During August 1980, the U.S. Geological Survey (USGS) collected 982 km of single-channel seismic-reflection data on the Continental Slope and upper Rise between Lindenkohl Canyon and Toms Canyon, off New Jersey (fig. 1). The work was conducted aboard R/V GYRE (cruise 80-G-7A). The trackline grid of this cruise extends and supplements a grid of seismic-reflection lines collected by the USGS over this area in 1978 and 1979 (Robb, 1980a, b). These data were collected in cooperation with the Bureau of Land Management (Memorandum of Understanding AA851-MUO-18) to map the geology and the topography of the area in order to identify potential geologic hazards to oil and gas exploration and development. The suite of profiles that was collected includes 40-in3 airgun (recorded as 4-second and 2-second) and 800-J sparker (recorded as 1-second) profiles and 3.5-kHz bathymetry, recorded as 1-second profiles. All times represent two-way travel times. Details of the sources, cables, and instruments, as well as filter settings, are shown in table 1.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82305","usgsCitation":"Hampson, J., 1982, High-resolution seismic-reflection profiles collected aboard R/V GYRE, cruise GYRE 80-G-7A, over the continental slope and upper continental rise, offshore New Jersey: U.S. Geological Survey Open-File Report 82-305, 4 p., https://doi.org/10.3133/ofr82305.","productDescription":"4 p.","costCenters":[],"links":[{"id":495905,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142325,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0305/report-thumb.jpg"}],"country":"United States","state":"New 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Henry Wilderness, Montana","language":"ENGLISH","doi":"10.3133/ofr821073","usgsCitation":"Bankey, V., Kleinkopf, M.D., Brickey, M., and Mancinelli, J., 1982, Principal facts and a complete Bouguer anomaly map for a gravity study of the proposed Mt. Henry Wilderness, Montana: U.S. Geological Survey Open-File Report 82-1073, 1 map ;32 x 38 cm. +1 text (14 p. ; 28 cm.), https://doi.org/10.3133/ofr821073.","productDescription":"1 map ;32 x 38 cm. +1 text (14 p. ; 28 cm.)","costCenters":[],"links":[{"id":172948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1073/report-thumb.jpg"},{"id":71859,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71860,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668160","contributors":{"authors":[{"text":"Bankey, Viki viki@usgs.gov","contributorId":1238,"corporation":false,"usgs":true,"family":"Bankey","given":"Viki","email":"viki@usgs.gov","affiliations":[],"preferred":true,"id":223212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kleinkopf, M. Dean","contributorId":37723,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","email":"","middleInitial":"Dean","affiliations":[],"preferred":false,"id":223214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brickey, Mike","contributorId":105298,"corporation":false,"usgs":true,"family":"Brickey","given":"Mike","email":"","affiliations":[],"preferred":false,"id":223215,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mancinelli, Joe","contributorId":19180,"corporation":false,"usgs":true,"family":"Mancinelli","given":"Joe","email":"","affiliations":[],"preferred":false,"id":223213,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7742,"text":"ofr82298 - 1982 - Allanite-bearing calc-silicate rocks, southern Bighorn Mountains, Wyoming; geologic setting and resources of thorium, uranium, and rare-earth elements","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr82298","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":"82-298","title":"Allanite-bearing calc-silicate rocks, southern Bighorn Mountains, Wyoming; geologic setting and resources of thorium, uranium, and rare-earth elements","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82298","usgsCitation":"Armbrustmacher, T.J., and Sargent, K., 1982, Allanite-bearing calc-silicate rocks, southern Bighorn Mountains, Wyoming; geologic setting and resources of thorium, uranium, and rare-earth elements: U.S. Geological Survey Open-File Report 82-298, 13 p., maps ;28 cm., https://doi.org/10.3133/ofr82298.","productDescription":"13 p., maps ;28 cm.","costCenters":[],"links":[{"id":140662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0298/report-thumb.jpg"},{"id":35202,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687f45","contributors":{"authors":[{"text":"Armbrustmacher, Theodore J.","contributorId":31376,"corporation":false,"usgs":true,"family":"Armbrustmacher","given":"Theodore","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":156524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, Kenneth A.","contributorId":15998,"corporation":false,"usgs":true,"family":"Sargent","given":"Kenneth A.","affiliations":[],"preferred":false,"id":156523,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8099,"text":"ofr82205 - 1982 - Seismicity of the Parkfield, California, region, 1969 to 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr82205","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":"82-205","title":"Seismicity of the Parkfield, California, region, 1969 to 1979","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82205","usgsCitation":"Buhr, G., and Lindh, A., 1982, Seismicity of the Parkfield, California, region, 1969 to 1979: U.S. Geological Survey Open-File Report 82-205, 89 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82205.","productDescription":"89 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0205/report-thumb.jpg"},{"id":35698,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0205/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa8b5","contributors":{"authors":[{"text":"Buhr, G.S.","contributorId":84371,"corporation":false,"usgs":true,"family":"Buhr","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":157144,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindh, A.G.","contributorId":24784,"corporation":false,"usgs":true,"family":"Lindh","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":157143,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10275,"text":"ofr82971 - 1982 - Radon, conductivity, and pH values for 146 water samples from Snowy Range, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82971","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":"82-971","title":"Radon, conductivity, and pH values for 146 water samples from Snowy Range, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82971","usgsCitation":"McHugh, J.B., Ficklin, W.H., and Miller, W.R., 1982, Radon, conductivity, and pH values for 146 water samples from Snowy Range, Wyoming: U.S. Geological Survey Open-File Report 82-971, 8 p., ill. ;28 cm., https://doi.org/10.3133/ofr82971.","productDescription":"8 p., ill. ;28 cm.","costCenters":[],"links":[{"id":142610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0971/report-thumb.jpg"},{"id":38132,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0971/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649a40","contributors":{"authors":[{"text":"McHugh, J. B.","contributorId":79462,"corporation":false,"usgs":true,"family":"McHugh","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":161119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161120,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, W. R.","contributorId":92239,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161121,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8934,"text":"ofr82407 - 1982 - In-situ measurements of seismic velocity at 10 strong motion accelerograph stations in central California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82407","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":"82-407","title":"In-situ measurements of seismic velocity at 10 strong motion accelerograph stations in central California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82407","usgsCitation":"Fumal, T.E., Gibbs, J., and Roth, E.F., 1982, In-situ measurements of seismic velocity at 10 strong motion accelerograph stations in central California: U.S. Geological Survey Open-File Report 82-407, i, 78 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82407.","productDescription":"i, 78 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0407/report-thumb.jpg"},{"id":36541,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0407/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5921","contributors":{"authors":[{"text":"Fumal, T. E.","contributorId":25942,"corporation":false,"usgs":true,"family":"Fumal","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":158579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibbs, J. F.","contributorId":50894,"corporation":false,"usgs":true,"family":"Gibbs","given":"J. F.","affiliations":[],"preferred":false,"id":158580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roth, E. F.","contributorId":6056,"corporation":false,"usgs":true,"family":"Roth","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":158578,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11361,"text":"ofr82297 - 1982 - An alternative hypothesis for sink development above salt cavities in the Detroit area","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82297","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":"82-297","title":"An alternative hypothesis for sink development above salt cavities in the Detroit area","docAbstract":"Subsidence and sink formation resulting from brining operations in the Windsor-Detroit area include the 1954 sink at the Canadian Salt Company brine field near Windsor, Ontario, and the 1971 sinks at the BASF Wyandotte Corporation brine field at Grosse Ile, Mich. Earlier investigations into both occurrences concluded that the mechanism of sink development consisted of the gradual stoping of poorly supported brine-gallery roof rock to the near surface with subsequent surface collapse. A more recent study attempted to describe the mechanism of sink development in terms of the geometry of a cylindrical chimney formed by stoping of roof rock, the height of a cavity at depth, the depth of overlying rock, and the bulking ratio of the rubble formed during stoping. \r\n\r\nPersons with extensive experience in solution mining in the Windsor-Detroit area have expressed doubt that the stoping mechanism could fully explain the development of these sinks. Further, they have proposed that the relatively shallow (300-ft-deep) Sylvania Sandstone, in this case, may be responsible for the sinks by a secondary undermining mechanism to be examined in this paper. The mechanism involves downwarping of the beds overlying the salt cavity and development of a shallower cavity in the Sylvania Sandstone by downward migration of cohesionless sand grains from the Sylvania through openings in the disturbed rock to the lower cavity. This study indicates that under natural conditions the Sylvania will not migrate, even in the presence of large underground water flows because the sandstone possesses some cohesion throughout its depth. However, further investigation has formulated a mechanism that could allow the Sylvania Sandstone to loose its cohesion in response to high horizontal stresses. These stresses could be the result of deformation that accompanies general subsidence and (or) of past geologic processes.\r\n\r\nIncluded in this study were experimental and analytical investigations. As determined by uniaxial and triaxial testing, the Sylvania Sandstone in the Detroit area has been shown to have low compressive strength. In addition, it exhibits an explosive type failure whereby over 50 percent of the sample is reduced to loose granular sand. As a result of these characteristics, the Sylvania Sandstone can loose its cohesion when subjected to high horizontal stresses. \r\n\r\nEfforts at mechanically modeling the Sylvania were made to account for the measurements and observations. Linear arch theory was used for an elastic analysis. Linear arch theory predicts two modes of failure: (1) arch crushing, a compressive failure of the upper portion of the arch due to compressive stresses exceeding the compressive strength of the material, and (2) arch collapse, a sagging of the beds due to compressive strains which reduce the arch line to a length less than the original arch length. The arch crushing mode of failure would then yield the loose granular sand as observed in laboratory testing. Arch collapse would simply result in bed sagging without granulation of the sandstone. Arch collapse is favored by thin-bedded material while arch crushing is favored by thick-bedded material. Arch crushing seems to be a likely mode of failure for the Windsor-Detroit sinks. \r\n\r\nIt is believed that after a crushing failure the sand-water slurry (specific gravity 1.2) which exceeds the density of the cavity brine will migrate downward through cracks and open joints eventually reaching the practically limitless open spaces of the rubble column and salt cavity. As the extent of the cavity within the Sylvania increases in depth and width because of sand migration, a critical span will be reached where the immediately overlying upper Sylvania and the overlying Detroit River Dolomite will fail. The collapse will allow a path for the approximately 100 ft of clay to collapse, resulting in a sink as the surface manifestation.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82297","usgsCitation":"Stump, D., Nieto, A., and Ege, J., 1982, An alternative hypothesis for sink development above salt cavities in the Detroit area: U.S. Geological Survey Open-File Report 82-297, 65 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82297.","productDescription":"65 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0297/report-thumb.jpg"},{"id":39188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0297/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bad","contributors":{"authors":[{"text":"Stump, Daniel","contributorId":35318,"corporation":false,"usgs":true,"family":"Stump","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":163001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nieto, A.S.","contributorId":30629,"corporation":false,"usgs":true,"family":"Nieto","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":163000,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ege, J. R.","contributorId":106117,"corporation":false,"usgs":false,"family":"Ege","given":"J. R.","affiliations":[],"preferred":false,"id":163002,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8885,"text":"ofr82467 - 1982 - Semiquantitative spectrographic analyses of rocks from the Mount Jordan vicinity, Custer County, Idaho","interactions":[],"lastModifiedDate":"2017-06-28T11:55:26","indexId":"ofr82467","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":"82-467","title":"Semiquantitative spectrographic analyses of rocks from the Mount Jordan vicinity, Custer County, Idaho","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82467","usgsCitation":"Foster, F., and Cooley, E., 1982, Semiquantitative spectrographic analyses of rocks from the Mount Jordan vicinity, Custer County, Idaho: U.S. Geological Survey Open-File Report 82-467, 13 p., maps ;28 cm., https://doi.org/10.3133/ofr82467.","productDescription":"13 p., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":36449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0467/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0467/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7a1a","contributors":{"authors":[{"text":"Foster, Fess","contributorId":94308,"corporation":false,"usgs":true,"family":"Foster","given":"Fess","email":"","affiliations":[],"preferred":false,"id":158487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, E.F.","contributorId":83072,"corporation":false,"usgs":true,"family":"Cooley","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":158486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7799,"text":"ofr82738 - 1982 - Principal facts for gravity stations in the Whetstone Roadless Area, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82738","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":"82-738","title":"Principal facts for gravity stations in the Whetstone Roadless Area, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82738","usgsCitation":"Bankey, V., and Kleinkopf, M.D., 1982, Principal facts for gravity stations in the Whetstone Roadless Area, Arizona: U.S. Geological Survey Open-File Report 82-738, 17 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82738.","productDescription":"17 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0738/report-thumb.jpg"},{"id":35299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0738/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6679c8","contributors":{"authors":[{"text":"Bankey, Viki viki@usgs.gov","contributorId":1238,"corporation":false,"usgs":true,"family":"Bankey","given":"Viki","email":"viki@usgs.gov","affiliations":[],"preferred":true,"id":156627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kleinkopf, M. D.","contributorId":10036,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","middleInitial":"D.","affiliations":[],"preferred":false,"id":156628,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11563,"text":"ofr80676 - 1982 - Estimating peak discharges of small rural streams in Massachusetts","interactions":[{"subject":{"id":11563,"text":"ofr80676 - 1982 - Estimating peak discharges of small rural streams in Massachusetts","indexId":"ofr80676","publicationYear":"1982","noYear":false,"title":"Estimating peak discharges of small rural streams in Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":2880,"text":"wsp2214 - 1983 - Estimating peak discharges of small, rural streams in Massachusetts","indexId":"wsp2214","publicationYear":"1983","noYear":false,"title":"Estimating peak discharges of small, rural streams in Massachusetts"},"id":1}],"supersededBy":{"id":2880,"text":"wsp2214 - 1983 - Estimating peak discharges of small, rural streams in Massachusetts","indexId":"wsp2214","publicationYear":"1983","noYear":false,"title":"Estimating peak discharges of small, rural streams in Massachusetts"},"lastModifiedDate":"2022-08-09T15:49:04.64596","indexId":"ofr80676","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":"80-676","title":"Estimating peak discharges of small rural streams in Massachusetts","docAbstract":"Floodflows on natural-flow streams in Massachusetts with drainage areas between 0.25 square miles and 260 square miles may be estimated from drainage area, main-channel slope, mean basin elevation, and the area of swamps, lakes, and ponds. Multiple-regression techniques were used to define the relationship between a suite of basin and climatic characteristics and flood peaks in three flood-frequency regions at a total of 95 sites. Station flood-frequency data were computed following guidelines in Bulletin I7A of the U.S. Water Resources Council. The frequency analyses are based upon weighted skew values, and adjustments for high and low outliers, and historic peak data. Regression equations for estimation of peak discharges for 0.5, 0.2, 0.1, 0.04, 0.02, and 0.01 exceedance probabilities are provided for ungaged sites. An improved sample of flood peaks and gaging stations and the definition of three flood-frequency regions reduced the standard error of estimate by about 5 percent over those for the 1977 relations. Included in this analysis were the synthetic flood-frequency data at eight sites computed using historic climatic data and 10 parameters optimized by calibration of the U.S. Geological Survey's rainfall-runoff model with storm data observed over II years. The equations are applicable to streams unaffected by regulation where the usable manmade storage is less than 4.5 million cubic feet per square mile, or by diversions or urbanization. The equations are restricted to sites where the basin indices are within a specified range outside of eastern Plymouth, Barnstable, Dukes or Nantucket Counties. In these areas, the available data do not adequately define the influence of high infiltration and storage capacities of drainage basins on floodflows.
","largerWorkType":{"id":18,"text":"Report"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80676","collaboration":"Prepared in cooperation with the Massachusetts Department of Public Works and the U.S. Department of Highway Transportation, Federal Highway Administration","usgsCitation":"Wandle, S.W., 1982, Estimating peak discharges of small rural streams in Massachusetts: U.S. Geological Survey Open-File Report 80-676, iv, 33 p., https://doi.org/10.3133/ofr80676.","productDescription":"iv, 33 p.","costCenters":[],"links":[{"id":405034,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0676/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0676/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648677","contributors":{"authors":[{"text":"Wandle, S. William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":163363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40980,"text":"ofr8290 - 1982 - Position of the saltwater-freshwater interface in the upper part of the Floridan Aquifer, southwest Florida, 1979","interactions":[],"lastModifiedDate":"2022-03-17T13:47:15.932115","indexId":"ofr8290","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":"82-90","title":"Position of the saltwater-freshwater interface in the upper part of the Floridan Aquifer, southwest Florida, 1979","docAbstract":"Ground-water withdrawals in southwest Florida are increasing because of urban growth, industrial expansion and increased agricultural irrigation. As a result, the potentiometric surface of the Floridian aquifer has been lowered in some areas, allowing seawater to encroach into the aquifer and threaten the freshwater resources of the area. Effective management of groundwater is needed to control the encroachment and protect the freshwater aquifer.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8290","usgsCitation":"Causseaux, K., and Fretwell, J.D., 1982, Position of the saltwater-freshwater interface in the upper part of the Floridan Aquifer, southwest Florida, 1979: U.S. Geological Survey Open-File Report 82-90, 1 Plate: 38.07 x 28.97 inches, https://doi.org/10.3133/ofr8290.","productDescription":"1 Plate: 38.07 x 28.97 inches","costCenters":[],"links":[{"id":397224,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13851.htm"},{"id":397182,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0090/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0090/report-thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.880859375,\n 25.085598897064752\n ],\n [\n -80.9033203125,\n 25.085598897064752\n ],\n [\n -80.9033203125,\n 29.132970130878636\n ],\n [\n -82.880859375,\n 29.132970130878636\n ],\n [\n -82.880859375,\n 25.085598897064752\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683c48","contributors":{"authors":[{"text":"Causseaux, K.W.","contributorId":7306,"corporation":false,"usgs":true,"family":"Causseaux","given":"K.W.","affiliations":[],"preferred":false,"id":224277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fretwell, J. D.","contributorId":97933,"corporation":false,"usgs":true,"family":"Fretwell","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":224278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11511,"text":"ofr82666C - 1982 - Estimated areas and volumes of sedimentary rock in the United States by province; statistical background data for U.S. Geological Survey Circular 860","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82666C","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":"82-666","chapter":"C","title":"Estimated areas and volumes of sedimentary rock in the United States by province; statistical background data for U.S. Geological Survey Circular 860","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82666C","usgsCitation":"Varnes, K.L., and Dolton, G., 1982, Estimated areas and volumes of sedimentary rock in the United States by province; statistical background data for U.S. Geological Survey Circular 860: U.S. Geological Survey Open-File Report 82-666, 12 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82666C.","productDescription":"12 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0666c/report-thumb.jpg"},{"id":39374,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0666c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1b3","contributors":{"authors":[{"text":"Varnes, K. L.","contributorId":74386,"corporation":false,"usgs":true,"family":"Varnes","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dolton, G.L.","contributorId":51722,"corporation":false,"usgs":true,"family":"Dolton","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":163278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11720,"text":"ofr811180 - 1982 - Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr811180","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":"81-1180","title":"Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida","docAbstract":"This report provides results of reliability and cost-effective studies of the goes satellite data-collection system used to operate a small hydrologic data network in west-central Florida. The GOES system, in its present state of development, was found to be about as reliable as conventional methods of data collection. Benefits of using the GOES system include some cost and manpower reduction, improved data accuracy, near real-time data availability, and direct computer storage and analysis of data. The GOES system could allow annual manpower reductions of 19 to 23 percent with reduction in cost for some and increase in cost for other single-parameter sites, such as streamflow, rainfall, and ground-water monitoring stations. Manpower reductions of 46 percent or more appear possible for multiple-parameter sites. Implementation of expected improvements in instrumentation and data handling procedures should further reduce costs. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811180","usgsCitation":"Woodham, W.M., 1982, Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida: U.S. Geological Survey Open-File Report 81-1180, iv, 27 p., map ;28 cm., https://doi.org/10.3133/ofr811180.","productDescription":"iv, 27 p., map ;28 cm.","costCenters":[],"links":[{"id":143920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1180/report-thumb.jpg"},{"id":39606,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3a6","contributors":{"authors":[{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41283,"text":"ofr82583 - 1982 - Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada","interactions":[{"subject":{"id":41283,"text":"ofr82583 - 1982 - Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada","indexId":"ofr82583","publicationYear":"1982","noYear":false,"title":"Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":4365,"text":"cir877 - 1982 - Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment","indexId":"cir877","publicationYear":"1982","noYear":false,"title":"Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment"},"id":1}],"supersededBy":{"id":4365,"text":"cir877 - 1982 - Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment","indexId":"cir877","publicationYear":"1982","noYear":false,"title":"Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment"},"lastModifiedDate":"2022-03-18T18:03:09.490823","indexId":"ofr82583","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":"82-583","title":"Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82583","usgsCitation":"Miller, C.D., Crandell, D.R., Mullineaux, D.R., Hoblitt, R., and Bailey, R., 1982, Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada: U.S. Geological Survey Open-File Report 82-583, 3 Plates: 42.66 x 21.93 inches or smaller, https://doi.org/10.3133/ofr82583.","productDescription":"3 Plates: 42.66 x 21.93 inches or smaller","costCenters":[],"links":[{"id":171229,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":397323,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0583/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397194,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13768.htm"}],"scale":"500000","country":"United States","state":"California, Nevada","otherGeospatial":"Long Valley - Mono Lake area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.45,\n 36.5\n ],\n [\n -117.417,\n 36.5\n ],\n [\n -117.417,\n 38.833\n ],\n [\n -120.45,\n 38.833\n ],\n [\n -120.45,\n 36.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca8f","contributors":{"authors":[{"text":"Miller, C. Dan","contributorId":38145,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"Dan","affiliations":[],"preferred":false,"id":224767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crandell, D. R.","contributorId":78385,"corporation":false,"usgs":true,"family":"Crandell","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224769,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mullineaux, D. R.","contributorId":64248,"corporation":false,"usgs":true,"family":"Mullineaux","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224768,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hoblitt, R.","contributorId":89536,"corporation":false,"usgs":true,"family":"Hoblitt","given":"R.","affiliations":[],"preferred":false,"id":224771,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bailey, R. A.","contributorId":87531,"corporation":false,"usgs":true,"family":"Bailey","given":"R. A.","affiliations":[],"preferred":false,"id":224770,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":11366,"text":"ofr82203A - 1982 - Multielement chemical and statistical analyses from a uranium hydrogeochemical and stream-sediment survey in and near the Elkhorn Mountains, Jefferson County, Montana. Part I: Surface water","interactions":[],"lastModifiedDate":"2022-09-14T19:18:54.035728","indexId":"ofr82203A","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":"82-203","chapter":"A","title":"Multielement chemical and statistical analyses from a uranium hydrogeochemical and stream-sediment survey in and near the Elkhorn Mountains, Jefferson County, Montana. Part I: Surface water","docAbstract":"Fifty-two surface-water samples, collected from an area south of Helena, Jefferson County, were analyzed for 51 chemical species. Of these variables, 35 showed detectable variation over the area, and 29 were utilized in a correlation analysis.
Two populations are distinguished in the collected samples and are especially evident in the plot of Ca versus U. Samples separated on the basis of U versus Ca proved to represent drainage areas of two differing lithologies. One group was from waters that drain the Boulder batholith, the other from those that drain the Elkhorn Mountains volcanic rocks. These two groups of samples, in general, proved to have parallel but different linear trends between U and other elements. Therefore, the two groups of samples were treated separately in the statistical analyses.
Over the area that drains the Boulder batholith, U concentrations in water ranged from 0.37 to 13.0 μg/l , with a mean of 1.9 μg/l. The samples from streams draining volcanic areas ranged from 0.04 to 1.5 μg/l, with a mean of 0.42 μg/l. The highest U values (12 and 13 μg/l) occur along Badger Creek, Rawhide Creek, Little Buffalo Gulch, and an unnamed tributary to Clancy Creek.
Conductivity, hardness, Ba, Ca, CI, K, Mg, Na and Sr are significantly correlated with U at or better than the 95 percent confidence limit in both populations. For water draining the Boulder batholith, uranium correlates significantly with akalinity, pH, bicarbonate, Li, Mo, NO2+NO3, P04, SiO2, SO4, F, and inorganic carbon. These correlations are similar to those found in a previous study of water samples in north-central New Mexico (Wenrich-Verbeek, 1977b). Uranium in water from the volcanic terrane does not show correlations with any of the above constituents, but does correlate well with V. This relationship with V is absent within the Boulder batholith samples.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82203A","usgsCitation":"Suits, V., and Wenrich, K., 1982, Multielement chemical and statistical analyses from a uranium hydrogeochemical and stream-sediment survey in and near the Elkhorn Mountains, Jefferson County, Montana. Part I: Surface water: U.S. Geological Survey Open-File Report 82-203, ii, 94 p., https://doi.org/10.3133/ofr82203A.","productDescription":"ii, 94 p.","costCenters":[],"links":[{"id":143129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0203a/report-thumb.jpg"},{"id":39192,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0203a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406713,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13681.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","county":"Jefferson County","otherGeospatial":"Elkhorn Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.25,\n 46.25\n ],\n [\n -111.75,\n 46.25\n ],\n [\n -111.75,\n 46.5\n ],\n [\n -112.25,\n 46.5\n ],\n [\n -112.25,\n 46.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48a0","contributors":{"authors":[{"text":"Suits, V. J.","contributorId":30988,"corporation":false,"usgs":true,"family":"Suits","given":"V. J.","affiliations":[],"preferred":false,"id":163008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wenrich, K. J.","contributorId":40203,"corporation":false,"usgs":true,"family":"Wenrich","given":"K. J.","affiliations":[],"preferred":false,"id":163009,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23607,"text":"ofr81330 - 1982 - Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin","interactions":[],"lastModifiedDate":"2017-06-22T11:08:23","indexId":"ofr81330","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":"81-330","title":"Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin","docAbstract":"Volume III presents ground-water quality and physical data on about 1,250 wells and springs in the Delaware River Basin in Pennsylvania. Locations are shown on site-location maps derived from the hydrologic unit map. Codes showing the geologic age and aquifer are provided.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg,, PA","doi":"10.3133/ofr81330","issn":"0094-9140","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Resources","usgsCitation":"Koester, H., and Miller, D., 1982, Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin: U.S. Geological Survey Open-File Report 81-330, iii, 111 p., https://doi.org/10.3133/ofr81330.","productDescription":"iii, 111 p.","numberOfPages":"116","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":154891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0330/report-thumb.jpg"},{"id":277909,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0330/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.8054,39.7241 ], [ -76.8054,41.9983 ], [ -74.707,41.9983 ], [ -74.707,39.7241 ], [ -76.8054,39.7241 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673f1","contributors":{"authors":[{"text":"Koester, H.E.","contributorId":26323,"corporation":false,"usgs":true,"family":"Koester","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":190398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, D.R.","contributorId":106147,"corporation":false,"usgs":true,"family":"Miller","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":190399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11481,"text":"ofr82602 - 1982 - A geochemical survey using heavy mineral concentrates in the Mount Belknap caldera vicinity, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr82602","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":"82-602","title":"A geochemical survey using heavy mineral concentrates in the Mount Belknap caldera vicinity, Utah","docAbstract":"Geochemical surveys of the rocks, heavy-mineral concentrates, and surface and spring waters in the vicinity of the Mount Belknap caldera, Tushar Mountains, west-central Utah, were conducted during the summers of 1978 and 1979. Anomalous concentrations of mostly lithophile elements, particularly niobium, beryllium, lead, yttrium, tin, zinc, manganese, and molybdenum in the magnetic and nonmagnetic fraction of heavy-mineral concentrates derived from stream sediment suggest that late stage, highly differentiated felsic rocks were involved in the eruptive history of the Mount Belknap caldera. Q-mode factor analysis was used to characterize the geochemical assemblages within the survey area, and the areal distribution of high-factor scores associated with mineralization indicates favorable target areas for future exploration. The results of these studies indicate that porphyry-type molybdenum and possible associated vein-type uranium mineralized deposits may exist in or near the Mount Belknap caldera.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82602","usgsCitation":"Tucker, R.E., Miller, W.R., and Motooka, J.M., 1982, A geochemical survey using heavy mineral concentrates in the Mount Belknap caldera vicinity, Utah: U.S. Geological Survey Open-File Report 82-602, iii, 136 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr82602.","productDescription":"iii, 136 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":146606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0602/report-thumb.jpg"},{"id":39352,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0602/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6ba","contributors":{"authors":[{"text":"Tucker, R. E.","contributorId":50520,"corporation":false,"usgs":true,"family":"Tucker","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":163213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":163214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Motooka, J. M.","contributorId":8834,"corporation":false,"usgs":true,"family":"Motooka","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":163212,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23792,"text":"ofr82862 - 1982 - A national water-use information program","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr82862","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":"82-862","title":"A national water-use information program","docAbstract":"The U.S. Geological Survey has compiled estimates of water use every five years since 1950. These estimates have been derived from many sources, and have a wide range of accuracy. Therefore, they fall short of providing a national data base that is both current and reliable. In 1977, the Congress of the United States recognized the need for uniform information on water use and directed the U.S. Geological Survey to establish a National Water-Use Information Program to complement the Survey's data on the availability and quality of the Nation's water resources. \r\n\r\nThe National Water-Use Information Program was designed as a cooperative program between the States and the Federal Government. The goals of the program are: to collect and compile water-use data; to develop and refine computerized water-use data systems at both the State and national levels; to devise new methods and techniques to improve the collection and analysis of water-use information; and to disseminate this information to those involved in establishing water-resources policy and to those managing the resources. \r\n\r\nThe program that started in 1978 in 20 States now includes participation by 47 States. Water-Use information is being compiled for 12 categories of use. Each State will have a automated data system that contains site-specific information about the water use in each category. The National Water-Use Data System will contain information for the 12 categories of use summarized by counties and river basins within each State. \r\n\r\nThe national system will aid in defining how much fresh and saline surface water and ground water is withdrawn and for what purpose, how much water is consumed during use, and how much water is returned to a water body (stream, lake, or aquifer) after use.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82862","issn":"0094-9140","usgsCitation":"Mann, W., Moore, J.E., and Chase, E.B., 1982, A national water-use information program: U.S. Geological Survey Open-File Report 82-862, 15 p. ill., 1 map ;28 cm., https://doi.org/10.3133/ofr82862.","productDescription":"15 p. ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":156846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0862/report-thumb.jpg"},{"id":53014,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0862/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a33d6","contributors":{"authors":[{"text":"Mann, William B.","contributorId":21985,"corporation":false,"usgs":true,"family":"Mann","given":"William B.","affiliations":[],"preferred":false,"id":190732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John E.","contributorId":33688,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190731,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":42855,"text":"ofr821127 - 1982 - Reconnaissance geologic map of the Tum Tum Lake Quadrangle, Harney County, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr821127","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":"82-1127","title":"Reconnaissance geologic map of the Tum Tum Lake Quadrangle, Harney County, Oregon","language":"ENGLISH","doi":"10.3133/ofr821127","usgsCitation":"Rytuba, J.J., Vander Meulen, D., Vercoutere, T., Minor, S., Caress, M., and Kriens, B., 1982, Reconnaissance geologic map of the Tum Tum Lake Quadrangle, Harney County, Oregon: U.S. Geological Survey Open-File Report 82-1127, 1 map ;58 x 43 cm., https://doi.org/10.3133/ofr821127.","productDescription":"1 map ;58 x 43 cm.","costCenters":[],"links":[{"id":108425,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13657.htm","linkFileType":{"id":5,"text":"html"},"description":"13657"},{"id":136484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80685,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1127/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641237","contributors":{"authors":[{"text":"Rytuba, James J. jrytuba@usgs.gov","contributorId":3043,"corporation":false,"usgs":true,"family":"Rytuba","given":"James","email":"jrytuba@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":227265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vander Meulen, D. B.","contributorId":30958,"corporation":false,"usgs":true,"family":"Vander Meulen","given":"D. B.","affiliations":[],"preferred":false,"id":227266,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vercoutere, T. L.","contributorId":102445,"corporation":false,"usgs":true,"family":"Vercoutere","given":"T. L.","affiliations":[],"preferred":false,"id":227269,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minor, S.A.","contributorId":65047,"corporation":false,"usgs":true,"family":"Minor","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":227267,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Caress, M.E.","contributorId":99104,"corporation":false,"usgs":true,"family":"Caress","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":227268,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kriens, B.J.","contributorId":104869,"corporation":false,"usgs":true,"family":"Kriens","given":"B.J.","affiliations":[],"preferred":false,"id":227270,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":9203,"text":"ofr82207 - 1982 - Geology and ore deposits of the Section 23 Mine, Ambrosia Lake District, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82207","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":"82-207","title":"Geology and ore deposits of the Section 23 Mine, Ambrosia Lake District, New Mexico","docAbstract":"The section 23 mine is one of about 18 large uranium mines opened in sandstones of the fluvial Westwater Canyon Member of the Jurassic Morrison Formation in the Ambrosia Lake mining district during the early 1960s. The Ambrosia Lake district is one of several mining districts within the Grants mineral belt, an elongate zone containing many uranium deposits along the southern flank of the San Juan basin. \r\n\r\nTwo distinct types of ore occur in the mine. Primary ore occurs as peneconcordant layers of uranium-rich authigenic organic matter that impregnates parts of the reduced sandstone host rocks and which are typically elongate in an east-southeast direction subparallel both to the sedimentary trends and to the present-day regional strike of the strata. These are called prefault or trend ores because of their early genesis and their elongation and alinement. \r\n\r\nA second type of ore in the mine is referred to as postfault, stacked, or redistributed ore. Its genesis was similar to that of the roll-type deposits in Tertiary rocks of Wyoming and Texas. Oxidation, related to the development of a large tongue of oxidized rock extending from Gallup to Ambrosia Lake, destroyed much of the primary ore and redistributed it as massive accumulations of lower grade ores bordering the redox interface at the edge of the tongue. Host rocks in the southern half of sec. 23 (T. 14 N., R. 10 W.) are oxidized and contain only remnants of the original, tabular, organic-rich ore. Thick bodies of roll-type ore are distributed along the leading edge of the oxidized zone, and pristine primary ore is found only near the north edge of the section.\r\n\r\nOrganic matter in the primary ore was derived from humic acids that precipitated in the pores of the sandstones and fixed uranium as both coffinite and urano-organic compounds. Vanadium, molybdenum, and selenium are also associated with the ore. The secondary or roll-type ores are essentially free of organic carbon and contain uranium both as coffinite and uraninite. They also contain vanadium and selenium but are virtually devoid of molybdenum. \r\n\r\nAlthough much has been learned about these deposits since the time this study was conducted, in 1966, a great deal more study will by required to completely elucidate their geologic history.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr82207","usgsCitation":"Granger, H., and Santos, E., 1982, Geology and ore deposits of the Section 23 Mine, Ambrosia Lake District, New Mexico: U.S. Geological Survey Open-File Report 82-207, 74 p. ill., maps ;29 cm., https://doi.org/10.3133/ofr82207.","productDescription":"74 p. ill., maps ;29 cm.","costCenters":[],"links":[{"id":141973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0207/report-thumb.jpg"},{"id":36812,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b30e4b07f02db6b409a","contributors":{"authors":[{"text":"Granger, H.C.","contributorId":15203,"corporation":false,"usgs":true,"family":"Granger","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":159279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Santos, E.S.","contributorId":95883,"corporation":false,"usgs":true,"family":"Santos","given":"E.S.","email":"","affiliations":[],"preferred":false,"id":159280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23559,"text":"ofr82913 - 1982 - A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr82913","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":"82-913","title":"A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama","docAbstract":"The report is a reference source on hydrologic information related to coal-mining activities in the Warrior and Plateau coal fields of Alabama. It contains a bibliography of more than 200 references and selected annotations. Also included is information on maps, automated-data bases, water-monitoring programs, and data-source agencies and organizations.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr82913","issn":"0094-9140","usgsCitation":"Kidd, R.E., and Hill, T.J., 1982, A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama: U.S. Geological Survey Open-File Report 82-913, iv, 63 p. 1 map ;28 cm., https://doi.org/10.3133/ofr82913.","productDescription":"iv, 63 p. 1 map ;28 cm.","costCenters":[],"links":[{"id":156551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0913/report-thumb.jpg"},{"id":52852,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0913/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5fad","contributors":{"authors":[{"text":"Kidd, Robert E.","contributorId":21523,"corporation":false,"usgs":true,"family":"Kidd","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, Thomas J.","contributorId":13270,"corporation":false,"usgs":true,"family":"Hill","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":190316,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":45885,"text":"ofr82463 - 1982 - Oblique map of Loihi Seamount and Papa'u Landslide, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr82463","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":"82-463","title":"Oblique map of Loihi Seamount and Papa'u Landslide, Hawaii","language":"ENGLISH","doi":"10.3133/ofr82463","usgsCitation":"Alpha, T.R., Morley, J.M., Gutmacher, C., and Austin, W., 1982, Oblique map of Loihi Seamount and Papa'u Landslide, Hawaii: U.S. Geological Survey Open-File Report 82-463, 1 map ;56 x 66 cm., https://doi.org/10.3133/ofr82463.","productDescription":"1 map ;56 x 66 cm.","costCenters":[],"links":[{"id":135920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20577,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0463/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6965b2","contributors":{"authors":[{"text":"Alpha, Tau Rho","contributorId":63371,"corporation":false,"usgs":true,"family":"Alpha","given":"Tau","email":"","middleInitial":"Rho","affiliations":[],"preferred":false,"id":232227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morley, J. M.","contributorId":77505,"corporation":false,"usgs":true,"family":"Morley","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":232228,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gutmacher, C. E.","contributorId":45284,"corporation":false,"usgs":true,"family":"Gutmacher","given":"C. E.","affiliations":[],"preferred":false,"id":232226,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Austin, W.A.","contributorId":17590,"corporation":false,"usgs":true,"family":"Austin","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":232225,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":11537,"text":"ofr811055 - 1982 - Drainage areas of New York streams, by river basins; a stream gazetteer; Part 1, Data compiled as of October 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr811055","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":"81-1055","title":"Drainage areas of New York streams, by river basins; a stream gazetteer; Part 1, Data compiled as of October 1980","docAbstract":"Hydrologic studies concerned with surface water require geographic data of several types, among which are stream length and size of drainage area from which runoff is contributed. This gazetteer presents all drainage-area data on New York streams that were available as of October 1980. The information is grouped by river basin, and each section consists of two lists. The first gives sites alphabetically by stream name and includes the body of water to which the stream is tributary, county in which the site is located, drainage area above the mouth, coordinates of the topographic quadrangle on the State index map , and the Geological Survey site number. The second list presents site information by U.S. Geological Survey site number (downstream order along the main stream) and includes drainage area, distance of measurement site above the mouth, and location by latitude and longitude. Data were compiled from published and unpublished sources, all of which are available for inspection at the U.S. Geological Survey in Albany, N.Y. Also included are updated values on several river basins that have been redelineated and whose drainage areas have been recomputed and retabulated since 1977. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811055","usgsCitation":"Wagner, L., 1982, Drainage areas of New York streams, by river basins; a stream gazetteer; Part 1, Data compiled as of October 1980: U.S. Geological Survey Open-File Report 81-1055, 365 p., 1 over-size sheet, maps (1 col.) ;28 cm., https://doi.org/10.3133/ofr811055.","productDescription":"365 p., 1 over-size sheet, maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":144574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1055/report-thumb.jpg"},{"id":39399,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1055/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633c77","contributors":{"authors":[{"text":"Wagner, L.A.","contributorId":12427,"corporation":false,"usgs":true,"family":"Wagner","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":163323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11766,"text":"ofr82312 - 1982 - Contract report on a remote-reference magnetotelluric survey in the southern Appalachian overthrust belt, North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr82312","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":"82-312","title":"Contract report on a remote-reference magnetotelluric survey in the southern Appalachian overthrust belt, North Carolina","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82312","usgsCitation":"Argonaut Enterprises, W.A., 1982, Contract report on a remote-reference magnetotelluric survey in the southern Appalachian overthrust belt, North Carolina: U.S. Geological Survey Open-File Report 82-312, 165 p., 1 over-size sheet, ill., maps ;28 cm., https://doi.org/10.3133/ofr82312.","productDescription":"165 p., 1 over-size sheet, ill., maps ;28 cm.","costCenters":[],"links":[{"id":144475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0312/report-thumb.jpg"},{"id":39644,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0312/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39645,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6984a8","contributors":{"authors":[{"text":"Argonaut Enterprises, with an introduction by Wynn J. C. J. C.","contributorId":14416,"corporation":false,"usgs":true,"family":"Argonaut Enterprises","given":"with","suffix":"J. C.","email":"","middleInitial":"an introduction by Wynn J. C.","affiliations":[],"preferred":false,"id":163699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}