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,{"id":30048,"text":"wri824125 - 1983 - Mudflow hazards along the Toutle and Cowlitz Rivers from a hypothetical failure of Spirit Lake blockage","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri824125","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":"82-4125","title":"Mudflow hazards along the Toutle and Cowlitz Rivers from a hypothetical failure of Spirit Lake blockage","docAbstract":"The debris avalanche accompanying the May 18, 1980, eruption of Mount St. Helens, in southwestern Washington, buried the former outlet of Spirit Lake, located 5 miles north of the volcano, to a depth ranging to 500 feet. Since that time, Spirit Lake has had no natural outlet and its lake level and contents have increased significantly. Erosion at the crest of the debris dam on the surface of the blockage and recent studies of theblockage stratigraphy and soil properties showing that the effective crest elevation is lower than the surface crest have led to concern that the lake may someday breach through or spill over the top of the blockage. A study was made by the U.S. Geological Survey to determine the extent of inundation that might result downstream in the Toutle and Cowlitz Rivers if a hypothetical breach should occur and generate a mudflow flood of catastrophic proportions. A hypothetical breach of Spirit Lake produced a hypothetical mudflow hydrograph with a peak discharge of 2.65 million cu ft/s and a sediment concentration of 65 percent by volume at Camp Baker on the North Fork Toutle River. Elevations determined by the hydraulic routing of the mudflow were used to prepare inundation maps, indicating depths of inundation to be about 60 feet at Castle Rock and Lexington; 30-40 feet at Toutle, Toutle Lake at Silver Lake, Kelson, and Longview; and 15-20 feet at Toledo. Travel times for the peak elevation were estimated to be about 15 hours to Kid Valley on the North Fork Toutle River, 21 hours to Castle Rock, 22 hours to Toledo, and 23 hours to Kelso and Longview on the Cowlitz River. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824125","usgsCitation":"Swift, C., and Kresch, D., 1983, Mudflow hazards along the Toutle and Cowlitz Rivers from a hypothetical failure of Spirit Lake blockage: U.S. Geological Survey Water-Resources Investigations Report 82-4125, v, 15 p. :maps ;28 cm., https://doi.org/10.3133/wri824125.","productDescription":"v, 15 p. :maps ;28 cm.","costCenters":[],"links":[{"id":123441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4125/report-thumb.jpg"},{"id":58847,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58848,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58849,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58850,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58851,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58852,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58853,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58854,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58855,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58856,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58857,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b484e","contributors":{"authors":[{"text":"Swift, C.H.","contributorId":61821,"corporation":false,"usgs":true,"family":"Swift","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":202593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kresch, D. L.","contributorId":52559,"corporation":false,"usgs":true,"family":"Kresch","given":"D. L.","affiliations":[],"preferred":false,"id":202592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6245,"text":"pp1262 - 1983 - Origin and character of loesslike silt in unglaciated south-central Yakutia, Siberia, U.S.S.R.","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1262","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":"1262","title":"Origin and character of loesslike silt in unglaciated south-central Yakutia, Siberia, U.S.S.R.","docAbstract":"Loesslike silt mantles upland terraces and low plateaus throughout unglaciated south-central Yakutia but is thickest along the south side of the lower Aldan River valley and the east side of the Lena River valley. The silt is probably loess deposited during glacial advances by winds blowing southward from the Verkhoyansk Range and eastward across the broad vegetation-free flood plain of the braided Lena River. \r\n\r\nThe well-sorted uniform tan silt is well displayed along the Aldan and Lena Rivers; the thickest exposure measured, more than 60 m, is on the Tyungyulyu Terrace on the east side of the Lena River. On the west side of the valley, it is 10-25 m thick but thins rapidly to a featheredge west of Yakutsk. Almost all scarps along the south side of the Aldan River are capped by 10-35 m of silt. \r\n\r\nThe texture and mineral composition of the loess like silt are uniform throughout south-central Yakutia, whether it overlies limestone, poorly consolidated sandstone, alluvium, and glacial outwash. All silt samples examined contained a high percentage of quartz and feldspar. The silt stands in sheer cliffs and is massive, with little or no stratification. \r\n\r\nThe origin of the loesslike silt has been ascribed to disintegration in place of country rock by a marine, estuarine, lacustrine, fluvial, residual, or eolian source, or to a combination of these processes. The marine and estuarine hypotheses have never had strong support, but the lacustrine, fluvial, and residual hypotheses have been advanced by many Soviet workers. \r\n\r\nThe most widely accepted explanation of the origin of the upland silt is that it is a combination of lacustrine and alluvial deposits formed on great flood plains and marshy plains. This origin is unlikely, however, because there are no shorelines, wave-cut beaches, deltas, mudcracks, or ripple marks. Neither distinct stratification nor an appreciable amount of clay exists in the silt. Moreover, there is no definite upper boundary to the deposits, as would be expected of lacustrine deposits. \r\n\r\nThe loesslike silt has also been described as a residual deposit formed by the breakdown, by freezing and thawing, of the underlying rocks. The silt bears no chemical, mineralogic, or textural relation to the underlying strata, however, and it is too thick to represent only breakdown of rocks in place. \r\n\r\nThe widespread mantle of uniform loesslike silt is here considered to be windblown, derived from glacial outwash in braided streams and on broad plains, because: (1) it occurs as a surficial mantle; (2) it is lithologically independent of the underlying material; (3) it is stratified indistinctly or not at all, except in retransported material; (4) it is associated with sand dunes; (5) it contains fossils of land animals; (6) its sorting and texture are similar to that of loess and windblown dust from many places elsewhere in the world; (7) its grains are angular and relatively unweathered.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1262","usgsCitation":"Pewe, T.L., and Journaux, A., 1983, Origin and character of loesslike silt in unglaciated south-central Yakutia, Siberia, U.S.S.R.: U.S. Geological Survey Professional Paper 1262, 46 p., https://doi.org/10.3133/pp1262.","productDescription":"46 p.","costCenters":[],"links":[{"id":125041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1262/report-thumb.jpg"},{"id":33459,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a68b","contributors":{"authors":[{"text":"Pewe, Troy Lewis","contributorId":80654,"corporation":false,"usgs":true,"family":"Pewe","given":"Troy","email":"","middleInitial":"Lewis","affiliations":[],"preferred":false,"id":152375,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Journaux, Andre","contributorId":100838,"corporation":false,"usgs":true,"family":"Journaux","given":"Andre","email":"","affiliations":[],"preferred":false,"id":152376,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8134,"text":"ofr83180 - 1983 - Final report on the permeability of geopressured Gulf Coastal shale cores","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr83180","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":"83-180","title":"Final report on the permeability of geopressured Gulf Coastal shale cores","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83180","usgsCitation":"Byerlee, J., and Morrow, C., 1983, Final report on the permeability of geopressured Gulf Coastal shale cores: U.S. Geological Survey Open-File Report 83-180, 9 p. ill. ;28 cm., https://doi.org/10.3133/ofr83180.","productDescription":"9 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0180/report-thumb.jpg"},{"id":35738,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4707","contributors":{"authors":[{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":157204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morrow, C.A.","contributorId":99977,"corporation":false,"usgs":true,"family":"Morrow","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":157205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8034,"text":"ofr83549 - 1983 - Map showing coal deposits, oil and gas wells and seeps, and tar sandstone occurrences in the Basin and Range Provinces","interactions":[{"subject":{"id":8034,"text":"ofr83549 - 1983 - Map showing coal deposits, oil and gas wells and seeps, and tar sandstone occurrences in the Basin and Range Provinces","indexId":"ofr83549","publicationYear":"1983","noYear":false,"title":"Map showing coal deposits, oil and gas wells and seeps, and tar sandstone occurrences in the Basin and Range Provinces"},"predicate":"SUPERSEDED_BY","object":{"id":64813,"text":"i1522E - 1984 - Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences","indexId":"i1522E","publicationYear":"1984","noYear":false,"chapter":"E","title":"Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences"},"id":1}],"supersededBy":{"id":64813,"text":"i1522E - 1984 - Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences","indexId":"i1522E","publicationYear":"1984","noYear":false,"title":"Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences"},"lastModifiedDate":"2019-11-26T11:23:26","indexId":"ofr83549","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":"83-549","title":"Map showing coal deposits, oil and gas wells and seeps, and tar sandstone occurrences in the Basin and Range Provinces","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83549","usgsCitation":"Brady, B., 1983, Map showing coal deposits, oil and gas wells and seeps, and tar sandstone occurrences in the Basin and Range Provinces: U.S. Geological Survey Open-File Report 83-549, Report: vi, 92 p.; 1 Plate: 43.59 x 33.79 inches , https://doi.org/10.3133/ofr83549.","productDescription":"Report: vi, 92 p.; 1 Plate: 43.59 x 33.79 inches ","costCenters":[],"links":[{"id":369643,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0549/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140537,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0549/report-thumb.jpg"},{"id":369644,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0549/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659c56","contributors":{"authors":[{"text":"Brady, Bruce T.","contributorId":8059,"corporation":false,"usgs":true,"family":"Brady","given":"Bruce T.","affiliations":[],"preferred":false,"id":157024,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":8216,"text":"ofr83399 - 1983 - Sourcebook of locations of geophysical surveys in tunnels and horizontal holes including results of seismic-refraction surveys, Rainier Mesa, Aqueduct Mesa, and Area 16, Nevada Test Site","interactions":[],"lastModifiedDate":"2021-11-23T20:25:52.204531","indexId":"ofr83399","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":"83-399","title":"Sourcebook of locations of geophysical surveys in tunnels and horizontal holes including results of seismic-refraction surveys, Rainier Mesa, Aqueduct Mesa, and Area 16, Nevada Test Site","docAbstract":"<p>Seismic refraction surveys have been obtained sporadically in tunnels in zeolitized tuff at the Nevada Test Site since the late 1950's. Commencing in 1967 and continuing to date (1982), extensive measurements of shear- and compressional-wave velocities have been made in five tunnel complexes in Rainier and Aqueduct Mesas and in one tunnel complex in Shoshone Mountain. The results of these surveys to 1980 are compiled in this report. In addition, extensive horizontal drilling was initiated in 1967 in connection with geologic exploration in these tunnel complexes for sites for nuclear weapons tests. Seismic and electrical surveys were conducted in the majority of these holes. The type and location of these tunnel and borehole surveys are indexed in this report. Synthesis of the seismic refraction data indicates a mean compressional-wave velocity near the nuclear device point (WP) of 23 tunnel events of 2,430 m/s (7,970 f/s) with a range of 1,846-2,753 m/s (6,060-9,030 f/s). The mean shear-wave velocity of 17 tunnel events is 1,276 m/s (4,190 f/s) with a range of 1,140-1,392 m/s (3,740-4,570 f/s). Experience indicates that these velocity variations are due chiefly to the extent of fracturing and (or) the presence of partially saturated rock in the region of the survey.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83399","usgsCitation":"Carroll, R.D., and Kibler, J.E., 1983, Sourcebook of locations of geophysical surveys in tunnels and horizontal holes including results of seismic-refraction surveys, Rainier Mesa, Aqueduct Mesa, and Area 16, Nevada Test Site: U.S. Geological Survey Open-File Report 83-399, Report: iv, 85 p.; 12 Plates: 24.94 × 9.99 inches or smaller, https://doi.org/10.3133/ofr83399.","productDescription":"Report: iv, 85 p.; 12 Plates: 24.94 × 9.99 inches or smaller","costCenters":[],"links":[{"id":141557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0399/report-thumb.jpg"},{"id":35830,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35831,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35832,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35833,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35834,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35835,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35836,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35837,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35838,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35839,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35842,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0399/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392065,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14011.htm"},{"id":35840,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35841,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Aqueduct Mesa, Area 16, Nevada Test Site, Rainier Mesa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.25,\n              37\n            ],\n            [\n              -116,\n              37\n            ],\n            [\n              -116,\n              37.25\n            ],\n            [\n              -116.25,\n              37.25\n            ],\n            [\n              -116.25,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e76e6","contributors":{"authors":[{"text":"Carroll, R. 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,{"id":64694,"text":"i1424 - 1983 - Geologic map of the Freel Peak 15-minute Quadrangle, California and Nevada","interactions":[{"subject":{"id":41400,"text":"ofr801075 - 1980 - Preliminary geologic map of the Freel Peak 15-minute Quadrangle, California and Nevada","indexId":"ofr801075","publicationYear":"1980","noYear":false,"title":"Preliminary geologic map of the Freel Peak 15-minute Quadrangle, California and Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":64694,"text":"i1424 - 1983 - Geologic map of the Freel Peak 15-minute Quadrangle, California and Nevada","indexId":"i1424","publicationYear":"1983","noYear":false,"title":"Geologic map of the Freel Peak 15-minute Quadrangle, California and Nevada"},"id":1}],"lastModifiedDate":"2019-04-22T10:01:46","indexId":"i1424","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1424","title":"Geologic map of the Freel Peak 15-minute Quadrangle, California and Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1424","usgsCitation":"Armin, R.A., and John, D.A., 1983, Geologic map of the Freel Peak 15-minute Quadrangle, California and Nevada: U.S. Geological Survey IMAP 1424, 1 map :col ;45 x 34 cm., on sheet 81 x 108 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1424.","productDescription":"1 map :col ;45 x 34 cm., on sheet 81 x 108 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":187206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101798,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12.htm","linkFileType":{"id":5,"text":"html"},"description":"12"}],"scale":"62500","country":"United States","state":"California, Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,38.75 ], [ -120,39 ], [ -119.75,39 ], [ -119.75,38.75 ], [ -120,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698eff","contributors":{"authors":[{"text":"Armin, Richard A.","contributorId":43767,"corporation":false,"usgs":true,"family":"Armin","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":271993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"John, David A. 0000-0001-7977-9106 djohn@usgs.gov","orcid":"https://orcid.org/0000-0001-7977-9106","contributorId":1748,"corporation":false,"usgs":true,"family":"John","given":"David","email":"djohn@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":271992,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7435,"text":"ofr83300A - 1983 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: January 1983","interactions":[],"lastModifiedDate":"2024-05-06T20:10:56.271381","indexId":"ofr83300A","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":"83-300","chapter":"A","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: January 1983","docAbstract":"<p>The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83300A","usgsCitation":"Townshend, J.B., Papp, J., Sauter, E., Cunningham, T., and Torrence, L., 1983, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: January 1983: U.S. Geological Survey Open-File Report 83-300, 25 p., https://doi.org/10.3133/ofr83300A.","productDescription":"25 p.","costCenters":[],"links":[{"id":428448,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0300-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140371,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0300-a/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Fairbanks","otherGeospatial":"College Observatory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -147.9716829972995,\n              64.92275521538983\n            ],\n            [\n              -147.9716829972995,\n              64.77266196148724\n            ],\n            [\n              -147.4142995458633,\n              64.77266196148724\n            ],\n            [\n              -147.4142995458633,\n              64.92275521538983\n            ],\n            [\n              -147.9716829972995,\n              64.92275521538983\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673736","contributors":{"authors":[{"text":"Townshend, John B.","contributorId":70383,"corporation":false,"usgs":true,"family":"Townshend","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":155602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Papp, J.E.","contributorId":95057,"corporation":false,"usgs":true,"family":"Papp","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":155603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sauter, E.A.","contributorId":51738,"corporation":false,"usgs":true,"family":"Sauter","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":155600,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cunningham, T.K.","contributorId":103270,"corporation":false,"usgs":true,"family":"Cunningham","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":155604,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Torrence, L.Y.","contributorId":62587,"corporation":false,"usgs":true,"family":"Torrence","given":"L.Y.","email":"","affiliations":[],"preferred":false,"id":155601,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7515,"text":"ofr83197 - 1983 - Spectrographic analyses of stream-sediment samples from the Mazatzal Wilderness Area and Mazatzal Wilderness Contiguous Roadless Area, Gila, Maricopa, and Yavapai counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr83197","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":"83-197","title":"Spectrographic analyses of stream-sediment samples from the Mazatzal Wilderness Area and Mazatzal Wilderness Contiguous Roadless Area, Gila, Maricopa, and Yavapai counties, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83197","usgsCitation":"Marsh, S.P., Erickson, M.S., Forn, C., and McDougal, C.M., 1983, Spectrographic analyses of stream-sediment samples from the Mazatzal Wilderness Area and Mazatzal Wilderness Contiguous Roadless Area, Gila, Maricopa, and Yavapai counties, Arizona: U.S. Geological Survey Open-File Report 83-197, 38 p. maps ;28 cm., https://doi.org/10.3133/ofr83197.","productDescription":"38 p. maps ;28 cm.","costCenters":[],"links":[{"id":108447,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13933.htm","linkFileType":{"id":5,"text":"html"},"description":"13933"},{"id":141997,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0197/report-thumb.jpg"},{"id":34982,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0197/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34983,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0197/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4df6","contributors":{"authors":[{"text":"Marsh, Sherman P.","contributorId":42950,"corporation":false,"usgs":true,"family":"Marsh","given":"Sherman","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":155960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, M. S.","contributorId":35302,"corporation":false,"usgs":true,"family":"Erickson","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155959,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forn, C.L.","contributorId":46935,"corporation":false,"usgs":true,"family":"Forn","given":"C.L.","affiliations":[],"preferred":false,"id":155961,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDougal, C. M.","contributorId":21129,"corporation":false,"usgs":true,"family":"McDougal","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":155958,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":18480,"text":"ofr83540 - 1983 - Bibliography of U.S. Geological Survey reports on the water resources of Florida, 1886-1982","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr83540","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":"83-540","title":"Bibliography of U.S. Geological Survey reports on the water resources of Florida, 1886-1982","docAbstract":"The U.S. Geological Survey (USGS) has been making investigations of the water resources of Florida since the latter part of the 19th century. Early work consisted mainly of data collection at a few spring and river sites at intermittent intervals with the exception of a statewide groundwater study made during 1910-12. In 1930, an office was established for surface water studies in Florida and in 1938 for groundwater studies. Since 1930, practically all of the water resources investigations made by USGS have been in cooperation with State and local agencies. The third edition, ' Bibliography of U.S. Geological Survey Reports on the Water Resources of Florida, 1886-1982 ' includes reports approved for release in calendar years 1981 and 1982. In addition to updating the second edition (1981) several reports released prior to that time, which were inadvertently omitted, have been added. The bibliographic list of publications is arranged alphabetically by senior author. The publications are also indexed by geographic area and by subject. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83540","usgsCitation":"Claiborne, M., Nierstheimer, L., and Hoy, N., 1983, Bibliography of U.S. Geological Survey reports on the water resources of Florida, 1886-1982: U.S. Geological Survey Open-File Report 83-540, viii, 318 p. :map ;28 cm., https://doi.org/10.3133/ofr83540.","productDescription":"viii, 318 p. :map ;28 cm.","costCenters":[],"links":[{"id":153099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0540/report-thumb.jpg"},{"id":47837,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0540/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db628059","contributors":{"authors":[{"text":"Claiborne, Maude","contributorId":95061,"corporation":false,"usgs":true,"family":"Claiborne","given":"Maude","email":"","affiliations":[],"preferred":false,"id":179208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nierstheimer, L.O.","contributorId":13265,"corporation":false,"usgs":true,"family":"Nierstheimer","given":"L.O.","email":"","affiliations":[],"preferred":false,"id":179206,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoy, N.D.","contributorId":15618,"corporation":false,"usgs":true,"family":"Hoy","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":179207,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8051,"text":"ofr80594 - 1983 - Quality of rivers of the United States, 1976 water year--based on the National Stream Quality Accounting Network (NASQAN)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr80594","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":"80-594","title":"Quality of rivers of the United States, 1976 water year--based on the National Stream Quality Accounting Network (NASQAN)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80594","usgsCitation":"Britton, L.J., Goddard, K.E., and Briggs, J.C., 1983, Quality of rivers of the United States, 1976 water year--based on the National Stream Quality Accounting Network (NASQAN): U.S. Geological Survey Open-File Report 80-594, vi, 423 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr80594.","productDescription":"vi, 423 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":140578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0594/report-thumb.jpg"},{"id":35625,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0594/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654a3f","contributors":{"authors":[{"text":"Britton, Linda J.","contributorId":72780,"corporation":false,"usgs":true,"family":"Britton","given":"Linda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goddard, Kimball E.","contributorId":24348,"corporation":false,"usgs":true,"family":"Goddard","given":"Kimball","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157055,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briggs, John C.","contributorId":24349,"corporation":false,"usgs":true,"family":"Briggs","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":157056,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20611,"text":"ofr83589 - 1983 - Helium concentrations in soil gas of the Ely and Delta 1° x 2° quadrangles, Basin and Range Province","interactions":[],"lastModifiedDate":"2021-11-08T20:04:27.672949","indexId":"ofr83589","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":"83-589","title":"Helium concentrations in soil gas of the Ely and Delta 1° x 2° quadrangles, Basin and Range Province","docAbstract":"A reconnaissance soil-gas helium survey was made of the Ely, Nevada and Delta, Utah 1? x 2? quadrangles in the Basin and Range Province. Helium concentrations in 510 samples ranged from -147 to 441 ppb He with respect to ambient air. The median helium value for the study area was 36 ppb. Concentrations of more than 100 ppb He, and less than -20 ppb He, occur more commonly in the Ely Quadrangle and are especially numerous in the western one-half of this quadrangle. The data are presented both in figures and tables, and some of the geologic factors that may affect the helium distribution are discussed.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83589","usgsCitation":"Reimer, G., and Bowles, C., 1983, Helium concentrations in soil gas of the Ely and Delta 1° x 2° quadrangles, Basin and Range Province: U.S. Geological Survey Open-File Report 83-589, Report: 25 p.; 2 Plates: 33.65 × 20.69 inches and 34.38 × 21.07 inches, https://doi.org/10.3133/ofr83589.","productDescription":"Report: 25 p.; 2 Plates: 33.65 × 20.69 inches and 34.38 × 21.07 inches","costCenters":[],"links":[{"id":391476,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14116.htm"},{"id":50136,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0589/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0589/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50137,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0589/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0589/report-thumb.jpg"}],"country":"United States","state":"Nevada, Utah","otherGeospatial":"Ely and Delta 1° x 2° quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116,\n              39\n            ],\n            [\n              -112,\n              39\n            ],\n            [\n              -112,\n              40\n            ],\n            [\n              -116,\n              40\n            ],\n            [\n              -116,\n              39\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635dac","contributors":{"authors":[{"text":"Reimer, G.M.","contributorId":59800,"corporation":false,"usgs":true,"family":"Reimer","given":"G.M.","affiliations":[],"preferred":false,"id":182934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowles, C.G.","contributorId":14369,"corporation":false,"usgs":true,"family":"Bowles","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":182933,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20476,"text":"ofr83871 - 1983 - Selected hydrologic data, Kolob-Alton-Kaiparowits coal-fields area, south-central Utah","interactions":[],"lastModifiedDate":"2024-01-11T20:20:06.523467","indexId":"ofr83871","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":"83-871","title":"Selected hydrologic data, Kolob-Alton-Kaiparowits coal-fields area, south-central Utah","docAbstract":"<p>The Kolob-Alton-Kaiparowits coal-field area (pi. 1) includes about 4,500 square miles in parts of the Colorado River Basin and the Great Basin. The area varies in altitude from less than 4,000 to more than 10,000 feet, and is comprised chiefly of plateaus, benches, and terraces that are dissected by deep, narrow canyons. Principal streams draining the area are the Virgin, Sevier, Escalante, and Paria Rivers, and Coal, Kanab, and Wahweap Creeks.</p><p>Most of the data included in this report were collected by the U.S. Geological Survey from October 1980 to September 1982. They were collected as part of a hydrologic study in cooperation with the U.S. Bureau of Land Management to evaluate potential impacts of coal mining on the area's water resources. The results of that study are to be published in a separate report.</p><p>Several earlier coal-related hydrologic studies have been made in the Alton and Kolob coal-fields area. Hydrologic data collected during those studies may be found in the following reports: Goode (1964, 1966), Sandberg (1979), and Cordova (1981). Data collected at the streamflow-gaging stations shown on plate 1 are published separately in annual reports of the U.S. Geological Survey. Information about the availability of these data is given in table 8.</p><p>The writer extends thanks to Judy Steiger and Dave Darby (former employees of the U.S. Geological Survey) for their contribution to this report. Officials of the following companies and agencies also were helpful and cooperative in providing data: Utah Power &amp; Light Co.; El Paso Natural Gas Co.; U.S. Bureau of Reclamation; and U.S. Bureau of Land Management.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr83871","collaboration":"Prepared in cooperation with th U.S. Bureau of Land Management","usgsCitation":"Plantz, G.G., 1983, Selected hydrologic data, Kolob-Alton-Kaiparowits coal-fields area, south-central Utah: U.S. Geological Survey Open-File Report 83-871, Report: iv, 25 p.; 1 Plate: 34.00 x 21.68 inches, https://doi.org/10.3133/ofr83871.","productDescription":"Report: iv, 25 p.; 1 Plate: 34.00 x 21.68 inches","numberOfPages":"29","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":424340,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14257.htm","linkFileType":{"id":5,"text":"html"}},{"id":50010,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0871/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50011,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0871/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152163,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0871/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Kolob-Alton-Kaiparowits coal-fields area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.1419,\n              37.972\n            ],\n            [\n              -113.1419,\n              37.026\n            ],\n            [\n              -110.949,\n              37.026\n            ],\n            [\n              -110.949,\n              37.972\n            ],\n            [\n              -113.1419,\n              37.972\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f94ca","contributors":{"authors":[{"text":"Plantz, Gerald G.","contributorId":96149,"corporation":false,"usgs":true,"family":"Plantz","given":"Gerald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":182715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20461,"text":"ofr83818 - 1983 - Comparison of abundances of chemical elements in mineralized and unmineralized sandstone of the Brushy Basin Member of the Morrison Formation, Smith Lake District, Grants uranium region, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr83818","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":"83-818","title":"Comparison of abundances of chemical elements in mineralized and unmineralized sandstone of the Brushy Basin Member of the Morrison Formation, Smith Lake District, Grants uranium region, New Mexico","docAbstract":"Statistical treatment of analytical data from the Mariano Lake and Ruby uranium deposits in the Smith Lake district, New Mexico, indicates that organic carbon, arsenic, barium, calcium, cobalt, copper, gallium, iron, lead, manganese, molybdenum, nickel, selenium, strontium, sulfur, vanadium, yttrium, and zirconium are concentrated along with uranium in primary ore. Comparison of the Smith Lake data with information from other primary deposits in the Grants uranium region and elsewhere in the Morrison Formation of the Colorado Plateau suggests that these elements, with the possible exceptions of zirconium and gallium and with the probable addition of aluminum and magnesium, are typically associated with primary, tabular uranium deposits. Chemical differences between the Ruby and Mariano Lake deposits are consistent with the interpretation that the Ruby deposit has been more affected by post-mineralization oxidizing solutions than has the Mariano Lake deposit.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83818","usgsCitation":"Pierson, C.T., Spirakis, C., and Robertson, J., 1983, Comparison of abundances of chemical elements in mineralized and unmineralized sandstone of the Brushy Basin Member of the Morrison Formation, Smith Lake District, Grants uranium region, New Mexico: U.S. Geological Survey Open-File Report 83-818, 47 p. :ill. ;28 cm., https://doi.org/10.3133/ofr83818.","productDescription":"47 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0818/report-thumb.jpg"},{"id":50002,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0818/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d489","contributors":{"authors":[{"text":"Pierson, C. T.","contributorId":57055,"corporation":false,"usgs":true,"family":"Pierson","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":182696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spirakis, C.S.","contributorId":46088,"corporation":false,"usgs":true,"family":"Spirakis","given":"C.S.","affiliations":[],"preferred":false,"id":182695,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robertson, J. F.","contributorId":11194,"corporation":false,"usgs":true,"family":"Robertson","given":"J. F.","affiliations":[],"preferred":false,"id":182694,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7181,"text":"ofr83672 - 1983 - Geological and geochemical studies in the Wadi Bidah District, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr83672","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":"83-672","title":"Geological and geochemical studies in the Wadi Bidah District, Kingdom of Saudi Arabia","docAbstract":"Geological and geochemical followup studies of airborne electromagnetic anomalies in the Wadi Bidah district, southwestern Saudi Arabia, did not reveal metals of economic grade. \r\n\r\nInvestigation of an anomaly enclosing the Rabathan ancient mine disclosed tightly folded and sheared Proterozoic tuffaceous rocks interlayered mostly with chert, dolomite, carbonaceous rocks, and volcanic wacke including cherty iron-manganese formations slightly anomalous in copper and zinc. Three drill holes placed to test anomalies within these formations yielded negative results. \r\n\r\nStudies of a long, narrow anomaly north of the Rabathan area indicated a similar geological environment. This northern area also contains limited zones that are highly anomalous in copper and zinc and extensive zones that are slightly anomalous in those metals. Drilling was not undertaken in this area. \r\n\r\nThe Bilajimah airborne electromagnetic anomaly west of Wadi Bidah coincides with a broad synclinorium of layered felsic turfs and gossans. Geochemical studies indicated slightly anomalous copper, zinc, and silver values in gossans within the anomaly area. Two drill holes intersected carbonaceous rock that contained approximately 15 percent pyrrhotite and traces of sphalerite and chalcopyrite. \r\n\r\nTwo geophysically anomalous areas west of Wadi Bidah surround ancient mines at Mahawiyah and Khayal al Masna'ah. Results of geochemical sampling at these workings were positive. An airborne electromagnetic anomaly located in the Assifar area in the southwestern corner of the Wadi Bidah district is underlain principally by metasedimentary rocks that include large linear zones of cherty iron-manganese formation and a few gossans .containing secondary base metal minerals.\r\n\r\nDetailed mapping and sampling of the Mulhal ancient mine, located west of Wadi Bidah, revealed two types of polymetallic gossans : (1) stratiform deposits interlayered with ignimbrites and mafic volcanic rocks and (2) barite-bearing gossanous material in shear zones that grade into hydrothermally altered shear zones and extend beyond the mine area. The gossans and gossanous shear zones contain anomalous amounts of gold, silver, lead, copper, zinc, barium, and selenium. \r\n\r\nTwo gossans west of Wadi Bidah were mapped and sampled in detail; both gossans are interlayered, with siliceous volcanic rocks. Although the gossan at Jabal Mohr covers a large area, it contains low amounts of precious and base metals. The gossan at Mulhal No. 2 contains moderate to high amounts of gold, silver, copper, lead, and zinc.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83672","usgsCitation":"Smith, C.W., Waters, B., Naqvi, M., Worl, R.G., Helaby, A., Flanigan, V.J., Sadek, H., and Samater, R., 1983, Geological and geochemical studies in the Wadi Bidah District, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-672, v, 101 p., 6 over-size sheets, ill., maps ;1983., https://doi.org/10.3133/ofr83672.","productDescription":"v, 101 p., 6 over-size sheets, ill., maps ;1983.","costCenters":[],"links":[{"id":142103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0672/report-thumb.jpg"},{"id":34537,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34538,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0672/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34532,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34533,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34534,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34535,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34536,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876b4","contributors":{"authors":[{"text":"Smith, C. W.","contributorId":57457,"corporation":false,"usgs":true,"family":"Smith","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":154648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waters, B.C.","contributorId":87412,"corporation":false,"usgs":true,"family":"Waters","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":154653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Naqvi, M.","contributorId":84210,"corporation":false,"usgs":true,"family":"Naqvi","given":"M.","email":"","affiliations":[],"preferred":false,"id":154652,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Worl, R. G.","contributorId":13984,"corporation":false,"usgs":true,"family":"Worl","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":154647,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Helaby, A. M.","contributorId":64241,"corporation":false,"usgs":true,"family":"Helaby","given":"A. M.","affiliations":[],"preferred":false,"id":154649,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Flanigan, V. J.","contributorId":81097,"corporation":false,"usgs":true,"family":"Flanigan","given":"V.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154650,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sadek, H.S.","contributorId":93915,"corporation":false,"usgs":true,"family":"Sadek","given":"H.S.","affiliations":[],"preferred":false,"id":154654,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Samater, R.M.","contributorId":82694,"corporation":false,"usgs":true,"family":"Samater","given":"R.M.","affiliations":[],"preferred":false,"id":154651,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":36424,"text":"fwsobs83_30 - 1983 - Marine birds of the southeastern United States and the Gulf of Mexico. Part III, Charadriiformes","interactions":[],"lastModifiedDate":"2012-02-02T00:09:28","indexId":"fwsobs83_30","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"83/30","title":"Marine birds of the southeastern United States and the Gulf of Mexico. Part III, Charadriiformes","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Clapp, R.B., Morgan-Jacobs, D., and Banks, R.C., 1983, Marine birds of the southeastern United States and the Gulf of Mexico. Part III, Charadriiformes: FWS/OBS 83/30, 3 v. : ill., maps; 28 cm.","productDescription":"3 v. : ill., maps; 28 cm.","costCenters":[],"links":[{"id":163066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606477","contributors":{"authors":[{"text":"Clapp, Roger B.","contributorId":12904,"corporation":false,"usgs":true,"family":"Clapp","given":"Roger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":216297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan-Jacobs, Deborah","contributorId":16069,"corporation":false,"usgs":true,"family":"Morgan-Jacobs","given":"Deborah","email":"","affiliations":[],"preferred":false,"id":216298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Banks, Richard C.","contributorId":102933,"corporation":false,"usgs":true,"family":"Banks","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68747,"text":"oc122 - 1983 - Stratigraphic sections of middle Jurassic Entrada sandstone and related rocks from Dewey Bridge, Utah, to Bridgeport, Colorado","interactions":[],"lastModifiedDate":"2019-11-15T17:14:20","indexId":"oc122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"122","title":"Stratigraphic sections of middle Jurassic Entrada sandstone and related rocks from Dewey Bridge, Utah, to Bridgeport, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/oc122","usgsCitation":"O'Sullivan, R., and Pipiringos, G., 1983, Stratigraphic sections of middle Jurassic Entrada sandstone and related rocks from Dewey Bridge, Utah, to Bridgeport, Colorado: U.S. Geological Survey Oil and Gas Investigation Chart 122, Map: 41.67 x 30.75 inches, https://doi.org/10.3133/oc122.","productDescription":"Map: 41.67 x 30.75 inches","costCenters":[],"links":[{"id":104781,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5149.htm","linkFileType":{"id":5,"text":"html"},"description":"5149"},{"id":188259,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"300000","country":"United States","state":"Colorado, Utah","city":"Bridgeport, Colorado, Dewey Bridge, Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.2917,\n              38.7500\n            ],\n            [\n              -108.2917,\n              38.7500\n            ],\n            [\n              -108.2917,\n              39.2500\n            ],\n            [\n              -109.2917,\n              39.2500\n            ],\n            [\n              -109.2917,\n              38.7500\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae582","contributors":{"authors":[{"text":"O'Sullivan, Robert Brett","contributorId":26695,"corporation":false,"usgs":true,"family":"O'Sullivan","given":"Robert Brett","affiliations":[],"preferred":false,"id":278869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pipiringos, G. N.","contributorId":11210,"corporation":false,"usgs":true,"family":"Pipiringos","given":"G. N.","affiliations":[],"preferred":false,"id":278868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9649,"text":"ofr83584 - 1983 - Principal facts for 382 gravity stations in Lassen Volcanic National Park and vicinity, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr83584","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":"83-584","title":"Principal facts for 382 gravity stations in Lassen Volcanic National Park and vicinity, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83584","usgsCitation":"Jachens, R.C., Spydell, D., and Saltus, R.W., 1983, Principal facts for 382 gravity stations in Lassen Volcanic National Park and vicinity, California: U.S. Geological Survey Open-File Report 83-584, 14 p. ;28 cm., https://doi.org/10.3133/ofr83584.","productDescription":"14 p. ;28 cm.","costCenters":[],"links":[{"id":140937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0584/report-thumb.jpg"},{"id":37379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0584/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668cb3","contributors":{"authors":[{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":160050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spydell, D.R.","contributorId":86764,"corporation":false,"usgs":true,"family":"Spydell","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":160052,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Saltus, R. W.","contributorId":85588,"corporation":false,"usgs":true,"family":"Saltus","given":"R.","middleInitial":"W.","affiliations":[],"preferred":false,"id":160051,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26426,"text":"wri834064 - 1983 - Sediment transport in the Tanana River near Fairbanks, Alaska, 1980-81","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri834064","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":"83-4064","title":"Sediment transport in the Tanana River near Fairbanks, Alaska, 1980-81","docAbstract":"Suspended-sediment- and bedload-transport rates for the Tanana River near Fairbanks, Alaska, can be related to water discharge. Annual sediment loads can be computed using these relations. For a site at Fairbanks, the annual loads in 1980 were 22.0 million metric tons of suspended sediment and 272,000 metric tons of bedload; in 1981, 27.3 million metric tons of suspended sediment and 333,000 metric tons of bedload passed the Fairbanks site. Data collected at five other locations within a 40 km reach of the river indicate very similar suspended-sediment transport relations, but bedload-transport relations vary from site to site and between 1980 and 1981. For all sites bedload is usually 1 to 1.5 percent of suspended-sediment load. Particle-size distribution for suspended sediment is similar at all six sites. Median particle size is generally in the silt range; only occasionally is it in the very fine sand range. Median particle size of bedload varied from the gravel range to the medium sand range for five of the six sampling sites in both years. At the sixth site, the most downstream location, median particle size of bedload was in the sand range. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834064","usgsCitation":"Burrows, R., and Harrold, P., 1983, Sediment transport in the Tanana River near Fairbanks, Alaska, 1980-81: U.S. Geological Survey Water-Resources Investigations Report 83-4064, vii, 122 p. :ill., map ;28 cm., https://doi.org/10.3133/wri834064.","productDescription":"vii, 122 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":110158,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35700.htm","linkFileType":{"id":5,"text":"html"},"description":"35700"},{"id":119134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_83_4064.jpg"},{"id":13747,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri83-4064/","linkFileType":{"id":5,"text":"html"}},{"id":55217,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4064/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55218,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4064/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbeaf","contributors":{"authors":[{"text":"Burrows, R.L.","contributorId":19977,"corporation":false,"usgs":true,"family":"Burrows","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":196368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrold, P.E.","contributorId":89935,"corporation":false,"usgs":true,"family":"Harrold","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":196369,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11094,"text":"ofr83594 - 1983 - Mineral resource potential of the southeast addition to the White Mountain Wilderness, Lincoln County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr83594","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":"83-594","title":"Mineral resource potential of the southeast addition to the White Mountain Wilderness, Lincoln County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83594","usgsCitation":"Segerstrom, K.K., Hladky, F.R., and Briggs, J.P., 1983, Mineral resource potential of the southeast addition to the White Mountain Wilderness, Lincoln County, New Mexico: U.S. Geological Survey Open-File Report 83-594, 11 p. maps ;28 cm., https://doi.org/10.3133/ofr83594.","productDescription":"11 p. maps ;28 cm.","costCenters":[],"links":[{"id":143139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0594/report-thumb.jpg"},{"id":38859,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0594/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c113","contributors":{"authors":[{"text":"Segerstrom, Kenneth K.","contributorId":105276,"corporation":false,"usgs":true,"family":"Segerstrom","given":"Kenneth","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":162525,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hladky, Frank R.","contributorId":19228,"corporation":false,"usgs":true,"family":"Hladky","given":"Frank","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":162524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briggs, John P.","contributorId":9397,"corporation":false,"usgs":true,"family":"Briggs","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":162523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29423,"text":"wri824022 - 1983 - Quality of ground water in southern Buchanan County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri824022","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":"82-4022","title":"Quality of ground water in southern Buchanan County, Virginia","docAbstract":"In seven small contiguous stream basins in the coal area of southwest Virginia, ground water is predominantly bicarbonate in anion composition, with calcium as the major cation in the ridges and sodium the major cation in the lower altitudes. Sulfate is the major anion in water associated with coal seams and in stream waters draining areas extensively disturbed by mining activities. Water found along a major linear feature in the Big Prater Creek valley and water from deep wells in Levisa Fork basin contain chloride as the predominant anion. Hydrogen ion activities (pH) in the ground water range from 5.2 to 8.4. Iron concentrations as high as 14,000 micrograms per liter are present in domestic wells. The chemical composition of most streams changes with diminishing discharge and at baseflow is similar to the composition of local ground water. At high flows, streams draining mined areas are enriched with sulfate. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824022","usgsCitation":"Rogers, S.M., and Powell, J.D., 1983, Quality of ground water in southern Buchanan County, Virginia: U.S. Geological Survey Water-Resources Investigations Report 82-4022, vi, 32 p. :ill., maps.; 12 over-size sheets, scale 1:48,000, https://doi.org/10.3133/wri824022.","productDescription":"vi, 32 p. :ill., maps.; 12 over-size sheets, scale 1:48,000","costCenters":[],"links":[{"id":159705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4022/report-thumb.jpg"},{"id":58269,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4022/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654b0a","contributors":{"authors":[{"text":"Rogers, Stanley M.","contributorId":37761,"corporation":false,"usgs":true,"family":"Rogers","given":"Stanley","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, John D.","contributorId":6045,"corporation":false,"usgs":true,"family":"Powell","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":201504,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20288,"text":"ofr83750 - 1983 - In situ geomechanics of crystalline and sedimentary rocks; Part IV, continued field testing of the modified U.S. Geological Survey 3-D borehole stress probe","interactions":[],"lastModifiedDate":"2012-02-02T00:07:37","indexId":"ofr83750","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":"83-750","title":"In situ geomechanics of crystalline and sedimentary rocks; Part IV, continued field testing of the modified U.S. Geological Survey 3-D borehole stress probe","docAbstract":"Two modified and calibrated U.S. Geological Survey 3-D borehole probes were successfully tested in the field at a site on South Table Mountain, near Golden, Colo. The probes were installed in separate core holes at depths of 84 and 99 cm in the latite cap rock and subsequently stress relieved with overcoring techniques. The determined stresses from both probes are very low and contain both tensile and compressive components. Magnitudes range from 1196 KPa in tension to 832 KPa in compression. The principal stress orientations are in fair agreement whereas the horizontal secondary principal stress directions are in good agreement; the maximum horizontal compressive stress is oriented N. 76? W.-S. 76? E. for one probe and N. 63? W.-S. 63? E. for the second probe. The greatest determined Young's modulus of the rock is in the N. 89? E. direction, only 15? from the maximum horizontal compressive stress direction.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83750","usgsCitation":"Nichols, T.C., 1983, In situ geomechanics of crystalline and sedimentary rocks; Part IV, continued field testing of the modified U.S. Geological Survey 3-D borehole stress probe: U.S. Geological Survey Open-File Report 83-750, ii, 14 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83750.","productDescription":"ii, 14 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":152310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0750/report-thumb.jpg"},{"id":49822,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0750/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5ac1","contributors":{"authors":[{"text":"Nichols, Thomas C.","contributorId":65843,"corporation":false,"usgs":true,"family":"Nichols","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":182390,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20237,"text":"ofr83771 - 1983 - Test wells T21, T22, and T25, White Sands Missile Range, Dona Ana County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr83771","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":"83-771","title":"Test wells T21, T22, and T25, White Sands Missile Range, Dona Ana County, New Mexico","docAbstract":"Three test wells, T21, T22, and T25, were drilled at White Sands Missile Range in south-central New Mexico as part of a joint military program sponsored by the U.S. Army in September 1982. T21 and T22 were drilled as observation wells for two old landfills. T25 was drilled as an exploratory hole to obtain lithologic and borehole-geophysical data in the vicinity of the proposed replacement well for Supply Well 15. Information obtained from these wells includes borehole-geophysical and driller's logs.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83771","usgsCitation":"Myers, R.G., 1983, Test wells T21, T22, and T25, White Sands Missile Range, Dona Ana County, New Mexico: U.S. Geological Survey Open-File Report 83-771, iv, 37 p. :ill. ;28 cm., https://doi.org/10.3133/ofr83771.","productDescription":"iv, 37 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0771/report-thumb.jpg"},{"id":49778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0771/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684b56","contributors":{"authors":[{"text":"Myers, R. G.","contributorId":30642,"corporation":false,"usgs":true,"family":"Myers","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":182302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36527,"text":"fwsobs82_11_1 - 1983 - Species Profiles: Life histories and environmental requirements (Gulf of Mexico): Brown shrimp","interactions":[],"lastModifiedDate":"2022-02-15T14:24:38.364138","indexId":"fwsobs82_11_1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/11.1","title":"Species Profiles: Life histories and environmental requirements (Gulf of Mexico): Brown shrimp","docAbstract":"Species profiles are literature summaries on the taxonomy, morphology, range, life history, and environmental requirements of coastal aquatic species. They are designed to assist in environmental impact assessment. The brown shrimp, Penaeus aztecus, is the major species in the Gulf of Mexico shrimp fishery, the most valuable $302 million in 1980) commercial fishery in the United States. It is heavily preyed on by many fishes. Spawning occurs offshore from about September to May and most postlarvae move into estuaries from February through April. Within the estuary they occupy shallow water near marshes with soft substrate. Juveniles emigrate from estuaries to offshore areas from May through August. They grow as fast as 3.3 mm per day in estuaries. Adults concentrate around the 55-m contour offshore. Postlarval and juvenile shrimp are normal1y taken in water temperatures above 10?C and rapid growth occurs above 18?C. Few shrimp are collected below 5 ppt salinity. Brown shrimp are benthic feeders and prefer soft substrates. High populatiorls are associated with coastal marshes.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Lassuy, D.R., 1983, Species Profiles: Life histories and environmental requirements (Gulf of Mexico): Brown shrimp: FWS/OBS 82/11.1, 21 p.","productDescription":"21 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":167274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e41","contributors":{"authors":[{"text":"Lassuy, Dennis R.","contributorId":19616,"corporation":false,"usgs":true,"family":"Lassuy","given":"Dennis","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":216473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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