The purpose of this report, which was prepared in cooperation with the City of Houston, the Harris-Galveston Coastal Subsidence District, and the Texas Department of Water Resources, is to show the altitudes of water levels in wells in the Chicot and Evangeline aquifers in the Houston, Texas, metropolitan area. The maps are based on water-level measurements in spring of 1982 in about 550 wells.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82559","usgsCitation":"Ranzau, C., and Strause, J.L., 1982, Approximate altitude of water levels in wells in the Chicot and Evangeline aquifers in the Houston area, Texas, spring 1982: U.S. Geological Survey Open-File Report 82-559, 2 Plates: 14.64 x 10.77 inches and 14.95 x 10.74 inches, https://doi.org/10.3133/ofr82559.","productDescription":"2 Plates: 14.64 x 10.77 inches and 14.95 x 10.74 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":79572,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0559/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79573,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0559/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79574,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0559/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0559/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a22b","contributors":{"authors":[{"text":"Ranzau, C.E. Jr.","contributorId":41831,"corporation":false,"usgs":true,"family":"Ranzau","given":"C.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":225625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strause, Jeffrey L.","contributorId":61420,"corporation":false,"usgs":true,"family":"Strause","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225626,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10993,"text":"ofr821058 - 1982 - A model for hydrostatic consolidation of Pierre Shale","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr821058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1058","title":"A model for hydrostatic consolidation of Pierre Shale","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821058","usgsCitation":"Savage, W.Z., 1982, A model for hydrostatic consolidation of Pierre Shale: U.S. Geological Survey Open-File Report 82-1058, 23 p., ill. ;28 cm., https://doi.org/10.3133/ofr821058.","productDescription":"23 p., ill. ;28 cm.","costCenters":[],"links":[{"id":143352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1058/report-thumb.jpg"},{"id":38759,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf73","contributors":{"authors":[{"text":"Savage, W. Z.","contributorId":106481,"corporation":false,"usgs":true,"family":"Savage","given":"W.","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":162345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10693,"text":"ofr82177 - 1982 - USGS Mineralogy Laboratory user's guide to the TECO editing program for the DEC RT-11 operating system; Part C","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr82177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-177","title":"USGS Mineralogy Laboratory user's guide to the TECO editing program for the DEC RT-11 operating system; Part C","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82177","usgsCitation":"Phillips, R., and Hauff, P.L., 1982, USGS Mineralogy Laboratory user's guide to the TECO editing program for the DEC RT-11 operating system; Part C: U.S. Geological Survey Open-File Report 82-177, ii, 42 p., ill. ;28 cm., https://doi.org/10.3133/ofr82177.","productDescription":"ii, 42 p., ill. ;28 cm.","costCenters":[],"links":[{"id":144297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0177/report-thumb.jpg"},{"id":38509,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0177/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611717","contributors":{"authors":[{"text":"Phillips, R.E.","contributorId":51241,"corporation":false,"usgs":true,"family":"Phillips","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":161809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hauff, P. L.","contributorId":95470,"corporation":false,"usgs":true,"family":"Hauff","given":"P.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11000,"text":"ofr821095 - 1982 - GLORIA sidescan and seismic data collected by the DESV STARELLA along the continental slope and upper continental rise of the Eastern United States in 1979","interactions":[],"lastModifiedDate":"2018-06-19T08:27:45","indexId":"ofr821095","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1095","title":"GLORIA sidescan and seismic data collected by the DESV STARELLA along the continental slope and upper continental rise of the Eastern United States in 1979","docAbstract":"A cruise on the- DESV STARELLA was conducted between October 23. 1979, and November 8, 1979, by the U.S. Geologic.al Survey (USGS) in cooperation with the United Kingdom's Institute of Oceanographic Sciences (IOS). The purpose of the study was to gain an overview of the morphology of large areas of the Continental Slope and upper Continental Rise off the eastern ·united States. Sidescan-sonar and single-channel seismic-reflection data were collected along the tracklines. The ship's position. was monitored using LORAN_C and satellite navigation techniques.
The sidescan data were collected using the !OS-developed Geologic Long-Range Inclined Asdic, Mark II (GLORIA II) system. GLORIA was operated at either a 20-second or 40-second sweep, giving maximum slant-range distances of 15 or 30 kilometers, respectively, to each side of the towed fish. The sidescan data were collected on graphic recorders and analog tapes. The tapes were played onto photographic paper in a facsimile machine; then these prints were photographically stretched to produce approximately isometric images .. The images were not corrected for slant-range distortion. Mosaics at a scale of 1:250,000 (Mercator projection) were made from the photographic images.
The seismic· data consist of 40-in3 airgun and 10-kHz echo-sounder profiles. The airgun data were recorded on EPC recorders at both 8- and 4- second sweep rates. The 10-kHz echo-sounder data were recorded on a wet-paper recorder at a 2-second sweep rate.
Approximately 4,820 km of seismic and sonar-data wera collected from four areas of interest and along the lines connecting those areas. Area 1 includes the Continental Slope and upper Rise seaward of Georges Bank, between Northeast Channel and Alvin Canyon. Numerous lines were run here, resulting in approximately 2,500 km of seismic data and complete and overlapping GLORIA coverage of the area. A similar survey, consisting of approximately 1 2 200 km of trackline, was run in area 2, which includes the Continental Slope and upper Rise seaward of the middle Atlantic states between Hudson Canyon and Baltimore Canyon. A single line, 250 km long, was run through area 3 along the base of the Continental Slope from Cape Hatteras to latitude 33°N. off North and South Carolina. Two parallel lines, totaling 870 km, were run through area 4 along the Blake Escarpment, from the Blake Spur south to latitude 27°40'N. One line was run along the top of the escarpment and the other was run along the base of the escarpment.
All the data can be studied at the U.S. Geological Survey offices in Woods Hole, MA 02543. Microfilm copies of the sidescan-monitor record as well as the airgun and 10-kHz profiles can be purchased only from the National Geophysical Data Center, NOAA, Code E64, 325 Broadway, Boulder, CO 80303 (303/497-6338). Photographic copies of the GLORIA mosaics can also be obtained only from this address.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr821095","usgsCitation":"Scanlon, K.M., 1982, GLORIA sidescan and seismic data collected by the DESV STARELLA along the continental slope and upper continental rise of the Eastern United States in 1979: U.S. Geological Survey Open-File Report 82-1095, 3 p., https://doi.org/10.3133/ofr821095.","productDescription":"3 p.","costCenters":[],"links":[{"id":143369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr821095.PNG"},{"id":259857,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1095/ofr19821095.pdf","text":"Report","size":"1.94 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-1095"}],"contact":"Coastal and Marine Geology Program U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82982","usgsCitation":"Schafer, C.M., Conte, C.J., and Fleischer, M., 1982, List of published articles on mineralogy and geochemistry for which translations by U.S. Geological Survey members are deposited at the USGS Library in Reston, Virginia: U.S. Geological Survey Open-File Report 82-982, 129 p., https://doi.org/10.3133/ofr82982.","productDescription":"129 p.","costCenters":[],"links":[{"id":144074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0982/report-thumb.jpg"},{"id":38779,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0982/report.pdf","text":"Report","size":"1.39 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f36","contributors":{"authors":[{"text":"Schafer, Constance M.","contributorId":67092,"corporation":false,"usgs":true,"family":"Schafer","given":"Constance","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conte, Constance J.","contributorId":80284,"corporation":false,"usgs":true,"family":"Conte","given":"Constance","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":162371,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10613,"text":"ofr811011 - 1982 - Ground-water quality in east-central Idaho valleys","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr811011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1011","title":"Ground-water quality in east-central Idaho valleys","docAbstract":"From May through November 1978, water quality, geologic, and hydrologic data were collected for 108 wells in the Lemhi, Pahsimeroi, Salman River (Stanley to Salmon), Big Lost River, and Little Lost River valleys in east-central Idaho. Data were assembled to define, on a reconnaissance level, water-quality conditions in major aquifers and to develop an understanding of factors that affected conditions in 1978 and could affect future ground-water quality. Water-quality characteristics determined include specific conductance, pH, water temperature, major dissolved cations, major dissolved anions, and coliform bacteria. Concentrations of hardness, nitrite plus nitrate, coliform bacteria, dissolved solids, sulfate, chloride, fluoride , iron, calcium, magnesium, sodium, potassium or bicarbonate exceed public drinking water regulation limits or were anomalously high in some water samples. Highly mineralized ground water probably is due to the natural composition of the aquifers and not to surface contamination. Concentrations of coliform bacteria that exceed public drinking water limits and anomalously high dissolved nitrite-plus-nitrite concentrations are from 15- to 20-year old irrigation wells in heavily irrigated or more densely populated areas of the valleys. Ground-water quality and quantity in most of the study area are sufficient to meet current (1978) population and economic demands. Ground water in all valleys is characterized by significant concentrations of calcium, magnesium, and bicarbonate plus carbonate ions. Variations in the general trend of ground-water composition (especially in the Lemhi Valley) probably are most directly related to variability in aquifer lithology and proximity of sampling site to source of recharge. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811011","usgsCitation":"Parliman, D., 1982, Ground-water quality in east-central Idaho valleys: U.S. Geological Survey Open-File Report 81-1011, 62 p., 3 over-size sheets, ill., maps ;35 cm., https://doi.org/10.3133/ofr811011.","productDescription":"62 p., 3 over-size sheets, ill., maps ;35 cm.","costCenters":[],"links":[{"id":142548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1011/report-thumb.jpg"},{"id":38446,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1011/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38447,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1011/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38448,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1011/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667390","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":161682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11012,"text":"ofr8257 - 1982 - Regional neotectonic analysis of the Sonoran Desert","interactions":[],"lastModifiedDate":"2021-09-20T18:58:17.291385","indexId":"ofr8257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-57","title":"Regional neotectonic analysis of the Sonoran Desert","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8257","usgsCitation":"Schell, B.A., and Wilson, K.L., 1982, Regional neotectonic analysis of the Sonoran Desert: U.S. Geological Survey Open-File Report 82-57, Report: 60 p.; 2 Plates: 29.88 × 59.25 inches and \t29.88 × 64.31 inches, https://doi.org/10.3133/ofr8257.","productDescription":"Report: 60 p.; 2 Plates: 29.88 × 59.25 inches and \t29.88 × 64.31 inches","costCenters":[],"links":[{"id":389492,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13764.htm"},{"id":38782,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38781,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0057/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38780,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0057/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143177,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0057/report-thumb.jpg"}],"country":"Mexico, United States","state":"Arizona, California, Nevada","otherGeospatial":"Sonoran Desert","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.0,\n 31.3240\n ],\n [\n -110.0,\n 31.3240\n ],\n [\n -110.0,\n 36.9170\n ],\n [\n -117.0,\n 36.9170\n ],\n [\n -117.0,\n 31.3240\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634e96","contributors":{"authors":[{"text":"Schell, B. A.","contributorId":77151,"corporation":false,"usgs":true,"family":"Schell","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":162377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, K. L.","contributorId":75535,"corporation":false,"usgs":true,"family":"Wilson","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":162376,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11014,"text":"ofr82551 - 1982 - Continuous water sampling and water analysis in estuaries","interactions":[],"lastModifiedDate":"2016-07-27T11:57:29","indexId":"ofr82551","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-551","title":"Continuous water sampling and water analysis in estuaries","docAbstract":"Salinity, temperature, light transmission, oxygen saturation, pH, pCO2, chlorophyll a fluorescence, and the concentrations of nitrate, nitrite, dissolved silica, orthophosphate, and ammonia are continuously measured with a system designed primarily for estuarine studies. Near-surface water (2-m depth) is sampled continuously while the vessel is underway; on station, water to depths of 100 m is sampled with a submersible pump. The system is comprised of commercially available instruments, equipment, and components, and of specialized items designed and fabricated by the authors. Data are read from digital displays, analog strip-chart recorders, and a teletype printout, and can be logged in disc storage for subsequent plotting. Data records made in San Francisco Bay illustrate physical, biological, and chemical estuarine processes, such as mixing and phytoplankton net production. The system resolves large- and small-scale events, which contributes to its reliability and usefulness.
","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82551","usgsCitation":"Schemel, L., and Dedini, L., 1982, Continuous water sampling and water analysis in estuaries: U.S. Geological Survey Open-File Report 82-551, 28 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82551.","productDescription":"28 p., ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":143179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0551/report-thumb.jpg"},{"id":38784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0551/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e86","contributors":{"authors":[{"text":"Schemel, L. E.","contributorId":89529,"corporation":false,"usgs":true,"family":"Schemel","given":"L. E.","affiliations":[],"preferred":false,"id":162381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dedini, L.A.","contributorId":54996,"corporation":false,"usgs":true,"family":"Dedini","given":"L.A.","affiliations":[],"preferred":false,"id":162380,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11022,"text":"ofr82991 - 1982 - Petrographic study of sandstones from measured sections of the Morrison Formation and related units, southwestern San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82991","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-991","title":"Petrographic study of sandstones from measured sections of the Morrison Formation and related units, southwestern San Juan Basin, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82991","usgsCitation":"Schmitt, L., 1982, Petrographic study of sandstones from measured sections of the Morrison Formation and related units, southwestern San Juan Basin, New Mexico: U.S. Geological Survey Open-File Report 82-991, 63 p., map ;28 cm., https://doi.org/10.3133/ofr82991.","productDescription":"63 p., map ;28 cm.","costCenters":[],"links":[{"id":143224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0991/report-thumb.jpg"},{"id":38789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0991/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881a0","contributors":{"authors":[{"text":"Schmitt, L.J.","contributorId":48565,"corporation":false,"usgs":true,"family":"Schmitt","given":"L.J.","affiliations":[],"preferred":false,"id":162392,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11723,"text":"ofr82313 - 1982 - Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr82313","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-313","title":"Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis","docAbstract":"Published and unpublished data on 2575 fluid inclusions in ore and gangue minerals from the Creede, Colorado, Ag-Pb-Zn-Cu vein deposit collected in our laboratories from 1959 to 1981 have shown that the average salinity (wt. % NaCl equivalent, hereinafter termed wt.% eq.) and homogenization temperature (Th), and the ranges of these two parameters for fluid inclusions in sphalerite, quartz, fluorite, and rhodochrosite, respectively, are 8.1 (4.6 - 13.4), 239?C (195-274?C); 6.1 (1.1-10.0), 260?C (190->400?C); 10.7 (6.1-11.1), 217?C (213-229?C) and 260?C (247-268?C) (bimodal distribution of Th); and 9.9 (9.3 - 10.6), 214?C (185-249?C). Inclusions have been measured in minerals from four of the five stages of mineralization previously recognized at Creede. The few inclusions of fluids depositing rhodochrosite (A-stage, earliest in the paragenesis) yield Th and salinity values more similar to those of the low-temperature (average Th 217?C) fluids forming some of the much later fluorite (C-stage) than to any of the other fluids. Th measurements on A-stage quartz range from 192?C to 263?C and average 237?C. The early, fine-grained, B-stage sphalerites yielded Th of 214 to 241?C and salinities of 6.1 to 10.2 wt. % eq. \r\n\r\nD-stage sphalerite (late in the paragenesis) has been studied in detail (growth-zone by growth-zone) for several localities along the OH vein and reveals a generally positive correlation among Th, salinity and iron content of the host sphalerite. The deposition of D-stage sphalerite was characterized by repeated cycling through different regions of salinity/Th space, as Th and salinity generally decreased with time. Seventeen salinity-Th measurements were made on D-stage sphalerite from one locality on the Bulldog Mountain vein system, which, like the OH vein, is one of four major ore-producing vein systems at Creede. These data suggest a lower Th for a given salinity fluid from sphalerite on the Bulldog Mountain vein than on the OH vein. The very high values of Th for some quartz samples (mostly D-stage) are believed to be a result of the trapping of both gas and liquid from a boiling fluid in the upper levels of the vein system. Boiling of fluids depositing D-stage quartz is indicated by the presence of steam inclusions in quartz and the extreme variability of Th values measured on quartz. The pressure was low (< 125 kg/cm 2) throughout ore deposition. \r\n\r\nThree major growth zones in D-stage sphalerite are recognized throughout the OH vein. Deposition of the first major zone began from fluids having intermediate salinities and temperatures (7.8-9.2 wt. % eq., 240?C) but the characteristics of the fluids oscillated after that, ranging from 7.2 to 10.1 wt. % eq. and from 225?C to 270?C. Deposition of the second major, most Fe-rich zone began with the hottest, most saline fluids present during D-stage mineralization (. 270?C, 10.5-12.5 wt. % eq., 3 mole % FeS in sphalerite). The fluid then oscillated with respect to Th and salinity (213-274?C, 5.2-12.5 wt. % eq.) but showed a general decrease in both with time. Deposition of the youngest major zone began with a very Fe-poor sphalerite (0.25-0.75 mole % FeS), from the least saline, coolest fluids (5-6.5 wt. % eq., 200-212?C) and ended with a trend of increasing temperature at approximately constant salinity.\r\n\r\nThe fluid-inclusion data can best be explained by a mixing model involving at least two fluids--one hot and saline, the other cool and fresher. Sudden changes in the mixing ratio, presumably from changes in the plumbing, punctuated long periods of remarkably uniform conditions of ore fluid flow and deposition. The effects of other processes such as convection and heat exchange with wall rocks must have been superimposed on this simple mixing model, however. In contrast to an earlier interpretation, several aspects of the inclusion data may be interpreted to suggest exceedingly slow ore deposition. Work in progress may resolve some of these ambiguities and refine","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82313","usgsCitation":"Woods, T., Roedder, E., and Bethke, P.M., 1982, Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis: U.S. Geological Survey Open-File Report 82-313, 77 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82313.","productDescription":"77 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":143786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0313/report-thumb.jpg"},{"id":39610,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0313/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de77a","contributors":{"authors":[{"text":"Woods, T.L.","contributorId":6052,"corporation":false,"usgs":true,"family":"Woods","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":163620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roedder, Edwin","contributorId":25571,"corporation":false,"usgs":true,"family":"Roedder","given":"Edwin","affiliations":[],"preferred":false,"id":163621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bethke, P. M.","contributorId":32921,"corporation":false,"usgs":true,"family":"Bethke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163622,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10619,"text":"ofr811121 - 1982 - Water resources of the Ochlockonee River area, northwest Florida","interactions":[],"lastModifiedDate":"2022-08-31T19:15:04.672539","indexId":"ofr811121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1121","title":"Water resources of the Ochlockonee River area, northwest Florida","docAbstract":"The Ochlockonee River area comprises about 1,420 square miles in the panhandle of northwest Florida. In 1975, the population of the area was about 48,000. Water use averaged 11.4 million gallons per day; about half was pumped from wells and half from streams.
The area receives 57 inches of precipitation per year on the average. Much of this water enters the surficial sand aquifer, seeps to streams, or enters the underlying water-bearing zone of the upper confining unit and the Floridan aquifer.
The water-bearing zone of the upper confining unit is used for rural domestic supplies and is also important because the water it stores is a source of recharge to the underlying Floridan aquifer.
The Floridan aquifer underlies all of the Ochlockonee River area and, except for the city of Quincy, is the principal source of municipal water supply. Well yields range from as little as 20 gallons per minute in Gadsden County to as much as 4,500 gallons per minute in Leon County. The transmissivity of the Floridan aquifer ranges from about 170 feet squared per day in the southern part of the area to 5,100 feet squared per day in the northern part. Storage coefficients calculated from two aquifer tests are 2 x 10-4 and 2.6 x 10-4. At Tallahassee, directly east of the Ochlockonee River, transmissivity is as high as 130,000 feet squared per day. The Floridan aquifer is recharged by downward leakage of water from the surficial sand aquifer and from the water-bearing zone of the upper confining unit. The Floridan aquifer is also recharged directly by rainfall in northern Leon County and in southern Georgia where it is near or at land surface. Ground water moves toward the southeast from the potentiometric high in southwestern Gadsden County and south from Leon County toward Wakulla Springs, located about 10 miles south of Tallahassee. The potentiometric surface of the upper part of the Floridan aquifer ranges from about 50 feet higher than that of the middle and lower part of the Floridan aquifer in southwestern Gadsden County to about 10 feet higher near Midway in eastern Gadsden County. The aquifer discharge in the basin area is by wells and by natural discharge through seeps and springs along the Ochlockonee River and at Ochlockonee Bay.
Water levels in the Floridan aquifer fluctuate in response to seasonal and long-term variations in rainfall. Hydrographs do not show evidence of any long-term water-level declining trend.
Saline water (more than 1,000 milligrams per liter of dissolved solids) occurs naturally within the Floridan aquifer throughout the Ochlockonee River area at depths ranging from 200 to 600 feet below sea level. The depth below which dissolved solids in water exceed 500 milligrams per liter in the Havana area ranges from 200 to 250 feet below sea level; in the Quincy area, from 400 to 450 feet below; and in the Greensboro area, from 200 to 250 feet below.
Concentrations of dissolved solids in water pumped from wells tapping the Floridan aquifer in the Ochlockonee River area range from 60 to 1,370 milligrams per liter; chloride from 0 to 630 milligrams per liter; sulfate from 0.0 to 280 milligrams per liter; and fluoride from 0.0 to 1.3 milligrams per liter.
Streamflow originating in the Ochlockonee River area in Florida averages about 1,000 million gallons per day; minimum discharge during dry periods is about 285 million gallons per day. Stream yields range from 0.90 to 2.62 cubic feet per second per square mile. Quincy Creek, at State Highway 267 at Quincy, the primary source of water for the city of Quincy, yields an average flow of 19 million gallons per day, has a 7-day 10-year low flow of 2.8 million gallons per day, and contains water of acceptable quality. The chemical quality of most streams in the basin is acceptable for most uses. Dissolved-solids concentration is generally less than 135 milligrams per liter; pH ranges from 5.3 to 7.3 units; color from 20 to 90 platinum-cobalt units; and turbidity from 3 to 85 Jackson turbidity units. Variations in chloride concentration in water from the Ochlockonee River (5.2 to 140 milligrams per liter) are influenced by discharge of food processing waste and municipal sewage plant effluent to the river.
The three large lakes in the basin range from 4,000 to 7,000 acres in surface area. All are now used primarily for recreation. Dissolved-solids concentrations of water from the lakes range from less than 20 to 50 milligrams per liter. A major flood occurred in 1975 when the Ochlockonee River near Havana reached the third highest stage of record and the peak flood at the Sopchoppy River exceeded that for the period of record (11 years in 1975); no significant damage occurred.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811121","collaboration":"Prepared in cooperation with the Northwest Florida Water Management District, Gadsden County and the City of Quincy","usgsCitation":"Pascale, C.A., and Wagner, J.R., 1982, Water resources of the Ochlockonee River area, northwest Florida: U.S. Geological Survey Open-File Report 81-1121, vii, 114 p., https://doi.org/10.3133/ofr811121.","productDescription":"vii, 114 p.","costCenters":[],"links":[{"id":406025,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1121/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1121/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Ochlockonee River area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.75814819335936,\n 29.846599772557077\n ],\n [\n -84.38735961914062,\n 29.846599772557077\n ],\n [\n -84.38735961914062,\n 30.198552988693212\n ],\n [\n -84.75814819335936,\n 30.198552988693212\n ],\n [\n -84.75814819335936,\n 29.846599772557077\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0499","contributors":{"authors":[{"text":"Pascale, Charles A.","contributorId":99978,"corporation":false,"usgs":true,"family":"Pascale","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, Jeffry R.","contributorId":48179,"corporation":false,"usgs":true,"family":"Wagner","given":"Jeffry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11037,"text":"ofr82402 - 1982 - Application of computer graphics to generate coal resources of the Cache coal bed, Recluse geologic model area, Campbell County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82402","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-402","title":"Application of computer graphics to generate coal resources of the Cache coal bed, Recluse geologic model area, Campbell County, Wyoming","docAbstract":"Low-sulfur subbituminous coal resources have been calculated, using both manual and computer methods, for the Cache coal bed in the Recluse Model Area, which covers the White Tail Butte, Pitch Draw, Recluse, and Homestead Draw SW 7 1/2 minute quadrangles, Campbell County, Wyoming. Approximately 275 coal thickness measurements obtained from drill hole data are evenly distributed throughout the area. The Cache coal and associated beds are in the Paleocene Tongue River Member of the Fort Union Formation. The depth from the surface to the Cache bed ranges from 269 to 1,257 feet. The thickness of the coal is as much as 31 feet, but in places the Cache coal bed is absent. Comparisons between hand-drawn and computer-generated isopach maps show minimal differences. Total coal resources calculated by computer show the bed to contain 2,316 million short tons or about 6.7 percent more than the hand-calculated figure of 2,160 million short tons.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82402","usgsCitation":"Schneider, G.B., Crowley, S., and Carey, M., 1982, Application of computer graphics to generate coal resources of the Cache coal bed, Recluse geologic model area, Campbell County, Wyoming: U.S. Geological Survey Open-File Report 82-402, 17 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82402.","productDescription":"17 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0402/report-thumb.jpg"},{"id":38801,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0402/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aaac","contributors":{"authors":[{"text":"Schneider, G. B.","contributorId":102077,"corporation":false,"usgs":true,"family":"Schneider","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":162422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crowley, S.S.","contributorId":43754,"corporation":false,"usgs":true,"family":"Crowley","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":162420,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carey, M.A.","contributorId":62581,"corporation":false,"usgs":true,"family":"Carey","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":162421,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11042,"text":"ofr82626 - 1982 - Discussion of proposed rule in Federal Register, 10 CFR Part 60, pertaining to ground-water travel time; an appendix to report by Sandia National Laboratories to U.S. Nuclear Regulatory Commission, assessing the technical criteria for geologic disposal of high-level radioactive waste","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82626","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-626","title":"Discussion of proposed rule in Federal Register, 10 CFR Part 60, pertaining to ground-water travel time; an appendix to report by Sandia National Laboratories to U.S. Nuclear Regulatory Commission, assessing the technical criteria for geologic disposal of high-level radioactive waste","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82626","usgsCitation":"Schneider, R., 1982, Discussion of proposed rule in Federal Register, 10 CFR Part 60, pertaining to ground-water travel time; an appendix to report by Sandia National Laboratories to U.S. Nuclear Regulatory Commission, assessing the technical criteria for geologic disposal of high-level radioactive waste: U.S. Geological Survey Open-File Report 82-626, 32 p., 28 cm., https://doi.org/10.3133/ofr82626.","productDescription":"32 p., 28 cm.","costCenters":[],"links":[{"id":142604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0626/report-thumb.jpg"},{"id":38812,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0626/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a70c","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":162428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11043,"text":"ofr82509 - 1982 - U.S. Geological Survey research in radioactive waste disposal; fiscal year 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82509","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-509","title":"U.S. Geological Survey research in radioactive waste disposal; fiscal year 1980","docAbstract":"The report summarizes progress on geologic and hydrologic research related to the disposal of radioactive wastes. The research is described according to whether it is related most directly to: (1) High-level and transuranic wastes; (2) Low-level wastes, or (3) Uranium mill tailings. Included is research applicable to the identification and geohydrologic characterization of waste-disposal sites, to investigations of specific sites where wastes have been stored, and to studies of regions or environments where waste-disposal sites might be located. A significant part of the activity is concerned with techniques and methods for characterizing disposal sites and studies of geologic and hydrologic processes related to the transport and (or) retention of waste radionuclides.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82509","usgsCitation":"Schneider, R., and Trask, N., 1982, U.S. Geological Survey research in radioactive waste disposal; fiscal year 1980: U.S. Geological Survey Open-File Report 82-509, 115 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr82509.","productDescription":"115 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0509/report-thumb.jpg"},{"id":38813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0509/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4fde","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":162430,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":162429,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":48770,"text":"ofr82300L - 1982 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, December 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:06","indexId":"ofr82300L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-300","chapter":"L","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, December 1982","language":"ENGLISH","doi":"10.3133/ofr82300L","usgsCitation":"Townshend, J., Papp, J., Sauter, E., and Torrence, L., 1982, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, December 1982: U.S. Geological Survey Open-File Report 82-300, 25 p.; 12 v. : ill. ; 28 cm., https://doi.org/10.3133/ofr82300L.","productDescription":"25 p.; 12 v. : ill. ; 28 cm.","costCenters":[],"links":[{"id":162847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0300l/report-thumb.jpg"},{"id":85567,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0300l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673de9","contributors":{"authors":[{"text":"Townshend, J.B.","contributorId":30623,"corporation":false,"usgs":true,"family":"Townshend","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":238208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Papp, J.E.","contributorId":95057,"corporation":false,"usgs":true,"family":"Papp","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":238211,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sauter, E.A.","contributorId":51738,"corporation":false,"usgs":true,"family":"Sauter","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":238209,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Torrence, L.Y.","contributorId":62587,"corporation":false,"usgs":true,"family":"Torrence","given":"L.Y.","email":"","affiliations":[],"preferred":false,"id":238210,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":10630,"text":"ofr82504 - 1982 - Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980","interactions":[],"lastModifiedDate":"2018-03-19T10:48:45","indexId":"ofr82504","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-504","title":"Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980","docAbstract":"An intensive study of nonpoint-source runoff was conducted in the Twin Cities metropolitan area in Minnesota during 1980. The purpose of the study was to determine the relationships between land use, watershed characteristics, and the quantity, quality, and timing of runoff.
\nDischarge and water-quality data were collected at 19 sites located in 6 rural and 4 urban watersheds. Basin characteristics and land use were determined for each watershed. Recording instruments provided continuous discharge records at 17 sites and continuous rainfall records at 12 sites. Automatic samplers were used at 12 sites. Water-quality samples were collected at 15- to 60-minute intervals during periods of increased runoff. Samples were collected periodically during low flow. Primary emphasis was placed on analysis of samples for suspended solids, nutrients, and oxygen-demanding constituents. Secondary emphasis was placed on analysis for chloride, metals, bacteria, pesticides, and PCB's. Wetfall and dryfall precipitation-quality data were collected at six sites.
\nDischarge and water-quality data were used to calculate storm and daily loads of chemical oxygen demand, total suspended solids, ammonia plus organic nitrogen, nitrite plus nitrate-nitrogen, total phosphorus, chloride, and lead.
\nAll data collected during the study are documented in tables that contain watershed characteristics and land use, daily and unit values for discharge and rainfall, rainfall characteristics, water-quality data for runoff and precipitation, results of laboratory settling tests, results of quality-assurance tests, dally loads, and storm loads.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr82504","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities","usgsCitation":"Payne, G.A., Ayers, M.A., and Brown, R.G., 1982, Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980: U.S. Geological Survey Open-File Report 82-504, iv, 289 p., https://doi.org/10.3133/ofr82504.","productDescription":"iv, 289 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":142533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0504/report-thumb.jpg"},{"id":38464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0504/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cities Metropolitan 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S. Geological Survey. The database was designed and created for input to the Geologic Retrieval and Synopsis Program (GRASP) to allow selective retrievals of information pertaining to location of data, data format, cruise, geographical bounds and collection dates of data. This information is then used to locate the stored data for administrative purposes or further processing. \r\n\r\nDatabase utilization is divided into three distinct operations. 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(La. only)","indexId":"ofr75236","publicationYear":"1975","noYear":false,"title":"Ozarks land use data set; Tyler, Tex.; La. (La. only)"},"predicate":"SUPERSEDED_BY","object":{"id":43867,"text":"ofr82805 - 1982 - Land use and land cover and associated maps for Tyler, Texas","indexId":"ofr82805","publicationYear":"1982","noYear":false,"title":"Land use and land cover and associated maps for Tyler, Texas"},"id":1}],"lastModifiedDate":"2012-02-02T00:11:02","indexId":"ofr82805","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-805","title":"Land use and land cover and associated maps for Tyler, Texas","language":"ENGLISH","doi":"10.3133/ofr82805","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land use and land cover and associated maps for Tyler, Texas: U.S. Geological Survey Open-File Report 82-805, maps :photocopy ;45 x 67 cm., https://doi.org/10.3133/ofr82805.","productDescription":"maps :photocopy ;45 x 67 cm.","costCenters":[],"links":[{"id":168130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec05","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10816,"text":"ofr8262 - 1982 - Earthquake hazard and prediction in NW Mexico and the California/Mexico border","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr8262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-62","title":"Earthquake hazard and prediction in NW Mexico and the California/Mexico border","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8262","usgsCitation":"Reichle, M., and Brune, J., 1982, Earthquake hazard and prediction in NW Mexico and the California/Mexico border: U.S. Geological Survey Open-File Report 82-62, 30 p., ill. ;28 cm., https://doi.org/10.3133/ofr8262.","productDescription":"30 p., ill. ;28 cm.","costCenters":[],"links":[{"id":144002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0062/report-thumb.jpg"},{"id":38624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62982c","contributors":{"authors":[{"text":"Reichle, Michael","contributorId":23954,"corporation":false,"usgs":true,"family":"Reichle","given":"Michael","affiliations":[],"preferred":false,"id":162016,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brune, J.N.","contributorId":49362,"corporation":false,"usgs":true,"family":"Brune","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":162017,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11075,"text":"ofr82937 - 1982 - Aspects of the palynology of the Chinle Formation (Upper Triassic), Colorado Plateau, Arizona, Utah, and New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr82937","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-937","title":"Aspects of the palynology of the Chinle Formation (Upper Triassic), Colorado Plateau, Arizona, Utah, and New Mexico","docAbstract":"This study deals with 16 palynological samples from Arizona, New Mexico, and Utah, that represent six members of the Chinle Formation of Late Triassic age. The samples, in ascending sequence, show a gradual change in the spore-bisaccate ratio from a preponderance of spores to numerical dominance of bisaccate pollen grains. This change is interpreted to indicate a climatic trend toward increasing aridity. The trend is thought to represent the decreasing energy phase of the oldest of three depositional cycles posited by Lupe (1977, 1979). The late Karnian age indicated for the Chinle Formation by pollen and spores is based on material from the lower part of the formation, leaving open the possibility that the upper part of the Chinle may be younger.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82937","usgsCitation":"Scott, R., 1982, Aspects of the palynology of the Chinle Formation (Upper Triassic), Colorado Plateau, Arizona, Utah, and New Mexico: U.S. Geological Survey Open-File Report 82-937, 21 p. ill., map ;28 cm., https://doi.org/10.3133/ofr82937.","productDescription":"21 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":144161,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0937/report-thumb.jpg"},{"id":38833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0937/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672a24","contributors":{"authors":[{"text":"Scott, Richard A.","contributorId":14414,"corporation":false,"usgs":true,"family":"Scott","given":"Richard A.","affiliations":[],"preferred":false,"id":162487,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11076,"text":"ofr82965 - 1982 - Results of USGS oil-shale core drilling in the eastern Uinta Basin; Red Wash-1 drill hole","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr82965","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-965","title":"Results of USGS oil-shale core drilling in the eastern Uinta Basin; Red Wash-1 drill hole","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82965","usgsCitation":"Scott, R.W., and Pantea, M., 1982, Results of USGS oil-shale core drilling in the eastern Uinta Basin; Red Wash-1 drill hole: U.S. Geological Survey Open-File Report 82-965, 41 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82965.","productDescription":"41 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":144162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0965/report-thumb.jpg"},{"id":38834,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0965/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625432","contributors":{"authors":[{"text":"Scott, R. 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