{"pageNumber":"5070","pageRowStart":"126725","pageSize":"25","recordCount":165549,"records":[{"id":7305,"text":"ofr791663 - 1979 - Measured sections of Ordovician strata in northeast Kentucky","interactions":[],"lastModifiedDate":"2024-06-07T18:29:50.87976","indexId":"ofr791663","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1663","title":"Measured sections of Ordovician strata in northeast Kentucky","docAbstract":"

The sections described in this report are part of the data used in studies of the Upper Ordovician rocks of Kentucky. The studies were part of a geologic mapping program by the U. S. Geological Survey in cooperation with the Kentucky Geological Survey. Formations of Late Ordovician age described in this report are the Drakes, Bull Fork, Grant Lake, Fairview, and Kope.

Most sections were measured in the field with Jacob staff and tape. Color names with numbers are based on comparison with the rock chart by Goddard and others (1948). The core described is on file at the core library of the Kentucky Geological Survey in Lexington, Kentucky.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791663","collaboration":"Prepared in cooperation with the Kentucky Geological Survey","usgsCitation":"Weir, G.W., Peterson, W.L., and Swadley, W.C., 1979, Measured sections of Ordovician strata in northeast Kentucky: U.S. Geological Survey Open-File Report 79-1663, i, 31 p., https://doi.org/10.3133/ofr791663.","productDescription":"i, 31 p.","costCenters":[],"links":[{"id":429665,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1663/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140593,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1663/report-thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"northeast Kentucky","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -84.37806941318598,\n 38.913753035461184\n ],\n [\n -84.37806941318598,\n 37.72642497446316\n ],\n [\n -83.26029427044637,\n 37.72642497446316\n ],\n [\n -83.26029427044637,\n 38.913753035461184\n ],\n [\n -84.37806941318598,\n 38.913753035461184\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610da6","contributors":{"authors":[{"text":"Weir, Gordon Whitney","contributorId":59790,"corporation":false,"usgs":true,"family":"Weir","given":"Gordon","email":"","middleInitial":"Whitney","affiliations":[],"preferred":false,"id":155147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, Warren Lee","contributorId":68303,"corporation":false,"usgs":true,"family":"Peterson","given":"Warren","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":155148,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":155146,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7306,"text":"ofr791317 - 1979 - Measured stratigraphic sections of Jurassic San Rafael Group and adjacent rocks in Emery and Sevier counties, Utah","interactions":[],"lastModifiedDate":"2023-11-21T23:04:02.963599","indexId":"ofr791317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1317","title":"Measured stratigraphic sections of Jurassic San Rafael Group and adjacent rocks in Emery and Sevier counties, Utah","docAbstract":"

These sections were measured prior to 1960, before adoption of the metric system. Publication was delayed by other assignments of the authors and later by the untimely death of J. C. Wright. They are being released at this time because of the increased interest in the uranium potential of Jurassic rocks. The Curtis, Summerville, Entrada, and Carmel Formations are the formations of the San Rafael Group in these sections.


","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791317","usgsCitation":"Wright, J., Dickey, D., Snyder, R., Craig, L., and Cadigan, R.A., 1979, Measured stratigraphic sections of Jurassic San Rafael Group and adjacent rocks in Emery and Sevier counties, Utah: U.S. Geological Survey Open-File Report 79-1317, i, 157 p., https://doi.org/10.3133/ofr791317.","productDescription":"i, 157 p.","costCenters":[],"links":[{"id":422812,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1317/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140594,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1317/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Emery County, Sevier County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.5,38.5 ], [ -111.5,39 ], [ -111,39 ], [ -111,38.5 ], [ -111.5,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610f31","contributors":{"authors":[{"text":"Wright, J.C.","contributorId":79078,"corporation":false,"usgs":true,"family":"Wright","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":155153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickey, D.D.","contributorId":15612,"corporation":false,"usgs":true,"family":"Dickey","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":155150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snyder, R.P.","contributorId":9647,"corporation":false,"usgs":true,"family":"Snyder","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":155149,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Craig, L.C.","contributorId":61419,"corporation":false,"usgs":true,"family":"Craig","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":155152,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155151,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":7310,"text":"ofr79530 - 1979 - Metals in Devonian kerogenous marine strata at Gibellini and Bisoni properties in southern Fish Creek Range, Eureka County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr79530","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-530","title":"Metals in Devonian kerogenous marine strata at Gibellini and Bisoni properties in southern Fish Creek Range, Eureka County, Nevada","docAbstract":"A kerogen-rich sequence of siliceous mudstone, siltstone, and chert as much as 60 m thick on ridge 7129 in the southern Fish Creek Range, referred to as Gibellini facies of the Woodruff Formation, has been evaluated on the surface and in drill holes principally for its potential resources of vanadium, zinc, selenium, molybdenum, and syncrude oil content. The strata are part of a strongly deformed allochthonous mass of eugeosynclinal Devonian marine rocks that overlie deformed allochthonous Mississippian siliceous rocks and relatively undeformed autochthonous Mississippian Antler flysch at this locality. The vanadium in fresh black rocks obtained from drill holes and fresh exposures in trenches and roadcuts occurs chiefly in organic matter. Concentrations of vanadium oxide (V2O5) in unoxidized samples range from 3,000 to 7,000 ppm. In oxidized and bleached rock that is prevalent at the surface, concentrations of vanadium oxide range from 6,000 to 8,000 ppm, suggesting a tendency toward enrichment due to surficial weathering and ground-water movement. Zinc occurs in sphalerite, and selenium occurs in organic matter; molybdenum appears to occur both in molybdenite and in organic matter. Concentrations of zinc in unoxidized rock range from 4,000 to 18,000 ppm, whereas in oxidized rock they range from 30 to 100 ppm, showing strong depletion due to weathering. Concentrations of selenium in unoxidized rock range from 30 to 200 ppm, whereas in oxidized rock they range from 200 to 400 ppm, indicating some enrichment upon weathering. Concentrations of molybdenum in unoxidized rock range from 70 to 960 ppm, whereas in oxidized rock they range from 30 to 80 ppm, indicating strong depletion upon weathering. Most fresh black rock is low-grade oil shale, and yields as much as 12 gallons/short ton of syncrude oil. Metahewettite is the principal vanadium mineral in the oxidized zone, but it also occurs sparsely as small nodules and fillings of microfractures in unweathered strata. In fresh rock, bluish-white opaline-like silica (chalcedonic quartz) fills microfractures, and is believed to have originated by diagenetic mobilization of opaline silica from radiolarian tests and sponge spicules. \r\n\r\nAs revealed by microscopic study, the Gibellini facies originally consisted of siliceous muds, slimes, and oozes high in organic constituents. The organic matter is amorphous flaky and stringy sapropel, and probably includes remains of bacteria, phytoplankton, zooplankton, and minor higher plants. Recognizable organic remnants include radiolarian tests, sponge spicules, conodonts, brachiopod shells, algae, and humic debris. Diagnostic radiolarians indicate a Late Devonian age for the Gibellini facies of the Woodruff Formation. Some pyrite is disseminated through the rock and may be primary (syngenetic) but significant pyrite and marcasite occur in chalcedonic quartz veinlets and appear to be diagenetic. In fresh rock, black solid bitumen and liquid oil fill voids and microfractures. These early phase hydrocarbons probably were released during diagenesis from complex nonhydrocarbon molecular structures originating from living organisms, and formed without any major thermal degradation of the kerogen. Gas chromatographic analysis of the saturated hydrocarbon fraction indicates a very complex mixture dominated by branched and cyclic compounds. Conodont and palynomorph color alteration, vitrinite reflectance, and other organic geochemical data suggest that the organic matter in the rock is thermally immature and has not been subjected to temperatures greater than 60?C since deposition in Devonian time. All of these characteristics are consistent with the interpretation of a relatively low temperature and a shallow-burial history for the Gibellini facies on ridge 7129.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79530","usgsCitation":"Desborough, G.A., Poole, F.G., Hose, R.K., and Radtke, A.S., 1979, Metals in Devonian kerogenous marine strata at Gibellini and Bisoni properties in southern Fish Creek Range, Eureka County, Nevada: U.S. Geological Survey Open-File Report 79-530, iii, 35 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr79530.","productDescription":"iii, 35 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0530/report-thumb.jpg"},{"id":34700,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0530/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db62875c","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poole, F. G. 0000-0001-8487-0799","orcid":"https://orcid.org/0000-0001-8487-0799","contributorId":104883,"corporation":false,"usgs":true,"family":"Poole","given":"F.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":155169,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hose, R. K.","contributorId":63388,"corporation":false,"usgs":true,"family":"Hose","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":155167,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Radtke, A. S.","contributorId":16408,"corporation":false,"usgs":true,"family":"Radtke","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155166,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5706,"text":"pp941B - 1979 - Seismic safety and land-use planning; selected examples from California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"pp941B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"941","chapter":"B","title":"Seismic safety and land-use planning; selected examples from California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp941B","usgsCitation":"Blair, M.L., and Spangle, W.E., 1979, Seismic safety and land-use planning; selected examples from California: U.S. Geological Survey Professional Paper 941, 81 p., https://doi.org/10.3133/pp941B.","productDescription":"81 p.","costCenters":[],"links":[{"id":121681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0941b/report-thumb.jpg"},{"id":32275,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0941b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c4f","contributors":{"authors":[{"text":"Blair, M. L.","contributorId":59789,"corporation":false,"usgs":true,"family":"Blair","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":151464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spangle, W. E.","contributorId":10793,"corporation":false,"usgs":true,"family":"Spangle","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":151463,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7840,"text":"ofr791330 - 1979 - Sediment deposition in the White River Reservoir, northwestern Wisconsin","interactions":[{"subject":{"id":7840,"text":"ofr791330 - 1979 - Sediment deposition in the White River Reservoir, northwestern Wisconsin","indexId":"ofr791330","publicationYear":"1979","noYear":false,"title":"Sediment deposition in the White River Reservoir, northwestern Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":999,"text":"wsp2069 - 1980 - Sediment deposition in the White River Reservoir, northwestern Wisconsin","indexId":"wsp2069","publicationYear":"1980","noYear":false,"title":"Sediment deposition in the White River Reservoir, northwestern Wisconsin"},"id":1}],"supersededBy":{"id":999,"text":"wsp2069 - 1980 - Sediment deposition in the White River Reservoir, northwestern Wisconsin","indexId":"wsp2069","publicationYear":"1980","noYear":false,"title":"Sediment deposition in the White River Reservoir, northwestern Wisconsin"},"lastModifiedDate":"2015-10-13T14:17:39","indexId":"ofr791330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1330","title":"Sediment deposition in the White River Reservoir, northwestern Wisconsin","docAbstract":"

The history of deposition in the White River Reservoir was reconstructed from a study of sediment in the reservoir. Suspended-sediment concentrations, particle size, and streamflow characteristics were measured at gaging stations upstream and downstream from the reservoir from November 1975 through September 1977- Characteristics of the sediments were determined from borings and samples taken while the reservoir was drained in September 1976. The sediment surface and the prereservoir topography were mapped. Sediment thickness ranged from less than 1 foot near the shore to more than 20 feet in the old stream channel.

\n

The original reservoir capacity and volume of deposited sediment were calculated to be 815 acre-feet and 487 acre-feet, respectively.

\n

Sediment size ranged from clay and silt in the pool area to large cobbles and boulders at the upstream end of the reservoir. Analyses of all samples averaged 43 percent sand, 40 percent silt, and 17 percent clay, and particle size typically increased upstream. Cobbles, boulders, and gravel deposits were not sampled. The average density of the deposited sediments was about 80 pounds per cubic foot for the entire reservoir.

\n

The reservoir was able to trap about 80 percent of the sediment entering from upstream early in its history. This trap efficiency has declined as the reservoir filled with sediment. Today (1976) it traps only sand and silt-sized sediment, or only about 20 percent of the sediment entering from upstream. Data collected during this study indicate that essentially all of the clay-sized sediment (<0.062 mm) passes through the reservoir.

\n

The gross rate of deposition was 7.0 acre-feet per year over the reservoir history, 1907-76. Rates during 1907-63 and 1963-76 were 7.4 and 5.7 acre-feet per year, respectively, determined by the Cesium-137 method.

\n

Based on scant data, the average annual sediment yield of the total 279 square mile drainage area above the gaging station at the powerplant was about 50 tons per square mile. Analysis of the drainage-basin characteristics indicates that most of this sediment was derived from less than 10 percent of the total drainage area and from steep unvegetated streambanks.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791330","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Batten, W.G., and Hindall, S.M., 1979, Sediment deposition in the White River Reservoir, northwestern Wisconsin: U.S. Geological Survey Open-File Report 79-1330, Report: v, 34 p.; 1 Plate: 24.00 x 20.50 inches, https://doi.org/10.3133/ofr791330.","productDescription":"Report: v, 34 p.; 1 Plate: 24.00 x 20.50 inches","numberOfPages":"39","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":140552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1330/report-thumb.jpg"},{"id":110616,"rank":700,"type":{"id":15,"text":"Index 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W. G.","contributorId":89504,"corporation":false,"usgs":true,"family":"Batten","given":"W.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":156708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hindall, S. M.","contributorId":59414,"corporation":false,"usgs":true,"family":"Hindall","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156707,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6058,"text":"pp1136 - 1979 - Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","interactions":[{"subject":{"id":9682,"text":"ofr79270 - 1979 - Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","indexId":"ofr79270","publicationYear":"1979","noYear":false,"title":"Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":6058,"text":"pp1136 - 1979 - Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","indexId":"pp1136","publicationYear":"1979","noYear":false,"title":"Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia"},"id":1}],"lastModifiedDate":"2017-01-05T12:46:45","indexId":"pp1136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1136","title":"Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","docAbstract":"A coupled flow-temperature model has been developed and verified for a 27.9-km reach of the Chattahoochee River between Buford Dam and Norcross, Ga. Flow in this reach of the Chattahoochee is continuous but highly regulated by Buford Dam, a flood-control and hydroelectric facility located near Buford, Ga. Calibration and verification utilized two sets of data collected under highly unsteady discharge conditions. Existing solution techniques, with certain minor improvements, were applied to verify the existing technology of flow and transport modeling. \r\n\r\nThe linear, implicit finite-difference flow model was calibrated by use of a depth profile obtained at steady low flow and unsteady flow data obtained in March 1976. During the calibration period, the model was generally able to reproduce observed stages to within 0.15 m and discharges at less than 100 m 3 /s, to within 5 percent. Peak discharges of about 200 m 3 /s were under-estimated by about 20 percent. During the verification period, October 1975, the flow model reproduced observed stage changes to within about 0.15 m, and its timing and over-all performance was considered to be very good. \r\n\r\nDye was added to the upstream end of the river reach at a constant rate while the river flow was highly unsteady. The numerical solution of either the conservative or nonconservative form of the mass-transport equation did an excellent job of simulating the observed concentrations of dye in the river. \r\n\r\nThe temperature model was capable of predicting temperature changes through this reach of as large as 5.8?C with a RMS (root-mean-square) error of 0.32?C in October 1975 and 0.20?C in March 1976. \r\n\r\nHydropulsation has a significant effect on the water temperature below Buford Dam. These effects are very complicated because they are quite dependent on the timing of the release with respect to both the time of day and past releases.","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/pp1136","usgsCitation":"Jobson, H.E., and Keefer, T.N., 1979, Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia: U.S. Geological Survey Professional Paper 1136, 41 p., https://doi.org/10.3133/pp1136.","productDescription":"41 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":33058,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1136/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1136/report-thumb.jpg"}],"country":"United States","state":"Georgia","city":"Atlanta","otherGeospatial":"Chattahoochee 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California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"pp1137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1137","title":"Comprehensive monitoring of meteorology, hydraulics, and thermal regime of the San Diego Aqueduct, California","docAbstract":"Water temperature, as well as meteorologic and hydraulic variables which influence the energy budget of the San Diego Aqueduct in southern California, were continuously monitored for a 1-year period beginning July 24, 1973. Incoming solar and atmospheric radiation, windspeed and direction, water temperature, and wet- and dry-bulb air temperatures were recorded at 10-minute intervals at each end of the 26-kilometer concrete-lined canal, while flow-rates and stages were determined at hourly intervals for five locations. Although only daily averaged values are presented in this report, all information necessary for the use and interpretation of these data are presented. Windspeeds were minimum during the early morning hours and maximum during the late afternoon; however, they were variable spatially. On the other hand, incoming radiation and absolute vapor pressure varied little from point to point. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1137","usgsCitation":"Jobson, H.E., and Sturrock, A.M., 1979, Comprehensive monitoring of meteorology, hydraulics, and thermal regime of the San Diego Aqueduct, California: U.S. Geological Survey Professional Paper 1137, 29 p., https://doi.org/10.3133/pp1137.","productDescription":"29 p.","costCenters":[],"links":[{"id":123400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1137/report-thumb.jpg"},{"id":33057,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1137/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f8c","contributors":{"authors":[{"text":"Jobson, Harvey E.","contributorId":27032,"corporation":false,"usgs":true,"family":"Jobson","given":"Harvey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sturrock, Alex M.","contributorId":48948,"corporation":false,"usgs":true,"family":"Sturrock","given":"Alex","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7830,"text":"ofr79582 - 1979 - Age control for the latest movements on the Melones fault zone in the Sierra Nevada foothills belt from K-Ar dates for Late Tertiary intrusions","interactions":[],"lastModifiedDate":"2024-02-07T20:36:36.99903","indexId":"ofr79582","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-582","title":"Age control for the latest movements on the Melones fault zone in the Sierra Nevada foothills belt from K-Ar dates for Late Tertiary intrusions","docAbstract":"

K-Ar dates of 4.12 million years (m.y.) and 4.03 m.y. for two small dacite and rhyodacite intrusive bodies near Mokelumne Hill, Calif., provide important age control for the late Tertiary Mehrten Formation in this area because the Mehrten is both intruded by the dacite and rhyodacite and depositionally overlies the dacite of one intrusion. These dates also establish a maximum age for the latest movement on the Mother Lode fault, a part of the Melones fault zone, because the Mehrten Formation is displaced by this fault and because younger colluvium containing clasts from one of the intrusive bodies is in fault contact with the Mehrten.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79582","usgsCitation":"Bartow, J.A., 1979, Age control for the latest movements on the Melones fault zone in the Sierra Nevada foothills belt from K-Ar dates for Late Tertiary intrusions: U.S. Geological Survey Open-File Report 79-582, 10 p., https://doi.org/10.3133/ofr79582.","productDescription":"10 p.","costCenters":[],"links":[{"id":425478,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0582/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141964,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0582/report-thumb.jpg"}],"country":"United States","state":"California","city":"Mokelumne Hill","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.71737682671821,\n 38.304984481671994\n ],\n [\n -120.71737682671821,\n 38.29308764516935\n ],\n [\n -120.69017999343481,\n 38.29308764516935\n ],\n [\n -120.69017999343481,\n 38.304984481671994\n ],\n [\n -120.71737682671821,\n 38.304984481671994\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68966a","contributors":{"authors":[{"text":"Bartow, J. Alan","contributorId":84373,"corporation":false,"usgs":true,"family":"Bartow","given":"J.","email":"","middleInitial":"Alan","affiliations":[],"preferred":false,"id":156691,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6963,"text":"ofr79542 - 1979 - Analyses and description of geochemical samples, Dolly Sods Wilderness, Grant, Randolph, and Tucker Counties, West Virginia","interactions":[],"lastModifiedDate":"2022-08-23T21:47:56.848409","indexId":"ofr79542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-542","title":"Analyses and description of geochemical samples, Dolly Sods Wilderness, Grant, Randolph, and Tucker Counties, West Virginia","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79542","usgsCitation":"Motooka, J.M., Mei, L., Curtis, C.A., and Lesure, F., 1979, Analyses and description of geochemical samples, Dolly Sods Wilderness, Grant, Randolph, and Tucker Counties, West Virginia: U.S. Geological Survey Open-File Report 79-542, 19 p., https://doi.org/10.3133/ofr79542.","productDescription":"19 p.","costCenters":[],"links":[{"id":405507,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75003.htm","linkFileType":{"id":5,"text":"html"}},{"id":139545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0542/report-thumb.jpg"},{"id":275910,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0542/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"West Virginia","county":"Grant County, Randolph County, Tucker County","otherGeospatial":"Dolly Sods Wilderness","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.4583,\n 38.9167\n ],\n [\n -79.2917,\n 38.9167\n ],\n [\n -79.2917,\n 39.0833\n ],\n [\n -79.4583,\n 39.0833\n ],\n [\n -79.4583,\n 38.9167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683a02","contributors":{"authors":[{"text":"Motooka, J. M.","contributorId":8834,"corporation":false,"usgs":true,"family":"Motooka","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":153690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mei, Leung","contributorId":40204,"corporation":false,"usgs":true,"family":"Mei","given":"Leung","email":"","affiliations":[],"preferred":false,"id":153691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtis, C. A.","contributorId":47782,"corporation":false,"usgs":true,"family":"Curtis","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":153692,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lesure, F. G.","contributorId":7694,"corporation":false,"usgs":true,"family":"Lesure","given":"F. G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":153689,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7338,"text":"ofr79705 - 1979 - Mineral resources evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin","interactions":[{"subject":{"id":7338,"text":"ofr79705 - 1979 - Mineral resources evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin","indexId":"ofr79705","publicationYear":"1979","noYear":false,"title":"Mineral resources evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":33315,"text":"b1512 - 1981 - Mineral-resource evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin","indexId":"b1512","publicationYear":"1981","noYear":false,"title":"Mineral-resource evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin"},"id":1}],"supersededBy":{"id":33315,"text":"b1512 - 1981 - Mineral-resource evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin","indexId":"b1512","publicationYear":"1981","noYear":false,"title":"Mineral-resource evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin"},"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr79705","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-705","title":"Mineral resources evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79705","usgsCitation":"Cannon, W.F., Cameron, C., Klasner, J.S., Grosz, A.E., and Williams, B.B., 1979, Mineral resources evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin: U.S. Geological Survey Open-File Report 79-705, ii, 26 p. :ill., maps (1 fold.) ;28 cm., https://doi.org/10.3133/ofr79705.","productDescription":"ii, 26 p. :ill., maps (1 fold.) ;28 cm.","costCenters":[],"links":[{"id":140130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69bbad","contributors":{"authors":[{"text":"Cannon, William F. 0000-0002-2699-8118 wcannon@usgs.gov","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":1883,"corporation":false,"usgs":true,"family":"Cannon","given":"William","email":"wcannon@usgs.gov","middleInitial":"F.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":155301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cameron, C. C.","contributorId":94299,"corporation":false,"usgs":true,"family":"Cameron","given":"C. C.","affiliations":[],"preferred":false,"id":155304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klasner, J. S.","contributorId":66228,"corporation":false,"usgs":true,"family":"Klasner","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155302,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grosz, A. E.","contributorId":87925,"corporation":false,"usgs":true,"family":"Grosz","given":"A.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155303,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williams, B. B.","contributorId":106488,"corporation":false,"usgs":true,"family":"Williams","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":155305,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":7363,"text":"ofr791284 - 1979 - An oilspill risk analysis for the Northern Gulf of Alaska (proposed sale 55), Outer Continental Shelf lease area","interactions":[],"lastModifiedDate":"2024-07-12T19:34:06.331219","indexId":"ofr791284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1284","title":"An oilspill risk analysis for the Northern Gulf of Alaska (proposed sale 55), Outer Continental Shelf lease area","docAbstract":"

An oilspill risk analysis was conducted to determine the relative environmental hazards of developing oil in different regions of the Northern Gulf of Alaska Outer Continental Shelf lease area. The study analyzed the probability of spill occurrences, likely paths of the spilled oil, and locations of resources vulnerable to spilled oil. The combined results yielded estimates of the overall oilspill risks associated with development of the proposed lease area. The analysis implicitly includes estimates of weathering rates and slick dispersion and an indication of the possibility of mitigating effects by cleanup efforts. The leasing of the tracts proposed for Sale 55 will result in an expected number of 2.8 spills. The estimated probability that land will be contacted by one or more spills within 30 days is 0.84; however, this probability varies greatly for the different targets and different contact times.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791284","usgsCitation":"Lanfear, K.J., Nakassis, A., Samuels, W., and Schoen, C., 1979, An oilspill risk analysis for the Northern Gulf of Alaska (proposed sale 55), Outer Continental Shelf lease area: U.S. Geological Survey Open-File Report 79-1284, v, 79 p., https://doi.org/10.3133/ofr791284.","productDescription":"v, 79 p.","costCenters":[],"links":[{"id":431036,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1284/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140362,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1284/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Northern Gulf of Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -142.6766332039728,\n 60.05936535955627\n ],\n [\n -142.6766332039728,\n 59.057513548528874\n ],\n [\n -140.1387914070865,\n 59.057513548528874\n ],\n [\n -140.1387914070865,\n 60.05936535955627\n ],\n [\n -142.6766332039728,\n 60.05936535955627\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cca","contributors":{"authors":[{"text":"Lanfear, Kenneth J.","contributorId":20738,"corporation":false,"usgs":true,"family":"Lanfear","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":155409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nakassis, Anastasis","contributorId":107280,"corporation":false,"usgs":true,"family":"Nakassis","given":"Anastasis","email":"","affiliations":[],"preferred":false,"id":155412,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Samuels, William B.","contributorId":13238,"corporation":false,"usgs":true,"family":"Samuels","given":"William B.","affiliations":[],"preferred":false,"id":155410,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schoen, C.T.","contributorId":86761,"corporation":false,"usgs":true,"family":"Schoen","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":155411,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7365,"text":"ofr791062 - 1979 - A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana","interactions":[],"lastModifiedDate":"2023-11-24T19:31:09.75019","indexId":"ofr791062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1062","title":"A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana","docAbstract":"

The Indiana State Board of Health is developing a State water-quality management plan that includes the establishing of limits for wastewater effluents discharged into Indiana streams. A digital model calibrated to conditions in Cedar Creek was used to develop alternatives for future waste loadings that would be compatible with Indiana stream water-quality standards defined for two critical hydrologic conditions, summer and winter low flows. All point-source waste loads affecting Cedar Creek are in the four incorporated municipalities of Auburn, Garrett, Huntertown, and Waterloo, in a primarily agricultural area. Avilla, because of its distance from Cedar Creek, does not significantly affect the water quality of the modeled segment.

The model indicates that the dissolved-oxygen concentration of the Auburn wastewater effluent and nitrification are the most significant factors affecting the dissolved-oxygen concentration in Cedar Creek during summer low flows. The observed dissolved-oxygen concentration of the Auburn wastewater effluent was low, and averaged 30 percent of saturation. Whether the effluent is aerated before discharge will ultimately define the waste-load assimilative capacity of Cedar Creek. Projected nitrogenous biochemical-oxygen demand loads, from the Indiana State Board of Health, for the Auburn and Waterloo wastewater-treatment facilities will result in violations of the current instream dissolved-oxygen standard (5 milligrams per liter), even with an effluent dissolved-oxygen concentration of 80 percent saturation.

Natural streamflow for Cedar Creek upstream from the confluence of Willow and Little Cedar Creeks is small compared with the waste discharge, so benefits of dilution for Waterloo and Auburn are minimal. Stream reaeration capacity is not sufficient to maintain an average dissolved-oxygen concentration of at least 5 milligrams per liter, the State's water-quality standard for streams.

The model also indicates that, during winter low flows, ammonia toxicity, rather than dissolved oxygen, is the limiting water-quality criterion in the reach of Cedar Creek downstream from the wastewater-treatment facility at Auburn and the confluence of Garrett ditch. Ammonia-nitrogen concentrations predicted for 2978 through 2000 downstream from the Waterloo wastewater-treatment facility do not exceed Indiana water-quality standards for streams.

Calculations of the stream's assimilative capacity indicate that future waste discharge in the Cedar Creek basin will be limited to the reaches between the Auburn wastewater-treatment facility and County Road 68.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791062","collaboration":"Prepared in cooperation with the Indiana State Board of Health","usgsCitation":"Wilber, W.G., Peters, J.G., Ayers, M.A., and Crawford, C.G., 1979, A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana: U.S. Geological Survey Open-File Report 79-1062, viii, 79 p., https://doi.org/10.3133/ofr791062.","productDescription":"viii, 79 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":422925,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1062/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1062/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Allen County, Dekalb County","otherGeospatial":"Cedar Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -85.38216090798966,\n 41.60787742256892\n ],\n [\n -85.38216090798966,\n 41.14208690200232\n ],\n [\n -84.81087184548976,\n 41.14208690200232\n ],\n [\n -84.81087184548976,\n 41.60787742256892\n ],\n [\n -85.38216090798966,\n 41.60787742256892\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abb2c","contributors":{"authors":[{"text":"Wilber, William G. wgwilber@usgs.gov","contributorId":297,"corporation":false,"usgs":true,"family":"Wilber","given":"William","email":"wgwilber@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":155417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, James G.","contributorId":69137,"corporation":false,"usgs":true,"family":"Peters","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":155420,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ayers, Mark A.","contributorId":84730,"corporation":false,"usgs":true,"family":"Ayers","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155419,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":155418,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7814,"text":"ofr79848 - 1979 - Ice gouge obliteration and sediment redistribution event: 1977-1978, Beaufort Sea, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr79848","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-848","title":"Ice gouge obliteration and sediment redistribution event: 1977-1978, Beaufort Sea, Alaska","docAbstract":"In 1978 major changes in shelf morphology were observed during a routine re-survey of part of the inner shelf region of the central Beaufort Sea. Regional observations are coupled with a detailed diving and side-scan study of a single ice gouge of known age to develop a detailed description of the altered seabed conditions. Hydrodynamic activity has caused extensive sediment reworking, obliterating ice gouges to water depths of at least 13 m and has caused ponding of sediment in ice gouge terrain in deeper waters. Ponded sediment is characterized as a soft, sometimes very poorly consolidated, mud unit underlain by a stiffer, more consolidated, silty clay. In places, stiff silty clay is exposed in windows in the sediment pond and displays a fine-textured ice gouge morphology. Rates of sediment reworking and redisposition from apparently episodic events are an order of magnitude greater than the average sediment accumulation rates on the Beaufort Sea shelf. Reported maximum ice gouge incision depths are not representative of maximum ice keel penetrations into the seabed because these sedimentation events preferentially infill gouges. Furthermore, because these sedimentation events concentrate sediments in gouge troughs, a series of overlapping and interfingering 'shoestring' deposits is developed which should characterize the ice gouge stratigraphy. The specific hydraulic mechanisms for sediment redistribution and sediment compaction observed in this study are only poorly understood.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79848","usgsCitation":"Barnes, P.W., and Reimnitz, E., 1979, Ice gouge obliteration and sediment redistribution event: 1977-1978, Beaufort Sea, Alaska: U.S. Geological Survey Open-File Report 79-848, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr79848.","productDescription":"22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0848/report-thumb.jpg"},{"id":35309,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0848/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb850","contributors":{"authors":[{"text":"Barnes, Peter W.","contributorId":6042,"corporation":false,"usgs":true,"family":"Barnes","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":156656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":156657,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6271,"text":"pp1038 - 1979 - Stillwater Complex, Montana— Structure, mineralogy, and petrology of the basal zone with emphasis on the occurrence of sulfides","interactions":[{"subject":{"id":15318,"text":"ofr70252 - 1970 - Sulfide minerals in the G and H chromatite zones of the Stillwater Complex, Montana","indexId":"ofr70252","publicationYear":"1970","noYear":false,"title":"Sulfide minerals in the G and H chromatite zones of the Stillwater Complex, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":6271,"text":"pp1038 - 1979 - Stillwater Complex, Montana— Structure, mineralogy, and petrology of the basal zone with emphasis on the occurrence of sulfides","indexId":"pp1038","publicationYear":"1979","noYear":false,"title":"Stillwater Complex, Montana— Structure, mineralogy, and petrology of the basal zone with emphasis on the occurrence of sulfides"},"id":1}],"lastModifiedDate":"2021-11-15T20:27:28.424086","indexId":"pp1038","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1038","title":"Stillwater Complex, Montana— Structure, mineralogy, and petrology of the basal zone with emphasis on the occurrence of sulfides","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1038","usgsCitation":"Page, N.J., 1979, Stillwater Complex, Montana— Structure, mineralogy, and petrology of the basal zone with emphasis on the occurrence of sulfides: U.S. Geological Survey Professional Paper 1038, 69 p., https://doi.org/10.3133/pp1038.","productDescription":"69 p.","costCenters":[],"links":[{"id":391691,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4691.htm"},{"id":33529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1038/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1038/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Stillwater Complex","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.250,\n 45.3547\n ],\n [\n -109.7833,\n 45.3547\n ],\n [\n -109.7833,\n 45.5\n ],\n [\n -110.250,\n 45.5\n ],\n [\n -110.250,\n 45.3547\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4408","contributors":{"authors":[{"text":"Page, Norman J.","contributorId":46492,"corporation":false,"usgs":true,"family":"Page","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":152425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5637,"text":"pp1052 - 1979 - A study of global sand seas","interactions":[{"subject":{"id":8927,"text":"ofr78405 - 1978 - Techniques for the evaluation of surface wind data in terms of eolian sand drift","indexId":"ofr78405","publicationYear":"1978","noYear":false,"title":"Techniques for the evaluation of surface wind data in terms of eolian sand drift"},"predicate":"SUPERSEDED_BY","object":{"id":5637,"text":"pp1052 - 1979 - A study of global sand seas","indexId":"pp1052","publicationYear":"1979","noYear":false,"title":"A study of global sand seas"},"id":1}],"lastModifiedDate":"2018-01-12T14:20:03","indexId":"pp1052","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1052","title":"A study of global sand seas","docAbstract":"

The birth of the idea that led to this publication on \"Global Sand Seas\" dates back to the late 1920's. At that time I was engaged in a study of the Coconino Sandstone of Arizona's Grand Canyon. Considerable controversy existed then as to whether this sandstone was a subaqueous deposit or was composed of wind-formed dunes. It became apparent that definitive literature was sparse or lacking on types of dunes, global distribution of these types, the mechanics of their development, the precise nature of their internal structure of cross-stratificiation, and the relation of wind systems to these sand forms. Especially lacking were data on criteria that could confidently be used in the recognition of ancient dunes. 

The common denominator in this publication is eolian sand bodies. Although the book is concerned primarily with desert sand seas, the subject matter is not restricted to deserts; it includes many references to deposits of coastal sand and to sand bodies in humid climates. Nor does the book deal exclusively with dunes, which, according to most definitions, involve mounds or hills. Many references are made to sand sheets, sand stringers, and other types of sand deposits that have no prominent topographic expression. All sand bodies accumulated by the action of wind are discussed.

Chapters A-J of this publication are primarily topical. Chapters cover the grain texture, the color, and the structure of modern dunes and other eolian sands. Special treatment is given to the relation of wind data to dune interpretation, the evolution of form in current-deposited sand bodies as determined from experimental studies, and the discriminant analysis technique for differentiating between coastal and inland desert sands. This topical part of the publication also includes an analysis of criteria used in ancient deposits to interpret their eolian genesis and a consideration of economic application of the principles described, including a discussion of potentials and problems associated with eolian hydrocarbon reservoirs. The final chapters present a discussion of the morphology and distribution of dunes as determined largely from Landsat images.

Chapter K of the publication is devoted to descriptions of major sand seas based largely on thematic maps derived from Landsat (ERTS) mosaics. Although inclusion herein of the actual mosaics proved to be impractical, the maps derived from them do show the distribution and abundance of various dune types and the relations of these types to certain associated features, such as bedrock, water bodies, and juxtaposed dunes. Furthermore, sand roses included with each of these maps enable the user to draw conclusions on the probable relations of wind strength and direction to dune type in a particular area.

Regional studies (chapter K) were a team effort. Analysis of the Landsat (ERTS) mosaics and mapping boundaries of individual dune types were by Carol Breed. Synthesis of the rather voluminous literature and preparation of abstracts covering it was by Camilla MacCauley. Actual preparation of maps was by Franci Lennartz and later by Sarah Andrews. The gathering of data on wind, the calculation of wind roses, and the interpretation of their relations to sand bodies were by Steven Fryberger, assisted by Gary Dean.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1052","usgsCitation":"1979, A study of global sand seas: U.S. Geological Survey Professional Paper 1052, ix, 429 p., https://doi.org/10.3133/pp1052.","productDescription":"ix, 429 p.","numberOfPages":"439","costCenters":[],"links":[{"id":122640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1052/report-thumb.jpg"},{"id":32135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a61c2","contributors":{"editors":[{"text":"McKee, Edwin D.","contributorId":60207,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":725490,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":8017,"text":"ofr79524 - 1979 - Possible reestablishment of sawtimber production following mining in the Osceola National Forest, an analysis of the state-of-the-art, February 9, 1978","interactions":[],"lastModifiedDate":"2022-10-17T20:35:24.181515","indexId":"ofr79524","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-524","title":"Possible reestablishment of sawtimber production following mining in the Osceola National Forest, an analysis of the state-of-the-art, February 9, 1978","docAbstract":"

There is a good possibility that sawtimber production could be reestablished on the Osceola National Forest. Engineering technology that is coming on-line should allow the establishment of land/water relationships that meet the requirements of desired tree species. Information available on soil-plant relationships indicate an absence of phytotoxic materials in various mining wastes and that good tree growth is possible.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79524","usgsCitation":"Boyce, J.S., 1979, Possible reestablishment of sawtimber production following mining in the Osceola National Forest, an analysis of the state-of-the-art, February 9, 1978: U.S. Geological Survey Open-File Report 79-524, 25 p., https://doi.org/10.3133/ofr79524.","productDescription":"25 p.","costCenters":[],"links":[{"id":141575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0524/report-thumb.jpg"},{"id":408426,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0524/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Osceola National Forest","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.6885986328125,\n 30.183121842195515\n ],\n [\n -82.22991943359375,\n 30.183121842195515\n ],\n [\n -82.22991943359375,\n 30.60482195075795\n ],\n [\n -82.6885986328125,\n 30.60482195075795\n ],\n [\n -82.6885986328125,\n 30.183121842195515\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683b4e","contributors":{"authors":[{"text":"Boyce, J. Scott","contributorId":42963,"corporation":false,"usgs":true,"family":"Boyce","given":"J.","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":156994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8157,"text":"ofr79229 - 1979 - Mineral resources of the Wambaw Swamp Wilderness Study Area, Charleston County, South Carolina","interactions":[],"lastModifiedDate":"2023-01-03T22:35:21.788186","indexId":"ofr79229","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-229","title":"Mineral resources of the Wambaw Swamp Wilderness Study Area, Charleston County, South Carolina","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79229","usgsCitation":"Cameron, C.C., Force, E.R., Gazdik, G.C., and Rodehamel, E.C., 1979, Mineral resources of the Wambaw Swamp Wilderness Study Area, Charleston County, South Carolina: U.S. Geological Survey Open-File Report 79-229, Report: ii, 35 p.; 2 Plates: 34.29 x 26.07 inches and 27.63 x 29.02 inches, https://doi.org/10.3133/ofr79229.","productDescription":"Report: ii, 35 p.; 2 Plates: 34.29 x 26.07 inches and 27.63 x 29.02 inches","costCenters":[],"links":[{"id":411307,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11229.htm","linkFileType":{"id":5,"text":"html"}},{"id":35767,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0229/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35766,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0229/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35765,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0229/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141513,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0229/report-thumb.jpg"}],"country":"United States","state":"South Carolina","county":"Charleston County","otherGeospatial":"Wambaw Swamp Wilderness Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -79.625,\n 33\n ],\n [\n -79.564,\n 33\n ],\n [\n -79.564,\n 33.125\n ],\n [\n -79.625,\n 33.125\n ],\n [\n -79.625,\n 33\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699fd7","contributors":{"authors":[{"text":"Cameron, Cornelia Clermont","contributorId":20737,"corporation":false,"usgs":true,"family":"Cameron","given":"Cornelia","email":"","middleInitial":"Clermont","affiliations":[],"preferred":false,"id":157241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Force, Eric R.","contributorId":32916,"corporation":false,"usgs":true,"family":"Force","given":"Eric","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gazdik, Gertrude C.","contributorId":56220,"corporation":false,"usgs":true,"family":"Gazdik","given":"Gertrude","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":157244,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rodehamel, Edward Charles","contributorId":21955,"corporation":false,"usgs":true,"family":"Rodehamel","given":"Edward","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":157242,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":8138,"text":"ofr791555 - 1979 - Sediment transport in Norton Sound, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr791555","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1555","title":"Sediment transport in Norton Sound, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791555","usgsCitation":"Cacchione, D.A., and Drake, D.E., 1979, Sediment transport in Norton Sound, Alaska: U.S. Geological Survey Open-File Report 79-1555, 90 p. :ill., maps, graphs ;28 cm., https://doi.org/10.3133/ofr791555.","productDescription":"90 p. :ill., maps, graphs ;28 cm.","costCenters":[],"links":[{"id":142131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1555/report-thumb.jpg"},{"id":35741,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1555/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbef2","contributors":{"authors":[{"text":"Cacchione, David A.","contributorId":37327,"corporation":false,"usgs":true,"family":"Cacchione","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drake, David E.","contributorId":74752,"corporation":false,"usgs":true,"family":"Drake","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157213,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5634,"text":"pp1163AD - 1979 - Studies of the Permian Phosphoria Formation and related rocks, Great Basin-Rocky Mountain region","interactions":[],"lastModifiedDate":"2024-11-19T14:30:39.994209","indexId":"pp1163AD","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1163","chapter":"A-D","title":"Studies of the Permian Phosphoria Formation and related rocks, Great Basin-Rocky Mountain region","docAbstract":"

PART A: The transgression of the Permian Retort Phosphatic Shale Member of the Phosphoria Formation is dated by the occurrence of diagnostic brachiopods. The complex pattern of this transgression reflects the paleogeography and indicates two initial basins of deposition: one in southwestern Montana and one in southeastern Idaho. PART B: A new formation is proposed for middle Permian rocks of a transitional facies positioned laterally between the Rex Chert Member of the Phosphoria Formation in northeastern Utah and southeastern Idaho and the Plympton Formation in northeastern Nevada and northwestern Utah. PART C: The relationships of the Permian Park City Group to the Phosphoria and Park City Formations are clarified by the stratigraphy of four sections in northwestern Utah, northeastern Nevada, and southern Idaho. PART D: Five biostratigraphic zones based on the distribution of brachiopods and conodonts are proposed for the Park City Group. They are: the Peniculauris ivesi-Neostreptognathodus prayi Zone, the Peniculauris bassi-Neostreptognathodus sulcoplicatus Zone, the Peniculauris bassi-Neostreptognathodus sp. C Zone, the Thamnosia depressa Zone, and the Yakovlevia. multistriata-Neogondolella bitteri Zone. They range in age from Leonardian to Wordian.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1163AD","usgsCitation":"Wardlaw, B.R., 1979, Studies of the Permian Phosphoria Formation and related rocks, Great Basin-Rocky Mountain region: U.S. Geological Survey Professional Paper 1163, iii, 22 p., https://doi.org/10.3133/pp1163AD.","productDescription":"iii, 22 p.","costCenters":[],"links":[{"id":125047,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1163a-d/report-thumb.jpg"},{"id":32133,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1163a-d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402236,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74398.htm","text":"The Murdock Mountain Formation: a new unit of the Permian Park City Group","linkFileType":{"id":5,"text":"html"}},{"id":464240,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74399.htm","text":"Stratigraphy of Park City Group equivalents (Permian) in southern Idaho, northeastern Nevada, and northwestern Utah","linkFileType":{"id":5,"text":"html"}},{"id":464241,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92994.htm","text":"Transgression of the Retort Phosphatic Shale Member of the Phosphoria Formation (Permian) in Idaho, Montana, Utah, and Wyoming","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho, Montana, Nevada, Utah, Wyoming","otherGeospatial":"Great Basin, Permian Phosphoria Formation, Rocky Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.63134765625001,\n 42.50450285299051\n ],\n [\n -108.03955078125,\n 42.50450285299051\n ],\n [\n -108.03955078125,\n 45.874712248904764\n ],\n [\n -114.63134765625001,\n 45.874712248904764\n ],\n [\n -114.63134765625001,\n 42.50450285299051\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.65283203124999,\n 37.64903402157866\n ],\n [\n -111.09374999999999,\n 37.64903402157866\n ],\n [\n -111.09374999999999,\n 42.35854391749705\n ],\n [\n -116.65283203124999,\n 42.35854391749705\n ],\n [\n -116.65283203124999,\n 37.64903402157866\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e36","contributors":{"authors":[{"text":"Wardlaw, Bruce R. bwardlaw@usgs.gov","contributorId":266,"corporation":false,"usgs":true,"family":"Wardlaw","given":"Bruce","email":"bwardlaw@usgs.gov","middleInitial":"R.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":151338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8040,"text":"ofr79839 - 1979 - The mineralogy and geochemistry of lithium in the Popotosa Formation, Socorro County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr79839","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-839","title":"The mineralogy and geochemistry of lithium in the Popotosa Formation, Socorro County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79839","usgsCitation":"Brenner-Tourtelot, E.F., and Machette, M., 1979, The mineralogy and geochemistry of lithium in the Popotosa Formation, Socorro County, New Mexico: U.S. Geological Survey Open-File Report 79-839, ii, 24 leaves :ill., map ;28 cm., https://doi.org/10.3133/ofr79839.","productDescription":"ii, 24 leaves :ill., map ;28 cm.","costCenters":[],"links":[{"id":140553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0839/report-thumb.jpg"},{"id":35616,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0839/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a035","contributors":{"authors":[{"text":"Brenner-Tourtelot, Elizabeth F.","contributorId":103672,"corporation":false,"usgs":true,"family":"Brenner-Tourtelot","given":"Elizabeth","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":157036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Machette, Michael N.","contributorId":28963,"corporation":false,"usgs":true,"family":"Machette","given":"Michael N.","affiliations":[],"preferred":false,"id":157035,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8142,"text":"ofr791302 - 1979 - Radioactive springs geochemical data related to uranium exploration: basic data and use of multivariate factor scores","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr791302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1302","title":"Radioactive springs geochemical data related to uranium exploration: basic data and use of multivariate factor scores","docAbstract":"Radioactive springs and wells at 33 localities in the States of Colorado, Utah, Arizona, and New Mexico have been studied and sampled to obtain geochemical data to determine whether such data are useful in a uranium exploration program. Most samples were collected from mineral-rich springs probably related to hydrothermal systems of various ages. Two sets of data were obtained, the first based on the chemical composition and physical and chemical properties of spring and ground water, and the second based on the chemical composition of mineral precipitates deposited by radioactive springs. Multivariate statistical analysis of the water data suggests four major geochemical factors affecting the 23 parameters measured. These factors were labeled as total dissolved solids, alkalinity, temperature, and Fe-U concentration. Multivariate statistical analysis of the precipitate data suggests five factors affecting the 32 element values measured. These factors were labeled as mineral contamination, Mn precipitation, Fe-As-Be precipitation, heavy metals precipitation, and Ba-Ra precipitation. \r\n\r\nRelative intensities of the geochemical processes represented by the factors were computed using factor scores. Sample localities were ranked on the basis of relative intensities, and the five localities with the highest intensities were selected as being the most favorable for more intensive exploration for uranium. Immediate use of such selection would be experimental because of the lack of industry experience at this time in the exploration of active hydrothermal systems for uranium.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791302","usgsCitation":"Cadigan, R.A., and Felmlee, J., 1979, Radioactive springs geochemical data related to uranium exploration: basic data and use of multivariate factor scores: U.S. Geological Survey Open-File Report 79-1302, iii, 37 p. :2 maps ;28 cm., https://doi.org/10.3133/ofr791302.","productDescription":"iii, 37 p. :2 maps ;28 cm.","costCenters":[],"links":[{"id":142292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1302/report-thumb.jpg"},{"id":35745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1302/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686386","contributors":{"authors":[{"text":"Cadigan, Robert Allen","contributorId":27051,"corporation":false,"usgs":true,"family":"Cadigan","given":"Robert","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":157219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Felmlee, J. Karen","contributorId":90311,"corporation":false,"usgs":true,"family":"Felmlee","given":"J. Karen","affiliations":[],"preferred":false,"id":157220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8042,"text":"ofr791433 - 1979 - Computer retrieval of bibliographies using an editing program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr791433","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1433","title":"Computer retrieval of bibliographies using an editing program","docAbstract":"A simple program permits use of the text .editor 'qedx,' part of many computer systems, to input bibliographic entries and to retrieve specific entries which contain keywords of interest. Multiple keywords may be used sequentially to find specific entries.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791433","usgsCitation":"Brethauer, G., and Brokaw, V., 1979, Computer retrieval of bibliographies using an editing program: U.S. Geological Survey Open-File Report 79-1433, 10 p. ;28 cm., https://doi.org/10.3133/ofr791433.","productDescription":"10 p. ;28 cm.","costCenters":[],"links":[{"id":140555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1433/report-thumb.jpg"},{"id":35619,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1433/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a768d","contributors":{"authors":[{"text":"Brethauer, G.E.","contributorId":69548,"corporation":false,"usgs":true,"family":"Brethauer","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":157040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brokaw, V.L.","contributorId":40212,"corporation":false,"usgs":true,"family":"Brokaw","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":157039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7409,"text":"ofr791634 - 1979 - Petroleum source rock and reservoir quality data from outcrop samples, onshore North Slope of Alaska, east of Prudhoe Bay","interactions":[],"lastModifiedDate":"2022-11-22T22:53:43.789569","indexId":"ofr791634","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1634","title":"Petroleum source rock and reservoir quality data from outcrop samples, onshore North Slope of Alaska, east of Prudhoe Bay","docAbstract":"

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This professional paper is the fifth in a series of paleotectonic studies each covering a geologic system in the conterminous United States. Part I provides a region-by-region discussion of data concerning the Mississippian System and an explanation and documentation for the maps and sections contained in part III. Part II of the paper provides a summary of the Mississippian System, presents interregional interpretations permitted by this study, and includes sections on notable features of the system. The maps contained in the separate case as part III may be divided into two groups: (1) a sequence of factual or basic maps that shows, with a minimum of interpretation, the Mississippian System as it occurs today, and (2) interpretive maps that attempt a reasonable reconstruction of the original extent of the system, its tectonics, environment, and geography.

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