{"pageNumber":"4869","pageRowStart":"121700","pageSize":"25","recordCount":184563,"records":[{"id":41331,"text":"ofr86192 - 1986 - Preliminary geologic map of Agua de Pau volcano, Sao Miguel, Azores","interactions":[],"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr86192","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":"86-192","title":"Preliminary geologic map of Agua de Pau volcano, Sao Miguel, Azores","language":"ENGLISH","doi":"10.3133/ofr86192","usgsCitation":"Moore, R.B., 1986, Preliminary geologic map of Agua de Pau volcano, Sao Miguel, Azores: U.S. Geological Survey Open-File Report 86-192, 1 map :photocopy ;85 x 102 cm., on sheet 107 x 163 cm., https://doi.org/10.3133/ofr86192.","productDescription":"1 map :photocopy ;85 x 102 cm., on sheet 107 x 163 cm.","costCenters":[],"links":[{"id":176307,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21198,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0192/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21199,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0192/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c114","contributors":{"authors":[{"text":"Moore, Richard B. rmoore@usgs.gov","contributorId":1464,"corporation":false,"usgs":true,"family":"Moore","given":"Richard","email":"rmoore@usgs.gov","middleInitial":"B.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":224845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30074,"text":"wri864065 - 1986 - Traveltime and dispersion in the Shenandoah River and its tributaries, Waynesboro, Virginia, to Harpers Ferry, West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri864065","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":"86-4065","title":"Traveltime and dispersion in the Shenandoah River and its tributaries, Waynesboro, Virginia, to Harpers Ferry, West Virginia","docAbstract":"Two traveltime and dispersion measurements using rhodamin dye were conducted on a 178-mile reach of the Shenandoah River between Waynesboro, Virginia, and Harpers Ferry, West Virginia. The flows during the two measurements were at approximately the 85% and 45% flow durations. The two sets of data were used to develop a generalized procedure for predicting traveltimes and downstream concentrations resulting from spillage of water soluble substances at any point along the river reach studied. The procedure can be used to calculate traveltime and concentration data for almost any spillage that occurs during relatively steady flow between a 40% to 95% flow duration. Based on an analogy between the general shape of a time concentration curve and a scalene triangle, the procedures can be used on long river reaches to approximate the conservative time concentration curve for instantaneous spills of contaminants. The triangular approximation technique can be combined with a superposition technique to predict the approximate, conservative time concentration curve for constant rate and variable rate injections of contaminants. The procedure was applied to a hypothetical situation in which 5,000 pounds of contaminants is spilled instantaneously at Island Ford, Virginia. The times required for the leading edge, the peak concentration, and the trailing edge of the contaminant cloud to reach the water intake at Front Royal, Virginia (85 miles downstream), are 234,280, and 340 hrs, respectively, for a flow at an 80% flow duration. The conservative peak concentration would be approximately 940 micrograms/L at Front Royal. The procedures developed cannot be depended upon when a significant hydraulic wave or other unsteady flow condition exists in the flow system or when the spilled material floats or is immiscible in water. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nOpen-File Services Section, Western Distribution Branch,","doi":"10.3133/wri864065","usgsCitation":"Taylor, K., James, R., and Helinsky, B., 1986, Traveltime and dispersion in the Shenandoah River and its tributaries, Waynesboro, Virginia, to Harpers Ferry, West Virginia: U.S. Geological Survey Water-Resources Investigations Report 86-4065, vi, 58 p. :ill., map ;28 cm., https://doi.org/10.3133/wri864065.","productDescription":"vi, 58 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":160151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4065/report-thumb.jpg"},{"id":58883,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4065/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58884,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0e72","contributors":{"authors":[{"text":"Taylor, K.R.","contributorId":36929,"corporation":false,"usgs":true,"family":"Taylor","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":202628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"James, R.W.","contributorId":70434,"corporation":false,"usgs":true,"family":"James","given":"R.W.","affiliations":[],"preferred":false,"id":202629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Helinsky, B.M.","contributorId":82344,"corporation":false,"usgs":true,"family":"Helinsky","given":"B.M.","affiliations":[],"preferred":false,"id":202630,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":42528,"text":"ofr86209 - 1986 - Gold in the conterminous United States, perspective of 1986 — Preliminary map of selected geographic, economic, and geologic attributes of productive (>10,000 oz) gold districts","interactions":[],"lastModifiedDate":"2022-08-01T19:56:16.548842","indexId":"ofr86209","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":"86-209","title":"Gold in the conterminous United States, perspective of 1986 — Preliminary map of selected geographic, economic, and geologic attributes of productive (>10,000 oz) gold districts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86209","usgsCitation":"Tooker, E.W., and Vercoutere, T.L., 1986, Gold in the conterminous United States, perspective of 1986 — Preliminary map of selected geographic, economic, and geologic attributes of productive (>10,000 oz) gold districts: U.S. Geological Survey Open-File Report 86-209, Report: i, 32 p.; 1 Plate: 39.90 × 31.61 inches, https://doi.org/10.3133/ofr86209.","productDescription":"Report: i, 32 p.; 1 Plate: 39.90 × 31.61 inches","costCenters":[],"links":[{"id":80275,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0209/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404598,"rank":2,"type":{"id":36,"text":"NGMDB Index 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,{"id":42643,"text":"ofr85715 - 1986 - Preliminary geologic map of the Pahoa South quadrangle, eastern Hawaii","interactions":[{"subject":{"id":42643,"text":"ofr85715 - 1986 - Preliminary geologic map of the Pahoa South quadrangle, eastern Hawaii","indexId":"ofr85715","publicationYear":"1986","noYear":false,"title":"Preliminary geologic map of the Pahoa South quadrangle, eastern Hawaii"},"predicate":"SUPERSEDED_BY","object":{"id":66640,"text":"i2225 - 1991 - Geologic map of the lower east rift zone of Kilauea Volcano, Hawaii","indexId":"i2225","publicationYear":"1991","noYear":false,"title":"Geologic map of the lower east rift zone of Kilauea Volcano, Hawaii"},"id":1}],"supersededBy":{"id":66640,"text":"i2225 - 1991 - Geologic map of the lower east rift zone of Kilauea Volcano, Hawaii","indexId":"i2225","publicationYear":"1991","noYear":false,"title":"Geologic map of the lower east rift zone of Kilauea Volcano, Hawaii"},"lastModifiedDate":"2022-04-06T16:42:15.838715","indexId":"ofr85715","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":"85-715","title":"Preliminary geologic map of the Pahoa South quadrangle, eastern Hawaii","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85715","usgsCitation":"Moore, R.B., 1986, Preliminary geologic map of the Pahoa South quadrangle, eastern Hawaii: U.S. Geological Survey Open-File Report 85-715, 1 Plate, https://doi.org/10.3133/ofr85715.","productDescription":"1 Plate","costCenters":[],"links":[{"id":172545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398129,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16902.htm"}],"scale":"24000","country":"United States","state":"Hawaii","otherGeospatial":"Pahoa South quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155,\n              19.375\n            ],\n            [\n              -154.875,\n              19.375\n            ],\n            [\n              -154.875,\n              19.5\n            ],\n            [\n              -155,\n              19.5\n            ],\n            [\n              -155,\n              19.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aea6","contributors":{"authors":[{"text":"Moore, Richard B. rmoore@usgs.gov","contributorId":1464,"corporation":false,"usgs":true,"family":"Moore","given":"Richard","email":"rmoore@usgs.gov","middleInitial":"B.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":226872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30060,"text":"wri854332 - 1986 - Results of exploratory drilling for water in Waihanau Valley, Molokai, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri854332","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":"85-4332","title":"Results of exploratory drilling for water in Waihanau Valley, Molokai, Hawaii","docAbstract":"Three exploratory wells, located in lower Waihanau Valley on Molokai, were drilled and tested for their yields during the period May to October 1983. The first well, 582 ft deep, tapped the main water body in a basaltic aquifer intruded by scattered near-parallel volcanic dikes. Water in this water body is impounded by the dikes and has a head of about nine feet above sea level. A 48-hour pumping test was conducted on this well. The well was pumped at various rates ranging from 144 to 455 gal/min for nine hours. Thereafter, the well was pumped for 39 hours at a rate of 156 gal/min approximating the planned operational rate of 150 gal/min. The specific capacities of the well at the rates pumped averaged about 30 gal/min/ft of drawdown. The temperature of the pumped water remained nearly constant at 69 F (20.5 C). The chloride concentration ranged from 19 to 22 mg/L during the test. Analyses of the chemical constituents and trace metals of the water pumped indicated that it was of excellent quality. Based on these results, the well was finished as a production well. A shallow water body perched about 30 ft below ground surface and more than 400 ft above the main water body was discovered during the drilling of the first well when about 50 gal/min of water cascaded down the well. Two wells were drilled to depths of 200 and 150 ft, respectively, to explore this perched water. The yields obtained from this perched water body were low and indicated that its development was not feasible. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854332","usgsCitation":"Takasaki, K., 1986, Results of exploratory drilling for water in Waihanau Valley, Molokai, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 85-4332, v, 26 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854332.","productDescription":"v, 26 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4332/report-thumb.jpg"},{"id":58873,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4332/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605ac4","contributors":{"authors":[{"text":"Takasaki, K. J.","contributorId":44523,"corporation":false,"usgs":true,"family":"Takasaki","given":"K. J.","affiliations":[],"preferred":false,"id":202608,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30112,"text":"wri854207 - 1986 - Simulation analysis of water-level changes in the Navajo sandstone due to changes in the altitude of Lake Powell near Wahweap Bay, Utah and Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri854207","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":"85-4207","title":"Simulation analysis of water-level changes in the Navajo sandstone due to changes in the altitude of Lake Powell near Wahweap Bay, Utah and Arizona","docAbstract":"A two-dimensional, finite difference, digital computer model was used to simulate various concepts of groundwater flow near Wahweap Bay, Lake Powell. The filling of Lake Powell started in March 1963; and by 1983 the lake had risen almost 550 ft. This resulted in a maximum observed water level rise of 395 ft in a well in the Navajo Sandstone 1 mi from the lake. A steady-state model was prepared with subsurface recharge rates of 5,720 acre-ft/yr, 10,440 acre-ft/yr, and 14,820 acre-ft/yr, resulting in a range of hydraulic conductivity of 0.25 to 3.38 ft/da. Comparing measured and simulated water level changes resulted in a range of specific yield of 0.02 to 0.15. Using larger values for hydraulic conductivity in the model area corresponding to the axis of the Wahweap syncline and the Echo monocline was instrumental in attaining a reasonable match for the water level distribution. This supports previous concepts that areas where rocks are structurally deformed more readily transmit groundwater because of the higher degree of fracturing. Using the most likely simulation of the flow system, groundwater storage in the Navajo increased by about 25,000 acre ft/mi of shoreline form 1963-83, but the flow system will require about 400 yr to reach a state of equilibrium. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854207","usgsCitation":"Thomas, B.E., 1986, Simulation analysis of water-level changes in the Navajo sandstone due to changes in the altitude of Lake Powell near Wahweap Bay, Utah and Arizona: U.S. Geological Survey Water-Resources Investigations Report 85-4207, v, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854207.","productDescription":"v, 45 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":160076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4207/report-thumb.jpg"},{"id":58927,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3da4","contributors":{"authors":[{"text":"Thomas, B. E.","contributorId":90767,"corporation":false,"usgs":true,"family":"Thomas","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55213,"text":"wdrIA851 - 1986 - Water resources data Iowa, water year 1985","interactions":[],"lastModifiedDate":"2016-03-04T16:16:44","indexId":"wdrIA851","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":"IA-85-1","title":"Water resources data Iowa, water year 1985","docAbstract":"<p>Water resources data for the 1985 water year for Iowa consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground-water levels and ground-water quality. This report contains discharge records for 111 stream-gaging stations; stage and contents for 8 lakes and reservoirs; water quality for 8 stream-gaging stations; sediment records for 12 streamgaging stations; water levels for 94 observation wells; and chemical analyses for 214 observation wells. Also included are 118 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. The data represent that part of the National Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Iowa.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrIA851","collaboration":"Prepared in cooperation with the Iowa Geological Survey and with other State and Federal agencies","usgsCitation":"Melcher, N., Detroy, M., Matthes, W., and Hansen, R., 1986, Water resources data Iowa, water year 1985: U.S. Geological Survey Water Data Report IA-85-1, xiv, 332 p., https://doi.org/10.3133/wdrIA851.","productDescription":"xiv, 332 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":60776,"text":"mf1831 - 1986 - Isopach map of interval between top of the Pictured Cliffs Sandstone and the Huerfanito Bentonite bed of the Lewis Shale, La Plata County, Colorado, and Rio Arriba and San Juan counties, New Mexico","interactions":[],"lastModifiedDate":"2016-08-23T09:22:08","indexId":"mf1831","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":"1831","title":"Isopach map of interval between top of the Pictured Cliffs Sandstone and the Huerfanito Bentonite bed of the Lewis Shale, La Plata County, Colorado, and Rio Arriba and San Juan counties, New Mexico","docAbstract":"<p>This thickness map of a Late Cretaceous interval in the northwestern part of the San Juan Basin is part of a study of the relationship between ancient shore 1ines and coal-forming swamps during the filial regression of the Cretaceous epicontinental sea. The top of the thickness interval is the top of the Pictured Cliffs Sands tone. The base of the interval is a thin time marker, the Huerfanito Bentonite Bed of the Lewis Shale. The interval includes all of the Pictured Cliffs Sandstone and the upper part of the Lewis Shale. The northwest boundary of the map area is the outcrop of the Pictured Cliffs Sandstone and the Lewis Shale.</p>\n<p>Data used for the isopach map are mostly from interpretation of geophysical logs of oil and gas wells, southeast of the outcrop in parts of the Cortez, Durango, Farmington, and Navajo Reservoir 1: 100,000-scale quadrangles, Colorado and New Mexico. Cross sections A-A&rsquo; and B-B' give examples of geophysical logs that show some of the variations in the isopach interval.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1831","usgsCitation":"Sandberg, D., 1986, Isopach map of interval between top of the Pictured Cliffs Sandstone and the Huerfanito Bentonite bed of the Lewis Shale, La Plata County, Colorado, and Rio Arriba and San Juan counties, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1831, 2 Plates: 37.83 x 52.35 inches and 40.54 x 39.40 inches, https://doi.org/10.3133/mf1831.","productDescription":"2 Plates: 37.83 x 52.35 inches and 40.54 x 39.40 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1831.JPG"},{"id":327474,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1831/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327475,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1831/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Colorado, New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.5,36.75 ], [ -108.5,37.25 ], [ -107.5,37.25 ], [ -107.5,36.75 ], [ -108.5,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667123","contributors":{"authors":[{"text":"Sandberg, D.T.","contributorId":91123,"corporation":false,"usgs":true,"family":"Sandberg","given":"D.T.","email":"","affiliations":[],"preferred":false,"id":264380,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60626,"text":"mf1794 - 1986 - Map showing slope movements in the Oak Forest Quadrangle, Greene County, southwestern Pennsylvania","interactions":[],"lastModifiedDate":"2016-08-23T08:56:58","indexId":"mf1794","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":"1794","title":"Map showing slope movements in the Oak Forest Quadrangle, Greene County, southwestern Pennsylvania","docAbstract":"<p>This map is the first example in the eastern United States of a 1:24,000-scale 7.5&ndash; minute quadrangle map that identifies areas with slope&mdash;stability problems in detail. Such a map enables the user to make a rapid evaluation of the potential for mass movement. Furthermore, detailed slope movement inventory of this type can serve as a framework for statistical analyses of several factors that cause slope failures, such as the effects of bedrock lithology, soil and slope characteristics, and precipitation. Planners, engineers, soil scientists, geologists, and elected officials should find the map useful in the assessment of slope hazards and planning for future land use. Final evaluation of any site within the quadrangle should be based on an examination by a soils engineer or an engineering geologist.</p>\n<p>Field investigations in the springs of 1981 and 1982 and the fall of 1981 involved nearly 60 days of traverses. The foot traverses were supplemented by the interpretation of the land surface on vertical black-and-white aerial photography flown in January and February of 1973 at a scale of nearly 1:24,000. Earlier aerial photography flown in June and July 1939 at a scale of 1:20,000 and more recent but significantly smaller scale photography (1:80,000) flown in June 1977 supplied additional documentation. More than 1,200 active or recently active and 900 older slope movements were identified.</p>\n<p>The geologic map of the Oak Forest quadrangle (Roen, 1972) is one of several geologic maps at a scale of 1:24,000 in eastern and central Greene County. Stone (1932) wrote an earlier report of the geology and mineral resources of Greene County. A series of reconnaissance landslide maps at 1:24,000 scale based mainly on aerial photographic interpretation included Greene and adjacent counties (Hackman and Thomas, 1978).</p>\n<p>Selection of the Oak Forest quadrangle for a more comprehensive study of the slope movements was based on the existence of a recent geologic map (Roen, 1972), sizeable tracts of both forested and non-forested land, nearby precipitation record stations, a large number of pipelines which could offer pertinent data, and good accessibility of terrain from secondary roads. Finally, Hackman and Thomas (1978) showed that the area was representative of any quadrangle in the northern part of the Dunkard basin in its distribution and density of slope movements.</p>\n<p>The quadrangle is located about 65 km southwest of Pittsburgh, Penn. (fig. 1). Three distinct drainage systems (north, east, and south trending) are represented within the quadrangle (fig. 2).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1794","usgsCitation":"Pomeroy, J.S., 1986, Map showing slope movements in the Oak Forest Quadrangle, Greene County, southwestern Pennsylvania: U.S. Geological Survey Miscellaneous Field Studies Map 1794, Plate: 47.33 x 41.52 inches, https://doi.org/10.3133/mf1794.","productDescription":"Plate: 47.33 x 41.52 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326201,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1794.JPG"},{"id":327414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1794/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Pennsylvania","county":"Greene County","otherGeospatial":"Oak Forest Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.25,39.75 ], [ -80.25,39.8675 ], [ -80.11749999999999,39.8675 ], [ -80.11749999999999,39.75 ], [ -80.25,39.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2a7b","contributors":{"authors":[{"text":"Pomeroy, J. S.","contributorId":16807,"corporation":false,"usgs":true,"family":"Pomeroy","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":264094,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40602,"text":"ofr86388 - 1986 - China oil and gas, geologic evaluation of potential for exploration and development","interactions":[],"lastModifiedDate":"2012-02-02T00:10:33","indexId":"ofr86388","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":"86-388","title":"China oil and gas, geologic evaluation of potential for exploration and development","language":"ENGLISH","doi":"10.3133/ofr86388","usgsCitation":"Masters, C., Lee, K.Y., Ulmishek, G., and Robinson, K., 1986, China oil and gas, geologic evaluation of potential for exploration and development: U.S. Geological Survey Open-File Report 86-388, 1 map :photocopy ;87 x 101 cm., on sheet 98 x 107 cm., https://doi.org/10.3133/ofr86388.","productDescription":"1 map :photocopy ;87 x 101 cm., on sheet 98 x 107 cm.","costCenters":[],"links":[{"id":173381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":77126,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0388/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a3cf","contributors":{"authors":[{"text":"Masters, C.D.","contributorId":96664,"corporation":false,"usgs":true,"family":"Masters","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":223592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, K. Y.","contributorId":74351,"corporation":false,"usgs":true,"family":"Lee","given":"K.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":223589,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ulmishek, Gregory","contributorId":88361,"corporation":false,"usgs":true,"family":"Ulmishek","given":"Gregory","email":"","affiliations":[],"preferred":false,"id":223591,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":223590,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":60806,"text":"mf1817 - 1986 - Preliminary map showing the occurrence of siliceous rocks in central North Carolina derived from enhanced principal component Landsat images","interactions":[],"lastModifiedDate":"2012-02-10T00:10:28","indexId":"mf1817","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":"1817","title":"Preliminary map showing the occurrence of siliceous rocks in central North Carolina derived from enhanced principal component Landsat images","language":"ENGLISH","doi":"10.3133/mf1817","usgsCitation":"Schmidt, R.G., and Koslow, M., 1986, Preliminary map showing the occurrence of siliceous rocks in central North Carolina derived from enhanced principal component Landsat images: U.S. Geological Survey Miscellaneous Field Studies Map 1817, 2 maps ;44 x 46 cm. and 44 x 41 cm., on sheet 106 x 88 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1817.","productDescription":"2 maps ;44 x 46 cm. and 44 x 41 cm., on sheet 106 x 88 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106268,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7785.htm","linkFileType":{"id":5,"text":"html"},"description":"7785"},{"id":182363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.5,36 ], [ -79.5,37 ], [ -78.5,37 ], [ -78.5,36 ], [ -79.5,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696781","contributors":{"authors":[{"text":"Schmidt, R. G.","contributorId":107690,"corporation":false,"usgs":true,"family":"Schmidt","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":264420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koslow, M.H.","contributorId":90592,"corporation":false,"usgs":true,"family":"Koslow","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":264419,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40997,"text":"ofr86385 - 1986 - Preliminary charts of selected structure & thickness maps and diagrams from the Powder River Basin, Wyoming & Montana","interactions":[],"lastModifiedDate":"2021-12-09T20:42:33.176173","indexId":"ofr86385","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":"86-385","title":"Preliminary charts of selected structure & thickness maps and diagrams from the Powder River Basin, Wyoming & Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86385","usgsCitation":"Fox, J.E., and McGrath, L.A., 1986, Preliminary charts of selected structure & thickness maps and diagrams from the Powder River Basin, Wyoming & Montana: U.S. Geological Survey Open-File Report 86-385, 5 Plates: 40.24 × 25.07 inches, https://doi.org/10.3133/ofr86385.","productDescription":"5 Plates: 40.24 × 25.07 inches","costCenters":[],"links":[{"id":78882,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0385/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78881,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0385/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392690,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17021.htm"},{"id":78880,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0385/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78879,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0385/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78878,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0385/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana, Wyoming","otherGeospatial":"Powder River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.267,\n              42.703\n            ],\n            [\n              -104,\n              42.703\n            ],\n            [\n              -104,\n              45.176\n            ],\n            [\n              -107.267,\n              45.176\n            ],\n            [\n              -107.267,\n              42.703\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6983fe","contributors":{"authors":[{"text":"Fox, J. E.","contributorId":79080,"corporation":false,"usgs":true,"family":"Fox","given":"J.","middleInitial":"E.","affiliations":[],"preferred":false,"id":224303,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGrath, L. A.","contributorId":20392,"corporation":false,"usgs":true,"family":"McGrath","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":224302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69745,"text":"i1251J - 1986 - Mineral resource potential for beryllium, molybdenum, and niobium in the Charlotte 1 degree x 2 degrees quadrangle, North Carolina and South Carolina","interactions":[],"lastModifiedDate":"2026-01-23T16:21:47.833857","indexId":"i1251J","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":"1251","chapter":"J","title":"Mineral resource potential for beryllium, molybdenum, and niobium in the Charlotte 1 degree x 2 degrees quadrangle, North Carolina and South Carolina","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1251J","isbn":"0607782986","usgsCitation":"Gair, J.E., 1986, Mineral resource potential for beryllium, molybdenum, and niobium in the Charlotte 1 degree x 2 degrees quadrangle, North Carolina and South Carolina: U.S. Geological Survey IMAP 1251, 1 Plate: 44.50 x 26.85 inches, https://doi.org/10.3133/i1251J.","productDescription":"1 Plate: 44.50 x 26.85 inches","costCenters":[],"links":[{"id":256730,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1251j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256731,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1251j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256732,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1251j/report-thumb.jpg"},{"id":493394,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9073.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"North Carolina, South Carolina","otherGeospatial":"Charlotte 1 degree x 2 degrees quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80,\n              35\n            ],\n            [\n              -80,\n              36\n            ],\n            [\n              -82,\n              36\n            ],\n            [\n              -82,\n              35\n            ],\n            [\n              -80,\n              35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876e5","contributors":{"authors":[{"text":"Gair, Jacob E.","contributorId":18381,"corporation":false,"usgs":true,"family":"Gair","given":"Jacob","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":281192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6233,"text":"pp1383 - 1986 - Pliocene volcanic rocks of the Coso Range, Inyo County, California","interactions":[],"lastModifiedDate":"2018-10-24T15:38:16","indexId":"pp1383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1383","title":"Pliocene volcanic rocks of the Coso Range, Inyo County, California","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1383","usgsCitation":"Novak, S.W., and Bacon, C.R., 1986, Pliocene volcanic rocks of the Coso Range, Inyo County, California: U.S. Geological Survey Professional Paper 1383, 44 p., https://doi.org/10.3133/pp1383.","productDescription":"44 p.","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":117925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1383/report-thumb.jpg"},{"id":33438,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1383/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Inyo","otherGeospatial":"Coso Range","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684d96","contributors":{"authors":[{"text":"Novak, Steven W.","contributorId":26294,"corporation":false,"usgs":true,"family":"Novak","given":"Steven","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":152351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bacon, Charles R. 0000-0002-2165-5618 cbacon@usgs.gov","orcid":"https://orcid.org/0000-0002-2165-5618","contributorId":2909,"corporation":false,"usgs":true,"family":"Bacon","given":"Charles","email":"cbacon@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":152350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60641,"text":"mf1855 - 1986 - Map showing areas of visible land disturbances caused by two military training operations in the Mojave Desert, California","interactions":[],"lastModifiedDate":"2016-08-23T09:04:34","indexId":"mf1855","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":"1855","title":"Map showing areas of visible land disturbances caused by two military training operations in the Mojave Desert, California","docAbstract":"<p>This map shows areas that retain visible land disturbances produced during two military armored-vehicle training operations in the Mojave Desert, California. The map documents the lasting visual effects these operations have on this arid region and provides a data base for monitoring changes in the extent of visual disturbances in the future.</p>\n<p>The first training operation was initiated in April 1942, by General George S. Patton, Jr., to ready armored-vehicle divisions for desert warfare in North Africa (Meller, 1946). The Desert Training Center (DTC) encompassed 17,500 mi<sup>2</sup> of arid lands in California, Nevada, and Arizona, and for two years, more than one million soldiers trained under simulated battle conditions. Troops were stationed at 12 main base camps, each housing as many as 15,000 soldiers in canvas tents. From these camps, armored units would radiate into the broad valleys of the Mojave and Sonoran Deserts. Thousands of tanks, trucks, jeeps, and aircraft were used in the war games. When the DTC was inactivated in May 1944, most man-made structures were removed or buried by the U.S. Army.</p>\n<p>The second operation, called Operation Desert Strike, was held for two weeks in May 1964 (Moenk, 1964) in the same general area as the DTC. However, no temporary camps were established, and the tanks used were much larger than their World War II counterparts. Over 89,000 troops participated in this exercise.</p>\n<p>Land disturbances caused by these training exercises are still evident today throughout the designated training areas (Lathrop, 1983; Prose, 1985; Prose and Metzger, 1985). The World War II base-camp locations are easily identified because the networks of dirt roads are still used by campers, hunters, artifact seekers, and other visitors. Vehicle trails and single tracks remain on many relatively stable surfaces and are most conspicuous on surfaces composed of a veneer of stones (desert pavement).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1855","usgsCitation":"Prose, D., 1986, Map showing areas of visible land disturbances caused by two military training operations in the Mojave Desert, California: U.S. Geological Survey Miscellaneous Field Studies Map 1855, Plate: 29.51 x 43.22 inches, https://doi.org/10.3133/mf1855.","productDescription":"Plate: 29.51 x 43.22 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1855.JPG"},{"id":327434,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1855/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","otherGeospatial":"Mojave Desert","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,32.75 ], [ -116,35.5 ], [ -114,35.5 ], [ -114,32.75 ], [ -116,32.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db659419","contributors":{"authors":[{"text":"Prose, D.V.","contributorId":92682,"corporation":false,"usgs":true,"family":"Prose","given":"D.V.","email":"","affiliations":[],"preferred":false,"id":264123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60775,"text":"mf1848 - 1986 - Correlation of coal beds in the Fruitland Formation as interpreted from geophysical logs, east-central San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2016-08-23T09:24:02","indexId":"mf1848","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":"1848","title":"Correlation of coal beds in the Fruitland Formation as interpreted from geophysical logs, east-central San Juan County, New Mexico","docAbstract":"<p>Correlation of coal beds in the Fruitland Formation (Upper Cretaceous) in the subsurface, from interpretation of geophysical logs, is an outgrowth of unpublished studies of deep coal on the Navajo Reservation by the author in the Toadlena 30 x 60 minute quadrangle, New Mexico, and by W. J. Mapel in the Farmington 30 x 60 minute quadrangle, New Mexico. &nbsp;The lines of sections of this report extend eastward from the reservation into east-central San Juan County, which is in the western part of the San Juan Basin. &nbsp;In this area, the rocks dip gently northeast toward the central part of the basin. &nbsp;The thick coal is less than 1,500 feet beneath the surface. &nbsp;Of the 53 logs in the sections, 48 are from oil- and gas-test holes, and 5 are from coal-test holes (see table 1). &nbsp;Stratigraphic relations of the Upper Cretaceous Lewis Shale, Pictured Cliffs Sandstone, and Fruitland Formation, shown on the cross sections and briefly reviewed below, have been previously described for this or other parts of the San Juan Basin by Hayes and Zapp (1955), Beaumont (1971), Fassett and hinds (1971), O;Sullivan and other (1972), and Molenaar (1983), among others.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1848","usgsCitation":"Sandberg, D.T., 1986, Correlation of coal beds in the Fruitland Formation as interpreted from geophysical logs, east-central San Juan County, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1848, 2 Plates: 58.60 x 35.59 inches and 52.04 x 38.13 inches, https://doi.org/10.3133/mf1848.","productDescription":"2 Plates: 58.60 x 35.59 inches and 52.04 x 38.13 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1848.PNG"},{"id":327481,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1848/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327482,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1848/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"San Juan County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.36749999999999,36.25 ], [ -108.36749999999999,36.5 ], [ -107.75,36.5 ], [ -107.75,36.25 ], [ -108.36749999999999,36.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684676","contributors":{"authors":[{"text":"Sandberg, Dorothy T.","contributorId":19240,"corporation":false,"usgs":true,"family":"Sandberg","given":"Dorothy","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":264379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44410,"text":"wri864201 - 1986 - Ground-water availability in the eastern part of the Lake Ontario Basin, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864201","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":"86-4201","title":"Ground-water availability in the eastern part of the Lake Ontario Basin, New York","docAbstract":"A set of three maps show surficial geology, significant unconsolidated aquifers and well yield, and selected well locations for the Lake Ontario basin, New York. In the low areas , glaciers and wave action of former high-level lakes deposited permeable sand and gravel to form aquifers that yield more than 10 gal/min of water to wells. Small quantities of water (less than 2 gal/min) can be pumped from dug wells that top till and fine lake-sediment deposits. (USGS)","language":"ENGLISH","doi":"10.3133/wri864201","usgsCitation":"Miller, T.S., 1986, Ground-water availability in the eastern part of the Lake Ontario Basin, New York: U.S. Geological Survey Water-Resources Investigations Report 86-4201, 3 maps ; 66 x 66 cm., on sheets 76 x 76 cm. and 76 x 96 cm., folded in envelope 33 x 25 cm., https://doi.org/10.3133/wri864201.","productDescription":"3 maps ; 66 x 66 cm., on sheets 76 x 76 cm. and 76 x 96 cm., folded in envelope 33 x 25 cm.","costCenters":[],"links":[{"id":173688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81704,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81705,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81706,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d355","contributors":{"authors":[{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44426,"text":"wri864120 - 1986 - Potentiometric surface, ground-water withdrawals, and recharge area for the Lisbon aquifer in Alabama, fall 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864120","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":"86-4120","title":"Potentiometric surface, ground-water withdrawals, and recharge area for the Lisbon aquifer in Alabama, fall 1982","docAbstract":"The U.S. Geological Survey began a nationwide program in 1978, termed Regional Aquifer-System Analysis (RASA), to study a number of the major aquifer systems that provide a significant part of the country 's water supply. One of the aquifer systems chosen for study was the thick and extensive sequence of sands of Cretaceous and early Tertiary age that underlies the Coastal Plain of the southeastern United States. This system, which extends from Mississippi eastward to South Carolina, is called the Southeastern Coastal Plain aquifer system. It can be divided geohydrologically into several separate aquifers. The map presented, one of a series that portray the potentiometric surface, groundwater withdrawals, and recharge areas for aquifers in Alabama that are included in the regional system, deals with the Lisbon aquifer. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864120","usgsCitation":"Williams, J.S., Planert, M., and DeJarnette, S.S., 1986, Potentiometric surface, ground-water withdrawals, and recharge area for the Lisbon aquifer in Alabama, fall 1982: U.S. Geological Survey Water-Resources Investigations Report 86-4120, 1 map : col. ; 55 x 36 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864120.","productDescription":"1 map : col. ; 55 x 36 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81725,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4120/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db6811f6","contributors":{"authors":[{"text":"Williams, John S. johnw@usgs.gov","contributorId":329,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"johnw@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":229745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Planert, Michael","contributorId":56659,"corporation":false,"usgs":true,"family":"Planert","given":"Michael","email":"","affiliations":[],"preferred":false,"id":229747,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeJarnette, Sydney S.","contributorId":13947,"corporation":false,"usgs":true,"family":"DeJarnette","given":"Sydney","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229746,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44437,"text":"wri864010 - 1986 - Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864010","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":"86-4010","title":"Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system","docAbstract":"An investigation was conduced to define the configuration and hydrology of the rock surface upon which the sand aquifers and confining beds of the Southeastern Coastal Plain aquifer system were deposited. The base of the Southeastern Coastal Plain aquifer system consists of crystalline rocks, saprolite, Paleozoic rocks, Triassic sedimentary rocks (some of which are intruded by basalt), and Jurassic sedimentary rocks. The permeability of these rocks is extremely low and little exchange of water occurs upward to the overlying Cretaceous aquifers. Porosity values are in the range of 10% or less in some of the rocks, indicating little water is stored in them. The transmissivity values are extremely low, indicating very slow movement of water in these rocks. The small volume of water moving at a very slow rate has a long residence time and is usually mineralized to a greater degree than water in the more permeable overlying sediments. (Peters-PTT)","language":"ENGLISH","doi":"10.3133/wri864010","usgsCitation":"Wait, R.L., and Davis, M.E., 1986, Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system: U.S. Geological Survey Water-Resources Investigations Report 86-4010, 1 map : col. ; 35 x 60 cm., on sheet 80 x 79 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864010.","productDescription":"1 map : col. ; 35 x 60 cm., on sheet 80 x 79 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4010/report-thumb.jpg"},{"id":81750,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3499","contributors":{"authors":[{"text":"Wait, Robert L.","contributorId":12839,"corporation":false,"usgs":true,"family":"Wait","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Marvin E.","contributorId":36553,"corporation":false,"usgs":true,"family":"Davis","given":"Marvin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229766,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48941,"text":"ofr86240 - 1986 - Confined-drift aquifers in Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T10:25:53","indexId":"ofr86240","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":"86-240","title":"Confined-drift aquifers in Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr86240","usgsCitation":"Delin, G., 1986, Confined-drift aquifers in Minnesota: U.S. Geological Survey Open-File Report 86-240, 2 p., https://doi.org/10.3133/ofr86240.","productDescription":"2 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,{"id":27327,"text":"wri864044 - 1986 - Hydrologic conditions in Connors Bog Area, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri864044","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":"86-4044","title":"Hydrologic conditions in Connors Bog Area, Anchorage, Alaska","docAbstract":"Connors Bog is a wetland in Anchorage, Alaska, which provides a habitat for many wildlife species and is a popular area for driving off-road vehicles. A landfill, and residential and commercial developments are present in areas which were once wetland. The main source of water is precipitation, which averages about 15 in/yr. Estimates of evapotranspiration, which is the main component of water outflow, range from 10 to 20 in/yr. Minor amounts of groundwater and surface runoff flow into the area from the northeast and southwest and flow out of the area to the northwest and south. Within the wetland, water in peat and sand is unconfined and becomes more mineralized with depth. A leachate beneath and near an abandoned landfill is characterized by concentrations of dissolved solids, dissolved chloride, and total organics that are higher than those of the area 's natural water. The maximum lateral extent of detectable contamination in 1984 was &lt; 500 ft from the landfill 's edge. Water in glacial deposits that underlie a poorly permeable layer of silt and clay is confined. A well completed in this confined aquifer yielded water that had a low concentration of dissolved solids, 150 mg/L. The potentiometric surface of this aquifer was about 20 ft lower than the water table during 1984. Connors Lake occupies a depression that extends below adjacent groundwater levels. The 40-acre lake has a maximum depth of about 9 ft and a low rate of biological production. The quality of water in the lake has not been adversely impacted by nearby residential development or landfill operations. Lake levels appear to be influenced by precipitation and adjacent groundwater levels. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864044","usgsCitation":"Glass, R.L., 1986, Hydrologic conditions in Connors Bog Area, Anchorage, Alaska: U.S. Geological Survey Water-Resources Investigations Report 86-4044, iii, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864044.","productDescription":"iii, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4044/report-thumb.jpg"},{"id":56194,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6113e8","contributors":{"authors":[{"text":"Glass, R. L.","contributorId":80279,"corporation":false,"usgs":true,"family":"Glass","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34069,"text":"b1730A - 1986 - Mineral resources of the La Madre Mountains Wilderness Study Area, Clark County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:27","indexId":"b1730A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1730","chapter":"A","title":"Mineral resources of the La Madre Mountains Wilderness Study Area, Clark County, Nevada","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1730A","usgsCitation":"Conrad, J.E., Barton, H.N., and Lipton, D.A., 1986, Mineral resources of the La Madre Mountains Wilderness Study Area, Clark County, Nevada: U.S. Geological Survey Bulletin 1730, p. A1-A9, ill., maps ;28 cm., https://doi.org/10.3133/b1730A.","productDescription":"p. A1-A9, ill., maps ;28 cm.","costCenters":[],"links":[{"id":163240,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1730a/report-thumb.jpg"},{"id":61985,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1730a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a261","contributors":{"authors":[{"text":"Conrad, James E. 0000-0001-6655-694X jconrad@usgs.gov","orcid":"https://orcid.org/0000-0001-6655-694X","contributorId":2316,"corporation":false,"usgs":true,"family":"Conrad","given":"James","email":"jconrad@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":212406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barton, Harlan N.","contributorId":27842,"corporation":false,"usgs":true,"family":"Barton","given":"Harlan","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":212407,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipton, David A.","contributorId":36604,"corporation":false,"usgs":true,"family":"Lipton","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":212408,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57230,"text":"wdrTN851 - 1986 - Water resources data, Tennessee, water year 1985","interactions":[],"lastModifiedDate":"2020-11-10T17:12:26.190696","indexId":"wdrTN851","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":"TN-85-1","title":"Water resources data, Tennessee, water year 1985","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrTN851","usgsCitation":"Lowery, J., Counts, P., Edmiston, H., and Edwards, F., 1986, Water resources data, Tennessee, water year 1985: U.S. Geological Survey Water Data Report TN-85-1, xii, 411 p., https://doi.org/10.3133/wdrTN851.","productDescription":"xii, 411 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