{"pageNumber":"379","pageRowStart":"9450","pageSize":"25","recordCount":10956,"records":[{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","interactions":[{"subject":{"id":19438,"text":"ofr76496 - 1976 - Hydrologic evaluation of Ashley Valley, northern Uinta Basin area, Utah","indexId":"ofr76496","publicationYear":"1976","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta Basin area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","indexId":"70043723","publicationYear":"1977","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah"},"id":1},{"subject":{"id":52966,"text":"ofr5086 - 1950 - Progress report on ground-water investigation in Ashley Valley, Uintah County, Utah","indexId":"ofr5086","publicationYear":"1950","noYear":false,"title":"Progress report on ground-water investigation in Ashley Valley, Uintah County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","indexId":"70043723","publicationYear":"1977","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah"},"id":2}],"lastModifiedDate":"2017-01-05T17:07:01","indexId":"70043723","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"54","title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","docAbstract":"<p>The water resources of the northern Uinta Basin, Utah and Colorado, were studied during 1971-74. Ashley Valley was evaluated in slightly greater detail than the general area, in order to assess the general relation of ground- and surface-water supplies.</p>\n<br>\n<p>In Ashley Valley , the principal source of both irrigation supply\nand ground-water recharge is the flow from Ashley Creek canyon .\nGround-water recharge to the valley fill, however, is mainly from canal\nand field losses along the west side of the valley. The permeability of\nthe fill in most places is high, and water-level records indicate rapid\nchanges in storage in response to the annual applications of irrigation\nwater.</p>\n<br>\n<p>Prior to the distribution of water from Steinaker Reservoir, the\nshort runoff season led to a brief, intense irrigation period that was\nfollowed by a long period of post-irrigation drainage. After the\nreservoir began operation, smaller applications of water were made\nduring a longer season, and ground-water levels rose in parts of the\nvalley , mainly the lower areas. Despite local water-level rises, no\nperennially gaining reaches of the canals were observed.</p>\n<br>\n<p>The amount of ground water available from storage in Ashley\nValley is estimated to be 50,000-75,000 acre-feet (62-92 cubic\nhectometres), or enough water to supply irrigation in the valley for a\nmaximum of 2 years. The ground-water storage varies annually about 10\npercent and has not changed significantly. Ground water is discharged\nfrom Ashley Valley both by seepage back to Ashley Creek and by\nevapotranspiration .</p>\n<br>\n<p>Evapotranspiration of surface and ground water has increased by an estimate 20 percent above the 48,000 acre-feet (59 cubic hectometers) determined for pre-reservoir conditions. As a result, the water that flows from Ashley Valley has been degraded in chemical quality.</p>\n<br>\n<p>The water from Ashley Creek canyon is fresh . Mixing of snowmelt\nand base flow in Steinaker Reservoir yields a water of more uniform\nquality; but despite some concentration by evaporation from the\nreservoir, the outflow from the reservoir is fresh. Ground water in\nmost of the valley is fresh , but the water increases in dissolved-solids\nconcentration toward the south and east as a result of both\nevapotranspiration and solution of minerals from the valley fill and\nsoils .</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Hood, J.W., 1977, Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah: Technical Publication 54, Report: iv, 25 p.; 1 Plate: 25.51 x 26.76 inches.","productDescription":"Report: iv, 25 p.; 1 Plate: 25.51 x 26.76 inches","numberOfPages":"31","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267700,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70043723.jpg"},{"id":286044,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70043723/plate-1.pdf","text":"Plate 1"},{"id":331880,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-350"},{"id":286045,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043723/report.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Ashley Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,37.0 ], [ -114.0,42.0 ], [ -109.0,42.0 ], [ -109.0,37.0 ], [ -114.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad43e4b0b6328103b447","contributors":{"authors":[{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220873,"text":"5220873 - 1977 - Atlantic Flyway review: Region V","interactions":[{"subject":{"id":70184468,"text":"70184468 - 1977 - Atlantic Flyway review: Region V: Laurel, Prince Georges County, MD","indexId":"70184468","publicationYear":"1977","noYear":false,"title":"Atlantic Flyway review: Region V: Laurel, Prince Georges County, MD"},"predicate":"IS_PART_OF","object":{"id":5220873,"text":"5220873 - 1977 - Atlantic Flyway review: Region V","indexId":"5220873","publicationYear":"1977","noYear":false,"title":"Atlantic Flyway review: Region V"},"id":1}],"lastModifiedDate":"2017-03-09T16:46:15","indexId":"5220873","displayToPublicDate":"2010-06-16T12:19:25","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2881,"text":"North American Bird Bander","active":true,"publicationSubtype":{"id":10}},"title":"Atlantic Flyway review: Region V","docAbstract":"<p>Banding activities in Region V in 1975 were similar to those of 1974. The stations at Woodend and St. Michaels were discontinued, but a new station 5 miles south of St. Michaels was opened at Bellevue by Henry Armistead. For the locations of the various banding stations in Region V see the map in the 1974 report (North American Bird Bander 1:75-82).</p><p>As in the past several years, the great majority of the birds banded were caught at the three full-time stations: Adventure in the Potomac Valley near the fall line, Damsite on the east shore of Chesapeake Bay, and Kiptopeke at the mouth of Chesapeake Bay. At these three stations, 17,244 birds were banded during the 1975 fall season; this is 77% of the regional total of 22,315 birds. </p>","language":"English","publisher":"Western, Inland, and Eastern Bird Banding Associations","usgsCitation":"Robbins, C.S., 1977, Atlantic Flyway review: Region V: North American Bird Bander, v. 2, no. 2, p. 79-85.","productDescription":"7 p.","startPage":"79","endPage":"85","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18336,"rank":300,"type":{"id":15,"text":"Index Page"},"url":"https://www.westernbirdbanding.org/nabb.html","text":"Journal's Website","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b396","contributors":{"authors":[{"text":"Robbins, Chandler S. crobbins@usgs.gov","contributorId":4275,"corporation":false,"usgs":true,"family":"Robbins","given":"Chandler","email":"crobbins@usgs.gov","middleInitial":"S.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":332629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220937,"text":"5220937 - 1977 - Fall migration of woodcock at Cape May, New Jersey","interactions":[],"lastModifiedDate":"2025-02-14T20:18:48.691472","indexId":"5220937","displayToPublicDate":"2010-06-16T12:19:24","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Fall migration of woodcock at Cape May, New Jersey","docAbstract":"<p>From 1968 to 1973, 2,337 American woodcock (<i>Philohela minor</i>) were banded during late fall on the Cape May Peninsula of southern New Jersey. Direct recovery rates averaged 3.6 percent for hatching-year birds and 1.7 percent for adults. Distribution of recoveries indicated that Cape May migrants wintered on the coastal plain of Virginia and North Carolina. Indirect recoveries showed that Peninsula woodcock originated from as far north as New England and eastern Canada. The percentage of woodcock seen which were caught by night-lighting averaged 2.5 times greater from a truck than on foot. Age-sex structure of ban dings was similar each year with the overall composition as follows: immaturemales, 57 percent; immature females, 28 percent; adult males, 10 percent; and adult females, 5 percent. Compared to the continental population, there was an unusually high proportion of immature woodcock at Cape May during late fall.</p>","language":"English","doi":"10.2307/3800098","usgsCitation":"Krohn, W., Fieffenberger, J., and Ferrigno, F., 1977, Fall migration of woodcock at Cape May, New Jersey: Journal of Wildlife Management, v. 41, no. 1, p. 104-111, https://doi.org/10.2307/3800098.","productDescription":"8 p.","startPage":"104","endPage":"111","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198531,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","county":"Cape May County","city":"Cape 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,{"id":5210118,"text":"5210118 - 1977 - The status and distribution of woodcock in Oklahoma","interactions":[],"lastModifiedDate":"2013-08-27T09:59:27","indexId":"5210118","displayToPublicDate":"2009-06-09T09:23:00","publicationYear":"1977","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The status and distribution of woodcock in Oklahoma","docAbstract":"The seasonal and spatial distributions of the American woodcock (Philohela minor) in Oklahoma were determined through field surveys and the collection of all known reports of woodcock sightings. Woodcock were reported in Oklahoma in all seasons and were most Jrequently sighted from 11 October to 10 January.  The peak in fall migration occurred between 11 November and 10 December.  Woodcock were found in 5 major areas across the eastern two-thirds of the state but 57 percent of the birds reported during the study were in the eastern one-third. A total of 148 displaying males were encountered on 25 sites in 15 of 29 counties included roadside singing ground surveys in 1975 and 1976.  The peak number of displaying birds (58) was observed during the second IO-day period in February; displays occurred from January through late March.  Personal observations plus data reported via volunteer survey cards, indicated that the typical site used for diurnal cover by woodcock in Oklahoma is a brushy bottomland with moist loamy soils, vegetated by oaks (Quercus spp.), elms (Ulmus spp,), bluestem grasses (Andropogon spp.), dogwoods (Cornus spp.) and green briars (Smilax spp.).","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Sixth Woodcock Symposium, held at Fredericton, New Brunswick, October 4, 5 and 6","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"University of New Brunswick","publisherLocation":"Frederiction, New Brunswick","collaboration":"OCLC: 37723545","usgsCitation":"Barclay, J., and Smith, R., 1977, The status and distribution of woodcock in Oklahoma, <i>in</i> Proceedings of the Sixth Woodcock Symposium, held at Fredericton, New Brunswick, October 4, 5 and 6, p. 39-50.","productDescription":"12 p.","startPage":"39","endPage":"50","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db63488e","contributors":{"editors":[{"text":"Keppie, Daniel M.","contributorId":113918,"corporation":false,"usgs":true,"family":"Keppie","given":"Daniel M.","affiliations":[],"preferred":false,"id":506019,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Owen, Ray B. Jr.","contributorId":35030,"corporation":false,"usgs":true,"family":"Owen","given":"Ray","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":506018,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Barclay, J.S.","contributorId":46661,"corporation":false,"usgs":true,"family":"Barclay","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":327813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R.W.","contributorId":31787,"corporation":false,"usgs":true,"family":"Smith","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":327812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70164407,"text":"70164407 - 1977 - Occurrence of bloedite and related minerals in marine shale of Diablo and Temblor Ranges, California","interactions":[],"lastModifiedDate":"2016-02-03T12:50:19","indexId":"70164407","displayToPublicDate":"2008-12-28T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of bloedite and related minerals in marine shale of Diablo and Temblor Ranges, California","docAbstract":"<p>Bloedite, epsomite, and related minerals occur in small amounts throughout the arid eastern foothills of the Diablo and Temblor Ranges, as efflorescences on siliceous shale and as deposits around small springs and a brine pond. These minerals ultimately are products of weathering of underlying organic shale, and they are reminders that the chemistry of weathering of reduced organic shale is largely a reversal of the chemistry of its early diagenesis.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Murata, K.J., 1977, Occurrence of bloedite and related minerals in marine shale of Diablo and Temblor Ranges, California: Journal of Research of the U.S. Geological Survey, v. 5, no. 5, p. 637-642.","productDescription":"6 p.","startPage":"637","endPage":"642","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316526,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":316525,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue5/report.pdf","text":"Report","size":"17.16 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"California","otherGeospatial":"Diablo Range, Temblor Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              34.5\n            ],\n            [\n              -121,\n              37\n            ],\n            [\n              -119,\n              37\n            ],\n            [\n              -119,\n              34.5\n            ],\n            [\n              -121,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b332fae4b0cc79997f33cd","contributors":{"authors":[{"text":"Murata, K. J.","contributorId":18759,"corporation":false,"usgs":true,"family":"Murata","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":597167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009981,"text":"70009981 - 1977 - Structure and sediment distribution in the western Bering Sea","interactions":[],"lastModifiedDate":"2025-04-18T13:55:21.623452","indexId":"70009981","displayToPublicDate":"2003-04-15T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Structure and sediment distribution in the western Bering Sea","docAbstract":"<p><span>Eleven seismic reflection profiles across Shirshov Ridge and the adjacent deep-water sedimentary basins (Komandorsky and Aleutian Basins) are presented to illustrate the sediment distribution in the western Bering Sea. A prominent seismic reflecting horizon, Reflector P (Middle—Late Miocene in age), is observed throughout both the Aleutian and Komandorsky Basins at an approximate subbottom depth of 1 km. This reflector is also present, in places, on the flanks and along the crest of Shirshov Ridge. The thickness of sediments beneath Reflector P is significantly different within the two abyssal basins. In the Aleutian Basin, the total subbottom depth to acoustic basement (basalt?) is about 4 km, while in the Komandorsky Basin the depth is about 2 km.</span></p><p><span>Shirshov Ridge, a Cenozoic volcanic feature that separates the Aleutian and Komandorsky Basins, is an asymmetric bathymetric ridge characterized by thick sediments along its eastern flank and steep scarps on its western side. The southern portion of the ridge has more structural relief that includes several deep, sediment-filled basins along its summit.</span></p><p><span>Velocity data from sonobuoy measurements indicate that acoustic basement in the Komandorsky Basin has an average compressional wave velocity of 5.90 km/sec. This value is considerably larger than the velocities measured for acoustic basement in the northwestern Aleutian Basin (about 5.00 km/sec) and in the central Aleutian Basin (5.40–5.57 km/sec). In the northwestern Aleutian Basin, the low-velocity acoustic basement may be volcaniclastic sediments or other indurated sediments that are overlying true basaltic basement. A refracting horizon with similar velocities (4.6–5.0 km/sec) as acoustic basement dips steeply beneath the Siberian continental margin, reaching a maximum subbottom depth of about 8 km. The thick welt of sediment at the base of the Siberian margin may be the result of sediment loading or tectonic depression prior to Late Cenozoic time.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(77)90074-3","issn":"00253227","usgsCitation":"Rabinowitz, P.D., and Cooper, A., 1977, Structure and sediment distribution in the western Bering Sea: Marine Geology, v. 24, no. 4, p. 309-320, https://doi.org/10.1016/0025-3227(77)90074-3.","productDescription":"12 p.","startPage":"309","endPage":"320","costCenters":[],"links":[{"id":219662,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","state":"Alaska","otherGeospatial":"western Bering Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -179.9,\n              56.285168320056385\n            ],\n            [\n              -179.9,\n              51.00071364602036\n            ],\n            [\n              -174.83958193767174,\n              51.00071364602036\n            ],\n            [\n              -174.83958193767174,\n              56.285168320056385\n            ],\n            [\n              -179.9,\n              56.285168320056385\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              179.9,\n              56.28905975329704\n            ],\n            [\n              164.84405712674976,\n              56.28905975329704\n            ],\n            [\n              164.84405712674976,\n              50.95540695542479\n            ],\n            [\n              179.9,\n              50.95540695542479\n            ],\n            [\n              179.9,\n              56.28905975329704\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9c2ce4b08c986b31d2fe","contributors":{"authors":[{"text":"Rabinowitz, P. D.","contributorId":102624,"corporation":false,"usgs":true,"family":"Rabinowitz","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":357579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, A.","contributorId":47517,"corporation":false,"usgs":true,"family":"Cooper","given":"A.","affiliations":[],"preferred":false,"id":357578,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10130,"text":"ofr77169A - 1977 - Map showing metalliferous and selected nonmetalliferous mineral deposits in eastern southern Alaska","interactions":[],"lastModifiedDate":"2022-09-08T18:34:53.780367","indexId":"ofr77169A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-169","chapter":"A","title":"Map showing metalliferous and selected nonmetalliferous mineral deposits in eastern southern Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77169A","usgsCitation":"MacKevett, E., and Holloway, C.D., 1977, Map showing metalliferous and selected nonmetalliferous mineral deposits in eastern southern Alaska: U.S. Geological Survey Open-File Report 77-169, Report: 99 p.; 1 Plate: 52.00 × 38.00 inches, https://doi.org/10.3133/ofr77169A.","productDescription":"Report: 99 p.; 1 Plate: 52.00 × 38.00 inches","costCenters":[],"links":[{"id":406389,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14323.htm","linkFileType":{"id":5,"text":"html"}},{"id":143297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0169a/report-thumb.jpg"},{"id":94964,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0169a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0169a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -153.3251953125,\n              58.60833366077633\n            ],\n            [\n              -140.18554687499997,\n              58.60833366077633\n            ],\n            [\n              -140.18554687499997,\n              63.60721668033077\n            ],\n            [\n              -153.3251953125,\n              63.60721668033077\n            ],\n            [\n              -153.3251953125,\n              58.60833366077633\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ad9b","contributors":{"authors":[{"text":"MacKevett, E.M. Jr.","contributorId":58613,"corporation":false,"usgs":true,"family":"MacKevett","given":"E.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":160862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holloway, Carleen D.","contributorId":105719,"corporation":false,"usgs":true,"family":"Holloway","given":"Carleen","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160863,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42273,"text":"ofr77523 - 1977 - Bedrock map of Fairfax County, Virginia","interactions":[{"subject":{"id":42273,"text":"ofr77523 - 1977 - Bedrock map of Fairfax County, Virginia","indexId":"ofr77523","publicationYear":"1977","noYear":false,"title":"Bedrock map of Fairfax County, Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":41234,"text":"ofr79398 - 1979 - Preliminary geologic map of Fairfax County, Virginia","indexId":"ofr79398","publicationYear":"1979","noYear":false,"title":"Preliminary geologic map of Fairfax County, Virginia"},"id":1}],"supersededBy":{"id":41234,"text":"ofr79398 - 1979 - Preliminary geologic map of Fairfax County, Virginia","indexId":"ofr79398","publicationYear":"1979","noYear":false,"title":"Preliminary geologic map of Fairfax County, Virginia"},"lastModifiedDate":"2016-10-12T09:59:15","indexId":"ofr77523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-523","title":"Bedrock map of Fairfax County, Virginia","docAbstract":"<p>The generalized rock-type of lithologic map separates the firm consolidated bedrock that underlies most of Fairfax County into thirteen (13) major rock types; each type groups rock units with grossly similar physical characteristics. &nbsp;Although crystalline bedrock underlies the Coastal Plain deposits of Eastern Fairfax County, it was not subdivided on this map. &nbsp;The only available information is based on interpretations from a few widely scattered deep drill holes and aeromagnetic and gravity surveys. Three sedimentary and ten (10) crystalline rocks on the Explanation are arranged in order from softest, best bedded, most foliated and readily splittable - to hardest, most massive, and least readily splittable.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77523","usgsCitation":"Drake, A.A., and Froelich, A., 1977, Bedrock map of Fairfax County, Virginia: U.S. Geological Survey Open-File Report 77-523, 46.46 x 56.34 inches, https://doi.org/10.3133/ofr77523.","productDescription":"46.46 x 56.34 inches","costCenters":[],"links":[{"id":172743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77523.PNG"},{"id":329402,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0523/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Virginia","county":"Fairfax 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Avery A. Jr.","contributorId":81090,"corporation":false,"usgs":true,"family":"Drake","given":"Avery","suffix":"Jr.","middleInitial":"A.","affiliations":[],"preferred":false,"id":650633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Froelich, A.J.","contributorId":13593,"corporation":false,"usgs":true,"family":"Froelich","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":650634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9222,"text":"ofr77718 - 1977 - Geology of the Monterey Bay region","interactions":[],"lastModifiedDate":"2021-10-26T21:35:25.827402","indexId":"ofr77718","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-718","title":"Geology of the Monterey Bay region","docAbstract":"Geophysical data and sea floor samples collected from the continental shelf and slope between Ano Nuevo Point and Point Sur, California indicate that the Monterey Bay region has had a complex late Cenozoic tectonic history. Uplift and depression have produced a succession of regressive and transgressive sedimentary units, while contemporaneous right-slip along faults of the San Andreas system have offset major structural and lithologic elements. This deformation produced three regional and several local unconformities within upper Tertiary rocks and initiated development of a canyon system that today includes the Monterey, Ascension, Carmel, and other large submarine canyons. The Tertiary stratigraphy of the offshore Monterey Bay area is divided into two provinces by a major structural boundary, the north-trending Palo Colorado-San Gregorio fault zone. East of this zone in the offshore are four seismically distinct sequences that can be correlated with major sequences onshore. These sequences comprise (1) pre-Tertiary basement, and (2) middle Miocene, (3) upper Miocene to Pliocene, and (4) upper Pliocene to Holocene sedimentary intervals. Each of the latter three sequences is bounded by unconformities, as is its counterpart on land. Only Neogene sedimentary rocks are present offshore; Paleogene units, if originally present, have been removed completely by pre-middle Miocene erosion. \r\n\r\nAn extensive erosional surface was cut during Zemorrian time into the late Mesozoic granitic basement rocks. Incised into this surface are the ancestral Monterey Canyon and an unnamed canyon. Marine sedimentary rocks of upper Miocene and Pliocene age overlie this unconformably and fill the unnamed canyon. Similar rocks also may have once filled Monterey Canyon. Near shore these strata are covered by terrestrial alluvial and eolian deposits, deltaic deposits, marine canyon fill, landslide and slump deposits, and unconsolidated sediments that range in age from upper Pliocene to Holocene. Monterey Canyon appears to have been filled and exhumed at least twice since its inception in Oligocene time, once in late Miocene and once in Pleistocene time. Three major seismic stratigraphic units are apparent in continuous seismic reflection profiles from the offshore area west of the Palo Colorado-San Gregorio fault zone. These are (1) acoustical basement, and (2) middle Tertiary and (3) late Tertiary to Quaternary sedimentary intervals. Acoustical basement comprises Cretaceous to early Tertiary sedimentary rocks, Mesozoic or older metamorphic rocks, and Cretaceous or Jurassic rocks of the Franciscan assemblage. The middle Tertiary sequence consists of sedimentary rocks of questionable Miocene age. The late Tertiary to Quaternary sequence is composed of Pliocene sedimentary rocks and unconsolidated marine sediments, and submarine landslide and slump deposits. \r\n\r\nSeismic reflection surveys indicate two major, intersecting, northwest-trending fault zones to be present in the offshore Monterey Bay area. The Palo Colorado-San Gregorio fault zone may be more than 200 km long; it is narrow (approximately 3 km wide) and is represented in most places by one or two faults. This zone appears to connect with faults mapped on land near Ano Nuevo Point and Point Sur. The Monterey Bay fault zone, located in the area between Santa Cruz and Monterey, is a diffuse zone, approximately 10 to 15 km wide, of en echelon faults. Faults within this zone appear to connect with faults on land near Monterey, and the zone appears to be truncated by the Palo Colorado-San Gregorio fault zone west of Santa Cruz. \r\n\r\nLocations of more than 110 earthquakes (1968-1976) show that the newly mapped fault zones in Monterey Bay are seismically active. Epicenters in the bay form two clusters, one at the intersection of the Monterey Bay and Palo Colorado-San Gregorio fault zones, and the other in a linear belt that trends northwest along the Palo Colorado-San Gregorio fault zone. Faults within th","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77718","usgsCitation":"Greene, H., 1977, Geology of the Monterey Bay region: U.S. Geological Survey Open-File Report 77-718, Report: xvi, 347 p.; 9 Plates: 38.94 × 40.32 inches or smaller, https://doi.org/10.3133/ofr77718.","productDescription":"Report: xvi, 347 p.; 9 Plates: 38.94 × 40.32 inches or smaller","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":36839,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36837,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36836,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36838,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36841,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36835,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390989,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74775.htm"},{"id":36840,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36842,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36843,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0718/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0718/report-thumb.jpg"},{"id":36844,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0718/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Monterey Bay region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.17620849609374,\n              36.516258626036624\n            ],\n            [\n              -121.71340942382812,\n              36.516258626036624\n            ],\n            [\n              -121.71340942382812,\n              37.019001724461155\n            ],\n            [\n              -122.17620849609374,\n              37.019001724461155\n            ],\n            [\n              -122.17620849609374,\n              36.516258626036624\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf30","contributors":{"authors":[{"text":"Greene, H. Gary","contributorId":38958,"corporation":false,"usgs":true,"family":"Greene","given":"H. Gary","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":159309,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16185,"text":"ofr78124 - 1977 - Triaxial and consolidation testing of cores from the 1976 Atlantic Margin Coring Project of the United States Geological Survey","interactions":[],"lastModifiedDate":"2024-05-08T18:23:11.015031","indexId":"ofr78124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"78-124","title":"Triaxial and consolidation testing of cores from the 1976 Atlantic Margin Coring Project of the United States Geological Survey","docAbstract":"<p>This report contains the results of triaxial and consolidation-compression testing on selected cores taken by the Atlantic Margin Coring Project, a 60-day expedition to obtain core samples by drilling beneath the Continental Shelf and Slope of the eastern United States. The coring took place in July, August and September, 1976 aboard the D/V GLOMAR CONCEPTION, and penetrated as much as 310 meters below the sea floor at 19 sites (Figure 1) along the continental margin from Georgia to Georges Bank off New England in water depth ranging from 20 to 300 meters.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78124","usgsCitation":"Swanson, P.G., and Brown, R.E., 1977, Triaxial and consolidation testing of cores from the 1976 Atlantic Margin Coring Project of the United States Geological Survey: U.S. Geological Survey Open-File Report 78-124, iv, 144 p., https://doi.org/10.3133/ofr78124.","productDescription":"iv, 144 p.","costCenters":[],"links":[{"id":428537,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0124/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148585,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0124/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Georgia to Georges Bank","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.75683968804638,\n              41.66992961819466\n            ],\n            [\n              -81.24003722734089,\n              41.66992961819466\n            ],\n            [\n              -81.24003722734089,\n              31.17169868819218\n            ],\n            [\n              -70.75683968804638,\n              31.17169868819218\n            ],\n            [\n              -70.75683968804638,\n              41.66992961819466\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6246ce","contributors":{"authors":[{"text":"Swanson, Paul G.","contributorId":97376,"corporation":false,"usgs":true,"family":"Swanson","given":"Paul","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":172388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Ralph E.","contributorId":15882,"corporation":false,"usgs":true,"family":"Brown","given":"Ralph","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":172387,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28881,"text":"wri76123 - 1977 - Geohydrology of the Englishtown Formation in the northern Coastal Plain of New Jersey","interactions":[],"lastModifiedDate":"2012-09-19T17:16:46","indexId":"wri76123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"76-123","title":"Geohydrology of the Englishtown Formation in the northern Coastal Plain of New Jersey","docAbstract":"The Englishtown Formation of the Matawan Group of Late Cretaceous age is exposed in the western part of the New Jeresy Coastal Plain along a northeast-southwest trending zone extending from Raritan Bay to Delaware Bay. In outcrop, in the northern part of the Coastal Plain, the Englishtown typically consists of a series of thin, cross-stratified, fine- to medium-grained lignitic quartz sand beds intercalated with thin beds of sandy silty clay and clayey silt, ranging in total thickness from about 140 feet (43 meters) near Raritan Bay to about 50 feet (15 meters) near Trenton. In the subsurface of the northern part of the Coastal Plain, the formation retains most of the lithologic characteristics displayed in outcrop. In northern and eastern Ocean County the Englishtown can be subdivided into three distinct lithologic units; upper and lower units of quartz sand with thin interbeds of dark sandy silt, separated by a thick sequence of sandy and clayey lignitic silt. The confined part of the aquifer in the Englishtown Formation is utilized as a source of water over an area of about 1,100 square miles (2,849 square kilometers) of the New Jersey Coastal Plain and is an important source of supply in Monmouth and northern Ocean Counties. The annual average rate of withdrawal from the aquifer in the two-county area increased from 5.5 million gallons per day (0.24 cubic meters per second) in 1959 to 9.5 million gallons per day (0.4 cubic meters per second) in 1970. Water levels in parts of this area were declining 8 to 12 feet (2.4 to 3.6 meters) per year as of 1970 and they declined as much as 140 feet (43 meters) between 1959 and 1970 near pumping centers. The aquifer transmissivity ranges from 2,400 square feet per day to 650 square feet per day (223 square meters per day to 60 square meters per day); the estimated hydraulic conductivity ranges from about 11 feet per day to 20 feet per day (3.3 meters per day to 6.1 meters per day); and the storage coefficient ranges from 8 x 10<sup>-5</sup> to 3 x 10<sup>-4</sup>. The underlying and overlying confining beds, which have an average thickness of 200 feet (61 meters) and 40 feet (12 meters), respectively, have vertical hydraulic conductivities on the order of 1 x 10<sup>-5</sup> feet per day (3 x 10<sup>-6</sup> meters per day) and specific storage on the order of 8 x 10<sup>-5</sup> ft<sup>-1</sup> (2.4 x 10<sup>-5</sup> m<sup>-1</sup>). The Englishtown aquifer is an integral part of the complex multi- aquifer system of the New Jersey Coastal Plain. The withdrawal of water from the Englishtown aquifer has had a marked effect on the water level in the overlying Moutn Laurel aquifer, and these effects will continue so long as the water level in the Englishtown continues to decline. Any increase in the development of the Mount Laurel aquifer that reduces the volume of leakage to the Englishtown will cause an increase in the rate of water-level decline in the Englishtown even with no increase in direct withdrawals. The interrelationship and interdependency between pumping stresses in individual aquifers within the complex Coastal Plain aquifer sytem must be recognized and appreciated, and the hydrodynamics of all parts of the system must be considered if reliable predictions of aquifer response to these stresses are to be made. Such predictions generally require a simulation model analysis of the system.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Trenton, NJ","doi":"10.3133/wri76123","collaboration":"Prepared in cooperation with the New Jersey Department of Environmental Protection, Division of Water Resources","usgsCitation":"Nichols, W.D., 1977, Geohydrology of the Englishtown Formation in the northern Coastal Plain of New Jersey: U.S. Geological Survey Water-Resources Investigations Report 76-123, vi, 62 p., https://doi.org/10.3133/wri76123.","productDescription":"vi, 62 p.","numberOfPages":"68","onlineOnly":"Y","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":159621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_76_123.gif"},{"id":261954,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1976/123/","linkFileType":{"id":5,"text":"html"}},{"id":261955,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/123/pdf/wrir76-123.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75,39.666666666666664 ], [ -75,40.666666666666664 ], [ -73.83333333333333,40.666666666666664 ], [ -73.83333333333333,39.666666666666664 ], [ -75,39.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89af","contributors":{"authors":[{"text":"Nichols, W. D.","contributorId":73220,"corporation":false,"usgs":true,"family":"Nichols","given":"W.","middleInitial":"D.","affiliations":[],"preferred":false,"id":200553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30590,"text":"wri77134 - 1977 - Hydrologic map of the Orlando East Quadrangle, Florida","interactions":[],"lastModifiedDate":"2019-08-05T09:21:15","indexId":"wri77134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-134","title":"Hydrologic map of the Orlando East Quadrangle, Florida","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri77134","usgsCitation":"Wood, W., and Snell, L., 1977, Hydrologic map of the Orlando East Quadrangle, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-134, 8 Plates: 26.02 x 36.03 inches or smaller, https://doi.org/10.3133/wri77134.","productDescription":"8 Plates: 26.02 x 36.03 inches or smaller","costCenters":[],"links":[{"id":366146,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0134/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0134/report-thumb.jpg"},{"id":366147,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0134/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366148,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0134/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366149,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0134/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366150,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0134/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366151,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0134/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366152,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0134/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366153,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0134/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.38568878173828,\n              28.50520367835768\n            ],\n            [\n              -81.2545394897461,\n              28.50520367835768\n            ],\n            [\n              -81.2545394897461,\n              28.622199454920608\n            ],\n            [\n              -81.38568878173828,\n              28.622199454920608\n            ],\n            [\n              -81.38568878173828,\n              28.50520367835768\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6067dc","contributors":{"authors":[{"text":"Wood, W.D.","contributorId":31799,"corporation":false,"usgs":true,"family":"Wood","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":203502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snell, L.J.","contributorId":25555,"corporation":false,"usgs":true,"family":"Snell","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":203501,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8579,"text":"ofr77308 - 1977 - Municipal, industrial, and irrigation water use in Washington, 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr77308","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-308","title":"Municipal, industrial, and irrigation water use in Washington, 1975","docAbstract":"An assessment of water use in 1975 in the 39 counties and 62 Water Resources Inventory Areas of Washington, indicated that 2.49 trillion gallons of water was used for municipal, industrial, and irrigation purposes. That amount represents a 10-percent increase over a similar water-use assessment in 1965, but a slight decrease from that of 1970. Total municipal water use, which includes municipally supplied industrial water, was 283 billion gallons. Industry used 442 billion gallons, of which 121 billion gallons was from municipal systems and 321 billion gallons was for self-suppled systems. Of the 604 billion gallons of water used for municipal and industrial supplies 145 billion gallons was ground water, 444 billion gallons was fresh surface water, and 14.8 billion gallons was saline surface water. A compilation of statewide industrial use as categorized by SIC (Lumber and Wood Products), SIC 28 (Chemicals and Allied Products), and SIC 20 (Food and Kindred Products)--accounted for about 65 percent of the total water used in industrial processes , In 1975, 5.79 million acre-feet of irrigation water (1,890 billion gallons) as applied to 1.52 million acres. This water was 95 percent surface water and 5 percent ground water. About 97 percent of the irrigation water was supplied in eastern Washington, to about 94 percent of the irrigated acreage in the State. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77308","usgsCitation":"Dion, N.P., and Lum, W., 1977, Municipal, industrial, and irrigation water use in Washington, 1975: U.S. Geological Survey Open-File Report 77-308, vi, 18, [23] leaves :ill., 6 maps (col.) ;33 cm.; (24 p. - PGS), https://doi.org/10.3133/ofr77308.","productDescription":"vi, 18, [23] leaves :ill., 6 maps (col.) ;33 cm.; (24 p. - PGS)","costCenters":[],"links":[{"id":141030,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698a84","contributors":{"authors":[{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":157974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lum, W. E.","contributorId":57847,"corporation":false,"usgs":true,"family":"Lum","given":"W. E.","affiliations":[],"preferred":false,"id":157975,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10583,"text":"ofr77264 - 1977 - January 1977 water levels, and data related to water-level changes since 1950, western Kansas","interactions":[],"lastModifiedDate":"2017-09-29T08:07:58","indexId":"ofr77264","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-264","title":"January 1977 water levels, and data related to water-level changes since 1950, western Kansas","docAbstract":"<p>This report contains basic data on water-level measurements in observation wells in western Kansas. Most of the measurements were made in January 1977; a few were made in December 1976 and in February 1977. The measurements were made in mid-winter when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also contains basic hydrologic data for 1950-77 that are provided for consideration in relation to the January 1977 water-level measurements.</p><p>The annual water-level measurements are made by personnel of the Division of Water Resources of the Kansas State Board of Agriculture and of the U.S. Geological Survey. State-agency support for this program is provided through the Kansas Geological Survey.</p><p>Wells in this report are numbered according to the Bureau of Land Management's system of land subdivision. In this system, the first set of digits of a well number indicates the township; the second set, the range east or west of the sixth prinicipal meridian; and the third set, the section in which the well is situated. The first letter denotes the 160-acre tract, the second, the 40-acre tract, and the third, the 10-acre tract. The letters are designated in a counterclockwise direction beginning in the northeast quarter of the section. Where there is more than one well in a 10-acre tract, consecutive numbers, beginning with \"2\", are added in the order in which the wells are inventoried.<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77264","usgsCitation":"Pabst, M.E., 1977, January 1977 water levels, and data related to water-level changes since 1950, western Kansas: U.S. Geological Survey Open-File Report 77-264, 209 p., https://doi.org/10.3133/ofr77264.","productDescription":"209 p.","numberOfPages":"213","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":346201,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0264/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0264/report-thumb.jpg"}],"country":"United States","state":"Kansas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fc7","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30552,"text":"wri7726 - 1977 - Hydrology of the Creeping Swamp Watershed, North Carolina with reference to potential effects of stream channelization","interactions":[],"lastModifiedDate":"2019-07-22T12:15:02","indexId":"wri7726","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-26","title":"Hydrology of the Creeping Swamp Watershed, North Carolina with reference to potential effects of stream channelization","docAbstract":"Hydrologic data were collected for four years at six sites in the Creeping Swamp watershed in eastern North Carolina in a preliminary effort to study the effects of stream channelization on the hydrology of a small watershed. A water-budget evaluation for pre-channelized conditions showed that runoff accounts for about 17 percent of the total rainfall, base runoff about 20 percent, ground-water outflow about 2 percent, and evapotranspiration about 61 percent. Channelization would have caused the greatest decline in ground-water levels nearest the stream, with the decline diminishing with increased distance from the stream. Channelization would also have resulted in a decrease in overland runoff and an increase in the amount of water reaching Creeping Swamp through the ground-water system, although the total volume of runoff would not change significantly. The water-quality characteristics of Creeping Swamp indicate that the stream is relatively free of pollution, although it is likely that channelization would increase (1) suspended-sediment loads, (2) stream temperatures, and (3) concentrations of dissolved solids, especially during low flows.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7726","usgsCitation":"Winner, M., and Simmons, C., 1977, Hydrology of the Creeping Swamp Watershed, North Carolina with reference to potential effects of stream channelization: U.S. Geological Survey Water-Resources Investigations Report 77-26, vi, 54 p. , https://doi.org/10.3133/wri7726.","productDescription":"vi, 54 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":365792,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0026/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Creeping Swamp 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691232","contributors":{"authors":[{"text":"Winner, M.D.","contributorId":59801,"corporation":false,"usgs":true,"family":"Winner","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":203444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, C.E.","contributorId":32572,"corporation":false,"usgs":true,"family":"Simmons","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":203443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26265,"text":"wri7742 - 1977 - Water-level changes in the northern high plains of Colorado, 1964 to 1976 and 1972 to 1976","interactions":[],"lastModifiedDate":"2018-11-16T09:42:19","indexId":"wri7742","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-42","title":"Water-level changes in the northern high plains of Colorado, 1964 to 1976 and 1972 to 1976","docAbstract":"<p>The northern High Plains of Colorado is an area of about 9,500 mi<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>2</sup><span id=\"_mce_caret\" data-mce-bogus=\"true\"> (24,600 km<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>2</sup><span id=\"_mce_caret\" data-mce-bogus=\"true\">) in the eastern part of the State (index map). The boundaries of the High Plains of Colorado are the State line and the limit of the Ogallala Formation of late Tertiary age. The Ogallala Formation is an unconsolidated or partly consolidated deposit of sand, gravel, clay, and silt and is the major aquifer in the northern High Plains.</span></span></span></span><br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7742","usgsCitation":"Borman, R.G., and Major, T.J., 1977, Water-level changes in the northern high plains of Colorado, 1964 to 1976 and 1972 to 1976: U.S. Geological Survey Water-Resources Investigations Report 77-42, 35.92 x 30.55 inches, https://doi.org/10.3133/wri7742.","productDescription":"35.92 x 30.55 inches","costCenters":[],"links":[{"id":157802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0042/report-thumb.jpg"},{"id":359486,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.7,\n              38.33\n            ],\n            [\n              -102.04376220703125,\n              38.33\n            ],\n            [\n              -102.04376220703125,\n              41\n            ],\n            [\n              -103.7,\n              41\n            ],\n            [\n              -103.7,\n              38.33\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e776a","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":196083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Major, Thomas J.","contributorId":32529,"corporation":false,"usgs":true,"family":"Major","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29408,"text":"wri76132 - 1977 - Ground-water quality near a sewage-sludge recycling site and a landfill near Denver, Colorado","interactions":[],"lastModifiedDate":"2018-08-08T13:48:57","indexId":"wri76132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"76-132","title":"Ground-water quality near a sewage-sludge recycling site and a landfill near Denver, Colorado","docAbstract":"<p>The Metropolitan Denver Sewage Disposal District and the City and County of Denver operate a sewage-sludge recycling site and a landfill in an area about 15 miles (24 kilometers) east of Denver. The assessment of the effects of these facilities on the ground-water system included determining the direction of ground-water movement in the area, evaluating the impact of the wastedisposal activities on the chemical quality of local ground water, and evaluating the need for continued water-quality monitoring.</p><p>Surficial geology of the area consists of two principal units: (1) Alluvium with a maximum thickness of about 25 feet (7.6 meters) deposited along stream channels, and (2) bedrock consisting of undifferentiated Denver and Dawson Formations. Ground water in formations less than 350 feet (110 meters) deep moves to the north, as does surface flow, while ground water in formations between 570 and 1,500 feet (170 and 460 meters) deep moves to the west. Estimates of ground-water velocity were made using assumed values for hydraulic conductivity and porosity, and the observed hydraulic gradient from the study area. Lateral velocities are estimated to be 380 feet (120 meters) per year in alluvium and 27 feet (8.2 meters) per year in the upper part of the bedrock formations. Vertical velocity is estimated to be 0.58 foot (0.18 meter) per year in the upper part of the bedrock formations.</p><p>Potentiometric head decreases with depth in the bedrock formations indicating a potential for downward movement of ground water. However, waterquality analysis and the rate and direction of ground-water movement suggest that ground-water movement in the area is primarily in the lateral rather than the vertical direction. </p><p>Five wells perforated in alluvium were found to have markedly degraded water quality. One well was located in the landfill and water that was analyzed was obtained from near the base of the buried refuse, two others were located downgradient and near sewage-sludge burial areas, and the remaining two are located near stagnant surface ponds. Concentrations of nitrate in&nbsp;wells downgradient from fields where sludge is plowed into the soil were higher than background concentrations due to the effects of the sludge disposal. No evidence of water-quality degradation was detected in deeper wells perforated in the bedrock formations. Continued water-quality monitoring is needed because of the continuing disposal of wastes. A suggested monitoring program would consist of monitoring wells near the landfill twice a year and monitoring wells near the sludge-disposal areas on an annual basis. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76132","usgsCitation":"Robson, S.G., 1977, Ground-water quality near a sewage-sludge recycling site and a landfill near Denver, Colorado: U.S. Geological Survey Water-Resources Investigations Report 76-132, Report: iv, 137 p.; 2 Plates: 15.57 x 15.37 inches and 15.33 x 15.43 inches, https://doi.org/10.3133/wri76132.","productDescription":"Report: iv, 137 p.; 2 Plates: 15.57 x 15.37 inches and 15.33 x 15.43 inches","costCenters":[],"links":[{"id":356332,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0132/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":356333,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0132/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0132/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123300,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0132/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.625,\n              39.625\n            ],\n            [\n              -104.7083,\n              39.625\n            ],\n            [\n              -104.7083,\n              39.6833\n            ],\n            [\n              -104.625,\n              39.6833\n            ],\n            [\n              -104.625,\n              39.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667191","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8675,"text":"ofr77487 - 1977 - Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma","interactions":[{"subject":{"id":8675,"text":"ofr77487 - 1977 - Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma","indexId":"ofr77487","publicationYear":"1977","noYear":false,"title":"Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046142,"text":"70046142 - 1986 - Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","indexId":"70046142","publicationYear":"1986","noYear":false,"title":"Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water"},"id":1}],"supersededBy":{"id":70046142,"text":"70046142 - 1986 - Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","indexId":"70046142","publicationYear":"1986","noYear":false,"title":"Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water"},"lastModifiedDate":"2017-09-29T07:58:43","indexId":"ofr77487","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-487","title":"Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma","docAbstract":"<p>Most of the data presented in this report were collected by the U.S. Geological Survey as part of a study of the geohydrology of the Vamoosa aquifer, in east-central Oklahoma, in cooperation with the Oklahoma Geological Survey. Some of the data listed in the tables were collected by Bingham and Moore (1975) and Bingham and Bergman (in press).</p><p>Acknowledgment is extended to city officials and individuals who provided the data for this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77487","usgsCitation":"D’Lugosz, J.J., and McClaflin, R.G., 1977, Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma: U.S. Geological Survey Open-File Report 77-487, iii, 38 p., https://doi.org/10.3133/ofr77487.","productDescription":"iii, 38 p.","numberOfPages":"43","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":142224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0487/report-thumb.jpg"},{"id":346195,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0487/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oklahoma","otherGeospatial":"Vamoosa Aquifer","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.3006,36.1632],[-96.3002,36.1577],[-96.2991,36.0778],[-96.085,36.0773],[-96.0281,36.0764],[-96.0288,36.0006],[-96.0286,35.9906],[-96.0304,35.9026],[-96.0326,35.9027],[-96.0319,35.8565],[-96.1928,35.8589],[-96.1936,35.6365],[-96.1944,35.553],[-96.0898,35.5532],[-96.0892,35.3756],[-95.9803,35.3751],[-95.9809,35.2896],[-96.4413,35.2902],[-96.4393,35.1158],[-96.4932,35.116],[-96.4944,35.0275],[-96.4961,34.9076],[-96.5043,34.8978],[-96.5046,34.8878],[-96.5128,34.8775],[-96.5237,34.8678],[-96.5344,34.8671],[-96.5437,34.875],[-96.5585,34.9026],[-96.5572,34.9085],[-96.5608,34.919],[-96.5675,34.9205],[-96.5749,34.9156],[-96.585,34.9163],[-96.5872,34.9159],[-96.5924,34.911],[-96.5975,34.9088],[-96.6045,34.9031],[-96.6186,34.9006],[-96.6337,34.8996],[-96.646,34.9016],[-96.6559,34.9068],[-96.658,34.9123],[-96.6615,34.9274],[-96.6726,34.9312],[-96.6831,34.9364],[-96.6932,34.9357],[-96.7017,34.9314],[-96.7081,34.9242],[-96.715,34.9189],[-96.7146,34.9139],[-96.7074,34.9092],[-96.6986,34.9036],[-96.6927,34.8953],[-96.6891,34.8866],[-96.6921,34.8776],[-96.6951,34.8726],[-96.7032,34.8646],[-96.706,34.8633],[-96.7151,34.858],[-96.732,34.8566],[-96.7391,34.8612],[-96.7411,34.8694],[-96.7465,34.8782],[-96.7529,34.8906],[-96.7549,34.897],[-96.7626,34.9026],[-96.7681,34.9054],[-96.7783,34.9015],[-96.7823,34.8988],[-96.7896,34.899],[-96.7912,34.9004],[-96.7989,34.9087],[-96.8005,34.9119],[-96.7998,34.9142],[-96.7998,34.9332],[-96.8013,34.9396],[-96.8035,34.9419],[-96.8197,34.9431],[-96.8237,34.9428],[-96.8311,34.9393],[-96.8329,34.9357],[-96.8346,34.9348],[-96.8397,34.9326],[-96.8419,34.9336],[-96.843,34.9354],[-96.8446,34.9363],[-96.8599,34.9294],[-96.8668,34.9268],[-96.8785,34.9265],[-96.8902,34.9295],[-96.8991,34.9337],[-96.9041,34.937],[-96.9051,34.9406],[-96.9033,34.9456],[-96.906,34.9497],[-96.9087,34.952],[-96.9086,34.9548],[-96.9096,34.9598],[-96.914,34.963],[-96.9218,34.9654],[-96.933,34.9665],[-96.9431,34.9658],[-96.9494,34.9618],[-96.9563,34.9533],[-96.9627,34.9448],[-96.9662,34.9403],[-96.9685,34.9376],[-96.9709,34.935],[-96.9817,34.9265],[-96.9921,34.9176],[-97.0068,34.9106],[-97.0147,34.9094],[-97.0169,34.9099],[-97.0253,34.9104],[-97.0453,34.918],[-97.0537,34.9205],[-97.0621,34.9202],[-97.0715,34.9244],[-97.0797,34.9318],[-97.0859,34.9328],[-97.1027,34.9313],[-97.1161,34.9356],[-97.1285,34.9344],[-97.1432,34.9305],[-97.1433,35.2021],[-97.1405,35.202],[-97.1442,35.3742],[-97.1437,35.4645],[-97.1452,35.6361],[-97.1436,35.7246],[-97.1438,35.8112],[-97.1433,35.8988],[-97.1405,35.8988],[-97.1409,35.9283],[-97.1428,35.9442],[-97.1423,35.9641],[-97.1557,35.9485],[-97.1729,35.9428],[-97.1872,35.9426],[-97.2013,35.9469],[-97.2163,35.9576],[-97.2252,35.9677],[-97.236,35.9683],[-97.2461,35.9721],[-97.2523,35.9744],[-97.2734,35.9734],[-97.2841,35.9767],[-97.2863,35.9795],[-97.2862,35.9835],[-97.2883,35.9931],[-97.2927,36.0004],[-97.2982,36.0091],[-97.3055,36.011],[-97.3203,36.0108],[-97.3329,36.0078],[-97.3359,36.0024],[-97.34,35.9947],[-97.3475,35.9885],[-97.3556,35.9841],[-97.3569,36.1583],[-97.1426,36.1588],[-97.1417,36.245],[-96.9277,36.246],[-96.9276,36.3313],[-97.0338,36.3326],[-97.0333,36.5059],[-97.0116,36.506],[-97.0109,36.5105],[-97.0096,36.5155],[-97.0083,36.5204],[-97.0025,36.5249],[-96.9978,36.5275],[-96.9915,36.5292],[-96.988,36.531],[-96.9828,36.5327],[-96.977,36.5344],[-96.9667,36.5352],[-96.9564,36.535],[-96.9506,36.5367],[-96.946,36.538],[-96.939,36.5424],[-96.9355,36.5455],[-96.929,36.5513],[-96.9261,36.554],[-96.9243,36.554],[-96.9175,36.5529],[-96.906,36.5536],[-96.9003,36.554],[-96.8968,36.5553],[-96.8921,36.5597],[-96.8909,36.5634],[-96.8873,36.5683],[-96.8866,36.5732],[-96.8876,36.5792],[-96.8932,36.5824],[-96.9034,36.5867],[-96.9162,36.6001],[-96.9387,36.5959],[-96.9468,36.5911],[-96.9526,36.5889],[-96.9549,36.589],[-96.9612,36.5882],[-96.974,36.5843],[-96.982,36.583],[-96.986,36.5827],[-96.9952,36.5837],[-97.0032,36.5839],[-97.0153,36.5827],[-97.029,36.5847],[-97.0415,36.5858],[-97.0512,36.5883],[-97.0568,36.5929],[-97.055,36.5979],[-97.0532,36.601],[-97.0469,36.6018],[-97.0473,36.6054],[-97.049,36.6068],[-97.0547,36.6106],[-97.0551,36.6165],[-97.0528,36.6364],[-97.0617,36.651],[-97.0656,36.6547],[-97.067,36.6656],[-97.0666,36.6829],[-97.0606,36.6918],[-97.0548,36.6926],[-97.0491,36.6939],[-97.0253,36.7012],[-97.0238,36.6953],[-97.017,36.6907],[-97.0038,36.6909],[-96.994,36.6903],[-96.9878,36.6875],[-96.9682,36.6889],[-96.958,36.6865],[-96.9477,36.6836],[-96.9345,36.6852],[-96.9263,36.691],[-96.9262,36.6937],[-96.9267,36.6982],[-96.9254,36.7014],[-96.9206,36.7085],[-96.9204,36.7176],[-96.9151,36.7216],[-96.9061,36.7351],[-96.8907,36.7525],[-96.8786,36.7536],[-96.8689,36.7521],[-96.8604,36.7483],[-96.849,36.7445],[-96.8404,36.7434],[-96.8248,36.7472],[-96.8218,36.7531],[-96.821,36.7589],[-96.822,36.7662],[-96.8133,36.7665],[-96.8041,36.7663],[-96.7967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Joseph J.","contributorId":71172,"corporation":false,"usgs":true,"family":"D’Lugosz","given":"Joseph","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McClaflin, Roger G.","contributorId":50157,"corporation":false,"usgs":true,"family":"McClaflin","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10352,"text":"ofr77428 - 1977 - Progress report on uranium investigations in the Zane Hills area, west-central Alaska","interactions":[],"lastModifiedDate":"2023-08-29T20:45:06.015711","indexId":"ofr77428","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-428","title":"Progress report on uranium investigations in the Zane Hills area, west-central Alaska","docAbstract":"<p>The Zane Hills pluton underlies a mountainous area of about 460 km<sup>2</sup> in west-central Alaska and is locally enriched in uranium and thorium (Miller and Ferrians, 1968; Miller, 1970; Staatz and Miller, 1976). While over 90 percent of the pluton consists of granodiorite with average contents of uranium and thorium, zones of porphyritic to gneissic monzonite along the southern and eastern margins of the pluton (fig. 1) contain as much as 100 ppm (parts per million) uranium and 269 ppm thorium (Staatz and Miller, 1976; table 1, this report). This report presents information obtained in 1976 on the relationship of the uraniferous monzonite to the granodiorite and on uranium enrichment outside the pluton as part of an on-going study of the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77428","usgsCitation":"Miller, T.P., and Elliott, R.L., 1977, Progress report on uranium investigations in the Zane Hills area, west-central Alaska: U.S. Geological Survey Open-File Report 77-428, 12 p., https://doi.org/10.3133/ofr77428.","productDescription":"12 p.","costCenters":[],"links":[{"id":420265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0428/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143550,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0428/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Zane Hills area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -152.67015825439097,\n              66.36915590077189\n            ],\n            [\n              -152.67015825439097,\n              65.57079937978608\n            ],\n            [\n              -150.11332818389027,\n              65.57079937978608\n            ],\n            [\n              -150.11332818389027,\n              66.36915590077189\n            ],\n            [\n              -152.67015825439097,\n              66.36915590077189\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699043","contributors":{"authors":[{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":161239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Raymond L.","contributorId":82667,"corporation":false,"usgs":true,"family":"Elliott","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161240,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8823,"text":"ofr77136 - 1977 - Geologic framework of lower Cook Inlet, Alaska","interactions":[{"subject":{"id":8823,"text":"ofr77136 - 1977 - Geologic framework of lower Cook Inlet, Alaska","indexId":"ofr77136","publicationYear":"1977","noYear":false,"title":"Geologic framework of lower Cook Inlet, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70047582,"text":"70047582 - 1978 - Geologic framework of lower Cook Inlet, Alaska","indexId":"70047582","publicationYear":"1978","noYear":false,"title":"Geologic framework of lower Cook Inlet, Alaska"},"id":1}],"supersededBy":{"id":70047582,"text":"70047582 - 1978 - Geologic framework of lower Cook Inlet, Alaska","indexId":"70047582","publicationYear":"1978","noYear":false,"title":"Geologic framework of lower Cook Inlet, Alaska"},"lastModifiedDate":"2024-03-25T18:14:13.131377","indexId":"ofr77136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-136","title":"Geologic framework of lower Cook Inlet, Alaska","docAbstract":"<p>Lower Cook Inlet is located in south-central Alaska between lat 58°45' and 60°30' N. and between long 151° and 154° W. (fig. 1). Geographic features on the perimeter of the area are the Aleutian Range on the northwest, Kalgin Island on the northeast, the Kenai Peninsula on the east, the Barren Islands on the southeast, and the Kamishak Hills-Cape Douglas area on the south. Augustine Island, a prominent active composite volcano, is in the southwestern part of lower Cook Inlet. Lower Cook Inlet is part of a large bay that is nearly surrounded by mountains except where it opens southeastward into the Gulf of Alaska and southward into Shelikof Strait. In anticipation of oil and gas lease sales in lower Cook Inlet, the U.S. Geological Survey acquired geological and geophysical data to study the geologic framework and petroleum geology of this area. These data were included in the lower Cook Inlet environmental impact statements (Alaska Outer Continental Shelf Office, 1976a, b) and are being made available to other government agencies and the public.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77136","usgsCitation":"Fisher, M.A., and Magoon, L.B., 1977, Geologic framework of lower Cook Inlet, Alaska: U.S. Geological Survey Open-File Report 77-136, 73 p., https://doi.org/10.3133/ofr77136.","productDescription":"73 p.","costCenters":[],"links":[{"id":426976,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0136/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141692,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0136/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"lower Cook Inlet","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -153.1402801546936,\n              59.832636487498206\n            ],\n            [\n              -153.1402801546936,\n              58.700441131804695\n            ],\n            [\n              -152.0271083182426,\n              58.700441131804695\n            ],\n            [\n              -152.0271083182426,\n              59.832636487498206\n            ],\n            [\n              -153.1402801546936,\n              59.832636487498206\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a56bd","contributors":{"authors":[{"text":"Fisher, Michael A. mfisher@usgs.gov","contributorId":1991,"corporation":false,"usgs":true,"family":"Fisher","given":"Michael","email":"mfisher@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158390,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":158391,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5636,"text":"pp1028 - 1977 - Studies related to the Charleston, South Carolina, earthquake of 1886: A preliminary report","interactions":[],"lastModifiedDate":"2024-11-19T14:26:59.152609","indexId":"pp1028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"1028","title":"Studies related to the Charleston, South Carolina, earthquake of 1886: A preliminary report","docAbstract":"<p>PART A: The seismic history of the southeastern United States is dominated by the 1886 earthquake near Charleston, S.C. An understanding of the specific source and the uniqueness of the neotectonic setting of this large earthquake is essential in order to properly assess seismic hazards in the southeastern United States. Such knowledge will also contribute to the fundamental understanding of intraplate earthquakes and will aid indirectly in deciphering the evolution of Atlantic-type continental margins. The 15 chapters in this volume report on the first stage of an ongoing multidisciplinary study of the Charleston earthquake of 1886. The Modified Mercalli intensity for the 1886 earthquake was X in the meizoseismal area, an elliptical area 35 by 50 km, the center of which was Middleton Place. Seismic activity is continuing today in the Middleton Place-Summerville area at a higher level than prior to 1886. The present seismicity is originating at depths of 1 to 8 km, mostly in the crystalline basement beneath sedimentary rocks of the Coastal Plain. The crystalline basement beneath the Charleston-Summerville area is not simply a seaward extension of crystalline rocks of the Appalachian orogen that are exposed in the Piedmont to the northwest, but has a distinctive magnetic signature that does not reflect Appalachian orogenic trends. The area underlain by this distinctive geophysical basement, the Charleston block, may represent a broad zone of Triassic and (or) Jurassic crustal extension formed during the early stages of the opening of the Atlantic Ocean. The Charleston block is characterized in part by prominent, roughly circular magnetic and gravity highs that are thought to reflect maflc or ultramafic plutons. A continuously cored borehole put down over the shallowest (about 1.5 km deep) of these magnetic anomalies on the edge of the meizoseismal area bottomed at 792 m in amygdaloidal basalt. Although the K-Ar ages of about 100 m.y. for the basalt are consistent with the Late Cretaceous (Cenomanian) age of the overlying Cape Fear Formation, this must be a minimum age as a result of chemical alteration. The interpreted magmatic composition of the basalt most closely resembles the high-Ti quartz-normative tholeiites of Late Triassic and Early Jurassic age from eastern North America; age of the basalt is probably similar. Various geophysical surveys suggest that Coastal Plain sedimentary rocks do not simply dip homoclinally to the southeast on a gently dipping basement surface but are disturbed by structures not yet clearly deciphered. The present stress regime of the Charleston-Summerville area appears to be one of NE-SW. compression rather than of extension as it presumably was in the Mesozoic. The present stress regime seems similar to that of much of the eastern United States. Comparison of several seismic source areas in eastern North America shows that epicenters are typically near the periphery of positive gravity features interpreted to represent mafic or ultramafic bodies. Earthquakes may be caused by the concentration of regional stress around the peripheries of these inhomogeneities in an otherwise more homogeneous plate. Whether the inhomogeneities are more or less rigid than the. surrounding material is uncertain. PART B: In 1889, C. E. Dutton published all his basic intensity data for the 1886 Charleston, S.C., shock but did not list what intensity values he assigned to each report, nor did he show the distribution of the locations of these data reports on his isoseismal map. The writer and two other seismologists have each independently evaluated Dutton's 1,300 intensity reports (at least two of the. three interpreters agreed on intensity values for 90 percent of the reports), and the consensus values were plotted and contoured. One map was prepared on which contours emphasized the broad regional pattern of effects (with results similar to Dutton's) ; another map was contoured to depict the more</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1028","usgsCitation":"Rankin, D., 1977, Studies related to the Charleston, South Carolina, earthquake of 1886: A preliminary report: U.S. Geological Survey Professional Paper 1028, iii, 204 p., https://doi.org/10.3133/pp1028.","productDescription":"iii, 204 p.","costCenters":[],"links":[{"id":464242,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92981.htm","text":"Biostratigraphy of the deep corehole (Clubhouse Crossroads corehole 1) near Charleston, South Carolina","linkFileType":{"id":5,"text":"html"}},{"id":140112,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1028/report-thumb.jpg"},{"id":32134,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402866,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92975.htm","text":"Lithostratigraphy of the deep corehole (Clubhouse Crossroads corehole 1) near Charleston, South Carolina","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","city":"Charleston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.17822265625,\n              32.637061996573436\n            ],\n            [\n              -79.79095458984375,\n              32.637061996573436\n            ],\n            [\n              -79.79095458984375,\n              32.95567280997862\n            ],\n            [\n              -80.17822265625,\n              32.95567280997862\n            ],\n            [\n              -80.17822265625,\n              32.637061996573436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d3b","contributors":{"authors":[{"text":"Rankin, Douglas W. dwrankin@usgs.gov","contributorId":1770,"corporation":false,"usgs":true,"family":"Rankin","given":"Douglas W.","email":"dwrankin@usgs.gov","affiliations":[],"preferred":true,"id":151342,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9426,"text":"ofr77209 - 1977 - Floods in the Big Creek basin, Linn County, Iowa","interactions":[],"lastModifiedDate":"2016-02-22T15:12:42","indexId":"ofr77209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-209","title":"Floods in the Big Creek basin, Linn County, Iowa","docAbstract":"<p>Flood information for the Big Creek basin in Linn County, Iowa, should be of use to those concerned with the design of bridges and other structures on the flood plains of the streams. Water-surface profiles for the flood of May 1974 are given for Big Creek and its major tributaries, East Big, Crabapple, Elbow, and Abbe Creeks. The May 1974 flood was at least a 50-year flood on East Big Creek and along certain reaches of Big and Abbe Creeks. Also included for Big Creek are a profile of the December 1971 medium-stage flow and a partial profile for the minor flood of July 1971. Profiles for the low-water condition of October 26, 1972, are shown for all reaches. Water-surface profiles for the 25- and 50-year floods are estimated in relation to the May 1974 flood.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr77209","collaboration":"Prepared in cooperation with Linn County, Iowa","usgsCitation":"Heinitz, A.J., 1977, Floods in the Big Creek basin, Linn County, Iowa: U.S. Geological Survey Open-File Report 77-209, iv, 35 p., https://doi.org/10.3133/ofr77209.","productDescription":"iv, 35 p.","numberOfPages":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318295,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77209.JPG"},{"id":286617,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0209/report.pdf"}],"country":"United States","state":"Iowa","county":"Linn County","otherGeospatial":"Big Creek Basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.3649,42.2964],[-91.3651,42.2082],[-91.3653,42.1215],[-91.3661,42.0343],[-91.3669,41.948],[-91.3677,41.8603],[-91.4836,41.8608],[-91.5989,41.8612],[-91.716,41.862],[-91.8318,41.8617],[-91.8329,41.9485],[-91.8338,42.0366],[-91.8342,42.1242],[-91.8328,42.2087],[-91.8319,42.2987],[-91.7153,42.2971],[-91.5969,42.2959],[-91.4809,42.296],[-91.3649,42.2964]]]},\"properties\":{\"name\":\"Linn\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0e18","contributors":{"authors":[{"text":"Heinitz, Albert J.","contributorId":43355,"corporation":false,"usgs":true,"family":"Heinitz","given":"Albert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159665,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10158,"text":"ofr77672 - 1977 - Shelled benthic fauna of the eastern Chukchi Sea","interactions":[],"lastModifiedDate":"2024-02-28T22:32:29.743817","indexId":"ofr77672","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-672","title":"Shelled benthic fauna of the eastern Chukchi Sea","docAbstract":"<p>The purposes of this study were to identify the benthic shelled infauna and epifauna of the eastern Chukchi Sea, compile species lists and distribution maps, determine recurrent groups of species (communities), and examine the environmental parameters that may control the distribution of the faunal groups. The study was partly supported by the Bureau of Land Management through an interagency agreement with the National Oceanic and Atmospheric Administration, under which a multi-year program responding to the needs of petroleum development of the Alaskan continental shelf is managed by the Outer Continental Shelf Environmental Assessment Program (OCSEAP) Office. The objective of this study is to provide an assessment of the biological patterns of the region as related to petroleum development. Future offshore oil leases proposed by the State of Alaska and the Federal Government require a biological data base from which impact statements can be derived.</p><p>Samples used in this report were collected by the U.S. Geological Survey in August 1974 from the U.S. Coast Guard Cutter Burton Island under the direction of Arthur Grantz. Sampling was conducted using van Veen grabs, gravity cores, dart cores, and bottom dredges. Only the van Veen grabs contained material useful for this study. At present 103 samples containing 90 species have been examined.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77672","usgsCitation":"Mann, D.M., 1977, Shelled benthic fauna of the eastern Chukchi Sea: U.S. Geological Survey Open-File Report 77-672, i, 112 p., https://doi.org/10.3133/ofr77672.","productDescription":"i, 112 p.","costCenters":[],"links":[{"id":426093,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0672/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411645,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14495.htm","linkFileType":{"id":5,"text":"html"}},{"id":144283,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0672/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"eastern Chukchi Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -156,\n              72.5\n            ],\n            [\n              -170,\n              72.5\n            ],\n            [\n              -170,\n              66.25\n            ],\n            [\n              -156,\n              66.25\n            ],\n            [\n              -156,\n              72.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698c55","contributors":{"authors":[{"text":"Mann, Dennis M.","contributorId":50528,"corporation":false,"usgs":true,"family":"Mann","given":"Dennis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30071,"text":"wri7788 - 1977 - Hydrology of Lake Panasoffkee, Sumter County, Florida","interactions":[],"lastModifiedDate":"2018-07-25T16:28:41","indexId":"wri7788","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-88","title":"Hydrology of Lake Panasoffkee, Sumter County, Florida","docAbstract":"<p>Lake Panasoffkee, in midwest Sumter County of central Florida, receives water from three creeks and discharges water through Outlet River at an average daily rate of 207 cubic feet per second. The eastern shore of the lake is marsh and wooded swamp with inflow to the lake coming from the northeast and southeast. About 15 percent of the basin contributes surface water to the lake and about 50 percent of the 420-square-mile topographic drainage basin contributes ground water to the lake. The water from the remainder of the basin either evaporates from low areas or directly recharges the Floridan aquifer for discharge outside the basin. The maximum stage on record is 44.28 feet above mean sea level and the minimum stage on record is 37.65 feet above. The lake level is partly affected by the Wysong Dam and has stabilized in recent years at about 40.95 feet above mean sea level. The quality of the water is generally good. The lake supports a favorably balanced fish population even though minor fish kills were reported in 1973 and 1974. These kills were probably the result of algal blooms.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7788","usgsCitation":"Taylor, G., 1977, Hydrology of Lake Panasoffkee, Sumter County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-88, 1 Plate: 37.03 x 26.10 inches, https://doi.org/10.3133/wri7788.","productDescription":"1 Plate: 37.03 x 26.10 inches","costCenters":[],"links":[{"id":160141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0088/report-thumb.jpg","linkFileType":{"id":1,"text":"pdf"}},{"id":355975,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0088/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Sumter County","otherGeospatial":"Lake Panasoffkee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.18597412109375,\n              28.75742632675056\n            ],\n            [\n              -82.06581115722656,\n              28.75742632675056\n            ],\n            [\n              -82.06581115722656,\n              28.87774838672653\n            ],\n            [\n              -82.18597412109375,\n              28.87774838672653\n            ],\n            [\n              -82.18597412109375,\n              28.75742632675056\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604738","contributors":{"authors":[{"text":"Taylor, G.F.","contributorId":6486,"corporation":false,"usgs":true,"family":"Taylor","given":"G.F.","email":"","affiliations":[],"preferred":false,"id":202624,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29487,"text":"wri7789 - 1977 - Hydrologic reconnaissance of Tsala Apopka Lake, Citrus County, Florida","interactions":[],"lastModifiedDate":"2019-07-22T10:19:52","indexId":"wri7789","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-89","title":"Hydrologic reconnaissance of Tsala Apopka Lake, Citrus County, Florida","docAbstract":"The swamps, marshes, and open waters of Tsala Apopka Lake, Florida, were mapped and the hydrologic connection between the lake and the Floridan limestone aquifer was studied from October 1975 to September 1976. Tsala Apopka Lake is a series of shallow , interconnected lakes, ponds, and marshes whose water surface slopes northward at 0.5 foot per mile. According to aerial photographs of December 1972, only 6 percent of the 103 square miles of study area is covered by open water. Open water is abundant along the western side of the lake, dense and sparse marshes occupy most of the lake area, and swamps occupy a thick zone around the Withlacoochee River which borders the lake to the east. Only a small fraction of the total surface flow occurs through the lake. The average lake outflow through S-351 canal is 23.6 cfs; while the average river flow at Holder is 714 cfs. Tsala Apopka Lake is hydraulically connected to the Floridan aquifer. At low flow, the major source of water in the river is ground water from the Floridan aquifer. The specific conductance of water in the Floridan aquifer averages 250-350 umho/cm (micromhos per centimeter) at 25C in this area. The specific conductance of water in the Withlacoochee River near Holder averages 268 umho/cm at 25C, while water in Tsala Apopka Lake at Hernando averages 139 umho/cm at 25C. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7789","usgsCitation":"Rutledge, A.T., 1977, Hydrologic reconnaissance of Tsala Apopka Lake, Citrus County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-89, 2 Plates: 37.40 x 27.79 inches and 37.92 x 28.06 inches, https://doi.org/10.3133/wri7789.","productDescription":"2 Plates: 37.40 x 27.79 inches and 37.92 x 28.06 inches","costCenters":[],"links":[{"id":365758,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0089/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0089/report-thumb.jpg"},{"id":365759,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0089/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Citrus County","otherGeospatial":"Tsala Apopka Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.70806884765625,\n              28.553163550610673\n            ],\n            [\n              -81.54327392578125,\n              28.553163550610673\n            ],\n            [\n              -81.54327392578125,\n              28.697815516328\n            ],\n            [\n              -81.70806884765625,\n              28.697815516328\n            ],\n            [\n              -81.70806884765625,\n              28.553163550610673\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88d7","contributors":{"authors":[{"text":"Rutledge, A. T.","contributorId":38532,"corporation":false,"usgs":true,"family":"Rutledge","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":201598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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