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,{"id":66207,"text":"i668 - 1971 - Geologic map of the Marshall Quadrangle, western Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"i668","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"668","subseriesTitle":"NONE","title":"Geologic map of the Marshall Quadrangle, western Alaska","language":"ENGLISH","doi":"10.3133/i668","usgsCitation":"Hoare, J., and Condon, W.H., 1971, Geologic map of the Marshall Quadrangle, western Alaska: U.S. Geological Survey IMAP 668, 1 map., https://doi.org/10.3133/i668.","productDescription":"1 map.","costCenters":[],"links":[{"id":106904,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9445.htm","linkFileType":{"id":5,"text":"html"},"description":"9445"},{"id":188730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165,61 ], [ -165,62 ], [ -162,62 ], [ -162,61 ], [ -165,61 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c54","contributors":{"authors":[{"text":"Hoare, J. M.","contributorId":52143,"corporation":false,"usgs":true,"family":"Hoare","given":"J. M.","affiliations":[],"preferred":false,"id":274170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Condon, W. H.","contributorId":28611,"corporation":false,"usgs":true,"family":"Condon","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":274169,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66355,"text":"i676 - 1971 - Map showing distribution of ultramafic and intrusive mafic rocks from New York to Maine","interactions":[],"lastModifiedDate":"2025-08-05T16:51:12.305036","indexId":"i676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"676","title":"Map showing distribution of ultramafic and intrusive mafic rocks from New York to Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i676","usgsCitation":"Larrabee, D.M., 1971, Map showing distribution of ultramafic and intrusive mafic rocks from New York to Maine: U.S. Geological Survey IMAP 676, 2 Plates: 51.00 x 37.34 inches and 50.96 x 31.50 inches, https://doi.org/10.3133/i676.","productDescription":"2 Plates: 51.00 x 37.34 inches and 50.96 x 31.50 inches","costCenters":[],"links":[{"id":493576,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9453.htm","linkFileType":{"id":5,"text":"html"}},{"id":255824,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0676/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255823,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0676/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255826,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0676/report-thumb.jpg"},{"id":255825,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0676/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -66.9,\n              47.4\n            ],\n            [\n              -73.94286321187913,\n              47.4\n            ],\n            [\n              -73.94286321187913,\n              40.448541759993645\n            ],\n            [\n              -66.9,\n              40.448541759993645\n            ],\n            [\n              -66.9,\n              47.4\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660ffe","contributors":{"authors":[{"text":"Larrabee, D. M.","contributorId":67571,"corporation":false,"usgs":true,"family":"Larrabee","given":"D.","middleInitial":"M.","affiliations":[],"preferred":false,"id":274398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66013,"text":"i589 - 1971 - Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington","interactions":[{"subject":{"id":47150,"text":"ofr6566 - 1965 - Geologic map and sections for the Columbia Basin Irrigation Project area, Washington","indexId":"ofr6566","publicationYear":"1965","noYear":false,"title":"Geologic map and sections for the Columbia Basin Irrigation Project area, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":66013,"text":"i589 - 1971 - Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington","indexId":"i589","publicationYear":"1971","noYear":false,"title":"Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington"},"id":1}],"lastModifiedDate":"2014-05-09T07:56:46","indexId":"i589","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"589","title":"Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/i589","collaboration":"Prepared in cooperation with the Washington State Department of Water Resources","usgsCitation":"Grolier, M., and Bingham, J., 1971, Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington: U.S. Geological Survey IMAP 589, 6 Plates: 41.76 x 35.5 inches and smaller, https://doi.org/10.3133/i589.","productDescription":"6 Plates: 41.76 x 35.5 inches and smaller","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":106855,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9372.htm","linkFileType":{"id":5,"text":"html"},"description":"9372"},{"id":187199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0589/report-thumb.jpg"},{"id":287009,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0589/plate-4.pdf"},{"id":287010,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0589/plate-3.pdf"},{"id":287011,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0589/plate-2.pdf"},{"id":287012,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0589/plate-1.pdf"},{"id":281734,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0589/plate-5.pdf"},{"id":281735,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0589/plate-6.pdf"}],"scale":"62500","country":"United States","state":"Washington","county":"Adams County;Franklin County;Grant County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.0250,46.1830 ], [ -120.0250,47.5250 ], [ -118.6050,47.5250 ], [ -118.6050,46.1830 ], [ -120.0250,46.1830 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b14e4b07f02db6a4781","contributors":{"authors":[{"text":"Grolier, M. J.","contributorId":46946,"corporation":false,"usgs":true,"family":"Grolier","given":"M. J.","affiliations":[],"preferred":false,"id":273853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, J.W.","contributorId":35295,"corporation":false,"usgs":true,"family":"Bingham","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":273852,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61887,"text":"gq922 - 1971 - Geologic map of the Garfield quadrangle, Salt Lake and Tooele Counties, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq922","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"922","title":"Geologic map of the Garfield quadrangle, Salt Lake and Tooele Counties, Utah","language":"ENGLISH","doi":"10.3133/gq922","usgsCitation":"Tooker, E.W., and Roberts, R.J., 1971, Geologic map of the Garfield quadrangle, Salt Lake and Tooele Counties, Utah: U.S. Geological Survey Geologic Quadrangle 922, 1 map., https://doi.org/10.3133/gq922.","productDescription":"1 map.","costCenters":[],"links":[{"id":103636,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2222.htm","linkFileType":{"id":5,"text":"html"},"description":"2222"},{"id":248176,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0922/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":252919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0922/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,40.6175 ], [ -112.25,40.75 ], [ -112.11749999999999,40.75 ], [ -112.11749999999999,40.6175 ], [ -112.25,40.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698d5f","contributors":{"authors":[{"text":"Tooker, Edwin Wilson","contributorId":33295,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":266511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Ralph Jackson","contributorId":63010,"corporation":false,"usgs":true,"family":"Roberts","given":"Ralph","email":"","middleInitial":"Jackson","affiliations":[],"preferred":false,"id":266512,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18832,"text":"ofr7195 - 1971 - Geology of the Stroudsburg quadrangle and Adjacent areas, Pennsylvania--New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:26","indexId":"ofr7195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-95","title":"Geology of the Stroudsburg quadrangle and Adjacent areas, Pennsylvania--New Jersey","docAbstract":"The Stroudsburg area is within the Valley and Ridge and Great Valley physiographic provinces, Northampton and Monroe Counties, Pennsylvania, and Warren County, New Jersey. The northeast-trending subparallel valleys and ridges resulted from erosion of folded heterogeneous sedimentary rocks. These are Middle Ordovician to Middle Devonian in age and are more than 17,000 feet thick. Deposition of a thick flysch sequence (Martinsburg Formation of Ordovician age) accompanied onset of Taconic orogenesis. It was followed by deposition of a thick molasse sequence of Silurian and Early Devonian age (continental and marginal-marine clastics--Shawangunk Formation and Bloomsburg Red Beds--overlain by predominantly marginal-marine and subtidal limestone, dolomite, shale, and sandstone--Poxono Island Formation through Oriskany Group). Basin deepening and gradual shallowing occurred during Esopus through Mahantango deposition, heralding the Acadian clastic wedge exposed north of the Stroudsburg area. Interpretation of sedimentary structures and regional stratigraphic relations suggest that the Silurian and Devonian rocks were deposited in the following environments: A1luviated coastal plain (meandering and braided streams), tidal flats (supratidal and intertidal), barrier zone, and neritic zone (upper and lower). \r\n\r\nThe rock stratigraphic units have been grouped into four lithotectonic units, each having a different style of deformation. Folds produced in these rocks are disharmonic, and it is believed that each rock sequence is set off from units above and below by \r\ndecollements, or zones of detachment. Movement was northwest into the Appalachian basin, primarily by gravitational sliding. The contact between the Shawangunk Formation of Silurian age and Martinsburg Formation of Ordovician age, is one zone of detachment as well as an angular unconformity. \r\n\r\nDeformational effects of the Middle to Late Ordovician Taconic orogeny are elusive, but it appears that the folds and most minor structures, including the prominent regional cleavage, were produced during the late Paleozoic Appalachian orogeny and are superimposed upon larger Taconic folds and faults. \r\n\r\nField relations and microscopic study suggest that the regional cleavage in the Stroudsburg area is due to laminar flow of pelitic material along cleavage folia accompanied by mechanical reorientation of platy and elongate minerals and neocrystallization of mica, quartz, chlorite, and probably albite. Numerous lines of evidence point to the conclusion that cleavage developed after the rock was indurated and formed at, and Just below, conditions of low-grade metamorphism. Intensity of cleavage development increases to the southeast across the area. Second-generation slip cleavage, also believed to be Appalachian in age, formed by mechanical reorientation of minerals as well as by limited new mineral growth. \r\n\r\nThe topography had a profound effect on the direction of movement of the Wisconsin glacier, as well as the manner of its retreat and the deposits that were formed. Till and stratified drift of Wisconsin age and till of Illinoian(?) age are common in the area. Wisconsin deglaciation occurred by northeastward retreat and by stagnation. A conspicuous terminal moraine marks the limit of Wisconsin ice movement. Lake Sciota was dammed between the retreating ice, the moraine, and the surrounding ridges north of Godfrey Ridge. Several deltas mark ice stand positions during the retreat of the ice. Lake-bottom and kame deposits are locally common in Cherry Valley. South of Kittatinny Mountain, on the other hand, melt water was freely discharged to the south. \r\n\r\nThe wind and water gaps in the Stroudsburg area (including Delaware Water Gap and Wind Gap) are structurally controlled; specifically they are located where folds die out in short distances, where folding is locally more intense, or where resistant rocks dip steeply and have a narrow width of outcrop. 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,{"id":925,"text":"wsp1999C - 1971 - Water resources of the upper White River basin, east-central Indiana","interactions":[],"lastModifiedDate":"2022-11-07T16:50:28.66113","indexId":"wsp1999C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1999","chapter":"C","title":"Water resources of the upper White River basin, east-central Indiana","docAbstract":"<p>Ground-water discharge to the streams sustains year-round streamflow in the upper White River basin. This discharge, referred to as ground-water runoff or base runoff, is considered to be an index to the amount of g ound water available for development. A comparison of the variations of groundwater runoff and aquifer distribution in the basin shows that the areas of best development potential are areas where thick sand and gravel aquifers are adjacent to the streams. The average ground-water runoff for these areas is between 400,000 and 500,000 gallons per day per square mile.</p>\n<p>The most permeable aquifers in the basin are the sand and gravel deposits of Quaternary age. These aquifers occur mainly as relatively thick elongate bodies along bedrock valleys and as relatively thin sheetlike deposits at or near land surface. The representative hydraulic conductivity of these aquifers ranges from 1,500 to 2,500 gallons per day per square foot. The limestone and dolomite formations of the bedrock are a source of moderate quar tities of water.</p>\n<p>The long-term average streamflow in the basin is approximately 0.9 cubic feet per second per square mile. The yearly average discharge varies from about one-fourth to twice the long-term average. The 7-day 10-year low flow ranges from about 0.01 to 0.3 cubic feet per second per square mile; the main-stem flow ranges from 0.10 to 0.13 cubic feet per second per square mile.</p>\n<p>The water in the aquifers is predominately a very hard calcium bicarbonate type; it is generally high in iron and contains a moderate amount of dissolved solids. Fresh water (1,000 milligrams per liter dissolved solids or less) is present to depths of approximately 400 feet below land surface. In the tributaries and in the headwaters region of the White River, the composition of surface water is very similar to that of ground water. The quality cf the water in the White River deteriorates in the downstream direction owing to the cumulative effects of sewage effluent.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1999C","usgsCitation":"Cable, L.W., Daniel, J.F., Wolf, R.J., and Tate, C.H., 1971, Water resources of the upper White River basin, east-central Indiana: U.S. Geological Survey Water Supply Paper 1999, Report: v, 38 p.; 4 Plates: 25.00 × 20.50 inches or smaller, https://doi.org/10.3133/wsp1999C.","productDescription":"Report: v, 38 p.; 4 Plates: 25.00 × 20.50 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":25397,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409195,"rank":7,"type":{"id":36,"text":"NGMDB Index 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