{"pageNumber":"384","pageRowStart":"9575","pageSize":"25","recordCount":11004,"records":[{"id":3771,"text":"cir743 - 1976 - Land and natural resource information and some potential environmental effects of surface mining of coal in the Gillette area, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"cir743","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"743","title":"Land and natural resource information and some potential environmental effects of surface mining of coal in the Gillette area, Wyoming","docAbstract":"Campbell County, along the east margin of the Powder River Basin in northeastern Wyoming, contains more coal than any other county in the United States. The principal deposit is the Wyodak-Anderson coal bed. The bed is 50-100 feet (15-30 meters) thick over large areas, lies less than 200 feet (60 meters) deep in a north-south trending strip nearly 100 miles (161 kilometers) long and 2-3 miles (3-5 kilometers) wide, and contains an estimated 15 billion tons (13.6 billion metric tons) of sub-bituminous, low-sulfur coal that is presently considered to be accessible to surface mining. Extensive mining of this deposit has the potential for causing a variety of environmental impacts and has been a matter of much public concern and debate in recent years. \r\n\r\nAn integrated program of geologic, hydrologic, geochemical, and related studies by the U.S. Geological Survey in central Campbell County provides basic information about the land and its resources, including (1) characteristics of the landscape, (2) properties of rocks and surface materials, (3) depth and thickness of coal, (4) streamflow, (5) depth to ground water, (6) quality of ground water, (7) sediment yield, (8) concentrations of trace elements in soils, rocks, coal, vegetation, and water, and (9) current land use. The data are used to analyze and predict some of the potential environmental effects of surface mining, such as the extent of land disturbance, nature and degree of landscape modification, and disruption of surface-water and ground-water systems. Advance knowledge and understanding of these and other problems are useful in the planning and regulation of future leasing, mining, reclamation, and related activities.","language":"ENGLISH","publisher":"U.S. Dept. of Interior, Geological Survey : distributed by Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir743","usgsCitation":"Keefer, W.R., and Hadley, R.F., 1976, Land and natural resource information and some potential environmental effects of surface mining of coal in the Gillette area, Wyoming: U.S. Geological Survey Circular 743, vi, 27 p. :ill., maps ;26 cm. , https://doi.org/10.3133/cir743.","productDescription":"vi, 27 p. :ill., maps ;26 cm. ","costCenters":[],"links":[{"id":124502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1976/0743/report-thumb.jpg"},{"id":30838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1976/0743/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b12d5","contributors":{"authors":[{"text":"Keefer, William Richard","contributorId":12024,"corporation":false,"usgs":true,"family":"Keefer","given":"William","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":147572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":147573,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38660,"text":"pp909 - 1976 - Boundaries of the United States and the several States","interactions":[],"lastModifiedDate":"2018-07-31T10:56:53","indexId":"pp909","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"909","title":"Boundaries of the United States and the several States","docAbstract":"<p>The original territory of the United States, as defined by the treaties of November 30, 1782, and September 3, 1783, with Great Britain, was bounded on the north by Canada, on the south by the Spanish Colonies of East and West Florida, on the east by the Atlantic Ocean, and on the west by the Mississippi River. It included the Thirteen Original Colonies and the areas claimed by them.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp909","usgsCitation":"Van Zandt, F., 1976, Boundaries of the United States and the several States: U.S. Geological Survey Professional Paper 909, ix, 191 p., https://doi.org/10.3133/pp909.","productDescription":"ix, 191 p.","costCenters":[],"links":[{"id":93854,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0909/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0909/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fce11","contributors":{"authors":[{"text":"Van Zandt, F. K.","contributorId":96743,"corporation":false,"usgs":true,"family":"Van Zandt","given":"F. K.","affiliations":[],"preferred":false,"id":220237,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11371,"text":"ofr76580 - 1976 - Water resources of Dinosaur National Monument, Colorado and Utah","interactions":[],"lastModifiedDate":"2017-09-03T13:33:22","indexId":"ofr76580","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-580","title":"Water resources of Dinosaur National Monument, Colorado and Utah","docAbstract":"<p>Dinosaur National Monument, partly in the Rocky Mountain System and partly in the Colorado Plateaus physiographic province, covers an area of 322 square miles (834 square kilometres) in northwestern Colorado and northeastern Utah. The climate is generally cool and pleasant in May, early June, September, and October; winters are cold. Normal annual precipitation ranges from less than 8 to more than 16 inches (203 to 406 millimetres).</p><p>Geologic formations in the monument range in age from upper Precambrian to Holocene, but not all ages are represented. The monument is on the south limb of the east-trending regional fold representing the Uinta Mountains. Faults and subsidary folds on the south slope of the Uinta Mountains complicate the geology and hydrology of the area.</p><p>None of the surface streams in the monument are diverted for public supply, but the Green and Yampa Rivers are a recreational resource for boaters. The flow of the Green River is regulated by Flaming Gorge Reservoir; however, flood potentials are estimated for the Yampa River and three smaller streams. Facilities in the monument are not endangered by probable mean annual floods, but may sustain some damage to facilities by the 25- or 50-year floods.</p><p>Major aquifers in the monument are sandstone and limestone formations, but these formations are drained in the higher areas. Alluvium along the major stream channels yields small amounts of water to wells, but some of the water is not of suitable chemical quality for public supply. All public water supplies in 1971 were obtained from wells, and the use of water during 1970 was estimated to be 15 million gallons (46 acre-feet or 0.057 cubic hectometres). Most of the ground water obtained from sandstone and limestone is of suitable chemical quality for public supply.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr76580","usgsCitation":"Sumsion, C.T., 1976, Water resources of Dinosaur National Monument, Colorado and Utah: U.S. Geological Survey Open-File Report 76-580, Report: 68 p.; 3 Plates: 48.25 in. x. 27.49 in. or smaller, https://doi.org/10.3133/ofr76580.","productDescription":"Report: 68 p.; 3 Plates: 48.25 in. x. 27.49 in. or smaller","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":143158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0580/report-thumb.jpg"},{"id":39195,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0580/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Topographic map of the Dinosaur National Monument, Colorado-Utah"},{"id":39196,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0580/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39197,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0580/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39198,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0580/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Dinosaur National Monument","publicComments":"Prepared for the U.S. National Park Service","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601a2c","contributors":{"authors":[{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":163018,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15025,"text":"ofr76206 - 1976 - Report on the environmental geology OCS area, eastern Gulf of Alaska","interactions":[],"lastModifiedDate":"2023-07-31T22:54:36.648543","indexId":"ofr76206","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-206","title":"Report on the environmental geology OCS area, eastern Gulf of Alaska","docAbstract":"<p>In anticipation of oil and gas leasing of the outer continental shelf (OCS lease area 39) in the northeastern Gulf of Alaska, the U. S. Geological Survey began a regional reconnaissance in 1974. The study area, which extends from Prince William Sound on the west to Yakutat Bay on the east, is in a region fraught with natural hazards. The tectonic history of the area suggests that future major earthquakes could pose serious hazards to installations on the continental shelf or along the coast of the Gulf of Alaska. The hazard may be either direct, by ground shaking or fault displacement, or indirect, through ground failure or generation of tsunami waves. Storm waves sometimes are responsible for ground failures, especially in areas of rapid accumulation of sediment.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76206","usgsCitation":"Molnia, B.F., Carlson, P.R., and Bruns, T.R., 1976, Report on the environmental geology OCS area, eastern Gulf of Alaska: U.S. Geological Survey Open-File Report 76-206, 28 p., https://doi.org/10.3133/ofr76206.","productDescription":"28 p.","costCenters":[],"links":[{"id":419458,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0206/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148074,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0206/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"eastern Gulf of Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -150.30411340796635,\n              60.79330727975059\n            ],\n            [\n              -150.30411340796635,\n              58.63019074389118\n            ],\n            [\n              -138.8408174572727,\n              58.63019074389118\n            ],\n            [\n              -138.8408174572727,\n              60.79330727975059\n            ],\n            [\n              -150.30411340796635,\n              60.79330727975059\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f56f","contributors":{"authors":[{"text":"Molnia, Bruce F. bmolnia@usgs.gov","contributorId":4002,"corporation":false,"usgs":true,"family":"Molnia","given":"Bruce","email":"bmolnia@usgs.gov","middleInitial":"F.","affiliations":[{"id":410,"text":"National Center","active":false,"usgs":true}],"preferred":false,"id":170434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":170436,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bruns, Terry R.","contributorId":29420,"corporation":false,"usgs":true,"family":"Bruns","given":"Terry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":170435,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68405,"text":"ha550 - 1976 - Water resources of south-central Missouri","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"ha550","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"550","title":"Water resources of south-central Missouri","docAbstract":"This atlas describes hydrology in an area of approximately 23 ,000 sq mi and includes all or parts of 38 counties in Missouri. The area is bounded on the north by the southern edge of the Missouri River flood plain, on the east by the Mississippi River and the Plateaus-Lowlands boundary (Ozark Escarpment), on the south by the Missouri-Arkansas State line, and on the west by the western drainage divides of the Gasconade and White River basins. The alluvial valley of the Missouri River is excluded. Although the populations of several rural counties in the area have declined in recent years, significant population increases have occurred in the vicinity of the two principal population centers, St. Louis in the northeast and Springfield in the southwest. Future population increases are expected to occur as a result of continued urban expansion, increased recreational use of land and water resources, and additional development of the mining industry. (Woodard-USGS)","language":"ENGLISH","doi":"10.3133/ha550","usgsCitation":"Gann, E.E., Harvey, E.J., and Miller, D.E., 1976, Water resources of south-central Missouri: U.S. Geological Survey Hydrologic Atlas 550, 19 maps on 4 sheets :col. ;127 x 108 or smaller fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha550.","productDescription":"19 maps on 4 sheets :col. ;127 x 108 or smaller fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89917,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/550/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89918,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/550/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89919,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/550/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89920,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/550/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94,36.083333333333336 ], [ -94,39 ], [ -90,39 ], [ -90,36.083333333333336 ], [ -94,36.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3dcf","contributors":{"authors":[{"text":"Gann, E. E.","contributorId":71562,"corporation":false,"usgs":true,"family":"Gann","given":"E.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278161,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harvey, Edward Joseph","contributorId":32131,"corporation":false,"usgs":true,"family":"Harvey","given":"Edward","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":278160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Don E.","contributorId":29485,"corporation":false,"usgs":true,"family":"Miller","given":"Don","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278159,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68650,"text":"ha553 - 1976 - Water resources of the Des Moines River Watershed, southwestern Minnesota","interactions":[{"subject":{"id":44064,"text":"ofr74340 - 1974 - Water resources of the Des Moines River watershed, southwestern Minnesota","indexId":"ofr74340","publicationYear":"1974","noYear":false,"title":"Water resources of the Des Moines River watershed, southwestern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":68650,"text":"ha553 - 1976 - Water resources of the Des Moines River Watershed, southwestern Minnesota","indexId":"ha553","publicationYear":"1976","noYear":false,"title":"Water resources of the Des Moines River Watershed, southwestern Minnesota"},"id":1}],"lastModifiedDate":"2021-11-12T19:55:11.918985","indexId":"ha553","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"553","title":"Water resources of the Des Moines River Watershed, southwestern Minnesota","docAbstract":"<p>The Des Moines River drains about 1,350 square miles (3,496 km<sup>2</sup>) of the north, west, and central parts of&nbsp;the watershed, and the East Fork Des Moines River along with several small creeks drain about 200 square miles (518 km<sup>2</sup>) in the east part. These tributaries join the Des Moines river in Iowa.</p>\n<p>The watershed is on the Coteau des Prairies, the most prominent upland in southern Minnesota. the Coteau rises to altitudes of more than 1,900 feet (579 m) within the watershed. The west boundary is along the crest of the Coteau and was formed by a terminal moraine during late Wisconsin Glaciation. This moraine forms part of the divide between the Mississippi and Missouri Rivers. The north and east boundaries are also formed by morainic highs which represent recessions of the Des Moines lobe during late Wisconsin Glaciation. Surficial materials consist mostly of clayey drift with a few surficial outwash (sand and gravel) areas near the streams.</p>\n<p>Topographic quadrangle maps published by the U.S. Geological Survey are available for the entire watershed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha553","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources Division of Waters, Soils, and Minerals","usgsCitation":"Anderson, H., Broussard, W., Farrell, D., and Hult, M.F., 1976, Water resources of the Des Moines River Watershed, southwestern Minnesota: U.S. Geological Survey Hydrologic Atlas 553, 3 Plates: 45.00 x 40.00 inches or smaller, https://doi.org/10.3133/ha553.","productDescription":"3 Plates: 45.00 x 40.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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H.W.","contributorId":78016,"corporation":false,"usgs":true,"family":"Anderson","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":278637,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broussard, W.L.","contributorId":35334,"corporation":false,"usgs":true,"family":"Broussard","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":626460,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Farrell, D.F.","contributorId":91163,"corporation":false,"usgs":true,"family":"Farrell","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":626461,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hult, M. F.","contributorId":29817,"corporation":false,"usgs":true,"family":"Hult","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":626462,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8825,"text":"ofr76561 - 1976 - Interpretation and description of seismic data from Lower Cook Inlet, Alaska","interactions":[],"lastModifiedDate":"2025-01-31T22:32:07.906657","indexId":"ofr76561","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-561","title":"Interpretation and description of seismic data from Lower Cook Inlet, Alaska","docAbstract":"<p>A coarse grid of 480 kilometres of seismic lines was collected in lower Cook Inlet, Alaska between Homer on the north and Cape Douglas on the south. Paper and mylar copies of the seismic sections and shot point maps are available to the public from NOAA in Boulder, Colorado.</p><p>The seismic data shows two strong reflections that have been interpreted as returns from erosional surfaces and a third reflection that represents the acoustic basement. From indications in the seismic data, shallow reflectors onlap to the northwest; deep reflectors onlap to the southeast. A major structural feature in lower Cook Inlet is an east-trending transbasin arch here informally named the Augustine-Seldovia arch. Anticlines smaller than the arch trend approximately northeast and may offer good structural traps for petroleum where they intersect the arch.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76561","usgsCitation":"Fisher, M.A., 1976, Interpretation and description of seismic data from Lower Cook Inlet, Alaska: U.S. Geological Survey Open-File Report 76-561, 191 p., https://doi.org/10.3133/ofr76561.","productDescription":"191 p.","costCenters":[],"links":[{"id":141711,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0561/report-thumb.jpg"},{"id":481580,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0561/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Lower Cook 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,{"id":27754,"text":"wri7640 - 1976 - Water-resources data for deep aquifers of eastern Montana","interactions":[],"lastModifiedDate":"2019-07-17T13:47:34","indexId":"wri7640","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-40","title":"Water-resources data for deep aquifers of eastern Montana","docAbstract":"Water from aquifers of Mesozoic and Paleozoic age in eastern Montana is little used. This report presents maps and tables to assist in the evaluation of the water in terms of possible utility. In the southern third of eastern Montana water from the Madison Group or from the Tensleep Sandstone contains less than 2,000 milligrams per liter dissolved solids and is available in amounts of as much as 3,700 gallons per minute (230 liters per second) from individual wells. Elsewhere, dissolved-solids concentrations of water from Mesozoic and Paleozoic aquifers commonly exceed 1,000 milligrams per liter, well yields range from 5 to about 1,500 gallons per minute (0.3 to 95 liters per second), and well depths generally are greater than 1,500 feet (460 meters). (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7640","usgsCitation":"Hopkins, W., 1976, Water-resources data for deep aquifers of eastern Montana: U.S. Geological Survey Water-Resources Investigations Report 76-40, iv, 37 p. , https://doi.org/10.3133/wri7640.","productDescription":"iv, 37 p. ","costCenters":[],"links":[{"id":157957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0040/report-thumb.jpg"},{"id":365594,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0040/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.12695312499999,\n              44.99588261816546\n            ],\n            [\n              -104.08447265624999,\n              44.99588261816546\n            ],\n            [\n              -104.08447265624999,\n              48.99463598353405\n            ],\n            [\n              -110.12695312499999,\n              48.99463598353405\n            ],\n            [\n              -110.12695312499999,\n              44.99588261816546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ead","contributors":{"authors":[{"text":"Hopkins, W.B.","contributorId":10072,"corporation":false,"usgs":true,"family":"Hopkins","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":198644,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27696,"text":"wri7554 - 1976 - Measurement and prediction of sediment yields in Wisconsin streams","interactions":[],"lastModifiedDate":"2015-10-21T12:12:03","indexId":"wri7554","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-54","title":"Measurement and prediction of sediment yields in Wisconsin streams","docAbstract":"<p>Sediment data of some form have been collected by the U.S. Geological Survey at 118 stream-gaging sites throughout Wisconsin, beginning in 1935. The average concentration of suspended sediment for Wisconsin streams is low in comparison with that of many streams in the United States&mdash;110 milligrams per litre for Wisconsin, as compared with 600 milligrams per litre for 50 percent of the United States (Rainwater, 1962). Enough data have been collected at 84 of the 118 sites to calculate an average annual suspended-sediment yield at those sites.</p>\n<p>Measured average annual yields range from about 680 tons per square mile (238 tonnes per square kilometre) in the \"Driftless Area\" to 3.1 tons per square mile (1.1 tonnes per square kilometre) in the Northern Highland province. The average suspended-sediment yield for Wisconsin is about 80 tons per square mile per year (28 tonnes per square kilometre per year). Only three areas in the State may be considered to have a sediment problem. They are sections of the \"Driftless Area\" of southwestern Wisconsin, the Lake Superior red-clay area, and areas of expanding urbanization in southeastern Wisconsin.</p>\n<p>Sediment-yield prediction equations have been developed for the Northern Highland province, the Central Plain province, the Eastern Ridges and Lowlands province, and the \"Driftless Area\" (Martin, 1932 and Thwaites, 1956). These four equations make it possible to predict average annual suspendedsediment yields at any point on about 95 percent of the streams in the State. The prediction technique involves regression equations that relate average annual suspended-sediment yields to factors, such as topography, soils, land use and cover, stream hydraulics, and climatic conditions. The standard error of estimate for these equations, which only represents the accuracy of an estimated sediment yield at an ungaged site, ranges from 28 to 38 percent.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7554","collaboration":"Prepared n cooperation wit the City of Madison, City of Middleton, Douglas County, University of Wisconsin-Extension, Geological and Natural History Survey, U.S. Army Corps of Engineers, Wisconsin Department of Natural Resources","usgsCitation":"Hindall, S.M., 1976, Measurement and prediction of sediment yields in Wisconsin streams: U.S. Geological Survey Water-Resources Investigations Report 75-54, iv, 27 p., https://doi.org/10.3133/wri7554.","productDescription":"iv, 27 p.","numberOfPages":"36","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science 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,{"id":60753,"text":"mf785 - 1976 - Free-air gravity anomaly map of the eastern Chukchi and southern Beaufort seas","interactions":[],"lastModifiedDate":"2023-05-16T15:29:38.690128","indexId":"mf785","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"785","title":"Free-air gravity anomaly map of the eastern Chukchi and southern Beaufort seas","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf785","usgsCitation":"Ruppel, B.D., and McHendrie, A.G., 1976, Free-air gravity anomaly map of the eastern Chukchi and southern Beaufort seas: U.S. Geological Survey Miscellaneous Field Studies Map 785, 1 Plate: 33.90 x 21.57 inches, https://doi.org/10.3133/mf785.","productDescription":"1 Plate: 33.90 x 21.57 inches","costCenters":[],"links":[{"id":417053,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0785/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182313,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0785/report-thumb.jpg"},{"id":417095,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3956.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Chukchi Sea, Beaufort Sea","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -175,66 ], [ -175,72 ], [ -135,72 ], [ -135,66 ], [ -175,66 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8688","contributors":{"authors":[{"text":"Ruppel, Byron D.","contributorId":64254,"corporation":false,"usgs":true,"family":"Ruppel","given":"Byron","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":264345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McHendrie, A. Graig","contributorId":13635,"corporation":false,"usgs":true,"family":"McHendrie","given":"A.","email":"","middleInitial":"Graig","affiliations":[],"preferred":false,"id":264346,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58763,"text":"mf716 - 1976 - Preliminary residual magnetic map of the eastern Bering Shelf and parts of western Alaska","interactions":[],"lastModifiedDate":"2023-04-14T21:59:52.217426","indexId":"mf716","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"716","title":"Preliminary residual magnetic map of the eastern Bering Shelf and parts of western Alaska","docAbstract":"<p>Residual magnetic anomalies for the offshore data were calculated by subtracting the Earth's main dipole field, adjusted for secular variations (based on the International Geomagnetic Reference Field (IGRF), epoch 1965, Fabiano and Peddie, 1969), from the observed values of the surveys listed below. The effects of diurnal variations and magnetic storms have been ignored. Individual marine magnetic profiles have been upward continued to an elevation of 1 km (Robinson, 1970; Henderson, 1970) on the assumption that the magnetic sources are two-dimensional in a direction normal to the ship's track. The upward continued profiles were computed by convolving each profile with an optimum (7, 15 or 30 points) upward continuation operator. Additional errors of unknown magnitude result from the use of two-dimensional analytic techniques in a three-dimensional field. However, on the average, values at crossings differ by only 10 percent.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf716","usgsCitation":"Bailey, K.A., Cooper, A.K., Marlow, M.S., and Scholl, D.W., 1976, Preliminary residual magnetic map of the eastern Bering Shelf and parts of western Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 716, 1 Plate: 42.71 x 33.03 inches, https://doi.org/10.3133/mf716.","productDescription":"1 Plate: 42.71 x 33.03 inches","costCenters":[],"links":[{"id":415812,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0716/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184033,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0716/report-thumb.jpg"}],"scale":"2500000","country":"United States","state":"Alaska","otherGeospatial":"eastern Bering Shelf, western Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180,52 ], [ -180,64 ], [ -156,64 ], [ -156,52 ], [ -180,52 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b405","contributors":{"authors":[{"text":"Bailey, Kimberly A.","contributorId":48626,"corporation":false,"usgs":true,"family":"Bailey","given":"Kimberly","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":260697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":260698,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":260696,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":260699,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":42782,"text":"ofr76839 - 1976 - Preliminary geologic maps showing Quaternary deposits of the Chowchilla area (Santa Rita Bridge, Bliss Ranch, Chowchilla, Berenda, and Kismet 7 1/2-minute quadrangles), eastern San Joaquin Valley, Madera and Merced Counties, California","interactions":[],"lastModifiedDate":"2021-10-15T19:37:48.543731","indexId":"ofr76839","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-839","title":"Preliminary geologic maps showing Quaternary deposits of the Chowchilla area (Santa Rita Bridge, Bliss Ranch, Chowchilla, Berenda, and Kismet 7 1/2-minute quadrangles), eastern San Joaquin Valley, Madera and Merced Counties, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76839","usgsCitation":"Marchand, D.E., 1976, Preliminary geologic maps showing Quaternary deposits of the Chowchilla area (Santa Rita Bridge, Bliss Ranch, Chowchilla, Berenda, and Kismet 7 1/2-minute quadrangles), eastern San Joaquin Valley, Madera and Merced Counties, California: U.S. Geological Survey Open-File Report 76-839, Report: 12 p.; 5 Plates: 21.11 × 27.10 inches or smaller, https://doi.org/10.3133/ofr76839.","productDescription":"Report: 12 p.; 5 Plates: 21.11 × 27.10 inches or smaller","costCenters":[],"links":[{"id":390576,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15443.htm"},{"id":80596,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0839/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80595,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0839/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80594,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0839/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80593,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0839/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80592,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0839/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80591,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0839/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135612,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0839/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"California","county":"Madera County, Merced County","otherGeospatial":"Chowchilla area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.625,\n              37\n            ],\n            [\n              -120,\n              37\n            ],\n            [\n              -120,\n              37.125\n            ],\n            [\n              -120.625,\n              37.125\n            ],\n            [\n              -120.625,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673f50","contributors":{"authors":[{"text":"Marchand, Denis E.","contributorId":98280,"corporation":false,"usgs":true,"family":"Marchand","given":"Denis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":227110,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11776,"text":"ofr76537 - 1976 - Geology of the Deep Creek area, Washington, and its regional significance","interactions":[],"lastModifiedDate":"2024-11-26T21:06:51.931994","indexId":"ofr76537","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-537","title":"Geology of the Deep Creek area, Washington, and its regional significance","docAbstract":"This report, although primarily concerned with the stratigraphy and structure of a lead-zinc mining district in northern Stevens County, Washington, discusses and integrates the geology of the region about the Deep Creek area. Although the study centers in an area of about 200 square miles immediately south of the International Boundary, the regional background comes from: (1)the previously undescribed Northport quadrangle to the west, (2) published reports and reconnaissance of the Metaline quadrangle to the east, and (3) from published reports and maps of a 16 mile wide area that lies to the north adjacent to these three quadrangles in British Columbia. The report is divided into three parts: (1) descriptions of rocks and structures of the Deep Creek area, (2) descriptions of the regional setting of the Deep Creek area, and (3) an analysis and interpretation of the depositional and tectonic events that produced the geologic features exposed today. \r\n\r\nIn the Deep Creek area surficial deposits of sand and gravel of glacial origin cover much of the consolidated rocks, which range in age from greenschist of the late Precambrlan to albite granite of the Eocene. Three broad divisions of depositional history are represented: (1) Precambrian, (2) lower Paleozoic and (3) upper Paleozoic; the record of the Mesozoic and Eocene is fragmentary. The lower Paleozoic division is the only fossil-controlled sequence; the age of the other two divisions were established by less direct methods. Both Precambrian and upper Paleozoic sequences are dominated by fine-grained detrital sediments, the Precambrian tending towards the alumina-rich and the upper Paleozoic tending towards the black shale facies with high silica. Neither sequence has more than trivial amounts of coarse clastics. Both include limestones, but in minor abundance. \r\n\r\nThe lower Paleozoic sequence, on the other hand, represents a progressive change in deposition. The sequence began during the very late Precambrian with the deposition of clean quartz sand. This was followed by the accumulation of a comparatively thin limestone unit succeeded by a thick shale. The shale grades into a thick carbonate unit which in turn is overlain by black graptolitic slates (Ordovician). This general order of deposition holds for the Cambro-Ordovician throughout the area.\r\n\r\nPrecambrian rocks indigenous to the Deep Creek area, have undergone at least six tectonic events of greatly different intensities. The first three of these events are epeirogentic, the fourth involves intense folding, the fifth, crossfolding, and the sixth, block faulting without folding. These events are dated with varying degrees of precision. The two epeirogentic events of the Precambrian, one gentle folding at the beginning of Windermere time and the other high angle faulting and volcanism in mid-Windermere time, did little to deform or metamorphose the rocks. The third event consists of uplift of northern Idaho and adjacent Montana and westward decollement thrusting of essentially unfolded lower Paleozoic rocks. The decollement faulting is inferred to explain anomalous rock distribution and cannot be accurately dated. It occurred sometime after the Devonian and before the Jurassic. A late Paleozoic age is favored.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76537","usgsCitation":"Yates, R.G., 1976, Geology of the Deep Creek area, Washington, and its regional significance: U.S. Geological Survey Open-File Report 76-537, Report: xi, 435 p.; 11 Plates: 36.21 x 45.51 inches or smaller, https://doi.org/10.3133/ofr76537.","productDescription":"Report: xi, 435 p.; 11 Plates: 36.21 x 45.51 inches or smaller","costCenters":[],"links":[{"id":39663,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0537/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39662,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39661,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39660,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39659,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39658,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39657,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39656,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39655,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39654,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39653,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39652,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0537/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144980,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0537/report-thumb.jpg"},{"id":108657,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15370.htm","text":"Deep Creek Area, Stevens and Pend Oreille Counties, Washington","linkFileType":{"id":5,"text":"html"},"description":"15370"},{"id":108656,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15368.htm","text":"northeastern Washington and adjacent Idaho and British Columbia","linkFileType":{"id":5,"text":"html"},"description":"15368"}],"country":"Canada, United States","state":"British Columbia, Idaho, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118,\n              49.25\n            ],\n            [\n              -118,\n              48.5\n            ],\n            [\n              -117,\n              48.5\n            ],\n            [\n              -117,\n              49.25\n            ],\n            [\n              -118,\n              49.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680561","contributors":{"authors":[{"text":"Yates, Robert Giertz","contributorId":69524,"corporation":false,"usgs":true,"family":"Yates","given":"Robert","email":"","middleInitial":"Giertz","affiliations":[],"preferred":false,"id":163715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38696,"text":"pp813H - 1976 - Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region","interactions":[{"subject":{"id":7852,"text":"ofr75559 - 1975 - Summary appraisals of the nation's groundwater resources: Arkansas-White-Red region","indexId":"ofr75559","publicationYear":"1975","noYear":false,"title":"Summary appraisals of the nation's groundwater resources: Arkansas-White-Red region"},"predicate":"SUPERSEDED_BY","object":{"id":38696,"text":"pp813H - 1976 - Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region","indexId":"pp813H","publicationYear":"1976","noYear":false,"chapter":"H","title":"Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region"},"id":1}],"lastModifiedDate":"2021-12-14T21:16:32.492485","indexId":"pp813H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"H","title":"Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region","docAbstract":"<p>The Arkansas-White-Red Region, an area of265,000 square miles (6.86x10<sup>11&nbsp;</sup>square metres), is characterized by diversity in geography, climate, and geology and, in turn, by diversity in water resources and water problems. The western semiarid part of the region is water deficient, that is, potential evapotranspiration exceeds precipitation. The eastern, humid part has a surplus. Water use in the region in 1970 averaged 10 billion gallons per day (438 cubic metres per second), of which more than 65 percent was ground water. The largest use of ground water was for irrigation of crops, mostly in the water-deficient areas of Texas, Oklahoma, Kansas, and Colorado. Because of its ready availability and widespread occurrence, ground water is used throughout the region to supply municipal and rural water needs. The most productive aquifers, capable of yielding more than 50 gallons per minute (0.0032 cubic metres per second) to individual wells, are alluvium, carbonate. rocks, gypsum, and sandstone. Fresh water in storage in aquifers in the region is estimated to be 2 billion acre-feet (2.5x10<sup>12</sup> cubic metres). In addition, a large, unmeasured volume of saline water (containing more than 1,000 milligrams per litre of dissolved solids) underlies the fresh water at depths generally less than 500 feet (150 metres).</p>\n<p>The flow of water in each aquifer depends upon the physical and hydrologic characteristics of the aquifer, the climate, and the relation to, and the character of, adjacent rocks and streams. These factors also determine the effect of water-supply development or other man-induced stresses on the flow and the quality of water in the aquifers. Analog and digital models of aquifers can be used to evaluate stresses on aquifers and thereby provide water managers and planners with efficient tools for planning the development and continued use of aquifers.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813H","usgsCitation":"Bedinger, M.S., and Sniegocki, R., 1976, Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region: U.S. Geological Survey Professional Paper 813, vi, 31 p., https://doi.org/10.3133/pp813H.","productDescription":"vi, 31 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":122583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813h/report-thumb.jpg"},{"id":65550,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392887,"rank":3,"type":{"id":36,"text":"NGMDB 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S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":220303,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sniegocki, R. T.","contributorId":38546,"corporation":false,"usgs":true,"family":"Sniegocki","given":"R. T.","affiliations":[],"preferred":false,"id":220302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9395,"text":"ofr76844 - 1976 - Preliminary summary of the 1976 Atlantic Margin Coring Project of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2017-11-05T09:51:59","indexId":"ofr76844","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-844","title":"Preliminary summary of the 1976 Atlantic Margin Coring Project of the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey Atlantic Margin Coring Project, 1976, a 60-day expedition to obtain core samples by drilling beneath the floor of the Continental Shelf and Slope of the eastern United States, was carried out in July, August, and September 1976 aboard D/V GLOMAR CONCEPTION. The coring penetrated as much as 310 meters below the sea floor at 19 sites along the continental margin from Georgia to Georges Bank off New England in water depths ranging from 20 to 300 meters; 1,020 meters of material were recovered in 380 cores, ranging in age from Late Cretaceous to Holocene. One of the major findings was the discovery of relatively fresh water (salinities less than 3 parts per thousand) extending beneath the Continental Shelf as much as 60 nautical miles seaward from the New Jersey coast. Water of about 1 part per thousand salinity was found beneath the shelf more than 7 nautical miles off Ocean City, Maryland and Barnegat Inlet, New Jersey. Analyses for light hydrocarbons in the cores show the highest concentrations (as much as 412,000 ppm) at sites in water depth greater than 200 meters (the shelf-slope break), principally in Pleistocene sediments, although methane concentrations greater than 400,000 ppm also were found in Miocene sediments at one site near the shelf edge. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76844","usgsCitation":"Hathaway, J.C., Schlee, J., Poag, C.W., Valentine, P.C., Weed, E.G., Bothner, M., Kohout, F.A., Manheim, F., Schloam, R., Miller, R., and Schultz, D., 1976, Preliminary summary of the 1976 Atlantic Margin Coring Project of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 76-844, 217 p., https://doi.org/10.3133/ofr76844.","productDescription":"217 p.","costCenters":[],"links":[{"id":142922,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0844/report-thumb.jpg"},{"id":37111,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0844/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a12f","contributors":{"authors":[{"text":"Hathaway, John Cummins","contributorId":95477,"corporation":false,"usgs":true,"family":"Hathaway","given":"John","email":"","middleInitial":"Cummins","affiliations":[],"preferred":false,"id":159611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schlee, J.J.","contributorId":23542,"corporation":false,"usgs":true,"family":"Schlee","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":159604,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poag, C. W.","contributorId":16402,"corporation":false,"usgs":true,"family":"Poag","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159603,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Valentine, P. C.","contributorId":46505,"corporation":false,"usgs":true,"family":"Valentine","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":159605,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Weed, Elaine G. A.","contributorId":91496,"corporation":false,"usgs":true,"family":"Weed","given":"Elaine","email":"","middleInitial":"G. A.","affiliations":[],"preferred":false,"id":159610,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bothner, Michael H. mbothner@usgs.gov","contributorId":139855,"corporation":false,"usgs":true,"family":"Bothner","given":"Michael H.","email":"mbothner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":159607,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kohout, F. A.","contributorId":11593,"corporation":false,"usgs":true,"family":"Kohout","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":159602,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":159606,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Schloam, R.","contributorId":71550,"corporation":false,"usgs":true,"family":"Schloam","given":"R.","email":"","affiliations":[],"preferred":false,"id":159608,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Miller, R.E.","contributorId":86754,"corporation":false,"usgs":true,"family":"Miller","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":159609,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Schultz, D.M.","contributorId":98310,"corporation":false,"usgs":true,"family":"Schultz","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":159612,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":9216,"text":"ofr76582 - 1976 - Generalized descriptions of uranium-bearing veins, pegmatites, and disseminations in non-sedimentary rocks, eastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr76582","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-582","title":"Generalized descriptions of uranium-bearing veins, pegmatites, and disseminations in non-sedimentary rocks, eastern United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76582","usgsCitation":"Grauch, R.I., and Zarinski, K., 1976, Generalized descriptions of uranium-bearing veins, pegmatites, and disseminations in non-sedimentary rocks, eastern United States: U.S. Geological Survey Open-File Report 76-582, [2], 114 leaves :maps ;28 cm., https://doi.org/10.3133/ofr76582.","productDescription":"[2], 114 leaves :maps ;28 cm.","costCenters":[],"links":[{"id":142884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0582/report-thumb.jpg"},{"id":36827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0582/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6afc6e","contributors":{"authors":[{"text":"Grauch, Richard I. 0000-0002-1763-0813 rgrauch@usgs.gov","orcid":"https://orcid.org/0000-0002-1763-0813","contributorId":1193,"corporation":false,"usgs":true,"family":"Grauch","given":"Richard","email":"rgrauch@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":159301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zarinski, Katrin","contributorId":101263,"corporation":false,"usgs":true,"family":"Zarinski","given":"Katrin","email":"","affiliations":[],"preferred":false,"id":159302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42665,"text":"ofr76805 - 1976 - Regional flood limits of lower Yahara River, Lake Waubesa and south, in Dane County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-08T14:47:54","indexId":"ofr76805","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-805","title":"Regional flood limits of lower Yahara River, Lake Waubesa and south, in Dane County, Wisconsin","docAbstract":"<p>The purpose of this report is to provide information on the extent , depth, and frequency of flooding of the lower Yahara River in Dane County, Wis.</p>\n<p>The report contains discharge-frequency data for flood peaks, flood&ndash;frequency profiles, and the regional flood&ndash; (100-year flood) inundation limits for the lower Yahara River. The study reach is in southern Dane County extending from part of the shoreline of Lake Waubesa downstream through Lake Kegonsa to the Dane-Rock County line. Specifically the parts of the shoreline of Lake Waubesa included are those in and south of section 8, T. 6 N., R. 10 E. on the west shore and the south half of section 3, , T. 7 N., R. 10 E. on the east shore. (See figure 2.) The reach is 21 river miles (31 km) long.</p>\n<p>The Wisconsin Legislature has enacted flood&ndash;plain&ndash;Zoning legislation (1965) to encourage economic use of flood plains and to minimize flood losses. This act gave counties, cities, and villages the responsibility of enacting, administering, and enforcing reasonable and effective flood-plain regulations.</p>\n<p>This report is a sequel to earlier reports by Lawrence and Holmstrom (1971) and Holmstrom and Lawrence (1971). The earlier reports provided much of the same information, but the scale of the maps defining limits of flooding was much smaller. This report , using Orthophotographs at a scale of 1 in - 100 ft., provides greater detail.</p>\n<p>The report is based on conditions existing in 1971. All elevations are referenced to mean sea level, datum of 1929.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76805","collaboration":"Prepared in cooperation with Dane County Regional Planning Commission","usgsCitation":"Lawrence, C.L., 1976, Regional flood limits of lower Yahara River, Lake Waubesa and south, in Dane County, Wisconsin: U.S. Geological Survey Open-File Report 76-805, 20 Sheets: 36 x 24 inches, https://doi.org/10.3133/ofr76805.","productDescription":"20 Sheets: 36 x 24 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":176612,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80441,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80442,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80443,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80444,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80445,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80446,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80447,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80448,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80449,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80450,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80451,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80452,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80453,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80454,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80455,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80456,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80457,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-21.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80440,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80437,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80438,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80439,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0805/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Dane County","otherGeospatial":"Lake Waubesa, Yahara River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.62371826171875,\n              42.827638636242284\n            ],\n            [\n              -89.62371826171875,\n              43.21718664827096\n            ],\n            [\n              -89.07714843749999,\n              43.21718664827096\n            ],\n            [\n              -89.07714843749999,\n              42.827638636242284\n            ],\n            [\n              -89.62371826171875,\n              42.827638636242284\n            ]\n          ]\n        ]\n      }\n    }\n  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,{"id":30550,"text":"wri7660 - 1976 - Ground-water resources of Wilson County, North Carolina","interactions":[],"lastModifiedDate":"2019-03-08T12:00:33","indexId":"wri7660","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-60","title":"Ground-water resources of Wilson County, North Carolina","docAbstract":"<p>The most important sources of ground water for Wilson County, North Carolina are (1) the sand beds of the Cretaceous aquifer system in the Coastal Plain section in the eastern part of the county and (2) the bedrock aquifer system in the Piedmont section in the western part of the county.</p><p>The Cretaceous aquifer is recharged from leakage through overlying beds composed primarily of clay. This leakage rate is estimated to average about 67,000 gallons per day per square mile (100 cubic metres per day per square kilometre). Present withdrawals from the Cretaceous aquifer in the county average about 740 gallons per day per square mile (1.1 cubic metres per day per square kilometre), or about 1 percent of the amount of water available to the aquifer. Most of the withdrawals from the Cretaceous aquifer are in the Saratoga-Stantonsburg area in eastern Wilson County around which a widespread decline in water level has occurred in the aquifer. Since 1942, the rate of decline has averaged nearly 1.5 feet (0.45 metre) per year in the center of the pumping area.</p><p>Individual wells can yield as much as 500 gallons per minute (32 litres per second) in the easternmost part of the county where the aquifer is thickest, but wells pumped continually at this rate would increase the rate of water-level decline throughout the aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7660","usgsCitation":"Winner, M.D., 1976, Ground-water resources of Wilson County, North Carolina: U.S. Geological Survey Water-Resources Investigations Report 76-60, vii, 85 p., https://doi.org/10.3133/wri7660.","productDescription":"vii, 85 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":160593,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0060/report-thumb.jpg"},{"id":361885,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","county":"Wilson County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-77.8278,35.8684],[-77.8206,35.8633],[-77.797,35.8551],[-77.7484,35.827],[-77.752,35.8189],[-77.7511,35.8121],[-77.7194,35.7338],[-77.6771,35.6895],[-77.668,35.6729],[-77.7009,35.6523],[-77.7535,35.616],[-77.8238,35.5729],[-77.8234,35.5856],[-77.9993,35.5859],[-78.0578,35.5978],[-78.0644,35.5857],[-78.1284,35.6035],[-78.1641,35.6953],[-78.1632,35.7107],[-78.1693,35.7149],[-78.1738,35.7163],[-78.1771,35.72],[-78.1822,35.7214],[-78.1855,35.7247],[-78.1871,35.7292],[-78.1922,35.7302],[-78.1887,35.7347],[-78.1812,35.7387],[-78.1482,35.7454],[-78.0015,35.8066],[-77.9,35.8429],[-77.8729,35.8601],[-77.8446,35.8374],[-77.8368,35.8518],[-77.8278,35.8684]]]},\"properties\":{\"name\":\"Wilson\",\"state\":\"NC\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d4ec","contributors":{"authors":[{"text":"Winner, M. D. Jr.","contributorId":51766,"corporation":false,"usgs":true,"family":"Winner","given":"M.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":203440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26987,"text":"wri7653 - 1976 - Waterlogging in an alluvial aquifer near Lake Minnequa, Pueblo, Colorado","interactions":[],"lastModifiedDate":"2022-09-06T21:50:04.156263","indexId":"wri7653","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-53","title":"Waterlogging in an alluvial aquifer near Lake Minnequa, Pueblo, Colorado","docAbstract":"The Lake Minnequa area, located immediately south of the Arkansas River near Pueblo, Colo., is mantled with as much as 46 feet (14 meters) of alluvium covering bedrock of Pierre Shale and Niobrara Formation. Surface water enters the area by the Minnequa Canal and the St. Charles Flood Ditch. The water is stored in Lake Minnequa and other reservoirs. Seepage from St. Charles Reservoirs No. 2 and No. 3 is the major source of water to the alluvial aquifer. The depth of the water table ranges from 0 to 40 feet (0 to 12.2 meters). An 0.5-square-mile (1.3-square-kilometer) area immediately south of Lake Minnequa has a water table less than 6 feet (1.8 meters) below land surface. Lake Minnequa is the principal cause of the shallow water table and resulting waterlogged soil. The bedrock hill east of Lake Minnequa and ground-water flow also contribute to the problem. To eliminate the waterlogging problem, the water table would have to be at least 6 feet (1.8 meters) below land surface. Possible alternatives for eliminating the problem include lowering the water level in Lake Minnequa, placing a network of dewatering wells, or constructing a drainage system in the waterlogged area. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7653","usgsCitation":"Emmons, P.J., 1976, Waterlogging in an alluvial aquifer near Lake Minnequa, Pueblo, Colorado: U.S. Geological Survey Water-Resources Investigations Report 76-53, iv, 34 p., https://doi.org/10.3133/wri7653.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":55874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0053/report-thumb.jpg"},{"id":406280,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35069.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Pueblo","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.72442626953124,\n              38.13023573104302\n            ],\n            [\n              -104.59945678710936,\n              38.13023573104302\n            ],\n            [\n              -104.59945678710936,\n              38.28670289852796\n            ],\n            [\n              -104.72442626953124,\n              38.28670289852796\n            ],\n            [\n              -104.72442626953124,\n              38.13023573104302\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47d9e4b07f02db4b5cc0","contributors":{"authors":[{"text":"Emmons, Patrick J.","contributorId":48958,"corporation":false,"usgs":true,"family":"Emmons","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33386,"text":"b1385E - 1976 - Mineral resources of the Eagle Cap Wilderness and adjacent areas, Oregon","interactions":[{"subject":{"id":21344,"text":"ofr71319 - 1971 - Mineral resources of ten areas proposed as additions to the Eagle Cap Wilderness, Oregon","indexId":"ofr71319","publicationYear":"1971","noYear":false,"title":"Mineral resources of ten areas proposed as additions to the Eagle Cap Wilderness, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":33386,"text":"b1385E - 1976 - Mineral resources of the Eagle Cap Wilderness and adjacent areas, Oregon","indexId":"b1385E","publicationYear":"1976","noYear":false,"chapter":"E","title":"Mineral resources of the Eagle Cap Wilderness and adjacent areas, Oregon"},"id":1}],"lastModifiedDate":"2023-01-03T20:53:13.67728","indexId":"b1385E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1385","chapter":"E","title":"Mineral resources of the Eagle Cap Wilderness and adjacent areas, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1385E","usgsCitation":"Weis, P., Gualtieri, J.L., Cannon, W.F., Tuchek, E.T., McMahan, A.B., and Federspiel, F.E., 1976, Mineral resources of the Eagle Cap Wilderness and adjacent areas, Oregon: U.S. Geological Survey Bulletin 1385, Report: ix, 100 p.; 2 Plates: 40.30 x 43.51 inches and 38.51 x 40.94 inches, https://doi.org/10.3133/b1385E.","productDescription":"Report: ix, 100 p.; 2 Plates: 40.30 x 43.51 inches and 38.51 x 40.94 inches","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":61242,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1385e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164237,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1385e/report-thumb.jpg"},{"id":95971,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1385e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95970,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1385e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109713,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21496.htm","linkFileType":{"id":5,"text":"html"},"description":"21496"}],"country":"United States","state":"Oregon","otherGeospatial":"Eagle Cap Wilderness","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.042,\n              45.517\n            ],\n            [\n              -117.733,\n              45.517\n            ],\n            [\n              -117.733,\n              45\n            ],\n            [\n              -117.042,\n              45\n            ],\n            [\n              -117.042,\n              45.517\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db657fa5","contributors":{"authors":[{"text":"Weis, Paul L.","contributorId":102872,"corporation":false,"usgs":true,"family":"Weis","given":"Paul L.","affiliations":[],"preferred":false,"id":210796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gualtieri, J. L.","contributorId":106492,"corporation":false,"usgs":true,"family":"Gualtieri","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":210797,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cannon, William F. 0000-0002-2699-8118 wcannon@usgs.gov","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":1883,"corporation":false,"usgs":true,"family":"Cannon","given":"William","email":"wcannon@usgs.gov","middleInitial":"F.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":210793,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tuchek, Ernest T.","contributorId":62631,"corporation":false,"usgs":true,"family":"Tuchek","given":"Ernest","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":210795,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McMahan, Arel B.","contributorId":107339,"corporation":false,"usgs":true,"family":"McMahan","given":"Arel","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":210798,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Federspiel, Francis E.","contributorId":28290,"corporation":false,"usgs":true,"family":"Federspiel","given":"Francis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":210794,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":9009,"text":"ofr7622 - 1976 - Data for calibrating unsteady-flow sediment-transport models, East Fork River, Wyoming, 1975","interactions":[],"lastModifiedDate":"2017-03-23T16:27:10","indexId":"ofr7622","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-22","title":"Data for calibrating unsteady-flow sediment-transport models, East Fork River, Wyoming, 1975","docAbstract":"<p>In 1975, data to calibrate a one-dimensional unsteady-flow and sediment-transport routing model were collected on a reach of the East Fork River of western Wyoming. The reach, 3.1 miles (5 kilometers) in length, wan immediately upstream from a previously established bedload sampling station. Nineteen channel cross sections were sounded at regular intervals during the spring-runoff period. Four stage recorders provided continuous records of water-surface elevations. Samples of bed material at most of the cross sections were obtained prior to high water. Streamflow and sediment-discharge measurements were collected at four of the sections.</p><p>The physiography and hydrology of the contributing watershed, the study reach, and the equipment and techniques used in data collection are described briefly. The bulk of the report is a presentation of data for the several-week period of late May to early June 1975, for which concurrent water discharge data, bedload transport and size data, and cross-section depth measurements were collected. In addition, some data collected in 1973 and 1974 and before and after the calibration period in 1975 are included for completeness.</p><p></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr7622","usgsCitation":"Mahoney, H.A., Andrews, E.D., Emmett, W.W., Leopold, L.B., Meade, R.H., Myrick, R.M., and Nordin, C.F., 1976, Data for calibrating unsteady-flow sediment-transport models, East Fork River, Wyoming, 1975: U.S. Geological Survey Open-File Report 76-22, ix, 293 p., https://doi.org/10.3133/ofr7622.","productDescription":"ix, 293 p.","numberOfPages":"309","costCenters":[],"links":[{"id":140802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0022/report-thumb.jpg"},{"id":36646,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"East Fork River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9bb6","contributors":{"authors":[{"text":"Mahoney, Holly A.","contributorId":39781,"corporation":false,"usgs":true,"family":"Mahoney","given":"Holly","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, Edmund D. eandrews@usgs.gov","contributorId":3828,"corporation":false,"usgs":true,"family":"Andrews","given":"Edmund","email":"eandrews@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":158749,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158755,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":158752,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meade, Robert H. 0000-0002-4965-3040 rhmeade@usgs.gov","orcid":"https://orcid.org/0000-0002-4965-3040","contributorId":2744,"corporation":false,"usgs":true,"family":"Meade","given":"Robert","email":"rhmeade@usgs.gov","middleInitial":"H.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":158754,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Myrick, Robert M.","contributorId":24345,"corporation":false,"usgs":true,"family":"Myrick","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":158751,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Nordin, Carl F.","contributorId":68297,"corporation":false,"usgs":true,"family":"Nordin","given":"Carl","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":158750,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":47614,"text":"wri76104 - 1976 - Maps showing ground-water conditions in the Concho, St. Johns, and White Mountains areas, Apache and Navajo Counties, Arizona, 1975","interactions":[],"lastModifiedDate":"2018-01-24T16:21:05","indexId":"wri76104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-104","title":"Maps showing ground-water conditions in the Concho, St. Johns, and White Mountains areas, Apache and Navajo Counties, Arizona, 1975","docAbstract":"The Concho, St. Johns, and White Mountains areas cover about 2 ,300 sq mi in eastern Arizona. Ground water is present in several aquifers that are made up of one or more formations. The maps show ground-water conditions in the Coconini aquifer; in the Triassic, Cretaceous, and Tertiary rocks; and in the alluvium and basaltic rocks. Information on the maps includes depth to water, altitude of the water level, chemical quality of the water, irrigated area, and hydrographs of the water level in selected wells. Scale 1:125,000. (Woodard-USGS).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76104","collaboration":"Prepared in cooperation with the Arizona Water Commission","usgsCitation":"Harper, R., and Anderson, T.W., 1976, Maps showing ground-water conditions in the Concho, St. Johns, and White Mountains areas, Apache and Navajo Counties, Arizona, 1975: U.S. Geological Survey Water-Resources Investigations Report 76-104, 4 Plates: 32.82 x 36.90 inches or smaller, https://doi.org/10.3133/wri76104.","productDescription":"4 Plates: 32.82 x 36.90 inches or smaller","costCenters":[],"links":[{"id":350581,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0104/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350582,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0104/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350583,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0104/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350580,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0104/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":134640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0104/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Apache County, Navajo County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.25,\n              33.75\n            ],\n            [\n              -109,\n              33.75\n            ],\n            [\n              -109,\n              34.75\n            ],\n            [\n              -110.25,\n              34.75\n            ],\n            [\n              -110.25,\n              33.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60596e","contributors":{"authors":[{"text":"Harper, R.W.","contributorId":36104,"corporation":false,"usgs":true,"family":"Harper","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":235902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, T. W.","contributorId":105686,"corporation":false,"usgs":true,"family":"Anderson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":235903,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4231,"text":"cir734 - 1976 - The Alaskan Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Tanacross quadrangle, Alaska","interactions":[],"lastModifiedDate":"2021-10-28T21:16:16.877528","indexId":"cir734","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"734","title":"The Alaskan Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Tanacross quadrangle, Alaska","docAbstract":"The Tanacross quadrangle, consisting of 17,400 km 2 (6,700 mi 2) in east-central Alaska, was investigated by an interdisciplinary research team for the purpose of assessing the mineral resource potential of the quadrangle. This report provides the background information for a folio of maps on the geology, geophysics, reconnaissance geochemistry, Landsat imagery, and mineral resource evaluation of the quadrangle. Revisions to the previously published geologic map of the Tanacross quadrangle, 18 new potassium-argon ages, and a comprehensive bibliography are also included.","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/cir734","usgsCitation":"Foster, H.L., Albert, N.R., Barnes, D., Curtin, G., Griscom, A., Singer, D., and Smith, J., 1976, The Alaskan Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Tanacross quadrangle, Alaska: U.S. Geological Survey Circular 734, iv, 23 p., https://doi.org/10.3133/cir734.","productDescription":"iv, 23 p.","costCenters":[],"links":[{"id":31345,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1976/0734/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1976/0734/report-thumb.jpg"},{"id":391119,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24019.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Tanacross quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -144,\n              64.250\n            ],\n            [\n              -141,\n              64.250\n            ],\n            [\n              -141,\n              63\n            ],\n            [\n              -144,\n              63\n            ],\n            [\n              -144,\n              64.250\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68346d","contributors":{"authors":[{"text":"Foster, Helen Laura","contributorId":21936,"corporation":false,"usgs":true,"family":"Foster","given":"Helen","email":"","middleInitial":"Laura","affiliations":[],"preferred":false,"id":148490,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Albert, N. R. D.","contributorId":63789,"corporation":false,"usgs":true,"family":"Albert","given":"N.","email":"","middleInitial":"R. D.","affiliations":[],"preferred":false,"id":148494,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barnes, D.F.","contributorId":48960,"corporation":false,"usgs":true,"family":"Barnes","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":148493,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Curtin, G.C.","contributorId":89501,"corporation":false,"usgs":true,"family":"Curtin","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":148496,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":148491,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Singer, D.A.","contributorId":69128,"corporation":false,"usgs":true,"family":"Singer","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":148495,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Smith, James G.","contributorId":44534,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":148492,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":2688,"text":"wsp1798O - 1976 - Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina","interactions":[],"lastModifiedDate":"2019-12-30T10:11:16","indexId":"wsp1798O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1798","chapter":"O","title":"Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina","docAbstract":"The sediment-transport characteristics of streams were determined in a 15,500-square-kilometre (6,000-square-mile) area of the Coastal Plain and Piedmont regions of eastern North Carolina during 1969-73. The study covered all or parts of 21 counties and included data for 28 sediment-sampling stations in parts of 4 major river basins?the Roanoke, Pamlico, Neuse, and Cape Fear. Annual suspended-sediment yields ranged from 117 to 4.2 tonnes per square kilometre (333 to 12 tons per square mile). Streams in the Piedmont region have the highest yields. Suspended-sediment yield decreases in an eastward direction from the Piedmont to the Coastal Plain region.\r\n\r\nSediment characteristics are directly affected by topography, storm runoff, geology, land use, and man-made detention structures. At one sampling station in the 1973 water year 44 percent of the suspended sediment tonnage was transported during 34 days of high flow. In the Piedmont region, sediment yields vary indirectly with the percentage of forest cover in the basin, but there appears to be no definite relationship between forest cover and sediment yield in the Coastal Plain region. Large lakes act as sediment-detention reservoirs. Average annual sediment yields ranged from 34 to 117 tonnes per square kilometre (98 to 333 tons per square mile) for 3 headwater streams which flow into Hyco Lake in Person County; however, the yield for the station less than 3.2 kilometres (2 miles) downstream from Hyco Dam was about 4.2 tonnes per square kilometre (12 tons per square mile).\r\n\r\nMost suspended sediment during floods in Piedmont streams ranges in size from sand to silt, whereas the suspended material in flooding streams in the Coastal Plain is generally clay size.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1798O","usgsCitation":"Simmons, C.E., 1976, Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina: U.S. Geological Survey Water Supply Paper 1798, vi, 32 p., https://doi.org/10.3133/wsp1798O.","productDescription":"vi, 32 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":138801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1798o/report-thumb.jpg"},{"id":29045,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1798o/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.92529296875,\n              35.24561909420681\n            ],\n            [\n              -77.178955078125,\n              35.24561909420681\n            ],\n            [\n              -77.178955078125,\n              36.55377524336089\n            ],\n            [\n              -80.92529296875,\n              36.55377524336089\n            ],\n            [\n              -80.92529296875,\n              35.24561909420681\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a136","contributors":{"authors":[{"text":"Simmons, Clyde E.","contributorId":71528,"corporation":false,"usgs":true,"family":"Simmons","given":"Clyde","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8335,"text":"ofr76632 - 1976 - Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Charley River and Coleen quadrangles, Alaska","interactions":[],"lastModifiedDate":"2023-07-21T18:57:48.72795","indexId":"ofr76632","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-632","title":"Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Charley River and Coleen quadrangles, Alaska","docAbstract":"<p>These summaries of references are designed to aid in library research on metallic and nonmetallic (other than mineral fuels and construction materials) mineral occurrences in the Charley River and Coleen quadrangles in east-central Alaska. All references to reports of the Geological Survey, to most reports of the U.S. Bureau of Mines, and to most reports of the State of Alaska Division of Geological and Geophysical Surveys and its predecessor State and Territorial agencies released before January 1, 1976, are summarized. Certain, mainly statistical, reports such as the annual Minerals Yearbook of the U.S. Bureau of Mines and the biennial and annual reports of the State of Alaska Division of Geological and Geophysical Surveys and its predecessor State and Territorial agencies are not included.</p><p>This report is divided into three parts: a section made up of summaries of references arranged alphabetically first by quadrangle and second by occurrence name; a section that lists synonyms for names in the first section, claim names, and the names of operators and owners of mines and prospects; and a section that lists, by author, all references summarized in the first section.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76632","usgsCitation":"Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Charley River and Coleen quadrangles, Alaska: U.S. Geological Survey Open-File Report 76-632, 43 p., https://doi.org/10.3133/ofr76632.","productDescription":"43 p.","costCenters":[],"links":[{"id":419226,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0632/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140294,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0632/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Charley River Quadrangle, Coleen Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -147.69683958362222,\n              67.46365399665677\n            ],\n            [\n              -147.69683958362222,\n              63.14007909157186\n            ],\n            [\n              -141.00530371629782,\n              63.14007909157186\n            ],\n            [\n              -141.00530371629782,\n              67.46365399665677\n            ],\n            [\n              -147.69683958362222,\n              67.46365399665677\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699018","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":157567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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