{"pageNumber":"378","pageRowStart":"9425","pageSize":"25","recordCount":11004,"records":[{"id":33288,"text":"b1440 - 1978 - A gravity study of the northern part of the Arctic National Wildlife Range, Alaska","interactions":[],"lastModifiedDate":"2016-12-20T14:25:32","indexId":"b1440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1440","title":"A gravity study of the northern part of the Arctic National Wildlife Range, Alaska","docAbstract":"<p>Interpretation of all publicly available onshore gravity data provides a basis for outlining regional elements of the basement and overlying structure in the northern part of the Arctic National Wildlife Range. Major post-Carboniferous sedimentary basins whose centers lie offshore on the Beaufort Shelf extend onshore in the northern part of the study area. There is strong evidence that dense basement rocks beneath these onshore extensions rise to relatively shallow depths along the northeast Alaskan coast. Geologic studies and interpretation of the gravity data indicate that the gross structural and stratigraphic framework of this area is similar to that of the Prudhoe Bay region to the west. </p><p>A high potential for petroleum accumulation in the Wildlife Range is indicated by the surface presence of oil seeps, oil sands, and outcrops of reservoir and source rocks along the southern margins of the onshore basinal areas. Present data suggest that the greatest potential for onshore accumulations of hydrocarbons lies in the area south and east of Barter Island and that possibilities exist there for commercially substantial reserves. The potential of this area cannot be fully assessed, however, until the subsurface extent of several major unconformities is known. Unfortunately, gravity data alone are of little use in such determinations. </p><p>South of the mountain front, large granitic intrusions are marked by a sharply defined gravity minimum. The subsurface distribution of these bodies could probably be mapped by detailed gravity surveys. Detailed aeromagnetic surveys should serve equally well for such a purpose.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1440","usgsCitation":"Kososki, B.A., Reiser, H.N., Cavit, C.D., and Detterman, R.L., 1978, A gravity study of the northern part of the Arctic National Wildlife Range, Alaska: U.S. Geological Survey Bulletin 1440, Report: iii, 21 p.; 3 Plates: 46.50 x 22.00 inches or smaller, https://doi.org/10.3133/b1440.","productDescription":"Report: iii, 21 p.; 3 Plates: 46.50 x 22.00 inches or smaller","costCenters":[],"links":[{"id":331286,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":61070,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1440/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61071,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1440/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61072,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1440/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61073,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1440/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Arctic National Wildlife Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147,\n              69\n            ],\n            [\n              -147,\n              70.5\n            ],\n            [\n              -141,\n              70.5\n            ],\n            [\n              -141,\n              69\n            ],\n            [\n              -147,\n              69\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae587","contributors":{"authors":[{"text":"Kososki, B. A.","contributorId":85182,"corporation":false,"usgs":true,"family":"Kososki","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":210362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiser, H. N.","contributorId":13199,"corporation":false,"usgs":true,"family":"Reiser","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":210359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cavit, C. D.","contributorId":20370,"corporation":false,"usgs":true,"family":"Cavit","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":210360,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Detterman, R. L.","contributorId":71525,"corporation":false,"usgs":true,"family":"Detterman","given":"R.","middleInitial":"L.","affiliations":[],"preferred":false,"id":210361,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":28940,"text":"wri7851 - 1978 - Physiography and surficial geology of the copper-nickel study region, northeastern Minnesota","interactions":[],"lastModifiedDate":"2024-01-08T22:28:23.652704","indexId":"wri7851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-51","title":"Physiography and surficial geology of the copper-nickel study region, northeastern Minnesota","docAbstract":"<p>The Copper-Nickel study region lies in the Superior Upland physiographic province and is located approximately 60 miles north of Duluth and 100 miles southeast of International Falls, Minnesota. It straddles the Laurentian Divide, which separates Hudson Bay and Lake Superior drainage. The topography exhibits a southwesterly trending lineation that parallels the strike of southeastward-dipping bedrock units and the southwestward direction of ice movement during Pleistocene glaciation. For this study, the region has been divided into seven physiographic areas based on geomorphic features related to the bedrock surface, glacial deposits, and hydrogeologic significance.</p>\n<p>The surficial geology is largely a result of two southwestward advances of the Rainy Lobe of the Laurentian ice sheet. The Toimi Drumlin Field, the oldest glacial deposit, covers much of the southern part of the region. It is bounded on the north by the Vermilion Moraine Complex, an east-west trending series of terminal and recessional moraines that mark the southerly extent of the second advance of the Rainy Lobe. Thin ground moraine and small outwash deposits occur both within and north of the Vermilion Moraine Complex except in the Embarrass and Dunka River basins where outwash deposits up to 200 feet in thickness fill a deep bedrock valley.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri7851","collaboration":"Prepared in cooperation with Minnesota Environmental Quality Board Copper-Nickel Study Staff","usgsCitation":"Olcott, P.G., and Siegel, D.I., 1978, Physiography and surficial geology of the copper-nickel study region, northeastern Minnesota: U.S. Geological Survey Water-Resources Investigations Report 78-51, Document: iv, 22 p.; 3 Plates: 20.99 x 25.11 inches or smaller, https://doi.org/10.3133/wri7851.","productDescription":"Document: iv, 22 p.; 3 Plates: 20.99 x 25.11 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":424201,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35256.htm","linkFileType":{"id":5,"text":"html"}},{"id":95737,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0051/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95735,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0051/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95734,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158311,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0051/report-thumb.jpg"},{"id":95736,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0051/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.25,\n              47.75\n            ],\n            [\n              -91.916667,\n              47.75\n            ],\n            [\n              -91.75,\n              47.916667\n            ],\n            [\n              -91.5,\n              47.77\n            ],\n            [\n              -91.5,\n              47.5\n            ],\n            [\n              -91.75,\n              47.5\n            ],\n            [\n              -91.75,\n              47.25\n            ],\n            [\n              -92.25,\n              47.25\n            ],\n            [\n              -92.25,\n              47.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685996","contributors":{"authors":[{"text":"Olcott, P. G.","contributorId":79903,"corporation":false,"usgs":true,"family":"Olcott","given":"P.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siegel, D. I.","contributorId":77562,"corporation":false,"usgs":true,"family":"Siegel","given":"D.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":200650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46083,"text":"ofr78937 - 1978 - Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1978","interactions":[],"lastModifiedDate":"2022-01-03T22:22:13.733594","indexId":"ofr78937","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-937","title":"Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1978","docAbstract":"The U.S. Geological Survey has released to the open file a map showing ground-water subunits and areas, and depth to water for spring 1978, in the Antelope Valley-East Kern Water Agency area, California.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78937","usgsCitation":"Blankenbaker, G.G., 1978, Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1978: U.S. Geological Survey Open-File Report 78-937, 1 Plate: 43.00 × 41.00 inches, https://doi.org/10.3133/ofr78937.","productDescription":"1 Plate: 43.00 × 41.00 inches","costCenters":[],"links":[{"id":162625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393811,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14962.htm"},{"id":99640,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0937/plate-1.pdf","size":"8956","linkFileType":{"id":1,"text":"pdf"}}],"scale":"124000","country":"United States","state":"California","otherGeospatial":"Antelope Valley - East Kern Water Agency area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.75,\n              34.4260\n            ],\n            [\n              -117.655,\n              34.4260\n            ],\n            [\n              -117.655,\n              35.3610\n            ],\n            [\n              -118.75,\n              35.3610\n            ],\n            [\n              -118.75,\n              34.4260\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b45f","contributors":{"authors":[{"text":"Blankenbaker, G. G.","contributorId":17993,"corporation":false,"usgs":true,"family":"Blankenbaker","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":232589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28240,"text":"wri7861 - 1978 - Maps showing ground-water conditions in the eastern part of the Salt River Valley area, Maricopa and Pinal counties, Arizona, 1976","interactions":[],"lastModifiedDate":"2019-07-23T15:34:27","indexId":"wri7861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-61","title":"Maps showing ground-water conditions in the eastern part of the Salt River Valley area, Maricopa and Pinal counties, Arizona, 1976","docAbstract":"In 1976 about 1.68 million acre-feet of ground water was pumped in the Salt River Valley, Ariz. Since 1923, more than 73 million acre-feet has been withdrawn, which has resulted in a general decline in water levels. Water levels in the eastern part of the Salt River Valley area have declined as much as 420 feet. Information on the maps includes altitude of the water level, depth to water, change in water level (1923-76), and irrigated area. Hydrographs of the water level in selected wells, a table of historical pumpage, and a brief discussion of the chemical quality of the ground water are included also. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7861","usgsCitation":"Laney, R., Ross, P.P., and Littin, G.R., 1978, Maps showing ground-water conditions in the eastern part of the Salt River Valley area, Maricopa and Pinal counties, Arizona, 1976: U.S. Geological Survey Water-Resources Investigations Report 78-61, 2 Plates: 38.06 x 30.85 inches and 38.36 x 30.93 inches, https://doi.org/10.3133/wri7861.","productDescription":"2 Plates: 38.06 x 30.85 inches and 38.36 x 30.93 inches","costCenters":[],"links":[{"id":365897,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0061/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365898,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0061/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0061/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Maricopa County, Pinal County","otherGeospatial":"Salt River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.27752685546875,\n              33.38501292737507\n            ],\n            [\n              -111.81198120117188,\n              33.38501292737507\n            ],\n            [\n              -111.81198120117188,\n              33.45321401062559\n            ],\n            [\n              -112.27752685546875,\n              33.45321401062559\n            ],\n            [\n              -112.27752685546875,\n              33.38501292737507\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6059fb","contributors":{"authors":[{"text":"Laney, R. L.","contributorId":83889,"corporation":false,"usgs":true,"family":"Laney","given":"R. L.","affiliations":[],"preferred":false,"id":199448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, P. P.","contributorId":78742,"corporation":false,"usgs":true,"family":"Ross","given":"P.","middleInitial":"P.","affiliations":[],"preferred":false,"id":199447,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Littin, G. R.","contributorId":95924,"corporation":false,"usgs":true,"family":"Littin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199449,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7348,"text":"ofr78596 - 1978 - Mineral resources of the Rincon wilderness study area, Pima County, Arizona","interactions":[{"subject":{"id":7348,"text":"ofr78596 - 1978 - Mineral resources of the Rincon wilderness study area, Pima County, Arizona","indexId":"ofr78596","publicationYear":"1978","noYear":false,"title":"Mineral resources of the Rincon wilderness study area, Pima County, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":33444,"text":"b1500 - 1981 - Mineral resources of the Rincon wilderness study area, Pima County, Arizona","indexId":"b1500","publicationYear":"1981","noYear":false,"title":"Mineral resources of the Rincon wilderness study area, Pima County, Arizona"},"id":1}],"supersededBy":{"id":33444,"text":"b1500 - 1981 - Mineral resources of the Rincon wilderness study area, Pima County, Arizona","indexId":"b1500","publicationYear":"1981","noYear":false,"title":"Mineral resources of the Rincon wilderness study area, Pima County, Arizona"},"lastModifiedDate":"2023-02-22T20:14:10.180388","indexId":"ofr78596","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-596","title":"Mineral resources of the Rincon wilderness study area, Pima County, Arizona","docAbstract":"<p>The Rincon wilderness study area comprises about 254 km<sup>2</sup> (98 mi<sup>2</sup>) of the Rincon Mountains 15-30 km (10-20 mi) east of Tucson, Arizona. The area lies within the Coronado National Forest and forms a belt around the north, east, and south sides of the Saguaro National Monument (fig. 1). A mineral resource survey was made of the area in 1977 by the U.S. Geological Survey and the U.S. Bureau of Mines. This study indicates that the potential for finding metallic or nonmetallic mineral deposits, petroleum or coal or geothermal energy in the study area is low. This appraisal is based on geologic and geochemical investigations and on examination of all mineralized prospects. A geologic map was made of the area and its immediate surrounding. Chemical and spectrographic analyses were made of 1.30 stream-sediment samples and of 143 rock samples. The locations of mining claims were compiled and samples from most of the claims were assayed. There has been no recorded mineral production from within the study area.</p><p>The geology of the Rincon Mountains is structurally complex. The core of the Rincon Mountains, lying mainly within the Saguaro National Monument, is underlain by igneous and metamorphic rocks chiefly of Precambrian and Tertiary ages. The study area lies on the flanks of the mountains in a terrain of sedimentary, metamorphic, and igneous rocks mainly of Precambrian through mid-Tertiary age. The rocks of this area are cut by many faults, with low-angle or bedding-parallel faults abundant. the distribution of these faulted rocks around the flanks of the Rincon Mountains is the result of a doming in the core area, the sliding of rock masses from the high part of the dome down its flanks, and to the effects of erosion.</p><p>The potential for economic metallic mineral deposits is considered low because the known areas of anomalous concentrations of metals are small and the concentration of metals weak and erratic. The surface signs of mineralization are largely restricted to 4 locales in which some prospects exist (fig. 1): (1) east of Colossal Cave, southwest or the Rincon Mountains, (2) north of Happy Valley, east of the mountains, (3) between Roble and Youtcy Canyons, northeast of the mountains, and (4) near Italian Trap north of the mountains. Very little primary sulfide mineralization is present and signs of alteration are restricted to narrow zones along faults and fractures. The geochemical anomalies are weak. The sites at which anomalous values of copper, molybdenum, or silver were obtained are mainly controlled by faults.</p><p>Nonmetallic mineral resources occur in deposits that are too small and too remote to be economically attractive. Sand and gravel deposits in the main drainages are similar to larger deposits that occur closer to nearby highways and cities. Limestone and marble present in some of the metamorphic rocks are too impure and too broken for use as dimension stone. Use of this marble as decorative rock is limited by remote markets. Limestone suitable for making cement is not likely to be found in large quantities within the Rincon wilderness study area. Closely spaced fractures in the granitic rocks makes them of little value for building stone.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78596","collaboration":"Prepared in cooperation with the U.S. Bureau of Mines","usgsCitation":"Thorman, C.H., Drewes, H., and Lane, M., 1978, Mineral resources of the Rincon wilderness study area, Pima County, Arizona: U.S. Geological Survey Open-File Report 78-596, iii, 58 p., https://doi.org/10.3133/ofr78596.","productDescription":"iii, 58 p.","costCenters":[],"links":[{"id":413305,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0596/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140150,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0596/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Pima County","otherGeospatial":"Rincon wilderness study area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.76135252193272,\n              32.26816566918097\n            ],\n            [\n              -110.76135252193272,\n              32.088986940125736\n            ],\n            [\n              -110.3780838038202,\n              32.088986940125736\n            ],\n            [\n              -110.3780838038202,\n              32.26816566918097\n            ],\n            [\n              -110.76135252193272,\n              32.26816566918097\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8f5f","contributors":{"authors":[{"text":"Thorman, Charles H. cthorman@usgs.gov","contributorId":254,"corporation":false,"usgs":false,"family":"Thorman","given":"Charles","email":"cthorman@usgs.gov","middleInitial":"H.","affiliations":[{"id":7065,"text":"USGS emeritus","active":true,"usgs":false}],"preferred":false,"id":155357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drewes, Harald","contributorId":52567,"corporation":false,"usgs":true,"family":"Drewes","given":"Harald","affiliations":[],"preferred":false,"id":155359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, Michael","contributorId":39756,"corporation":false,"usgs":true,"family":"Lane","given":"Michael","affiliations":[],"preferred":false,"id":155358,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28609,"text":"wri7845 - 1978 - Ground-water quality near the northwest 58th Street solid-waste disposal facility, Dade County, Florida","interactions":[],"lastModifiedDate":"2019-07-23T11:48:55","indexId":"wri7845","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-45","title":"Ground-water quality near the northwest 58th Street solid-waste disposal facility, Dade County, Florida","docAbstract":"The Northwest 58th Street solid-waste disposal facility, 3 miles west of a major Dade County municipal water-supply well field, overlays the Biscayne aquifer, a permeable, solution-riddled limestone which transmits leachates eastward at a calculated rate of 2.9 feet per day. A discrete, identifiable leachate plume has been recognized under and downgradient from the waste disposal facility. Concentrations of sodium, ammonia, and dissolved solids decreased with depth beneath the disposal area and downgradient in response to an advective and convective dispersion. At a distance of about one-half downgradient, the rate of contribution of leachate from the source to the leading edge of the plume was about equal to the rate of loss of leachate from the leading edge of the plume by diffusion and dilution by rainfall infiltration during the period August 1973 - July 1975. Heavy metals and pesticides are filtered, adsorbed by aquifer materials, or are precipitated near the disposal area. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7845","usgsCitation":"Mattraw, H.C., Hull, J.E., and Klein, H., 1978, Ground-water quality near the northwest 58th Street solid-waste disposal facility, Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 78-45, vi, 61 p. , https://doi.org/10.3133/wri7845.","productDescription":"vi, 61 p. ","costCenters":[],"links":[{"id":159071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0045/report-thumb.jpg"},{"id":365858,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Dade County","otherGeospatial":"58th Street solid-waste disposal facility","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.33880650997162,\n              25.826282502041245\n            ],\n            [\n              -80.33802598714828,\n              25.826282502041245\n            ],\n            [\n              -80.33802598714828,\n              25.82660601878737\n            ],\n            [\n              -80.33880650997162,\n              25.82660601878737\n            ],\n            [\n              -80.33880650997162,\n              25.826282502041245\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697556","contributors":{"authors":[{"text":"Mattraw, H. C. Jr.","contributorId":21996,"corporation":false,"usgs":true,"family":"Mattraw","given":"H.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":200111,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hull, John E.","contributorId":15616,"corporation":false,"usgs":true,"family":"Hull","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klein, Howard","contributorId":62189,"corporation":false,"usgs":true,"family":"Klein","given":"Howard","email":"","affiliations":[],"preferred":false,"id":200112,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8656,"text":"ofr78559 - 1978 - Analyses of rock samples from the Hunt Fork Shale and related Upper Devonian rocks, Philip Smith Quadrangle, Arctic Alaska","interactions":[],"lastModifiedDate":"2023-09-08T17:40:41.209035","indexId":"ofr78559","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-559","title":"Analyses of rock samples from the Hunt Fork Shale and related Upper Devonian rocks, Philip Smith Quadrangle, Arctic Alaska","docAbstract":"<p>More than 1400 m of fine-grained clastic rocks and reefoid limestones constitute the lower part of an Upper Devonian transgressive-regressive cycle in the central Brooks Range, Alaska (Dutro and others, 1977). The Hunt Fork Shale and an underlying heterogeneous unit (unnamed) were measured and sampled on the east side of the upper Beaucoup Creek in the Philip Smith Mountains A-1 quadrangle (secs. 17, 19, and 20, T. 14 S.,<br>R. 20 E.) (Brosge and others, 1977).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78559","usgsCitation":"Dutro, J.T., and Detra, D.E., 1978, Analyses of rock samples from the Hunt Fork Shale and related Upper Devonian rocks, Philip Smith Quadrangle, Arctic Alaska: U.S. Geological Survey Open-File Report 78-559, 7 p., https://doi.org/10.3133/ofr78559.","productDescription":"7 p.","costCenters":[],"links":[{"id":420669,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0559/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141135,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0559/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Philip Smith Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -150,\n              68\n            ],\n            [\n              -147,\n              68\n            ],\n            [\n              -147,\n              69\n            ],\n            [\n              -150,\n              69\n            ],\n            [\n              -150,\n              68\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680f2f","contributors":{"authors":[{"text":"Dutro, J. Thomas","contributorId":54204,"corporation":false,"usgs":true,"family":"Dutro","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":158099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detra, David E.","contributorId":17342,"corporation":false,"usgs":true,"family":"Detra","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":158100,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28358,"text":"wri787 - 1978 - A rainfall-runoff modeling procedure for improving estimates of T-year (annual) floods for small drainage basins","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri787","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-7","title":"A rainfall-runoff modeling procedure for improving estimates of T-year (annual) floods for small drainage basins","docAbstract":"Maps depicting the influence of a climatic factor, C, on the magnitude of synthetic T-year (annual) floods were prepared for a large portion of the eastern United States. The climatic factors were developed by regression analysis of flood data using a parametric rainfall-runoff model and long-term rainfall records. Map estimates of C values and calibrated values of rainfall-runoff model parameters were used as variables in a synthetic T-year flood relation to compute ' map-model ' flood estimates for 98 small drainage basins in a six-state study area. Improved estimates of T-year floods were computed as a weighted average of the map-model estimate and an observed estimate, with the weights proportional to the relative accuracies of the two estimates. The accuracy of the map-model estimates was appraised by decomposing components of variance into average time-sampling error associated with the observed estimates and average map-model error. Map-model estimates have an accuracy, in terms of equivalent length of observed record, that ranges from 6 years for the 1.25-year flood up to 30 years for the 50- and 100-year flood. (Woodard-USGS)","language":"ENGLISH","publisher":"Geological Survey, Water Resources Division,","doi":"10.3133/wri787","usgsCitation":"Lichty, R.W., and Liscum, F., 1978, A rainfall-runoff modeling procedure for improving estimates of T-year (annual) floods for small drainage basins: U.S. Geological Survey Water-Resources Investigations Report 78-7, iv, 44 p. :ill., maps ;27 cm., https://doi.org/10.3133/wri787.","productDescription":"iv, 44 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":123294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0007/report-thumb.jpg"},{"id":57162,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a870a","contributors":{"authors":[{"text":"Lichty, Robert W.","contributorId":7697,"corporation":false,"usgs":true,"family":"Lichty","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liscum, Fred","contributorId":95463,"corporation":false,"usgs":true,"family":"Liscum","given":"Fred","email":"","affiliations":[],"preferred":false,"id":199661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10976,"text":"ofr78351 - 1978 - Biostratigraphic guide to Upper Devonian and Mississippian rocks along the Wasatch Front and Cordilleran hingeline, Utah","interactions":[],"lastModifiedDate":"2023-02-17T21:31:29.746195","indexId":"ofr78351","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-351","title":"Biostratigraphic guide to Upper Devonian and Mississippian rocks along the Wasatch Front and Cordilleran hingeline, Utah","docAbstract":"<p>This paper provides a guide to measured sections of Upper Devonian (Famennian) and Mississippian (Kinderhookian, Osagean, and Meramecian) rocks visited on a three-day field trip between Provo, Utah, on the Wasatch Front and the Crawford Mountains in the Overthrust Belt along the Utah-Wyoming State line. The field trip, sponsored by the Pander Society, was held on April 30-May 2, 1978 in conjunction with the meeting of the Rocky Mountain section of the Geological Society of America at Provo, Utah. The rocks that may be sampled for conodonts are represented by the Middle to Upper <i>Scaphignathus velifer</i> (middle Famennian) through <i>Cavusgnathus</i> (middle Meramecian) conodont Zones. The measured sections and field trip provide a west to east traverse of the Sevier thrust system. The sections demonstrate the biostratigraphic, paleogeographic, and sedimentational differences among equivalent Famennian rocks as well as the transition from the Osagean and early Meramecian starved phosphatic basin on the west to time-equivalent carbonate rocks of the shelf margin on the east.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78351","usgsCitation":"Sandberg, C.A., and Gutschick, R., 1978, Biostratigraphic guide to Upper Devonian and Mississippian rocks along the Wasatch Front and Cordilleran hingeline, Utah: U.S. Geological Survey Open-File Report 78-351, 52 p., https://doi.org/10.3133/ofr78351.","productDescription":"52 p.","costCenters":[],"links":[{"id":413196,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0351/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143011,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0351/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a45e4b07f02db621001","contributors":{"authors":[{"text":"Sandberg, Charles A. sandberg@usgs.gov","contributorId":2362,"corporation":false,"usgs":true,"family":"Sandberg","given":"Charles","email":"sandberg@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":162309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gutschick, Raymond","contributorId":74003,"corporation":false,"usgs":true,"family":"Gutschick","given":"Raymond","affiliations":[],"preferred":false,"id":162310,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7341,"text":"ofr781091 - 1978 - Mineral resources of the Craggy Mountain Wilderness Study Area, Buncombe County, North Carolina","interactions":[{"subject":{"id":7341,"text":"ofr781091 - 1978 - Mineral resources of the Craggy Mountain Wilderness Study Area, Buncombe County, North Carolina","indexId":"ofr781091","publicationYear":"1978","noYear":false,"title":"Mineral resources of the Craggy Mountain Wilderness Study Area, Buncombe County, North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":33371,"text":"b1515 - 1982 - Mineral resources of the Craggy Mountain wilderness study area and extension, Buncombe County, North Carolina","indexId":"b1515","publicationYear":"1982","noYear":false,"title":"Mineral resources of the Craggy Mountain wilderness study area and extension, Buncombe County, North Carolina"},"id":1}],"supersededBy":{"id":33371,"text":"b1515 - 1982 - Mineral resources of the Craggy Mountain wilderness study area and extension, Buncombe County, North Carolina","indexId":"b1515","publicationYear":"1982","noYear":false,"title":"Mineral resources of the Craggy Mountain wilderness study area and extension, Buncombe County, North Carolina"},"lastModifiedDate":"2023-03-13T18:49:23.936158","indexId":"ofr781091","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-1091","title":"Mineral resources of the Craggy Mountain Wilderness Study Area, Buncombe County, North Carolina","docAbstract":"<p>The Craggy Mountain Wilderness Study Area covers about 550 hectares of the Pisgah National Forest in the Blue Ridge Mountains of western North Carolina (fig. 1). The area is 21 km northeast of Asheville, Buncombe County, N.C., and 11 km southwest of Mount Mitchell, the highest point in eastern North America. The study area is bounded on the southeast by the Blue Ridge Parkway, on the northeast by Bullhead Ridge, and on the southwest and west by Big Fork Ridge (Plate 1b). It includes all of the Craggy Mountain scenic area established by the Forest Service in 1961 and some additional land west of Bearwallow Branch and along the middle part of Carter Creek for a short distance beyond the mouth of Peach Orchard Creek.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781091","usgsCitation":"Lesure, F.G., Grosz, A.E., Williams, B.B., and Gazdik, G., 1978, Mineral resources of the Craggy Mountain Wilderness Study Area, Buncombe County, North Carolina: U.S. Geological Survey Open-File Report 78-1091, Report: iii, 23 p.; 1 Plate: 31.17 x 28.59 inches, https://doi.org/10.3133/ofr781091.","productDescription":"Report: iii, 23 p.; 1 Plate: 31.17 x 28.59 inches","costCenters":[],"links":[{"id":140133,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1091/report-thumb.jpg"},{"id":414021,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1091/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414020,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","county":"Buncombe County","otherGeospatial":"Craggy Mountain Wilderness Study Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.416667,35.683333 ], [ -82.416667,35.75 ], [ -82.35,35.75 ], [ -82.35,35.683333 ], [ -82.416667,35.683333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db657f40","contributors":{"authors":[{"text":"Lesure, Frank Gardner","contributorId":70752,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"Gardner","affiliations":[],"preferred":false,"id":155314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grosz, A. E.","contributorId":87925,"corporation":false,"usgs":true,"family":"Grosz","given":"A.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, B. B.","contributorId":106488,"corporation":false,"usgs":true,"family":"Williams","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":155317,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gazdik, Gertrude C.","contributorId":76736,"corporation":false,"usgs":true,"family":"Gazdik","given":"Gertrude C.","affiliations":[],"preferred":false,"id":155315,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9912,"text":"ofr78691 - 1978 - Geology of the Arco-Big Southern Butte area, eastern Snake River Plain, and potential volcanic hazards to the radioactive waste management complex, and other waste storage and reactor facilities at the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2022-01-05T22:21:56.455564","indexId":"ofr78691","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-691","title":"Geology of the Arco-Big Southern Butte area, eastern Snake River Plain, and potential volcanic hazards to the radioactive waste management complex, and other waste storage and reactor facilities at the Idaho National Engineering Laboratory, Idaho","docAbstract":"The Arco-Big Southern Butte area of the eastern Snake River Plain, Idaho, includes a volcanic rift zone and more than 70 Holocene and late Quaternary basalt volcanoes. The Arco volcanic rift zone extends southeast for 50 km from Arco to about 10 km southeast of Big Southern Butte. The rift zone is the locus of extensional faults, graben, fissure basaltic volcanic vents, several rhyolite domes at Big Southern Butte, and a ferrolatite volcano at Cedar Butte. Limited radiometric age data and geological field criteria suggest that all volcanism in the area is younger than 700,000 years; at least 67 separate basaltic eruptions are estimated to have occurred within the last 200,000 years. The average volcanic recurrence interval for the Arco-Big Southern Butte area is approximately one eruption per 3,000 years. \r\n\r\nRadioactive waste storage and reactor facilities at the Idaho National Engineering Laboratory may be subject to potential volcanic hazards. The geologic history and inferred past volcanic events in the Arco-Big Southern Butte area provide a basis for assessing the volcanic hazard. It is recommended that a radiometric age-dating study be performed on rocks in cored drill holes to provide a more precise estimate of the eruption recurrence interval for the region surrounding and including the Radioactive Waste Management Complex. It is also recommended that several geophysical monitoring systems (dry tilt and seismic) be installed to provide adequate warning of future volcanic eruptions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78691","usgsCitation":"Kuntz, M., and Kork, J.O., 1978, Geology of the Arco-Big Southern Butte area, eastern Snake River Plain, and potential volcanic hazards to the radioactive waste management complex, and other waste storage and reactor facilities at the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Open-File Report 78-691, v, 70 p., https://doi.org/10.3133/ofr78691.","productDescription":"v, 70 p.","costCenters":[],"links":[{"id":393943,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74923.htm"},{"id":37702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0691/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0691/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Arco-Big Southern Butte area,  eastern Snake River Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.8139,\n              43\n            ],\n            [\n              -112.3833,\n              43\n            ],\n            [\n              -112.3833,\n              44.3069\n            ],\n            [\n              -112.8139,\n              44.3069\n            ],\n            [\n              -112.8139,\n              43\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6833ff","contributors":{"authors":[{"text":"Kuntz, Mel A. 0000-0001-8828-5474","orcid":"https://orcid.org/0000-0001-8828-5474","contributorId":6446,"corporation":false,"usgs":true,"family":"Kuntz","given":"Mel A.","affiliations":[],"preferred":false,"id":160499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kork, John O.","contributorId":20323,"corporation":false,"usgs":true,"family":"Kork","given":"John","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":160500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18298,"text":"ofr78963 - 1978 - Floods of July 19-20, 1977 in the Johnstown area, western Pennsylvania","interactions":[],"lastModifiedDate":"2019-12-27T11:57:22","indexId":"ofr78963","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-963","title":"Floods of July 19-20, 1977 in the Johnstown area, western Pennsylvania","docAbstract":"Intense rainfall on the evening of July 19 and early morning hours of July 20, 1977, resulted in moderate to record flooding throughout much of an eight-county area of southwest Pennsylvania. In a 400-square-mile area directly north and east of Johnstown, rainfall totals of 6 to 12 inches were measured in a six to eight-hour period. Flood peaks having recurrence intervals greater than 100 years were recorded at several sites, primarily in the Conemaugh River basin. Runoff rates were as high as 2,390 cubic feet per second per square mile, in a 5.86-square-mile drainage area in the Little Conemaugh River basin. The Conemaugh River at Seward, which drains 715 square miles, had a peak discharge of 161 cubic feet per second per square mile. The flood waters claimed at least 78 lives and caused total losses in excess of $300 million. Also, seven earthfill dams, used mainly for water supply in the Johnstown area, failed. This report describes the storm and the associated flooding. A tabulation of peak gage heights and discharges for the July 1977 flood and for the maximum flood previously known is included for 57 sites. Data pertaining to the dams that failed are included also. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr78963","collaboration":"Prepared in cooperation with the Pennsylvania.Department of  Environmental Resources and the U. S. Army Corps of Engineers.  Pittsburgh District","usgsCitation":"Brua, S.A., 1978, Floods of July 19-20, 1977 in the Johnstown area, western Pennsylvania: U.S. Geological Survey Open-File Report 78-963, viii, 62 p., https://doi.org/10.3133/ofr78963.","productDescription":"viii, 62 p.","numberOfPages":"72","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":151758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0963/report-thumb.jpg"},{"id":279466,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0963/report.pdf"}],"country":"United States","state":"Pennsylvania","city":"Johnstown","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.02122497558594,\n              40.27350122374328\n            ],\n            [\n              -78.80870819091797,\n              40.27350122374328\n            ],\n            [\n              -78.80870819091797,\n              40.37427447537182\n            ],\n            [\n              -79.02122497558594,\n              40.37427447537182\n            ],\n            [\n              -79.02122497558594,\n              40.27350122374328\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfb74","contributors":{"authors":[{"text":"Brua, Stan A.","contributorId":58292,"corporation":false,"usgs":true,"family":"Brua","given":"Stan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":178872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30051,"text":"wri7819 - 1978 - Stream quality in the San Lorenzo River Basin, Santa Cruz County, California","interactions":[],"lastModifiedDate":"2020-08-12T19:15:46.213443","indexId":"wri7819","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-19","title":"Stream quality in the San Lorenzo River Basin, Santa Cruz County, California","docAbstract":"<p><span>Stream quality in the San Lorenzo River basin, Calif., was studied from </span><span>November 1973 through June 1975 to determine areal and temporal variations in </span><span>water quality, problem areas and times of water quality degradation, and </span><span>compliance with State and local water-quality objectives. Sampling from </span><span>November 1973 through July 1974 was done at five stations in the Zayante Creek </span><span>drainage basin and at one station on the San Lorenzo River at Big Trees. </span><span>Sampling from August 1974 through June 1975 was done at 15 stations in the San </span><span>Lorenzo River basin, including one station in the Zayante Creek subbasin. </span><span>Properties and constituents measured were water temperature, specific </span><span>conductance, pH, alkalinity, dissolved oxygen, turbidity, fecal-coliform and </span><span>fecal-streptococcal bacteria, major dissolved ions, nutrients (nitrogen and </span><span>phosphorus), chemical and biochemical oxygen demand, and trace elements. </span><span>Benthic invertebrates were collected during autumn 1974 and spring 1975 at two </span><span>stations.</span></p><p><span>Results show that the water in most streams in the basin can be classified as calcium bicarbonate, but based on the dissolved-ion concentrations the basin can be divided into three water-quality areas that correspond generally to three geologic areas. The most pronounced change in water quality occurs during storms when streamflow, turbidity, and total Kjeldahl-nitrogen, total-phosphorus, dissolved-potassium, and fecal-coliform concentrations increase, while concentrations of most dissolved ions decrease owing to dilution of the nonstorm part of the flow. Late winter and early spring nonstorm flows yield water of the best quality because the concentrations of most dissolved ions and fecal-coliform and fecal-streptococcal bacteria are relatively low, whereas turbidity values are the same as, or not appreciably greater than, during the summer low-flow period. </span></p><p><span>Dissolved-ion concentrations exceeded objectives at stations on east-side streams north of the Zayante fault, probably because of lower-than-normal streamflows during water year 1975. Total-nitrogen and fecal-coliform concentrations exceeded objectives in the Zayante Creek and Branciforte Creek drainage basins, probably because of domestic sewage from improperly operating septic-tank systems. The high total-nitrogen and fecal-coliform concentrations in the Zayante Creek basin might also result from the primary-treated effluent discharged by the city of Scotts Valley into an old sand pit. </span></p><p><span>Results of diel studies (intensive sampling for a 24-hour period) made at two stations on the San Lorenzo River indicate that residential areas between the stations do not contribute sufficient quantities of oxygen-demanding wastes to the river during low streamflow to cause appreciable dissolved-oxygen depletion. Greater streamflows and residential development seem to be responsible for unstable streambed substrates and reduced diversity of benthic invertebrates during the spring at a station downstream of most of the residential areas in the San Lorenzo River valley. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7819","collaboration":"Prepared in cooperation with the Santa Cruz Flood Control and Water Conservation District","usgsCitation":"Sylvester, M.A., and Covay, K.J., 1978, Stream quality in the San Lorenzo River Basin, Santa Cruz County, California: U.S. Geological Survey Water-Resources Investigations Report 78-19, v, 61 p., https://doi.org/10.3133/wri7819.","productDescription":"v, 61 p.","costCenters":[],"links":[{"id":377418,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0019/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0019/report-thumb.jpg"}],"country":"United States","state":"California","county":"Santa Cruz County","otherGeospatial":"San Lorenzo River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.18333333,\n              36.91666667\n            ],\n            [\n              -121.98333333,\n              36.91666667\n            ],\n            [\n              -121.98333333,\n              37.25\n            ],\n            [\n              -122.18333333,\n              37.25\n            ],\n            [\n              -122.18333333,\n              36.91666667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a5100","contributors":{"authors":[{"text":"Sylvester, Marc A.","contributorId":90706,"corporation":false,"usgs":true,"family":"Sylvester","given":"Marc","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Covay, Kenneth J.","contributorId":61865,"corporation":false,"usgs":true,"family":"Covay","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202596,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10223,"text":"ofr78377 - 1978 - Pennsylvanian (Upper Carboniferous) system of Wyoming","interactions":[],"lastModifiedDate":"2023-02-17T20:53:18.558114","indexId":"ofr78377","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-377","title":"Pennsylvanian (Upper Carboniferous) system of Wyoming","docAbstract":"<p>Pennsylvanian rocks in Wyoming comprise two stratigraphic sequences bounded by regional unconformities. Red mudstone and limestone characterize the strata in the lower sequence, and sandstone and dolomite characterize the strata in the upper sequence. Initial deposits of the lower sequence are-red mudstone probably of no older age than about middle Morrowan, except in the subsurface of southwestern Wyoming where early Morrowan strata may be present. The basal red mudstone lies unconformably upon Mississippian strata except in the vicinity of the ancestral Rocky Mountain Front Range where they lie upon Precambrian rocks. The red beds grade upward to interbedded limestone and mudstone of late Morrowan and early Atokan age; but the limestone strata are absent at many places because of beveling on a Middle Pennsylvanian erosional surface.</p><p>Initial deposits of the upper sequence are heterogeneous and locally may be thinly bedded red, green, or varicolored mudstone, sandstone, or dolomite of late Atokan to early Des Moinesian age. Basal strata of the upper sequence lie unconformably upon lower Pennsylvanian strata at most places in Wyoming; but locally, where the lower Pennsylvanian strata are absent by erosion or possibly by nondeposition, the upper sequence lies upon Mississippian rocks. The upper sequence in central and northwestern Wyoming comprises mostly dolomite in the lower part but grades upward into mostly sandstone no younger than Des Moinesian. The upper sequence in eastern Wyoming comprises sandstone and dolomite about equally and also includes Upper Pennsylvanian strata as young as Virgilian. Upper Pennsylvanian strata also occur as part of the upper sequence in the thrust belt in western Wyoming. Pennsylvanian strata terminate upward at an erosional unconformity beneath Permian rocks everywhere in Wyoming.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78377","usgsCitation":"Maughan, E.K., 1978, Pennsylvanian (Upper Carboniferous) system of Wyoming: U.S. Geological Survey Open-File Report 78-377, 32 p., https://doi.org/10.3133/ofr78377.","productDescription":"32 p.","costCenters":[],"links":[{"id":144177,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0377/report-thumb.jpg"},{"id":413181,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0377/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-110.048476,40.997555],[-110.121639,40.997101],[-110.125709,40.99655],[-110.237848,40.995427],[-110.250709,40.996089],[-110.375714,40.994947],[-110.500718,40.994746],[-110.539819,40.996346],[-110.715026,40.996347],[-110.750727,40.996847],[-111.046723,40.997959],[-111.046551,41.251716],[-111.0466,41.360692],[-111.046264,41.377731],[-111.045789,41.565571],[-111.045818,41.579845],[-111.046689,42.001567],[-111.047109,42.142497],[-111.047107,42.148971],[-111.047058,42.182672],[-111.047097,42.194773],[-111.047074,42.280787],[-111.04708,42.34942],[-111.046801,42.504946],[-111.046719,42.513118],[-111.046017,42.582723],[-111.043564,42.722624],[-111.044135,42.874924],[-111.043959,42.96445],[-111.043957,42.969482],[-111.043924,42.975063],[-111.044129,43.018702],[-111.044156,43.020052],[-111.044206,43.022614],[-111.044034,43.024581],[-111.044034,43.024844],[-111.044033,43.026411],[-111.044094,43.02927],[-111.043997,43.041415],[-111.044058,43.04464],[-111.044063,43.046302],[-111.044086,43.054819],[-111.044117,43.060309],[-111.04415,43.066172],[-111.044162,43.068222],[-111.044143,43.072364],[-111.044235,43.177121],[-111.044266,43.177236],[-111.044232,43.18444],[-111.044168,43.189244],[-111.044229,43.195579],[-111.044617,43.31572],[-111.045205,43.501136],[-111.045706,43.659112],[-111.04588,43.681033],[-111.046118,43.684902],[-111.046051,43.685812],[-111.04611,43.687848],[-111.046421,43.722059],[-111.046435,43.726545],[-111.04634,43.726957],[-111.046715,43.815832],[-111.046515,43.908376],[-111.046917,43.974978],[-111.047064,43.983467],[-111.047349,43.999921],[-111.049077,44.020072],[-111.048751,44.060403],[-111.048751,44.060838],[-111.048633,44.062903],[-111.048452,44.114831],[-111.049119,44.124923],[-111.049695,44.353626],[-111.049148,44.374925],[-111.049216,44.435811],[-111.049194,44.438058],[-111.048974,44.474072],[-111.055208,44.624927],[-111.055333,44.666263],[-111.055511,44.725343],[-111.056416,44.749928],[-111.056888,44.866658],[-111.055629,44.933578],[-111.056207,44.935901],[-111.055199,45.001321],[-111.044275,45.001345],[-110.785008,45.002952],[-110.761554,44.999934],[-110.750767,44.997948],[-110.705272,44.992324],[-110.552433,44.992237],[-110.547165,44.992459],[-110.48807,44.992361],[-110.402927,44.99381],[-110.362698,45.000593],[-110.342131,44.999053],[-110.324441,44.999156],[-110.28677,44.99685],[-110.199503,44.996188],[-110.110103,45.003905],[-110.026347,45.003665],[-110.025544,45.003602],[-109.99505,45.003174],[-109.875735,45.003275],[-109.798687,45.002188],[-109.75073,45.001605],[-109.663673,45.002536],[-109.574321,45.002631],[-109.386432,45.004887],[-109.375713,45.00461],[-109.269294,45.005283],[-109.263431,45.005345],[-109.103445,45.005904],[-109.08301,44.99961],[-109.062262,44.999623],[-108.621313,45.000408],[-108.578484,45.000484],[-108.565921,45.000578],[-108.500679,44.999691],[-108.271201,45.000251],[-108.249345,44.999458],[-108.238139,45.000206],[-108.218479,45.000541],[-108.14939,45.001062],[-108.000663,45.001223],[-107.997353,45.001565],[-107.911743,45.001292],[-107.750654,45.000778],[-107.608854,45.00086],[-107.607824,45.000929],[-107.49205,45.00148],[-107.351441,45.001407],[-107.13418,45.000109],[-107.125633,44.999388],[-107.105685,44.998734],[-107.084939,44.996599],[-107.074996,44.997004],[-107.050801,44.996424],[-106.892875,44.995947],[-106.888773,44.995885],[-106.263586,44.993788],[-106.024814,44.993688],[-105.928184,44.993647],[-105.914258,44.999986],[-105.913382,45.000941],[-105.848065,45.000396],[-105.076607,45.000347],[-105.038405,45.000345],[-105.025266,45.00029],[-105.019284,45.000329],[-105.01824,45.000437],[-104.765063,44.999183],[-104.759855,44.999066],[-104.72637,44.999518],[-104.665171,44.998618],[-104.663882,44.998869],[-104.470422,44.998453],[-104.470117,44.998453],[-104.250145,44.99822],[-104.057698,44.997431],[-104.055914,44.874986],[-104.056496,44.867034],[-104.055963,44.768236],[-104.055963,44.767962],[-104.055934,44.72372],[-104.05587,44.723422],[-104.055777,44.700466],[-104.055938,44.693881],[-104.05581,44.691343],[-104.055877,44.571016],[-104.055892,44.543341],[-104.055927,44.51773],[-104.055389,44.249983],[-104.054487,44.180381],[-104.054562,44.141081],[-104.05495,43.93809],[-104.055077,43.936535],[-104.055488,43.853477],[-104.055488,43.853476],[-104.055138,43.750421],[-104.055133,43.747105],[-104.054902,43.583852],[-104.054885,43.583512],[-104.05484,43.579368],[-104.055032,43.558603],[-104.054787,43.503328],[-104.054786,43.503072],[-104.054779,43.477815],[-104.054766,43.428914],[-104.054614,43.390949],[-104.054403,43.325914],[-104.054218,43.30437],[-104.053884,43.297047],[-104.053876,43.289801],[-104.053127,43.000585],[-104.052863,42.754569],[-104.052809,42.749966],[-104.052583,42.650062],[-104.052741,42.633982],[-104.052586,42.630917],[-104.052773,42.611766],[-104.052775,42.61159],[-104.052775,42.610813],[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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688660","contributors":{"authors":[{"text":"Maughan, Edwin K.","contributorId":85172,"corporation":false,"usgs":true,"family":"Maughan","given":"Edwin","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":161028,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10814,"text":"ofr78272 - 1978 - Drilling during 1977 in the Danforth Hills coal field, Easton Gulch and Devils Hole Gulch quadrangles, Moffat County, Colorado","interactions":[],"lastModifiedDate":"2022-02-23T23:01:12.95253","indexId":"ofr78272","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-272","title":"Drilling during 1977 in the Danforth Hills coal field, Easton Gulch and Devils Hole Gulch quadrangles, Moffat County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78272","usgsCitation":"Reheis, M.J., 1978, Drilling during 1977 in the Danforth Hills coal field, Easton Gulch and Devils Hole Gulch quadrangles, Moffat County, Colorado: U.S. Geological Survey Open-File Report 78-272, Report: i, 29 p.; 1 Plate: 28.00 × 50.00 inches, https://doi.org/10.3133/ofr78272.","productDescription":"Report: i, 29 p.; 1 Plate: 28.00 × 50.00 inches","costCenters":[],"links":[{"id":396412,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14663.htm"},{"id":38611,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0272/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0272/report-thumb.jpg"},{"id":94994,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0272/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Moffat County","otherGeospatial":"Easton Gulch and Devils Hole Gulch quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.883,\n              40.227\n            ],\n            [\n              -108,\n              40.227\n            ],\n            [\n              -108,\n              40.325\n            ],\n            [\n              -107.883,\n              40.325\n            ],\n            [\n              -107.883,\n              40.227\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633d98","contributors":{"authors":[{"text":"Reheis, Marith J. 0000-0002-8359-323X","orcid":"https://orcid.org/0000-0002-8359-323X","contributorId":9657,"corporation":false,"usgs":true,"family":"Reheis","given":"Marith","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19286,"text":"ofr78458 - 1978 - Water levels in artesian and nonartesian aquifers of Florida, 1975-76","interactions":[],"lastModifiedDate":"2023-09-08T17:35:45.908665","indexId":"ofr78458","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-458","title":"Water levels in artesian and nonartesian aquifers of Florida, 1975-76","docAbstract":"<p>From May 1975 through May 1976, water levels in the Floridan aquifer through most of north and central peninsular Florida declined 2 to 4 feet, on the basis of water-level measurements in 664 wells. These 664 were selected from a network of about 2,100 observation wells for which water-level measurements are in the files of the Geological Survey.</p><p>Hydrographs of 60 wells show that the downward trends of groundwater levels continued in areas of heavy pumping and in some areas not affected by pumping. In west-central Polk County, the most notable area of pumping, levels in the Floridan and other aquifers declined to new record lows in 1975 but recovered 3 to 6 feet in 1976. In north Florida where fluctuations of ground-water levels are primarily influenced by changes in stage of the Suwannee River, levels declined 18 and 23 feet in Suwannee and Hamilton Counties. In northwest Florida, declines in level in the sand-and-gravel aquifer ranged from less than 1 foot to 2 feet. In Nassau County, in Northern Brevard County, and at Stuart in Martin County--in the northeastern, eastern, and southwestern coastal parts of the State--levels declined to new record lows also.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78458","collaboration":"Prepared in cooperation with the Florida Department of Environmental Regulation Bureau of Water Resources Management, Northwest Florida Water Management District, St. Johns Water Management District, South Florida Water Management District, Southwest Florida Water Management District, Suwannee River Water Management District, and other state and local agencies","usgsCitation":"Healy, H.G., 1978, Water levels in artesian and nonartesian aquifers of Florida, 1975-76: U.S. Geological Survey Open-File Report 78-458, ix, 115 p., https://doi.org/10.3133/ofr78458.","productDescription":"ix, 115 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,{"id":10364,"text":"ofr78448 - 1978 - Spectral reflectance measurements of plants in the East Tintic Mountains, Utah","interactions":[],"lastModifiedDate":"2026-02-04T17:43:23.773158","indexId":"ofr78448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-448","title":"Spectral reflectance measurements of plants in the East Tintic Mountains, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78448","usgsCitation":"Milton, N., 1978, Spectral reflectance measurements of plants in the East Tintic Mountains, Utah: U.S. Geological Survey Open-File Report 78-448, 126 p., 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,{"id":40118,"text":"ofr78893 - 1978 - Contour map of the base of Pennsylvanian strata in eastern Kentucky","interactions":[],"lastModifiedDate":"2021-11-29T19:24:40.661432","indexId":"ofr78893","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-893","title":"Contour map of the base of Pennsylvanian strata in eastern Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78893","usgsCitation":"Coskren, T., 1978, Contour map of the base of Pennsylvanian strata in eastern Kentucky: U.S. Geological Survey Open-File Report 78-893, 3 Plates: 33.82 × 44.32 inches or smaller, https://doi.org/10.3133/ofr78893.","productDescription":"3 Plates: 33.82 × 44.32 inches or smaller","costCenters":[],"links":[{"id":170128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":69363,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0893/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":69362,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0893/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392184,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74962.htm"},{"id":69364,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0893/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kentucky","otherGeospatial":"Pennsylvanian strata","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.1667,\n              39.1439\n            ],\n            [\n              -81.9642,\n              39.1439\n            ],\n            [\n              -81.9642,\n              36.5914\n            ],\n            [\n              -85.1667,\n              36.5914\n            ],\n            [\n              -85.1667,\n              39.1439\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dbd","contributors":{"authors":[{"text":"Coskren, T. Dennis","contributorId":84430,"corporation":false,"usgs":true,"family":"Coskren","given":"T. Dennis","affiliations":[],"preferred":false,"id":222993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38702,"text":"pp813Q - 1978 - Summary appraisals of the nation's ground-water resources – Missouri basin region","interactions":[],"lastModifiedDate":"2021-12-14T21:56:38.395429","indexId":"pp813Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"Q","title":"Summary appraisals of the nation's ground-water resources – Missouri basin region","docAbstract":"<p>The Missouri Basin Region lies in the north-central part of the United States and southern Canada. It includes parts of Alberta and Saskatchewan in Canada; parts of Montana, Wyoming, North Dakota, South Dakota, Minnesota, Iowa, Colorado, Kansas, and Missouri, and all of Nebraska in the United States. The region includes about one-sixth of the contiguous United States and requires large water supplies for irrigation, industrial, public, and rural uses. Climate ranges from semiarid to subhumid. Normal annual precipitation increases generally eastward in the downstream direction, but precipitation is not a dependable source of supply. The Missouri River and its tributaries furnish water to many users, but surface water is often inadequate to meet large demands. Numerous surface reservoirs help to regulate streamflow and provide storage, but they also allow an increase in evapotranspiration, which in some areas exceeds normal precipitation. Ground water occurs in aquifers classified as alluvial deposits of sand and gravel, glacial deposits, dune-sand deposits, basin-fill deposits of sand and gravel, sandstone, siltstone, fractured sandy clay, limestone, and dolomite. Ground water can be developed and managed in an orderly manner provided adequate geologic and hydrologic data are available to determine aquifer characteristics and response to pumping and other hydraulic stresses. These data and determinations are essential to design, testing, and implementation of water management plans.</p>\n<p>Unconsolidated and semiconsolidated aquifers include valley-fill alluvium, areally extensive alluvium, glacial deposits, and basin-fill deposits. The aquifers normally consist of alluvial sand and gravel that contain unconfined ground water that lies near the land surface. Many wells completed in the alluvial aquifers have high yields of good-quality water because most alluvial aquifers are highly transmissive and hydraulically connected to streams. Aquifers in glacial deposits may be difficult to locate and in some areas contain saline water; nevertheless, these aquifers are sources of water supply for many users. Basin-fill aquifers are as much as several thousand feet thick, and many contain large ground-water supplies. Ground-water mining has occurred in semiconsolidated aquifers because of withdrawals from wells.&nbsp;Unconsolidated and semiconsolidated aquifers have potential for conjunctive use with surface water, recycling to reuse available supplies, artificial recharge, and salvage of evapotranspired water.</p>\n<p>Sandstone aquifers lie near the land surface and in structural basins. Interbasin movement of ground water occurs in the Virgelle (Milk River aquifer), Fox Hills-basal Hell Creek, and Dakota aquifers. Sandstone aquifers are less transmissive than unconsolidated and semiconsolidated aquifers in general. Confined sandstone aquifers are common, and flowing wells are obtained in many areas. However, flowing wells may cause large declines in water levels if uncontrolled. Water quality is variable in sandstone aquifers but is adequate for most needs.&nbsp;Sandstone aquifers have potential for artificial recharge, induced interaquifer leakage, conjunctive use with surface water, and mining of ground water.</p>\n<p>Limestone and dolomite aquifers are extensive in the region, but in some areas they lie deep below the land surface. The occurrence of ground water in small pores, fractures, or large caverns causes yields from wells to range widely. Large flows through cavern systems in the aquifers are indicated by large springs in some areas. Water quality is extremely variable and must be considered in any water-development plan.&nbsp;Limestone and dolomite aquifers have potential for development of large water supplies in some areas. The development may be aided by induced recharge and interaquifer leakage.</p>\n<p>Saline ground water occurs throughout the Missouri Basin Region. Dissolved-solids concentration as much as 30,000 milligrams per liter has been measured in aquifers in glacial deposits in Montana. Saline water is common in sandstone aquifers in Wyoming, North Dakota, and South Dakota; maximum reported concentration is 280,000 milligrams per liter in water from the Tensleep Sandstone in Wyoming. Limestone contains saline water in many areas; maximum dissolved-solids concentration is about 350,000 milligrams per liter for the Madison Group in the Williston Basin in North Dakota.</p>\n<p>Comprehensive water-management planning in the Missouri Basin Region will require periodic or continuing inventory of precipitation, streamflow, surface-water storage, and ground water. Water demands for irrigation, industrial, public supply, and rural use are increasing rapidly. Reliance on ground-water supplies is increasing even though in many areas the ground water is still mostly undeveloped. Optimal use of water supplies will require the establishment of realistic goals and carefully conceived water-management plans, each of which will necessarily be based on an adequate baseline of hydrologic data and knowledge of the highly variable hydrologic systems in the region.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813Q","usgsCitation":"Taylor, O., 1978, Summary appraisals of the nation's ground-water resources – Missouri basin region: U.S. Geological Survey Professional Paper 813, Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller, https://doi.org/10.3133/pp813Q.","productDescription":"Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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,{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","interactions":[{"subject":{"id":10803,"text":"ofr77565 - 1977 - Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","indexId":"ofr77565","publicationYear":"1977","noYear":false,"title":"Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region"},"predicate":"SUPERSEDED_BY","object":{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","indexId":"pp813K","publicationYear":"1978","noYear":false,"chapter":"K","title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region"},"id":1}],"lastModifiedDate":"2021-12-14T22:08:19.164288","indexId":"pp813K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"K","title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","docAbstract":"<p>A broad-perspective analysis of the ground-water resources and present and possible future water development and management in the Souris-Red-Rainy Region is presented. The region includes the basins of the Souris River within Montana and North Dakota; the Red River of the North in South Dakota, North Dakota, and Minnesota; and the Rainy River within Minnesota. The region includes 59,645 square miles, mostly in North Dakota and Minnesota.</p>\n<p>The terrain is relatively flat, but ranges in altitude from 2,541 to 750 feet. Annual average precipitation ranges from 14 inches in the west to 28 inches in the east and about 75 percent of it is rain. The mean annual snowfall ranges from 32 inches in the west to 64 inches in the east. Temperatures range from -55&deg; to 118&deg; F (-48.3&deg; to 47.8&deg; C). Irrigation is needed at least part of the time to assure crop production, particularly in the western part of the region.</p>\n<p>Sand and gravel deposits in the drift form the most important freshwater aquifers. Other aquifers are found in at least parts of the region in the Precambrian, Paleozoic, Cretaceous, and Tertiary rocks. The potentiometric surface in the bedrock aquifers generally decreases in altitude toward the Red River of the North, indicating that the general direction of ground-water movement is toward the river. Ground water with less than 3,000 milligrams per liter dissolved solids is available throughout the region. Ground water with less than 1,000 milligrams per liter occurs in most of the region east of the Red River of the North and in most of the shallow aquifers west of the river. The total volume of water available from storage having less than 3,000 milligrams per liter dissolved solids is estimated to be 5x10<sup>8</sup> acre-feet. In addition to the fresh and slightly saline water, the region has abundant highly mineralized water that can be considered as a resource. Yields of wells in individual bedrock aquifers are generally less than 100 gallons per minute but locally yields may be as much as 500 gallons per minute and more. Yields in drift aquifers are frequently less than 100 gallons per minute but range from 5 to 1,000 gallons per minute. In a few places outwash yields more than 1,000 gallons per minute.</p>\n<p>Ground water is the sole or a primary source of water supply in much of the region, including supplies for irrigation, domestic and livestock, municipal, and industrial needs. Reportedly, the potential irrigation development is 1,550,000 acres, as compared with 50,200 acres in 1975. Both ground- and surface-water supplies would be required to meet these demands. Rural domestic and livestock water supplies are derived almost entirely from ground-water sources. Smaller communities and towns generally rely on ground water, and the cities and industries use ground water, surface water, or both. The municipalities using surface water generally depend upon reservoir storage. Water quality rather than quantity is the greater water-supply problem for many communities in the region.</p>\n<p>Increased demands on both ground-water and surface-water supplies likely will be made in the future. Storage of surface water in the ground-water reservoirs during times of surplus for withdrawal during times of scarcity would aid in meeting these demands. The surplus (flood) water is of better chemical quality than underlying ground water in parts of the western half of the region. Freshwater could be stored in saline- or freshwater aquifers, and pumped out later, as needed. Thus, the ground-water reservoirs have a definite present and potential role in water management.</p>\n<p>To understand the hydrologic system for management purposes there is a need to determine more adequately the geologic and hydrologic characteristics of existing aquifers and the location of new aquifers. Also, as pumping and other stresses on any part of the hydrologic system affect other parts of the system, monitoring programs ideally should be started and maintained to detect changes and determine effects of the stresses.</p>\n<p>Many alternatives are available for managing water in the region. Some of these are operational and others are undergoing research. Adequate hydrologic information is needed to aid in solving problems of water supply, use, and pollution.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813K","usgsCitation":"Reeder, H.O., 1978, Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region: U.S. Geological Survey Professional Paper 813, vi, 25 p., https://doi.org/10.3133/pp813K.","productDescription":"vi, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":392905,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5066.htm"},{"id":122128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813k/report-thumb.jpg"},{"id":65552,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813k/report.pdf","text":"Report","size":"8.83 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Minnesota, Montana, North Dakota, South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ],\n            [\n              -95.185546875,\n              49.06666839558117\n            ],\n            [\n              -95.1416015625,\n              49.52520834197442\n            ],\n            [\n              -94.74609375,\n              49.32512199104001\n            ],\n            [\n              -94.482421875,\n              48.864714761802794\n            ],\n            [\n              -93.69140625,\n              48.69096039092549\n            ],\n            [\n              -93.0322265625,\n              48.719961222646276\n            ],\n            [\n              -92.28515625,\n              48.516604348867475\n            ],\n            [\n              -91.845703125,\n              48.40003249610685\n            ],\n            [\n              -91.3623046875,\n              48.19538740833338\n            ],\n            [\n              -90.7470703125,\n              48.28319289548349\n            ],\n            [\n              -89.384765625,\n              48.1367666796927\n            ],\n            [\n              -90,\n              47.724544549099676\n            ],\n            [\n              -91.2744140625,\n              47.15984001304432\n            ],\n            [\n              -92.373046875,\n              46.70973594407157\n            ],\n            [\n              -94.5703125,\n              45.73685954736049\n            ],\n            [\n              -95.712890625,\n              45.398449976304086\n            ],\n            [\n              -97.0751953125,\n              45.30580259943578\n            ],\n            [\n              -98.525390625,\n              45.82879925192134\n            ],\n            [\n              -99.5361328125,\n              46.10370875598026\n            ],\n            [\n              -100.81054687499999,\n              46.89023157359399\n            ],\n            [\n              -101.953125,\n              47.07012182383309\n            ],\n            [\n              -103.3154296875,\n              47.54687159892238\n            ],\n            [\n              -104.150390625,\n              47.84265762816538\n            ],\n            [\n              -105.2490234375,\n              48.3416461723746\n            ],\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6996cc","contributors":{"authors":[{"text":"Reeder, Harold O.","contributorId":14381,"corporation":false,"usgs":true,"family":"Reeder","given":"Harold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":220306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26721,"text":"wri77123 - 1978 - Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia","interactions":[],"lastModifiedDate":"2025-01-08T22:40:11.942634","indexId":"wri77123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"77-123","title":"Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia","docAbstract":"<p>Fourteen drainage basins above Fishtrap and Dewey Lakes in the Levisa Fork and Johns Creek drainage basins of eastern Kentucky and southwestern Virginia were studied to determine sedimentation rates and origin of sediment entering the two lakes. The basins ranged in size from 1.68 to 297 square miles. Sediment yields ranged from 2,890 to 21,000 tons per square mile where surface-mining techniques predominated, and from 732 to 3 ,470 tons per square mile where underground mining methods predominated. Yields, in terms of tons per acre-foot of runoff, ranged from 2.2 to 15 for surface-mined areas, and from 0.5 to 2.7 for underground-mined areas. Water and sediment discharges from direct runoff during storms were compared for selected surface-mined and underground-mined areas. Data points of two extensively surface-mined areas, one from the current project and one from a previous project in Beaver Creek basin, McCreary County, Kentucky, grouped similarly in magnitude and by season. Disturbed areas from mining activities determined from aerial photographs reached 17 percent in one study area where extensive surface mining was being practiced. For most areas where underground mining was practiced, percentage disturbed area was almost negligible. Trap efficiency of Fishtrap Lake was 89 percent, and was 62 percent for Dewey Lake. Average annual deposition rates were 464 and 146 acre-feet for Fishtrap and Dewey Lakes, respectively. The chemical quality of water in the Levisa Fork basin has been altered by man 's activities.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri77123","usgsCitation":"Curtis, W.F., Flint, R.F., George, F.H., and Santos, J.F., 1978, Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia: U.S. Geological Survey Water-Resources Investigations Report 77-123, xi, 92 p., https://doi.org/10.3133/wri77123.","productDescription":"xi, 92 p.","costCenters":[],"links":[{"id":366194,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158260,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0123/report-thumb.jpg"},{"id":465926,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35124.htm","text":"Dewey Lake","linkFileType":{"id":5,"text":"html"}},{"id":465927,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35125.htm","text":"Fishtrap Lake","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kentucky, Virginia","otherGeospatial":"Dewey Lake, Fishtrap Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.7764892578125,\n              37.38979975341983\n            ],\n            [\n              -82.29583740234375,\n              37.38979975341983\n            ],\n            [\n              -82.29583740234375,\n              37.75334401310656\n            ],\n            [\n              -82.7764892578125,\n              37.75334401310656\n            ],\n            [\n              -82.7764892578125,\n              37.38979975341983\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c3e4b07f02db4a7e1d","contributors":{"authors":[{"text":"Curtis, William F.","contributorId":70433,"corporation":false,"usgs":true,"family":"Curtis","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Russell F.","contributorId":91144,"corporation":false,"usgs":true,"family":"Flint","given":"Russell","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"George, Frederick H.","contributorId":16462,"corporation":false,"usgs":true,"family":"George","given":"Frederick","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":196886,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Santos, John F.","contributorId":21530,"corporation":false,"usgs":true,"family":"Santos","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196887,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":28325,"text":"wri77114 - 1978 - Altitude and configuration of the top of the Floridan Aquifer, Duval County, Florida","interactions":[],"lastModifiedDate":"2019-08-05T11:01:40","indexId":"wri77114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"77-114","title":"Altitude and configuration of the top of the Floridan Aquifer, Duval County, Florida","docAbstract":"Structural contours on the top of the Floridan aquifer in Duval County, Florida, show that the top of the aquifer ranges from less than 300 feet below sea level to more than 600 feet below sea level. Two inferred concealed faults occur in the aquifer; one trending northeast-southwest in the eastern part of the county. The maximum vertical displacement of the top of the aquifer of both faults is about 150 feet. A geologic section included on the map shows the geologic formations of Eocene age that comprise the Floridan aquifer. These are, in ascending order: the Lake City Limestone, the Avon Park Limestone, and the Ocala Limestone. 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,{"id":34083,"text":"b1383C - 1978 - Potential hazards from future eruptions of Mount St. Helens Volcano, Washington","interactions":[{"subject":{"id":18572,"text":"ofr76491 - 1976 - Potential hazards from future eruptions of Mount St. Helens volcano, Washington","indexId":"ofr76491","publicationYear":"1976","noYear":false,"title":"Potential hazards from future eruptions of Mount St. Helens volcano, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":34083,"text":"b1383C - 1978 - Potential hazards from future eruptions of Mount St. Helens Volcano, Washington","indexId":"b1383C","publicationYear":"1978","noYear":false,"chapter":"C","title":"Potential hazards from future eruptions of Mount St. Helens Volcano, Washington"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:27","indexId":"b1383C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1383","chapter":"C","title":"Potential hazards from future eruptions of Mount St. Helens Volcano, Washington","docAbstract":"Mount St. Helens has been more active and more explosive during the last 4,500 years than any other volcano in the conterminous United States. Eruptions of that period repeatedly formed domes, large volumes of pumice, hot pyroclastic flows, and, during the last 2,500 years, lava flows. Some of this activity resulted in mudflows that extended tens of kilometers down the floors of valleys that head at the volcano. This report describes the nature of the phenomena and their threat to people and property; the accompanying maps show areas likely to be affected by future eruptions of Mount St. Helens. Explosive eruptions that produce large volumes of pumice affect large areas because winds can carry the lightweight material hundreds of kilometers from the volcano. Because of prevailing winds, the 180-degree sector east of the volcano will be affected most often and most severely by future eruptions of this kind. However, the pumice from any one eruption will fall in only a small part of that sector. Pyroclastic flows and mudflows also can affect areas far from the volcano, but the areas they affect are smaller because they follow valleys. Mudflows and possibly pyroclastic flows moving rapidly down Swift and Pine Creeks could displace water in Swift Reservoir, which could cause disastrous floods farther downvalley.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1383C","usgsCitation":"Crandell, D.R., and Mullineaux, D.R., 1978, Potential hazards from future eruptions of Mount St. Helens Volcano, Washington: U.S. Geological Survey Bulletin 1383, 26 p, https://doi.org/10.3133/b1383C.","productDescription":"26 p","costCenters":[],"links":[{"id":3386,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://vulcan.wr.usgs.gov/Volcanoes/MSH/Publications/Bulletin1383-C/framework.html","linkFileType":{"id":5,"text":"html"}},{"id":163343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1383c/report-thumb.jpg"},{"id":61995,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1383c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61996,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1383c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61997,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1383c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae046","contributors":{"authors":[{"text":"Crandell, Dwight Raymond","contributorId":6440,"corporation":false,"usgs":true,"family":"Crandell","given":"Dwight","email":"","middleInitial":"Raymond","affiliations":[],"preferred":false,"id":212431,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullineaux, Donal Ray","contributorId":31759,"corporation":false,"usgs":true,"family":"Mullineaux","given":"Donal","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":212432,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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