType":{"id":5,"text":"html"},"description":"4764"},{"id":118821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1241e/report-thumb.jpg"},{"id":54008,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1241e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54009,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1241e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54010,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1241e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684716","contributors":{"authors":[{"text":"Rankin, Douglas W. dwrankin@usgs.gov","contributorId":1770,"corporation":false,"usgs":true,"family":"Rankin","given":"Douglas W.","email":"dwrankin@usgs.gov","affiliations":[],"preferred":true,"id":193021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stern, T. W.","contributorId":36122,"corporation":false,"usgs":true,"family":"Stern","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193024,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McLelland, James","contributorId":28271,"corporation":false,"usgs":true,"family":"McLelland","given":"James","email":"","affiliations":[],"preferred":false,"id":193023,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":193022,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Odom, A.L.","contributorId":106935,"corporation":false,"usgs":true,"family":"Odom","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":193025,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7937,"text":"ofr83440 - 1983 - Central and Eastern United States; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-440","title":"Central and Eastern United States; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83440","usgsCitation":"Bliss, J.D., 1983, Central and Eastern United States; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-440, iv, 87 p.  ;28 cm., https://doi.org/10.3133/ofr83440.","productDescription":"iv, 87 p.  ;28 cm.","costCenters":[],"links":[{"id":140806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0440/report-thumb.jpg"},{"id":35508,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0440/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6e35","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156865,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11271,"text":"ofr83123 - 1983 - General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr83123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-123","title":"General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data","docAbstract":"Two satellite systems launched by the National Aeronautics and Space Administration (NASA) in 1978 carried sensors which operated in the thermal infrared (IR) region of the electromagnetic spectrum, The final IR radiation data provide spectral information about the physical properties of the Earth's surficial materials not duplicated in either the visible or reflective IR wavelength regions. Landsat 3, launched on March 5, 1978, contained a thermal sensor as part of the multispectral scanner (MSS) system. The sensor operated in the 10.4- to 12.6-?m (band 8) wavelength region and produced imagery with a ground resolution of approximately 235 m. \r\n\r\nLaunched on April 26) 1978) the Heat Capacity Mapping Mission (HCMM) spacecraft carried a sensor, the heat capacity mapping radiometer (HCMR) which operated in the 10.5- to 12.5?m wavelength region and produced imagery with a ground resolution of approximately 600 m at nadir. The HCMM satellite acquired over 6,600 data passes of visible (0.55-1.1 ?m), as well as thermal IR data, over North America, Europe, and Australia. \r\n\r\nGeneral characteristics and availability of Landsat 3 and HCMM thermal IR data are discussed. Landsat 3 reflected IR band 7 (0.55-1.1 ?m) and Landsat 3 band 8 thermal data acquired over the eastern and western United States are analyzed and compared with HCMM visible, thermal IR, thermal inertia, and day-night temperature difference imagery for geologic applications. Digitally processed and enhanced HCMM data (high-pass filters, diagonal derivatives, and band ratios), produced by the U.S. Geological Survey, Flagstaff) Ariz., are presented for geologic interpretation.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83123","usgsCitation":"Southworth, C.S., 1983, General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data: U.S. Geological Survey Open-File Report 83-123, 30 p. maps (some col.) ;28 cm., https://doi.org/10.3133/ofr83123.","productDescription":"30 p. maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":142961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0123/report-thumb.jpg"},{"id":39063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec45","contributors":{"authors":[{"text":"Southworth, C. Scott 0000-0002-7976-7807 ssouthwo@usgs.gov","orcid":"https://orcid.org/0000-0002-7976-7807","contributorId":1608,"corporation":false,"usgs":true,"family":"Southworth","given":"C.","email":"ssouthwo@usgs.gov","middleInitial":"Scott","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":162841,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25978,"text":"wri824084 - 1983 - Geohydrology of the Meadowbrook artificial-recharge site at East Meadow, Nassau County, New York","interactions":[],"lastModifiedDate":"2023-01-04T20:51:39.419276","indexId":"wri824084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4084","title":"Geohydrology of the Meadowbrook artificial-recharge site at East Meadow, Nassau County, New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824084","usgsCitation":"Aronson, D.A., Lindner-Lunsford, J.B., and Katz, B., 1983, Geohydrology of the Meadowbrook artificial-recharge site at East Meadow, Nassau County, New York: U.S. Geological Survey Water-Resources Investigations Report 82-4084, vi, 44 p., https://doi.org/10.3133/wri824084.","productDescription":"vi, 44 p.","costCenters":[],"links":[{"id":54732,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121856,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4084/report-thumb.jpg"},{"id":411381,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35595.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"East Meadow","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.56278176511351,\n              40.79270194265632\n            ],\n            [\n              -73.56278176511351,\n              40.68814281175551\n            ],\n            [\n              -73.45373266539764,\n              40.68814281175551\n            ],\n            [\n              -73.45373266539764,\n              40.79270194265632\n            ],\n            [\n              -73.56278176511351,\n              40.79270194265632\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8926","contributors":{"authors":[{"text":"Aronson, D. A.","contributorId":20308,"corporation":false,"usgs":true,"family":"Aronson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindner-Lunsford, J. B.","contributorId":81938,"corporation":false,"usgs":true,"family":"Lindner-Lunsford","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":195577,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Katz, B. G.","contributorId":82702,"corporation":false,"usgs":true,"family":"Katz","given":"B. G.","affiliations":[],"preferred":false,"id":195578,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8287,"text":"ofr83187 - 1983 - Zinc, lead, and barite deposits and occurrences in Paleozoic rocks, east-central United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr83187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-187","title":"Zinc, lead, and barite deposits and occurrences in Paleozoic rocks, east-central United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83187","usgsCitation":"Clark, S.H., and Neeley, C.L., 1983, Zinc, lead, and barite deposits and occurrences in Paleozoic rocks, east-central United States: U.S. Geological Survey Open-File Report 83-187, 81 p. map ;28 cm., https://doi.org/10.3133/ofr83187.","productDescription":"81 p. map ;28 cm.","costCenters":[],"links":[{"id":140753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0187/report-thumb.jpg"},{"id":35897,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35898,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5ddeba","contributors":{"authors":[{"text":"Clark, Sandra H.","contributorId":40986,"corporation":false,"usgs":true,"family":"Clark","given":"Sandra","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neeley, Cathy L.","contributorId":47365,"corporation":false,"usgs":true,"family":"Neeley","given":"Cathy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25970,"text":"wri834242 - 1983 - Evaluation of the effects of Lake Audubon on ground- and surface-water levels in the Lake Nettie area, eastern McLean County, North Dakota","interactions":[],"lastModifiedDate":"2022-02-16T21:12:51.329822","indexId":"wri834242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4242","title":"Evaluation of the effects of Lake Audubon on ground- and surface-water levels in the Lake Nettie area, eastern McLean County, North Dakota","docAbstract":"<p>Water logging and flooding of some roads and agricultural lands have become a problem in the Lake Nettie area of eastern McLean County. Part of the flooding is caused by the raising of Lake Audubon about 13 feet from an elevation of about 1,835 feet to 1,848 feet and its effect on ground-water levels in the upper unit of the Lake Nettie aquifer by way of leakage from the lower unit. The major part of the flooding is caused by the greater than normal precipitation and the resulting runoff. </p><p>Recharge to the aquifer is from the direct infiltration of precipitation and snowmelt, the lateral percolation of water from the adjacent Fort Union Formation and glacial-drift aquifers, and from Lake Audubon. Discharge is by evapotranspiration and by ground-water movement into undrained surface-water basins in the Lake Holmes-Lake Williams area and southward through Lake Ordway or westward to Lake Audubon. </p><p>Trends shown on hydrographs indicate that near equilibrium between recharge and discharge has been reestablished in the lower unit of the Lake Nettie aquifer in the area between Lake Audubon and Lake Nettie, but east of Lake Nettie water levels are still rising. As of 1982, water-level rises caused by the raising of Lake Audubon are as much as 4 feet in the lower unit of the Lake Nettie aquifer and are between 1 and 2 feet in the upper unit of the Lake Nettie aquifer, which is hydraulically connected to Lake Nettie, Crooked Lake, and Slough No. 1. There is a rise in Slough No. 1, about 2 miles east of Lake Audubon, that can be attributed to the higher levels of Lake Audubon. Apparently rises also have occurred in many other sloughs. </p><p>Water levels have risen in the Turtle Lake aquifer both as a result of raising the water level in Lake Audubon to an elevation of about 1,848 feet and the McClusky Canal to an elevation of about 1,844 feet. Water levels have risen as much as 6 feet near the canal, but generally less than 1 foot at distances of about 0.5 mile.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834242","usgsCitation":"Armstrong, C.A., 1983, Evaluation of the effects of Lake Audubon on ground- and surface-water levels in the Lake Nettie area, eastern McLean County, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 83-4242, iv, 41 p., https://doi.org/10.3133/wri834242.","productDescription":"iv, 41 p.","numberOfPages":"45","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":396042,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49181.htm"},{"id":54716,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4242/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4242/report-thumb.jpg"}],"country":"United States","state":"North Dakota","county":"McLean County","otherGeospatial":"Lake Nettie area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -101.0833,\n              47.5\n            ],\n            [\n              -100.75,\n              47.5\n            ],\n            [\n              -100.75,\n              47.6667\n            ],\n            [\n              -101.0833,\n              47.6667\n            ],\n            [\n              -101.0833,\n              47.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa49f","contributors":{"authors":[{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8802,"text":"ofr83686 - 1983 - Ground-water quality data for Oklahoma, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83686","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-686","title":"Ground-water quality data for Oklahoma, 1981","docAbstract":"The U.S. Geological Survey has collected data on Oklahoma's ground-water resources since 1934. Most of these data were collected as part of specific ground-water studies conducted in cooperation with various Federal, State, and local agencies. Ground-water quality data, as well as data on construction, yield, water levels, and other physical well parameters collected prior to 1981 are available from the U.S. Geological Survey, Oklahoma District Office.\r\nAlthough water-quality data for wells, test holes, and springs have been published, they are scattered though a variety of reports and are not readily available on a statewide basis. The purpose of this report is to make available, annually, all of the ground-water quality data collected by the U.S. Geological Survey in the Sate of Oklahoma. This report contains ground-water quality data collected in 1981 from 524 sites in 15 counties, predominately in eastern Oklahoma.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83686","usgsCitation":"Ferree, D.M., 1983, Ground-water quality data for Oklahoma, 1981: U.S. Geological Survey Open-File Report 83-686, iv, 81 p. ill. ;28 cm., https://doi.org/10.3133/ofr83686.","productDescription":"iv, 81 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0686/report-thumb.jpg"},{"id":36384,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0686/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66732f","contributors":{"authors":[{"text":"Ferree, Dale M.","contributorId":96690,"corporation":false,"usgs":true,"family":"Ferree","given":"Dale","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":158355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9403,"text":"ofr82568 - 1983 - Instructions for using the U.S. Geological Survey data base of wells on Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82568","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-568","title":"Instructions for using the U.S. Geological Survey data base of wells on Long Island, New York","docAbstract":"The population of central and eastern Long Island, New York depends on ground water for its supply of fresh water. Data on more than 7,500 wells on the island have been collected by various State and local agencies and compiled by the U.S. Geological Survey since 1906. During 1975-81, the Geological Survey developed a data base for its Data General Nova 1220 minicomputer to store and process the well information. The data base is composed of seven sections, each of which may be revised and updated. Three types of magnetic devices with limited capacity are used for data storage--disk, Linctape, and 9-track tape. This breakdown makes each section small enough to store and update on a small minicomputer while allowing simultaneous data retrieval from all sections. This manual gives complete instructions for revising, storing, and retrieving well data. Most programming is in FORTRAN, but some is in assembly language. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82568","usgsCitation":"Hawkins, G.W., and Terlecki, G.M., 1983, Instructions for using the U.S. Geological Survey data base of wells on Long Island, New York: U.S. Geological Survey Open-File Report 82-568, 194 p. (in various pagings) :ill. ;28 cm., https://doi.org/10.3133/ofr82568.","productDescription":"194 p. (in various pagings) :ill. ;28 cm.","costCenters":[],"links":[{"id":142196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0568/report-thumb.jpg"},{"id":37116,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0568/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d6fe","contributors":{"authors":[{"text":"Hawkins, George W.","contributorId":42966,"corporation":false,"usgs":true,"family":"Hawkins","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terlecki, Gregory M.","contributorId":93910,"corporation":false,"usgs":true,"family":"Terlecki","given":"Gregory","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159625,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9421,"text":"ofr83172 - 1983 - Garnet peridotites from Williams kimberlites, north-central Montana, U.S.A","interactions":[],"lastModifiedDate":"2022-10-31T19:54:25.920382","indexId":"ofr83172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-172","title":"Garnet peridotites from Williams kimberlites, north-central Montana, U.S.A","docAbstract":"<p>Two Williams kimberlites, 250x350m and 37x390m, in the eastern part of a swarm of 30 middle Eocene alnoitic diatremes in north-central Montana, USA, contain xenoliths of garnet-bearing lherzolites, harzburgites and dunites, in addition to spinel peridotites and upper and lower crustal amphibolites and granulites. Colluvial purple, red, and pink garnets are dominantly Mg- and Cr-rich, indicating their derivation From peridotites or megacrysts, and have CaO and Cr<sub>2</sub>O<sub>3</sub> contents that fall in the lherzolite trend. </p><p>Temperatures were calculated by the Lindsley-Dixon 20 kb method for lherzolites and by the O'Neill-Wood method for harzburgites and dunites, and pressures were calculated by the MacGregor method, or were assumed to be 50 kb for dunites. Most peridotites equilibrated at 1220-1350°C and 50-60 kb, well above a 44mW/m<sup>2</sup> shield geotherm and on or at higher P than the graphite-diamond boundary. Four lherzolites are low T-P (830-990°C, 23-42 kb) and are close to the shield geotherm. All four low T-P lherzolites have coarse textures whereas the high T-P cluster has both coarse and porphyroclastic textures, indicating a range of conditions of deformation and recrystallization in a restricted high T-P range. The tiny size (0.01-0.2 mm) of granulated and euhedral olivines in several xenoliths shows that deformation was occurring just prior to incorporation in kimberlite and that ascent was rapid enough (40-70 km/hr) to retard Further coarsening of fine-grained olivine. For other high T-P peridotites, cessation of deformation and beginning of recrystallization before or during inclusion in kimberlite is suggested by larger (up to 3mm) euhedral olivines in a matrix of fine granulated olivine or by optical continuity of large and nearby small olivines. </p><p>Two low T-P lherzolites contain distinctive, phlogopite-rimmed, 5-8mm clots of moderate-Cr garnet + Cr-spinel + Cr-diopside + enstatite that are inferred to have formed by reaction of an initial high-Cr garnet brought into the garnet + spinel stability Field. This suggests a reduction in pressure and temperature prior to inclusion in the kimberlite, followed by metasomatic introduction of phlogopite. These textural and compositional variations of peridotites seem most compatible with kimberlite generation and ascent during dynamic diapiric perturbation of the upper mantle.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83172","usgsCitation":"Hearn, B., and McGee, E.S., 1983, Garnet peridotites from Williams kimberlites, north-central Montana, U.S.A: U.S. Geological Survey Open-File Report 83-172, i, 26 p., https://doi.org/10.3133/ofr83172.","productDescription":"i, 26 p.","costCenters":[],"links":[{"id":408926,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13923.htm","linkFileType":{"id":5,"text":"html"}},{"id":37132,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0172/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0172/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.667,\n              47.867\n            ],\n            [\n              -108.667,\n              47.842\n            ],\n            [\n              -108.708,\n              47.842\n            ],\n            [\n              -108.708,\n              47.867\n            ],\n            [\n              -108.667,\n              47.867\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b135c","contributors":{"authors":[{"text":"Hearn, B.C.","contributorId":7700,"corporation":false,"usgs":true,"family":"Hearn","given":"B.C.","affiliations":[],"preferred":false,"id":159657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGee, E. S.","contributorId":75927,"corporation":false,"usgs":true,"family":"McGee","given":"E.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159658,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9477,"text":"ofr83359 - 1983 - Regional magnetic and gravity features of the Gibson Dome area and surrounding region, Paradox Basin, Utah: A preliminary report","interactions":[],"lastModifiedDate":"2022-02-22T22:13:46.493453","indexId":"ofr83359","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-359","title":"Regional magnetic and gravity features of the Gibson Dome area and surrounding region, Paradox Basin, Utah: A preliminary report","docAbstract":"Analyses of regional gravity and magnetic anomaly maps have been carried out to assist in the evaluation of the Gibson Dome area as a possible repository site for high-level radioactive waste. Derivative, wavelength-filtered, and trend maps were compiled to aid in properly locating major geophysical trends corresponding to faults, folds, and lithologic boundaries. The anomaly maps indicate that Paradox Basin is characterized by a heterogeneous Precambrian basement, essentially a metamorphic complex of gneisses and schist intruded by granitic rocks and mafic to ultramafic bodies. Interpreted Precambrian structures trend predominantly northwest and northeast although east-west trending features are evident. Prominent gravity lows define the salt anticlines. Structural and lithologic trends in the Gibson Dome area are closely examined. Of greatest interest is a series of circular magnetic highs trending west-northwest into the Gibson Dome area. Further study of the exact definition and geologic significance of this series of anomalies is warranted.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83359","usgsCitation":"Hildenbrand, T., and Kucks, R., 1983, Regional magnetic and gravity features of the Gibson Dome area and surrounding region, Paradox Basin, Utah: A preliminary report: U.S. Geological Survey Open-File Report 83-359, Report: 34 p.; 3 Plates: 32.79 × 40.67 inches or smaller, https://doi.org/10.3133/ofr83359.","productDescription":"Report: 34 p.; 3 Plates: 32.79 × 40.67 inches or smaller","costCenters":[],"links":[{"id":396292,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13996.htm"},{"id":37186,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0359/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37185,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0359/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37184,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0359/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37183,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0359/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0359/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Gibson Dome area, Paradox Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.7130,\n              37.388\n            ],\n            [\n              -108.617,\n              37.388\n            ],\n            [\n              -108.617,\n              39.045\n            ],\n            [\n              -110.7130,\n              39.045\n            ],\n            [\n              -110.7130,\n              37.388\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4ae","contributors":{"authors":[{"text":"Hildenbrand, T.G.","contributorId":83892,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":159757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kucks, R.P.","contributorId":53758,"corporation":false,"usgs":true,"family":"Kucks","given":"R.P.","affiliations":[],"preferred":false,"id":159756,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9544,"text":"ofr82440 - 1983 - Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama","interactions":[],"lastModifiedDate":"2024-09-23T22:12:54.319025","indexId":"ofr82440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-440","title":"Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82440","usgsCitation":"Hollyday, E., 1983, Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama: U.S. Geological Survey Open-File Report 82-440, v, 145 p., https://doi.org/10.3133/ofr82440.","productDescription":"v, 145 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":462159,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13725.htm","linkFileType":{"id":5,"text":"html"}},{"id":94931,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0440/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142669,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0440/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia, Tennessee","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.15478515625,\n              34.38877925439021\n            ],\n            [\n              -86.15478515625,\n              35.8356283888737\n            ],\n            [\n              -84.869384765625,\n              35.8356283888737\n            ],\n            [\n              -84.869384765625,\n              34.38877925439021\n            ],\n            [\n              -86.15478515625,\n              34.38877925439021\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d35","contributors":{"authors":[{"text":"Hollyday, E. F.","contributorId":95062,"corporation":false,"usgs":true,"family":"Hollyday","given":"E. F.","affiliations":[],"preferred":false,"id":159866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27380,"text":"wri811108 - 1983 - Ground-water resources in the Hood Basin, Oregon","interactions":[],"lastModifiedDate":"2016-10-21T10:33:36","indexId":"wri811108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-1108","title":"Ground-water resources in the Hood Basin, Oregon","docAbstract":"<p>The Hood Basin, an area of 1,035 square miles in north-central Oregon, includes the drainage basins of all tributaries of the Columbia River between Eagle Creek and Fifteenmile Creek. The physical characteristics and climate of the basin are diverse. The Wasco subarea, in the eastern half of the basin, has moderate relief, mostly intermittent streams, and semiarid climate. The Hood subarea, in the western half, has rugged topography, numerous perennial streams, and a humid climate.</p><p>Water-bearing geologic units that underlie the basin include volcanic, volcaniclastic, and sedimentary rocks of Miocene to Holocene age, and unconsolidated surficial deposits of Pleistocene and Holocene age. The most important water-bearing unit, the Columbia River Basalt Group, underlies almost the entire basin. Total thickness probably exceeds 2,000 feet, but by 1980 only the upper 1,000 feet or less had been developed by wells. Wells in this unit generally yield from 15 to 1,000 gallons per minute and a few yield as much as 3,300 gallons per minute.</p><p>The most productive aquifer in the Columbia River Basalt Group is The Dalles Ground Water Reservoir, a permeable zone of fractured basalt about 25 to 30 square miles in extent that underlies the city of The Dalles. During the late 1950's and mid-1960's, withdrawals of 15,000 acre-feet per year or more caused water levels in the aquifer to decline sharply. Pumpage had diminished to about 5,000 acre-feet per year in 1979 and water levels have stabilized, indicating that ground water recharge and discharge, including the pumping, are in balance.</p><p>The other principal geologic units in the basin have more limited areal distribution and less saturated thickness than the Columbia River Basalt Group. Generally, these units are capable of yielding from a few to a hundred gallons per minute to wells.</p><p>Most of the ground water in the basin is chemically suitable for domestic, irrigation, or other uses. Some ground water has objectionable concentrations of iron (0.3 to 6.4 milligrams per liter) and manganese (0.05 to 1.2 milligrams per liter) or is moderately hard to very hard (60 to 260 milligrams per liter as CaCO<sub>3</sub>).</p><p>The principal use of ground water in the Hood Basin is for irrigation of crops, with an estimated withdrawal of 7,700 acre-feet in 1979. Additional ground-water withdrawals in 1979 were estimated as: Industrial, 2,600 acre-feet; public supply, 2,100 acre-feet; and domestic and stock supply, 200 acre-feet.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri811108","collaboration":"Prepared in cooperation with Wasco and Hood River Counties","usgsCitation":"Grady, S.J., 1983, Ground-water resources in the Hood Basin, Oregon: U.S. Geological Survey Water-Resources Investigations Report 81-1108, Report: viii, 58 p.; 2 Plates: 36.05 x 37.78 inches and 30.57 x 37.96 inches, https://doi.org/10.3133/wri811108.","productDescription":"Report: viii, 58 p.; 2 Plates: 36.05 x 37.78 inches and 30.57 x 37.96 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":159039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri811108.JPG"},{"id":330293,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/1108/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330295,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/1108/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330294,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/1108/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Hood Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122,\n              45.733333\n            ],\n            [\n              -122,\n              45.5\n            ],\n            [\n              -120.875,\n              45.5\n            ],\n            [\n              -120.875,\n              45.733333\n            ],\n            [\n              -122,\n              45.733333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696dbb","contributors":{"authors":[{"text":"Grady, Stephen J.","contributorId":101636,"corporation":false,"usgs":true,"family":"Grady","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9931,"text":"ofr83592 - 1983 - Eastern Gulf of Alaska seismicity: Final report to the National Oceanic and Atmospheric Administration for July 1, 1975, through September 30, 1981","interactions":[],"lastModifiedDate":"2022-12-12T22:32:38.805937","indexId":"ofr83592","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-592","title":"Eastern Gulf of Alaska seismicity: Final report to the National Oceanic and Atmospheric Administration for July 1, 1975, through September 30, 1981","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83592","usgsCitation":"Lahr, J.C., and Stephens, C., 1983, Eastern Gulf of Alaska seismicity: Final report to the National Oceanic and Atmospheric Administration for July 1, 1975, through September 30, 1981: U.S. Geological Survey Open-File Report 83-592, 48 p., https://doi.org/10.3133/ofr83592.","productDescription":"48 p.","costCenters":[],"links":[{"id":410335,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14119.htm","linkFileType":{"id":5,"text":"html"}},{"id":37713,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0592/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0592/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"eastern Gulf of Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -136.50699581919312,\n              58.25683134476469\n            ],\n            [\n              -141.03281680066513,\n              59.80148318152371\n            ],\n            [\n              -145.59090741484098,\n              60.788650974736555\n            ],\n            [\n              -147.08261119524425,\n              61.00000324280887\n            ],\n            [\n              -145.7721746037704,\n              56.60939795810589\n            ],\n            [\n              -136.0653342871446,\n              56.852428007950806\n            ],\n            [\n              -136.50699581919312,\n              58.25683134476469\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db629522","contributors":{"authors":[{"text":"Lahr, John C.","contributorId":20328,"corporation":false,"usgs":true,"family":"Lahr","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160531,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, C.D.","contributorId":18752,"corporation":false,"usgs":true,"family":"Stephens","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":160530,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10000,"text":"ofr801049 - 1983 - Ground water in the northern part of Clackamas County, Oregon","interactions":[],"lastModifiedDate":"2022-08-26T20:47:39.65998","indexId":"ofr801049","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"80-1049","title":"Ground water in the northern part of Clackamas County, Oregon","docAbstract":"<p>Northern Clackamas County is part of the rapidly growing Portland metropolitan area. Population of this 250-square-mile area increased about 50 percent between 1970 and 1976. The study area includes a small segment of the Willamette River alluvial valley near Canby, and extends northward to the Clackamas River and eastward to the western boundary of Mount Hood National Forest. Also included is the narrow, well-populated corridor along U.S. Highway 26 from Cherryville to Government Camp.</p><p>The main part of the study area is largely a rolling upland underlain by volcanic and stream-deposited rocks ranging in age from Eocene to Holocene. In most places, these rocks yield water in quantities adequate for individual homes. Locally, ground-water supplies are adequate for small irrigation, industrial, or public-supply uses. Depths of wells range from 50 to 1,000 feet; wells generally are shallowest in lowlands near streams and deepest in upland locations near deeply incised stream valleys.</p><p>All aquifers receive recharge at sufficient rates to sustain present rates of natural and man-produced discharge. All aquifers could supply additional water, but careful engineering is needed to avoid overdevelopment problems for the Columbia River Basalt Group near Oregon City.</p><p>Chemical analyses indicate that the ground water in the study area is of good quality for drinking and other uses. Mineralized water reported from some wells northeast of Canby may be from rocks of the Skamania Volcanics, which locally are at shallow depth. Although ground water locally may be subject to bacterial contamination where it occurs at shallow depths in alluvium and other unconsolidated deposits, no contaminated water was identified during the study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801049","collaboration":"Prepared in cooperation with the Oregon Water Resources Department","usgsCitation":"Leonard, A., and Collins, C.A., 1983, Ground water in the northern part of Clackamas County, Oregon: U.S. Geological Survey Open-File Report 80-1049, Report: v, 85 p., 2 Plates: 34.53 x 24.34 inches and 34.96 x 24.88 inches, https://doi.org/10.3133/ofr801049.","productDescription":"Report: v, 85 p., 2 Plates: 34.53 x 24.34 inches and 34.96 x 24.88 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":405726,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1049/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405725,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1049/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1049/report-thumb.jpg"},{"id":405724,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Clackamas County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.76123046875,\n              45.01141864227728\n            ],\n            [\n              -121.84936523437499,\n              45.01141864227728\n            ],\n            [\n              -121.84936523437499,\n              45.45627757127799\n            ],\n            [\n              -122.76123046875,\n              45.45627757127799\n            ],\n            [\n              -122.76123046875,\n              45.01141864227728\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d750","contributors":{"authors":[{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":160652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, C. A.","contributorId":43731,"corporation":false,"usgs":true,"family":"Collins","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":160651,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10766,"text":"ofr82638 - 1983 - Hydrology of area 34, eastern region, interior coal province, Kentucky, Indiana and Illinois","interactions":[],"lastModifiedDate":"2022-07-13T00:18:36.408378","indexId":"ofr82638","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-638","title":"Hydrology of area 34, eastern region, interior coal province, Kentucky, Indiana and Illinois","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82638","usgsCitation":"Quinones, F., York, K.L., and Plebuch, R., 1983, Hydrology of area 34, eastern region, interior coal province, Kentucky, Indiana and Illinois: U.S. Geological Survey Open-File Report 82-638, v, 83 p., https://doi.org/10.3133/ofr82638.","productDescription":"v, 83 p.","costCenters":[],"links":[{"id":94993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0638/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0638/report-thumb.jpg"},{"id":403556,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13783.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Illinois, Indiana, Kentucky","otherGeospatial":"area 34, Eastern Region, Interior Coal Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.217,\n              36.818\n            ],\n            [\n              -85.6,\n              36.818\n            ],\n            [\n              -85.6,\n              38.018\n            ],\n            [\n              -88.217,\n              38.018\n            ],\n            [\n              -88.217,\n              36.818\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db60206e","contributors":{"authors":[{"text":"Quinones, F.","contributorId":93037,"corporation":false,"usgs":true,"family":"Quinones","given":"F.","email":"","affiliations":[],"preferred":false,"id":161928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"York, K. L.","contributorId":72384,"corporation":false,"usgs":true,"family":"York","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plebuch, R. O.","contributorId":29429,"corporation":false,"usgs":true,"family":"Plebuch","given":"R. O.","affiliations":[],"preferred":false,"id":161926,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10642,"text":"ofr8335 - 1983 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981","interactions":[],"lastModifiedDate":"2017-03-29T14:22:44","indexId":"ofr8335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-35","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981","docAbstract":"<p>Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin and Houston. Studies were completed in the Fort Worth metropolitan area at the end of the 1977 water year, and in the Dallas metropolitan area at the end of the 1979 water year. The study in the San Antonio area was completed at the end of the 1981 water year.</p><p>The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing streamflow network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data. The Texas Department of Water Resources ended its participation in the project in 1979, and the city of San Antonio funded the program through the 1981 water year.</p><p>The operation and maintenance of stations 08178000, San Antonio River at San Antonio; 08178700, Salado Creek (upper station) at San Antonio; and 08178800, Salado Creek (lower station) at San Antonio are funded by the city of San Antonio and the U.S Geological Survey.</p><p>The operation and maintenance and collection of water-quality data at station 08178720, Lorence Creek at Thousand Oaks Blvd., San Antonio, station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio, are funded by the Edwards Underground Water District in cooperation with the Texas Department of Hater Resources and the U.S. Geological Survey. Station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio will provide hydrologic data on similar and adjacent watersheds. The West Elm watershed is still predominately rural but is undergoing extensive urbanization in some areas. The East Elm watershed is relatively stable and undeveloped.</p><p>The objectives of the San Antonio urban hydrology study are:</p><ol><li>To provide data showing the effects of various stages of urbanization on flood discharge and runoff.</li><li>To provide water-quality data on surface-water runoff from floods of various magnitudes, during all seasons of the year from areas with different types of urban development.</li></ol><p>Annual publication of the San Antonio urban studies was initiated in 1969.</p><p>A definition of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in the U.S. Geological Survey's 1979 and 1980 \"Water resources data for Texas\" reports.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8335","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., 1983, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981: U.S. Geological Survey Open-File Report 83-35, v, 58 p., https://doi.org/10.3133/ofr8335.","productDescription":"v, 58 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0035/report.pdf","text":"Report","size":"1.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":144085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0035/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6078df","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":161728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10272,"text":"ofr83286 - 1983 - A hydrogeochemical survey in east-central Nevada","interactions":[],"lastModifiedDate":"2022-07-22T21:20:44.950179","indexId":"ofr83286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-286","title":"A hydrogeochemical survey in east-central Nevada","docAbstract":"A hydrogeochemical survey utilizing waters from springs and wells was conducted in east-central Nevada. None of the trace elements commonly associated with mineralization were found to be highly anomalous in the study area. Slightly anomalous values for some elements were found in the southern valleys of the study area and in a few scattered areas that contained old mines. Data from this study revealed no new areas of significant mineralization.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83286","usgsCitation":"McHugh, J., Miller, W.R., and Ficklin, W.H., 1983, A hydrogeochemical survey in east-central Nevada: U.S. Geological Survey Open-File Report 83-286, i, 28 p., https://doi.org/10.3133/ofr83286.","productDescription":"i, 28 p.","costCenters":[],"links":[{"id":404396,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13966.htm","linkFileType":{"id":5,"text":"html"}},{"id":38129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0286/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.49,\n              37.874\n            ],\n            [\n              -114,\n              37.874\n            ],\n            [\n              -114,\n              38.5\n            ],\n            [\n              -114.49,\n              38.5\n            ],\n            [\n              -114.49,\n              37.874\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae468","contributors":{"authors":[{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":161115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":161114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ficklin, Walter H.","contributorId":52565,"corporation":false,"usgs":true,"family":"Ficklin","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161113,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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