No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8374","usgsCitation":"Motooka, J.M., and Miller, W.R., 1983, Analyses of the less than 0.180-mm fraction of drainage sediments, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Open-File Report 83-74, 103 p., https://doi.org/10.3133/ofr8374.","productDescription":"103 p.","costCenters":[],"links":[{"id":390734,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75667.htm"},{"id":144917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0074/report-thumb.jpg"},{"id":38279,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114,\n 38\n ],\n [\n -112,\n 38\n ],\n [\n -112,\n 39\n ],\n [\n -114,\n 39\n ],\n [\n -114,\n 38\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680e1f","contributors":{"authors":[{"text":"Motooka, J. M.","contributorId":8834,"corporation":false,"usgs":true,"family":"Motooka","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":161365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":161366,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":41863,"text":"ofr83611 - 1983 - Aeromagnetic map of south-central Alabama","interactions":[],"lastModifiedDate":"2021-11-16T21:51:27.917459","indexId":"ofr83611","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-611","title":"Aeromagnetic map of south-central Alabama","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83611","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Aeromagnetic map of south-central Alabama: U.S. Geological Survey Open-File Report 83-611, 9 Plates:32.24 × 22.31 inches or smaller, https://doi.org/10.3133/ofr83611.","productDescription":"9 Plates:32.24 × 22.31 inches or smaller","costCenters":[],"links":[{"id":172723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79594,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79593,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79592,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79591,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79590,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79589,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79588,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79587,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79586,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391774,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14133.htm"}],"country":"United States","state":"Alabama","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86,\n 31.5\n ],\n [\n -87,\n 31.5\n ],\n [\n -87,\n 32.833\n ],\n [\n -86,\n 32.833\n ],\n [\n -86,\n 31.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cc3","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":530667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10323,"text":"ofr83116 - 1983 - Specifications for updating USGS land use and land cover maps","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr83116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-116","title":"Specifications for updating USGS land use and land cover maps","docAbstract":"To meet the increasing demands for up-to-date land use and land cover information, a primary goal of the U.S. Geological Survey's (USGS) national land use and land cover mapping program is to provide for periodic updating of maps and data in a timely and uniform manner. The technical specifications for updating existing USGS land use and land cover maps that are presented here cover both the interpretive aspects of detecting and identifying land use and land cover changes and the cartographic aspects of mapping and presenting the change data in conventional map format. They provide the map compiler with the procedures and techniques necessary to then use these change data to update existing land use and land cover maps in a manner that is both standardized and repeatable. Included are specifications for the acquisition of remotely sensed source materials, selection of compilation map bases, handling of data base corrections, editing and quality control operations, generation of map update products for USGS open file, and the reproduction and distribution of open file materials. These specifications are planned to become part of the National Mapping Division's Technical Instructions.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83116","usgsCitation":"Milazzo, V.A., 1983, Specifications for updating USGS land use and land cover maps: U.S. Geological Survey Open-File Report 83-116, iii, 65 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83116.","productDescription":"iii, 65 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":143654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0116/report-thumb.jpg"},{"id":38174,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e03","contributors":{"authors":[{"text":"Milazzo, Valerie A.","contributorId":88717,"corporation":false,"usgs":true,"family":"Milazzo","given":"Valerie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26599,"text":"wri834110 - 1983 - Improvement of flood-frequency estimates for selected small watersheds in eastern Kansas using a rainfall-runoff model","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"wri834110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4110","title":"Improvement of flood-frequency estimates for selected small watersheds in eastern Kansas using a rainfall-runoff model","docAbstract":"The U.S. Geological Survey rainfall-runoff model was used to estimate model parameters for 13 small watersheds in eastern Kansas with drainage areas of less than 11 square miles. Model parameters and rainfall data from three long-term rainfall stations were used in the model to synthesize long-term records of simulated annual peak discharge, which were fitted to a log-Pearson Type III distribution. Final estimates of T-year floods, which were computed by combining weighted estimates of the synthesized and observed T-floods, represent the most reliable estimates based on observed and long-term synthesized records of peak discharges. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834110","usgsCitation":"Clement, R., 1983, Improvement of flood-frequency estimates for selected small watersheds in eastern Kansas using a rainfall-runoff model: U.S. Geological Survey Water-Resources Investigations Report 83-4110, iv, 26 p. :ill., map ;28 cm., https://doi.org/10.3133/wri834110.","productDescription":"iv, 26 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4110/report-thumb.jpg"},{"id":55465,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5cdc","contributors":{"authors":[{"text":"Clement, R.W.","contributorId":11247,"corporation":false,"usgs":true,"family":"Clement","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":196685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47748,"text":"wri8130 - 1983 - Reservoir-development impacts on surface-water quantity and quality in the Yampa River basin, Colorado and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"wri8130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-30","title":"Reservoir-development impacts on surface-water quantity and quality in the Yampa River basin, Colorado and Wyoming","docAbstract":"Development of coal resources and associated economy is accelerating in the Yampa River basin in northwestern Colorado and south-central Wyoming. Increased use of the water resources of the area will have a direct impact on their quantity and quality. As part of 18 surface-water projects, 35 reservoirs have been proposed with a combined total storage of 2.18 million acre-feet, 41% greater than the mean annual outflow from the basin. Three computer models were used to demonstrate methods of evaluating future impacts of reservoir development in the Yampa River basin. Four different reservoir configurations were used to simulate the effects of different degrees of proposed reservoir development. A multireservoir-flow model included both within-basin and transmountain diversions. Simulations indicated that in many cases diversion amounts would not be available for either type of diversion. A corresponding frequency analysis of reservoir storage levels indicated that most reservoirs would be operating with small percentages of total capacities and generally with less than 20% of conservation-pool volumes. Simulations using a dissolved-solids model indicated that extensive reservoir development could increase average annual concentrations at most locations. Simulations using a single-reservoir model indicated no significant occurrence of water-temperature stratification in most reservoirs due to limited reservoir storage. (USGS)","language":"ENGLISH","doi":"10.3133/wri8130","usgsCitation":"Adams, D.B., Bauer, D.P., Dale, R.H., and Steele, T.D., 1983, Reservoir-development impacts on surface-water quantity and quality in the Yampa River basin, Colorado and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 81-30, 98 p. ill., maps ;28 cm., https://doi.org/10.3133/wri8130.","productDescription":"98 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":169769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0030/report-thumb.jpg"},{"id":84659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62ba17","contributors":{"authors":[{"text":"Adams, D. Briane","contributorId":35707,"corporation":false,"usgs":true,"family":"Adams","given":"D.","email":"","middleInitial":"Briane","affiliations":[],"preferred":false,"id":236148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, Daniel P.","contributorId":24337,"corporation":false,"usgs":true,"family":"Bauer","given":"Daniel","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":236147,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dale, Robert H.","contributorId":85190,"corporation":false,"usgs":true,"family":"Dale","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":236149,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steele, Timothy Doak","contributorId":88723,"corporation":false,"usgs":true,"family":"Steele","given":"Timothy","email":"","middleInitial":"Doak","affiliations":[],"preferred":false,"id":236150,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":28441,"text":"wri8242 - 1983 - Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida","interactions":[],"lastModifiedDate":"2019-11-26T11:15:19","indexId":"wri8242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-42","title":"Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida","docAbstract":"Hydrologic data collected on nine small urban watersheds in the Tampa Bay area of west-central Florida and a method for estimating peak discharges in the study area are described. The watersheds have mixed land use and range in size from 0.34 to 3.45 square miles. Watershed soils, land use, and storm-drainage system data are described. Urban development ranged from a sparsely populated area with open-ditch storm sewers and 19% impervious area to a completely sewered watershed with 61% impervious cover. The U.S. Geological Survey natural-basin and urban-watershed models were calibrated for the nine watersheds using 5-minute interval rainfall data from the Tampa, Florida, National Weather Service rain gage to simulate annual peak discharge for the period 1906-52. A log-Pearson Type III frequency analysis of the simulated annual maximum discharge was used to determine the 2-, 5-, 10-, 25-, 50-, and 100-year flood discharges for each watershed. Flood discharges were related in a multiple-linear regression to drainage area, channel slope, detention storage area, and an urban-development factor determined by the extent of curb and gutter street drainage and storm-sewer system. The average standard error for the regional relations ranged from + or - 32 to + or - 42%. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8242","usgsCitation":"Lopez, M.A., and Woodham, W.M., 1983, Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 82-42, vi, 52 p. , https://doi.org/10.3133/wri8242.","productDescription":"vi, 52 p. ","costCenters":[],"links":[{"id":369640,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0042/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"Tampa Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.6336669921875,\n 27.81478637667891\n ],\n [\n -82.1832275390625,\n 27.81478637667891\n ],\n [\n -82.1832275390625,\n 28.14950321154457\n ],\n [\n -82.6336669921875,\n 28.14950321154457\n ],\n [\n -82.6336669921875,\n 27.81478637667891\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649519","contributors":{"authors":[{"text":"Lopez, M. A.","contributorId":12493,"corporation":false,"usgs":true,"family":"Lopez","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":199804,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10321,"text":"ofr82771 - 1983 - Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-771","title":"Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982","docAbstract":"The rockslide/debris avalanche from the north face of Mount St. Helens that precipitated the volcano 's eruption on May 18, 1980 , blocked outflow from Spirit Lake, Washington. There has been no surface outflow since that time. From May 21, 1980, when the first measurement of lake level was made, to August 1, 1982, Spirit Lake has increased its volume from 122,800 acre-ft to 264 ,000 acre-ft, an increase of 115%. Lake level has risen approximately 54 ft during this period. Hydrologic and geologic properties of the debris dam are unknown, but the materials obviously are easily erodible. Steep walled channels up to 60 ft deep have been eroded into the dam and are extending headward toward the lowest points on the crest. In addition, it appears that the lower areas on the crest of the dam are underlain by ash cloud deposits of low density. Indications are that the debris dam could fail by headward erosion, by overtopping with rapid downcutting, or by ' piping ' and rapid erosion. Each type of failure can produce rapid release of stored lake water with very high discharge rates. On the basis of observed filling rates of the lake over the last two yr and precipitation records at four long-term, low altitude National Weather Service stations, it is expected that normal precipitation will fill the lake to the dam crest in December 1985. This estimate is also based on the assumption that loss of water from the lake by seepage continues at the present rate until December 1985. With normal precipitation during the coming yr (August 1982 through July 1983 the lake will fill to a level 50 ft below the lowest existing point on the crest of the debris dam, which is at 3,532 ft altitude. If precipitation exceeds normal by 1.5 times during this coming year, the lake level will be 40 ft below the 3 ,532-ft crest of the debris dam by the end of July 1983. This same lake level can be reached by the end of March 1983 if precipitation from October through March is twice the winter mean. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82771","usgsCitation":"Meyer, W., and Carpenter, P.J., 1983, Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982: U.S. Geological Survey Open-File Report 82-771, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82771.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0771/report-thumb.jpg"},{"id":38172,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0771/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f481e","contributors":{"authors":[{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":161195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carpenter, Philip J.","contributorId":85034,"corporation":false,"usgs":true,"family":"Carpenter","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":33355,"text":"b1551 - 1983 - Mineral resources of the Caney Creek Wilderness, Polk County, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:27","indexId":"b1551","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1551","title":"Mineral resources of the Caney Creek Wilderness, Polk County, Arkansas","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1551","usgsCitation":"Ericksen, G.E., Patterson, S.H., Dunn, M.L., and Harrison, D.K., 1983, Mineral resources of the Caney Creek Wilderness, Polk County, Arkansas: U.S. Geological Survey Bulletin 1551, vi, 42 p. :ill., maps ;23 cm., https://doi.org/10.3133/b1551.","productDescription":"vi, 42 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":164251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1551/report-thumb.jpg"},{"id":61194,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1551/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69ae07","contributors":{"authors":[{"text":"Ericksen, George Edward","contributorId":38537,"corporation":false,"usgs":true,"family":"Ericksen","given":"George","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":210632,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, S. H.","contributorId":85232,"corporation":false,"usgs":true,"family":"Patterson","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":210634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunn, M. L. Jr.","contributorId":6502,"corporation":false,"usgs":true,"family":"Dunn","given":"M.","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":210631,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harrison, D. K.","contributorId":44912,"corporation":false,"usgs":true,"family":"Harrison","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":210633,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":26725,"text":"wri834051 - 1983 - Fortran computer programs to plot and process aquifer pressure and temperature data","interactions":[],"lastModifiedDate":"2018-03-12T10:24:28","indexId":"wri834051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4051","title":"Fortran computer programs to plot and process aquifer pressure and temperature data","docAbstract":"Two FORTRAN computer programs have been written to process water-well temperature and pressure data recorded automatically by a datalogger on magnetic tape. These programs process the data into tabular and graphical form. Both programs are presented with documentation. Sample plots of temperature versus time, water levels versus time, aquifer pressure versus log time , log drawdown versus log 1/time, and log drawdown versus log time/radius squared are presented and are obtained using standard CALCOM directives. Drawdown plots may be used directly to obtain aquifer transmissivities and storage coefficients as well as leakance coefficients.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri834051","usgsCitation":"Czarnecki, J., 1983, Fortran computer programs to plot and process aquifer pressure and temperature data: U.S. Geological Survey Water-Resources Investigations Report 83-4051, iii, 50 p., https://doi.org/10.3133/wri834051.","productDescription":"iii, 50 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":55600,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4051/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d4e4b07f02db5dd7ad","contributors":{"authors":[{"text":"Czarnecki, J.B.","contributorId":51768,"corporation":false,"usgs":true,"family":"Czarnecki","given":"J.B.","affiliations":[],"preferred":false,"id":196894,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10229,"text":"ofr83779 - 1983 - Stratigraphy, structure, and palinspastic synthesis of the western Brooks Range, northwestern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr83779","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-779","title":"Stratigraphy, structure, and palinspastic synthesis of the western Brooks Range, northwestern Alaska","docAbstract":"This report is an effort to describe and decipher the mid-Paleozoic to Lower Cretaceous stratigraphy and the orogenic evolution of the western Brooks Range. The western Brooks Range primarily is composed of stacks of complexly deformed thrust sheets that contain mostly coeval sequences of rocks with slightly different lithologic facies. In order to simplify the thrust-faulted stratigraphy and palinspastic restoration, the rocks are grouped into eight principal structural levels. The lowest structural level is believed to be autochthonous or parautochthonous and above that, each succeeding level is designated allochthon one through seven. Allochthon seven is composed of the remnants of an extensive ophiolite sheet. Allochthon six is composed of pillow basalt with subordinate intermediate volcanic rocks, chert, and Devonian limestone. It is not certain whether this allochthon was formed in a continental or oceanic setting. Allochthons five through one consist of distinctive and coeval sequences of Devonian to Lower Cretaceous sedimentary rocks that were deposited in a continental setting. The present geographic distribution of each structural level is shown on the allochthon map of the western Brooks Range. \r\n\r\nThe stratigraphy of the southern part of northern Alaska has been reconstructed by systematically unstacking lower allochthons to the north of higher allochthons. The palinspastic map that results from this procedure shows that the minimum thrust displacement between allochthon seven and the autochthon is approximately 700 to 800 km. Schematic cross sections drawn across the palinspastic map show how the stratigraphy of the southern part of northern. Alaska most likely appeared prior to the orogeny. During Devonian and Mississippian time, the sedimentary sequences that are now part of allochthons one to five are inferred to have been deposited in an ensialic basin with both northern and southern margins. During Pennsylvanian time, the sequences seem to have become part of a southward-sloping continental shelf when a southern land area moved away from northern Alaska by an inferred plate tectonic process of rifting or strike-slip motion. In Early Jurassic time just prior to the Brooks Range orogeny, northern Alaska probably was an extensive continental shelf with oceanic conditions to the south and land to the north. \r\n\r\nThe Brooks Range orogeny seems to have begun in the Middle Jurassic as the Arctic Alaska plate was underthrust (subducted) southward beneath oceanic crust of allochthon seven. At progressively later stages in the underthrusting process, the upper parts of the continental shelf were detached from the subthrust basement on which they were deposited, resulting in the other allochthons of the western Brooks Range. The period of major thrusting ceased by Albian time in the Early Cretaceous. During middle and Late Cretaceous time, epeirogenic uplift in the Brooks Range caused large quantities of clastic detritus to be shed into successor basins to the north and south. Broad folds and reverse faults in Upper Cretaceous sediments north of the Brooks Range provide evidence for a later period(s) of less intense deformation in northern Alaska.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83779","usgsCitation":"Mayfield, C.F., Tailleur, I.L., and Ellersieck, I., 1983, Stratigraphy, structure, and palinspastic synthesis of the western Brooks Range, northwestern Alaska: U.S. Geological Survey Open-File Report 83-779, ii, 61 p., 5 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr83779.","productDescription":"ii, 61 p., 5 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":144308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0779/report-thumb.jpg"},{"id":38093,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38094,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38095,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38096,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38097,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38098,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0779/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a530f","contributors":{"authors":[{"text":"Mayfield, Charles F.","contributorId":13623,"corporation":false,"usgs":true,"family":"Mayfield","given":"Charles","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":161043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tailleur, Irvin L.","contributorId":105304,"corporation":false,"usgs":true,"family":"Tailleur","given":"Irvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161045,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellersieck, Inyo","contributorId":34914,"corporation":false,"usgs":true,"family":"Ellersieck","given":"Inyo","affiliations":[],"preferred":false,"id":161044,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10759,"text":"ofr83331 - 1983 - Reconnaissance geology of the Ghazzalah Quadrangle, sheet 26/41 A, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr83331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-331","title":"Reconnaissance geology of the Ghazzalah Quadrangle, sheet 26/41 A, Kingdom of Saudi Arabia","docAbstract":"The Ghazzalah quadrangle is located in the northern Precambrian shield of Saudi Arabia between lat 26?30' and 27?00' N. and long 41?00' and 41?30' E. The area is underlain by two lithologically distinct, Precambrian volcanosedimentary units and a wide range of dioritoid and granitoid plutonic intrusive rocks. The only Phanerozoic rocks consist of one outcrop of Tertiary(?) basalt and widespread but thin deposits of Quaternary detritus. \r\n\r\nThe Banana greenstone, the oldest rock in the quadrangle, consists of intermediate volcanic and subvolcanic rocks and minor interbedded marble, which have been metamorphosed to greenschist-facies assemblages. Volcanic rocks mainly range in composition from basalt to andesite, and subvolcanic rocks consist of diorite and diabase. \r\n\r\nThe Banana greenstone is unconformably overlain by silicic volcanic rocks and minor arkosic sandstone and breccia of the Hadn formation. Preservation of delicate volcanic textures suggests that the rocks have been only incipiently metamorphosed. Unpublished rubidium/strontium isotopic data for the Hadn formation suggest an age of 620 to 610 Ma. \r\n\r\nIntrusive rocks are separable according to their ages relative to the Hadn formation. Those that are unconformably overlain by the Hadn formation consist of hornblende quartz diorite and gabbro, which may be consanguineous with the Banana greenstone, and younger tonalite, biotite-hornblende granodiorite, syenogranite, and monzogranite. Plutons of monzogranite, alkali-feldspar g,ranite, syenbgranite, peralkaline granite, and hypabyssal intrusions of granophyre were probably emplaced during a period coincident with and (or) following Hadn volcanism. Uranium-lead and rubidium/strontium isotopic data for two plutons in the adjacent Al Qasr quadrangle suggest that plutonic activity persisted in the region until about 580 to 570 Ma. \r\n\r\nFaulting appears to postdate all of the plutonic rocks. The dominant faults belong to a northeast-trending system of right-lateral shears; a subordinant system consists of mainly north- to northwest-trending faults.\r\n\r\nThe peralkaline-granite plutons underlying Jibal Ba'gham and Jibal ar Rumman have the most economic potential. Wadi samples from these areas show an anomalous concentrations of tin, lead, niobium, and yttrium. Localized, intense radiometric anomalies in the Ba'gham intrusive complex are associated with high concentrations )f thorium, uranium, andrare-earth elements.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83331","usgsCitation":"Quick, J.E., 1983, Reconnaissance geology of the Ghazzalah Quadrangle, sheet 26/41 A, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-331, 48 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83331.","productDescription":"48 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0331/report-thumb.jpg"},{"id":38563,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0331/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38564,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0331/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38565,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0331/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38566,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0331/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60422c","contributors":{"authors":[{"text":"Quick, James E.","contributorId":21552,"corporation":false,"usgs":true,"family":"Quick","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38620,"text":"pp1170D - 1983 - Merced Peak quadrangle, central Sierra Nevada, California— Analytic data","interactions":[],"lastModifiedDate":"2021-10-27T20:12:59.636263","indexId":"pp1170D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1170","chapter":"D","title":"Merced Peak quadrangle, central Sierra Nevada, California— Analytic data","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","doi":"10.3133/pp1170D","usgsCitation":"Peck, D., and Van Kooten, G.K., 1983, Merced Peak quadrangle, central Sierra Nevada, California— Analytic data: U.S. Geological Survey Professional Paper 1170, 29 p., https://doi.org/10.3133/pp1170D.","productDescription":"29 p.","costCenters":[],"links":[{"id":391035,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74408.htm"},{"id":65443,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1170d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1170d/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Merced Peak quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.25,\n 37.75\n ],\n [\n -119.5,\n 37.75\n ],\n [\n -119.5,\n 37.5\n ],\n [\n -119.25,\n 37.5\n ],\n [\n -119.25,\n 37.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db61420a","contributors":{"authors":[{"text":"Peck, D. L.","contributorId":53784,"corporation":false,"usgs":true,"family":"Peck","given":"D. L.","affiliations":[],"preferred":false,"id":220176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Kooten, G. K.","contributorId":41499,"corporation":false,"usgs":true,"family":"Van Kooten","given":"G.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":220175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10416,"text":"ofr8389 - 1983 - Geologic and grade-tonnage information on volcanic-hosted copper-zinc-lead massive sulfide deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr8389","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-89","title":"Geologic and grade-tonnage information on volcanic-hosted copper-zinc-lead massive sulfide deposits","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8389","usgsCitation":"Mosier, D.L., Singer, D., and Salem, B., 1983, Geologic and grade-tonnage information on volcanic-hosted copper-zinc-lead massive sulfide deposits: U.S. Geological Survey Open-File Report 83-89, 79 p. ;28 cm., https://doi.org/10.3133/ofr8389.","productDescription":"79 p. ;28 cm.","costCenters":[],"links":[{"id":145633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0089/report-thumb.jpg"},{"id":38275,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0089/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a824f","contributors":{"authors":[{"text":"Mosier, Dan L.","contributorId":42593,"corporation":false,"usgs":true,"family":"Mosier","given":"Dan","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Singer, D.A.","contributorId":69128,"corporation":false,"usgs":true,"family":"Singer","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":161351,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Salem, B.B.","contributorId":26699,"corporation":false,"usgs":true,"family":"Salem","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":161349,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11729,"text":"ofr83747 - 1983 - Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California","interactions":[],"lastModifiedDate":"2022-09-23T20:16:56.047888","indexId":"ofr83747","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-747","title":"Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California","docAbstract":"Hydration-rind ages based on hydration-rind thicknesses of obsidian and an assumed hydration rate of 5 microns /1000 yrs have been determined for the 26 exposed Mono domes and coulees. Hydration-rind thickness data give good estimates of relative age differences between the domes, but determination of absolute ages will depend upon calibration to radiometric ages. \r\n\r\nThe first extrusion of highly differentiated, sparsely porphyritic rhyolite occurred an estimated 32,000 to 40,000 yrs ago and consists of a small dome at the northwest end of the contiguous chain. The next major extrusive event occurred about 24,000 yrs ago and is represented by two domes and a major tephra. About 10,000 yrs ago the frequency of eruptive activity increases and rhyolite lave was extruded at an average rate of 0.2 km3/1000 yrs; periods of dormancy ranging in length from 300 to 2000 yrs. About 2000 to 3000 yrs ago the rate of extrusion increased dramatically to 0.8 km3/1000 yrs beginning with the eruption of the South Coulee and its associated tephra. At the same time, the nature of erupted magma changed from sparsely porphyritic (3 to 10 per cent sanidine) to aphyric rhyolite. All eruptions since 2000 radiocarbon yrs BP have produced magma that is aphyric but is of the same chemical composition as the earlier porphyritic magma. Volumes of porphyritic and aphyric extrusives, each of which includes volumes of lava and volumes of pumiceous pyroclastics reduced for porosity, are nearly equal and together total about 4 km3. Projecting the recent rate of extrusion over the time since the last major eruption, 1185 radiocarbon yrs ago suggests that a future eruption in the Mono Chain could release as much as 1 km 3 of magma. The recent increase in extrusion rate and the contemporaneous change in the nature of the magma are attributed to an event in the magma chamber that allowed the release of hotter, more fluid, crystal-free magma. The young age for the beginning of rhyolite volcanism from the mono magma chamber suggests that rhyolite magma may have been emplaced in the shallow crust as recently as 32,000 to 40,000 yrs ago. Calculations by Lachenbruch et al. (1976, Jour. Geophys. Research, v. 81, p. 769-784) that a thermal disturbance at this age would have propagated upward by solid conduction only 4 km and offer an explanation for the lack of a heat-flow anomaly and surface indications of hydrothermal activity over the Mono magma chamber and its associated ring-fracture system. This report also contains new information on the age and chemistry of volcanics on the Mono Lake island, the Inyo domes, and tephras within the Long Valley Caldera. \r\n\r\nA newly discovered rhyolite tuff ring of late Quaternary age in the Toowa volcanic field of the southern Sierra Nevada is briefly described for it represents a new area that should be examined for potential as a geothermal area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83747","usgsCitation":"Wood, S.H., 1983, Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California: U.S. Geological Survey Open-File Report 83-747, vii, 76 p., https://doi.org/10.3133/ofr83747.","productDescription":"vii, 76 p.","costCenters":[],"links":[{"id":407293,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14207.htm","linkFileType":{"id":5,"text":"html"}},{"id":143964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0747/report-thumb.jpg"},{"id":39615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0747/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Long Valley and Mono Basin geothermal area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.129,\n 37.681\n ],\n [\n -118.922,\n 37.681\n ],\n [\n -118.922,\n 38.046\n ],\n [\n -119.129,\n 38.046\n ],\n [\n -119.129,\n 37.681\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e073f","contributors":{"authors":[{"text":"Wood, S. H.","contributorId":66261,"corporation":false,"usgs":true,"family":"Wood","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":163631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10398,"text":"ofr83586 - 1983 - Results of oil-shale investigations in northeastern Nevada","interactions":[],"lastModifiedDate":"2024-11-26T20:29:37.522655","indexId":"ofr83586","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-586","title":"Results of oil-shale investigations in northeastern Nevada","docAbstract":"No abstract available.
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The data are conveniently made available to supplement an interpretive report that describes Statewide water-level trends and their causes, which will be published separately.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83225","usgsCitation":"Young, H., 1983, Hydrographs of water levels in observation wells in Idaho, 1971-82: U.S. Geological Survey Open-File Report 83-225, iv, 288 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83225.","productDescription":"iv, 288 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":144775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0225/report-thumb.jpg"},{"id":39680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0225/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b742","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":163730,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28692,"text":"wri834016 - 1983 - Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri834016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4016","title":"Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","docAbstract":"Geohydrologic data have been collected in the Los Medanos area at the U.S. Department of Energy 's proposed Waste Isolation Pilot Plant (WIPP) site in southeastern New Mexico since 1975 as part of an intensive study evaluating the feasibility of storing defense-associated nuclear wastes within the bedded salt of the Salado Formation of Permian age. Drilling and hydrologic testing have identified three principal water-producing zones above the salt, including the Rustler-Salado Formational contact and the Culebra and Magenta Dolomite Members of the Permian Rustler Formation. Below the bedded salt there is another water-bearing zone, the channel sandstones of the Bell Canyon formation of the Permian Delaware Mountain Group. Most data collected from 33 hydrologic test holes indicate that the water-bearing zones are characterized by low transmissivities and contain slightly saline to briny water. Data collected from drill-stem tests in the Bell Canyon Formation indicate the channel sandstones have hydraulic conductivities ranging from 0.02 to 0.36 feet per day grade vertically and laterally into siltstones and shales of very low permeability. The Rustler Formation contains the principal water-producing zones identified at the WIPP site. 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(USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834016","usgsCitation":"Mercer, J.W., 1983, Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 83-4016, viii, 121 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834016.","productDescription":"viii, 121 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4016/report-thumb.jpg"},{"id":57535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8824","contributors":{"authors":[{"text":"Mercer, Jerry W.","contributorId":32534,"corporation":false,"usgs":true,"family":"Mercer","given":"Jerry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67615,"text":"l135 - 1983 - Land use and land cover, 1973, Blytheville, Arkansas; 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