{"pageNumber":"377","pageRowStart":"9400","pageSize":"25","recordCount":10957,"records":[{"id":42180,"text":"ofr78330 - 1978 - Aeromagnetic form-line contour map of the east part of the Rolla, Missouri 1° x 2° quadrangle","interactions":[],"lastModifiedDate":"2022-02-23T22:29:06.578472","indexId":"ofr78330","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":"78-330","title":"Aeromagnetic form-line contour map of the east part of the Rolla, Missouri 1° x 2° quadrangle","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78330","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Aeromagnetic form-line contour map of the east part of the Rolla, Missouri 1° x 2° quadrangle: U.S. Geological Survey Open-File Report 78-330, 1 Plate: 20.86 × 24.12 inches, https://doi.org/10.3133/ofr78330.","productDescription":"1 Plate: 20.86 × 24.12 inches","costCenters":[],"links":[{"id":172341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":396406,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14690.htm"},{"id":79927,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0330/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Missouri","otherGeospatial":"Rolla 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.25,\n              37\n            ],\n            [\n              -90,\n              37\n            ],\n            [\n              -90,\n              38\n            ],\n            [\n              -91.25,\n              38\n            ],\n            [\n              -91.25,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698463","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530887,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36800,"text":"fwsobs78_81 - 1978 - Surface mining and fish/wildlife needs in the eastern United States: proceedings of a symposium","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"fwsobs78_81","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"78/81","title":"Surface mining and fish/wildlife needs in the eastern United States: proceedings of a symposium","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Samuel, D.E., Stauffer, J.R., Hocutt, C.H., and Mason, W., 1978, Surface mining and fish/wildlife needs in the eastern United States: proceedings of a symposium: FWS/OBS 78/81, 386 p. : ill., maps; 27 cm. + addendum.","productDescription":"386 p. : ill., maps; 27 cm. + addendum","costCenters":[],"links":[{"id":165632,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698252","contributors":{"authors":[{"text":"Samuel, David E.","contributorId":100916,"corporation":false,"usgs":true,"family":"Samuel","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":216970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stauffer, Jay R.","contributorId":51816,"corporation":false,"usgs":true,"family":"Stauffer","given":"Jay","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":216969,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hocutt, Charles H.","contributorId":41493,"corporation":false,"usgs":true,"family":"Hocutt","given":"Charles","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":216968,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mason, William T.","contributorId":27516,"corporation":false,"usgs":true,"family":"Mason","given":"William T.","affiliations":[],"preferred":false,"id":216967,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":36793,"text":"fwsobs78_95 - 1978 - Mined land reclamation for fish and wildlife in the eastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"fwsobs78_95","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"78/95","title":"Mined land reclamation for fish and wildlife in the eastern United States","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"U.S. Fish and Wildlife Service, 1978, Mined land reclamation for fish and wildlife in the eastern United States: FWS/OBS 78/95, 12 p. : col. ill.; 27 cm.","productDescription":"12 p. : col. ill.; 27 cm.","costCenters":[],"links":[{"id":165626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6356cc","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529593,"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":30805,"text":"ofr781071 - 1978 - Geotechnical properties of sediments from the Continental Shelf south of Icy Bay, northeastern Gulf of Alaska","interactions":[],"lastModifiedDate":"2023-07-25T20:33:20.398117","indexId":"ofr781071","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":"78-1071","title":"Geotechnical properties of sediments from the Continental Shelf south of Icy Bay, northeastern Gulf of Alaska","docAbstract":"<p>Studies of geotechnical properties of marine sediments have recently intensified as the search for natural resources has expanded on the continental shelf. The U. S. Geological Survey has begun a detailed evaluation of geologic environmental conditions in continental shelf regions in order to facilitate safe development of continental shelf resources. Investigations of geohazards in the northeastern Gulf of Alaska (Fig. 1) began in 1974 when 6500 km of high and medium resolution seismic reflection data were collected from the eastern gulf between Yakutat and Montague Island (Carlson, Bruns and Molnia, 1975; Von Huene and others, 1975). The first extensive sediment sampling program was begun in 1975 when approximately 400 samples of continental shelf sediments were collected from the same area of the gulf (Carlson and others, 1977b). A limited number of geotechnical measurements were made from these samples and samples collected by subsequent programs, however, systematic measurement of geotechnical properties was not started until the 1977 cruise of the NOAA ship DISCOVERER. Once unstable environments or \"geohazards\", such as slumps and slides, are delineated, geotechnical testing is an important means of quantifying such geologic processes and consequently furthering our understanding of them.</p><p>The purposes of this report are two-fold: (1) to report variations of physical properties in 1-2 meter gravity cores and (2) to recognize any variations in the areal distribution of these properties within and adjacent to an area of mass movement in the northeastern Gulf of Alaska.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781071","usgsCitation":"Carlson, P.R., Levy, W.P., Molnia, B.F., and Hampson, J.C., 1978, Geotechnical properties of sediments from the Continental Shelf south of Icy Bay, northeastern Gulf of Alaska: U.S. Geological Survey Open-File Report 78-1071, 29 p., https://doi.org/10.3133/ofr781071.","productDescription":"29 p.","costCenters":[],"links":[{"id":419318,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1071/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161005,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1071/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Icy Bay, northeastern Gulf of Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -141.74386722970848,\n              60.27643600738864\n            ],\n            [\n              -141.74386722970848,\n              59.78959667023767\n            ],\n            [\n              -141.0247576005145,\n              59.78959667023767\n            ],\n            [\n              -141.0247576005145,\n              60.27643600738864\n            ],\n            [\n              -141.74386722970848,\n              60.27643600738864\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b0a9","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":204000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Levy, William P.","contributorId":102910,"corporation":false,"usgs":true,"family":"Levy","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":203999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Molnia, Bruce F. 0000-0001-8102-6269","orcid":"https://orcid.org/0000-0001-8102-6269","contributorId":301013,"corporation":false,"usgs":true,"family":"Molnia","given":"Bruce","email":"","middleInitial":"F.","affiliations":[{"id":36171,"text":"National Civil Applications Center","active":true,"usgs":true}],"preferred":true,"id":203997,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hampson, John C. Jr.","contributorId":108033,"corporation":false,"usgs":true,"family":"Hampson","given":"John","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":203998,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":35336,"text":"b1438 - 1978 - Understanding natural systems; a perspective for land-use planning in Appalachian Kentucky","interactions":[],"lastModifiedDate":"2017-06-27T16:28:37","indexId":"b1438","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":"1438","title":"Understanding natural systems; a perspective for land-use planning in Appalachian Kentucky","docAbstract":"<p>An eight-county area at the headwaters of the Kentucky River has been designated the Kentucky River Area Development District (KRADD) by the Appalachian Regional Commission. The objective of the project described in this report has been to provide materials to KRADD planners in a format and containing terminology usable by local people untrained in earth science. </p><p>Experimental maps (not included in this report) have been prepared largely from preexisting data. Time and cost limitations required a regional analysis as well as somewhat more detailed examples of selected localities. Most of the maps produced to meet these needs show the abundance and distribution of naturally occurring materials and the areas affected by various geomorphic processes. Three types of maps, showing current land use, slope, and flood-prone areas, present both basic and derived data directly applicable to specific land-use decisions. Basic map information on quality and quantity of surface and ground water, bedrock and surficial geology, and mineral fuels can be interpreted for a wide variety of current and potential uses. Texts accompanying the maps explain bedrock control of geomorphic processes, distribution and significance of surficial deposits, and hydrologic characteristics of the intricately dissected eastern Kentucky terrain. Within this conceptual framework, geomorphic processes and the landscape may be evaluated in humanly significant terms of low to high potential risk, thereby indicating both opportunities and limitations for land use.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1438","usgsCitation":"Newell, W., 1978, Understanding natural systems; a perspective for land-use planning in Appalachian Kentucky: U.S. Geological Survey Bulletin 1438, iv, 50 p., https://doi.org/10.3133/b1438.","productDescription":"iv, 50 p.","costCenters":[],"links":[{"id":166073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1438/report-thumb.jpg"},{"id":63192,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1438/report.pdf","text":"Report","size":"5.20 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Kentucky","county":"Breathift County, Knott County, Lee County, 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Wayne L.","contributorId":48538,"corporation":false,"usgs":true,"family":"Newell","given":"Wayne L.","affiliations":[],"preferred":false,"id":214471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18369,"text":"ofr781019 - 1978 - An instrument system for long-term sediment transport studies on the continental shelf","interactions":[],"lastModifiedDate":"2024-02-09T20:05:45.390348","indexId":"ofr781019","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":"78-1019","title":"An instrument system for long-term sediment transport studies on the continental shelf","docAbstract":"<p>A bottom-mounted instrument system has been designed and built to monitor processes of bottom-sediment movement on the Continental Shelf. The system measures bottom current speed and direction, pressure, temperature, and light transmission, and photographs the bottom. The instrument operates in a burst sample mode. The system can be deployed for periods of 2-6 months to monitor intermittent processes of sediment movement such as storms, and to assess seasonal variability. Deployments of the system on the U.S. East Coast Continental Shelf show sediment resuspension and changes in bottom microtopography due to surface waves, tidal currents, and storms.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781019","usgsCitation":"Butman, B., and Folger, D.W., 1978, An instrument system for long-term sediment transport studies on the continental shelf: U.S. Geological Survey Open-File Report 78-1019, 24 p., https://doi.org/10.3133/ofr781019.","productDescription":"24 p.","costCenters":[],"links":[{"id":425549,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1019/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151765,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1019/report-thumb.jpg"}],"country":"United States","otherGeospatial":"East Coast Continental Shelf","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68456c","contributors":{"authors":[{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":178994,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Folger, David W.","contributorId":96663,"corporation":false,"usgs":true,"family":"Folger","given":"David","email":"","middleInitial":"W.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":178995,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27090,"text":"wri7849 - 1978 - Ten-year low mean monthly discharge determinations for ungaged streams near waste-stabilization ponds in Wisconsin","interactions":[],"lastModifiedDate":"2015-10-21T09:47:13","indexId":"wri7849","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":"78-49","title":"Ten-year low mean monthly discharge determinations for ungaged streams near waste-stabilization ponds in Wisconsin","docAbstract":"<p>Communities that use fill-and-draw waste-water treatment lagoons or waste-stabilization ponds are required to discharge during the spring and fall of the year at a rate that does not exceed the assimilative capacity of the receiving stream. The 10-year low mean monthly discharge (MMQ10) for October, November, April, and May for the receiving stream has been used to establish the discharge rate for the treatment systems at the appropriate time of the year. To determine the MMQ10 for the receiving stream the monthly mean discharge first was estimated by using a technique developed by Riggs (1969). Once the monthly mean discharge was determined the MMQ10 of the ungaged stream was estimated by using a graphical correlation between the monthly mean discharge and the MMQ10 of at least three gaging stations near the waste-stabilization pond.The MMQ10 for these gaging stations were determined by a log-Pearson Type III frequency analysis.</p>\n<p>The MMQ10 was determined for Maple Creek at Valmy, Aliens Creek near Oakdale, North Branch Manitowoc River at Sherwood, East Fork Poplar River near Curtiss, and Yellow River at Barronette.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7849","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Field, S.J., 1978, Ten-year low mean monthly discharge determinations for ungaged streams near waste-stabilization ponds in Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 78-49, iii, 16 p., 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,{"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":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":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}]}}
,{"id":26918,"text":"wri7814 - 1978 - Distribution of dissolved nitrate and fluoride in ground water, Highland-East Highlands, San Bernardino County, California","interactions":[],"lastModifiedDate":"2019-07-23T11:52:54","indexId":"wri7814","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":"78-14","title":"Distribution of dissolved nitrate and fluoride in ground water, Highland-East Highlands, San Bernardino County, California","docAbstract":"In the Highland-East Highlands area of southern California, concentrations of nitrate in water from many wells exceed the U.S. Environmental Protection Agency 's and the California Department of Health 's recommended limit for public water supplies. The nitrate standards for public water supplies in the study area are commonly met by blending the high-nitrate water with low-nitrate water before distribution; however, some of the low-nitrate water sources have fluoride concentrations that exceed the optimum level, or in a few cases exceed the maximum level recommended by the California Department of Health. Nitrate-nitrogen concentrations in the study area are generally between 1 and 20 milligrams per liter. In general, nitrate-nitrogen concentrations exceeding 10 milligrams per liter are found in water from wells perforated at depths of less than 500 feet. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7814","usgsCitation":"Eccles, L.A., and Klein, J.M., 1978, Distribution of dissolved nitrate and fluoride in ground water, Highland-East Highlands, San Bernardino County, California: U.S. Geological Survey Water-Resources Investigations Report 78-14, iv, 42 p. , https://doi.org/10.3133/wri7814.","productDescription":"iv, 42 p. ","costCenters":[],"links":[{"id":157596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0014/report-thumb.jpg"},{"id":365861,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0014/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.23716735839844,\n              34.10498222546687\n            ],\n            [\n              -117.14962005615236,\n              34.10498222546687\n            ],\n            [\n              -117.14962005615236,\n              34.13965669267611\n            ],\n            [\n              -117.23716735839844,\n              34.13965669267611\n            ],\n            [\n              -117.23716735839844,\n              34.10498222546687\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486b2","contributors":{"authors":[{"text":"Eccles, Lawrence A.","contributorId":90274,"corporation":false,"usgs":true,"family":"Eccles","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":197245,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klein, John M.","contributorId":27036,"corporation":false,"usgs":true,"family":"Klein","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":197244,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9954,"text":"ofr78779 - 1978 - Relationship of landslides to fractures in Potomac Group deposits, Fairfax County, Virginia","interactions":[],"lastModifiedDate":"2023-02-24T17:27:35.839704","indexId":"ofr78779","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":"78-779","title":"Relationship of landslides to fractures in Potomac Group deposits, Fairfax County, Virginia","docAbstract":"<p>Landsliding is a common problem in eastern Fairfax County, an area underlain by Potomac Group (Lower Cretaceous) Coastal Plain deposits of silt and clay interbedded and interfingered with sand and gravel. The slides commonly are present in clay and silt that, on the basis of laboratory tests, appear to be much too strong to have failed. However, the very plastic silt and clay deposits are commonly cut by long continuous to short discontinuous high-angle and subhorizontal joints, shears, and faults. These fractures can contribute to sliding. Failure along faults and shears takes place because the relative movement has greatly weakened and softened the clay and silt. The mechanism for failure along the joints is less obvious but may be related to infilling along joints, slight movement due to erosional unloading, swelling of clays, and softening along joints.&nbsp;</p><p>Field investigations suggest that the three best developed high-angle joint sets in eastern Fairfax County have trends in the northeast quadrant. Lineaments plotted on a lineament map prepared from Landsat imagery also trend northeast parallel to the regional joint orientation. This regional orientation suggests that some of the fractures are tectonic in origin. Therefore, they should be anticipated in a broad zone many miles wide in the vicinity of the Fall Line. In addition, fractures of unknown origin contributing to landsliding, have been observed in massive Potomac Group clay and silt deposits. Irrespective of origin, these fractures require careful investigation and engineering to prevent slope failure at critical locations during and after major excavation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78779","usgsCitation":"Langer, W.H., and Obermeier, S.F., 1978, Relationship of landslides to fractures in Potomac Group deposits, Fairfax County, Virginia: U.S. Geological Survey Open-File Report 78-779, iv, 33 p., https://doi.org/10.3133/ofr78779.","productDescription":"iv, 33 p.","costCenters":[],"links":[{"id":143612,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0779/report-thumb.jpg"},{"id":413404,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0779/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","county":"Fairfax 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William H. blanger@usgs.gov","contributorId":1241,"corporation":false,"usgs":true,"family":"Langer","given":"William","email":"blanger@usgs.gov","middleInitial":"H.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":false,"id":160565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Obermeier, Stephen F.","contributorId":102482,"corporation":false,"usgs":true,"family":"Obermeier","given":"Stephen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160566,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26881,"text":"wri7867 - 1978 - Predictive analyses of ground-water discharges in the Willow Creek Watershed, northeast Nebraska","interactions":[],"lastModifiedDate":"2019-05-06T14:43:58","indexId":"wri7867","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":"78-67","title":"Predictive analyses of ground-water discharges in the Willow Creek Watershed, northeast Nebraska","docAbstract":"<p>Ground-water discharge to Willow Creek, which drains a 204 mi<sup>2</sup> watershed in northeast Nebraska was predicted for six combinations of conditions of climate and ground-water development. A digital model of the ground water/surface-water system was stressed with recharge and withdrawal functions determined from a linear reservoir model of the soil zone.</p><p>The geohydrologic system includes a regional aquifer which containssand and gravel ranging in age from Pliocene through Pleistocene. The regional aquifer is unconfined in the western part of the watershed and confined in the eastern part. The confining layer, or blue clay, in the east is of Pleistocene age and comprises principally saturated eolian silts with very fine sand interbeds overlying a basal lacustrine clay. Where unconfined conditions exist in the regional aquifer, perennial flow of Willow Creek is sustained principally by ground-water discharge. Where confined conditions exist, the low hydraulic conductivity of the blue clay effectively isolates the regional aquifer from Willow Creek.</p><p>The stream-aquifer models were tested by comparing simulated against measured water levels and streamflow during 1975 and 1976. Agreement between simulated and observed values was obtained by modifying initial estimates of aquifer hydraulic conductivity and specific storage.</p><p>Future ground-water discharge to Willow Creek (base flow) was simulated by super-imposing different patterns of ground-water withdrawals upon variations from average recharge for a monthly climatic sequence identical with the period 1931 to 1954. Frequency analyses of the simulated monthly base flows showed that they would be less than 12 feet<sup>3</sup> per second at least 50 percent of the time under all but completely undeveloped conditions. Simulated water-level declines in the regional aquifer at the end of the pumping season after a drought period similar to that of the 1930's were less than 5 feet where unconfined conditions exist and were more than 80 feet where confined conditions exist. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7867","collaboration":"Prepared in cooperation with Lower Elkhorn Natural Resources District and Conservation and Survey Division, Institute of Agriculture and Natural Resources, the University of Nebraska-Lincoln","usgsCitation":"Dugan, J.T., and Lappala, E.G., 1978, Predictive analyses of ground-water discharges in the Willow Creek Watershed, northeast Nebraska: U.S. Geological Survey Water-Resources Investigations Report 78-67, v, 66 p., https://doi.org/10.3133/wri7867.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":363537,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0067/report-thumb.jpg"}],"country":"United States ","state":"Nebraska","otherGeospatial":"Willow Creek watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.97744750976562,\n              41.964085349226664\n            ],\n            [\n              -97.24067687988281,\n              41.964085349226664\n            ],\n            [\n              -97.24067687988281,\n              42.36919824433563\n            ],\n            [\n              -97.97744750976562,\n              42.36919824433563\n            ],\n            [\n              -97.97744750976562,\n              41.964085349226664\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605281","contributors":{"authors":[{"text":"Dugan, Jack T.","contributorId":102456,"corporation":false,"usgs":true,"family":"Dugan","given":"Jack","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":197175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lappala, Eric G.","contributorId":23182,"corporation":false,"usgs":true,"family":"Lappala","given":"Eric","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197174,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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., https://doi.org/10.3133/ofr78448.","productDescription":"126 p.","costCenters":[],"links":[{"id":143400,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0448/report-thumb.jpg"},{"id":499527,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"East Tintic Mountains","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"47\",\"properties\":{\"name\":\"Utah\",\"nation\":\"USA  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Nancy","contributorId":85188,"corporation":false,"usgs":true,"family":"Milton","given":"Nancy","affiliations":[],"preferred":false,"id":161260,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3805,"text":"cir786 - 1978 - General geology, petroleum appraisal, and nature of environmental hazards, eastern Pacific shelf latitude 28° to 38° north","interactions":[],"lastModifiedDate":"2022-01-05T22:06:07.063122","indexId":"cir786","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"786","title":"General geology, petroleum appraisal, and nature of environmental hazards, eastern Pacific shelf latitude 28° to 38° north","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir786","usgsCitation":"Howell, D.G., McCulloch, D.S., and Vedder, J.G., 1978, General geology, petroleum appraisal, and nature of environmental hazards, eastern Pacific shelf latitude 28° to 38° north: U.S. Geological Survey Circular 786, iii, 29 p., https://doi.org/10.3133/cir786.","productDescription":"iii, 29 p.","costCenters":[],"links":[{"id":393941,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23576.htm"},{"id":30875,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0786/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0786/report-thumb.jpg"}],"country":"Mexico, United States","otherGeospatial":"eastern Pacific shelf","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.617,\n              28\n            ],\n            [\n              -120.15,\n              28\n            ],\n            [\n              -120.15,\n              38\n            ],\n            [\n              -123.617,\n              38\n            ],\n            [\n              -123.617,\n              28\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b08e5","contributors":{"authors":[{"text":"Howell, D. G.","contributorId":52546,"corporation":false,"usgs":true,"family":"Howell","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":147636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":147635,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":147637,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7355,"text":"ofr78706 - 1978 - Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland","interactions":[],"lastModifiedDate":"2026-02-19T18:42:07.880284","indexId":"ofr78706","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":"78-706","title":"Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland","docAbstract":"<p>During the L1-78-SC cruise of the USGS research vessel S. P. Lee (April 25 - May 11, 1978) seven sonobuoy profiles and 200 km of 24-channel seismic reflection data were recorded in the outer southern California Continental Borderland. These data were obtained, at the request of the Deep Sea Drilling Project (DSDP), to evaluate possible drill sites along the southern California continental margin.&nbsp;</p><p>The drill sites shown in Figure 1 were proposed by the Ocean Paleo-environmental Panel for DSDP Leg 63--secheduled for Sept. - Nov. 1978. These sites were selected in order to provide an expanded Neogene record of paleoceanographic-paleoclimatic events and associated evolutionary development of planktic communities along the eastern side of the north Pacific Ocean. Site selection was made prior to this survey on the basis of available single-channel seismic reflection profiles. Thus, the proposed sites shown on Fig. 1 may be relocated or eliminated when the data presented in this report are incorporated with earlier data. The combined data will be evaluated for safety and pollution hazards by Leg 63 site proponents and the DSDP safety panels.&nbsp;</p><p>The ship's tracks (Fig. 1) were located by an integrated Satellite-Loran C-Doppler Sonar navigation system. Average survey speed was about 5 kts. A 1326 cu in (21,723 CC) tuned air gun array provided the sound source for both reflection and refraction profiles. The air gun array was fired at 50 m (about 18 sec.) intervals by the integrated navigation system.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78706","usgsCitation":"Crouch, J.K., Holmes, M., McCulloh, T.H., Long, A.T., and Brune, R., 1978, Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland: U.S. Geological Survey Open-File Report 78-706, 3 p., 10 sheets :ill., map ;29 cm., https://doi.org/10.3133/ofr78706.","productDescription":"25 p.","costCenters":[],"links":[{"id":500217,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0706/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141393,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0706/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"California 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H.","contributorId":106494,"corporation":false,"usgs":true,"family":"McCulloh","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":155384,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Long, A. T. along@usgs.gov","contributorId":20744,"corporation":false,"usgs":true,"family":"Long","given":"A.","email":"along@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":false,"id":155380,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Brune, R.H.","contributorId":91491,"corporation":false,"usgs":true,"family":"Brune","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":155383,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70112350,"text":"70112350 - 1978 - The metallogenic role of east-west fracture zones in South America with regard to the motion of lithospheric plates (with an example from Brazil)","interactions":[],"lastModifiedDate":"2017-01-18T15:10:00","indexId":"70112350","displayToPublicDate":"1990-06-12T15:58:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2135,"text":"Jornal de Mineralogia","active":true,"publicationSubtype":{"id":10}},"title":"The metallogenic role of east-west fracture zones in South America with regard to the motion of lithospheric plates (with an example from Brazil)","docAbstract":"<p>The role of east-west fracture zones in South America is discussed with regard to global fracturing and the motion of lithospheric plates. A set of major NW-trending lineaments has been derived which show a tendency to be spaced equidistantly and may correspond to a set of east-west fractures in the \"pre-drift\" position of the South American plate. Statistical analysis of linears in the ERTS-mosaics shows that NW-fractures are also among the most important ones in the Andes region, suggesting that the above major lineaments extend into the basement of the Andes. Some of the old major fractures, trending east-west in the present orientation of South America, are discussed and their NE orientation in the pre-drift position of the plate is considered. An example of structural control of ore deposition in the Brazilian Shield is presented, using the maps of the RADAM Project. It is concluded that the small tin-bearing granitic bodies concentrated in the region of Sao Felix do Xingu in the state of Para represent upper parts of an unexposed granitoid massif which is controlled by the intersection of a major east-west fracture zone probably represents westward extension of the Patos Lineament of the easternmost part of Brazil, connected with the east-west fracture zone of the Para state through the basement of the Maranhao Basin (Sineclise do Maranhao-Piaui). It is expected that the proposed \"Patos-Para Lineament\" extends further westward and may similarly control, at intersections with fractures of other trends, some mineralization centers in the western part of the state of Para and in the state of Amazonas.</p>","language":"English","publisher":"Clube de Mineralogía","publisherLocation":"Recife, Brazil","usgsCitation":"Kutina, J., Carter, W.D., and Lopez, F., 1978, The metallogenic role of east-west fracture zones in South America with regard to the motion of lithospheric plates (with an example from Brazil): Jornal de Mineralogia, v. 7, p. 97-110.","productDescription":"14 p.","startPage":"97","endPage":"110","numberOfPages":"14","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288560,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","otherGeospatial":"South America","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.0,-56.5 ], [ -94.0,13.1 ], [ -32.6,13.1 ], [ -32.6,-56.5 ], [ -94.0,-56.5 ] ] ] } } ] }","volume":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc58e4b0e83db6d0902f","contributors":{"authors":[{"text":"Kutina, J.","contributorId":65006,"corporation":false,"usgs":true,"family":"Kutina","given":"J.","affiliations":[],"preferred":false,"id":494702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, William D.","contributorId":64567,"corporation":false,"usgs":true,"family":"Carter","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":494701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lopez, F.X.","contributorId":99894,"corporation":false,"usgs":true,"family":"Lopez","given":"F.X.","email":"","affiliations":[],"preferred":false,"id":494703,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112349,"text":"70112349 - 1978 - Tectolinear interpretation of a 1:5,000,000 Landsat-1 mosaic compared with the structure of central and eastern United States","interactions":[],"lastModifiedDate":"2023-11-29T16:40:08.789381","indexId":"70112349","displayToPublicDate":"1990-06-12T15:55:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1843,"text":"Global Tectonics and Metallogeny","active":true,"publicationSubtype":{"id":10}},"title":"Tectolinear interpretation of a 1:5,000,000 Landsat-1 mosaic compared with the structure of central and eastern United States","docAbstract":"<p>The pattern of lineaments and curvilinear features interpreted from a 1:5,000,000 mosaic of satellite images (Landsat-1 was superimposed on a simplified version of the Geological Map of the United States, 1:2,500,000 scale, showing the structural scheme of Central and Eastern United States. A comparison of the above two patterns, shown in Fig. 1, is presented in this paper.</p>","language":"English","publisher":"Schweitzerbart Science Publishers","doi":"10.1127/gtm/1/1978/78","usgsCitation":"Kutina, J., and Carter, W.D., 1978, Tectolinear interpretation of a 1:5,000,000 Landsat-1 mosaic compared with the structure of central and eastern United States: Global Tectonics and Metallogeny, v. 1, no. 1, p. 78-82, https://doi.org/10.1127/gtm/1/1978/78.","productDescription":"5 p.","startPage":"78","endPage":"82","numberOfPages":"5","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288559,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.26275246803011,\n              29.77126505459266\n            ],\n            [\n              -97.11146138111035,\n              48.90789545281613\n            ],\n            [\n              -64.66899459867483,\n              47.321781303225585\n            ],\n            [\n              -79.05645173590027,\n              23.751133665900454\n            ],\n            [\n              -94.26275246803011,\n              29.77126505459266\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc58e4b0e83db6d09023","contributors":{"authors":[{"text":"Kutina, Jan","contributorId":48102,"corporation":false,"usgs":true,"family":"Kutina","given":"Jan","email":"","affiliations":[],"preferred":false,"id":494699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, William D.","contributorId":64567,"corporation":false,"usgs":true,"family":"Carter","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":494700,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70208753,"text":"70208753 - 1978 - Marine diatom sequence in Miocene strata of the Chesapeake Bay region, Maryland","interactions":[],"lastModifiedDate":"2020-03-02T11:49:14","indexId":"70208753","displayToPublicDate":"1978-12-31T12:40:26","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Marine diatom sequence in Miocene strata of the Chesapeake Bay region, Maryland","docAbstract":"<p><span>The Calvert and Choptank Formations exposed along the west shore of Chesapeake Bay in Maryland have been correlated with strata of early and middle Miocene age. The stratigraphic ranges of marine diatom marker species indicate a distinct diatom sequence in the deposits. A few diatoms that mark deep-sea Miocene deposits are found sparingly in these shallow neritic assemblages. Seven diatom zones based on well-recognized events in the diatom biostratigraphy are proposed for the mid-Atlantic region of the eastern United States. A suggested correlation of these zones is made with some of the deep-sea diatom zonations in the Atlantic and Pacific Ocean basins.</span></p>","language":"English","publisher":"Micropaleontology Press","doi":"10.2307/1485369","usgsCitation":"Andrews, G., 1978, Marine diatom sequence in Miocene strata of the Chesapeake Bay region, Maryland: Micropaleontology, v. 24, no. 4, p. 371-406, https://doi.org/10.2307/1485369.","productDescription":"36 p.","startPage":"371","endPage":"406","costCenters":[],"links":[{"id":372705,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Chesapeake Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.7230224609375,\n              38.248965760244644\n            ],\n            [\n              -75.849609375,\n              38.248965760244644\n            ],\n            [\n              -75.849609375,\n              39.65011210186371\n            ],\n            [\n              -76.7230224609375,\n              39.65011210186371\n            ],\n            [\n              -76.7230224609375,\n              38.248965760244644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Andrews, George W.","contributorId":40621,"corporation":false,"usgs":true,"family":"Andrews","given":"George W.","affiliations":[],"preferred":false,"id":783275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207416,"text":"70207416 - 1978 - Metallogenesis in the western United States","interactions":[],"lastModifiedDate":"2019-12-24T10:14:30","indexId":"70207416","displayToPublicDate":"1978-12-31T08:49:46","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2545,"text":"Journal of the Geological Society","active":true,"publicationSubtype":{"id":10}},"title":"Metallogenesis in the western United States","docAbstract":"<p>Although the Mesozoic-Cenozoic metallogeny of the western United States unquestionably resulted from convergence of the North American and Pacific Ocean plates, subduction alone does not adequately explain the distribution of the ore deposits in Laramide and post-Laramide time, when magmatism and mineralization extended irregularly eastward at least 1500 km from the continental margin. Stable isotopes (lead and initial<span>&nbsp;</span><sup>87</sup>Sr/<sup>86</sup>Sr) indicate derivation of some rock- and ore-forming elements from continental rather than oceanic lithosphere. A gross east-west metals zonation lacks the clearcut divisions evident to the north and south in the Cordillera. Lineaments, difficult or impossible to document unequivocally, seem nevertheless to have played some role in localizing mineral belts transverse to plate boundaries.</p><p>It is suggested that mantle convection in a reactivated ensialic back-arc, triggered at least in part by subduction on one or more Benioff Zones, became increasingly important both with time and with distance eastward from the Mesozoic trench. Small magma pockets were generated episodically by partial fusion of the continental lithosphere, itself probably in-homogeneous, where deep crustal flaws, many ancient but some perhaps newly created, relieved pressure and provided access to the upper crust.</p>","language":"English","publisher":"Geological Society of London","doi":"10.1144/gsjgs.135.4.0355","issn":"00167649","usgsCitation":"Guild, P.W., 1978, Metallogenesis in the western United States: Journal of the Geological Society, v. 135, no. 4, p. 355-376, https://doi.org/10.1144/gsjgs.135.4.0355.","productDescription":"22 p.","startPage":"355","endPage":"376","costCenters":[],"links":[{"id":370457,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Western United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -126.298828125,\n              41.44272637767212\n            ],\n            [\n              -118.47656249999999,\n              32.10118973232094\n            ],\n            [\n              -102.74414062499999,\n              30.751277776257812\n            ],\n            [\n              -104.23828125,\n              48.922499263758255\n            ],\n            [\n              -124.18945312500001,\n              50.28933925329178\n            ],\n            [\n              -126.298828125,\n              41.44272637767212\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"135","issue":"4","noUsgsAuthors":false,"publicationDate":"2022-05-04","publicationStatus":"PW","contributors":{"authors":[{"text":"Guild, P. W.","contributorId":39039,"corporation":false,"usgs":true,"family":"Guild","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":777933,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197663,"text":"70197663 - 1978 - Neogene basin formation in relation to plate tectonic evolution of San Andreas fault system, California","interactions":[],"lastModifiedDate":"2023-01-25T15:53:13.892756","indexId":"70197663","displayToPublicDate":"1978-12-31T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Neogene basin formation in relation to plate tectonic evolution of San Andreas fault system, California","docAbstract":"<p>More than 90% of the known petroleum accumulations west of the San Andreas fault in California are in strata deposited in areally restricted Neogene basins that formed during a major tectonic reorganization of western California. These deep, localized Neogene basins replaced broad, regionally persistent Paleogene depositional aprons, although some of the Neogene basins in northern and central California had Paleogene precursors. The evolution of each of the Neogene basins is complex, and aspects of the kinematics of each are unique; nonetheless, all can be considered products of an overall right-lateral shear system associated with a sliding margin between the Pacific and North American lithospheric plates.</p><p>The sliding margin developed in western California about 29 m.y. ago, when the Pacific plate contacted North America after subduction of the intervening Farallon plate. The initial position of the common boundary between the Pacific and North American plates was along the continental margin. Right slip between the Pacific and North American plates gradually shifted eastward to right-slip faults, such as the San Andreas, located farther inland. This shift seems to be documented by relations in the southern California area. About 300 km of right slip has occurred along the San Andreas fault during the past 10 to 15 m.y., and at least several hundred additional kilometers along associated right-slip faults of the San Andreas system.</p><p>The Neogene basins in southern California began to develop during the interval in which the boundary between the Pacific and North American plates shifted from the continental edge to the San Andreas fault, apparently because the step-by-step switch to different surfaces of weakness caused local extension and compression within a broad zone of right-lateral shear. A major phase of basin formation appears to have been synchronous with a change in azimuth of relative shear between the Pacific and North American plates to a more westerly direction, resulting in extensional strain. This change in motion initiated basin development in offshore central and northern California and affected the ongoing development of basins as a result of right slip along the San Andreas and related faults in other parts of California.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/C1EA484C-16C9-11D7-8645000102C1865D","usgsCitation":"Blake, Campbell, R.H., Dibblee, T.W., Howell, D.G., Nilsen, T., Normark, W.R., Vedder, J.G., and Silver, E.A., 1978, Neogene basin formation in relation to plate tectonic evolution of San Andreas fault system, California: American Association of Petroleum Geologists Bulletin, v. 62, no. 3, p. 344-372, https://doi.org/10.1306/C1EA484C-16C9-11D7-8645000102C1865D.","productDescription":"29 p.","startPage":"344","endPage":"372","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science 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R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":738126,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":738127,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Silver, E. A.","contributorId":18491,"corporation":false,"usgs":true,"family":"Silver","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":738128,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70119871,"text":"70119871 - 1978 - The IFG incremental methodology for physical instream habitat evaluation","interactions":[],"lastModifiedDate":"2014-08-11T10:39:10","indexId":"70119871","displayToPublicDate":"1978-12-03T10:38:00","publicationYear":"1978","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"The IFG incremental methodology for physical instream habitat evaluation","largerWorkTitle":"Surface Mining and Fish/Wildlife Needs in the Eastern United States: Proceedings of a Symposium","conferenceTitle":"Surface mining and fish/wildlife needs in the Eastern United States","conferenceDate":"1978-12-03T00:00:00","conferenceLocation":"Morgantown, WV","language":"English","publisher":"Department of the Interior, Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Stalnaker, C., 1978, The IFG incremental methodology for physical instream habitat evaluation.","costCenters":[],"links":[{"id":291942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e9d8d4e4b008eaa4f3f698","contributors":{"authors":[{"text":"Stalnaker, Clair B.","contributorId":30871,"corporation":false,"usgs":true,"family":"Stalnaker","given":"Clair B.","affiliations":[],"preferred":false,"id":497818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156353,"text":"70156353 - 1978 - CS<sub>2</sub> and COS in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Area, Beaver County, Utah","interactions":[],"lastModifiedDate":"2015-08-20T14:26:00","indexId":"70156353","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"CS<sub>2</sub> and COS in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Area, Beaver County, Utah","docAbstract":"<p>Soil-gas samples were collected in two parallel traverses across the Dome fault zone of the Roosevelt Hot Springs Known Geothermal Resource Area. Gas chromatographic analyses of the samples showed anomalous concentrations of CS<sub>3</sub> and COS east of the Dome fault; higher concentrations of CS<sub>2</sub> and COS also occurred over an area in which the hydrothermal system is close to the surface. Measurement of these gases may be useful in exploration for new geothermal sources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Hinkle, M., and Harms, T.F., 1978, CS<sub>2</sub> and COS in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Area, Beaver County, Utah: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 571-578.","productDescription":"8 p.","startPage":"571","endPage":"578","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306996,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":306995,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Roosevelt Hot Springs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.13034057617188,\n              38.28993659801203\n            ],\n            [\n              -113.13034057617188,\n              38.68014968334621\n            ],\n            [\n              -112.66754150390625,\n              38.68014968334621\n            ],\n            [\n              -112.66754150390625,\n              38.28993659801203\n            ],\n            [\n              -113.13034057617188,\n              38.28993659801203\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa30e4b0518e3546bc2e","contributors":{"authors":[{"text":"Hinkle, Margaret","contributorId":36918,"corporation":false,"usgs":true,"family":"Hinkle","given":"Margaret","affiliations":[],"preferred":false,"id":568840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harms, Thelma F.","contributorId":57841,"corporation":false,"usgs":true,"family":"Harms","given":"Thelma","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":568841,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156378,"text":"70156378 - 1978 - Holocene pyroclastic-flow deposits from Shastina and Black Butte, west of Mount Shasta, California","interactions":[],"lastModifiedDate":"2015-08-20T14:29:24","indexId":"70156378","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Holocene pyroclastic-flow deposits from Shastina and Black Butte, west of Mount Shasta, California","docAbstract":"<p>A broad apron of pyroclastic-flow deposits derived from dacitic domes of Holocene age at Black Butte and Shastina covers an area of more than 110 km<sup>2</sup> on the west flank of Mt. Shasta volcano. The stratigraphy of the deposits is exposed in readouts along a northwest-southeast line between the cities of Weed and Mount Shasta and includes, from bottom to top, pre-Shastina diamictons, a Shastina pyroclasticflow assemblage, and a Black Butte pyroclastic-flow assemblage. Pyroclastic flows from Shastina, a volcanic cone on the west flank of Mt. Shasta, form a fan of nonvesicular rock debris that overlies part of the Shastina cone and pre-Shastina deposits; the fan deposits thicken northward and underlie the town of Weed. Pyroclastic-flow deposits of both vesicular and nonvesicular rock debris caused by eruptions at the site of Black Butte, a large volcanic dome at the foot of Mt. Shasta, thicken southward and underlie part of the city of Mount Shasta. Soil-profile oxidation is 75-80 cm thick on deposits from both Shastina and Black Butte. As much as 10 m of vertical displacement occurred along east-trending faults 3.5 km northwest of Black Butte after deposition of the youngest two pyroclastic flows from that source. Evidence that faulting and volcanism were nearly simultaneous suggests that the area northwest of Black Butte subsided during a late eruptive phase of the plug dome. Future eruptions similar to those that produced the pyroclastic flows could endanger people and property in any direction downslope from vents, including the communities of Weed and Mount Shasta and possibly other communities in the Shasta Valley and upper Sacramento River area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Miller, C.D., 1978, Holocene pyroclastic-flow deposits from Shastina and Black Butte, west of Mount Shasta, California: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 611-623.","productDescription":"13 p.","startPage":"611","endPage":"623","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307032,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":307040,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Weed, Mount Shasta","otherGeospatial":"Black Butte, Shastina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.2,\n              41.34\n            ],\n            [\n              -122.2,\n              41.45\n            ],\n            [\n              -122.42,\n              41.45\n            ],\n            [\n              -122.42,\n              41.34\n            ],\n            [\n              -122.2,\n              41.34\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa33e4b0518e3546bc49","contributors":{"authors":[{"text":"Miller, C. Dan","contributorId":38145,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"Dan","affiliations":[],"preferred":false,"id":568943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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