{"pageNumber":"336","pageRowStart":"8375","pageSize":"25","recordCount":10961,"records":[{"id":5230189,"text":"5230189 - 1986 - The Breeding Bird Survey:  Its first fifteen years, 1965-1979","interactions":[],"lastModifiedDate":"2016-11-16T13:44:53","indexId":"5230189","displayToPublicDate":"2009-06-09T10:33:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"157","title":"The Breeding Bird Survey:  Its first fifteen years, 1965-1979","docAbstract":"The Breeding Bird Survey (BBS) is an ongoing cooperative program sponsored jointly by the U.S. Fish and Wildife Service and the Canadian Wildlife Service. Its main purpose is to estimate population trends of the many species of birds that nest in North America north of Mexico and that migrate across international boundaries. This survey provides information, both locally by ecological or political regions and on a continental scale, on (1) short-term population changes that can be correlated with specific weather incidents, (2) recovery periods following catastrophic declines, (3) normal year-to-year variations, (4) long-term population trends, and (5) invasions of exotics.  The BBS also permits detailed computer mapping of relative abundance of each species, either year by year to show changes in distribution and relative abundance, or the average over a period of years. It provides base-line data with which more intensive local studies can be compared.  For biogeographic studies it provides uniform sampling of bird populations by major physiographic regions across the continent. In conjunction with the Audubon Christmas Bird Count, it permits comparison of summer and winter distribution of species that winter in the United States.  Most species of North American birds migrate across international boundaries, especially those shared with Canada, Mexico, and the Soviet Union. As part of our responsibility under treaties with these nations, the U.S. Fish and Wildlife Service has developed the BBS to monitor avian population changes so that any adverse trends can be detected early. This provides the opportunity to determine the reasons for any increase or decrease, to define geographic areas in which changes are greatest, to study correlations between avian population changes and land-use changes, and to make recommendations for controlling undesirable bird population trends.  For example, the BBS can be used to detect and estimate the extent of losses resulting from widespread use of pesticides, and to reveal whether major population changes of a given species (e.g., Dickcissel) in certain States are related to a continental decline or are merely a result of population shifts within the breeding range. Effects of urban and suburban expansion are often reflected in the loss of forest interior birds.  Population trends for 230 species as well as several avian genera and families are discussed and graphed in this report. For most of these species, regional and well as continental trends are shown. The three major regions discussed are the Eastern, Central, and Western, bounded by the Mississippi River and the eastern base of the Rocky Mountains. Additional graphs for certain States or physiographic regions are included for selected species of special interest. The following paragraphs summarize general trends in the major bird families.  The native herons in general are maintaining their populations, whereas the exotic Cattle Egret continues its geographic spread and its steady increase. Waterfowl as a group are stable or increasing.  Although most widespread species of hawks are on the increase, the rarer species show evidence of decline.  Among the gallinaceous birds, the greatest change was a sharp drop in Northern Bobwhite as a result of the exceptionally cold winters of 1976-77 and 1977-78 in the Ohio Valley and the Middle Atlantic States. Killdeer populations, except for a minor decline during these two winters, showed strong increases except in the West. American Woodcock were poorly sampled by the BBS because they were relatively inactive during daylight. Common Snipe and the other common shorebirds that nest in the United States and southern Canada exhibited stable or increasing populations, especially in the Eastern and Central regions.  Herring Gull counts varied dramatically and irregularly from year to year. Laughing Gulls increased along the Atlantic coast and Franklin's Gulls declined in the interior of the continen","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Robbins, C., Bystrak, D., and Geissler, P., 1986, The Breeding Bird Survey:  Its first fifteen years, 1965-1979: Resource Publication 157, iii, 196 p.","productDescription":"iii, 196 p.","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":284991,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/5230189/report.pdf"},{"id":202759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/5230189/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad2e4b07f02db681c16","contributors":{"authors":[{"text":"Robbins, C.S.","contributorId":53907,"corporation":false,"usgs":true,"family":"Robbins","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":343697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bystrak, D.","contributorId":58220,"corporation":false,"usgs":true,"family":"Bystrak","given":"D.","email":"","affiliations":[],"preferred":false,"id":343698,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Geissler, P.H.","contributorId":24038,"corporation":false,"usgs":true,"family":"Geissler","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":343696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5210372,"text":"5210372 - 1986 - Aquatic birds and selenium in the San Joaquin Valley","interactions":[],"lastModifiedDate":"2017-05-03T16:29:30","indexId":"5210372","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1986","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Aquatic birds and selenium in the San Joaquin Valley","docAbstract":"<p>Kesterton Reservoir is a series of ponds comprising 1,200 acres sitting in the grasslands of the Kesterton National Wildlife Refuge. It is bounded on the east by the San Luis Drain, a concrete-lined canal that discharges agricultural drainage into the ponds at their southern end, from which point it then flows northward through the twelve ponds (see the map on the page following).<br></p><p>Mike Saki and I studied several of these ponds to determine the concentrations of selenium and other contaminants in food-chain organisms. You'll hear more about this from Mike shortly. My portion of the study was to determine the reproductive success of birds nesting in the ponds and to collect birds so that we could find out what they were eating and what levels of selenium were in their tissues.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Selenium and agricultural drainage:  Implications for San Francisco Bay and the California environment - Proceedings of the second selenium symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Second Selenium Symposium","conferenceDate":"Marsh 23, 1985","conferenceLocation":"Berkeley, CA","language":"English","publisher":"The Bay Institute of San Francisco","publisherLocation":"Tiburon, California","isbn":"0-937995-00-2","usgsCitation":"Ohlendorf, H.M., 1986, Aquatic birds and selenium in the San Joaquin Valley, chap. <i>of</i> Selenium and agricultural drainage:  Implications for San Francisco Bay and the California environment - Proceedings of the second selenium symposium, p. 14-24.","productDescription":"11 p.","startPage":"14","endPage":"24","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Kesterton Reservoir","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a090","contributors":{"authors":[{"text":"Ohlendorf, Harry M.","contributorId":60291,"corporation":false,"usgs":true,"family":"Ohlendorf","given":"Harry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":328279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015106,"text":"70015106 - 1986 - Mechanical response of the south flank of Kilauea volcano, Hawaii, to intrusive events along the rift systems","interactions":[],"lastModifiedDate":"2025-08-25T16:41:37.724639","indexId":"70015106","displayToPublicDate":"2003-04-10T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Mechanical response of the south flank of Kilauea volcano, Hawaii, to intrusive events along the rift systems","docAbstract":"<div class=\"u-margin-s-bottom\">Increased earthquake activity and compression of the south flank of Kilauea volcano, Hawaii, have been recognized by previous investigators to accompany rift intrusions. We further detail the temporal and spatial changes in earthquake rates and ground strain along the south flank induced by six major rift intrusions which occurred between December 1971 and January 1981. The seismic response of the south flank to individual rift intrusions is immediate; the increased rate of earthquake activity lasts from 1 to 4 weeks. Horizontal strain measurements indicate that compression of the south flank usually accompanies rift intrusions and eruptions. Emplacement of an intrusion at a depth greater than about 4 km, such as the June 1982 southwest rift intrusion, however, results in a slight extension of the subaerial portion of the south flank.</div><div class=\"u-margin-s-bottom\"><br data-mce-bogus=\"1\"></div><div class=\"u-margin-s-bottom\">Horizontal strain measurements along the south flank are used to locate the January 1983 east-rift intrusion, which resulted in eruptive activity. The intrusion is modeled as a vertical rectangular sheet with constant displacement perpendicular to the plane of the sheet. This model suggests that the intrusive body that compressed the south flank in January 1983 extended from the surface to about 2.4 km depth, and was aligned along a strike of N66°E. The intrusion is approximately 11 km in length, extended beyond the January 1983 eruptive fissures, which are 8 km in length and is contained within the 14-km-long region of shallow rift earthquakes.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(86)90200-3","issn":"00401951","usgsCitation":"Dvorak, J., Okamura, A., English, T., Koyanagi, R.Y., Nakata, J.S., Sako, M., Tanigawa, W., and Yamashita, K., 1986, Mechanical response of the south flank of Kilauea volcano, Hawaii, to intrusive events along the rift systems: Tectonophysics, v. 124, no. 3-4, p. 193-209, https://doi.org/10.1016/0040-1951(86)90200-3.","productDescription":"17 p.","startPage":"193","endPage":"209","costCenters":[],"links":[{"id":224019,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -155.46126003973447,\n              19.32313934378122\n            ],\n            [\n              -155.46126003973447,\n              19.19866425187726\n            ],\n            [\n              -155.2306109623595,\n              19.19866425187726\n            ],\n            [\n              -155.2306109623595,\n              19.32313934378122\n            ],\n            [\n              -155.46126003973447,\n              19.32313934378122\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"124","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a535ce4b0c8380cd6ca13","contributors":{"authors":[{"text":"Dvorak, J.J.","contributorId":52597,"corporation":false,"usgs":true,"family":"Dvorak","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":370089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Okamura, A.T.","contributorId":70400,"corporation":false,"usgs":true,"family":"Okamura","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":370092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"English, T.T.","contributorId":49799,"corporation":false,"usgs":true,"family":"English","given":"T.T.","email":"","affiliations":[],"preferred":false,"id":370087,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koyanagi, R. Y.","contributorId":35719,"corporation":false,"usgs":true,"family":"Koyanagi","given":"R.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":370086,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nakata, J. S.","contributorId":23940,"corporation":false,"usgs":true,"family":"Nakata","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":370085,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sako, M. K.","contributorId":50152,"corporation":false,"usgs":true,"family":"Sako","given":"M. K.","affiliations":[],"preferred":false,"id":370088,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tanigawa, W.T.","contributorId":56383,"corporation":false,"usgs":true,"family":"Tanigawa","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":370091,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Yamashita, K.M.","contributorId":54603,"corporation":false,"usgs":true,"family":"Yamashita","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":370090,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"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":60930,"text":"mf1829 - 1986 - Geologic map of the South Jackson Mountains Wilderness Study Area, Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2016-08-17T12:56:37","indexId":"mf1829","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":"1829","title":"Geologic map of the South Jackson Mountains Wilderness Study Area, Humboldt County, Nevada","docAbstract":"<p>The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine their mineral values, if any, that may be present. Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a mineral survey of the South Jackson Mountains (NV-020-603) Wilderness Study Area, Humboldt County, Nevada.</p>\n<p>The&nbsp;South Jackson Mountains Wilderness Study Area is in south-central Humboldt County, approximately 50 miles northwest of Winnemucca, Nevada. The boundaries originally specified for the wilderness study area encompassed an area of 60,211 acres. The draft Environmental Impact Statement issued in 1983 by the U.S. Bureau of Land Management (BLM) identified 20,094 acres within the wilderness study area as potentially suitable for inclusion into the National Wilderness Preservation System. Subsequent (August 27, 1984) deletions by the BLM have resulted in the present study area of approximately 10,300 acres. The boundaries of the study area are approximated by the range crestline to the east and the 4,400-ft contour along the west side of the range from King Lear Peak north to the divide between Hobo and Christiorsson Canyons.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1829","usgsCitation":"Sorensen, M.L., 1986, Geologic map of the South Jackson Mountains Wilderness Study Area, Humboldt County, Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 1829, 33.47 x 33.67 inches, https://doi.org/10.3133/mf1829.","productDescription":"33.47 x 33.67 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106085,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7501.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"48000","country":"United States","state":"Nevada","county":"Humboldt County","otherGeospatial":"South Jackson Mountains Wilderness Study Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.58333333333333,41.166666666666664 ], [ -118.58333333333333,41.333333333333336 ], [ -118.41666666666667,41.333333333333336 ], [ -118.41666666666667,41.166666666666664 ], [ -118.58333333333333,41.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a6d5","contributors":{"authors":[{"text":"Sorensen, Martin L.","contributorId":36563,"corporation":false,"usgs":true,"family":"Sorensen","given":"Martin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":264638,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57441,"text":"wdrOR841 - 1986 - Water resources data for Oregon, water year 1984. Volume 1. Eastern Oregon","interactions":[],"lastModifiedDate":"2020-10-02T21:08:31.889251","indexId":"wdrOR841","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":"OR-84-1","title":"Water resources data for Oregon, water year 1984. Volume 1. Eastern Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOR841","usgsCitation":"Hubbard, L., Smith, M., and Hubbard, L., 1986, Water resources data for Oregon, water year 1984. Volume 1. Eastern Oregon: U.S. Geological Survey Water Data Report OR-84-1, xiii, 224 p., https://doi.org/10.3133/wdrOR841.","productDescription":"xiii, 224 p.","costCenters":[],"links":[{"id":379002,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/or-84-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174531,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/or-84-1/report-thumb.jpg"}],"country":"United States","state":"Oregon","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"40\",\"properties\":{\"name\":\"Oregon\",\"nation\":\"USA  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L.L.","contributorId":81513,"corporation":false,"usgs":true,"family":"Hubbard","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":257019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, M.L.","contributorId":35386,"corporation":false,"usgs":true,"family":"Smith","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":257018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hubbard, L.E.","contributorId":104945,"corporation":false,"usgs":true,"family":"Hubbard","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":257020,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44425,"text":"wri864119 - 1986 - Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton aquifer in Alabama, fall 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864119","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":"86-4119","title":"Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton 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 for 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. This map, one of a series that portray the potentiometric surface, groundwater withdrawal, and recharge areas for the aquifers in Alabama that are included in the regional system, deals with the Nanafalia-Clayton aquifer. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864119","usgsCitation":"Williams, J.S., DeJarnette, S.S., and Planert, M., 1986, Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton aquifer in Alabama, fall 1982: U.S. Geological Survey Water-Resources Investigations Report 86-4119, 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/wri864119.","productDescription":"1 map : col. ; 55 x 36 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81724,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4119/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db682635","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":229742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeJarnette, Sydney S.","contributorId":13947,"corporation":false,"usgs":true,"family":"DeJarnette","given":"Sydney","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Planert, Michael","contributorId":56659,"corporation":false,"usgs":true,"family":"Planert","given":"Michael","email":"","affiliations":[],"preferred":false,"id":229744,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44490,"text":"wri844111 - 1986 - Hydrogeologic and water-quality characteristics of the Red River-Winnipeg aquifer northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:26:08","indexId":"wri844111","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":"84-4111","title":"Hydrogeologic and water-quality characteristics of the Red River-Winnipeg aquifer northwestern Minnesota","docAbstract":"<p>The Red River-Winnipeg aquifer of Ordovician age occupies a depression in the Proterozoic crystalline bedrock of northwestern Minnesota. The Winnipeg Formation, which underlies the Red River Formation, consists of two units: A lower shaley mudstone and an upper medium-grained sandstone. The Red River Formation consists of a lower dolomitic, dark-gray limestone and upper, slightly less-dolomitic, limestone. A porous zone at the top of the upper limestone yields most of the water to wells in the Red River-Winnipeg aquifer.</p>\n<p>Ground water generally flows eastward through the aquifer from North Dakota and discharges upward to wells and to overlying deposits. Yields of wells open to the full thickness of the aquifer range from 100 t 250 gallons per minute. The water is unsuitable for most uses because of the high mineral content. Dissolved-solids concentrations range from about 3,000 milligrams per liter in the eastern part of the aquifer to about 60,000 milligrams per liter in the northwestern corner of Minnesota.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844111","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Ruhl, J.F., and Adolphson, D.G., 1986, Hydrogeologic and water-quality characteristics of the Red River-Winnipeg aquifer northwestern Minnesota: U.S. Geological Survey Water-Resources Investigations Report 84-4111, 2 Plates: 36.02 x 29.44 inches and 36.23 x 30.42 inches, https://doi.org/10.3133/wri844111.","productDescription":"2 Plates: 36.02 x 29.44 inches and 36.23 x 30.42 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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F.","contributorId":81866,"corporation":false,"usgs":true,"family":"Ruhl","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":229868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68224,"text":"ha691 - 1986 - Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":43378,"text":"ofr84452 - 1984 - Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon","indexId":"ofr84452","publicationYear":"1984","noYear":false,"title":"Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68224,"text":"ha691 - 1986 - Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon","indexId":"ha691","publicationYear":"1986","noYear":false,"title":"Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-12T15:07:25","indexId":"ha691","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"691","title":"Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon","docAbstract":"Prompted by the need for a current, accurate, and repeatable delineation of irrigated acreage on the Snake River Plain, the U.S. Geological Survey entered into a cooperative agreement with the Idaho Department of Water Resources Image Analysis Facility and the U.S. Bureau of Reclamation to delineate 1980 land use form Landsat data. Irrigated acreage data were needed as input to groundwater flow models developed by the U.S. Geological Survey in a study of the regional aquifer system underlying the Snake River Plain. Single-date digital multispectral scanner data analyzed to delineate land-use classes. Source of irrigation water (surface water, ground water, and combined) was determined from county maps of 1975 water-related land use, data from previous investigations, and field checking. Surface-water diversions for irrigation on the Snake River Plain began in the 1840's. With the stimulus of Federal aid authorized by the Desert Land Act, Carey Act, and Reclamation Act, irrigated area increased rapidly in the early 1900's. By 1929, 2.2 million acres were irrigated. Ground water became and important source of irrigation water after World War II. In 1980, about 3.1 million acres of the Snake River Plain were irrigate: 2.0 million acres with surface water, 1.0 million with ground water, and 0.1 million with combined surface and ground water. About 5.2 million acres (half of the plain) are undeveloped rangeland, 1.0 million acres (one-tenth) are classified as barren. The remaining land is a mixture of dryland agriculture, water bodies, wetland, forests, and urban areas.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha691","usgsCitation":"Lindholm, G.F., and Goodell, S.A., 1986, Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon: U.S. Geological Survey Hydrologic Atlas 691, 1 Plate: 43.90 x 33.00 inches, https://doi.org/10.3133/ha691.","productDescription":"1 Plate: 43.90 x 33.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":187949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89581,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/691/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.25,42.0 ], [ -117.25,44.5 ], [ -111.5,44.5 ], [ -111.5,42.0 ], [ -117.25,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667289","contributors":{"authors":[{"text":"Lindholm, Gerald F.","contributorId":18374,"corporation":false,"usgs":true,"family":"Lindholm","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":277869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277870,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44493,"text":"wri844153 - 1986 - Hydrogeologic and water-quality characteristics of the Cretaceous aquifer, southwestern Minnesota","interactions":[],"lastModifiedDate":"2022-02-02T23:00:26.240537","indexId":"wri844153","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":"84-4153","title":"Hydrogeologic and water-quality characteristics of the Cretaceous aquifer, southwestern Minnesota","docAbstract":"<p>The Cretaceous aquifer in southwest Minnesota consists of discontinuous, basal sandstone beds in the Dakota Formation and the overlying Codell Sandstone Member of the Carlile Shale of the Colorado Group. These sandstone beds are not laterally or vertically persistent throughout the area and generally are separated shale beds in the Dakota Formation and in the overlying Colorado Group of Cretaceous age. Water in the Cretaceous aquifer is confined by overlying shale and by overlying till as much as 700 feet thick. Locally where the drift is permeable and thin and where the shale is missing, water in the aquifer is unconfined. Groundwater moves away from the Sioux Quartzite Ridge north toward the Minnesota River, south toward Iowa, and eastward toward the Mississippi River. Recharge to the aquifer primarily is by infiltration of precipitation that percolates through the overlying drift and underflow in the aquifer from South Dakota.</p>\n<p>Water in the Cretaceous aquifer consists of five chemical types based on predominant ions; including calcium-magnesium bicarbonate, calcium-magnesium sulfate, sodium chloride, sodium bicarbonate, and sodium sulfate type waters. Dissolved-solids, chloride, and sulfate concentrations in the aquifer locally exceed standards recommended by the U.S. Environmental Protection Agency for public supplies, particularly in areas southwest of the Minnesota River.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844153","collaboration":"Prepared in cooperation with the U.S. Geological Survey","usgsCitation":"Woodward, D.G., and Anderson, H.W., 1986, Hydrogeologic and water-quality characteristics of the Cretaceous aquifer, southwestern Minnesota: U.S. Geological Survey Water-Resources Investigations Report 84-4153, 2 Plates: 34.03 x 42.18 inches and 34.28 x 41.83 inches, https://doi.org/10.3133/wri844153.","productDescription":"2 Plates: 34.03 x 42.18 inches and 34.28 x 41.83 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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G.","contributorId":106458,"corporation":false,"usgs":true,"family":"Woodward","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":229874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, H. W. Jr.","contributorId":11187,"corporation":false,"usgs":true,"family":"Anderson","given":"H.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":229873,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59140,"text":"mf1527C - 1986 - Maps showing mines and prospects in the Southern Massanutten Roadless Area, Page and Rockingham counties, Virginia","interactions":[],"lastModifiedDate":"2016-08-22T10:06:40","indexId":"mf1527C","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":"1527","chapter":"C","title":"Maps showing mines and prospects in the Southern Massanutten Roadless Area, Page and Rockingham counties, Virginia","docAbstract":"<p>The Southern Massanutten Roadless Area contains about 11,800 acres in the George Washington National Forest in the Valley and Ridge physiographic province of west-central Virginia. &nbsp;The area, which is 13 mi long and 1 to 2 mi wide, is in Page and Rockingham Counties on the eastern side of the Shenandoah Valley, between the North and South Forks of the Shenandoah River. &nbsp;The north end is 11 mi southwest of Luray and the south end is 7 mi east of Harrisonburg (fig. 1). &nbsp;The roadless area is characterized by a series of long sandstone ridges collectively called Massanutten Mountain. &nbsp;Ridge crests are 1,100 to 1,900 ft above the Shenandoah Valley floor, and are composed principally of resistant Massanutten Sandstone, which is overlain by thin shales and limestones bearing iron mineralization. &nbsp;The Martinsburg Shale and several limestones rock units underlie the Massanutten Sandstone (Brent, 1960, pl. 1.; Allen, 1967, pl. 1). &nbsp;The entire sequence has been folded into a synclinorium (Brent, 1960, p. 81).</p>\n<p>Although many of these strata have been mined in the Shenandoah Valley, production of mineral commodities from within the roadless area has been minimal (fig. 1).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1527C","usgsCitation":"Chatman, M.L., and Behum, P.T., 1986, Maps showing mines and prospects in the Southern Massanutten Roadless Area, Page and Rockingham counties, Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1527, 37.17 x 27.33 inches, https://doi.org/10.3133/mf1527C.","productDescription":"37.17 x 27.33 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1527C.PNG"},{"id":327188,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1527-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Virginia","county":"Page County, Rockingham County","otherGeospatial":"Southern Massanutten Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78.75,38.3675 ], [ -78.75,38.6175 ], [ -78.61749999999999,38.6175 ], [ -78.61749999999999,38.3675 ], [ -78.75,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605cb3","contributors":{"authors":[{"text":"Chatman, Mark L.","contributorId":97878,"corporation":false,"usgs":true,"family":"Chatman","given":"Mark","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":261498,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behum, Paul T.","contributorId":86894,"corporation":false,"usgs":true,"family":"Behum","given":"Paul","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":261499,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44433,"text":"wri854305 - 1986 - Potentiometric-surface map of the Wyodak-Anderson coal bed, Powder River structural basin, Wyoming, 1973-84","interactions":[],"lastModifiedDate":"2022-12-15T21:01:05.133802","indexId":"wri854305","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":"85-4305","title":"Potentiometric-surface map of the Wyodak-Anderson coal bed, Powder River structural basin, Wyoming, 1973-84","docAbstract":"Previous water level maps of shallow aquifers in the Powder River structural basin in Wyoming were based on water levels from wells completed in different stratigraphic intervals within thick sequences of sedimentary rocks. A potentiometric surface using water levels from a single aquifer had never been mapped throughout the basin. The sandstone aquifers in the Fort Union Formation of Paleocene age and the Wasatch Formation of Eocene age are discontinuous and lenticular, and do not extend even short distances. Coal aquifers are more continuous and the Wyodak-Anderson coal bed, in the Fort Union Formation, has been mapped in much of the Powder River structural basin in Wyoming. Water level altitudes in the Wyodak-Anderson coal bed and other stratigraphically equivalent coal beds were mapped to determine if they represent a continuous potentiometric surface in the Powder River structural basin. The potentiometric surface, except in the vicinity of the Wyodak mine east of Gillette, represents a premining condition as it was based on water level measurements made during 1973-84 that were not significantly affected by mining. The map was prepared in cooperation with the U.S. Bureau of Land Management. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854305","usgsCitation":"Daddow, P.B., 1986, Potentiometric-surface map of the Wyodak-Anderson coal bed, Powder River structural basin, Wyoming, 1973-84: U.S. Geological Survey Water-Resources Investigations Report 85-4305, 1 Plate: 41.93 × 35.61 inches, https://doi.org/10.3133/wri854305.","productDescription":"1 Plate: 41.93 × 35.61 inches","costCenters":[],"links":[{"id":173276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410576,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36439.htm","linkFileType":{"id":5,"text":"html"}},{"id":81734,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4305/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Powder River structural basin, Wyodak-Anderson coal bed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107,\n              45\n            ],\n            [\n              -107,\n              43.317\n            ],\n            [\n              -105.094,\n              43.317\n            ],\n            [\n              -105.094,\n              45\n            ],\n            [\n              -107,\n              45\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681e8b","contributors":{"authors":[{"text":"Daddow, Pamela B.","contributorId":7762,"corporation":false,"usgs":true,"family":"Daddow","given":"Pamela","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":229761,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44445,"text":"wri864059 - 1986 - Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980","interactions":[],"lastModifiedDate":"2019-08-20T09:41:43","indexId":"wri864059","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":"86-4059","title":"Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980","docAbstract":"Generalized contours of the altitude of water levels in wells completed in the Catahoula aquifer in central Louisiana, are illustrated by this map. Most water level measurements used in compiling the map were made in 1980; however, in parts of the State where water levels from 1980 were unavailable and where evidence indicated little change in water level, some measurements from as early as 1961 and as late as 1982 were used. Groundwater levels in and near the outcrop areas fluctuate 2 ft or less yearly and no significant long-term declines have occurred. The slow downward trend in water level altitude since early 1976 may be caused by pumpage from the Catahoula aquifer by a rural water system approximately 3 miles away. Recharge to the Catahoula aquifer occurs by rainfall on the upland outcrop-subcrop areas. Saltwater occurs throughout the Catahoula aquifer downgradient from the outcrop area. The ' approximate limit of freshwater ' line on the map indicates the downgradient limit of water with a concentration of chloride &lt; 250 mg/L; the line was determined using water quality data and analysis of resistivity curves from geophysical well logs. Water from the Catahoula aquifer is used for municipal, industrial, and domestic purposes. Total pumpage from the aquifer in Louisiana was slightly over 1.1 million gallons/day in 1980. Local cones of depression result from pumpage just east of Anacoco in Vernon Parish and northwest of Jonesville in Catahoula Parish. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri864059","usgsCitation":"Martin, A., and Whiteman, C.D., 1986, Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980: U.S. Geological Survey Water-Resources Investigations Report 86-4059, 1 Plate: 35.86 x 22.96 inches, https://doi.org/10.3133/wri864059.","productDescription":"1 Plate: 35.86 x 22.96 inches","costCenters":[],"links":[{"id":366594,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4059/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4059/report-thumb.jpg"}],"country":"United States","state":"Louisiana","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aecc1","contributors":{"authors":[{"text":"Martin, Angel Jr.","contributorId":42571,"corporation":false,"usgs":true,"family":"Martin","given":"Angel","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":229777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whiteman, Charles D. Jr.","contributorId":108081,"corporation":false,"usgs":true,"family":"Whiteman","given":"Charles","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229778,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59645,"text":"mf1858 - 1986 - Log of an exploratory trench in the New Madrid seismic zone near Blytheville, Arkansas","interactions":[],"lastModifiedDate":"2026-02-20T21:47:40.836609","indexId":"mf1858","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":"1858","title":"Log of an exploratory trench in the New Madrid seismic zone near Blytheville, Arkansas","docAbstract":"<p>During the winter of 1811-12, at least three major earthquakes having estimated magnitudes of M<sub>S</sub> 8.3-8.8 (Nuttli and Herrmann, 1984) struck the area near New Madrid, Mo. Since the 1811-12 series of earthquakes, 20 damaging earthquakes have occurred in the area (Nuttli, 1982), making the New Madrid seismic zone (fig. 1) the most seismically active area in the Eastern United States (Hadley and Devine, 1974). &nbsp;The zone, extending from about lat 35<strong>&deg;&nbsp;</strong>to 37<strong>&deg;&nbsp;</strong>N., approximately parallels the Mississippi River and encompasses an area roughly 50 km wide (Nuttli, 1979).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1858","usgsCitation":"Haller, K., and Crone, A.J., 1986, Log of an exploratory trench in the New Madrid seismic zone near Blytheville, Arkansas: U.S. Geological Survey Miscellaneous Field Studies Map 1858, 53.88 x 40.29 inches, https://doi.org/10.3133/mf1858.","productDescription":"1 Plate: 53.88 x 40.29 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":327243,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1858/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185402,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1858.PNG"}],"country":"United States","state":"Arkansas","city":"Blytheville","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.0120162963867,\n              35.84063820179092\n            ],\n            [\n              -90.0120162963867,\n              35.88237433729238\n            ],\n            [\n              -89.92584228515625,\n              35.88237433729238\n            ],\n            [\n              -89.92584228515625,\n              35.84063820179092\n            ],\n            [\n              -90.0120162963867,\n              35.84063820179092\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c091","contributors":{"authors":[{"text":"Haller, Kathleen M. haller@usgs.gov","contributorId":1331,"corporation":false,"usgs":true,"family":"Haller","given":"Kathleen M.","email":"haller@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":262368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crone, Anthony J. 0000-0002-3006-406X crone@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-406X","contributorId":790,"corporation":false,"usgs":true,"family":"Crone","given":"Anthony","email":"crone@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":262367,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63495,"text":"gp969 - 1986 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":40338,"text":"ofr84587 - 1984 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"ofr84587","publicationYear":"1984","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":63495,"text":"gp969 - 1986 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"gp969","publicationYear":"1986","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2025-07-18T17:59:17.777186","indexId":"gp969","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"969","title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp969","usgsCitation":"Whitehead, R., 1986, Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Geophysical Investigations Map 969, 1 Plate: 51.75 x 38.21 inches, https://doi.org/10.3133/gp969.","productDescription":"1 Plate: 51.75 x 38.21 inches","costCenters":[],"links":[{"id":253138,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0969/report-thumb.jpg"},{"id":249608,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0969/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249609,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0969/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":492572,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6311.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"2000000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110,\n              42\n            ],\n            [\n              -110,\n              45\n            ],\n            [\n              -118,\n              45\n            ],\n            [\n              -118,\n              42\n            ],\n            [\n              -110,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a971b","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":268988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61520,"text":"mf1581B - 1986 - Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon","interactions":[],"lastModifiedDate":"2016-08-23T10:39:47","indexId":"mf1581B","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":"1581","chapter":"B","title":"Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon","docAbstract":"<p><span>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and submitted to the President&nbsp;and the Congress. This report presents the analytical results of a geochemical survey of the North Fork John Day River Roadless Area&nbsp;(B6253) in the Umatilla and Wallowa-Whitman&nbsp;National Forests, Grant County, Oregon. The North Fork John Day River Roadless Area was classified&nbsp;as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</span></p>\n<p><span>The North Fork John Day River Roadless Area comprised 21,210 acres in the&nbsp;Umatilla and Wallowa-Whitman&nbsp;National Forests, Grant County, Oregon, about 30 miles northwest of Baker, Oregon. The irregularly shaped area extends for about 1 mile on both sides of a 25-mile segment of the North Fork John Day River from Big Creek on the west to North Fork John Day Campground on the east. Most of the roadless area is in the northern half of the Desolation Butte 15-minute quadrangle. The eastern end of the area is in parts of the Granite and Trout Meadows 7&frac12;-minute quadrangles.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1581B","usgsCitation":"Evans, J.G., 1986, Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1581, 36.58 x 25.48 inches, https://doi.org/10.3133/mf1581B.","productDescription":"36.58 x 25.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":182476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1581b.PNG"},{"id":327606,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1581-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Grant County","otherGeospatial":"North Fork John Day River Roadless Area, Umatilla National Forest, Wallowa-Whitman National Forest","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.66666666666667,44.833333333333336 ], [ -118.66666666666667,45 ], [ -118.41666666666667,45 ], [ -118.41666666666667,44.833333333333336 ], [ -118.66666666666667,44.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1f7","contributors":{"authors":[{"text":"Evans, James G. jevans@usgs.gov","contributorId":2396,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"jevans@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":265863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44472,"text":"wri854109 - 1986 - Distribution and altitude of the top of saline ground water in the southeastern Coastal Plain","interactions":[],"lastModifiedDate":"2023-01-13T21:31:44.796146","indexId":"wri854109","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":"85-4109","title":"Distribution and altitude of the top of saline ground water in the southeastern Coastal Plain","docAbstract":"<p>A map prepared by the U.S. Geological Survey shows the approximate distribution of saline water (greater than 10,000 mg/L as NaCl) in the Southeastern Coastal Plain. The primary distribution of saline water is in Cretaceous sediments and may be characterized as an extensive body of fluid whose upper surface generally slopes upward from inland toward coastal areas. Some freshwater appears to occupy parts of the deeper water-bearing zones in Georgia. A small amount of saline water appears to occupy a narrow upper zone of limited extent in lower Tertiary sediments in Georgia and parts of South Carolina. The freshwater-saline water interface for the lower zone lies offshore, east of the South Carolina coast. Consequently, the saline water distribution is inferred offshore.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854109","usgsCitation":"Lee, R.W., DeJarnette, S.S., and Barker, R.A., 1986, Distribution and altitude of the top of saline ground water in the southeastern Coastal Plain: U.S. Geological Survey Water-Resources Investigations Report 85-4109, 1 Plate: 27.10 x 21.13 inches, https://doi.org/10.3133/wri854109.","productDescription":"1 Plate: 27.10 x 21.13 inches","costCenters":[],"links":[{"id":411923,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36275.htm","linkFileType":{"id":5,"text":"html"}},{"id":81821,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":134858,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4109/report-thumb.jpg"}],"country":"United States","otherGeospatial":"southeastern Coastal Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -91.604,\n              35\n            ],\n            [\n              -91.604,\n              30\n            ],\n            [\n              -80,\n              30\n            ],\n            [\n              -80,\n              35\n            ],\n            [\n              -91.604,\n              35\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649df9","contributors":{"authors":[{"text":"Lee, Roger W.","contributorId":105273,"corporation":false,"usgs":true,"family":"Lee","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":229835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeJarnette, Sydney S.","contributorId":13947,"corporation":false,"usgs":true,"family":"DeJarnette","given":"Sydney","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barker, Rene A.","contributorId":82669,"corporation":false,"usgs":true,"family":"Barker","given":"Rene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":229834,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":64956,"text":"i1687 - 1986 - Divisions of potential fracture permeability, based on distribution of structures and linear features in sedimentary rocks, northern Great Plains-Rocky Mountains region of Montana, North Dakota, South Dakota, Wyoming, and northern Nebraska","interactions":[],"lastModifiedDate":"2016-08-23T10:46:20","indexId":"i1687","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":"1687","title":"Divisions of potential fracture permeability, based on distribution of structures and linear features in sedimentary rocks, northern Great Plains-Rocky Mountains region of Montana, North Dakota, South Dakota, Wyoming, and northern Nebraska","docAbstract":"<p>Division of fracture traces in sedimentary rocks of Cenozoic to Precambrian Age - Eastern and central North and South Dakota and northern Nebraska include only Cenozoic to Pennsylvanian rocks at the surface and at relatively shallow depths; the area of shallow thrust faulting in north-central Montana includes many Cretaceous rocks. Fractures in the deeper rocks in these areas vary, depending on the local structure. Large areas of western Montana are underlain by Precambrian sedimentary rocks.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/i1687","usgsCitation":"Cooley, M.E., 1986, Divisions of potential fracture permeability, based on distribution of structures and linear features in sedimentary rocks, northern Great Plains-Rocky Mountains region of Montana, North Dakota, South Dakota, Wyoming, and northern Nebraska: U.S. Geological Survey IMAP 1687, 56.32 x 32.57 inches, https://doi.org/10.3133/i1687.","productDescription":"56.32 x 32.57 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":189617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i1687.PNG"},{"id":327620,"rank":701,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1687/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":107101,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9881.htm","linkFileType":{"id":5,"text":"html"},"description":"9881"}],"scale":"5000","country":"United States","state":"Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,41 ], [ -114,49 ], [ -96,49 ], [ -96,41 ], [ -114,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d85c","contributors":{"authors":[{"text":"Cooley, Maurice E.","contributorId":8077,"corporation":false,"usgs":true,"family":"Cooley","given":"Maurice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":272419,"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":56214,"text":"wdrNY851 - 1986 - Water resources data, New York, water year 1985, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2020-11-23T19:05:37.917599","indexId":"wdrNY851","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":"NY-85-1","title":"Water resources data, New York, water year 1985, volume 1, eastern New York, excluding Long Island","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY851","usgsCitation":"Firda, G., Lumia, R., Archer, R., and Burke, P.M., 1986, Water resources data, New York, water year 1985, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report NY-85-1, ix, 268 p., https://doi.org/10.3133/wdrNY851.","productDescription":"ix, 268 p.","costCenters":[],"links":[{"id":380707,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/ny-85-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/ny-85-1/report-thumb.jpg"}],"country":"United States","state":"New 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,{"id":59112,"text":"mf1572C - 1986 - Mineral resource assessment map of the Big Gum Swamp Roadless Area, Columbia and Baker counties, Florida","interactions":[],"lastModifiedDate":"2016-08-22T09:53:10","indexId":"mf1572C","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":"1572","chapter":"C","title":"Mineral resource assessment map of the Big Gum Swamp Roadless Area, Columbia and Baker counties, Florida","docAbstract":"<p>The Big Gum Swamp Roadless Area (figs, 1 and 2) comprises 13,600 acres in the north-central part of the Osceola National Forest in Columbia and Baker Counties, about 12 airline miles northeast of Lake City, Fla. The area is bounded by Forest Service road 211 and Florida highway 250 on the south, Forest Service roads 233 and 232 on the west and north, and Forest Service road 235 on the east. The area can be reached by traveling 11.7 mi on Florida Highway 250 northeast from its junction with U.S. Highway 441, north of Lake City to the junction of Highway 250 and Forest Service road 233, thence north 1.3 mi on the Forest Service road to the southern corner of the area.</p>\n<p>The geology of the Big Cum Swamp Roadless Area, which is discussed briefly in this report, is covered in somewhat more detail in a report by Patterson, Cathcart, Cameron, and Schruben (1984). The mineral resource potential is quite similar to that in the Natural Area Roadless Area outlined by Cathcart, Patterson and Crandall (1983). The Natural Area, which is east of the eastern boundary of the Big Gum Swamp (fig. 1), also was designated a Wilderness Study Area by Public Law 98-430, September 28, 1984.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1572C","usgsCitation":"Cathcart, J., Cameron, C., and Patterson, S.H., 1986, Mineral resource assessment map of the Big Gum Swamp Roadless Area, Columbia and Baker counties, Florida: U.S. Geological Survey Miscellaneous Field Studies Map 1572, Plate: 39.97 x 40.90 inches, https://doi.org/10.3133/mf1572C.","productDescription":"Plate: 39.97 x 40.90 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326361,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1572C.JPG"},{"id":327168,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1572-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Florida","county":"Baker County, Columbia County","otherGeospatial":"Big Gum Swamp Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.5,30 ], [ -82.5,30.5 ], [ -82.36749999999999,30.5 ], [ -82.36749999999999,30 ], [ -82.5,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aec5","contributors":{"authors":[{"text":"Cathcart, J.B.","contributorId":83533,"corporation":false,"usgs":true,"family":"Cathcart","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":261434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cameron, C. C.","contributorId":94299,"corporation":false,"usgs":true,"family":"Cameron","given":"C. C.","affiliations":[],"preferred":false,"id":261436,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patterson, S. H.","contributorId":85232,"corporation":false,"usgs":true,"family":"Patterson","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":261435,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66329,"text":"i1727B - 1986 - Generalized fence diagram showing principal coal and key marine beds of Pennsylvanian age in the Hazard 30' x 60' quadrangle, eastern Kentucky","interactions":[],"lastModifiedDate":"2025-08-13T21:04:30.040623","indexId":"i1727B","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":"1727","chapter":"B","title":"Generalized fence diagram showing principal coal and key marine beds of Pennsylvanian age in the Hazard 30' x 60' quadrangle, eastern Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1727B","usgsCitation":"Kradyna, J.W., and Rice, C.L., 1986, Generalized fence diagram showing principal coal and key marine beds of Pennsylvanian age in the Hazard 30' x 60' quadrangle, eastern Kentucky: U.S. Geological Survey IMAP 1727, 1 Plate: 50.23 x 30.30 inches, https://doi.org/10.3133/i1727B.","productDescription":"1 Plate: 50.23 x 30.30 inches","costCenters":[],"links":[{"id":494066,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9897.htm","linkFileType":{"id":5,"text":"html"}},{"id":255801,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1727b/report-thumb.jpg"},{"id":255800,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1727b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255799,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1727b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Kentucky","otherGeospatial":"Hazard 30' x 60' quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -83,\n              37.5\n            ],\n            [\n              -84,\n              37.5\n            ],\n            [\n              -84,\n              37\n            ],\n            [\n              -83,\n              37\n            ],\n            [\n              -83,\n              37.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6af9b2","contributors":{"authors":[{"text":"Kradyna, J. W.","contributorId":20020,"corporation":false,"usgs":true,"family":"Kradyna","given":"J.","middleInitial":"W.","affiliations":[],"preferred":false,"id":274358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, C. L.","contributorId":60658,"corporation":false,"usgs":true,"family":"Rice","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":274359,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58800,"text":"mf1532B - 1986 - Summary geochemical maps for samples of rock, stream sediment, and nonmagnetic heavy-mineral concentrate, Cypress Roadless Area, Kern County, California","interactions":[],"lastModifiedDate":"2016-08-22T09:34:04","indexId":"mf1532B","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":"1532","chapter":"B","title":"Summary geochemical maps for samples of rock, stream sediment, and nonmagnetic heavy-mineral concentrate, Cypress Roadless Area, Kern County, California","docAbstract":"<p>The Cypress Roadless Area comprises approximately 3 square miles (1,949 acres) of Sequoia National Forest, Kern County, California. The area is at the southern end of the Sierra Nevada, approximately 30 miles east-northeast of Bakersfield, and 2.5 miles and 3.5 miles south-southeast of the communities of Bodfish and Lake Isabella, respectively (index map). Geochemical sampling was conducted during 1980 and 1981. This report summarizes the results of that investigation and provides details of the geochemical evaluation used in the final mineral resource assessment of the study area (Kennedy and others, 1983).</p>\n<p>Map A shows the locations of all sites sampled for this report and the distributions of anomalous concentrations of 4 elements in 33 samples of rock, 5 elements in 34 samples of minus-60-mesh stream sediment, and 11 elements in 33 samples of nonmagnetic heavy-mineral concentrate derived from stream sediment. Map B shows outlines of those drainage basins containing samples of stream sediment and concentrate with anomalous concentrations and also shows weighted values for each outlined basin based on the number of elements with anomalous concentrations in each stream-sediment and concentrate sample and on the degree to which these concentrations are anomalous in each sample.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1532B","usgsCitation":"Chaffee, M., Fey, D., Hill, R.H., and Sutley, S.J., 1986, Summary geochemical maps for samples of rock, stream sediment, and nonmagnetic heavy-mineral concentrate, Cypress Roadless Area, Kern County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1532, Plate: 35.40 x 39.85 inches, https://doi.org/10.3133/mf1532B.","productDescription":"Plate: 35.40 x 39.85 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":184166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1532B.JPG"},{"id":327135,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1532-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"California","county":"Kern County","otherGeospatial":"Cypress Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.5,35.5 ], [ -118.5,35.583333333333336 ], [ -118.41666666666667,35.583333333333336 ], [ -118.41666666666667,35.5 ], [ -118.5,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6995a4","contributors":{"authors":[{"text":"Chaffee, M.A.","contributorId":108049,"corporation":false,"usgs":true,"family":"Chaffee","given":"M.A.","affiliations":[],"preferred":false,"id":260853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":260850,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hill, R. H.","contributorId":57059,"corporation":false,"usgs":true,"family":"Hill","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":260851,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":260852,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":60454,"text":"mf1842 - 1986 - Thermal maturity map of the lower part of the Upper Cretaceous Mesaverde Group, Uintah Basin, Utah","interactions":[],"lastModifiedDate":"2016-08-23T08:28:01","indexId":"mf1842","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":"1842","title":"Thermal maturity map of the lower part of the Upper Cretaceous Mesaverde Group, Uintah Basin, Utah","docAbstract":"<p>The ability of rock to generate oil and gas is directly related to the type and quantity of kerogen and to its thermal maturity; therefore, thermal maturity is a commonly used tool for oil and gas exploration. &nbsp;The purpose of this study ws to provide a thermal-maturity map for the lower part of the Upper Cretaceous Mesaverde Group in the eastern part of the Uinta Basin. &nbsp;Prior to this study, thermal-maturity data were not available for the Uinta Basin. &nbsp;This study uses coal rank to show the thermal maturity of the associated rocks. &nbsp;The map was prepared in cooperation with the U.S. Department of Energy under its western gas sands project.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1842","usgsCitation":"Nuccio, V.F., and Johnson, R.C., 1986, Thermal maturity map of the lower part of the Upper Cretaceous Mesaverde Group, Uintah Basin, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1842, 50.15 x 40.19 inches, https://doi.org/10.3133/mf1842.","productDescription":"50.15 x 40.19 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1842.PNG"},{"id":327388,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1842/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Utah","otherGeospatial":"Uinta Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,39 ], [ -111,40.25 ], [ -109,40.25 ], [ -109,39 ], [ -111,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a56e4b07f02db62dd8d","contributors":{"authors":[{"text":"Nuccio, Vito F. vnuccio@usgs.gov","contributorId":853,"corporation":false,"usgs":true,"family":"Nuccio","given":"Vito","email":"vnuccio@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":263778,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Ronald C. 0000-0002-6197-5165 rcjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-6197-5165","contributorId":1550,"corporation":false,"usgs":true,"family":"Johnson","given":"Ronald","email":"rcjohnson@usgs.gov","middleInitial":"C.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":263779,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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