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,{"id":65335,"text":"i1789 - 1986 - Controlled photomosaic of part of the Kasei Valles Region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:03","indexId":"i1789","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1789","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Kasei Valles Region of Mars","language":"ENGLISH","doi":"10.3133/i1789","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Controlled photomosaic of part of the Kasei Valles Region of Mars: U.S. Geological Survey IMAP 1789, 1 remote-sensing image ;61 x 60 cm., on sheet 94 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1789.","productDescription":"1 remote-sensing image ;61 x 60 cm., on sheet 94 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":187002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100902,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1789/plate-1.pdf","size":"8248","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a80a","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":533722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15102,"text":"ofr86190 - 1986 - Automatic rezeroing circuit for bore-hole strainmeter","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr86190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-190","title":"Automatic rezeroing circuit for bore-hole strainmeter","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86190","usgsCitation":"Mueller, R., and Myren, D., 1986, Automatic rezeroing circuit for bore-hole strainmeter: U.S. Geological Survey Open-File Report 86-190, 12 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86190.","productDescription":"12 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0190/report-thumb.jpg"},{"id":44024,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0190/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66806c","contributors":{"authors":[{"text":"Mueller, R.J.","contributorId":77135,"corporation":false,"usgs":true,"family":"Mueller","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":170574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Myren, D.","contributorId":14245,"corporation":false,"usgs":true,"family":"Myren","given":"D.","email":"","affiliations":[],"preferred":false,"id":170573,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15182,"text":"ofr8673 - 1986 - Dissolved-selenium data for wells in the western San Joaquin Valley, California, February to July 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr8673","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-73","title":"Dissolved-selenium data for wells in the western San Joaquin Valley, California, February to July 1985","docAbstract":"Water samples were collected for selenium analysis from 63 wells in western San Joaquin Valley, California, during February to July 1985. Results of the data collection indicate that dissolved selenium concentrations ranged from less than 1 to 120 micrograms per liter; more than 50 percent of the wells sampled had concentrations of less than 1 microgram per liter. Four additional samples collected from public supply wells in the western valley had concentrations ranging from less than 1 to 2 micrograms per liter. All samples from five public supply wells east of the study area had concentrations less than 1 microgram per liter. The U.S. Environmental Protection Agency 's drinking-water standard of 10 micrograms per liter for selenium was slightly exceeded in 2 of 39 domestic wells (11 and 13 micrograms per liter) and substantially exceeded in 2 of 11 irrigation and agricultural wells (55 and 120 micrograms per liter). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8673","usgsCitation":"Neil, J.M., 1986, Dissolved-selenium data for wells in the western San Joaquin Valley, California, February to July 1985: U.S. Geological Survey Open-File Report 86-73, iv, 10 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8673.","productDescription":"iv, 10 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":148214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0073/report-thumb.jpg"},{"id":44096,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3a1","contributors":{"authors":[{"text":"Neil, J. M.","contributorId":27464,"corporation":false,"usgs":true,"family":"Neil","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":170700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14824,"text":"ofr86227 - 1986 - Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow","interactions":[{"subject":{"id":14824,"text":"ofr86227 - 1986 - Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow","indexId":"ofr86227","publicationYear":"1986","noYear":false,"title":"Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow"},"predicate":"SUPERSEDED_BY","object":{"id":2222,"text":"wsp2308 - 1987 - Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow","indexId":"wsp2308","publicationYear":"1987","noYear":false,"title":"Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow"},"id":1}],"supersededBy":{"id":2222,"text":"wsp2308 - 1987 - Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow","indexId":"wsp2308","publicationYear":"1987","noYear":false,"title":"Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow"},"lastModifiedDate":"2019-11-27T10:52:38","indexId":"ofr86227","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-227","title":"Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow","docAbstract":"<p>The theory of anisotropic aquifer hydraulic properties and a computer program, written in Fortran 77, developed to compute the components of the anisotropic transmissivity tensor of two-dimensional groundwater flow are described. To determine the tensor components using one pumping well and three observation wells, the type-curve and straight-line approximation methods are developed. These methods are based on the equation of drawdown developed for two-dimensional nonsteady flow in an infinite anisotropic aquifer. To determine tensor components using more than three observation wells, a weighted least squares optimization procedure is described for use with the type-curve and straight-line approximation methods. The computer program described in this report allows the type-curve, straight-line approximation, and weighted least squares optimization methods to be used in conjunction with data from observation and pumping wells. Three example applications using the computer program and field data gathered during geohydrologic investigations at a site near Dawsonville, Georgia , are provided to illustrate the use of the computer program. The example applications demonstrate the use of the type-curve method using three observation wells, the weighted least squares optimization method using eight observation wells and equal weighting, and the weighted least squares optimization method using eight observation wells and unequal weighting. Results obtained using the computer program indicate major transmissivity in the range of 347-296 sq ft/day, minor transmissivity in the range of 139-99 sq ft/day, aquifer anisotropy in the range of 3.54 to 2.14, principal direction of flow in the range of N. 45.9 degrees E. to N. 58.7 degrees E., and storage coefficient in the range of 0.0063 to 0.0037. The numerical results are in good agreement with field data gathered on the weathered crystalline rocks underlying the investigation site. Supplemental material provides definitions of variables, data requirements and corresponding formats, input data and output results for the example applications, and a listing of the Fortran 77 computer code. (Author's abstract)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr86227","usgsCitation":"Maslia, M., and Randolph, R., 1986, Methods and computer program documentation for determining anisotropic transmissivity tensor components of two-dimensional ground-water flow: U.S. Geological Survey Open-File Report 86-227, v, 64 p.  , https://doi.org/10.3133/ofr86227.","productDescription":"v, 64 p.  ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":147828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0227/report-thumb.jpg"},{"id":369735,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0227/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a01c","contributors":{"authors":[{"text":"Maslia, M.L.","contributorId":24090,"corporation":false,"usgs":true,"family":"Maslia","given":"M.L.","affiliations":[],"preferred":false,"id":170077,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randolph, R.B.","contributorId":38606,"corporation":false,"usgs":true,"family":"Randolph","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":170078,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21082,"text":"ofr86467 - 1986 - Abstracts of the symposium on the Geology and Mineral Deposits of the Tonopah 1 degree x 2 degrees quadrangle, Nevada : presented at Reno, Nevada, September 26, 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr86467","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-467","title":"Abstracts of the symposium on the Geology and Mineral Deposits of the Tonopah 1 degree x 2 degrees quadrangle, Nevada : presented at Reno, Nevada, September 26, 1986","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86467","usgsCitation":"Whitebread, D.H., 1986, Abstracts of the symposium on the Geology and Mineral Deposits of the Tonopah 1 degree x 2 degrees quadrangle, Nevada : presented at Reno, Nevada, September 26, 1986: U.S. Geological Survey Open-File Report 86-467, 13 p. ;28 cm., https://doi.org/10.3133/ofr86467.","productDescription":"13 p. ;28 cm.","costCenters":[],"links":[{"id":154681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0467/report-thumb.jpg"},{"id":50676,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0467/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3856","contributors":{"authors":[{"text":"Whitebread, Donald Harvey (compiler)","contributorId":31018,"corporation":false,"usgs":true,"family":"Whitebread","given":"Donald","suffix":"(compiler)","email":"","middleInitial":"Harvey","affiliations":[],"preferred":false,"id":183809,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25448,"text":"wri864143 - 1986 - Digital data base of lakes on the North Slope, Alaska","interactions":[],"lastModifiedDate":"2017-03-29T11:05:37","indexId":"wri864143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4143","title":"Digital data base of lakes on the North Slope, Alaska","docAbstract":"<p>The National Mapping Division and Water Resources Division of the U.S. Geological Survey have produced a digital data base of approximately 23,330 lakes on the North Slope of Alaska. The inventoried region consists of the area north of the 69th parallel and is composed of sixteen 1° x 3° quadrangles. The data base includes (1) locations of lake centers in latitude and longitude, (2) a unique number for each lake within a quadrangle, and (3) acreage for water classes (deep, shallow or turbid, and ice) within each lake and lake total. The digital data base is an easily accessible storage and retrieval system that will allow for rapid identification of a particular lake or region of lakes and its characteristics. The data base is designed to accommodate field study data such as lake depth, water quality, volume of water, ice thickness, and other pertinent information. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864143","usgsCitation":"Walker, K., York, J., Murphy, D., and Sloan, C.E., 1986, Digital data base of lakes on the North Slope, Alaska: U.S. Geological Survey Water-Resources Investigations Report 86-4143, iii, 13 p., https://doi.org/10.3133/wri864143.","productDescription":"iii, 13 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":54182,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4143/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4143/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b464e","contributors":{"authors":[{"text":"Walker, Kim-Marie","contributorId":83947,"corporation":false,"usgs":true,"family":"Walker","given":"Kim-Marie","email":"","affiliations":[],"preferred":false,"id":193738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"York, James","contributorId":69604,"corporation":false,"usgs":true,"family":"York","given":"James","email":"","affiliations":[],"preferred":false,"id":193737,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murphy, Dennis","contributorId":15236,"corporation":false,"usgs":true,"family":"Murphy","given":"Dennis","email":"","affiliations":[],"preferred":false,"id":193735,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sloan, C. E.","contributorId":59037,"corporation":false,"usgs":true,"family":"Sloan","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193736,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":60925,"text":"mf1862 - 1986 - Preliminary map showing the thickness of glacial deposits in Ohio","interactions":[],"lastModifiedDate":"2016-08-23T09:34:33","indexId":"mf1862","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1862","title":"Preliminary map showing the thickness of glacial deposits in Ohio","docAbstract":"<p>This map was compiled as part of a U.S. Geological Survey project to portray the character and thickness of glacial deposits east of the Rocky Mountains. It is a preliminary map, compiled at a scale of 1:250,000 from sources of differing type and quality (fig. I, table 1). County drift-thickness maps produced by the Ohio Geological Survey are the most reliable source of data used. These county maps, either published or in manuscript form, were available for 36 of the 72 counties that contain glacial or glacially related deposits more than 50 ft thick. An earlier, reconnaissance drift-thickness map of northwestern Ohio (Ohio Department of Natural Resources, 1960) provided data for parts of 12 additional counties. Published maps of bedrock topography were utilized for 9 counties and for parts of 6 counties. The computation of drift thickness in these counties is less reliable then the drift-thickness maps published by the Ohio Geological Survey because the bedrock topography maps, most of which are at least 20 years old, were compiled from a more limited set of data. In the remaining counties, only well-log data were available. Drift-thickness data in these counties are the least reliable; the determination of thickness trends was commonly guided by the configuration of preglacial drainage channels (as drawn by Stout and others, 1943) and by topography.</p>\n<p>Throughout the glaciated areas of Ohio, and especially near the glacial margin, a network of drainage channels is buried by glacial drift. Some of these channels arc of a preglacial age while others were formed during interglacial periods; some were cut into the bedrock by rivers&mdash; either preglacial rivers or meltwater streams flowing along the glacial margin&mdash;while others, such as the lower Cuyahoga River valley, may have been overdeepened by the erosive power of glacial ice. The thickest deposits of drift in the state occur in the lower Cuyahoga River valley near Lake Erie, and above the buried valley in west-central Ohio that has been historically considered a part of the Teays Valley. The thickest drift reliably measured in Ohio to date is 602 ft in a drill hole near Cleveland.</p>\n<p>In contrast to the extreme variations in drift thickness encountered in the vicinity of buried channels, drift on the upland arcus is generally thinner and the variations in thickness are much less pronounced. Worthy of note, however, are three large areas where the drift sheet is relatively thick. In northwestern Ohio, a large volume of drift was deposited along the flanks of the Erie ice lobe (fig. 2) near the interlobate position with the Saginaw lobe to the northwest; drift thickness there exceeds 200 ft. Thick drift was also deposited in a roughly cast-west band across the Miami lobe. The mechanism that produced this band of thick drift is not obvious, but it may have been influenced in part by bedrock topography. Bedrock control of drift thickness is more clearly indicated to the cast of Columbus, along the eastern flank of the Scioto lobe, where ice slow was resisted by rocks of the Allegheny plateau. The edge of the plateau, or the Allegheny escarpment, is obscured by glacial deposits but its likely position (Fenneman, 1938; Stout and others, 1913; Dove, 1960; and Root and others, 1961) is shown on the map. Southward from the ice margin's reentrant position in southern Richland County, ice flowing eastward from the Scioto lobe encountered the topographically higher plateau, which constrained the ice and caused drift to accumulate in significant thicknesses just to the west of the escarpment.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1862","usgsCitation":"Soller, D.R., 1986, Preliminary map showing the thickness of glacial deposits in Ohio: U.S. Geological Survey Miscellaneous Field Studies Map 1862, Plate: 45.55 x 37.23 inches, https://doi.org/10.3133/mf1862.","productDescription":"Plate: 45.55 x 37.23 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326125,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1862.JPG"},{"id":327510,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1862/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Ohio","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85,38 ], [ -85,42 ], [ -81,42 ], [ -81,38 ], [ -85,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf03","contributors":{"authors":[{"text":"Soller, D. R.","contributorId":25923,"corporation":false,"usgs":true,"family":"Soller","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":264629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15274,"text":"ofr86228 - 1986 - Physical and chemical data for northern San Francisco Bay, California, September through November, 1984","interactions":[],"lastModifiedDate":"2016-07-27T12:57:46","indexId":"ofr86228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-228","title":"Physical and chemical data for northern San Francisco Bay, California, September through November, 1984","docAbstract":"<p>This report presents physical and chemical data for northern San Francisco Bay waters. Samples were collected during the late summer and fall of 1984 during six cruises at near-two-week intervals. Bay waters were sampled at designated (historical) stations and selected salinitis along the deep channel of northern San Francisco Bay. Measurements included temperature, salinity, turbidity, in vivo fluorescence, chlorophyll a, alkalinity, suspended particulate matter, dissolved organic carbon, and dissolved inorganic nutrients: nitrite, nitrate + nitrite, ammonium, dissolved silica, and ortho-phosphate. Numerical results are tabulated and methods are described. (USGS)</p>","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86228","usgsCitation":"Ota, A.Y., Schemel, L., and Hager, S., 1986, Physical and chemical data for northern San Francisco Bay, California, September through November, 1984: U.S. Geological Survey Open-File Report 86-228, 32 p. :map ;28 cm., https://doi.org/10.3133/ofr86228.","productDescription":"32 p. :map ;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":44205,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0228/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0228/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485e6","contributors":{"authors":[{"text":"Ota, Allan Y.","contributorId":85192,"corporation":false,"usgs":true,"family":"Ota","given":"Allan","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":170865,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schemel, L. E.","contributorId":89529,"corporation":false,"usgs":true,"family":"Schemel","given":"L. E.","affiliations":[],"preferred":false,"id":170866,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hager, S.W.","contributorId":51746,"corporation":false,"usgs":true,"family":"Hager","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":170864,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25723,"text":"wri824091 - 1986 - Preliminary delineation and description of the regional aquifers of Tennessee: the East Tennessee aquifer system","interactions":[],"lastModifiedDate":"2022-12-21T22:56:36.359639","indexId":"wri824091","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"82-4091","title":"Preliminary delineation and description of the regional aquifers of Tennessee: the East Tennessee aquifer system","docAbstract":"<p>The east Tennessee aquifer system occurs in the Valley and Ridge and the Blue Ridge provinces of Tennessee. These areas are underlain by rocks of Precambrian to Pennsylvanian age which have been structurally deformed and faulted during the Appalachian orogeny. Groundwater in the Valley and Ridge occurs primarily in solution openings in carbonate rocks and in fractures in sandstone and shale. Fractures in the crystalline rocks store and transmit most of the groundwater in the Blue Ridge province. The east Tennessee aquifer system is important as a source of rural and municipal drinking water. Within 300 ft of land surface, groundwater generally contains less than 500 milligrams/L dissolved solids. At greater depths, fractures and solution openings are smaller and fewer in number. There are very little data to define groundwater occurrence at depths greater than about 300 ft. Groundwater flow may be restricted and the dissolved solids concentrations in the groundwater may reach thousands or even ten thousands of milligrams/L.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824091","usgsCitation":"Brahana, J., Mulderink, D., Macy, J.A., and Bradley, M.W., 1986, Preliminary delineation and description of the regional aquifers of Tennessee: the East Tennessee aquifer system: U.S. Geological Survey Water-Resources Investigations Report 82-4091, iv, 30 p., https://doi.org/10.3133/wri824091.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":156170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410909,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35602.htm","linkFileType":{"id":5,"text":"html"}},{"id":1854,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri824091","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Tennessee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -85.5,\n              36.594\n            ],\n            [\n              -85.5,\n              35\n            ],\n            [\n              -81.667,\n              35\n            ],\n            [\n              -81.667,\n              36.594\n            ],\n            [\n              -85.5,\n              36.594\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6c3","contributors":{"authors":[{"text":"Brahana, J. V.","contributorId":32926,"corporation":false,"usgs":true,"family":"Brahana","given":"J. V.","affiliations":[],"preferred":false,"id":194802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mulderink, Dolores","contributorId":64667,"corporation":false,"usgs":true,"family":"Mulderink","given":"Dolores","email":"","affiliations":[],"preferred":false,"id":194804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Macy, J. A.","contributorId":10047,"corporation":false,"usgs":true,"family":"Macy","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bradley, M. W.","contributorId":40610,"corporation":false,"usgs":true,"family":"Bradley","given":"M.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":194803,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25127,"text":"cir930E - 1986 - International strategic minerals inventory summary report: platinum-group metals","interactions":[],"lastModifiedDate":"2014-12-02T10:27:03","indexId":"cir930E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"930","chapter":"E","title":"International strategic minerals inventory summary report: platinum-group metals","docAbstract":"<p>Major world resources of platinum-group metals are described in this summary report of information in the International Strategic Minerals Inventory {ISMI}. ISMI is a cooperative data-collection effort of earth-science and mineral-resource agencies in Australia, Canada, the Federal Republic of Germany, the Republic of South Africa, and the United States of America. This report, designed to be of benefit to policy analysts, contains two parts. Part I presents an overview of the resources and potential supply of platinum-group metals on the basis of inventory information. Part II contains tables of some of the geologic information and mineral-resource and production data that were collected by ISMI participants.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir930E","collaboration":"Prepared as a cooperative effort among earth-science and mineral-resource agencies of Australia, Canada, the Federal Republic of Germany, the Republic of South Africa, the United Kingdom, and the United States of America","usgsCitation":"Sutphin, D., and Page, N.J., 1986, International strategic minerals inventory summary report: platinum-group metals: U.S. Geological Survey Circular 930, vi, 34 p., https://doi.org/10.3133/cir930E.","productDescription":"vi, 34 p.","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":54107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0930e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0930e/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0831","contributors":{"authors":[{"text":"Sutphin, David M.","contributorId":53769,"corporation":false,"usgs":true,"family":"Sutphin","given":"David M.","affiliations":[],"preferred":false,"id":193260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, Norman J.","contributorId":46492,"corporation":false,"usgs":true,"family":"Page","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":193261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60942,"text":"mf1891 - 1986 - Side-looking airborne radar image map showing cross-strike structural discontinuities and lineaments of the central Appalachians","interactions":[],"lastModifiedDate":"2012-02-10T00:10:31","indexId":"mf1891","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1891","title":"Side-looking airborne radar image map showing cross-strike structural discontinuities and lineaments of the central Appalachians","language":"ENGLISH","doi":"10.3133/mf1891","usgsCitation":"Southworth, C., 1986, Side-looking airborne radar image map showing cross-strike structural discontinuities and lineaments of the central Appalachians: U.S. Geological Survey Miscellaneous Field Studies Map 1891, 1 remote sensing image ;88 x 106 cm., on sheet 101 x 112 cm., folded in envelope 25 x 32 cm. +1 pamphlet (14 p. : maps ; 28 cm.), https://doi.org/10.3133/mf1891.","productDescription":"1 remote sensing image ;88 x 106 cm., on sheet 101 x 112 cm., folded in envelope 25 x 32 cm. +1 pamphlet (14 p. : maps ; 28 cm.)","costCenters":[],"links":[{"id":183277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1986/1891/report-thumb.jpg"},{"id":88906,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1986/1891/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1986/1891/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82,37 ], [ -82,41 ], [ -76,41 ], [ -76,37 ], [ -82,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3db8","contributors":{"authors":[{"text":"Southworth, C.S.","contributorId":51272,"corporation":false,"usgs":true,"family":"Southworth","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":264659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25922,"text":"wri844148 - 1986 - Hydrogeology and leachate movement near two chemical-waste sites in Oswego County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri844148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4148","title":"Hydrogeology and leachate movement near two chemical-waste sites in Oswego County, New York","docAbstract":"Forty-five observation wells and test holes were installed at two chemical waste disposal sites in Oswego County, New York, to evaluate the hydrogeologic conditions and the rate and direction of leachate migration. At the site near Oswego groundwater moves northward at an average velocity of 0.4 ft/day through unconsolidated glacial deposits and discharges into White Creek and Wine Creek, which border the site and discharge to Lake Ontario. Leaking barrels by chemical wastes have contaminated the groundwater within the site, as evidenced by detection of 10 ' priority pollutant ' organic compounds, and elevated values of specific conductance, chloride, arsenic, lead, and mercury. At the site near Fulton, where 8,000 barrels of chemical wastes are buried, groundwater in the sandy surficial aquifer bordering the landfill on the south and east moves southward and eastward at an average velocity of 2.8 ft/day and discharges to Bell Creek, which discharges to the Oswego River, or moves beneath the landfill. Leachate is migrating eastward, southeastward, and southwestward, as evidenced by elevated values of specific conductance, temperature, and concentrations of several trace metals at wells east, southeast, and southwest of the site. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844148","usgsCitation":"Anderson, H., and Miller, T.S., 1986, Hydrogeology and leachate movement near two chemical-waste sites in Oswego County, New York: U.S. Geological Survey Water-Resources Investigations Report 84-4148, v, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844148.","productDescription":"v, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4148/report-thumb.jpg"},{"id":54680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4148/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625438","contributors":{"authors":[{"text":"Anderson, H. R.","contributorId":67487,"corporation":false,"usgs":true,"family":"Anderson","given":"H. R.","affiliations":[],"preferred":false,"id":195485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Todd S.","contributorId":85623,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":195486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25876,"text":"wri854230 - 1986 - Reconnaissance of ground-water resources in the North Fork Gunnison River basin, southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri854230","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4230","title":"Reconnaissance of ground-water resources in the North Fork Gunnison River basin, southwestern Colorado","docAbstract":"Aquifers of large areal extent in the North Fork Gunnison River basin are found in the alluvium and bedrock. Alluvial aquifers yielded water with dissolved solids concentrations ranging from 43 to 2,300 mg/L. Dissolved solids concentrations of water samples from the Mesaverde Formation of Late Cretaceous age and the Dakota Sandstone and Burro Canyon Formations of Late and Early Cretaceous age ranged from 56 to 3,200 mg/L. Dissolved solids concentrations of water samples from Mancos Shale ranged from 1,800 to 8,200 mg/L. Most wells in the North Fork Gunnison River basin are at altitudes below 7,500 ft, yield from 2 to 40 gal/min and are completed in alluvial sand and gravel, sandstone , or fractured bedrock. Springs generally are at altitudes above 7,000 ft, discharge from perched water tables at geologic contacts, have calcium magnesium bicarbonate water types, and are much less saline than water from wells. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854230","usgsCitation":"Ackerman, D.J., and Brooks, T., 1986, Reconnaissance of ground-water resources in the North Fork Gunnison River basin, southwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 85-4230, v, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854230.","productDescription":"v, 21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4230/report-thumb.jpg"},{"id":54630,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4230/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54631,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4230/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54632,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4230/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e817","contributors":{"authors":[{"text":"Ackerman, D. J.","contributorId":53380,"corporation":false,"usgs":true,"family":"Ackerman","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":195408,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, Tom","contributorId":76356,"corporation":false,"usgs":true,"family":"Brooks","given":"Tom","email":"","affiliations":[],"preferred":false,"id":195409,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57326,"text":"wdrVA851 - 1986 - Water resources data for Virginia water year 1985","interactions":[],"lastModifiedDate":"2020-11-25T18:40:15.476301","indexId":"wdrVA851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"VA-85-1","title":"Water resources data for Virginia water year 1985","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA851","usgsCitation":"Prugh, B., Easton, F., and Lynch, D.D., 1986, Water resources data for Virginia water year 1985: U.S. Geological Survey Water Data Report VA-85-1, xii, 398 p., https://doi.org/10.3133/wdrVA851.","productDescription":"xii, 398 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc89d","contributors":{"authors":[{"text":"Prugh, B.J.","contributorId":88811,"corporation":false,"usgs":true,"family":"Prugh","given":"B.J.","affiliations":[],"preferred":false,"id":256717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Easton, F.J.","contributorId":61096,"corporation":false,"usgs":true,"family":"Easton","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":256716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lynch, D. D.","contributorId":12075,"corporation":false,"usgs":true,"family":"Lynch","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":256715,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25512,"text":"wri864133 - 1986 - Flow testing of the Newberry 2 research drillhole, Newberry volcano, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"wri864133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4133","title":"Flow testing of the Newberry 2 research drillhole, Newberry volcano, Oregon","docAbstract":"A 20 hour flow test of the Newberry 2 research drillhole at Newberry Volcano produced about 33,000 kilograms of fluid. The flow rate declined from about 0.8 kilograms per sec to less than 0.3 kilograms per sec during the course of the test. The mass ratio of liquid water to vapor was about 3:2 at the separator and stayed fairly constant throughout the test. The vapor phase was about half steam and half CO2 by weight. The average enthalpy of the steam/water mixture at the separator was about 1 ,200 kilojoules per kilogram. Because of the low flow rate and the large temperature gradient into the surrounding rocks, heat loss from the wellbore was high; a simple conductive model gives overall losses of about 1,200 kilojoules per kilogram of H2O produced. The actual heat loss may have been even higher due to convective effects, and it is likely that the fluid entering the bottom of the wellbore was largely or entirely steam and CO2. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864133","usgsCitation":"Ingebritsen, S.E., Carothers, W., Mariner, R.H., Gudmundsson, J., and Sammel, E., 1986, Flow testing of the Newberry 2 research drillhole, Newberry volcano, Oregon: U.S. Geological Survey Water-Resources Investigations Report 86-4133, v, 23 p. :ill., map ;28 cm., https://doi.org/10.3133/wri864133.","productDescription":"v, 23 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":126433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4133/report-thumb.jpg"},{"id":54229,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4133/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de7fc","contributors":{"authors":[{"text":"Ingebritsen, S. E.","contributorId":8078,"corporation":false,"usgs":true,"family":"Ingebritsen","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carothers, W.W.","contributorId":43803,"corporation":false,"usgs":true,"family":"Carothers","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":193997,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mariner, Robert H.","contributorId":81075,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":193999,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gudmundsson, J.S.","contributorId":103315,"corporation":false,"usgs":true,"family":"Gudmundsson","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":194000,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sammel, E.A.","contributorId":59480,"corporation":false,"usgs":true,"family":"Sammel","given":"E.A.","affiliations":[],"preferred":false,"id":193998,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":14963,"text":"ofr86125 - 1986 - Catalog of Kansas and Oklahoma cores housed at the USGS Core Repository, Denver, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr86125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-125","title":"Catalog of Kansas and Oklahoma cores housed at the USGS Core Repository, Denver, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86125","usgsCitation":"Michalski, T., and Richards, D., 1986, Catalog of Kansas and Oklahoma cores housed at the USGS Core Repository, Denver, Colorado: U.S. Geological Survey Open-File Report 86-125, 12 p. ;28 cm., https://doi.org/10.3133/ofr86125.","productDescription":"12 p. ;28 cm.","costCenters":[],"links":[{"id":145992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0125/report-thumb.jpg"},{"id":43776,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efc28","contributors":{"authors":[{"text":"Michalski, T.C.","contributorId":106503,"corporation":false,"usgs":true,"family":"Michalski","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":170329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richards, D.L.","contributorId":8862,"corporation":false,"usgs":true,"family":"Richards","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":170328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60970,"text":"mf1852 - 1986 - Seismicity map of the state of Arizona","interactions":[],"lastModifiedDate":"2017-05-10T11:32:30","indexId":"mf1852","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1852","title":"Seismicity map of the state of Arizona","docAbstract":"<p>This map is one of a series of seismicity maps produced by the U. S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This map shows only those earthquakes with epicenters located within the boundaries of Arizona, even though earthquakes in nearby states or countries may have been felt or may have caused damage in Arizona.</p><p>The data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1982) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that had not been previously used. The data in table 1 represent best estimates of the location of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used.</p><p>Table 1 includes earthquakes reported felt in Yuma, Arizona that had no corroborating reports from other areas. These events are listed with coordinates (32.7°N., 114.6° W.) near Yuma even though it is suspected that they may have actually occurred in the Imperial Valley, California or Baja California, Mexico. Very few earthquakes have been instrumentally located near Yuma and it is believed that most historical felt reports correspond to earthquakes that occurred in the seismic zone extending from the Gulf of California northward into California. It is known that some earthquakes located graphically from phase data prior to epicenter determinations by electronic computer were erroneously located in southern Arizona and actually had locations in the Gulf of California or northern Mexico.</p><p>For detailed descriptions of the effects of earthquakes in Arizona see Bulletin 193, Arizona earthquakes, 1776-1980 (reference 343) which lists the localities where the earthquakes were felt and the effects at each place. This publication also includes isoseismal maps for 41 events.</p><p>The latitude and longitude coordinates of each epicenter were rounded to the nearest tenth of a degree and sorted so that all identical locations were grouped and counted. These locations are represented on the map by a triangle. The number of earthquakes at each location is shown on the map by the arabic number to the right of the triangle. The Roman numeral to the left of the triangle is the maximum Modified Mercalli intensity (Wood and Neumann, 1931) of al 1 earthquakes with epicenters at that geographic location. The absence of an intensity value indicates that no intensities have been assigned to earthquakes at that location. The year shown below each triangle is the latest year for which the maximum intensity was recorded.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1852","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1986, Seismicity map of the state of Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1852, 49.25 x 37.11 inches, https://doi.org/10.3133/mf1852.","productDescription":"49.25 x 37.11 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326144,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1852.JPG"},{"id":327507,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1852/plate-1.pdf","text":"Plate ","size":"15.66 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"country":"United 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,{"id":25616,"text":"wri864329 - 1986 - Investigation of possible effects of surface coal mining on hydrology and landscape stability in part of the Powder River structural basin, northeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"wri864329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4329","title":"Investigation of possible effects of surface coal mining on hydrology and landscape stability in part of the Powder River structural basin, northeastern Wyoming","docAbstract":"The effects of surface coal mining on the surface- and groundwater systems in a 5,400 sq mi area in the Powder River Basin, Wyoming, that includes 20 major coal mines were evaluated using three approaches: A surface water model, a landscape-stability analysis, and a groundwater model. A surface water model was developed for the Belle Fourche River basin. The Hydrological Simulation Program-Fortran model was used to simulate changes in streamflow and changes in dissolved-solids and sulfate concentrations. Simulated streamflows resulting from less than average rainfall were small, changes in flow from premining to during-mining and postmining conditions were less than 2.5%, and changes in mean dissolved-solids and sulfate concentrations ranged from 1 to 7%. A landscape-stability analysis resulted in regression relations to aid in the reconstruction of reclaimed drainage networks. Hypsometric analyses indicate the larger basins are relatively stable, and statistical data from these basins may be used to design the placement of material within a mined basin to approximate natural, stable landscapes in the area. The attempt to define and simulate the groundwater system in the area using a groundwater-flow model was unsuccessful. The steady-state groundwater-flow model could not be calibrated. The modeling effort failed principally because of insufficient quantity and quality of data to define the spatial distribution of aquifer properties; the hydraulic-head distribution within and between aquifers; and the rates of groundwater recharge and discharge, especially for steady-state conditions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864329","usgsCitation":"Bloyd, R., Daddow, P., Jordon, P., and Lowham, H., 1986, Investigation of possible effects of surface coal mining on hydrology and landscape stability in part of the Powder River structural basin, northeastern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 86-4329, vi, 101 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864329.","productDescription":"vi, 101 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4329/report-thumb.jpg"},{"id":54362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e479de4b07f02db49212b","contributors":{"authors":[{"text":"Bloyd, R. M.","contributorId":34549,"corporation":false,"usgs":true,"family":"Bloyd","given":"R. M.","affiliations":[],"preferred":false,"id":194423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daddow, P. B.","contributorId":26700,"corporation":false,"usgs":true,"family":"Daddow","given":"P. B.","affiliations":[],"preferred":false,"id":194422,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jordon, P.R.","contributorId":69605,"corporation":false,"usgs":true,"family":"Jordon","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":194424,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":194421,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25889,"text":"wri854178 - 1986 - Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California","interactions":[],"lastModifiedDate":"2018-02-15T12:01:33","indexId":"wri854178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4178","title":"Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California","docAbstract":"<p>Westward movement of ground water from the Long Meadow area of Sequoia National Park, California, to the General Sherman Tree area is prevented by an eastward hydraulic gradient and low fracture permeability of a granodiorite ridge separating the two areas. Clay beds present in the alluvium in the Long Meadow area would hinder, but not preclude, recharge to the ground-water system beneath Long Meadow from streams. </p><p>A dependable ground-water supply of about 50 gallons per minute (72,000 gallons per day) can be developed from the Long Meadow area. The withdrawal of this quantity of ground water from the Long Meadow area should not affect ground or surface water in the General Sherman Tree area. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/wri854178","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Akers, J.P., 1986, Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California: U.S. Geological Survey Water-Resources Investigations Report 85-4178, Report: iv, 15 p.; 1 Plate: 20.19 x 17.62 inches, https://doi.org/10.3133/wri854178.","productDescription":"Report: iv, 15 p.; 1 Plate: 20.19 x 17.62 inches","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":121514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4178/report-thumb.jpg"},{"id":54651,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4178/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Long Meadow Area, Sequoia National Park, California, showing locations of test-hole, stream-measuring, and water-sampling sites"},{"id":54652,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4178/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Sequoia National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.75456809997559,\n              36.572319932849254\n            ],\n            [\n              -118.71500015258789,\n              36.572319932849254\n            ],\n            [\n              -118.71500015258789,\n              36.599542913631645\n            ],\n            [\n              -118.75456809997559,\n              36.599542913631645\n            ],\n            [\n              -118.75456809997559,\n              36.572319932849254\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d999","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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