{"pageNumber":"4973","pageRowStart":"124300","pageSize":"25","recordCount":165618,"records":[{"id":7780,"text":"ofr80652 - 1980 - Single-channel seismic-reflection profiles from the Blake Plateau and Blake Outer Ridge, southeastern U.S. continental shelf","interactions":[],"lastModifiedDate":"2024-07-19T22:44:34.547197","indexId":"ofr80652","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-652","title":"Single-channel seismic-reflection profiles from the Blake Plateau and Blake Outer Ridge, southeastern U.S. continental shelf","docAbstract":"<p>Approximately 3,300 kilometers each of airgun and minisparker single-channel seismic-reflection data were collected by the<br>U.S. Geological Survey during the R/V FAY 025 cruise in September and October 1976.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80652","usgsCitation":"Bailey, N.G., and Grow, J.A., 1980, Single-channel seismic-reflection profiles from the Blake Plateau and Blake Outer Ridge, southeastern U.S. continental shelf: U.S. Geological Survey Open-File Report 80-652, 6 p., https://doi.org/10.3133/ofr80652.","productDescription":"6 p.","costCenters":[],"links":[{"id":141237,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0652/report-thumb.jpg"},{"id":431274,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0652/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Blake Outer Ridge, Blake Plateau, southeastern U.S. continental shelf","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.08819979149409,\n              36.44647174085226\n            ],\n            [\n              -81.5534034737089,\n              36.44647174085226\n            ],\n            [\n              -81.5534034737089,\n              28.366589957849328\n            ],\n            [\n              -76.08819979149409,\n              28.366589957849328\n            ],\n            [\n              -76.08819979149409,\n              36.44647174085226\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1a49","contributors":{"authors":[{"text":"Bailey, Norman G.","contributorId":59439,"corporation":false,"usgs":true,"family":"Bailey","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grow, John A.","contributorId":25943,"corporation":false,"usgs":true,"family":"Grow","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7057,"text":"ofr80267 - 1980 - Coal drilling during 1978 in Big Horn, Daniels, Dawson, Musselshell, Richland, Roosevelt, Rosebud, Valley, and Yellowstone counties, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr80267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-267","title":"Coal drilling during 1978 in Big Horn, Daniels, Dawson, Musselshell, Richland, Roosevelt, Rosebud, Valley, and Yellowstone counties, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80267","usgsCitation":"Montana Bureau of Mines and Geology, and Water Resources Division, U.S. Geological Survey, 1980, Coal drilling during 1978 in Big Horn, Daniels, Dawson, Musselshell, Richland, Roosevelt, Rosebud, Valley, and Yellowstone counties, Montana: U.S. Geological Survey Open-File Report 80-267, 273 p.  :maps ;28 cm., https://doi.org/10.3133/ofr80267.","productDescription":"273 p.  :maps ;28 cm.","costCenters":[],"links":[{"id":140588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0267/report-thumb.jpg"},{"id":34353,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0267/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5ddfad","contributors":{"authors":[{"text":"Montana Bureau of Mines and Geology","contributorId":128110,"corporation":true,"usgs":false,"organization":"Montana Bureau of Mines and Geology","id":528811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7789,"text":"ofr80960 - 1980 - Water resources and geology of the Los Coyotes Indian Reservation and vicinity, San Diego County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr80960","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-960","title":"Water resources and geology of the Los Coyotes Indian Reservation and vicinity, San Diego County, California","docAbstract":"The water resources of the Los Coyotes Indian Reservation, San Diego County, Calif., are sufficient to supply the limited domestic and stock-water needs of the present residents of the reservation. Surface-water runoff is derived from direct precipitation on the area and from intermittent spring flow. Groundwater occurs in the alluvial deposits and in the consolidated rocks where they are highly fractured or deeply weathered. The best potential for groundwater development on the reservation is in the small alluvial basins in the San Ysidro and San Ignacio areas. Most water on the reservation is good to excellent in chemical quality for domestic, stock, and irrigation use. Water from two wells (and one spring), however, exceeds the primary drinking-water standard for nitrate plus nitrate. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80960","usgsCitation":"Ballog, A., and Moyle, W.R., 1980, Water resources and geology of the Los Coyotes Indian Reservation and vicinity, San Diego County, California (WRI/OFR): U.S. Geological Survey Open-File Report 80-960, iv, 29 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr80960.","productDescription":"iv, 29 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0960/report-thumb.jpg"},{"id":35287,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0960/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35288,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0960/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0960/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6281c8","contributors":{"authors":[{"text":"Ballog, A.P. Jr.","contributorId":23950,"corporation":false,"usgs":true,"family":"Ballog","given":"A.P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":156602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moyle, W. R. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":156603,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6343,"text":"pp1098 - 1980 - Flood of April 1977 in the Appalachian region of Kentucky, Tennessee, Virginia, and West Virginia","interactions":[{"subject":{"id":49345,"text":"ofr7814 - 1978 - Flood of April 1977, Kentucky, Tennessee, Virginia, and West Virginia","indexId":"ofr7814","publicationYear":"1978","noYear":false,"title":"Flood of April 1977, Kentucky, Tennessee, Virginia, and West Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":6343,"text":"pp1098 - 1980 - Flood of April 1977 in the Appalachian region of Kentucky, Tennessee, Virginia, and West Virginia","indexId":"pp1098","publicationYear":"1980","noYear":false,"title":"Flood of April 1977 in the Appalachian region of Kentucky, Tennessee, Virginia, and West Virginia"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"pp1098","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1098","title":"Flood of April 1977 in the Appalachian region of Kentucky, Tennessee, Virginia, and West Virginia","docAbstract":"Heavy rains fell over the Appalachian region of Kentucky, Tennessee, Virginia and West Virginia April 2-5, 1977, causing record flooding. Rainfall amounts of 4 to 15.5 inches were observed. The maximum amount of 15.5 inches occurred at Jolo, WV , in about 30 hours. This was more than twice the amount which would be expected for a 100-year recurrence-interval storm. Flood discharges along the upper Guyandotte River; Tug Fork and Levisa Fork in the Big Sandy River basin; Cumberland River; and Clinch River and Dowell River in the Tennessee River basin exceeded those previously known. Severe flooding also occurred along the Holston River and along the North Fork Kentucky River. Recurrence intervals of observed flood discharges were greater than 100-years at 29 streamflow measurement sites. Substantial reductions in peak stages and discharges on Levisa Fork, North Pound River, and Guyandotte River, attained as a result of reservoir storage, were reported by U.S. Army Corps of Engineers. Maximum daily suspended-sediment discharges on Guyandotte River near Baileysville, WV, and Tug Fork at Glenhayes, WV, were 54,800 tons/day and 290,000 tons/day, respectively, April 5, 1977. Twenty-two lives were lost and total property damage reportedly exceeded $400 million in the four-State area. (USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1098","usgsCitation":"Runner, G.S., and Chin, E.H., 1980, Flood of April 1977 in the Appalachian region of Kentucky, Tennessee, Virginia, and West Virginia: U.S. Geological Survey Professional Paper 1098, 43 p., https://doi.org/10.3133/pp1098.","productDescription":"43 p.","costCenters":[],"links":[{"id":124003,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1098/report-thumb.jpg"},{"id":33683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1098/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eecc0","contributors":{"authors":[{"text":"Runner, Gerald S.","contributorId":90297,"corporation":false,"usgs":true,"family":"Runner","given":"Gerald","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":152552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chin, Edwin H.","contributorId":87921,"corporation":false,"usgs":true,"family":"Chin","given":"Edwin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":152551,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5957,"text":"pp1116 - 1980 - Geochemical-exploration studies in the Coeur d'Alene district, Idaho and Montana","interactions":[{"subject":{"id":9192,"text":"ofr77216 - 1977 - Geochemical exploration studies in the Coeur d'Alene district, Idaho","indexId":"ofr77216","publicationYear":"1977","noYear":false,"title":"Geochemical exploration studies in the Coeur d'Alene district, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":5957,"text":"pp1116 - 1980 - Geochemical-exploration studies in the Coeur d'Alene district, Idaho and Montana","indexId":"pp1116","publicationYear":"1980","noYear":false,"title":"Geochemical-exploration studies in the Coeur d'Alene district, Idaho and Montana"},"id":1}],"lastModifiedDate":"2021-11-09T21:12:31.338469","indexId":"pp1116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1116","title":"Geochemical-exploration studies in the Coeur d'Alene district, Idaho and Montana","docAbstract":"The principal ore deposits in the Coeur d'Alene district are lead-zinc-silver replacement veins in Precambrian rocks of the Belt Supergroup. The main ore minerals are galena, tetrahedrite, and sphalerite. The host rocks are mainly quartzite, siltite, and argillite. Cretaceous quartz monzonite locally intrudes the Beltrocks. \r\n\r\nThe geochemical investigations reported here were carried out to determine if geochemical methods would be useful in the search for concealed ore deposits. About 8,700 soil samples and 4,000 rock samples were collected from a 300-square-mile (780 square kilometer) area for this study. The samples were analyzed for 35 elements. \r\n\r\nAntimony, silver, lead, manganese, and copper form dispersion patterns and halos that are related to many of the ore deposits within the district, and these same elements were found to be most useful in delineating the known mineral belts that contain most of the orebodies. The dispersion patterns are probably primary, having only minor modifications due to secondary redistribution of the ore-forming elements. \r\n\r\nThe mineral belts and geochemical-dispersion patterns have been laterally offset, perhaps as much as 16 miles (26 km), by postore faulting. Prefault dispersion patterns can be restored by adjusting the geochemical maps along the postore faults to match the dispersion patterns across the fault trace. The reconstructed dispersion patterns of antimony, arsenic, lead, sulfur, and the ratio of cadmium to zinc form concentric halos around the restored position of the Gem stocks. Most of the Coeur d'Alene ore has been mined from this halo. It appears that the geochemical exploration methods reported here successfully delineate the major mineral belts and indicate unexplored areas in which to search for new deposits.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1116","usgsCitation":"Gott, G.B., and Cathrall, J.B., 1980, Geochemical-exploration studies in the Coeur d'Alene district, Idaho and Montana: U.S. Geological Survey Professional Paper 1116, Report: iv, 63 p.; 9 Plates: 41.00 × 39.50 inches or smaller, https://doi.org/10.3133/pp1116.","productDescription":"Report: iv, 63 p.; 9 Plates: 41.00 × 39.50 inches or smaller","costCenters":[],"links":[{"id":32852,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-9.pdf","text":"Plate 7-3","linkFileType":{"id":1,"text":"pdf"}},{"id":32851,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-8.pdf","text":"Plate 7-2","linkFileType":{"id":1,"text":"pdf"}},{"id":32850,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-7.pdf","text":"Plate 7-1","linkFileType":{"id":1,"text":"pdf"}},{"id":124887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1116/report-thumb.jpg"},{"id":32845,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104554,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4723.htm","linkFileType":{"id":5,"text":"html"},"description":"4723"},{"id":32853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32849,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32844,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32848,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32847,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32846,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1116/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Montana","otherGeospatial":"Coeur d'Alene district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.2792,\n              47.35\n            ],\n            [\n              -115.5,\n              47.35\n            ],\n            [\n              -115.5,\n              47.5833\n            ],\n            [\n              -116.2792,\n              47.5833\n            ],\n            [\n              -116.2792,\n              47.35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab7f7","contributors":{"authors":[{"text":"Gott, Garland Bayard","contributorId":6420,"corporation":false,"usgs":true,"family":"Gott","given":"Garland","email":"","middleInitial":"Bayard","affiliations":[],"preferred":false,"id":151872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cathrall, John B.","contributorId":26668,"corporation":false,"usgs":true,"family":"Cathrall","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":151873,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7276,"text":"ofr80313 - 1980 - Lassen Known Geothermal Resource Area, California: Audio-magnetotelluric telluric profiling, and self-potential studies","interactions":[],"lastModifiedDate":"2021-08-24T16:42:48.627","indexId":"ofr80313","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-313","title":"Lassen Known Geothermal Resource Area, California: Audio-magnetotelluric telluric profiling, and self-potential studies","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80313","usgsCitation":"Christopherson, K.R., Hoover, D., Lewis, V., Radtke, B., and Senterfit, R.M., 1980, Lassen Known Geothermal Resource Area, California: Audio-magnetotelluric telluric profiling, and self-potential studies: U.S. Geological Survey Open-File Report 80-313, 28 p., https://doi.org/10.3133/ofr80313.","productDescription":"28 p.","costCenters":[],"links":[{"id":388425,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75238.htm"},{"id":34653,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0313/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0313/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Lassen Known Geothermal Resource Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.5833,\n              40.3333\n            ],\n            [\n              -121.25,\n              40.3333\n            ],\n            [\n              -121.25,\n              40.5\n            ],\n            [\n              -121.5833,\n              40.5\n            ],\n            [\n              -121.5833,\n              40.3333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d86","contributors":{"authors":[{"text":"Christopherson, Karen R.","contributorId":91092,"corporation":false,"usgs":true,"family":"Christopherson","given":"Karen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":155006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoover, D.B.","contributorId":37734,"corporation":false,"usgs":true,"family":"Hoover","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":155004,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, Vernon","contributorId":30984,"corporation":false,"usgs":true,"family":"Lewis","given":"Vernon","email":"","affiliations":[],"preferred":false,"id":155003,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Radtke, Bruce","contributorId":77149,"corporation":false,"usgs":true,"family":"Radtke","given":"Bruce","email":"","affiliations":[],"preferred":false,"id":155005,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Senterfit, R. Michael","contributorId":10791,"corporation":false,"usgs":true,"family":"Senterfit","given":"R.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":155002,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7980,"text":"ofr801245 - 1980 - Exploratory trench across the Pleasant Valley Fault, Nevada","interactions":[],"lastModifiedDate":"2012-06-07T01:01:38","indexId":"ofr801245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1245","title":"Exploratory trench across the Pleasant Valley Fault, Nevada","docAbstract":"An exploratory trench was excavated across the 1915 trace of the Pleasant Valley fault 60 km south of Winnemucca, Nevada, to get information on the history of recent displacements on a fault that had produced a major earthquake in historic time, and on the appearance of such a fault in a trench cut in gravels, sands and silts of an alluvial fan. The trench exposed 16 mappable sedimentary units and four soils, including three buried paleosols. The ages of the mapped units could not be narrowly defined but they are of late Quaternary age. Some rodent bones suggest a possible age of about 5,000 years for one of the higher stratigraphic units. The fault zone is very clearly represented in the trench, and, to the full 4-m depth of the trench, consists of a zone of fault rubble as much as 1.5 m wide. Two fractures outside the fault rubble show no vertical displacement. In addition to the fault rubble, the fault is conspicuous because several of the mapped units terminate abruptly against the rubble zone, and because the sediments southeast of the zone are coarser-grained than the sediments northwest of the zone. Maximum vertical component of the 1915 displacement was estimated to be 0.4&ndash;0.6 m based on topography and 0.5&ndash;0.6 m based on displacement of stratigraphic units including soils. Two or more episodes of vertical displacement, one of about 0.3 m and another totaling at least 1.15 m prior to 1915 are recorded and may have occurred in the last 5,000 years. These and other displacement events prior to 1915 are poorly dated, but that several did occur in late Pleistocene and Holocene time is certain. Lack of wedge-shaped deposits or concentrations of large clasts adjacent to the fault suggest that all displacements were produced in small increments of probably less than one meter each.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801245","usgsCitation":"Bonilla, M.G., Villalobos, H.A., and Wallace, R.E., 1980, Exploratory trench across the Pleasant Valley Fault, Nevada: U.S. Geological Survey Open-File Report 80-1245, 24 p.; Tables; Figures; 1 Plate: 23.70 x 11 inches, https://doi.org/10.3133/ofr801245.","productDescription":"24 p.; Tables; Figures; 1 Plate: 23.70 x 11 inches","startPage":"1","endPage":"34","numberOfPages":"34","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":140334,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_80_1245.gif"},{"id":257251,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1980/1245/","linkFileType":{"id":5,"text":"html"}},{"id":257252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1245/of80-1245_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":257253,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1245/of80-1245_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Pleasant Valley Fault","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c14","contributors":{"authors":[{"text":"Bonilla, Manuel G.","contributorId":74384,"corporation":false,"usgs":true,"family":"Bonilla","given":"Manuel","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Villalobos, H. A.","contributorId":8133,"corporation":false,"usgs":true,"family":"Villalobos","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156928,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallace, R. E.","contributorId":6823,"corporation":false,"usgs":true,"family":"Wallace","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":156927,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7143,"text":"ofr80785 - 1980 - Gamma-ray spectrometric and semiquantitative spectrographic analytical data of the thorium and rare-earth disseminated deposits in the southern Bear Lodge Mountains, Wyoming","interactions":[],"lastModifiedDate":"2022-09-01T20:10:11.960411","indexId":"ofr80785","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-785","title":"Gamma-ray spectrometric and semiquantitative spectrographic analytical data of the thorium and rare-earth disseminated deposits in the southern Bear Lodge Mountains, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80785","usgsCitation":"Staatz, M.H., Conklin, N.M., Bunker, C., and Bush, C.A., 1980, Gamma-ray spectrometric and semiquantitative spectrographic analytical data of the thorium and rare-earth disseminated deposits in the southern Bear Lodge Mountains, Wyoming: U.S. Geological Survey Open-File Report 80-785, Report: 47 p.; 1 Plate: 21.21 × 25.39 inches, https://doi.org/10.3133/ofr80785.","productDescription":"Report: 47 p.; 1 Plate: 21.21 × 25.39 inches","costCenters":[],"links":[{"id":34453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0785/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34452,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0785/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0785/report-thumb.jpg"},{"id":406094,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75294.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","otherGeospatial":"southern Bear Lodge Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.4911,\n              44.4458\n            ],\n            [\n              -104.4131,\n              44.4458\n            ],\n            [\n              -104.4131,\n              44.5214\n            ],\n            [\n              -104.4911,\n              44.5214\n            ],\n            [\n              -104.4911,\n              44.4458\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b13d0","contributors":{"authors":[{"text":"Staatz, Mortimer Hay","contributorId":39754,"corporation":false,"usgs":true,"family":"Staatz","given":"Mortimer","email":"","middleInitial":"Hay","affiliations":[],"preferred":false,"id":154463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conklin, Nancy M.","contributorId":106108,"corporation":false,"usgs":true,"family":"Conklin","given":"Nancy","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":154465,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bunker, Carl M.","contributorId":45311,"corporation":false,"usgs":true,"family":"Bunker","given":"Carl M.","affiliations":[],"preferred":false,"id":154464,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bush, Charles A. cbush@usgs.gov","contributorId":1258,"corporation":false,"usgs":true,"family":"Bush","given":"Charles","email":"cbush@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":154462,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7371,"text":"ofr802010 - 1980 - Overconsolidated surficial sediment on the Beaufort Sea shelf","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr802010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-2010","title":"Overconsolidated surficial sediment on the Beaufort Sea shelf","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr802010","usgsCitation":"Reimnitz, E., Kempema, E., Ross, R., and Minkler, P., 1980, Overconsolidated surficial sediment on the Beaufort Sea shelf: U.S. Geological Survey Open-File Report 80-2010, 37 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr802010.","productDescription":"37 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2010/report-thumb.jpg"},{"id":34770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a30b","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":155442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kempema, Edward","contributorId":49353,"corporation":false,"usgs":true,"family":"Kempema","given":"Edward","email":"","affiliations":[],"preferred":false,"id":155444,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, Robin","contributorId":36547,"corporation":false,"usgs":true,"family":"Ross","given":"Robin","email":"","affiliations":[],"preferred":false,"id":155443,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minkler, Peter","contributorId":8846,"corporation":false,"usgs":true,"family":"Minkler","given":"Peter","email":"","affiliations":[],"preferred":false,"id":155441,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7974,"text":"ofr801300 - 1980 - Digital model simulation of the hydrologic flow system, with emphasis on ground water in Spokane Valley, Washington and Idaho","interactions":[],"lastModifiedDate":"2019-05-10T13:27:52","indexId":"ofr801300","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1300","title":"Digital model simulation of the hydrologic flow system, with emphasis on ground water in Spokane Valley, Washington and Idaho","docAbstract":"<p>A digital-computer model of the hydrologic flow system, with emphasis on ground water, was developed for Spokane Valley, Washington and Idaho. The current rate of ground-water pumping in Spokane Valley has little effect on water levels in the Spokane aquifer, although short-term water-level declines occur locally. The model was used to show the effects of increased ground-water pumpage on aquifer heads and streamflow. A simulated pumping rate twice that of actual 1977 pumping rates of 227 cubic feet per second lowered water levels in the Spokane aquifer less than 3 feet during a 1-year simulation period. This doubling of the ground water pumpage caused a decrease in discharge of the Spokane River, as measured at Spokane, of about 150 cubic feet per second during the summer months and about 50 cubic feet per second during the rest of the year. Leakage from the aquifer to the Little Spokane River was decreased by less than 10 cubic feet per second. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801300","collaboration":"Prepared in cooperation with State of Washington Department of Ecology and Spokane Engineers Office","usgsCitation":"Bolke, E., and Washington, J., 1980, Digital model simulation of the hydrologic flow system, with emphasis on ground water in Spokane Valley, Washington and Idaho (WRI/OFR): U.S. Geological Survey Open-File Report 80-1300, v, 43 p., https://doi.org/10.3133/ofr801300.","productDescription":"v, 43 p.","costCenters":[],"links":[{"id":363671,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1300/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1300/report-thumb.jpg"}],"country":"United States","state":"Idaho, Washington","otherGeospatial":"Spokane Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.71301269531249,\n              47.544090665057986\n            ],\n            [\n              -116.89590454101562,\n              47.544090665057986\n            ],\n            [\n              -116.89590454101562,\n              47.91173983456231\n            ],\n            [\n              -117.71301269531249,\n              47.91173983456231\n            ],\n            [\n              -117.71301269531249,\n              47.544090665057986\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65ab28","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":156917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Washington, J.J.","contributorId":93044,"corporation":false,"usgs":true,"family":"Washington","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":156918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7963,"text":"ofr8084 - 1980 - Chemical analyses of fruits, vegetables, and their associated soils from areas of commercial production in the conterminous United States","interactions":[],"lastModifiedDate":"2014-07-10T09:36:09","indexId":"ofr8084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-84","title":"Chemical analyses of fruits, vegetables, and their associated soils from areas of commercial production in the conterminous United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8084","usgsCitation":"Boerngen, J.G., and Shacklette, H.T., 1980, Chemical analyses of fruits, vegetables, and their associated soils from areas of commercial production in the conterminous United States: U.S. Geological Survey Open-File Report 80-84, ii, 135 p. ;28 cm., https://doi.org/10.3133/ofr8084.","productDescription":"ii, 135 p. ;28 cm.","costCenters":[],"links":[{"id":140250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0084/report-thumb.jpg"},{"id":289702,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0084/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ad6","contributors":{"authors":[{"text":"Boerngen, Josephine G.","contributorId":31750,"corporation":false,"usgs":true,"family":"Boerngen","given":"Josephine","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shacklette, Hansford Threlkeld","contributorId":94660,"corporation":false,"usgs":true,"family":"Shacklette","given":"Hansford","email":"","middleInitial":"Threlkeld","affiliations":[],"preferred":false,"id":156897,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5804,"text":"pp954F - 1980 - Geochemistry of bedrock units in Missouri and parts of adjacent states","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"pp954F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"954","chapter":"F","title":"Geochemistry of bedrock units in Missouri and parts of adjacent states","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geochemical survey of Missouri","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp954F","usgsCitation":"Connor, J.J., and Ebens, R.J., 1980, Geochemistry of bedrock units in Missouri and parts of adjacent states: U.S. Geological Survey Professional Paper 954, 54 p., https://doi.org/10.3133/pp954F.","productDescription":"54 p.","costCenters":[],"links":[{"id":117723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0954f/report-thumb.jpg"},{"id":32488,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0954f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab5d1","contributors":{"authors":[{"text":"Connor, Jon J.","contributorId":21948,"corporation":false,"usgs":true,"family":"Connor","given":"Jon","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":151607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ebens, Richard John","contributorId":27439,"corporation":false,"usgs":true,"family":"Ebens","given":"Richard","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":151608,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6230,"text":"pp1145 - 1980 - Paleozoic and Mesozoic deformations in the central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1145","title":"Paleozoic and Mesozoic deformations in the central Sierra Nevada, California","docAbstract":"Analysis of structural and stratigraphic data indicates that several periods of regional deformation, consisting of combined folding, faulting, cataclasis, and regional metamorphism, occurred throughout the central Sierra Nevada during Paleozoic and Mesozoic time. The oldest regional deformation occurred alono northward trends during the Devonian and Mississippian periods in most roof pendants containing lower Paleozoic metasedimentary rocks at the center and along the crest of the range. This deformation is expressed in some roof pendants by an angular unconformity separating older thrice-deformed from younger twice-deformed Paleozoic metasedimentary rocks. \r\n\r\nThe first Mesozoic deformation, which consisted of uplift and erosion and was accompanied by the onset of Andean-type volcanism during the Permian and Triassic, is expressed by an angular unconformity in several roof pendants from the Saddlebag Lake to the Mount Morrison areas. This unconformity is defined by Permian and Triassic andesitic to rhyolitic metavolcanic rocks unconformably overlying more intensely deformed Pennsylvanian, Permian(?), and older metasedimentary rocks. A later regional deformation occurred during the Triassic along N. 20?_30? W. trends in Permian and Triassic metavolcanic rocks of the Saddlebag Lake and Mount Dana roof pendants, in upper Paleozoic rocks of the Pine Creek roof pendant, and in the Calaveras Formation of the western metamorphic belt; the roof pendants are crosscut by Upper Triassic granitic rocks of the Lee Vining intrusive epoch. A still later period of Early and Middle Jurassic regional deformation occurred along N. 30?-60? E. trends in upper Paleozoic rocks of the Calaveras Formation of the western metamorphic belt. A further period of deformation was the Late Jurassic Nevadan orogeny, which occurred along N. 20?_40? W. trends in Upper Jurassic rocks of the western metamorphic belt that are crosscut by Upper Jurassic granitic rocks of the Yosemite intrusive epoch. Structures of similar age occur in intensely deformed oceanic-lithospheric and syntectonic plutonic rocks of the lower Kings River area, in Jurassic metavolcanic rocks of the Ritter Range roof pendant, and in Triassic metasedimentary rocks of the Mineral King roof pendant. The final Mesozoic deformation occurred along N. 50?-80? W. trends in both high-country roof pendants and the lower Kings River area; structures of this generation are crosscut by relatively undeformed Upper Cretaceous granitic rocks of the Cathedral Range intrusive epoch.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1145","usgsCitation":"Nokleberg, W.J., and Kistler, R.W., 1980, Paleozoic and Mesozoic deformations in the central Sierra Nevada, California: U.S. Geological Survey Professional Paper 1145, 24 p., https://doi.org/10.3133/pp1145.","productDescription":"24 p.","costCenters":[],"links":[{"id":124949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1145/report-thumb.jpg"},{"id":33435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688604","contributors":{"authors":[{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":152346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kistler, Ronald Wayne","contributorId":27857,"corporation":false,"usgs":true,"family":"Kistler","given":"Ronald","email":"","middleInitial":"Wayne","affiliations":[],"preferred":false,"id":152347,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7911,"text":"ofr80384 - 1980 - Schlumberger soundings in the Fish Springs Flat area, Juab County, Utah","interactions":[],"lastModifiedDate":"2022-10-25T19:42:02.707209","indexId":"ofr80384","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-384","title":"Schlumberger soundings in the Fish Springs Flat area, Juab County, Utah","docAbstract":"<p>In 1978 the U. S. Geological Survey made 43 Schlumberger soundings in the Fish Springs Flat area, Juab County, Utah. The purpose of this survey was to delineate water quality and obtain structural information. Fish Springs Flat consists mainly of Quaternery deposits of sand, gravel, clay, and silt. On the west Fish Springs Flat is bordered by the Fish Springs Range which is composed primarily of Paleozoic limestone. With the exception of a short section of metal fence and concrete culverts, disruptive cultural features did not appear to be present.</p><p>The purpose of this report is to release the field data obtained in this survey. In addition the automatic inversion of the sounding curves, computer-generated geoelectric cross sections, and interpreted resistivity maps are also given and briefly described.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80384","usgsCitation":"Bisdorf, R.J., and Zohdy, A.A., 1980, Schlumberger soundings in the Fish Springs Flat area, Juab County, Utah: U.S. Geological Survey Open-File Report 80-384, 73 p., https://doi.org/10.3133/ofr80384.","productDescription":"73 p.","costCenters":[],"links":[{"id":408712,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0384/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0384/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Juab County","otherGeospatial":"Fish Springs Flat area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0478,39.3132 ], [ -114.0478,40.0112 ], [ -111.583,40.0112 ], [ -111.583,39.3132 ], [ -114.0478,39.3132 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd44a","contributors":{"authors":[{"text":"Bisdorf, Robert J.","contributorId":107277,"corporation":false,"usgs":true,"family":"Bisdorf","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":156821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zohdy, Adel A. R.","contributorId":61799,"corporation":false,"usgs":true,"family":"Zohdy","given":"Adel","email":"","middleInitial":"A. R.","affiliations":[],"preferred":false,"id":156820,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5874,"text":"pp1177A - 1980 - Geographical analysis of Fenwick Island, Maryland, a middle Atlantic coast barrier island","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"pp1177A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1177","chapter":"A","title":"Geographical analysis of Fenwick Island, Maryland, a middle Atlantic coast barrier island","language":"ENGLISH","publisher":"GPO : for sale by the Supt. of Docs.,","doi":"10.3133/pp1177A","usgsCitation":"Dolan, R., Lins, H.F., and Stewart, J., 1980, Geographical analysis of Fenwick Island, Maryland, a middle Atlantic coast barrier island: U.S. Geological Survey Professional Paper 1177, 24 p., https://doi.org/10.3133/pp1177A.","productDescription":"24 p.","costCenters":[],"links":[{"id":117258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1177a/report-thumb.jpg"},{"id":32694,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1177a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8fcb","contributors":{"authors":[{"text":"Dolan, Robert","contributorId":16405,"corporation":false,"usgs":true,"family":"Dolan","given":"Robert","email":"","affiliations":[],"preferred":false,"id":151720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":151719,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stewart, John","contributorId":71966,"corporation":false,"usgs":true,"family":"Stewart","given":"John","affiliations":[],"preferred":false,"id":151721,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7897,"text":"ofr811032 - 1980 - Machine-generated displays of well logs and lithology from selected wells on the North Slope of Alaska; 10 wells from the western part of the National Petroleum Reserve in Alaska (NPRA)","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr811032","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"81-1032","title":"Machine-generated displays of well logs and lithology from selected wells on the North Slope of Alaska; 10 wells from the western part of the National Petroleum Reserve in Alaska (NPRA)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811032","usgsCitation":"Bird, K.J., 1980, Machine-generated displays of well logs and lithology from selected wells on the North Slope of Alaska; 10 wells from the western part of the National Petroleum Reserve in Alaska (NPRA): U.S. Geological Survey Open-File Report 81-1032, 7 p., 10 over-size sheets, ill., map ;28 cm., https://doi.org/10.3133/ofr811032.","productDescription":"7 p., 10 over-size sheets, ill., map ;28 cm.","costCenters":[],"links":[{"id":140046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1032/report-thumb.jpg"},{"id":35418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1032/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db649033","contributors":{"authors":[{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":156802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5878,"text":"pp1090 - 1980 - Ordovician and Silurian Phi Kappa and Trail Creek formations, Pioneer Mountains, central Idaho: Stratigraphic and structural revisions, and new data on graptolite faunas","interactions":[],"lastModifiedDate":"2023-08-29T20:47:29.939707","indexId":"pp1090","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1090","title":"Ordovician and Silurian Phi Kappa and Trail Creek formations, Pioneer Mountains, central Idaho: Stratigraphic and structural revisions, and new data on graptolite faunas","docAbstract":"Recent geologic mapping in the northern Pioneer Mountains combined with the identification of graptolites from 116 new collections indicate that the Ordovician and Silurian Phi Kappa and Trail Creek Formations occur in a series of thrust-bounded slices within a broad zone of imbricate thrust faulting. Though confirming a deformational style first reported in a 1963 study by Michael Churkin, our data suggest that the complexity and regional extent of the thrust zone were not previously recognized. Most previously published sections of the Phi Kappa and Trail Creek Formations were measured across unrecognized thrust faults and therefore include not only structural repetitions of graptolitic Ordovician and Silurian rocks but also other tectonically juxtaposed lithostratigraphic units of diverse ages as well. Because of this discovery, the need to reconsider the stratigraphic validity of these formations and their lithology, nomenclature, structural distribution, facies relations, and graptolite faunas has arisen. \r\n\r\nThe Phi Kappa Formation in most thrust slices has internal stratigraphic continuity despite the intensity of deformation to which it was subjected. As revised herein, the Phi Kappa Formation is restricted to a structurally repeated succession of predominantly black, carbonaceous, graptolitic argillite and shale. Some limy, light-gray-weathering shale occurs in the middle part of the section, and fine-grained locally pebbly quartzite is present at the base. The basal quartzite is here named the Basin Gulch Quartzite Member of the Phi Kappa. The Phi Kappa redefined on a lithologic basis represents the span of Ordovician time from W. B. N. Berry's graptolite zones 2-4 through 15 and also includes approximately 17 m of lithologically identical shale of Early and Middle Silurian age at the top. The lower contact of the formation as revised is tectonic. The Phi Kappa is gradationally overlain by the Trail Creek Formation as restricted herein. Most of the coarser clastic rocks reported in previously measured sections of the Phi Kappa, as well as the sequence along Phi Kappa Creek from which the name originates, are excluded from the Phi Kappa as revised and are reassigned to two structural plates of Mississippian Copper Basin Formation; other strata now excluded from the formation are reassigned to the Trail Creek Formation and to an unnamed Silurian and Devonian unit. As redefined, the Phi Kappa Formation is only about 240 m thick, compared with the 3,860 m originally estimated, and it occupies only about 25 percent of the outcrop area previously mapped in 1930 by H. G. Westgate and C. P. Ross. Despite this drastic reduction in thickness and the exclusion of the rocks along Phi Kappa Creek, the name Phi Kappa is retained because of widely accepted prior usage to denote the Ordovician graptolitic shale facies of central Idaho, and because the Phi Kappa Formation as revised is present in thrust slices on Phi Kappa Mountain, at the head of Phi Kappa Creek. The lithic and faunal consistency of this unit throughout the area precludes the necessity for major facies telescoping along individual faults within the outcrop belt. However, tens of kilometers of tectonic shortening seems required to juxtapose the imbricated Phi Kappa shale facies with the Middle Ordovician part of the carbonate and quartzite shale sequence of east central Idaho. The shelf rocks are exposed in the Wildhorse structural window of the northeastern Pioneer Mountains, and attain a thickness of at least 1,500 m throughout the region north and east of the Pioneer Mountains. The Phi Kappa is in direct thrust contact on intensely deformed medium- to high-grade metamorphic equivalents of the same shelf sequence in the Pioneer window at the south end of the Phi Kappa-Trail Creek outcrop belt. Along East Pass, Big Lake, and Pine Creeks, north of the Pioneer Mountains, some rocks previously mapped as Ramshorn Slate are lithologically and faunally equivalent to the P","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1090","usgsCitation":"Dover, J.H., Berry, W.B., and Ross, R.J., 1980, Ordovician and Silurian Phi Kappa and Trail Creek formations, Pioneer Mountains, central Idaho: Stratigraphic and structural revisions, and new data on graptolite faunas: U.S. Geological Survey Professional Paper 1090, Report: vi, 54 p.; 1 Plate: 29.00 x 39.00 inches, https://doi.org/10.3133/pp1090.","productDescription":"Report: vi, 54 p.; 1 Plate: 29.00 x 39.00 inches","costCenters":[],"links":[{"id":104549,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4718.htm","linkFileType":{"id":5,"text":"html"},"description":"4718"},{"id":32698,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1090/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32699,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1090/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121437,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1090/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Pioneer Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.3333,\n              43.9297\n            ],\n            [\n              -114.3333,\n              43.7728\n            ],\n            [\n              -114.1667,\n              43.7728\n            ],\n            [\n              -114.1667,\n              43.9297\n            ],\n            [\n              -114.3333,\n              43.9297\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635245","contributors":{"authors":[{"text":"Dover, James H.","contributorId":43382,"corporation":false,"usgs":true,"family":"Dover","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":151728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, William B. N.","contributorId":76372,"corporation":false,"usgs":true,"family":"Berry","given":"William","email":"","middleInitial":"B. N.","affiliations":[],"preferred":false,"id":151729,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, Reuben James Jr.","contributorId":36911,"corporation":false,"usgs":true,"family":"Ross","given":"Reuben","suffix":"Jr.","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":151727,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5881,"text":"pp1101 - 1980 - The Boulder Creek Batholith, Front Range, Colorado","interactions":[{"subject":{"id":14095,"text":"ofr6570 - 1965 - Allanites from the Boulder Creek batholith, Colorado","indexId":"ofr6570","publicationYear":"1965","noYear":false,"title":"Allanites from the Boulder Creek batholith, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":5881,"text":"pp1101 - 1980 - The Boulder Creek Batholith, Front Range, Colorado","indexId":"pp1101","publicationYear":"1980","noYear":false,"title":"The Boulder Creek Batholith, Front Range, Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"pp1101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1101","title":"The Boulder Creek Batholith, Front Range, Colorado","docAbstract":"The Boulder Creek batholith is the best known of several large Precambrian batholiths of similar rock composition that crop out across central Colorado. The rocks in the batholith belong to the calc-alkaline series and range in composition from granodiorite through quartz diorite (tonalite) to gneissic aplite. Two rock types dominate': the Boulder Creek Granodiorite, the major rock unit, and a more leucocratic and slightly younger unit herein named Twin Spruce Quartz Monzonite. Besides mafic inclusions, which occur mainly in hornblende-bearing phases of the Boulder Creek Granodiorite, there are cogenetic older and younger lenses, dikes, and small plutons of hornblende diorite, hornblendite, gabbro, and pyroxenite. Pyroxenite is not found in the batholith. The Boulder Creek Granodiorite in the batholith represents essentially two contemporaneous magmas, a northern body occurring in the Gold Hill and Boulder quadrangles and a larger southern body exposed in the Blackhawk and the greater parts of the Tungsten and Eldorado Springs quadrangles. The two bodies are chemically and mineralogically distinct. The northern body is richer in CaO and poorer in K2O, is more mafic, and has a larger percentage of plagioclase than the southern body. \r\n\r\nA crude sequence of rock types occurs from west to east in the batholith accompanied by a change in plagioclase composition from calcic plagioclase on the west to sodic on the east. Ore minerals tend to decrease, and the ratio potassium feldspar:plagioclase increases inward from the western contact of the batholith, indicating that the Boulder Creek batholith is similar to granodiorite batholiths the world over. Emplacement of the Boulder Creek batholith was contemporaneous with plastic deformation and high-grade regional metamorphism that folded the country rock and the batholith contact along west-northwest and north-northwest axes. Also, smaller satellitic granodiorite bodies tend to conform to the trends of foliation and fold axes in the country rock, suggesting that emplacement was controlled by preexisting structures in the country rock. \r\n\r\nOn a gross scale, chemical equilibrium in the Boulder Creek Granodiorite is expressed by a near 1:1 ratio, or straight-line relationship in the distribution of iron, magnesium, and manganese in biotite and hornblende. General mineralogical trends in the Boulder Creek Granodiorite indicate that modal biotite, hornblende, and plagioclase tend to increase and quartz and microcline tend to decrease as CaO increases. These trends were not found in the Twin Spruce Quartz Monzonite. \r\n\r\nDifferentiation is believed to have played a major role and assimilation a minor role in the development of the Boulder Creek batholith. The Boulder Creek Granodiorite is of probable mantle or lower crust origin, and, based on the scant data available, the Twin Spruce Quartz Monzonite may be of crustal origin, but the magma was extensively altered by contaminants of ambiguous origin. Mafic inclusions, possibly derived from a dioritic magma which was an early differentiate associated temporally with the Boulder Creek Granodiorite and (or) the Twin Spruce Quartz Monzonite, were in jected into the Boulder Creek Granodiorite during the mush stage and before the batholith was completely crystallized. \r\n\r\nBiotite, hornblende, and potassium feldspar were studied extensively. Their chemistry and petrology indicate a homogeneity throughout the batholith not believed possible by a casual observance of the batholithic rocks in the field. The accessory minerals, where investigated, also tend to indicate this same pervasive homogeneity.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1101","usgsCitation":"Gable, D.J., 1980, The Boulder Creek Batholith, Front Range, Colorado: U.S. Geological Survey Professional Paper 1101, 88 p;  2 plates in pocket, https://doi.org/10.3133/pp1101.","productDescription":"88 p;  2 plates in pocket","costCenters":[],"links":[{"id":104551,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4720.htm","linkFileType":{"id":5,"text":"html"},"description":"4720"},{"id":124378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1101/report-thumb.jpg"},{"id":32702,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1101/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32703,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1101/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1101/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db68231b","contributors":{"authors":[{"text":"Gable, Dolores J.","contributorId":52957,"corporation":false,"usgs":true,"family":"Gable","given":"Dolores","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":151739,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5884,"text":"pp1139 - 1980 - A field calibration of the sediment-trapping characteristics of the Helley-Smith bed-load sampler","interactions":[{"subject":{"id":8742,"text":"ofr79411 - 1979 - A field calibration of the sediment-trapping characteristics of the Helley-Smith bedload sampler","indexId":"ofr79411","publicationYear":"1979","noYear":false,"title":"A field calibration of the sediment-trapping characteristics of the Helley-Smith bedload sampler"},"predicate":"SUPERSEDED_BY","object":{"id":5884,"text":"pp1139 - 1980 - A field calibration of the sediment-trapping characteristics of the Helley-Smith bed-load sampler","indexId":"pp1139","publicationYear":"1980","noYear":false,"title":"A field calibration of the sediment-trapping characteristics of the Helley-Smith bed-load sampler"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"pp1139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1139","title":"A field calibration of the sediment-trapping characteristics of the Helley-Smith bed-load sampler","docAbstract":"For sediment particle sizes between 0.50 mm and 16 mm, the Helley-Smith bedload sampler has a near perfect sediment-trapping efficiency. For particles sizes smaller than 0.50 mm, the Helley-Smith sampler has a high bedload sediment-trapping efficiency because part of the sediement retained by the sampler has been transported in suspension and it cannot be quantified separately from the bedload. For particle sizes larger than about 16 mm, the Helley-Smith sampler has low sediment-trapping efficiency but this may be related to the paucity of coarse particles in transport in the calibration tests rather than reflecting an actual low trap efficiency for large-size particles. (USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1139","usgsCitation":"Emmett, W.W., 1980, A field calibration of the sediment-trapping characteristics of the Helley-Smith bed-load sampler: U.S. Geological Survey Professional Paper 1139, 44 p., https://doi.org/10.3133/pp1139.","productDescription":"44 p.","costCenters":[],"links":[{"id":121438,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1139/report-thumb.jpg"},{"id":32715,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec93","contributors":{"authors":[{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":151744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7872,"text":"ofr80141 - 1980 - Geochemical exploration studies in the Dillon, Montana-Idaho, 1 degree x 2 degrees quadrangle; applications of exploration geochemistry in regional resource studies","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr80141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-141","title":"Geochemical exploration studies in the Dillon, Montana-Idaho, 1 degree x 2 degrees quadrangle; applications of exploration geochemistry in regional resource studies","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80141","usgsCitation":"Berger, B.R., 1980, Geochemical exploration studies in the Dillon, Montana-Idaho, 1 degree x 2 degrees quadrangle; applications of exploration geochemistry in regional resource studies: U.S. Geological Survey Open-File Report 80-141, [i], 29 p. ill., maps ;29 cm., https://doi.org/10.3133/ofr80141.","productDescription":"[i], 29 p. ill., maps ;29 cm.","costCenters":[],"links":[{"id":140474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0141/report-thumb.jpg"},{"id":35380,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0141/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae279","contributors":{"authors":[{"text":"Berger, Byron R. bberger@usgs.gov","contributorId":1490,"corporation":false,"usgs":true,"family":"Berger","given":"Byron","email":"bberger@usgs.gov","middleInitial":"R.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":156761,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7851,"text":"ofr807 - 1980 - Hydrologic response of aquifers to droughts in the Great Plains, U.S.A.","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr807","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-7","title":"Hydrologic response of aquifers to droughts in the Great Plains, U.S.A.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr807","usgsCitation":"Bedinger, M.S., 1980, Hydrologic response of aquifers to droughts in the Great Plains, U.S.A.: U.S. Geological Survey Open-File Report 80-7, v, 21 p. map ;28 cm., https://doi.org/10.3133/ofr807.","productDescription":"v, 21 p. map ;28 cm.","costCenters":[],"links":[{"id":141304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0007/report-thumb.jpg"},{"id":35372,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60533a","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":156733,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7837,"text":"ofr80349 - 1980 - Preliminary data describing the distribution of fluoride and silica in the water in the Ogallala aquifer on the High Plains of Texas","interactions":[],"lastModifiedDate":"2022-07-25T17:47:02.900491","indexId":"ofr80349","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-349","title":"Preliminary data describing the distribution of fluoride and silica in the water in the Ogallala aquifer on the High Plains of Texas","docAbstract":"<p>The Ogallala aquifer of Texas historically has been known for elevated fluoride concentration, with many areas in excess of 4 milligrams per liter. In addition, on a regional scale, silica concentrations are also somewhat elevated, with concentrations averaging in the 40 to 50 milligrams per liter range. This aquifer provides a unique geochemical and epidemiological study area because it is completely contained within the High Plains physiographic province.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80349","usgsCitation":"Bassett, R., Perkins, S., and Waddell, R.K., 1980, Preliminary data describing the distribution of fluoride and silica in the water in the Ogallala aquifer on the High Plains of Texas: U.S. Geological Survey Open-File Report 80-349, iv, 109 p., https://doi.org/10.3133/ofr80349.","productDescription":"iv, 109 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":404427,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0349/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0349/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Ogallala Aquifer, High Plains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.095703125,\n              31.784216884487385\n            ],\n            [\n              -99.931640625,\n              31.784216884487385\n            ],\n            [\n              -99.931640625,\n              36.50963615733049\n            ],\n            [\n              -103.095703125,\n              36.50963615733049\n            ],\n            [\n              -103.095703125,\n              31.784216884487385\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c596","contributors":{"authors":[{"text":"Bassett, R.L.","contributorId":13233,"corporation":false,"usgs":true,"family":"Bassett","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":156701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, S.G.","contributorId":93483,"corporation":false,"usgs":true,"family":"Perkins","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":156703,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waddell, R. K.","contributorId":25560,"corporation":false,"usgs":true,"family":"Waddell","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":156702,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5913,"text":"pp1164 - 1980 - Effects of coal mine subsidence in the Sheridan, Wyoming, area","interactions":[{"subject":{"id":8650,"text":"ofr78473 - 1978 - Effects of coal mine subsidence in the western Powder River basin, Wyoming","indexId":"ofr78473","publicationYear":"1978","noYear":false,"title":"Effects of coal mine subsidence in the western Powder River basin, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":5913,"text":"pp1164 - 1980 - Effects of coal mine subsidence in the Sheridan, Wyoming, area","indexId":"pp1164","publicationYear":"1980","noYear":false,"title":"Effects of coal mine subsidence in the Sheridan, Wyoming, area"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"pp1164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1164","title":"Effects of coal mine subsidence in the Sheridan, Wyoming, area","docAbstract":"Analyses of the surface effects of past underground coal mining in the Sheridan, Wyoming, area suggest that underground mining of strippable coal deposits may damage the environment more over long periods of time than would modern surface mining, provided proper restoration procedures are followed after surface mining. Subsidence depressions and pits are a continuing hazard to the environment and to man's activities in the Sheridan, Wyo., area above abandoned underground mines in weak overburden less than about 60 m thick and where the overburden is less than about 10-15 times the thickness of coal mined. In addition, fires commonly start by spontaneous ignition when water and air enter the abandoned mine workings via subsidence cracks and pits. The fires can then spread to unmined coal as they create more cavities, more subsidence, and more cracks and pits through which air can circulate. \r\n\r\nIn modern surface mining operations the total land surface underlain by minable coal is removed to expose the coal. The coal is removed, the overburden and topsoil are replaced, and the land is regraded and revegetated. The land, although disturbed, can be more easily restored and put back into use than can land underlain by abandoned underground mine workings in areas where the overburden is less than about 60 m thick or less than about 10-15 times the thickness of coal mined. The resource recovery of modern surface mining commonly is much greater than that of underground mining procedures. Although present-day underground mining technology is advanced as compared to that of 25-80 years ago, subsidence resulting from underground mining of thick coal beds beneath overburden less than about 60 m thick can still cause greater damage to surface drainage, ground water, and vegetation than can properly designed surface mining operations. \r\n\r\nThis report discusses (11 the geology and surface and underground effects of former large-scale underground coal mining in a 50-km 2 area 5-20 km north of Sheridan, Wyo., (2) a ground and aerial reconnaissance study of a 5-km^2 coal mining area 8-10 km west of Sheridan, and (31 some environmental consequences and problems caused by coal mining.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1164","usgsCitation":"Dunrud, C., and Osterwald, F.W., 1980, Effects of coal mine subsidence in the Sheridan, Wyoming, area: U.S. Geological Survey Professional Paper 1164, 49 p., https://doi.org/10.3133/pp1164.","productDescription":"49 p.","costCenters":[],"links":[{"id":124834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1164/report-thumb.jpg"},{"id":32798,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615ca8","contributors":{"authors":[{"text":"Dunrud, C. Richard","contributorId":48964,"corporation":false,"usgs":true,"family":"Dunrud","given":"C. Richard","affiliations":[],"preferred":false,"id":151800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterwald, Frank W.","contributorId":98301,"corporation":false,"usgs":true,"family":"Osterwald","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":151801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6441,"text":"pp1132 - 1980 - Recent vegetation changes along the Colorado River between Glen Canyon Dam and Lake Mead, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1132","title":"Recent vegetation changes along the Colorado River between Glen Canyon Dam and Lake Mead, Arizona","docAbstract":"Vegetation changes in the canyon of the Colorado River between Glen Canyon Dam and Lake Mead were studied by comparing photographs taken prior to completion of Glen Canyon Dam in 1963 with photographs taken afterwards at the same sites. In general, the older pictures show an absence of riparian plants along the banks of the river. The newer photographs of each pair were taken in 1972 through 1976 and reveal an increased density of many plant species. Exotic species, such as saltcedar and camel-thorn, and native riparian plants such as sandbar willow, arrowweed, desert broom and cattail, now form a new riparian community along much of the channel of the Colorado River between Glen Canyon Dam and Lake Mead. The matched photographs also reveal that changes have occurred in the amount of sand and silt deposited along the banks. Detailed maps are presented showing distribution of 25 plant species along the reach of the Colorado River studied. Data showing changes in the hydrologic regime since completion of Glen Canyon Dam are presented. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1132","usgsCitation":"Turner, R.M., and Karpiscak, M.M., 1980, Recent vegetation changes along the Colorado River between Glen Canyon Dam and Lake Mead, Arizona: U.S. Geological Survey Professional Paper 1132, 125 p.;  plates in pocket, https://doi.org/10.3133/pp1132.","productDescription":"125 p.;  plates in pocket","costCenters":[],"links":[{"id":104556,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4730.htm","linkFileType":{"id":5,"text":"html"},"description":"4730"},{"id":121543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1132/report-thumb.jpg"},{"id":33851,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1132/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33852,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1132/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33853,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1132/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33854,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644bab","contributors":{"authors":[{"text":"Turner, Raymond Marriner","contributorId":20319,"corporation":false,"usgs":true,"family":"Turner","given":"Raymond","email":"","middleInitial":"Marriner","affiliations":[],"preferred":false,"id":152726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karpiscak, Martin M.","contributorId":106107,"corporation":false,"usgs":true,"family":"Karpiscak","given":"Martin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7480,"text":"ofr81449_vol2 - 1980 - Relationship of the 1979 southern California radon anomaly to a possible regional strain event","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr81449_vol2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"81-449","title":"Relationship of the 1979 southern California radon anomaly to a possible regional strain event","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81449_vol2","usgsCitation":"Shapiro, M.H., Melvin, J., Tombrello, T., and Mendenhall, M., 1980, Relationship of the 1979 southern California radon anomaly to a possible regional strain event (Volume 2): U.S. Geological Survey Open-File Report 81-449, 16 p. :ill. ;28 cm. [v.2], https://doi.org/10.3133/ofr81449_vol2.","productDescription":"16 p. :ill. ;28 cm. [v.2]","costCenters":[],"links":[{"id":247331,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0449vol2/report.pdf","size":"1021","linkFileType":{"id":1,"text":"pdf"}},{"id":251800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0449vol2/report-thumb.jpg"}],"edition":"Volume 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634740","contributors":{"authors":[{"text":"Shapiro, Mark H.","contributorId":65847,"corporation":false,"usgs":true,"family":"Shapiro","given":"Mark","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":155815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Melvin, J.D.","contributorId":14403,"corporation":false,"usgs":true,"family":"Melvin","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":155814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tombrello, T.A.","contributorId":13232,"corporation":false,"usgs":true,"family":"Tombrello","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":155813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mendenhall, M.H.","contributorId":92663,"corporation":false,"usgs":true,"family":"Mendenhall","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":155816,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}