The Fish Creek EMRIA site, an area of about 3.7 square miles (9.6 km2), is located in the southeastern part of the Yampa coal field on the steep to gently dipping beds of the Upper Cretaceous Williams Fork Formation.
The Fish Creek coal bed within 200 feet (60 m) of the surface was evaluated by five core holes. Coal resources--measured, indicated, and inferred--within the site are 2,512,000 short tons, 7,970,000 short tons, and 507,000 short tons respectively.
The coal has an apparent rank of bituminous C. The average Btu value of three core samples from the site on the as-received basis is 10,790, average ash content is 11.1 percent, and average sulfur content is 1.9 percent.
A comparison of the analyses of samples from the Fish Creek coal bed with other Rocky Mountain province coal sample analyses shows that nitrogen, total sulfur, and pyritic and organic sulfur contents are noticeably higher in the Fish Creek coal bed samples. A comparison of other element analyses shows that the Fish Creek coal bed is noticeably higher in As, Cr, F, Fe, Hg, and Sr, and noticeably lower in Th.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78848","usgsCitation":"Schneider, G.B., 1978, Coal resources of the Fish Creek EMRIA site, Routt County, Colorado: U.S. Geological Survey Open-File Report 78-848, iii, 28 p., https://doi.org/10.3133/ofr78848.","productDescription":"iii, 28 p.","costCenters":[],"links":[{"id":425159,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0848/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143625,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0848/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Routt County","otherGeospatial":"Fish Creek EMRIA site","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -107.46594143831412,\n 40.98936317017498\n ],\n [\n -107.46594143831412,\n 39.86701070778301\n ],\n [\n -106.65690663111283,\n 39.86701070778301\n ],\n [\n -106.65690663111283,\n 40.98936317017498\n ],\n [\n -107.46594143831412,\n 40.98936317017498\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aeda0","contributors":{"authors":[{"text":"Schneider, Gary B.","contributorId":64253,"corporation":false,"usgs":true,"family":"Schneider","given":"Gary","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":162414,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11507,"text":"ofr78431 - 1978 - Least-squares refinement of powder diffraction data for unit cell parameters: Program listing for DEC 10 computer","interactions":[],"lastModifiedDate":"2023-02-14T22:50:03.542506","indexId":"ofr78431","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-431","title":"Least-squares refinement of powder diffraction data for unit cell parameters: Program listing for DEC 10 computer","docAbstract":"This FORTRAN computer program is a time-sharing version of the classic program of Appleman and Evans (1973) and Evans, Appleman, and Handwerker (1963), which indexes powder patterns and refines unit-cell dimensions. The program, originally written to be processed in batch mode for an IBM computer, was modified to run in time-sharing mode on the DEC 10 computer.
This version does not depart philosophically from the original program; however, the input and output formats have been adapted to the time-sharing terminal. These modifications and the actual running of the program are not discussed in detail here, as this report is intended only to make the program itself available. Examples of the input and output formats are shown on pages 3-8.
Input can be entered through the terminal by two methods. An input file may either be independently created and then entered into the program later, or created directly through the interactive mode of the program. With the latter method a file of the input information may also be saved for later use. Both methods allow for the data to be edited after each refinement run.
The output format has been changed to an 80-column width, common to many terminals. Only the last refinement cycle is printed and some of the statistical computations have been surpressed.
Using the \"Unit Cell\" program from the terminal in a \"real time\" situation emphasizes the versatility of the program. This ability to interact directly with the computer gives the user a better appreciation of the program, its options, the data, and the problem being solved.
This report presents hydraulic and chemical data collected from March 1970 to December 1977 at a deep-well waste-injection system at the Monsanto Company's plant near Pensacola, Florida. The injection system presently consists of Injection Well A, Injection Well B, and two deep monitor wells all completed open hole in the lower limestone of the Floridan aquifer and one shallow monitor well completed in the upper limestone of the Floridan aquifer. The two deep monitor wells are used to observe hydraulic and geochemical effects of waste injection in the injection zone at locations 1.5 miles south-southeast and 1.9 miles north-northwest of the center of the injection site. The shallow monitor well, used to observe any effects in the first permeable zone above the 220-foot-thick confining bed, is 100 feet northeast of Injection Well A.
Since injection began in July 1963, about 14.2 billion gallons of acidic industrial waste consisting of an aqueous solution of nitric acid, inorganic salts, and numerous organic compounds have been injected into a limestone aquifer containing saline water. From July 1963 to April 1968, the pH of the waste was raised to about 5.5 with aqueous ammonia prior to injection. Since 1968, no aqueous ammonia has been added and the waste has been injected at a pH of about 2.3. Wellhead injection pressures at both injection wells in December 1977 averaged 170 pounds per square inch and the hydraulic pressure gradient was 0.52 pound per square inch per foot of depth to the top of the injection zone. Increases in pressures since 1970 at the north and south monitor wells ranged from 21 to 31 pounds per square inch. The pressure in the shallow monitor well declined about 6 pounds per square inch.
No changes were detected in the chemical characteristics of water from the shallow monitor and the north monitor wells. Since late 1973, concentrations of bicarbonate and dissolved organic carbon in water from the south monitor well have increased. These increases in bicarbonate and dissolved organic carbon have been accompanied by increases in gas content of water at the point of discharge from the well and a distinctive odor like that of the waste. In samples of water from the south monitor well, concentrations of nitrogen gas ranged from 5.1 to 12.7 milligrams per liter, methane from 24 to 70 milligrams per liter, and carbon dioxide from 14 to 56 milligrams per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78355","collaboration":"Prepared in cooperation with the Florida Department of Environmental Regulation","usgsCitation":"Pascale, C.A., and Martin, J., 1978, Hydrologic monitoring of waste-injection wells near Pensacola, Florida, March 1970 - December 1977: U.S. Geological Survey Open-File Report 78-355, v, 78 p., https://doi.org/10.3133/ofr78355.","productDescription":"v, 78 p.","costCenters":[],"links":[{"id":413197,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0355/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142485,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0355/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Pensacola","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -87.4352973536881,\n 30.602838004118823\n ],\n [\n -87.4352973536881,\n 30.347295597488937\n ],\n [\n -87.03446660204348,\n 30.347295597488937\n ],\n [\n -87.03446660204348,\n 30.602838004118823\n ],\n [\n -87.4352973536881,\n 30.602838004118823\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6065aa","contributors":{"authors":[{"text":"Pascale, Charles A.","contributorId":99978,"corporation":false,"usgs":true,"family":"Pascale","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, J.B.","contributorId":32923,"corporation":false,"usgs":true,"family":"Martin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":161690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10617,"text":"ofr78101 - 1978 - Hydrologic monitoring of a waste-injection well near Milton, Florida, June 1975 - June 1977","interactions":[],"lastModifiedDate":"2014-05-29T08:52:32","indexId":"ofr78101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-101","title":"Hydrologic monitoring of a waste-injection well near Milton, Florida, June 1975 - June 1977","docAbstract":"This report presents the hydraulic and chemical data collected from June 1, 1975, when injection began, to June 30, 1977 through a monitoring program at a deep-well waste-injection system at the American Cyanamid Company's plant near Milton, about 12 miles northwest of Pensacola. The injection system consists of a primary injection well, a standby injection well, and two deep monitor wells all completed open hole in the lower limestone of the Floridan aquifer and one shallow-monitor well completed in the upper limestone of the Floridan aquifer. Two of the monitor wells and the standby injection well are used to observe hydraulic and geochemical effects of waste injection in the injection zone at locations 8,180 feet northeast, 1,560 feet south, and 1,025 feet southwest of the primary injection well. The shallow-monitor well, used to observe any effects in the first permeable zone above the 200-foot-thick confining bed, is 28 feet north of the primary injection well.
\nSince injection began in June 1975, 607 million gallons of treated industrial liquid waste with a pH of 4.6 to 6.3 and containing high concentrations of nitrate, organic nitrogen and carbon have been injected into a saline-water-filled limestone aquifer. Wellhead pressure at the injection well in June 1977 average 137 pounds per square inch and the hydraulic pressure gradient was 0.53 pound per square inch per foot of depth to the top of the injection zone. Water levels rose from 36 to 74 feet at the three wells used to monitor the injection zone during the 25-month period. The water level in the shallow-monitor well declined about 8 feet. No changes were detected in the chemical character of water from the shallow-monitor well and deep-monitor well-north. Increases in concentration of bicarbonate and dissolved organic carbon were detected in water from the deep-test monitor well in February 1976 and at the standby injection well in August 1976. In addition to increases in bicarbonate and dissolved organic carbon, sulfate, total organic nitrogen, and total nitrogen concentrations have also increased substantially in samples from these wells. Nitrogen gas concentrations in water samples collected at the three deep-monitor wells ranged from 19 to 176 milligrams per liter, methane from 4.5 to 11.4 milligrams per liter, and carbon dioxide from 7.7 to 44 milligrams per liter. The most probable number of denitrifying bacteria in water samples collected at the three deep-monitor wells ranged from less than 2 colonies to 17 colonies per 100 milliliters.
\nNone of the water samples collected in April 1977 at the three deep-monitor wells showed positive concentrations of acetone, ethanol, methanol, or acrylonitrile.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tallahassee, FL","doi":"10.3133/ofr78101","collaboration":"Prepared in cooperation with the Florida Department of Environmental Regulation","usgsCitation":"Pascale, C.A., and Martin, J., 1978, Hydrologic monitoring of a waste-injection well near Milton, Florida, June 1975 - June 1977: U.S. Geological Survey Open-File Report 78-101, v, 74 p., https://doi.org/10.3133/ofr78101.","productDescription":"v, 74 p.","numberOfPages":"79","costCenters":[],"links":[{"id":287787,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287786,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0101/report.pdf"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.116667,30.5625 ], [ -87.116667,30.588889 ], [ -87.091667,30.588889 ], [ -87.091667,30.5625 ], [ -87.116667,30.5625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606573","contributors":{"authors":[{"text":"Pascale, Charles A.","contributorId":99978,"corporation":false,"usgs":true,"family":"Pascale","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, J.B.","contributorId":32923,"corporation":false,"usgs":true,"family":"Martin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":161688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10737,"text":"ofr78549 - 1978 - Bibliography of the PVTXE properties of the binary system H2O-NaCl","interactions":[],"lastModifiedDate":"2023-11-24T20:17:40.301386","indexId":"ofr78549","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-549","title":"Bibliography of the PVTXE properties of the binary system H2O-NaCl","docAbstract":"The following bibliography on the PVTXE (pressure, volume, temperature, composition and energy) properties of the binary system H20-NaCl was compiled to ascertain the status of the available literature data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78549","usgsCitation":"Potter, R., 1978, Bibliography of the PVTXE properties of the binary system H2O-NaCl: U.S. Geological Survey Open-File Report 78-549, 34 p., https://doi.org/10.3133/ofr78549.","productDescription":"34 p.","costCenters":[],"links":[{"id":422937,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0549/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143555,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0549/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627d8a","contributors":{"authors":[{"text":"Potter, Robert W.","contributorId":27045,"corporation":false,"usgs":true,"family":"Potter","given":"Robert W.","affiliations":[],"preferred":false,"id":161880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11452,"text":"ofr78693 - 1978 - Ice-gouged microrelief on the floor of the eastern Chukchi Sea, Alaska: a reconnaissance survey","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr78693","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-693","title":"Ice-gouged microrelief on the floor of the eastern Chukchi Sea, Alaska: a reconnaissance survey","docAbstract":"Side-scan sonar and bathymetric records obtained from 1,800 km of trackline from the eastern Chukchi Sea continental shelf, between water depths of 20 and 70 m show the ubiquitous presence of furrow-like linear depressions produced by gouging of the sea bed by ice keels. These sea bed micro-features are regionally widespread but are not uniformly distributed. Furthermore, the microrelief, texture, and lithologic structure of sea bed sediments have been significantly modified by the disruptive processes associated with ice gouge formation. \r\n\r\nAn analysis of some 10,.200 individual gouges shows that the density of ice gouges increases with increasing latitude, increasing slope gradients, and decreasing water depth. Across the northern half of the shelf few trackline segments are free of ice gouges; in the southern portion numerous segments contain no ice gouges. However, ice gouges extend at least as far south as Cape Prince of Wales Shoal. Densities of over 200 gouges per km of trackline are not uncommon in water depths less than 30 m ,but no values higher than 50 km are encountered in water deeper than 50 m. No ice gouges have been observed in water depths exceeding 58 m. Saturation ice gouge densities (greater than 300/Pan) occur along the eastern side 6f Barrow Sea Valley and the northeast flank of Hanna Shoal. \r\n\r\nMaximum gouge incision depths per km of trackline are greatest in water 36 to 50 m deep . A maximum incision depth of 4.5 m occurs in the 35-40 m water depth interval. Individual ice gouge events wider than 100 m, most produced by multi-keeled ice fragments, are found between 31 and 45 m depths. The dominant azimuth of gouge furrows shows no preferred orientation on the Chukchi Sea shelf; only locally does bathmetric control of the trend of gouges appear. \r\n\r\nThe occurrence of current-produced bedforms within individual ice gouges suggests an interaction between slow-moving grounded or gouging ice keels and swift currents. In other cases, current-produced bedforms, interpreted as being in equilibrium with existing flow regimes, lie adjacent to ice gouges, suggesting contemporary ice gouging to water depths of at least 43 m.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78693","usgsCitation":"Toimil, L.J., 1978, Ice-gouged microrelief on the floor of the eastern Chukchi Sea, Alaska: a reconnaissance survey: U.S. Geological Survey Open-File Report 78-693, 44, [68] leaves :ill., maps ;28 cm.; (113 p. - PGS), https://doi.org/10.3133/ofr78693.","productDescription":"44, [68] leaves :ill., maps ;28 cm.; (113 p. - PGS)","costCenters":[],"links":[{"id":144818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0693/report-thumb.jpg"},{"id":39316,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0693/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb725","contributors":{"authors":[{"text":"Toimil, Lawrence J.","contributorId":53806,"corporation":false,"usgs":true,"family":"Toimil","given":"Lawrence","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":163160,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42900,"text":"ofr78341 - 1978 - Preliminary geologic map of the west half of Owyhee County, Idaho","interactions":[{"subject":{"id":42900,"text":"ofr78341 - 1978 - Preliminary geologic map of the west half of Owyhee County, Idaho","indexId":"ofr78341","publicationYear":"1978","noYear":false,"title":"Preliminary geologic map of the west half of Owyhee County, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":67534,"text":"i1256 - 1981 - Geologic map of Owyhee County, Idaho, west of longitude 116 degrees W.","indexId":"i1256","publicationYear":"1981","noYear":false,"title":"Geologic map of Owyhee County, Idaho, west of longitude 116 degrees W."},"id":1}],"supersededBy":{"id":67534,"text":"i1256 - 1981 - Geologic map of Owyhee County, Idaho, west of longitude 116 degrees W.","indexId":"i1256","publicationYear":"1981","noYear":false,"title":"Geologic map of Owyhee County, Idaho, west of longitude 116 degrees W."},"lastModifiedDate":"2022-04-12T21:36:52.998485","indexId":"ofr78341","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-341","title":"Preliminary geologic map of the west half of Owyhee County, Idaho","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78341","usgsCitation":"Ekren, E.B., McIntyre, D.H., and Bennett, E.H., 1978, Preliminary geologic map of the west half of Owyhee County, Idaho: U.S. Geological Survey Open-File Report 78-341, 2 Plates: 40.72 x 65.57 inches and 39.55 x 31.07 inches, https://doi.org/10.3133/ofr78341.","productDescription":"2 Plates: 40.72 x 65.57 inches and 39.55 x 31.07 inches","costCenters":[],"links":[{"id":398605,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0341/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398604,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0341/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0341/report-thumb.jpg"},{"id":397087,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14692.htm"}],"scale":"125000","country":"United States","state":"Idaho","county":"Owyhee County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.8333,\n 42\n ],\n [\n -116,\n 42\n ],\n [\n -116,\n 43.583\n ],\n [\n -117.8333,\n 43.583\n ],\n [\n -117.8333,\n 42\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674196","contributors":{"authors":[{"text":"Ekren, E. B.","contributorId":14371,"corporation":false,"usgs":true,"family":"Ekren","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":227358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, D. H.","contributorId":45726,"corporation":false,"usgs":true,"family":"McIntyre","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, Earl H.","contributorId":97093,"corporation":false,"usgs":true,"family":"Bennett","given":"Earl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227360,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11342,"text":"ofr78591 - 1978 - The utility of petroleum seismic exploration data in delineating structural features within salt anticlines","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr78591","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-591","title":"The utility of petroleum seismic exploration data in delineating structural features within salt anticlines","docAbstract":"The Salt Valley anticline, in the Paradox Basin of southeastern Utah, is under investigation for use as a location for storage of solid nuclear waste. Delineation of thin, nonsalt interbeds within the upper reaches of the salt body is extremely important because the nature and character of any such fluid- or gas-saturated horizons would be critical to the mode of emplacement of wastes into the structure. \r\n\r\nAnalysis of 50 km of conventional seismic-reflection data, in the vicinity of the anticline, indicates that mapping of thin beds at shallow depths may well be possible using a specially designed adaptation of state-of-the-art seismic oil-exploration procedures. Computer ray-trace modeling of thin beds in salt reveals that the frequency and spatial resolution required to map the details of interbeds at shallow depths (less than 750 m) may be on the order of 500 Hz, with surface-spread lengths of less than 350 m. Consideration should be given to the burial of sources and receivers in order to attenuate surface noise and to record the desired high frequencies. \r\n\r\nCorrelation of the seismic-reflection data with available well data and surface geology reveals the complex, structurally initiated diapir, whose upward flow was maintained by rapid contemporaneous deposition of continental clastic sediments on its flanks. Severe collapse faulting near the crests of these structures has distorted the seismic response. Evidence exists, however, that intrasalt thin beds of anhydrite, dolomite, and black shale are mappable on seismic record sections either as short, discontinuous reflected events or as amplitude anomalies that result from focusing of the reflected seismic energy by the thin beds; computer modeling of the folded interbeds confirms both of these as possible causes of seismic response from within the salt diapir. Prediction of the seismic signatures of the interbeds can be made from computer-model studies. \r\n\r\nPetroleum seismic-reflection data are unsatisfactory for mapping the thin beds because of the lack of sufficient resolution to provide direct evidence of the presence of the thin beds. However, indirect evidence, present in these data as discontinuous seismic events, suggests that two geophysical techniques designed for this specific problem would allow direct detection of the interbeds in salt. These techniques are vertical seismic profiling and shallow, short-offset, high-frequency, seismic-reflection recording.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78591","usgsCitation":"Stockton, S., and Balch, A.H., 1978, The utility of petroleum seismic exploration data in delineating structural features within salt anticlines: U.S. Geological Survey Open-File Report 78-591, ii, 36 p. :ill., maps ;27 cm.; (41 p. - PGS), https://doi.org/10.3133/ofr78591.","productDescription":"ii, 36 p. :ill., maps ;27 cm.; (41 p. - PGS)","costCenters":[],"links":[{"id":143644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0591/report-thumb.jpg"},{"id":39150,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0591/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f170","contributors":{"authors":[{"text":"Stockton, S.L.","contributorId":89139,"corporation":false,"usgs":true,"family":"Stockton","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":162965,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balch, Alfred H.","contributorId":71553,"corporation":false,"usgs":true,"family":"Balch","given":"Alfred","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162964,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11331,"text":"ofr78605 - 1978 - Ground-water levels in Wyoming, 1977","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr78605","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-605","title":"Ground-water levels in Wyoming, 1977","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78605","usgsCitation":"Stevens, M.D., 1978, Ground-water levels in Wyoming, 1977: U.S. Geological Survey Open-File Report 78-605, iv, 203 p. :ill., maps ;28 cm. --, https://doi.org/10.3133/ofr78605.","productDescription":"iv, 203 p. :ill., maps ;28 cm. --","costCenters":[],"links":[{"id":143123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0605/report-thumb.jpg"},{"id":39140,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0605/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69855b","contributors":{"authors":[{"text":"Stevens, Marvin D.","contributorId":18774,"corporation":false,"usgs":true,"family":"Stevens","given":"Marvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":162946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10928,"text":"ofr78372 - 1978 - A 500-volt pulse transmitter for ice sounding","interactions":[],"lastModifiedDate":"2024-03-25T19:26:03.621588","indexId":"ofr78372","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-372","title":"A 500-volt pulse transmitter for ice sounding","docAbstract":"A high-voltage pulser developed by the U.S. Geological Survey for glacier soundings is a small battery-operated unit that weighs about one kg and was packaged in a case measuring 8.2 X 12 X 18.8 cm. It operates from an external 12 volt battery and supplies a 500-V pulse to a dipole antenna. The waveform changes shape only slightly for antenna impedances ranging from 20 ohms to thousands of ohms. Shunting a resistive load of 200 ohms with a capacitance of hundreds of pF causes only a very small rounding of the leading corner of the pulse. The pulse-rise time to the full voltage is about 100 nS and fall time to zero is about 150 nS. The 10 to 90-percent rise time is about 60 nS. The total pulse duration is adjustable from about 250 nS to about 1200 nS. Pulse-repetition rates range from 1000 to 10,000 pulses/sec. Maximum battery drain of 3 A occurs at the maximum repetition rate, and is less than 1 A at minimum-repetition rate.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78372","usgsCitation":"Roubique, C.J., 1978, A 500-volt pulse transmitter for ice sounding: U.S. Geological Survey Open-File Report 78-372, 4 p., https://doi.org/10.3133/ofr78372.","productDescription":"4 p.","costCenters":[],"links":[{"id":427063,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0372/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142395,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0372/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd493fe4b0b290850ef066","contributors":{"authors":[{"text":"Roubique, Charles J.","contributorId":70760,"corporation":false,"usgs":true,"family":"Roubique","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11316,"text":"ofr78155 - 1978 - A simple-harmonic model for depicting the annual cycle of seasonal temperatures of streams","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr78155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-155","title":"A simple-harmonic model for depicting the annual cycle of seasonal temperatures of streams","docAbstract":"Due to economic or operational constraints, stream-temperature records cannot always be collected at all sites where information is desired or at frequencies dictated by continuous or near-continuous surveillance requirements. For streams where only periodic measurements are made during the year, and that are not appreciably affected by regulation or by thermal loading , a simple harmonic function may adequately depict the annual seasonal cycle of stream temperature at any given site. Resultant harmonic coefficients obtained from available stream-temperature records may be used in the following ways: (1) To interpolate between discrete measurements by solving the harmonic function at specified times, thereby filling in estimates of stream-temperature values; (2) to characterize areal or regional patterns of natural stream-temperature values; (2) to characterize areal or regional patterns of natural stream-temperature conditions; and (3) to detect and to assess any significant at a site brought about by streamflow regulation or basin development. Moreover, less-than-daily or sampling frequencies at a given site may give estimates of annual variation of stream temperatures that are statistically comparable to estimates obtained from a daily or continuous sampling scheme. The latter procedure may result in potential savings of resources in network operations, with negligible loss in information on annual stream-temperature variations. (Woodard -USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78155","usgsCitation":"Steele, T.D., 1978, A simple-harmonic model for depicting the annual cycle of seasonal temperatures of streams: U.S. Geological Survey Open-File Report 78-155, iii, 16 p. :ill. ;28 cm.; (36 p. - PGS), https://doi.org/10.3133/ofr78155.","productDescription":"iii, 16 p. :ill. ;28 cm.; (36 p. - PGS)","costCenters":[],"links":[{"id":142577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0155/report-thumb.jpg"},{"id":39130,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0155/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6337","contributors":{"authors":[{"text":"Steele, Timothy Doak","contributorId":88723,"corporation":false,"usgs":true,"family":"Steele","given":"Timothy","email":"","middleInitial":"Doak","affiliations":[],"preferred":false,"id":162918,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11644,"text":"ofr78786 - 1978 - Progress toward a ground-water-quality monitoring network for Idaho","interactions":[{"subject":{"id":11644,"text":"ofr78786 - 1978 - Progress toward a ground-water-quality monitoring network for Idaho","indexId":"ofr78786","publicationYear":"1978","noYear":false,"title":"Progress toward a ground-water-quality monitoring network for Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":11645,"text":"ofr791477 - 1979 - A proposed ground water quality monitoring network for Idaho","indexId":"ofr791477","publicationYear":"1979","noYear":false,"title":"A proposed ground water quality monitoring network for Idaho"},"id":1}],"supersededBy":{"id":11645,"text":"ofr791477 - 1979 - A proposed ground water quality monitoring network for Idaho","indexId":"ofr791477","publicationYear":"1979","noYear":false,"title":"A proposed ground water quality monitoring network for Idaho"},"lastModifiedDate":"2015-10-22T11:48:14","indexId":"ofr78786","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-786","title":"Progress toward a ground-water-quality monitoring network for Idaho","docAbstract":"A ground-water-quality monitoring network is being designed for Idaho. The primary objectives of the network are to (1) determine the present quality of the State's ground water, (2) provide continual monitoring of groundwater quality for water-management purposes, and (3) serve as a warning system of undesirable changes in ground-water quality.
\nData are compiled for geohydrologic conditions, groundwater quality, cultural elements, and pollution sources. A \"Hydrologic Unit Priority Index\" is calculated from these data to select priority areas for monitoring purposes.
\nNew ground-water-quality data were collected where existing data were lacking and at some sites that were previously sampled. Old and new data at common sites correlated well, indicating that the water quality has not changed significantly. Most ground water in Idaho is of good quality for common uses; however, water quality may pose problems in local areas. The problems result from both natural and human causes.
\nThe potential for pollution of the aquifers is expected to be greatest in areas of greatest development. In Idaho, population centers and industries tend to be in areas of privately owned irrigated and arable · land. Therefore, these areas are of primary concern for monitoring ground-water quality. Other areas requiring monitoring include those with second-home development, mining and its related processes, and radioactive-waste disposal.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78786","usgsCitation":"Whitehead, R., 1978, Progress toward a ground-water-quality monitoring network for Idaho: U.S. Geological Survey Open-File Report 78-786, Report: 42 p.; 4 Plates: 23.17 x 35.69 inches or smaller, https://doi.org/10.3133/ofr78786.","productDescription":"Report: 42 p.; 4 Plates: 23.17 x 35.69 inches or smaller","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310450,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0786/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":143804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr78786.jpg"},{"id":310451,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0786/plate-2.pdf","text":"Plate 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da49","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":163494,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11435,"text":"ofr78413 - 1978 - Hydrologic data for the Copper Basin area, a potential mining area in Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2023-02-15T21:42:15.73389","indexId":"ofr78413","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-413","title":"Hydrologic data for the Copper Basin area, a potential mining area in Yavapai County, Arizona","docAbstract":"Large low-grade ore bodies have been discovered in Copper Basin, and a large copper-mining operation is anticipated in the near future. Hydrologic data are being collected to provide the data base necessary to determine the effects of a potential mining operation on the water resources of the area. The area of potential depletion or contamination of water supplies is the 50-square-mile alluvial slope downgradient from Copper Basin. In the Copper Basin area the streams generally are dry, except for the perennial flow in a 3-mile-long reach of Kirkland Creek, where the base flow ranges from about 1 to 3 cubic feet per second.
The water in the alluvium, which is more than 1,000 feet thick in places, generally is under unconfined conditions. The direction of ground-water movement is generally southwesterly toward Skull Valley Wash and Kirkland Creek. The depth to water in wells ranges from less than 10 to 675 feet below the land surface. Near the center of the area, test wells penetrate a clay confining bed at the base of the alluvium and an underlying sequence of volcanic rocks, which is more than 1,000 feet thick and contains water under confined conditions.
Pump tests indicate that the confining bed forms a barrier between the water in the alluvium and the water in the volcanic rocks and that, initially, pumping from the volcanic rocks would not affect the water level in the alluvium. The areal extent of the volcanic sequence is not known.
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B. W.","contributorId":39768,"corporation":false,"usgs":true,"family":"Thomsen","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":163136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stulik, R.S.","contributorId":51749,"corporation":false,"usgs":true,"family":"Stulik","given":"R.S.","affiliations":[],"preferred":false,"id":163137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11278,"text":"ofr78451 - 1978 - Geophysical and lithologic logs for 1977 coal drilling in McKenzie County, North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr78451","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-451","title":"Geophysical and lithologic logs for 1977 coal drilling in McKenzie County, North Dakota","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78451","usgsCitation":"Spencer, J.M., 1978, Geophysical and lithologic logs for 1977 coal drilling in McKenzie County, North Dakota: U.S. Geological Survey Open-File Report 78-451, i, 161 leaves :ill., map ;27 cm., https://doi.org/10.3133/ofr78451.","productDescription":"i, 161 leaves :ill., map ;27 cm.","costCenters":[],"links":[{"id":143216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0451/report-thumb.jpg"},{"id":39079,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0451/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c260","contributors":{"authors":[{"text":"Spencer, John M.","contributorId":79883,"corporation":false,"usgs":true,"family":"Spencer","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162851,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11640,"text":"ofr78256 - 1978 - Nuclear power reactor sites in the southeastern United States","interactions":[],"lastModifiedDate":"2022-09-28T14:59:25.569756","indexId":"ofr78256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-256","title":"Nuclear power reactor sites in the southeastern United States","docAbstract":"This report describes nuclear power reactor sites in the southeastern United States. The map indicates the location of all sites as of July 1976 in the conterminous United States, and a later published report will include all sites. The project is one of several in the National Environmental Overview Program of the U.S. Geological Survey which will identify and summarize geologic, hydrologic, and topographic topics associated with future energy, mineral resource, and land use development in the United States.
The increasing use of atomic energy creates a need for the dissemination of information about nuclear reactors. Because power plant safety is related, in part, to the geology and seismology of the plant area and surroundings, this study is focused primarily on that relationship.
Information about the geology and seismology is summarized from reports prepared by consultants to utility companies and submitted by the companies to the U.S. Nuclear Regulatory Commission (formerly the U.S. Atomic Energy Commission) in support of the application for a construction permit.
Coordinates for site locations were established by the author from descriptive information in the reports. The U.S. Geological Survey 7-1/2 minute topographic maps were used in confirming the geographic location of the sites. The coordinates may in some cases represent the planned location rather than the exact actual location.
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R.","affiliations":[],"preferred":false,"id":163777,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11639,"text":"ofr78433 - 1978 - Nuclear power reactor sites in the Great Lakes Region of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr78433","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-433","title":"Nuclear power reactor sites in the Great Lakes Region of the United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78433","usgsCitation":"West, M., 1978, Nuclear power reactor sites in the Great Lakes Region of the United States: U.S. Geological Survey Open-File Report 78-433, 24 leaves :fold. map ;28 cm., https://doi.org/10.3133/ofr78433.","productDescription":"24 leaves :fold. map ;28 cm.","costCenters":[],"links":[{"id":145103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0433/report-thumb.jpg"},{"id":39496,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0433/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39497,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0433/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69689d","contributors":{"authors":[{"text":"West, Mareta","contributorId":64221,"corporation":false,"usgs":true,"family":"West","given":"Mareta","affiliations":[],"preferred":false,"id":163488,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11315,"text":"ofr78226 - 1978 - Hydrologic reconnaissance of the Yampa River during low flow, Dinosaur National Monument, northwestern Colorado","interactions":[],"lastModifiedDate":"2018-10-25T10:40:54","indexId":"ofr78226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-226","title":"Hydrologic reconnaissance of the Yampa River during low flow, Dinosaur National Monument, northwestern Colorado","docAbstract":"A hydrologic reconnaissance of a 74-kilometer reach of the Yampa River in Dinosaur National Monument was made during low flow in mid-August 1976. Stream discharge, which was measured along this reach every 16 to 24 kilometers, ranged from 9.4 to 10.6 cubic meters per second. Variations in streamflow were explained, in part, by underflow, loss to ground water, and evaporation. Specific conductance was measured about every 2 kilometers and indicated a downstream increase on the order of 11 to 12 percent for the reach. Except for mercury, bottom-sediment trace-element concentrations in the study reach were less than maximum concentrations determined during August-September 1976 for bottom sediments at unperturbed sites upstream in the Yampa River basin. At one of five sampling sites, the mercury concentration in bottom sediments exceeded the maximum measured upstream level.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78226","usgsCitation":"Steele, T.D., Wentz, D.A., and Warner, J.W., 1978, Hydrologic reconnaissance of the Yampa River during low flow, Dinosaur National Monument, northwestern Colorado: U.S. Geological Survey Open-File Report 78-226, ii, 10 p., https://doi.org/10.3133/ofr78226.","productDescription":"ii, 10 p.","costCenters":[],"links":[{"id":142576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0226/report-thumb.jpg"},{"id":358795,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0226/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Dinosaur National Monument","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.05029296875,\n 40.43022363450862\n ],\n [\n -108.50372314453125,\n 40.43022363450862\n ],\n [\n -108.50372314453125,\n 40.71603763556807\n ],\n [\n -109.05029296875,\n 40.71603763556807\n ],\n [\n -109.05029296875,\n 40.43022363450862\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60545d","contributors":{"authors":[{"text":"Steele, Timothy Doak","contributorId":88723,"corporation":false,"usgs":true,"family":"Steele","given":"Timothy","email":"","middleInitial":"Doak","affiliations":[],"preferred":false,"id":162916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wentz, Dennis A. dawentz@usgs.gov","contributorId":1838,"corporation":false,"usgs":true,"family":"Wentz","given":"Dennis","email":"dawentz@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":162915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warner, James W.","contributorId":106119,"corporation":false,"usgs":true,"family":"Warner","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":162917,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11451,"text":"ofr78113 - 1978 - Geologic map of the Viejas Mountain Quadrangle, San Diego County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr78113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-113","title":"Geologic map of the Viejas Mountain Quadrangle, San Diego County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78113","usgsCitation":"Todd, V., 1978, Geologic map of the Viejas Mountain Quadrangle, San Diego County, California: U.S. Geological Survey Open-File Report 78-113, 21 leaves, 8 leaves of ill. :ill., maps (1 fold.) ;28 cm.; (30 p. - PGS), https://doi.org/10.3133/ofr78113.","productDescription":"21 leaves, 8 leaves of ill. :ill., maps (1 fold.) ;28 cm.; (30 p. - PGS)","costCenters":[],"links":[{"id":108523,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14605.htm","linkFileType":{"id":5,"text":"html"},"description":"14605"},{"id":144817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0113/report-thumb.jpg"},{"id":39314,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0113/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39315,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a1c6","contributors":{"authors":[{"text":"Todd, Victoria R.","contributorId":87544,"corporation":false,"usgs":true,"family":"Todd","given":"Victoria R.","affiliations":[],"preferred":false,"id":163159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10780,"text":"ofr78304 - 1978 - Ground-water pollution by nitrogen compounds at Olean, New York; progress report, June 1977","interactions":[],"lastModifiedDate":"2013-02-15T07:38:50","indexId":"ofr78304","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-304","title":"Ground-water pollution by nitrogen compounds at Olean, New York; progress report, June 1977","docAbstract":"Ground water in an area in Olean, New York contains high concentrations of nitrogen compounds, which are being slowly flushed from the aquifer as the ground water flows toward a nearby well field where it is pumped out. Construction and regular use of a new production well in the area of nitrogen-rich water would temporarily increase the rate of nitrogen removal by causing more rapid flow of water from the silty upper part of the aquifer downward to the more permeable lower part, and by reducing the distance the water must flow through the lower part to the nearest point of withdrawal. After such a well had been in use for several months and the system had adjusted to the new conditions, the rate of further nitrogen removal would depend on the rate at which nitrogen compounds are leached from the soil by infiltrating precipitation. Alternative techniques for speeding the flushing of the aquifer include artificially increasing the amount of infiltration, changing the rates of withdrawal from existing production wells, and pumping shallow low-yield wells in the area of nitrogen-rich water. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78304","usgsCitation":"Randall, A.D., 1978, Ground-water pollution by nitrogen compounds at Olean, New York; progress report, June 1977: U.S. Geological Survey Open-File Report 78-304, ii, 20 p. :maps ;29 cm., https://doi.org/10.3133/ofr78304.","productDescription":"ii, 20 p. :maps ;29 cm.","costCenters":[],"links":[{"id":145075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":267456,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0304/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66742e","contributors":{"authors":[{"text":"Randall, Allan D. arandall@usgs.gov","contributorId":1168,"corporation":false,"usgs":true,"family":"Randall","given":"Allan","email":"arandall@usgs.gov","middleInitial":"D.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":161951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10938,"text":"ofr78411 - 1978 - Water quality in the Old Plantation Water Control District, Broward County, Florida; progress report, July 1976-June 1977","interactions":[],"lastModifiedDate":"2023-02-15T21:48:36.5022","indexId":"ofr78411","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-411","title":"Water quality in the Old Plantation Water Control District, Broward County, Florida; progress report, July 1976-June 1977","docAbstract":"Water quality in the Old Plantation Water Control District in Broward County, Florida has been affected by effluent from sewage-treatment plants, agriculture, and storm-water runoff. Effect of the effluent from sewage-treatment plants on water quality was evident at 3 sites where concentrations of nutrients and bacteria in the Broward County canals exceeded state standards of 2,400 colonies per 100 milliliters for total coliform bacteria, and where at 2 of the 3 sites the fecal coliform/fecal streptococcus ratios indicated possible human contamination. The effect of agriculture on water quality was evident where relatively high levels of chlorinated hydrocarbon insecticides had concentrated in the bottom sediments of the canals. For example, DDD reached levels of 330 micrograms per kilogram at site 3. The effects of storm-water runoff on water quality were detected during the wet season when concentrations of several trace elements increased. For example, zinc averaged 30 micrograms per milliliter in the wet season compared with 20 micrograms per milliliter during the dry season.
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Gary M.","contributorId":42973,"corporation":false,"usgs":true,"family":"Russell","given":"Gary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanson, Chris E.","contributorId":21966,"corporation":false,"usgs":true,"family":"Hanson","given":"Chris","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162238,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pitt, William A.J.","contributorId":50904,"corporation":false,"usgs":true,"family":"Pitt","given":"William","email":"","middleInitial":"A.J.","affiliations":[],"preferred":false,"id":162240,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11132,"text":"ofr78789 - 1978 - Longitudinal turbidity structures in a bar-built coastal plain estuary, Corpus Christi Bay, Texas","interactions":[],"lastModifiedDate":"2023-02-24T17:31:50.82782","indexId":"ofr78789","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-789","title":"Longitudinal turbidity structures in a bar-built coastal plain estuary, Corpus Christi Bay, Texas","docAbstract":"Corpus Christi Bay is a shallow, bar-built variety of estuary that is characteristic of the South Texas Coastal Plain. On the basis of synoptic in situ measurements of light transmissivity and suspended-sediment concentrations at six monitoring stations, a time sequence of six turbidity structures was established along the longitudinal trend of the bay and its tidal inlet over a 16-month observation period. The bay turbidity structures were observed to be highly variable in time and space. Structures ranged from a vertically homogeneous water column, to a well-stratified column exhibiting an increasing turbidity gradient with depth. Wind appeared to be the dominant forcing agent influencing turbidity toward the bayhead sector, where it both generates waves for bottom-sediment resuspension and regulates fluvial sediment influx from the Nueces River. Turbidity toward the baymouth sector appeared to be dominantly regulated by tidal forcing effects from Aransas Pass inlet. Both the discharge characteristics of the Nueces River and the mean density of the bay's water column had no discernible influence on the observed bay turbidity structures.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78789","usgsCitation":"Shideler, G.L., 1978, Longitudinal turbidity structures in a bar-built coastal plain estuary, Corpus Christi Bay, Texas: U.S. Geological Survey Open-File Report 78-789, 34 p., https://doi.org/10.3133/ofr78789.","productDescription":"34 p.","costCenters":[],"links":[{"id":413412,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0789/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143562,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0789/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Corpus Christi Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -97.51778699827092,\n 27.89456789643843\n ],\n [\n -97.51778699827092,\n 27.68326330727676\n ],\n [\n -97.10734729025134,\n 27.68326330727676\n ],\n [\n -97.10734729025134,\n 27.89456789643843\n ],\n [\n -97.51778699827092,\n 27.89456789643843\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640a98","contributors":{"authors":[{"text":"Shideler, Gerald L.","contributorId":89137,"corporation":false,"usgs":true,"family":"Shideler","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":162600,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}