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,{"id":68767,"text":"oc98 - 1980 - Vitrinite reflectance and C1-C7 hydrocarbon data for Atigaru Point no. 1 Well, North Slope, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:35","indexId":"oc98","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"98","title":"Vitrinite reflectance and C1-C7 hydrocarbon data for Atigaru Point no. 1 Well, North Slope, Alaska","language":"ENGLISH","doi":"10.3133/oc98","isbn":"060782400X","usgsCitation":"Magoon, L.B., and Claypool, G.E., 1980, Vitrinite reflectance and C1-C7 hydrocarbon data for Atigaru Point no. 1 Well, North Slope, Alaska: U.S. Geological Survey Oil and Gas Investigation Chart 98, 12 well logs, 1 map ;106 x 103 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/oc98.","productDescription":"12 well logs, 1 map ;106 x 103 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":110328,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51825.htm","linkFileType":{"id":5,"text":"html"},"description":"51825"},{"id":191298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -151.71666666666667,70.55027777777778 ], [ -151.71666666666667,70.55055555555555 ], [ -151.71666666666667,70.55055555555555 ], [ -151.71666666666667,70.55027777777778 ], [ -151.71666666666667,70.55027777777778 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdaf6","contributors":{"authors":[{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":278899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Claypool, George E.","contributorId":76312,"corporation":false,"usgs":true,"family":"Claypool","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68816,"text":"oc96 - 1980 - Vitrinite reflectance and C1-C7 hydrocarbon data for North Kalikpik no.1 Well, North Slope, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:25","indexId":"oc96","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"96","title":"Vitrinite reflectance and C1-C7 hydrocarbon data for North Kalikpik no.1 Well, North Slope, Alaska","language":"ENGLISH","doi":"10.3133/oc96","isbn":"0607823984","usgsCitation":"Claypool, G., and Magoon, L.B., 1980, Vitrinite reflectance and C1-C7 hydrocarbon data for North Kalikpik no.1 Well, North Slope, Alaska: U.S. Geological Survey Oil and Gas Investigation Chart 96, 12 well logs ;on sheet 86 x 103 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/oc96.","productDescription":"12 well logs ;on sheet 86 x 103 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":110297,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51758.htm","linkFileType":{"id":5,"text":"html"},"description":"51758"},{"id":188720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -152.36666666666667,70.50083333333333 ], [ -152.36666666666667,70.50083333333333 ], [ -152.36666666666667,70.50083333333333 ], [ -152.36666666666667,70.50083333333333 ], [ -152.36666666666667,70.50083333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdacf","contributors":{"authors":[{"text":"Claypool, George E.","contributorId":8475,"corporation":false,"usgs":true,"family":"Claypool","given":"George E.","affiliations":[],"preferred":false,"id":278975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":278974,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60998,"text":"mf1229 - 1980 - Seismicity map of the State of Wisconsin","interactions":[],"lastModifiedDate":"2019-06-11T14:19:23","indexId":"mf1229","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1229","title":"Seismicity map of the State of Wisconsin","docAbstract":"<p>The earthquake data shown on this map and listed in table 1 are a list of earthquakes that were originally used in preparing the Seismic Risk Studies in the United States in the United States (Algermissen, 1969) which have been recompiled and updated through 1977. &nbsp;These data have been reexamined which resulted in some revisions of epicenters and intensities as well as assignment of intensities to earthquakes that previously had none assigned. &nbsp;Intensity values were updated from new and additional data sources that were not available at the time of original compilation. &nbsp;Some epicenters were relocated on the basis of new information. &nbsp;The data shown in table 1 are estimates of the most accurate epicenter, magnitude, and intensity of each earthquake, on the basis of historical and current information. &nbsp;Some of the aftershocks from large earthquakes are listed but are incomplete in many instances, especially for ones that occurred before seismic instruments were in univeral usage.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1229","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1980, Seismicity map of the State of Wisconsin: U.S. Geological Survey Miscellaneous Field Studies Map 1229, Plate: 39.73 x 24.04 inches, https://doi.org/10.3133/mf1229.","productDescription":"Plate: 39.73 x 24.04 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,{"id":68413,"text":"ha620 - 1980 - Water resources of the Cook Inlet Basin, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:13:24","indexId":"ha620","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"620","title":"Water resources of the Cook Inlet Basin, Alaska","docAbstract":"Ground-water and surface-water systems of Cook Inlet basin, Alaska, are analyzed. Geologic and topographic features that control the movement and regional availability of ground water are explained and illustrated. Five aquifer systems beneath the most populous areas are described. Estimates of ground-water yield were determined for the region by using ground-water data for the populated areas and by extrapolating known subsurface conditions and interpreting subsurface conditions from surficial features in the other areas. Area maps of generalized geology, Quaternary sediment thickness, and general availability of ground water are shown. Surface-water resources are summarized by describing how basin characteristics affect the discharge in streams. Seasonal trend of streamflow for three types of streams is described. Regression equations for 4 streamflow characteristics (annual, monthly minimum, and maximum discharge) were obtained by using gaging station streamflow characteristics and 10 basin characteristics. In the 24 regression equations presented, drainage area is the most significant basin characteristic, but 5 others are used. Maps of mean annual unit runoff and minimum unit yield for 7 consecutive days with a recurrence interval of 10 years are shown. Historic discharge data at gaging stations is tabulated and representative low-flow and flood-flow frequency curves are shown. (USGS)","language":"ENGLISH","doi":"10.3133/ha620","usgsCitation":"Freethey, G.W., and Scully, D.R., 1980, Water resources of the Cook Inlet Basin, Alaska: U.S. Geological Survey Hydrologic Atlas 620, 5 maps : col. ;55 x 41 cm. on 4 sheets 83 x 112 cm., https://doi.org/10.3133/ha620.","productDescription":"5 maps : col. ;55 x 41 cm. on 4 sheets 83 x 112 cm.","costCenters":[],"links":[{"id":188639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89931,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/620/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89932,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/620/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89933,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/620/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89934,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/620/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a4e4b07f02db496c05","contributors":{"authors":[{"text":"Freethey, Geoffrey W.","contributorId":25570,"corporation":false,"usgs":true,"family":"Freethey","given":"Geoffrey","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scully, David R.","contributorId":6857,"corporation":false,"usgs":true,"family":"Scully","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":278175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68768,"text":"oc93 - 1980 - Vitrinite reflectance and C1-C7 hydrocarbon data for South Harrison Bay no. 1 well, North Slope, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:35","indexId":"oc93","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93","title":"Vitrinite reflectance and C1-C7 hydrocarbon data for South Harrison Bay no. 1 well, North Slope, Alaska","language":"ENGLISH","doi":"10.3133/oc93","isbn":"060782395X","usgsCitation":"Magoon, L.B., and Claypool, G.E., 1980, Vitrinite reflectance and C1-C7 hydrocarbon data for South Harrison Bay no. 1 well, North Slope, Alaska: U.S. Geological Survey Oil and Gas Investigation Chart 93, 12 well logs, 1 map ;on sheet 104 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/oc93.","productDescription":"12 well logs, 1 map ;on sheet 104 x 104 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":110309,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51770.htm","linkFileType":{"id":5,"text":"html"},"description":"51770"},{"id":191299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -151.71777777777777,70.41722222222222 ], [ -151.71777777777777,70.4175 ], [ -151.7175,70.4175 ], [ -151.7175,70.41722222222222 ], [ -151.71777777777777,70.41722222222222 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdae1","contributors":{"authors":[{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":278901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Claypool, George E.","contributorId":76312,"corporation":false,"usgs":true,"family":"Claypool","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278902,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56851,"text":"wdrMS781 - 1980 - Water resources data for Mississippi, water year 1978","interactions":[],"lastModifiedDate":"2025-08-28T14:19:52.243104","indexId":"wdrMS781","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MS-78-1","title":"Water resources data for Mississippi, water year 1978","docAbstract":"<p> Water resources data for the 1978 water year for Mississippi consist of record of stage and discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels of wells. This report contains discharge records for 82 gaging stations; stage records for 15 of these gaging stations; stage only for 3 gaging stations; contents for 4 lakes; water quality for 25 gaging stations, and 164 wells; and water levels for 175 observation wells. Also included are data for 92 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Mississippi. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS781","collaboration":"Prepared in cooperation with the Mississippi Board of Water Commissioners and with other State, county, municipal, and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Mississippi, water year 1978: U.S. Geological Survey Water Data Report MS-78-1, vii, 507 p., https://doi.org/10.3133/wdrMS781.","productDescription":"vii, 507 p.","costCenters":[],"links":[{"id":494994,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1978/ms-78-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181744,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1978/ms-78-1/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f32c1","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":532938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8803,"text":"ofr80339 - 1980 - Limnological data for 12 reservoirs in Valley County, Montana","interactions":[],"lastModifiedDate":"2022-07-22T16:48:19.581587","indexId":"ofr80339","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":"80-339","title":"Limnological data for 12 reservoirs in Valley County, Montana","docAbstract":"<p>Water samples were collected from 12 reservoirs in northeastern Montana during the late winter, spring, summer, and early fall of 1978. The resulting physical and chemical water-quality data will be useful in managing the reservoirs for use of stock watering, waterfowl propagation, fish production, and recreation. The surface areas of the reservoirs range for 0.4 to 28.1 hectares with water depths ranging from 0.25 to 6.9 meters. The chemical composition of water varied among reservoirs and with season. Specific conductance ranged from 446 to 4,020 micromhos per centimeter during the winter sampling period and from 62 to 999 micromhos per centimeter during the spring sampling period. Although a pH of 6.9 was measured at one reservoir during the winter, pH values generally ranged from 7.7 to 9.8. Under ice cover, which averaged 1.0 meter thick in late February, three reservoirs attained dissolved-oxygen concentrations above saturation. Each reservoir can be classified as having one of the following three water types: sodium bicarbonate, sodium sulfate, or calcium sodium bicarbonate.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80339","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Ferreira, R.F., 1980, Limnological data for 12 reservoirs in Valley County, Montana: U.S. Geological Survey Open-File Report 80-339, iv, 68 p., https://doi.org/10.3133/ofr80339.","productDescription":"iv, 68 p.","costCenters":[],"links":[{"id":404362,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0339/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0339/report-thumb.jpg"}],"country":"United States","state":"Montana","county":"Valley County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.75,48.5 ], [ -106.75,49 ], [ -106,49 ], [ -106,48.5 ], [ -106.75,48.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5210","contributors":{"authors":[{"text":"Ferreira, Rodger F.","contributorId":13976,"corporation":false,"usgs":true,"family":"Ferreira","given":"Rodger","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":158356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10182,"text":"ofr802016 - 1980 - 210Pb-determined sedimentation rates and trace-metal concentrations, upper Klamath Lake and Lake Euwana, Oregon","interactions":[],"lastModifiedDate":"2022-08-29T22:13:38.544606","indexId":"ofr802016","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":"80-2016","title":"210Pb-determined sedimentation rates and trace-metal concentrations, upper Klamath Lake and Lake Euwana, Oregon","docAbstract":"<p>Rates of sedimentation calculated from analyses of <sup>210</sup>Pb activities in cores from Upper Klamath Lake and Lake Euwana (Klamath County, Ore.) indicate that the lakes, whose mean depths are 2.4 m, are filling at approximately 3.5 mm/yr. In Upper Klamath Lake, average accumulation rates range from 0.9 mm/yr at a site in Howard Bay to 12.5 mm/yr at a location near the input from Agency Lake. Divers collected cores, approximately 50 cm long, from eight locations in Upper Klamath Lake and from one location in Lake Euwana; coring sites were chosen to represent a variety of sedimentary environments. Plots of excess <sup>210</sup>Pb activity versus depth show that a sediment-mixing layer, ranging from 5 to 20 cm in thickness, is below the sediment-water interface at all coring locations; the mixing is due to biological activity, wave and current action, and gas generation. Two cores show changes in accumulation rates during the past 100-150 years that are probably related to changes in land use. X-radiographs indicate the presence of pumice layers and allow assessment of biological activity; these two kinds of information are important to the interpretation of <sup>210</sup><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\">P</span>b activity data. Trace-metal contents were determined to establish baseline information. The eight cores from Upper Klamath Lake contain much lower concentrations of all metals measured (Cd, Cu, Cr, Fe, Pb, Mn, and Zn) than are found in other lacustrine environments. The core taken from Lake Euwana contained higher concentrations of metals than the cores collected from Upper Klamath Lake.</p><p>This study was initiated in response to a concern that possible rapid accumulation of sediments in Upper Klamath Lake poses a threat to the lake's ability to support economically critical activities. The findings indicate that the lake is not filling at a rate that will cause an immediate threat to powerplant, agricultural, and recreational lake use.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr802016","usgsCitation":"Martin, E.A., and Rice, C.A., 1980, 210Pb-determined sedimentation rates and trace-metal concentrations, upper Klamath Lake and Lake Euwana, Oregon: U.S. Geological Survey Open-File Report 80-2016, iii, 48 p., https://doi.org/10.3133/ofr802016.","productDescription":"iii, 48 p.","costCenters":[],"links":[{"id":143046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2016/report-thumb.jpg"},{"id":405869,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Klamath Lake, Lake Euwana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.05398559570312,\n              42.18986405028881\n            ],\n            [\n              -121.75735473632812,\n              42.18986405028881\n            ],\n            [\n              -121.75735473632812,\n              42.49741548732684\n            ],\n            [\n              -122.05398559570312,\n              42.49741548732684\n            ],\n            [\n              -122.05398559570312,\n              42.18986405028881\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4929e4b0b290850eeeda","contributors":{"authors":[{"text":"Martin, E. Ann","contributorId":99550,"corporation":false,"usgs":true,"family":"Martin","given":"E.","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":160956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, Cynthia A.","contributorId":87140,"corporation":false,"usgs":true,"family":"Rice","given":"Cynthia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":160955,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4804,"text":"pp1162B - 1980 - Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","interactions":[{"subject":{"id":7300,"text":"ofr79581 - 1979 - Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","indexId":"ofr79581","publicationYear":"1979","noYear":false,"title":"Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":4804,"text":"pp1162B - 1980 - Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","indexId":"pp1162B","publicationYear":"1980","noYear":false,"chapter":"B","title":"Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington"},"id":1}],"lastModifiedDate":"2022-10-26T21:04:42.123337","indexId":"pp1162B","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":"1162","chapter":"B","title":"Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","docAbstract":"The Makah Formation of the Twin River Group crops out in a northwest-trending linear belt in the northwesternmost part of the Olympic Peninsula, Wash. This marine sequence consists of 2800 meters of predominantly thin-bedded siltstone and sandstone that encloses six distinctive newly named members--four thick-bedded amalgamated turbidite sandstone members, an olistostromal shallow-water marine sandstone and conglomerate member, and a thin-bedded water-laid tuff member. A local unconformity of submarine origin occurs within the lower part of the Makah Formation except in the central part of the study area, where it forms the contact between the older Hoko River Formation and the Makah. Foraminiferal faunas indicate that the Makah Formation ranges in age from late Eocene (late Narizian) to late Oligocene (Zemorrian) and was deposited in a predominantly lower to middle bathyal environment. \r\n\r\nThe Makah Formation is part of a deep-marginalbasin facies that crops out in the western part of the Olympic Peninsula, in southwesternmost Washington and coastal embayments in northwestern Oregon, and along the central part of the coast of western Vancouver Island. On the basis of limited subsurface data from exploratory wells, correlative deep-marginal-basin deposits underlie the inner continental shelf of Oregon and the continental shelf (Tofino basin) along the southwestern side of Vancouver Island. \r\n\r\nDirectional structures in the Makah Formation indicate that the predominantly lithic arkosic sandstone that forms the turbidite packets was derived from the northwest. A possible source of the clastic material is the dioritic, granitic, and volcanic terranes in the vicinity of the Hesquiat Peninsula and Barkley Sound on the west coast of Vancouver Island. Vertical and lateral variations of turbidite facies suggest that the four packets of sandstone were formed as depositional lobes on an outer submarine fan. The thin-bedded strata between the turbidite packets have characteristics of basin-plain and outer-fan fringe deposits.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1162B","usgsCitation":"Snavely, P.D., Niem, A.R., MacLeod, N.S., Pearl, J.E., and Rau, W.W., 1980, Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington: U.S. Geological Survey Professional Paper 1162, iii, 28 p., https://doi.org/10.3133/pp1162B.","productDescription":"iii, 28 p.","costCenters":[],"links":[{"id":31765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1162b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1162b/report-thumb.jpg"},{"id":408779,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74397.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Olympic Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.75,\n              48.4083\n            ],\n            [\n              -124.75,\n              48.1903\n            ],\n            [\n              -124.25,\n              48.1903\n            ],\n            [\n              -124.25,\n              48.4083\n            ],\n            [\n              -124.75,\n              48.4083\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e1b","contributors":{"authors":[{"text":"Snavely, P. D.","contributorId":13971,"corporation":false,"usgs":true,"family":"Snavely","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":149795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Niem, A. R.","contributorId":54984,"corporation":false,"usgs":true,"family":"Niem","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":149796,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"MacLeod, N. S.","contributorId":55816,"corporation":false,"usgs":true,"family":"MacLeod","given":"N.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":149797,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearl, J. E.","contributorId":89883,"corporation":false,"usgs":true,"family":"Pearl","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":149799,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rau, W. W.","contributorId":71963,"corporation":false,"usgs":true,"family":"Rau","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149798,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":10313,"text":"ofr81386 - 1980 - Water-level monitoring along San Andreas and San Jacinto faults, southern California, during fiscal year 1980","interactions":[],"lastModifiedDate":"2022-08-09T15:26:34.56685","indexId":"ofr81386","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":"81-386","title":"Water-level monitoring along San Andreas and San Jacinto faults, southern California, during fiscal year 1980","docAbstract":"<p>Beginning in October 1976, a program of water-level monitoring of abandoned water wells was initiated in the Palmdale area with the purpose of identifying possible water-level changes premonitory to a major earthquake on the San Andreas fault. In October 1977, the program was extended southeastward along the rift zone to the Valyermo area. In November 1977, the monitoring of water wells along the San Jacinto fault was initiated with the expectation of experiencing a moderate size earthquake while monitoring was in progress. Currently over thirty wells are being monitored. Eleven wells are monitored continuously with Stevens Type F recorders, two of which have been modified to operate with the Caltech Remote Observatory Support Systems (TIMS). The remaining wells are probed weekly, or in some cases semi-weekly or daily, by volunteers. We are endeavoring to improve the volunteer program by increasing the frequency of measurements and simplifying the procedure to minimize measurement errors. Weekly water-level data are displayed on computer-generated hydrographs for each well. Rainfall and earthquakes are plotted on the graphs for direct comparison with water levels. The hydrographs are updated and reviewed weekly. Weekly hydrographs are also prepared from recorder charts on two wells maintained by W. R. Moyle, Jr., of the U.S. Geological Survey, Water Resources Division Office, Laguna Niguel, California. A M5.5 earthquake occurred on 25 February 1980, between the Buck Ridge and San Jacinto strands of the San Jacinto fault zone, about 8 miles east-southeast of Anza. This is the largest earthquake which has occurred on the faults within our monitoring network. The Stevens recorder chart for well number 11S/6E-3N4 located in Borrego Valley about 20 miles southeast of the epicenter indicates that, during a period of about four hours on 21 February, the water level rose 1.5 to 1.6 feet and returned to its prior level. This is one of the most remarkable short-term water-level fluctuations observed during our monitoring program; it occurred about 88 hours prior to the earthquake. This well has been monitored since October 1977 and has had a Stevens recorder since October 1978. Long-term water levels have been remarkably steady compared to those in other wells we are monitoring. This well shows a strong response to earth tides. The Stevens record on a second well in Borrego Valley (11S/6E-1C1) showed a much smaller (0.1 foot) spike in water level at the same time as the spike in well number 11S/6E-3N4. Other continuously recording wells in Anza and Ocotillo Wells showed no identifiable water-level anomalies. The two wells in Borrego Valley which showed possible strain-induced water-level spikes appear to be more sensitive to earth tides than wells in the same area which did not show spikes in water level. We cannot conceive of any nontectonic cause for the spike on the Stevens record of well 11S/6E3N4. A creep event on the Coyote Creek fault about four miles from the well is one possibility. Because the spikes in the two wells in Borrego Valley are unique for the long-term record of these wells, they may represent precursors to the 25 February earthquake. Local seismic activity was also recorded in water levels of the two wells in Borrego Springs with continuous water-level recorders. One well showed peculiar high frequency water-level fluctuations from 22 July to 21 August 1980; since then the record has appeared normal. Several wells in the Palmdale-Valyermo area have shown peculiar changes in water level within the past year or so. The long-term hydrograph of well number 5N/12W-4H1 shows the most unusual behavior. The well showed no response to the 1977 and very heavy 1978 rainstorms, yet began to rise in early 1979 and continued to rise through the dry season of 1979. By comparison, most wells show a more normal seasonal response to rainfall. Eight wells in the Palmdale-Valyermo area have shown water-level changes which are different than would have been predicted from the previous history of water-level changes and seasonal rainfall. A longer period of observation is required to determine whether the changes are anomalous. Changes in the strain pattern and other geophysical phenomena have also been observed in southern California during about the same period as the water-level changes. If the water-level changes are the result of tectonic strain, the mechanism and significance are unknown. However, it is interesting that five of the eight wells with possibly anomalous water-level changes have been identified as good strain meters based on their response to earth tides. Six wells showing an unexpected rise in water level are located west of the earthquake swarm which occurred in 1976-1977 (McNally et al, 1978), whereas the two which show water levels lower than would have been predicted are located east of the earthquake swarm.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81386","usgsCitation":"Merifield, P., and Lamar, D., 1980, Water-level monitoring along San Andreas and San Jacinto faults, southern California, during fiscal year 1980: U.S. Geological Survey Open-File Report 81-386, x, 77 p., https://doi.org/10.3133/ofr81386.","productDescription":"x, 77 p.","costCenters":[],"links":[{"id":405009,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0386/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0386/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"southern California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.1572265625,\n              32.54681317351514\n            ],\n            [\n              -114.3017578125,\n              32.54681317351514\n            ],\n            [\n              -114.3017578125,\n              35.782170703266075\n            ],\n            [\n              -121.1572265625,\n              35.782170703266075\n            ],\n            [\n              -121.1572265625,\n              32.54681317351514\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb79d","contributors":{"authors":[{"text":"Merifield, P.M.","contributorId":69557,"corporation":false,"usgs":true,"family":"Merifield","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":161183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lamar, D.L.","contributorId":53801,"corporation":false,"usgs":true,"family":"Lamar","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":161182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8346,"text":"ofr80363 - 1980 - Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Mount McKinley Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2024-03-25T18:17:56.183826","indexId":"ofr80363","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":"80-363","title":"Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Mount McKinley Quadrangle, Alaska","docAbstract":"<p>These summaries of references are designed to aid in library research on metallic and nonmetallic (other than mineral fuels and construction materials) mineral occurrences in the Mount McKinley quadrangle, Alaska. All references to most reports of the Geological Survey, the U.S. Bureau of Mines, and the State of Alaska Division of Geological and Geophysical Surveys and its predecessor State and Territorial agencies released before November 1, 1979, are summarized. Certain, mainly statistical, reports such as the annual Mineral Yearbook of the U.S. Bureau of Mines and the biennial and annual reports of the State of Alaska Division of Geological and Geophysical Surveys and its predecessor State and Territorial agencies are not included. Also not included are data on many claims about which little more than their locations is known (for example, MacKevett and Holloway, 1977 (OF 77-169A), p. 48). These omissions should not be interpreted as a judgment on my part that the claims are not valid mineral occurrences, but only that there are insufficient data to describe any mineral deposit that might be present.</p><p>This report is divided into three parts: a section made up of summaries of references arranged alphabetically by occurrence name; a section that lists synonyms for names in the first section, claim names, and the names of operators and owners of mines and prospects; and a section that lists, by author, all references summarized in the first section and in these introductory paragraphs.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80363","usgsCitation":"Cobb, E.H., 1980, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Mount McKinley Quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-363, 150 p., https://doi.org/10.3133/ofr80363.","productDescription":"150 p.","costCenters":[],"links":[{"id":426983,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0363/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140347,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0363/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Mount McKinley Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -153.9969908293706,\n              62.396367997356236\n            ],\n            [\n              -153.9969908293706,\n              61.37419019224362\n            ],\n            [\n              -151.85728501365435,\n              61.37419019224362\n            ],\n            [\n              -151.85728501365435,\n              62.396367997356236\n            ],\n            [\n              -153.9969908293706,\n              62.396367997356236\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698d53","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":157578,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":999,"text":"wsp2069 - 1980 - Sediment deposition in the White River Reservoir, northwestern Wisconsin","interactions":[{"subject":{"id":7840,"text":"ofr791330 - 1979 - Sediment deposition in the White River Reservoir, northwestern Wisconsin","indexId":"ofr791330","publicationYear":"1979","noYear":false,"title":"Sediment deposition in the White River Reservoir, northwestern Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":999,"text":"wsp2069 - 1980 - Sediment deposition in the White River Reservoir, northwestern Wisconsin","indexId":"wsp2069","publicationYear":"1980","noYear":false,"title":"Sediment deposition in the White River Reservoir, northwestern Wisconsin"},"id":1}],"lastModifiedDate":"2015-09-29T16:14:35","indexId":"wsp2069","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2069","title":"Sediment deposition in the White River Reservoir, northwestern Wisconsin","docAbstract":"<p>The history of deposition in the White River Reservoir was reconstructed from a study of sediment in the reservoir. Suspended-sediment concentrations, particle size, and streamflow characteristics were measured at gaging stations upstream and downstream from the reservoir from November 1975 through September 1977. Characteristics of the sediments were determined from borings and samples taken while the reservoir was drained in September 1976. The sediment surface and the pre-reservoir topography were mapped. Sediment thickness ranged from less than 1 foot near the shore to more than 20 feet in the old stream channel. The original reservoir capacity and the volume of deposited sediment were calculated to be 815 acre-feet and 487 acre-feet, respectively. Sediment size ranged from clay and silt in the pool area to large cobbles and boulders at the upstream end of the reservoir. Analyses of all samples averaged 43 percent sand, 40 percent silt, and 17 percent clay, and particle size typically increased upstream. Cobbles, boulders, and gravel deposits were not sampled. The average density of the deposited sediment was about 80 pounds per cubic foot for the entire reservoir. The reservoir was able to trap about 80 percent of the sediment entering from upstream, early in its history. This trap efficiency has declined as the reservoir filled with sediment. Today (1976), it traps only sand and silt-sized sediment, or only about 20 percent of the sediment entering from upstream. Data collected during this study indicate that essentially all of the clay-sized sediment (&lt;0.062 mm) passes through the reservoir. The gross rate of deposition was 7.0 acre-feet per year over the reservoir history, 1907-76. Rates during 1907-63 and 1963-76 were 7.4 and 5.7 acre-feet per year, respectively, determined by the cesium-137 method. Based on scant data, the average annual sediment yield of the total 279 square mile drainage area above the gaging station at the powerhouse was about 50 tons per square mile. Analysis of the drainage-basin characteristics indicates that most of this sediment was derived from less than 10 percent of the total drainage area and from steep unvegetated streambanks.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2069","collaboration":"Preapared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Batten, W.G., and Hindall, S.M., 1980, Sediment deposition in the White River Reservoir, northwestern Wisconsin: U.S. Geological Survey Water Supply Paper 2069, Report: iv, 30 p.; 1 Plate: 16.88 x 13.63 inches: Preceeding Publications, https://doi.org/10.3133/wsp2069.","productDescription":"Report: iv, 30 p.; 1 Plate: 16.88 x 13.63 inches: Preceeding Publications","numberOfPages":"35","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":25570,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2069/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2069/report-thumb.jpg"},{"id":94695,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2069/plate-1.pdf","size":"208","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Bayfield County","otherGeospatial":"Lake Superior, White River Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.91162109375,\n              45.69850658738846\n            ],\n            [\n              -91.91162109375,\n              47.16730970131578\n            ],\n            [\n              -90.3955078125,\n              47.16730970131578\n            ],\n            [\n              -90.3955078125,\n              45.69850658738846\n            ],\n            [\n              -91.91162109375,\n              45.69850658738846\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635258","contributors":{"authors":[{"text":"Batten, W. G.","contributorId":89504,"corporation":false,"usgs":true,"family":"Batten","given":"W.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":142995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hindall, S. M.","contributorId":59414,"corporation":false,"usgs":true,"family":"Hindall","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":142994,"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":6302,"text":"pp1146 - 1980 - Revised nomenclature and stratigraphic relationships of the Fredericksburg Complex and Quantico Formation of the Virginia Piedmont","interactions":[],"lastModifiedDate":"2019-09-10T09:37:04","indexId":"pp1146","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":"1146","title":"Revised nomenclature and stratigraphic relationships of the Fredericksburg Complex and Quantico Formation of the Virginia Piedmont","docAbstract":"The Fredericksburg Complex, in part a migmatitic terrane in northeast Virginia, is subdivided on the basis of lithology, as well as aeromagnetic and aeroradiometric data, into two metamorphic suites. These suites are separated by the northeast-trending Spotsylvania lineament, a rectilinear geophysical feature that is probably the trace of an old fault zone. East of the lineament, the Po River Metamorphic Suite, of Proterozoic Z and (or) early Paleozoic age, consists dominantly of biotite gneiss, generally augen gneiss, and lesser amounts of hornblende gneiss and mica schist. West of the Spotsylvania lineament is the Ta River Metamorphic Suite, composed mostly of amphibolite and amphibole gneiss. However, to the southwest, along its strike belt, the Ta River contains abundant biotite gneiss and mica schist. Both the Ta River and Po River contain abundant foliated granitoid and pegmatoid bodies as concordant tabular masses and as crosscutting dikes; these rocks are considered part of the Ta River and Po River Metamorphic Suites. The amphibolitic Holly Corner Gneiss is interpreted to be a western allochthonous equivalent of the Ta River. Both the Ta River and Holly Corner are considered to be coeval, eastern, distal facies of the Lower Cambrian(?) Chopawamsic Formation. The Paleozoic Falls Run Granite Gneiss intrudes the Ta River Metamorphic Suite and the Holly Corner Gneiss; locally the Falls Run is interpreted to have been transported westward with the Holly Corner after intrusion. \r\n\r\nThe Quantico Formation, in the core of the Quantico-Columbia synclinorium, rests with angular unconformity along its northwest and southeast limbs, respectively, on the Chopawamsic Formation and the Ta River Metamorphic Suite. The Quantico Formation is assigned the same Late Ordovician age and similar stratigraphic position as the Arvonia Slate of the Arvonia syncline. \r\n\r\nThe youngest rocks of the area are the granitoid and pegmatoid bodies of the Falmouth Intrusive Suite. They consist of several generations of chiefly dikes and sills that are intrusive into the Fredericksburg Complex and into the Quantico Formation. Granitoid rocks also form small plutons. The Falmouth is isotopically dated as Carboniferous in age. \r\n\r\nSome of the metavolcanic rocks of the Evington Group and part of the amphibolite gneiss and amphibolite of the Hatcher Complex, named by W. B. Brown in 1969, are probably coeval with the Chopawamsic Formation and hence equivalents of the Ta River Metamorphic Suite and the Holly Corner Gneiss. The biotitic gneiss and granitoid rocks east of the Spotsylvania lineament in the Dillwyn area are considered to be coeval with the Po River Metamorphic Suite.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1146","usgsCitation":"Pavlides, L., 1980, Revised nomenclature and stratigraphic relationships of the Fredericksburg Complex and Quantico Formation of the Virginia Piedmont: U.S. Geological Survey Professional Paper 1146, Report: 29 p.; Plate; Companion Files, https://doi.org/10.3133/pp1146.","productDescription":"Report: 29 p.; Plate; Companion Files","costCenters":[],"links":[{"id":33590,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1146/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104558,"rank":700,"type":{"id":7,"text":"Companion Files"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4734.htm","linkFileType":{"id":5,"text":"html"},"description":"4734"},{"id":33591,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1146/report-thumb.jpg"}],"country":"United States","state":"Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.6129150390625,\n              38.043765107439675\n            ],\n            [\n              -76.92626953125,\n              38.043765107439675\n            ],\n            [\n              -76.92626953125,\n              38.792626957868904\n            ],\n            [\n              -77.6129150390625,\n              38.792626957868904\n            ],\n            [\n              -77.6129150390625,\n              38.043765107439675\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ebc","contributors":{"authors":[{"text":"Pavlides, Louis","contributorId":79444,"corporation":false,"usgs":true,"family":"Pavlides","given":"Louis","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":152471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9356,"text":"ofr81255 - 1980 - Support of the Southern California Geophysical Data and Analysis Center","interactions":[],"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr81255","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":"81-255","title":"Support of the Southern California Geophysical Data and Analysis Center","language":"ENGLISH","publisher":"Seismological Laboratory, California Institute of Technology,","doi":"10.3133/ofr81255","usgsCitation":"Harkrider, D.G., 1980, Support of the Southern California Geophysical Data and Analysis Center: U.S. Geological Survey Open-File Report 81-255, 1 leaf ;28 cm.; (3 p. - PGS), https://doi.org/10.3133/ofr81255.","productDescription":"1 leaf ;28 cm.; (3 p. - PGS)","costCenters":[],"links":[{"id":144167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0255/report-thumb.jpg"},{"id":37068,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0255/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6984b2","contributors":{"authors":[{"text":"Harkrider, David G.","contributorId":91111,"corporation":false,"usgs":true,"family":"Harkrider","given":"David","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":159537,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10368,"text":"ofr80361 - 1980 - Catalog of computer-based NOAA climatological data, relative to USGS earthquake research in California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr80361","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":"80-361","title":"Catalog of computer-based NOAA climatological data, relative to USGS earthquake research in California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80361","usgsCitation":"Miranda, S.L., and Herriot, J.W., 1980, Catalog of computer-based NOAA climatological data, relative to USGS earthquake research in California: U.S. Geological Survey Open-File Report 80-361, 37 p. :graphs, maps ;28 cm., https://doi.org/10.3133/ofr80361.","productDescription":"37 p. :graphs, maps ;28 cm.","costCenters":[],"links":[{"id":143559,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0361/report-thumb.jpg"},{"id":38204,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0361/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efb93","contributors":{"authors":[{"text":"Miranda, Sandra L.","contributorId":90734,"corporation":false,"usgs":true,"family":"Miranda","given":"Sandra","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herriot, James W.","contributorId":52184,"corporation":false,"usgs":true,"family":"Herriot","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":161267,"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":7028,"text":"ofr801253 - 1980 - Catalog of earthquakes in southern Alaska, January-March 1980","interactions":[],"lastModifiedDate":"2023-08-01T22:11:33.064005","indexId":"ofr801253","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":"80-1253","title":"Catalog of earthquakes in southern Alaska, January-March 1980","docAbstract":"<p>The National Center for Earthquake Research of the U.S. Geological Survey (USGS) began a program of telemetered seismic recording in south-central Alaska in 1971. The principal objectives of this program have been to use data recorded by this network to precisely locate earthquakes in the active seismic zones of southern Alaska, delineate seismically active faults, assess seismic risk, document potential premonitory earthquake phenomena, investigate current tectonic deformation, and study the structure and physical properties of the crust and upper mantle. A task fundamental to all of these goals is the routine cataloging of earthquake parameters for earthquakes located within and adjacent to the seismograph network.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801253","usgsCitation":"Stephens, C., Fogleman, K., Lahr, J., Helton, S., Cancilla, R., Tam, R., and Freiberg, J., 1980, Catalog of earthquakes in southern Alaska, January-March 1980: U.S. Geological Survey Open-File Report 80-1253, 55 p., https://doi.org/10.3133/ofr801253.","productDescription":"55 p.","costCenters":[],"links":[{"id":419479,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1253/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139493,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1253/report-thumb.jpg"}],"country":"United 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C.D.","contributorId":18752,"corporation":false,"usgs":true,"family":"Stephens","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":153974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fogleman, K.A.","contributorId":56212,"corporation":false,"usgs":true,"family":"Fogleman","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":153977,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lahr, J.C.","contributorId":34892,"corporation":false,"usgs":true,"family":"Lahr","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":153975,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Helton, S.M.","contributorId":60201,"corporation":false,"usgs":true,"family":"Helton","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":153978,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cancilla, R.S.","contributorId":76729,"corporation":false,"usgs":true,"family":"Cancilla","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":153979,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tam, Roy","contributorId":53780,"corporation":false,"usgs":true,"family":"Tam","given":"Roy","email":"","affiliations":[],"preferred":false,"id":153976,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Freiberg, J.A.","contributorId":13614,"corporation":false,"usgs":true,"family":"Freiberg","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":153973,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":7032,"text":"ofr80504 - 1980 - A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979","interactions":[{"subject":{"id":7032,"text":"ofr80504 - 1980 - A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979","indexId":"ofr80504","publicationYear":"1980","noYear":false,"title":"A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979"},"predicate":"SUPERSEDED_BY","object":{"id":16945,"text":"ofr84484 - 1984 - A Catalogue of drill core recovered from Kilauea Iki lava lake from 1967 to 1979","indexId":"ofr84484","publicationYear":"1984","noYear":false,"title":"A Catalogue of drill core recovered from Kilauea Iki lava lake from 1967 to 1979"},"id":1}],"supersededBy":{"id":16945,"text":"ofr84484 - 1984 - A Catalogue of drill core recovered from Kilauea Iki lava lake from 1967 to 1979","indexId":"ofr84484","publicationYear":"1984","noYear":false,"title":"A Catalogue of drill core recovered from Kilauea Iki lava lake from 1967 to 1979"},"lastModifiedDate":"2022-10-25T19:43:35.816708","indexId":"ofr80504","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":"80-504","title":"A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979","docAbstract":"<div><span>The purpose of this report is to serve as a descriptive catalogue for drill core recovered from Kilauea Iki lava lake, from 1967 to 1979. </span></div><div><span><br data-mce-bogus=\"1\"></span></div><div><span>Kilauea Iki lava lake was formed when lavas of the 1959 summit eruption were ponded in Kilauea Iki pit crater, a large pit crater at the extreme upper end of Kilauea's east rift zone (Fig. 1). This eruption is one of the best documented of Kilauean eruptions: Murata and Richter (1966) and Richter and Murata (1966) presented data on the chemistry and petrography of the lavas, respectively, and Richter et al. (1970) described the complex filling of the pit crater in considerable detail.</span></div><div><span><br data-mce-bogus=\"1\"></span></div><div><span>Investigation of the lava lake began a few months after the crust stabilized, with the establishment of two perpendicular lines of levelling stations on the surface of the lake. In 1960-62, four holes were drilled through the upper crust in the center of the lake; the crust was 22-44 feet (6.7-13.4 m) thick at that time. Richter and Moore (1966) presented petrographic, modal, and chemical data on the core recovered from this early drilling.</span></div><div><span><br data-mce-bogus=\"1\"></span></div><div><span>The upper crust of Kilauea Iki was drilled again in 1967 by staff members of the Hawaiian Volcano Observatory, and core was recovered from three holes. In 1975, U.S. Geological Survey workers drilled three more holes, each a few feet away from one of the 1 967 holes. A summary of all work done on Kilauea Iki and other Hawaiian lava lakes through 1975 has been given by Wright et al. (1976).</span></div><div><span><br data-mce-bogus=\"1\"></span></div><div><span>The lake has been redrilled twice since 1975, by workers from Sandia Laboratories, as part of their Magma Energy Research program, in cooperation with the U.S. Geological Survey. In 1976, they drilled two holes near the center of the lake. In 1978-79, they drilled a total of six holes; one, commissioned by the U.S. Geological Survey, went completely through the lava lake near its north edge, into the pre-1959 lavas below.</span></div>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80504","usgsCitation":"Helz, R.T., Banks, N.G., Casadevall, T.J., Fiske, R.S., and Moore, R.B., 1980, A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979: U.S. Geological Survey Open-File Report 80-504, 72 p., https://doi.org/10.3133/ofr80504.","productDescription":"72 p.","costCenters":[],"links":[{"id":140781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0504/report-thumb.jpg"},{"id":408713,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0504/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Iki lava lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.30925750732422,\n              19.39180098837034\n            ],\n            [\n              -155.22171020507812,\n              19.39180098837034\n            ],\n            [\n              -155.22171020507812,\n              19.43583809782748\n            ],\n            [\n              -155.30925750732422,\n              19.43583809782748\n            ],\n            [\n              -155.30925750732422,\n              19.39180098837034\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd497ee4b0b290850ef3c7","contributors":{"authors":[{"text":"Helz, Rosalind Tuthill 0000-0003-1550-0684","orcid":"https://orcid.org/0000-0003-1550-0684","contributorId":85587,"corporation":false,"usgs":true,"family":"Helz","given":"Rosalind","email":"","middleInitial":"Tuthill","affiliations":[],"preferred":false,"id":154002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Banks, Norman G.","contributorId":89524,"corporation":false,"usgs":true,"family":"Banks","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":154001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Casadevall, Thomas J. 0000-0002-9447-6864 tcasadevall@usgs.gov","orcid":"https://orcid.org/0000-0002-9447-6864","contributorId":2734,"corporation":false,"usgs":true,"family":"Casadevall","given":"Thomas","email":"tcasadevall@usgs.gov","middleInitial":"J.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":154003,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fiske, Richard S.","contributorId":229675,"corporation":false,"usgs":false,"family":"Fiske","given":"Richard","email":"","middleInitial":"S.","affiliations":[{"id":36606,"text":"Smithsonian Institution","active":true,"usgs":false}],"preferred":false,"id":154000,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moore, R. B.","contributorId":98720,"corporation":false,"usgs":true,"family":"Moore","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":154004,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":3949,"text":"cir829 - 1980 - The accuracy of selected land use and land cover maps at scales of 1:250,000 and 1:100,000","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"cir829","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"829","title":"The accuracy of selected land use and land cover maps at scales of 1:250,000 and 1:100,000","docAbstract":"Land use and land cover maps produced by the U.S. Geological Survey are found to meet or exceed the established standard of accuracy. When analyzed using a point sampling technique and binomial probability theory, several maps, illustrative of those produced for different parts of the country, were found to meet or exceed accuracies of 85 percent. Those maps tested were Tampa, Fla., Portland, Me., Charleston, W. Va., and Greeley, Colo., published at a scale of 1:250,000, and Atlanta, Ga., and Seattle and Tacoma, Wash., published at a scale of 1:100,000. For each map, the values were determined by calculating the ratio of the total number of points correctly interpreted to the total number of points sampled. Six of the seven maps tested have accuracies of 85 percent or better at the 95-percent lower confidence limit. When the sample data for predominant categories (those sampled with a significant number of points) were grouped together for all maps, accuracies of those predominant categories met the 85-percent accuracy criterion, with one exception. One category, Residential, had less than 85-percent accuracy at the 95-percent lower confidence limit. Nearly all residential land sampled was mapped correctly, but some areas of other land uses were mapped incorrectly as Residential.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/cir829","usgsCitation":"Fitzpatrick-Lins, K., 1980, The accuracy of selected land use and land cover maps at scales of 1:250,000 and 1:100,000: U.S. Geological Survey Circular 829, 24 p. : diagrs. ; 26 cm., https://doi.org/10.3133/cir829.","productDescription":"24 p. : diagrs. ; 26 cm.","costCenters":[],"links":[{"id":122525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0829/report-thumb.jpg"},{"id":31034,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0829/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66984f","contributors":{"authors":[{"text":"Fitzpatrick-Lins, Katherine","contributorId":75906,"corporation":false,"usgs":true,"family":"Fitzpatrick-Lins","given":"Katherine","email":"","affiliations":[],"preferred":false,"id":147881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2579,"text":"wsp2072 - 1980 - Suspended-sediment discharge in five streams near Harrisburg, Pennsylvania, before, during, and after highway construction","interactions":[{"subject":{"id":15598,"text":"ofr74140 - 1974 - Sediment characteristics of five streams near Harrisburg, Pa., before highway construction","indexId":"ofr74140","publicationYear":"1974","noYear":false,"title":"Sediment characteristics of five streams near Harrisburg, Pa., before highway construction"},"predicate":"SUPERSEDED_BY","object":{"id":2579,"text":"wsp2072 - 1980 - Suspended-sediment discharge in five streams near Harrisburg, Pennsylvania, before, during, and after highway construction","indexId":"wsp2072","publicationYear":"1980","noYear":false,"title":"Suspended-sediment discharge in five streams near Harrisburg, Pennsylvania, before, during, and after highway construction"},"id":1}],"lastModifiedDate":"2017-06-19T14:04:24","indexId":"wsp2072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2072","title":"Suspended-sediment discharge in five streams near Harrisburg, Pennsylvania, before, during, and after highway construction","docAbstract":"Rainfall, streamflow, sediment, and turbidity data were collected as part of a study to evaluate the effects of highway construction on suspended-sediment discharges in streams. The study was also designed to evaluate the effectiveness of different erosion-control measures in reducing sediment discharge. Although highway construction increased suspended-sediment discharges from two to four-fold, the rate of sediment discharge quickly returned to pre-construction levels when construction ended. The most effective sediment control evaluated was offstream ponds, which were designed to trap and store sediment laden water from the construction area. The offstream ponds trapped about 70 percent of the sediment that reached them during most storms. Seeding and mulching generally reduced sediment loads about 20 percent. Rock dams and bales reduced loads about 5 percent. An onstream pond, constructed on a large stream below the construction area, reduced sediment loads about 80 percent. However, unlike the offstream ponds, which stopped discharging runoff water soon after precipitation ended, the onstream pond kept discharging runoff water, and the stream below the pond remained turbid for extended periods.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2072","usgsCitation":"Reed, L.A., 1980, Suspended-sediment discharge in five streams near Harrisburg, Pennsylvania, before, during, and after highway construction: U.S. Geological Survey Water Supply Paper 2072, 37 p. : ill., maps ; 23 cm., https://doi.org/10.3133/wsp2072.","productDescription":"37 p. : ill., maps ; 23 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":28855,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2072/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2072/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fb6","contributors":{"authors":[{"text":"Reed, Lloyd A.","contributorId":79861,"corporation":false,"usgs":true,"family":"Reed","given":"Lloyd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3946,"text":"cir832 - 1980 - Estimating the costs of landslide damage in the United States","interactions":[],"lastModifiedDate":"2017-07-05T11:26:48","indexId":"cir832","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"832","title":"Estimating the costs of landslide damage in the United States","docAbstract":"Landslide damages are one of the most costly natural disasters in the United States. A recent estimate of the total annual cost of landslide damage is in excess of $1 billion {Schuster, 1978}. The damages can be significantly reduced, however, through the combined action of technical experts, government, and the public. \r\n\r\nBefore they can be expected to take action, local governments need to have an appreciation of costs of damage in their areas of responsibility and of the reductions in losses that can be achieved. Where studies of cost of landslide damages have been conducted, it is apparent that {1} costs to the public and private sectors of our economy due to landslide damage are much larger than anticipated; {2} taxpayers and public officials generally are unaware of the magnitude of the cost, owing perhaps to the lack of any centralization of data; and {3} incomplete records and unavailability of records result in lower reported costs than actually were incurred. \r\n\r\nThe U.S. Geological Survey has developed a method to estimate the cost of landslide damages in regional and local areas and has applied the method in three urban areas and one rural area. Costs are for different periods and are unadjusted for inflation; therefore, strict comparisons of data from different years should be avoided. Estimates of the average annual cost of landslide damage for the urban areas studied are $5,900,000 in the San Francisco Bay area; $4,000,000 in Allegheny County, Pa.; and $5,170,000 in Hamilton County, Ohio. Adjusting these figures for the population of each area, the annual cost of damages per capita are $1.30 in the nine-county San Francisco Bay region; $2.50 in Allegheny County, Pa.; and $5.80 in Hamilton County, Ohio. On the basis of data from other sources, the estimated annual damages on a per capita basis for the City of Los Angeles, Calif., are about $1.60. If the costs were available for the damages from landslides in Los Angeles in 1977-78 and 1979-80, the annual per capita costs probably would be much larger. \r\n\r\nThe landslide near the rural community of Manti, Utah, caused an expenditure of about $1,800,000 or about $1,000 per person during the period 1974-76. Because a recurrence for such a landslide cannot be established, it is not possible to develop a meaningful estimate of annual per capita damages. \r\n\r\nCommunities are urged to examine their costs of landslide damage and to evaluate the feasibility of several alternative programs that, for a modest investment, could significantly reduce these losses.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir832","usgsCitation":"Fleming, R.W., and Taylor, F.A., 1980, Estimating the costs of landslide damage in the United States: U.S. Geological Survey Circular 832, iii, 21 p. :ill., map ;27 cm., https://doi.org/10.3133/cir832.","productDescription":"iii, 21 p. :ill., map ;27 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":31031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0832/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0832/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc80a","contributors":{"authors":[{"text":"Fleming, Robert W.","contributorId":102062,"corporation":false,"usgs":true,"family":"Fleming","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Fred A.","contributorId":38142,"corporation":false,"usgs":true,"family":"Taylor","given":"Fred","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147874,"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":8873,"text":"ofr78556E - 1980 - Drainage areas of surface water bodies of the Kennebec River basin in southwestern Maine","interactions":[{"subject":{"id":8873,"text":"ofr78556E - 1980 - Drainage areas of surface water bodies of the Kennebec River basin in southwestern Maine","indexId":"ofr78556E","publicationYear":"1980","noYear":false,"chapter":"E","title":"Drainage areas of surface water bodies of the Kennebec River basin in southwestern Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1}],"isPartOf":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"lastModifiedDate":"2026-03-06T17:32:40.350332","indexId":"ofr78556E","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":"78-556","chapter":"E","title":"Drainage areas of surface water bodies of the Kennebec River basin in southwestern Maine","docAbstract":"<p>The report contains drainage-area values for: lakes and ponds included in the MIDAS (Maine Informational Display Analysis System) File 906-Z, streams that drain an area greater than 25 square miles, dams, and locations where hydrologic data are collected. Supplemental information includes State and Federal location systems used to identify these lake and stream sites.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556E","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Fontaine, R.A., 1980, Drainage areas of surface water bodies of the Kennebec River basin in southwestern Maine: U.S. Geological Survey Open-File Report 78-556, v, 83 p., https://doi.org/10.3133/ofr78556E.","productDescription":"v, 83 p.","costCenters":[],"links":[{"id":142630,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-e/report-thumb.jpg"},{"id":430920,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maine","otherGeospatial":"Kennebec River basin, southwestern Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.64716269660408,\n              45.578452261446074\n            ],\n            [\n              -70.64716269660408,\n              43.9178350922833\n            ],\n            [\n              -69.72485488923323,\n              43.9178350922833\n            ],\n            [\n              -69.72485488923323,\n              45.578452261446074\n            ],\n            [\n              -70.64716269660408,\n              45.578452261446074\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635ece","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}