{"pageNumber":"5313","pageRowStart":"132800","pageSize":"25","recordCount":184743,"records":[{"id":10110,"text":"ofr821091 - 1982 - Heavy-mineral variability in beach and dune sands in the vicinity of the mouth of the Columbia River","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr821091","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1091","title":"Heavy-mineral variability in beach and dune sands in the vicinity of the mouth of the Columbia River","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821091","usgsCitation":"Luepke, G., 1982, Heavy-mineral variability in beach and dune sands in the vicinity of the mouth of the Columbia River: U.S. Geological Survey Open-File Report 82-1091, 18 p. :map ;28 cm., https://doi.org/10.3133/ofr821091.","productDescription":"18 p. :map ;28 cm.","costCenters":[],"links":[{"id":144588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1091/report-thumb.jpg"},{"id":37959,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ae4b07f02db63c87c","contributors":{"authors":[{"text":"Luepke, Gretchen","contributorId":91827,"corporation":false,"usgs":true,"family":"Luepke","given":"Gretchen","email":"","affiliations":[],"preferred":false,"id":160832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59918,"text":"mf1443 - 1982 - Detailed bathymetric map of the United States continental slope between Lindenkohl Canyon and Toms Canyon, offshore New Jersey","interactions":[],"lastModifiedDate":"2019-05-29T14:32:30","indexId":"mf1443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1443","title":"Detailed bathymetric map of the United States continental slope between Lindenkohl Canyon and Toms Canyon, offshore New Jersey","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1443","usgsCitation":"Kirby, J., Robb, J.M., and Hampson, J., 1982, Detailed bathymetric map of the United States continental slope between Lindenkohl Canyon and Toms Canyon, offshore New Jersey: U.S. Geological Survey Miscellaneous Field Studies Map 1443, 1 map ;102 x 98 cm. folded in envleope 25 x 32 cm., https://doi.org/10.3133/mf1443.","productDescription":"1 map ;102 x 98 cm. folded in envleope 25 x 32 cm.","costCenters":[],"links":[{"id":364233,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1443/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1443/report-thumb.jpg"}],"scale":"0","country":"United States","state":"New Jersey","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73,38.833333333333336 ], [ -73,39.083333333333336 ], [ -72.33333333333333,39.083333333333336 ], [ -72.33333333333333,38.833333333333336 ], [ -73,38.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667c7a","contributors":{"authors":[{"text":"Kirby, J.R.","contributorId":6428,"corporation":false,"usgs":true,"family":"Kirby","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":262830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":262831,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampson, J.C. Jr.","contributorId":87945,"corporation":false,"usgs":true,"family":"Hampson","given":"J.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":262832,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10506,"text":"ofr821016 - 1982 - Vertical movement of ground water under the Merrill Field landfill, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr821016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1016","title":"Vertical movement of ground water under the Merrill Field landfill, Anchorage, Alaska","docAbstract":"Shallow groundwater under the Merrill Field sanitary landfill at Anchorage is polluted by leachate. Wells, including three Municipal-supply wells, obtain water from two confined aquifers 100-300 feet beneath the landfill area. Aquifer-test data and information on subsurface geology, ground-water levels, and properties of materials were used to estimate vertical gradients and vertical permeabilities under the landfill. The authors ' best estimates ' of vertical permeabilities of two confining units are 1 x 10 super -2 foot per day and 2 x 10 super -4 foot per day. Theoretical travel-time calculations indicate that minor amounts of pollutants may reach the upper confined aquifer after many tens of years, but that water of the composition of the leachate probably would not reach the aquifer for more than three centuries. The range of error in the theoretical travel-time calculations is likely to be plus or minus a factor of two or three. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821016","usgsCitation":"Nelson, G.L., and Dearborn, L., 1982, Vertical movement of ground water under the Merrill Field landfill, Anchorage, Alaska: U.S. Geological Survey Open-File Report 82-1016, iv, 28 p. ill. ;28 cm., https://doi.org/10.3133/ofr821016.","productDescription":"iv, 28 p. ill. ;28 cm.","costCenters":[],"links":[{"id":144659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1016/report-thumb.jpg"},{"id":38360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6020ca","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161515,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dearborn, L.L.","contributorId":53376,"corporation":false,"usgs":true,"family":"Dearborn","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":161514,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10587,"text":"ofr82649 - 1982 - January 1982 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82649","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-649","title":"January 1982 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Water-level measurements were made, mostly in January 1982, in about 1,530 wells in western and south-central Kansas. The measurements were made in mid-winter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base-reference year ' (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966 or 1974), and each of seven consecutive years of measurement (1976-82), the ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern and west-central areas. Water levels for the ' base-reference year ' are established by measurements made during that year and by interpretation of maps showing water-level altitudes. Data also are provided for relating the average annual water-level changes, saturated thicknesses of the deposits, and percentage changes in saturated thicknesses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82649","usgsCitation":"Pabst, M., 1982, January 1982 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 82-649, 167 p. :map ;28 cm., https://doi.org/10.3133/ofr82649.","productDescription":"167 p. :map ;28 cm.","costCenters":[],"links":[{"id":143111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0649/report-thumb.jpg"},{"id":38413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0649/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fde","contributors":{"authors":[{"text":"Pabst, M.E.","contributorId":17608,"corporation":false,"usgs":true,"family":"Pabst","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":161637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10868,"text":"ofr82277 - 1982 - Principal facts and density estimates for borehole gravity stations in exploratory wells Ue4ah, Ue7j, Ue1h, Ue1q, Ue2co, and USW-H1 at the Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr82277","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-277","title":"Principal facts and density estimates for borehole gravity stations in exploratory wells Ue4ah, Ue7j, Ue1h, Ue1q, Ue2co, and USW-H1 at the Nevada Test Site, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82277","usgsCitation":"Robbins, S.L., Schmoker, J., and Hester, T., 1982, Principal facts and density estimates for borehole gravity stations in exploratory wells Ue4ah, Ue7j, Ue1h, Ue1q, Ue2co, and USW-H1 at the Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 82-277, 36 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82277.","productDescription":"36 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0277/report-thumb.jpg"},{"id":38648,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0277/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a7d7","contributors":{"authors":[{"text":"Robbins, S. L.","contributorId":49766,"corporation":false,"usgs":true,"family":"Robbins","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":162101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoker, J. W.","contributorId":69964,"corporation":false,"usgs":true,"family":"Schmoker","given":"J. W.","affiliations":[],"preferred":false,"id":162102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hester, T.C.","contributorId":93054,"corporation":false,"usgs":true,"family":"Hester","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":162103,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10865,"text":"ofr82911 - 1982 - Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","interactions":[{"subject":{"id":23687,"text":"ofr80572 - 1980 - Effects of Urbanization on the Magnitude and Frequency of Floods on Small Streams in Tennessee - Basic Data Report No. 1","indexId":"ofr80572","publicationYear":"1980","noYear":false,"title":"Effects of Urbanization on the Magnitude and Frequency of Floods on Small Streams in Tennessee - Basic Data Report No. 1"},"predicate":"SUPERSEDED_BY","object":{"id":10865,"text":"ofr82911 - 1982 - Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","indexId":"ofr82911","publicationYear":"1982","noYear":false,"title":"Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2"},"id":1}],"lastModifiedDate":"2013-08-12T10:51:53","indexId":"ofr82911","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-911","title":"Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","docAbstract":"Peak stages, discharges, and rainfall recorded at 22 gaging stations on streams draining small (less than 25 mi super 2) urbanized basins across Tennessee are presented. The gaged basins are in 17 different municipalities with populations ranging between 5,000 and 100,000. The report gives a description of each gaged site along with a data sheet on which peak stages, discharges, and corresponding rainfall are listed. The description gives the station location, type of gage, basin characteristics, and general remarks. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82911","usgsCitation":"Robbins, C.H., 1982, Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2: U.S. Geological Survey Open-File Report 82-911, iii, 28 p. :map ;28 cm., https://doi.org/10.3133/ofr82911.","productDescription":"iii, 28 p. :map ;28 cm.","costCenters":[],"links":[{"id":971,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_82-911","linkFileType":{"id":5,"text":"html"}},{"id":145078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":276364,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/ofr_82-911/pdf/ofr_82-911_a.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fce8","contributors":{"authors":[{"text":"Robbins, Clarence H.","contributorId":44159,"corporation":false,"usgs":true,"family":"Robbins","given":"Clarence","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10794,"text":"ofr82959 - 1982 - Zeolites in the Pine Ridge Indian Reservation, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82959","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-959","title":"Zeolites in the Pine Ridge Indian Reservation, South Dakota","docAbstract":"Zeolites of possible commercial value occur in the Brule Formation of Oligocene age and the Sharps Formation (Harksen, 1961) of Miocene age which crop out in a wide area in the northern part of the Pine Ridge Indian Reservation. The thickness of the zeolite-bearing Interval and the extent of areas within the Interval which contain significant amounts of zeolites are far greater than was expected prior to this investigation. The shape of the zeolite-bearing Interval is tabular and the dimensions of Its exposure are roughly 10 ml x 200 mi x 150 ft (16 km x 160 km x 45 m) thick. Within the study area, there are tracts in which the zeolite resource potential is significant (see pl. 2). \r\n\r\nThis report is intended to inform the Oglala Sioux Tribe of some of the most promising zeolite occurrences. Initial steps can then be taken by the Tribe toward possible development of the resources, should they wish to do so. The data contained herein identify areas of high zeolite potential, but are not adequate to establish economic value for the deposits. If development is recommended by the tribal government, we suggest that the tribal government contact companies involved in research and production of natural zeolites and provide them with the data in this report.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82959","usgsCitation":"Raymond, W.H., Bush, A., and Gude, A.J., 1982, Zeolites in the Pine Ridge Indian Reservation, South Dakota: U.S. Geological Survey Open-File Report 82-959, 16 p., 1 over-size sheet, ill., map ;28 cm., https://doi.org/10.3133/ofr82959.","productDescription":"16 p., 1 over-size sheet, ill., map ;28 cm.","costCenters":[],"links":[{"id":144931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0959/report-thumb.jpg"},{"id":20760,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0959/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20761,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0959/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38591,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0959/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d978","contributors":{"authors":[{"text":"Raymond, William H.","contributorId":48555,"corporation":false,"usgs":true,"family":"Raymond","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, Alfred L.","contributorId":48977,"corporation":false,"usgs":true,"family":"Bush","given":"Alfred L.","affiliations":[],"preferred":false,"id":161976,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gude, Arthur J. 3rd 3rd","contributorId":34932,"corporation":false,"usgs":true,"family":"Gude","given":"Arthur","suffix":"3rd","email":"","middleInitial":"J. 3rd","affiliations":[],"preferred":false,"id":161974,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10727,"text":"ofr82136 - 1982 - A regional assessment of potential environmental hazards to and limitations on petroleum development of the Southeastern United States Atlantic continental shelf, slope, and rise, offshore North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr82136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-136","title":"A regional assessment of potential environmental hazards to and limitations on petroleum development of the Southeastern United States Atlantic continental shelf, slope, and rise, offshore North Carolina","docAbstract":"More than 11,000 km of high-resolution seismic-reflection data, 325 km of mid-range sidescan-sonar data, and 500 km of long-range sidescan-sonar data were examined and used to construct an environmental geology map of the Continental Shelf, Slope, and Rise for the area of the U.S. Atlantic margin between lats. 32?N. and 37?N. Hardgrounds and two faults described in previous literature also are shown on the map. \r\n\r\nOn the Continental Shelf, at least two faults, the Helena Banks fault and the White Oak lineament, appear to be tectonic in origin. However, a lack of historical seismicity associated with these faults indicates that they are probably not active at the present time. Hardgrounds are widely scattered but are most abundant in Onslow Bay. Although paleostream channels are common nearshore, they do not appear to be common on the central and outer shelf except off Albemarle Sound where extensive Pleistocene, Pliocene, and late Miocene channels extend across the shelf. Mobile bottom sediments are confined mainly to the shoals off Cape Romain, Cape Fear, Cape Lookout, and Cape Hatteras. Elsewhere the sand cover is thin, and older more indurated rocks are present in subcrop. \r\n\r\nNo slope-instability features were noted on the Florida-Hatteras slope off North Carolina. The lack of features indicates that this slope is relatively stable. \r\n\r\nEvidence for scour by strong currents is ubiquitous on the northern Blake Plateau although deep-water reefs are sparse. The outer edge of the plateau is dominated by a major growth fault and numerous splay and antithetic faults. These faults are the product of salt tectonism in the Carolina trough and thus are not associated with seismicity. Displacements observed near the sea floor and breached diapirs offshore indicate that the main fault is still moving. Associated with the faults are collapse features that are interpreted to be caused by karst solution and cavernous porosity in Eocene and Oligocene limestones at depth. \r\n\r\nMajor slumps have taken place in two large areas of the Continental Slope. Seismic-reflection profiles of the southern area, centered on the lower slope at 1at. 33?N., long. 76?W., show a 80-m-hlgh scarp in which bedding has been truncated. Rotational slump faults are present in this area on the middle and upper slope. Sidescan images show that large blocks have slid downslope from the scarp face, furrowing the bottom. High-resolution (3.5-kHz) records show that the rotational slump faults upslope are active. The association of these slumps and the scarps with salt diapirs suggests subsidence accompanying salt tectonism as the cause. Seismic-reflection records over the northern area, at about fat. 36?20'N., long. 74?40'W., show two steep scarps, each about 225 m high on the upper and middle-slope. These slump scars and an absence of Pleistocene sediments indicate that large blocks of the slope have been removed by slumping. \r\n\r\nThe slope north of fat. 35?N. is highly dissected by canyons. Mid-range sidescan-sonar records suggest that the canyons are the product of mass wasting and have probably formed largely by slumping. \r\n\r\nSediments in a wide zone on the upper rise are highly disturbed and faulted owing to salt tectonism. Twenty-six salt diapirs are mapped, as is a zone of disturbed bottom related to salt tectonism. \r\n\r\nAn area of frozen bottom (clathrate) under which shallow free gas is trapped underlies the outer Blake Plateau, the slope, and the upper rise. Although the hazards of drilling into or through clathrates have not been tested, the release of gas from beneath this frozen layer may prove to be a primary hazard to exploration.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82136","usgsCitation":"Popenoe, P., Coward, E., and Cashman, K.V., 1982, A regional assessment of potential environmental hazards to and limitations on petroleum development of the Southeastern United States Atlantic continental shelf, slope, and rise, offshore North Carolina: U.S. Geological Survey Open-File Report 82-136, 71 p., 1 over-size sheet, maps ;28 cm., https://doi.org/10.3133/ofr82136.","productDescription":"71 p., 1 over-size sheet, maps ;28 cm.","costCenters":[],"links":[{"id":143343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0136/report-thumb.jpg"},{"id":38538,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0136/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38539,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0136/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a849d","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":161864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coward, E. L.","contributorId":84375,"corporation":false,"usgs":true,"family":"Coward","given":"E. L.","affiliations":[],"preferred":false,"id":161865,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cashman, K. V.","contributorId":16831,"corporation":false,"usgs":true,"family":"Cashman","given":"K.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":161863,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10860,"text":"ofr82980 - 1982 - Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82980","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-980","title":"Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California","docAbstract":"Geological, geophysical, thermal, petrophysical and hydrological data available for the East Mesa hydrothermal system that are pertinent to the construction of a computer model of the natural flow of heat and fluid mass within the system are assembled and correlated. A conceptual model of the full system is developed and a subregion selected for quantitative modeling. By invoking the .Boussinesq approximation, valid for describing the natural flow of heat and mass in a liquid hydrothermal system, it is found practical to carry computer simulations far enough in time to ensure that steady-state conditions are obtained. Initial calculations for an axisymmetric model approximating the system demonstrate that the vertical formation permeability of the deep East Mesa system must be very low (kv ~ 0.25 to 0.5 md). Since subsurface temperature and surface heat flow data exhibit major deviations from the axisymmetric approximation, exploratory three-dimensional calculations are performed to assess the effects of various mechanisms which might operate to produce such observed asymmetries. A three-dimensional model evolves from this iterative data synthesis and computer analysis which includes a hot fluid convective source distributed along a leaky fault radiating northward from the center of the hot spot and realistic variations in the reservoir formation properties.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82980","usgsCitation":"Riney, T.D., Pritchett, J., and Rice, L., 1982, Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California: U.S. Geological Survey Open-File Report 82-980, 118 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82980.","productDescription":"118 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0980/report-thumb.jpg"},{"id":38644,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0980/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcb4b","contributors":{"authors":[{"text":"Riney, T. David","contributorId":92674,"corporation":false,"usgs":true,"family":"Riney","given":"T.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":162090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pritchett, J.W.","contributorId":29433,"corporation":false,"usgs":true,"family":"Pritchett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":162088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rice, L.F.","contributorId":59799,"corporation":false,"usgs":true,"family":"Rice","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":162089,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10568,"text":"ofr81128 - 1982 - Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr81128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-128","title":"Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado","docAbstract":"Analysis of hydrologic data from the Kansas River basin suggests that the channels of the lower Solomon, Saline, and Smoky Hill Rivers have narrowed and stabilized as a result of construction of upstream reservoirs. The Kansas River channel, however, remains relatively unstable and locally active. Streamflow regulation and sediment trapping by reservoirs are possible causes of changes occurring at various Kansas River sites. An inferred deficiency of the suspended-sediment load, however, is likely to cause continuing instability. Suspended sediment in the Kansas River apparently is too sparse to form and maintain stable alluvial banks. The deficiency probably results in an increase of bed material movement, general channel widening, and local braiding. Significant channel degradation is lacking at most sites, but may occur in response to long-term (decades-to-centuries) regulation. Recent degradation near Bonner Springs, Kans., may be the result of sand and gravel removal. Any imposed changes that shorten the channel or reduce the suspended-sediment discharge of the Kansas River are expected to cause additional channel instability. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81128","usgsCitation":"Osterkamp, W.R., Curtis, R., and Crowther, H., 1982, Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado: U.S. Geological Survey Open-File Report 81-128, 71 p.  :ill., maps ;28 cm., https://doi.org/10.3133/ofr81128.","productDescription":"71 p.  :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0128/report-thumb.jpg"},{"id":38401,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae003","contributors":{"authors":[{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Curtis, R.E.","contributorId":80741,"corporation":false,"usgs":true,"family":"Curtis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":161608,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crowther, H.G.","contributorId":86629,"corporation":false,"usgs":true,"family":"Crowther","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":161609,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33484,"text":"b1506AE - 1982 - Mineral resources of the Sheep Mountain Wilderness study area and the Cucamonga Wilderness and additions, Los Angeles and San Bernardino Counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"b1506AE","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1506","chapter":"A-E","title":"Mineral resources of the Sheep Mountain Wilderness study area and the Cucamonga Wilderness and additions, Los Angeles and San Bernardino Counties, California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1506AE","usgsCitation":"Evans, J.G., Ridenour, J., Pankratz, L., Schmauch, S., and and Zilka, N.T., 1982, Mineral resources of the Sheep Mountain Wilderness study area and the Cucamonga Wilderness and additions, Los Angeles and San Bernardino Counties, California: U.S. Geological Survey Bulletin 1506, v, 92 p. : ill., maps ; 24 cm., https://doi.org/10.3133/b1506AE.","productDescription":"v, 92 p. : ill., maps ; 24 cm.","costCenters":[],"links":[{"id":167668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1506a-e/report-thumb.jpg"},{"id":61392,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1506a-e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61390,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1506a-e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61391,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1506a-e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a0c9","contributors":{"authors":[{"text":"Evans, James G. jevans@usgs.gov","contributorId":2396,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"jevans@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":211337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ridenour, James","contributorId":87540,"corporation":false,"usgs":true,"family":"Ridenour","given":"James","email":"","affiliations":[],"preferred":false,"id":211341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pankratz, LeRoy","contributorId":32220,"corporation":false,"usgs":true,"family":"Pankratz","given":"LeRoy","affiliations":[],"preferred":false,"id":211339,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schmauch, S. W.","contributorId":53790,"corporation":false,"usgs":true,"family":"Schmauch","given":"S. W.","affiliations":[],"preferred":false,"id":211340,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"and Zilka, N. T.","contributorId":12096,"corporation":false,"usgs":true,"family":"and Zilka","given":"N.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":211338,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":10715,"text":"ofr82967 - 1982 - Disturbed zones: Indicators of deep-seated subsurface faults in the Valley and Ridge and Appalachian structural front of Pennsylvania","interactions":[],"lastModifiedDate":"2021-12-17T20:26:15.820299","indexId":"ofr82967","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-967","title":"Disturbed zones: Indicators of deep-seated subsurface faults in the Valley and Ridge and Appalachian structural front of Pennsylvania","docAbstract":"Field studies of geologic structures in the Valley and Ridge and adjacent parts of the Appalachian Plateau provinces in Pennsylvania have shown a new type of structure, formerly poorly understood and frequently unmapped, is a significant indicator of deep-seated subsurface faulting. These structures, herein called disturbed zones, are formed by movement between closely spaced pairs of thrust faults. Disturbed zones are characterized at the surface by long, narrow, intensely folded and faulted zones of rocks in a relatively undisturbed stratigraphic sequence. These zones are frequently kilometers to tens of kilometers long and tens to hundreds of meters wide. Although disturbed zones generally occur in sequences of alternating siltstone and shale beds, they can also occur in other lithologies including massively-bedded sandstones and carbonates. \r\n\r\nDisturbed zones are not only easily recognized in outcrop but their presence can also be inferred on geologic maps by disharmonic fold patterns, which necessitates a detachment between adjacent units that show the disharmony. \r\n\r\nA number of geologic problems can be clarified by understanding the principles of the sequence of formation and the method of location of disturbed zones, including the interpretation of some published geologic cross sections and maps. \r\n\r\nThe intense folding and faulting which accompanies the formation of a typical disturbed zone produces a region of fracture porosity which, if sealed off from the surface, might well serve as a commercially-exploitable hydrocarbon trap. We believe that the careful mapping of concentrations of disturbed zones can serve as an important exploration method which is much less expensive than speculation seismic lines.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82967","usgsCitation":"Pohn, H.A., and Purdy, T.L., 1982, Disturbed zones: Indicators of deep-seated subsurface faults in the Valley and Ridge and Appalachian structural front of Pennsylvania: U.S. Geological Survey Open-File Report 82-967, Report: 87 p.; 1 Plate: 29.75 × 30.57 inches, https://doi.org/10.3133/ofr82967.","productDescription":"Report: 87 p.; 1 Plate: 29.75 × 30.57 inches","costCenters":[],"links":[{"id":393053,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13879.htm"},{"id":38526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0967/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38525,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0967/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0967/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.875,\n              39.75\n            ],\n            [\n              -76.75,\n              39.75\n            ],\n            [\n              -76.75,\n              41.3750\n            ],\n            [\n              -78.875,\n              41.3750\n            ],\n            [\n              -78.875,\n              39.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d8d3","contributors":{"authors":[{"text":"Pohn, Howard A.","contributorId":66681,"corporation":false,"usgs":true,"family":"Pohn","given":"Howard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purdy, Terri L.","contributorId":87950,"corporation":false,"usgs":true,"family":"Purdy","given":"Terri","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161846,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56199,"text":"wdrNY813 - 1982 - Water resources data, New York, water year 1981, volume 3, western New York","interactions":[],"lastModifiedDate":"2020-12-14T23:43:29.321806","indexId":"wdrNY813","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"NY-81-3","title":"Water resources data, New York, water year 1981, volume 3, western New York","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY813","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, New York, water year 1981, volume 3, western New York: U.S. Geological Survey Water Data Report NY-81-3, viii, 223 p., 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,{"id":10487,"text":"ofr82591 - 1982 - Proceedings of Workshop XVI; The dynamic characteristics of faulting inferred from recordings of strong ground motion","interactions":[],"lastModifiedDate":"2016-05-09T11:01:11","indexId":"ofr82591","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-591","title":"Proceedings of Workshop XVI; The dynamic characteristics of faulting inferred from recordings of strong ground motion","docAbstract":"<p>The strong ground motions radiated by earthquake faulting are controlled by the dynamic characteristics of the faulting process. Although this assertion seems self-evident, seismologists have only recently begun to derive and test quantitative relations between common measures of strong ground motion and the dynamic characteristics of faulting. Interest in this problem has increased dramatically in past several years, however, resulting in a number of important advances. The research presented in this workshop is a significant part of this scientific development. Watching this development occur through the work of many scientists is exciting; to be able to gather a number of these scientists together in one workshop is a remarkable opportunity.</p>","conferenceTitle":"Workshop XVI","conferenceDate":"October 21-23, 1981","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Meno Park, CA","doi":"10.3133/ofr82591","collaboration":"Sponsored by U.S. Nuclear Regulatory Commission","usgsCitation":"1982, Proceedings of Workshop XVI; The dynamic characteristics of faulting inferred from recordings of strong ground motion: U.S. Geological Survey Open-File Report 82-591, 976 p., https://doi.org/10.3133/ofr82591.","productDescription":"976 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320995,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0591/report-2.pdf","text":"Volume II","linkFileType":{"id":1,"text":"pdf"}},{"id":143914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0591/report-thumb.jpg"},{"id":320994,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0591/report-1.pdf","text":"Volume I","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660798","contributors":{"compilers":[{"text":"Jacobson, Muriel L.","contributorId":79094,"corporation":false,"usgs":true,"family":"Jacobson","given":"Muriel L.","affiliations":[],"preferred":false,"id":628928,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"editors":[{"text":"Boatwright, John 0000-0002-6931-5241 boat@usgs.gov","orcid":"https://orcid.org/0000-0002-6931-5241","contributorId":1938,"corporation":false,"usgs":true,"family":"Boatwright","given":"John","email":"boat@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":628927,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":10720,"text":"ofr82931 - 1982 - Preliminary appraisal of gravity and magnetic data at Syncline Ridge, western Yucca Flat, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2021-12-02T22:27:21.928652","indexId":"ofr82931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-931","title":"Preliminary appraisal of gravity and magnetic data at Syncline Ridge, western Yucca Flat, Nevada Test Site, Nye County, Nevada","docAbstract":"A gravity and magnetic study of the Syncline Ridge area was conducted as part of an investigation of argillite rocks of the Eleana Formation under consideration as a medium for the possible storage of high-level radioactive waste. \r\n\r\nBouguer gravity anomaly data, viewed in light of densities obtained by gamma-gamma logs and previous work of D. L. Healey (1968), delineate two regions of steep negative gradient where Cenozoic rocks and sediments are inferred to abruptly thicken: (1) the western third of the study area where Tertiary volcanic rocks are extensively exposed and (2) the northeast corner of the area where Quaternary alluvium is exposed and where volcanic rocks are inferred to occur at depth. In the remainder of the area, a region extending contiguously from Mine Mountain northwestward through Syncline Ridge to the Eleana Range, the gravity data indicate that the Eleana Formation, where not exposed, is buried at depths of less than about 200 m, except in a limited area of exposed older Paleozoic rocks on Mine Mountain. Quaternary alluvium and Tertiary volcanic rocks are inferred to occur in this region as veneers or shallow dishes of deposit on Tippipah Limestone or Eleana Formation. Low-level aeromagnetic anomaly data, covering the western two-thirds of the study area, delineate relatively magnetic tuff units within the Tertiary volcanic rocks and provide a very attractive means for distinguishing units of normal polarization from units of reversed polarization. If used in conjunction with results of previous magnetization studies of G. D. Bath (1968), the low-level survey may prove to be an effective tool for mapping specific tuff members in the volcanic terrane. \r\n\r\nThe important question of the feasibility of discriminating high-quartz argillite from low-quartz argillite of the Eleana Formation using surface gravity data remains unresolved. If the more highly competent, denser, high-quartz phase should occur as stratigraphic units many tens of meters thick, closely spaced gravity data may reliably detect these units. If the high-quartz phase occurs only as relatively thin units, interbedded with low-quartz phase, borehole gravity surveying can be used much more effectively than equivalent surface gravity surveying.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82931","usgsCitation":"Ponce, D.A., and Hanna, W.F., 1982, Preliminary appraisal of gravity and magnetic data at Syncline Ridge, western Yucca Flat, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 82-931, ii, 22 p., https://doi.org/10.3133/ofr82931.","productDescription":"ii, 22 p.","costCenters":[],"links":[{"id":392418,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13861.htm"},{"id":38531,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0931/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0931/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Syncline Ridge, western Yucca Flat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.25,\n              37\n            ],\n            [\n              -116.125,\n              37\n            ],\n            [\n              -116.125,\n              37.117\n            ],\n            [\n              -116.25,\n              37.117\n            ],\n            [\n              -116.25,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca72","contributors":{"authors":[{"text":"Ponce, David A. 0000-0003-4785-7354 ponce@usgs.gov","orcid":"https://orcid.org/0000-0003-4785-7354","contributorId":1049,"corporation":false,"usgs":true,"family":"Ponce","given":"David","email":"ponce@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":161853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanna, William F.","contributorId":104045,"corporation":false,"usgs":true,"family":"Hanna","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":161854,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44525,"text":"wri824080 - 1982 - Hydrogeologic and water-quality characteristics of the Ironton-Galesville aquifer, southeast Minnesota","interactions":[],"lastModifiedDate":"2022-02-18T22:27:58.766312","indexId":"wri824080","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4080","title":"Hydrogeologic and water-quality characteristics of the Ironton-Galesville aquifer, southeast Minnesota","docAbstract":"<p>Quality of water in the Ironton-Galesville aquifer is generally acceptable for all kinds of uses. Calcium magnesium bicarbonate type water is most common. The dissolved-solids concentration ranges from about 200 to 1,000 milligrams per liter. The lowest values are in the northern part of the aquifer, where the bedrock is at or close to land surface, and the lowest ones are in the southwestern part, where leakage into the aquifer from overlying Cretaceous deposits is highly mineralized water. The concentrations of the major ions, except for bicarbonate and chloride, also increase toward the southwest. Confining beds protect the aquifer from surface pollutants, but high sulfate and iron concentrations and hardness degrade water quality locally in some places.</p>\n<p>The aquifer was deposited from Paleozoic seas that occupied a shallow depression known as the Hollandale embayment. The surface of the Ironton-Galesville aquifer dips toward the interior of the embayment. The aquifer is as deep as 1,000 feet below land surface and as thick as 325 feet. The Ironton and Galesville Sandstones are both white and medium grained. The aquifer is used mainly in the northern and western parts of the study area, where it is the uppermost bedrock aquifer,</p>\n<p>This report is one of a series on the hydrogeology and water quality of the 14 principal aquifers in Minnesota prepared by the U.S. Geological Survey. The U.S. Environmental Protection Agency requested these studies because of the need for information to develop its Underground Injection Control Program.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri824080","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Ruhl, J.F., Wolf, R.J., and Adolphson, D.G., 1982, Hydrogeologic and water-quality characteristics of the Ironton-Galesville aquifer, southeast Minnesota: U.S. Geological Survey Water-Resources Investigations Report 82-4080, 2 Plates: 39.95 x 34.69 inches and 40.18 x 35.25 inches, https://doi.org/10.3133/wri824080.","productDescription":"2 Plates: 39.95 x 34.69 inches and 40.18 x 35.25 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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F.","contributorId":81866,"corporation":false,"usgs":true,"family":"Ruhl","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229931,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":229933,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20582,"text":"ofr82308 - 1982 - Fortran program to compute chemical geothermometers for geothermal fluids","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr82308","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-308","title":"Fortran program to compute chemical geothermometers for geothermal fluids","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82308","usgsCitation":"Rapport, A., 1982, Fortran program to compute chemical geothermometers for geothermal fluids: U.S. Geological Survey Open-File Report 82-308, 27 p., 28 cm., https://doi.org/10.3133/ofr82308.","productDescription":"27 p., 28 cm.","costCenters":[],"links":[{"id":152952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0308/report-thumb.jpg"},{"id":50101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0308/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49aae4b07f02db5c4afd","contributors":{"authors":[{"text":"Rapport, A.L.","contributorId":42240,"corporation":false,"usgs":true,"family":"Rapport","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":182886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59863,"text":"mf1376 - 1982 - Map showing the 200-foot thickness contour of surficial deposits and the landward limit of bay mud deposits of San Francisco, California","interactions":[],"lastModifiedDate":"2019-05-29T14:33:32","indexId":"mf1376","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1376","title":"Map showing the 200-foot thickness contour of surficial deposits and the landward limit of bay mud deposits of San Francisco, California","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1376","usgsCitation":"Joyner, W.B., 1982, Map showing the 200-foot thickness contour of surficial deposits and the landward limit of bay mud deposits of San Francisco, California: U.S. Geological Survey Miscellaneous Field Studies Map 1376, 1 Plate: 77 x 68 cm. , https://doi.org/10.3133/mf1376.","productDescription":"1 Plate: 77 x 68 cm. ","costCenters":[],"links":[{"id":364234,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1376/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1376/report-thumb.jpg"}],"scale":"0","country":"United States","state":"California","city":"San Francisco ","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.5,37.700833333333335 ], [ -122.5,37.8675 ], [ -122.33333333333333,37.8675 ], [ -122.33333333333333,37.700833333333335 ], [ -122.5,37.700833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644768","contributors":{"authors":[{"text":"Joyner, W. B.","contributorId":70746,"corporation":false,"usgs":true,"family":"Joyner","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":262730,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46878,"text":"ofr82818A - 1982 - Geologic map of the Lion Canyon, Matilija, Ojai, Wheeler Springs, and White Ledge Peak quadrangles, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:45","indexId":"ofr82818A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-818","chapter":"A","title":"Geologic map of the Lion Canyon, Matilija, Ojai, Wheeler Springs, and White Ledge Peak quadrangles, California","language":"ENGLISH","doi":"10.3133/ofr82818A","usgsCitation":"Moser, F., and Frizzell, V.A., 1982, Geologic map of the Lion Canyon, Matilija, Ojai, Wheeler Springs, and White Ledge Peak quadrangles, California: U.S. Geological Survey Open-File Report 82-818, 1 map :photocopy ;56 x 69 cm., https://doi.org/10.3133/ofr82818A.","productDescription":"1 map :photocopy ;56 x 69 cm.","costCenters":[],"links":[{"id":108441,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13833.htm","linkFileType":{"id":5,"text":"html"},"description":"13833"},{"id":170758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83767,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0818a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e42","contributors":{"authors":[{"text":"Moser, F.C.","contributorId":99828,"corporation":false,"usgs":true,"family":"Moser","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":234243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frizzell, V. A. Jr.","contributorId":39376,"corporation":false,"usgs":true,"family":"Frizzell","given":"V.","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":234242,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43809,"text":"ofr82388 - 1982 - Heavy-metal content of stream sediments and stream waters, Rolla 1 °X 2° quadrangle, Missouri","interactions":[],"lastModifiedDate":"2021-09-17T19:30:57.230742","indexId":"ofr82388","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-388","title":"Heavy-metal content of stream sediments and stream waters, Rolla 1 °X 2° quadrangle, Missouri","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82388","usgsCitation":"Proctor, P.D., Sinha, B., Afzali, B., Vanhorst, T., and Odland, S., 1982, Heavy-metal content of stream sediments and stream waters, Rolla 1 °X 2° quadrangle, Missouri: U.S. Geological Survey Open-File Report 82-388, 2 Plates: 45.08 × 29.51 inches and 36.88 × 41.79 inches, https://doi.org/10.3133/ofr82388.","productDescription":"2 Plates: 45.08 × 29.51 inches and 36.88 × 41.79 inches","costCenters":[],"links":[{"id":134719,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389441,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13717.htm"},{"id":81360,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0388/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81359,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0388/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Missouri","otherGeospatial":"Rolla 1 °X 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92,\n              37\n            ],\n            [\n              -90,\n              37\n            ],\n            [\n              -90,\n              38\n            ],\n            [\n              -92,\n              38\n            ],\n            [\n              -92,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636397","contributors":{"authors":[{"text":"Proctor, Paul Dean","contributorId":18328,"corporation":false,"usgs":true,"family":"Proctor","given":"Paul","email":"","middleInitial":"Dean","affiliations":[],"preferred":false,"id":228717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sinha, B.","contributorId":29786,"corporation":false,"usgs":true,"family":"Sinha","given":"B.","email":"","affiliations":[],"preferred":false,"id":228718,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Afzali, B.","contributorId":84327,"corporation":false,"usgs":true,"family":"Afzali","given":"B.","email":"","affiliations":[],"preferred":false,"id":228721,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vanhorst, T.","contributorId":69112,"corporation":false,"usgs":true,"family":"Vanhorst","given":"T.","email":"","affiliations":[],"preferred":false,"id":228720,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Odland, S. K.","contributorId":48933,"corporation":false,"usgs":true,"family":"Odland","given":"S. K.","affiliations":[],"preferred":false,"id":228719,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":9927,"text":"ofr82329 - 1982 - Acoustic systems for the measurement of streamflow","interactions":[{"subject":{"id":9927,"text":"ofr82329 - 1982 - Acoustic systems for the measurement of streamflow","indexId":"ofr82329","publicationYear":"1982","noYear":false,"title":"Acoustic systems for the measurement of streamflow"},"predicate":"SUPERSEDED_BY","object":{"id":2066,"text":"wsp2213 - 1983 - Acoustic systems for the measurement of streamflow","indexId":"wsp2213","publicationYear":"1983","noYear":false,"title":"Acoustic systems for the measurement of streamflow"},"id":1}],"supersededBy":{"id":2066,"text":"wsp2213 - 1983 - Acoustic systems for the measurement of streamflow","indexId":"wsp2213","publicationYear":"1983","noYear":false,"title":"Acoustic systems for the measurement of streamflow"},"lastModifiedDate":"2017-02-07T09:28:38","indexId":"ofr82329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-329","title":"Acoustic systems for the measurement of streamflow","docAbstract":"Very little information is available concerning acoustic velocity meter (AVM) operation, performance, and limitations. This report provides a better understanding about the application of AVM instrumentation to streamflow measurment. Operational U.S. Geological Survey systems have proven that AVM equipment is accurate and dependable. AVM equipment has no practical upper limit of measureable velocity if sonic transducers are securely placed and adequately protected, and will measure velocitites as low as 0.1 meter per second which is normally less than the threshold level for mechanical or head-loss meters. In some situations the performance of AVM equipment may be degraded by multipath interference, signal bending, signal attenuation, and variable streamline orientation. Smaller, less-expensive, more conveniently operable microprocessor equipment is now available which should increase use of AVM systems in streamflow applications. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82329","usgsCitation":"Laenen, A., and Smith, W., 1982, Acoustic systems for the measurement of streamflow: U.S. Geological Survey Open-File Report 82-329, viii, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82329.","productDescription":"viii, 53 p. :ill., maps ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":144043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0329/report-thumb.jpg"},{"id":112929,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0329/report.pdf","size":"3506","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a178","contributors":{"authors":[{"text":"Laenen, Antonius","contributorId":107673,"corporation":false,"usgs":true,"family":"Laenen","given":"Antonius","email":"","affiliations":[],"preferred":false,"id":160526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Winchell","contributorId":20311,"corporation":false,"usgs":true,"family":"Smith","given":"Winchell","email":"","affiliations":[],"preferred":false,"id":160525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43750,"text":"ofr8286 - 1982 - Hydrogeology for land-use planning: The Potter Creek area, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2021-12-17T22:06:13.061761","indexId":"ofr8286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-86","title":"Hydrogeology for land-use planning: The Potter Creek area, Anchorage, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8286","usgsCitation":"Emanuel, R.P., and Cowing, D.J., 1982, Hydrogeology for land-use planning: The Potter Creek area, Anchorage, Alaska: U.S. Geological Survey Open-File Report 82-86, 4 Plates: 35.00 × 23.50 inches, https://doi.org/10.3133/ofr8286.","productDescription":"4 Plates: 35.00 × 23.50 inches","costCenters":[],"links":[{"id":135227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81308,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0086/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81307,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0086/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81306,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0086/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81305,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0086/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393066,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13844.htm"}],"scale":"25000","country":"United States","state":"Alaska","city":"Anchorage","otherGeospatial":"Potter Creek area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.812,\n              61.037\n            ],\n            [\n              -149.625,\n              61.037\n            ],\n            [\n              -149.625,\n              61.08\n            ],\n            [\n              -149.812,\n              61.08\n            ],\n            [\n              -149.812,\n              61.037\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6250e7","contributors":{"authors":[{"text":"Emanuel, Richard P.","contributorId":98287,"corporation":false,"usgs":true,"family":"Emanuel","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":228644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cowing, Derrill J.","contributorId":97473,"corporation":false,"usgs":true,"family":"Cowing","given":"Derrill","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":228643,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66274,"text":"i1411 - 1982 - Topographic map of Mount St. Helens, Washington, showing changes between April 11 and May 16, 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:13:24","indexId":"i1411","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1411","subseriesTitle":"NONE","title":"Topographic map of Mount St. Helens, Washington, showing changes between April 11 and May 16, 1980","language":"ENGLISH","doi":"10.3133/i1411","usgsCitation":"Jordan, R., and Kieffer, H.H., 1982, Topographic map of Mount St. Helens, Washington, showing changes between April 11 and May 16, 1980: U.S. Geological Survey IMAP 1411, 1 map :col. ;73 x 79 cm., on sheet 86 x 110 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1411.","productDescription":"1 map :col. ;73 x 79 cm., on sheet 86 x 110 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":255732,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1411/plate-1.pdf","size":"15461","linkFileType":{"id":1,"text":"pdf"}},{"id":255733,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1411/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":255734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1411/report-thumb.jpg"}],"scale":"10000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629df8","contributors":{"authors":[{"text":"Jordan, Raymond","contributorId":91466,"corporation":false,"usgs":true,"family":"Jordan","given":"Raymond","email":"","affiliations":[],"preferred":false,"id":274282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kieffer, H. H.","contributorId":40725,"corporation":false,"usgs":false,"family":"Kieffer","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":274281,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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