Observations of the semidiurnal (M2) tidal current, bottom pressure, and coastal sea level from Nova Scotia to Cape May, New Jersey) show that: 1) the surface pressure at the edge of the Continental Shelf in the study area has a relatively uniform amplitude (40 cm) and phase (12 hr Greenwich); 2) in the Mid-Atlantic Bight, the semidiurnal M2 tide is co-oscillating, and the onshore M2 tidal current reaches a maximum 2 approximately 90° or 3.1 hr before high water; 3) in the Georges Bank region of the shelf, the M tide is more progressive than it is in the 2 Mid-Atlantic Bight, and the onshore M2 tidal current in the Georges Bank 2 region of the shelf reaches a maximum about 7 ° or 14 min before high water; 4) the strongest M2 tidal currents observed in the study area are 2 near the crest of Georges Bank (typical amplitudes are 74 cm/s near the surface); 5) the M2 tidal currents are weaker in the Mid-Atlantic Bight 2 (typical amplitudes are 16 cm/s near the surface) than on Georges Bank; and 6) the tidal currents are weakest near the bottom south of Cape Cod in a region of transition between progressive and co-oscillating tides.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801137","collaboration":"Prepared in cooperation with the Bureau of Land Management","usgsCitation":"Moody, J.A., and Butman, B., 1980, Semidiurnal bottom pressure and tidal currents on Georges Bank and in the Mid-Atlantic Bight: U.S. Geological Survey Open-File Report 80-1137, 22 p., https://doi.org/10.3133/ofr801137.","productDescription":"22 p.","costCenters":[],"links":[{"id":413966,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1137/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142337,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1137/report-thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Georges Bank, Mid-Atlantic Bight","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.59456951669301,\n 41.83978923652438\n ],\n [\n -64.81830245678367,\n 41.83978923652438\n ],\n [\n -64.81830245678367,\n 45.351632868480095\n ],\n [\n -70.59456951669301,\n 45.351632868480095\n ],\n [\n -70.59456951669301,\n 41.83978923652438\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7a2e","contributors":{"authors":[{"text":"Moody, John A. 0000-0003-2609-364X jamoody@usgs.gov","orcid":"https://orcid.org/0000-0003-2609-364X","contributorId":771,"corporation":false,"usgs":true,"family":"Moody","given":"John","email":"jamoody@usgs.gov","middleInitial":"A.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":161297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":161298,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10604,"text":"ofr801164 - 1980 - Lithology and lithium content of sediments drilled in a test hole on Alkali Flat (Franklin Lake), Inyo County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr801164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1164","title":"Lithology and lithium content of sediments drilled in a test hole on Alkali Flat (Franklin Lake), Inyo County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801164","usgsCitation":"Pantea, M.P., 1980, Lithology and lithium content of sediments drilled in a test hole on Alkali Flat (Franklin Lake), Inyo County, California: U.S. Geological Survey Open-File Report 80-1164, 21 p. ill., map ;28 cm., https://doi.org/10.3133/ofr801164.","productDescription":"21 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":143049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1164/report-thumb.jpg"},{"id":38442,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635c73","contributors":{"authors":[{"text":"Pantea, Michael P. mpantea@usgs.gov","contributorId":1549,"corporation":false,"usgs":true,"family":"Pantea","given":"Michael","email":"mpantea@usgs.gov","middleInitial":"P.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":161665,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10688,"text":"ofr8073 - 1980 - A one-dimensional, steady-state, dissolved-oxygen model and waste-load assimilation study for Little Lick and Big Lick Creeks, Blackford and Delaware counties, Indiana","interactions":[],"lastModifiedDate":"2022-04-06T17:48:51.326652","indexId":"ofr8073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-73","title":"A one-dimensional, steady-state, dissolved-oxygen model and waste-load assimilation study for Little Lick and Big Lick Creeks, Blackford and Delaware counties, Indiana","docAbstract":"The Indiana State Board of Health is developing a State water-quality management plan that includes establishing limits for liquid wastes discharged into Indiana streams. A digital computer model was used to predict alternatives for future waste loadings on Little Lick and Big Lick Creeks that would be compatible with Indiana stream water-quality standards defined for two critical hydrologic conditions, summer and winter low flows.
The model parameters included atmospheric reaeration, carbonaceous and nitrogenous biochemical-oxygen demand, and benthic-oxygen demand. The model was calibrated with data collected during three water-quality surveys at low flow. Verification of the model was not possible owing to varied effluent discharge during sampling. During these surveys, in-stream dissolved-oxygen concentration averaged less than 3 milligrams per liter, well below the State minimum requirement of 5.0 milligrams per liter. The model indicated that these low concentrations were caused by high waste loadings, lack of dilution, low reaeration, and benthic-oxygen demand.
The hypothetical summer waste-assimilation study assumed that future reductions in discharge Loadings would decrease carbonaceous and benthic decay and increase nitrogenous decay. This hypothetical study indicated that projected effluent waste loads that would provide acceptable in-stream dis-solved-oxygen concentrations are highly dependent on rates of nitrification. Ammonia toxicity became the limiting water-quality criterion at low nitrification rates.
The hypothetical winter waste-assimilation study indicated that projected dissolved-oxygen concentrations in Little Lick and Big Lick Creeks did not fall below the State standard. Owing to a lack of dilution, however, ammonia-nitrogen concentrations would violate in-stream toxicity standards in both Little Lick and Big Lick Creeks. In order to quantify the results of the waste-assimilation study, it would be necessary to collect additional stream data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8073","collaboration":"Prepared in cooperation with the Indiana State Board of Health","usgsCitation":"Peters, J.G., Crawford, C.G., and Wilber, W.G., 1980, A one-dimensional, steady-state, dissolved-oxygen model and waste-load assimilation study for Little Lick and Big Lick Creeks, Blackford and Delaware counties, Indiana: U.S. Geological Survey Open-File Report 80-73, ix, 102 p., https://doi.org/10.3133/ofr8073.","productDescription":"ix, 102 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":144253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0073/report-thumb.jpg"},{"id":398235,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Blackford County, Delaware County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.4453,40.567],[-85.3327,40.5674],[-85.2208,40.5677],[-85.2008,40.5679],[-85.2012,40.4804],[-85.2066,40.4804],[-85.2073,40.3789],[-85.2091,40.3793],[-85.2205,40.379],[-85.2182,40.3073],[-85.2168,40.2198],[-85.2165,40.135],[-85.2157,40.0765],[-85.5763,40.0769],[-85.5784,40.3794],[-85.4451,40.3792],[-85.4448,40.3933],[-85.4454,40.4799],[-85.4453,40.567]]]},\"properties\":{\"name\":\"Blackford\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ab901","contributors":{"authors":[{"text":"Peters, James G.","contributorId":69137,"corporation":false,"usgs":true,"family":"Peters","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":161803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":161802,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilber, William G. wgwilber@usgs.gov","contributorId":297,"corporation":false,"usgs":true,"family":"Wilber","given":"William","email":"wgwilber@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":161801,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28521,"text":"wri8057 - 1980 - Use of geophysical logs to estimate water-quality trends in carbonate aquifers","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri8057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-57","title":"Use of geophysical logs to estimate water-quality trends in carbonate aquifers","docAbstract":"The water quality in carbonate aquifers can be determined by analysis of resistivity and porosity logs. When supporting data from water analyses are available, the value of the cementation exponent m can be determined more precisely. Data for this study were taken from logs of oil-test wells, Amstrat sample studies, drill-stem tests and water test wells in parts of Montana, North and South Dakota, and Wyoming. The preferred resistivity curves for apparent water resistivity (Rwa) analyses are the deeply focused laterolog and the induction log. The standard electric log can be used if the drilling mud is not saturated with salt. The preferred porosity logs are the sonic, sidewall neutron, compensated neutron, and the density logs. Older, uncalibrated neutron curves can be empirically calibrated in some instances, however, resulting porosities are frequently anomalous when compared to those determined from core or modern logs. When apparent water resistivity is determined for many wells, the data can be plotted and contoured to outline areas of recharge, direction of probable ground-water movement, and location and salinity of brine areas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8057","usgsCitation":"MacCary, L.M., 1980, Use of geophysical logs to estimate water-quality trends in carbonate aquifers: U.S. Geological Survey Water-Resources Investigations Report 80-57, iv, 23 p. :ill., map ;26 cm., https://doi.org/10.3133/wri8057.","productDescription":"iv, 23 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":159339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0057/report-thumb.jpg"},{"id":57320,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df7f4","contributors":{"authors":[{"text":"MacCary, Lawrence Mead","contributorId":67131,"corporation":false,"usgs":true,"family":"MacCary","given":"Lawrence","email":"","middleInitial":"Mead","affiliations":[],"preferred":false,"id":199956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10294,"text":"ofr80853 - 1980 - Competition and performance in OCS oil and gas lease sales and lease development, 1954-1969","interactions":[],"lastModifiedDate":"2017-03-27T14:15:17","indexId":"ofr80853","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-853","title":"Competition and performance in OCS oil and gas lease sales and lease development, 1954-1969","docAbstract":"The oil and gas resources of the Outer Continental Shelf represent one of America's largest publicly-owned assets. Through 1978, OCS oil and gas leases had yielded \\$40.5 billion in gross production value and produced over \\$28.3 billion in direct revenue to the federal government.
Policies and procedures for managing the oil and gas resources of the OCS were established by Congress in the Outer Continental Shelf Lands Act of 1953. The Department of Interior was given the central responsibility for carrying out this management role in the 1953 Act; this responsibility has been re-established in the 1978 Amendments to the OCS Lands Act. As stated in the 1978 legislation, the goals of OCS management are to:
...preserve, protect and develop oil and natural gas resources in a manner which is consistent with the need (A) to make such resources available to meet the Nation's energy needs as rapidly as possible... (C) to insure the public a fair and equitable return on the resources of the Outer Continental Shelf, and (D) to preserve and maintain free enterprise competition.
As part of its continuing effort to monitor the effectiveness of federal policies relating to OCS oil and gas resources, the Conservation Division of U.S. Geological Survey, Department of Interior, has sponsored the research which is the basis for the present report. The objectives of the research have been to determine the extent to which the historical policies of OCS management have resulted in achievement of the goals set forth by Congress in the section quoted above.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80853","usgsCitation":"Mead, W.J., and Sorensen, P.E., 1980, Competition and performance in OCS oil and gas lease sales and lease development, 1954-1969: U.S. Geological Survey Open-File Report 80-853, ix, 179 p., https://doi.org/10.3133/ofr80853.","productDescription":"ix, 179 p.","costCenters":[],"links":[{"id":144083,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0853/report-thumb.jpg"},{"id":338394,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0853/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa321","contributors":{"authors":[{"text":"Mead, Walter J.","contributorId":36564,"corporation":false,"usgs":true,"family":"Mead","given":"Walter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorensen, Philip Edward","contributorId":103686,"corporation":false,"usgs":true,"family":"Sorensen","given":"Philip","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":161152,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10349,"text":"ofr802021 - 1980 - Thermal infrared aircraft scanner data of the area of underground coal fires, Sheridan, Wyoming, July 1975 and October 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr802021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-2021","title":"Thermal infrared aircraft scanner data of the area of underground coal fires, Sheridan, Wyoming, July 1975 and October 1978","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr802021","usgsCitation":"Miller, S., and Watson, K., 1980, Thermal infrared aircraft scanner data of the area of underground coal fires, Sheridan, Wyoming, July 1975 and October 1978: U.S. Geological Survey Open-File Report 80-2021, 5 p. ill. ;28 cm., https://doi.org/10.3133/ofr802021.","productDescription":"5 p. ill. ;28 cm.","costCenters":[],"links":[{"id":143547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2021/report-thumb.jpg"},{"id":38198,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e0e8","contributors":{"authors":[{"text":"Miller, S.H.","contributorId":8857,"corporation":false,"usgs":true,"family":"Miller","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":161234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watson, Kenneth","contributorId":91109,"corporation":false,"usgs":true,"family":"Watson","given":"Kenneth","email":"","affiliations":[],"preferred":false,"id":161235,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10298,"text":"ofr8171 - 1980 - Preliminary delineation of salty ground water in the northern Atlantic Coastal Plain","interactions":[{"subject":{"id":10298,"text":"ofr8171 - 1980 - Preliminary delineation of salty ground water in the northern Atlantic Coastal Plain","indexId":"ofr8171","publicationYear":"1980","noYear":false,"title":"Preliminary delineation of salty ground water in the northern Atlantic Coastal Plain"},"predicate":"SUPERSEDED_BY","object":{"id":38437,"text":"pp1404D - 1989 - The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain","indexId":"pp1404D","publicationYear":"1989","noYear":false,"chapter":"D","title":"The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain"},"id":1}],"supersededBy":{"id":38437,"text":"pp1404D - 1989 - The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain","indexId":"pp1404D","publicationYear":"1989","noYear":false,"title":"The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain"},"lastModifiedDate":"2025-04-17T18:03:25.706033","indexId":"ofr8171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-71","title":"Preliminary delineation of salty ground water in the northern Atlantic Coastal Plain","docAbstract":"Salty ground water underlies freshwater in the eastern part of the northern Atlantic Coastal Plain. The transition zone between freshwater and saltwater is represented in this report by a series of maps showing the depths to chloride concentrations of 250, 1,000, 10,000, and 18,000 milligrams per liter. The maps are based on chloride concentrations obtained from self-potential logs as well as from water-quality analyses.
Depths to the designated chloride concentrations generally increase inland from the coast except in New Jersey where they are greatest along the coast and in North Carolina where depths to the 10,000 and 18,000 milligrams per liter concentrations are greatest beneath Pamlico Sound. The transition zone between 250 and 18,000 milligrams per liter of chloride is generally 1,500 to 2,300 feet thick except in part of North Carolina, where it is less than 1,000 feet.
Depths to 250 and 1,000 milligrams per liter of chloride are probably controlled by the natural flow pattern of fresh ground water. Areas where these concentrations are relatively shallow generally coincide with areas of natural ground-water discharge. Depths to 10,000 and 18,000 milligrams per liter of chloride, and the occurrence offshore of ground water that is fresher than seawater, is attributed to long-term hydrologic conditions during which sea level fluctuations of a few hundred feet recurred several times. The origin of ground water that is saltier than seawater is attributed to the leaching of evaporitic strata beneath the Continental Shelf and Slope followed by westward movement of the brines during periods of sea-level rise.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8171","usgsCitation":"Meisler, H., 1980, Preliminary delineation of salty ground water in the northern Atlantic Coastal Plain: U.S. Geological Survey Open-File Report 81-71, Report: 41 p.; 4 Figures: 50.22 x 22.92 inches or smaller, https://doi.org/10.3133/ofr8171.","productDescription":"Report: 41 p.; 4 Figures: 50.22 x 22.92 inches or smaller","costCenters":[],"links":[{"id":484706,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1981/0071/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":484705,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1981/0071/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":484704,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1981/0071/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":484703,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1981/0071/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":484702,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144076,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0071/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Northern Atlantic Coastal Plain","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47e4e4b07f02db4bb3fb","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":161159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10348,"text":"ofr80469 - 1980 - Ground support data from July 10 to July 29, 1978, for HCMM thermal satellite data of the Powder River Basin, Wyoming","interactions":[],"lastModifiedDate":"2022-08-01T21:34:39.649417","indexId":"ofr80469","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-469","title":"Ground support data from July 10 to July 29, 1978, for HCMM thermal satellite data of the Powder River Basin, Wyoming","docAbstract":"Radiometric and meteorological data were acquired at three ground stations located approximately 150 km apart in the Powder River Basin, Wyoming. These data were collected from July. 10 through July 29, 1978, to support the HCMM (Heat Capacity Mapping Mission) thermal satellite data acquired during this same time period. The parameters measured are direct solar radiance, total solar radiance, sky radiance, air temperature, relative humidity, wind speed, and wind direction
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- Chemical and physical characteristics of precipitation at selected sites in Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"wri8081","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-81","title":"Chemical and physical characteristics of precipitation at selected sites in Florida","docAbstract":"Infrequent sampling of precipitation in Florida has been conducted by the U.S. Geological Survey since 1965. A summary of the historical data from 24 sites throughout Florida indicate that the principal ionic composition of atmospheric precipitation samples is calcium-sodium and bicarbonate-chloride with an average specific conductance of 32 micromhos per centimeter at 25 C. Historically, much of the sampling focused on primary nutrients and selected trace elements. Historical data indicate that nitrogen and phosphorus concentrations averaged 1.1 and 0.1 milligrams per liter, respectively. The limited trace metal data indicate that motor-vehicle activity may have a significant impact on local precipitation quality. Lead, for example, was measured in concentrations of as much as 2,400 micrograms per liter in samples collected in a highly populated, commerical area in south Florida. Statistical testing indicated that most major inorganic constituents, primary nutrients, and trace metals were significantly differnet among the sampling sites. The pH data indicated a range of about 5.0 to 7.0, but only limited pH data were collected and analyzed at the historical sites in such a timely manner as to represent pH conditions of the atmospheric precipitation during active rainfall. A critical review of the historical data suggested that while they may reflect local atmospheric quality conditions they likely do not define baseline conditions from a regional perspective. The application of these data were generally limited regarding regional extrapolation due to lack of standardization of sampling techniques, variable methods of sample preservation, nonuniform sampling intervals, variable sample sizes, and different periods of record. (USGS)","language":"ENGLISH","doi":"10.3133/wri8081","usgsCitation":"Irwin, G.A., and Kirkland, R., 1980, Chemical and physical characteristics of precipitation at selected sites in Florida: U.S. Geological Survey Water-Resources Investigations Report 80-81, 70 p., https://doi.org/10.3133/wri8081.","productDescription":"70 p.","costCenters":[],"links":[{"id":125168,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0081/report-thumb.jpg"},{"id":84560,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0081/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e47b9","contributors":{"authors":[{"text":"Irwin, G. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1261","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Controlled photomosaic of the Tharsis Southwest quadrangle of Mars: U.S. Geological Survey IMAP 1261, 26.38 x 34.63 inches, https://doi.org/10.3133/i1261.","productDescription":"26.38 x 34.63 inches","costCenters":[],"links":[{"id":360514,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1261/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":191745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":" https://pubs.usgs.gov/imap/1261/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881b8","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68844,"text":"oc91 - 1980 - Petrography, x-ray mineralogy, and palynology of a measured section of the Upper Cretaceous Mesaverde Group in Hunter Canyon, western Colorado","interactions":[],"lastModifiedDate":"2018-02-15T15:11:51","indexId":"oc91","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91","title":"Petrography, x-ray mineralogy, and palynology of a measured section of the Upper Cretaceous Mesaverde Group in Hunter Canyon, western Colorado","language":"ENGLISH","doi":"10.3133/oc91","isbn":"0607823933","usgsCitation":"Johnson, R.C., May, F., Hansley, P., Pitman, J.K., and Fouch, T.D., 1980, Petrography, x-ray mineralogy, and palynology of a measured section of the Upper Cretaceous Mesaverde Group in Hunter Canyon, western Colorado: U.S. Geological Survey Oil and Gas Investigation Chart 91, 1 geologic section ;on sheet 102 x 120 cm., https://doi.org/10.3133/oc91.","productDescription":"1 geologic section ;on sheet 102 x 120 cm.","costCenters":[],"links":[{"id":104872,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5242.htm","linkFileType":{"id":5,"text":"html"},"description":"5242"},{"id":191435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.58333333333333,39.284166666666664 ], [ -108.58333333333333,39.3175 ], [ -108.53416666666666,39.3175 ], [ -108.53416666666666,39.284166666666664 ], [ -108.58333333333333,39.284166666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687f4e","contributors":{"authors":[{"text":"Johnson, Ronald C. 0000-0002-6197-5165 rcjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-6197-5165","contributorId":1550,"corporation":false,"usgs":true,"family":"Johnson","given":"Ronald","email":"rcjohnson@usgs.gov","middleInitial":"C.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":279060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, Fred","contributorId":94918,"corporation":false,"usgs":true,"family":"May","given":"Fred","affiliations":[],"preferred":false,"id":279064,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hansley, P. L.","contributorId":82299,"corporation":false,"usgs":true,"family":"Hansley","given":"P. L.","affiliations":[],"preferred":false,"id":279062,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":279063,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fouch, T. 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This report contains records of water discharge at 56' gaging stations; stage only at 1 gaging station; tidal volume at 1 gaging station; stage only records at 2 tidal-gaging stations; contents at 36 lakes and reservoirs; water quality at 50 gaging stations, 5 lakes and reservoirs, 2 harbors; 34 wells, and 1 spring; and water levels at 66 observation wells. Also included are data for 41 creststage partial-record stations. Locations of these sites are shown on figures 2, 3, and 4. Additional water data were collected at various sites, not involved in the systematic data-collection program, and are published as miscellaneous measurements and analysis. A few pertinent stations (not included above) in bordering States are also enclosed in this report. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Connecticut.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrCT791","collaboration":"Prepared in cooperation with the State of Connecticut and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Connecticut, water year 1979: U.S. Geological Survey Water Data Report CT-79-1, x, 366 p., https://doi.org/10.3133/wdrCT791.","productDescription":"x, 366 p.","costCenters":[],"links":[{"id":412759,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1979/ct-79-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174015,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1979/ct-79-1/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4cfb","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532294,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24625,"text":"ofr80552 - 1980 - Index of streamflow and water quality records to September 30, 1978, Yukon Basin, Alaska","interactions":[],"lastModifiedDate":"2019-04-29T12:58:51","indexId":"ofr80552","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-552","title":"Index of streamflow and water quality records to September 30, 1978, Yukon Basin, Alaska","docAbstract":"This report, which is one of a series of reports for Alaska, lists stations in Yukon Basin, Alaska, at which streamflow and water quality data have been collected by the U.S. Geological Survey. Included are a hydrologic subregion map of Yukon Basin, Alaska, and a table listing the types of data collected and periods of record. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80552","issn":"0094-9140","usgsCitation":"Still, P.J., 1980, Index of streamflow and water quality records to September 30, 1978, Yukon Basin, Alaska: U.S. Geological Survey Open-File Report 80-552, i, 41 p., https://doi.org/10.3133/ofr80552.","productDescription":"i, 41 p.","costCenters":[],"links":[{"id":157870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0552/report-thumb.jpg"},{"id":111908,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/11300","linkFileType":{"id":5,"text":"html"}},{"id":363310,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0552/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614479","contributors":{"authors":[{"text":"Still, Patsy J.","contributorId":27077,"corporation":false,"usgs":true,"family":"Still","given":"Patsy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":192276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24510,"text":"ofr80914 - 1980 - The microzonation of the Memphis, Tennessee area","interactions":[],"lastModifiedDate":"2022-07-18T16:31:47.09312","indexId":"ofr80914","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-914","title":"The microzonation of the Memphis, Tennessee area","docAbstract":"Although the probability of a major earthquake in the central U.S. is only one-tenth of the Californian events, any such event is expected to result in damage ten times greater than that anticipated in California. The city of Memphis, which is situated very close to the inferred epicenter of one of the three major 1811-1812 earthquakes, is in a potentially hazardous zone which will be susceptible to the usual seismic hazards. By recognizing the high level of seismicity in the New Madrid area, this study attempts to microzone the potential hazards in the city of Memphis.
This study examines the pertinent criteria necessary for any microzonation study. The subjects considered include:
(i) The seismicity of the central United States,
(ii) Design earthquakes,
(iii) Response analysis which allows us to construct the necessary microzonation maps.
The seismicity of the region is evaluated according to the state-of-the-art literature available as there is no recorded strong motion data available for the central U.S. The maximum credible earthquakes which are likely to affect Memphis are evaluated as the one in a thousand year occurrence. However, earthquakes of a lower intensity (and lower recurrence rates) are selected as design earthquakes to permit a more realistic microzonation to be performed.
For the response analysis, these earthquakes are simulated using synthetically generated accelerograms which exhibit the relevant parameters. These accelerograms displaying the significant characteristics of amplitude, predominant frequency and duration were selected to display, as accurately as possible, the anticipated nature of the horizontal bedrock-motions at Memphis. The horizontal motions (SH-waves) were applied at a depth of 45m below ground surface at numerous sites in the city of Memphis, where the soil stratigraphy had been conceptualized from borehole data.
The soils data made available by local sources was the only information used for this study as any laboratory testing was outside the scope of this study. The dynamic soil properties were thus established from the available Standard Penetration Resistances and soil classifications.
The results of the response analysis were transformed into microzonation maps depicting
(i) zones showing qualitative estimates of ground response,
(ii) zones showing the natural frequency of the soils,
(iii) zones showing the peak spectral acceleration for 2% damping ratio,
(iv) zones of liquefaction potential.
These maps are essentially useful for preliminary investigation and we do not expect them to be used on a quantitative basis. However, further investigation is necessary in determining the stratigraphy and soil properties to a more accurate level if an earthquake hazard is anticipated.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80914","usgsCitation":"Sharma, S., and Kovacs, W.D., 1980, The microzonation of the Memphis, Tennessee area: U.S. Geological Survey Open-File Report 80-914, vi, 129 p., https://doi.org/10.3133/ofr80914.","productDescription":"vi, 129 p.","costCenters":[],"links":[{"id":403923,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0914/report.pdf"},{"id":156554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0914/report-thumb.jpg"}],"country":"United States","state":"Tennessee","city":"Memphis area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.076904296875,\n 35.074964853989556\n ],\n [\n -89.85992431640625,\n 35.074964853989556\n ],\n [\n -89.85992431640625,\n 35.22318504970181\n ],\n [\n -90.076904296875,\n 35.22318504970181\n ],\n [\n -90.076904296875,\n 35.074964853989556\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a28f","contributors":{"authors":[{"text":"Sharma, Sunil","contributorId":81522,"corporation":false,"usgs":true,"family":"Sharma","given":"Sunil","email":"","affiliations":[],"preferred":false,"id":192053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kovacs, William D.","contributorId":95096,"corporation":false,"usgs":true,"family":"Kovacs","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":192054,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36356,"text":"fdl60 - 1980 - Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum","interactions":[{"subject":{"id":36356,"text":"fdl60 - 1980 - Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum","indexId":"fdl60","publicationYear":"1980","noYear":false,"title":"Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum"},"predicate":"SUPERSEDED_BY","object":{"id":2001381,"text":"2001381 - 1988 - Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum","indexId":"2001381","publicationYear":"1988","noYear":false,"title":"Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum"},"id":1}],"supersededBy":{"id":2001381,"text":"2001381 - 1988 - Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum","indexId":"2001381","publicationYear":"1988","noYear":false,"title":"Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum"},"lastModifiedDate":"2013-07-10T14:47:43","indexId":"fdl60","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":22,"text":"Fish Disease Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"60","title":"Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Bullock, G.L., 1980, Bacterial kidney disease of salmonid fishes caused by Renibacterium salmoninarum (Supersedes Fish Disease Leaflet 41, 1975; Superceded by Fish Disease Leaflet 78, 1988): Fish Disease Leaflet 60, 10 p.","productDescription":"10 p.","costCenters":[],"links":[{"id":166955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fdl60.PNG"},{"id":274835,"type":{"id":11,"text":"Document"},"url":"https://babel.hathitrust.org/cgi/pt?id=coo.31924000778476;view=1up;seq=199"}],"edition":"Supersedes Fish Disease Leaflet 41, 1975; Superceded by Fish Disease Leaflet 78, 1988","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ac8e","contributors":{"authors":[{"text":"Bullock, Graham L.","contributorId":9323,"corporation":false,"usgs":true,"family":"Bullock","given":"Graham","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":216191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24687,"text":"ofr80845 - 1980 - Utah computerized resource information file; CRIB-UTAH","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"ofr80845","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-845","title":"Utah computerized resource information file; 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The 1977 daily use was 14,812 million gallons of saline water and 6,654 million gallons of freshwater. Most of the saline water, largely surface water, was pumped from tidal estuaries. Only 107.6 million gallons per day of saline water--less than 1 percent--was obtained from wells. Thermoelectric power generation used virtually all the saline water, 14,738 million gallons per day, whereas all other industrial uses were only 73 million gallons of saline water per day. The freshwater supply was almost equally divided between ground water (53 percent) and surface water (47 percent). Of the total freshwater used, 43 percent was for irrigation--an average of 2,873 million gallons of freshwater daily on the average. The remaining daily use of freshwater was 21 percent for thermoelectric power generation, 19 percent for public supply; 14 percent for industrial use other than thermoelectric power generation; and 3 percent for domestic and rural use. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc61","contributors":{"authors":[{"text":"Leach, Stanley D.","contributorId":101670,"corporation":false,"usgs":true,"family":"Leach","given":"Stanley","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":199526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, Henry G.","contributorId":89916,"corporation":false,"usgs":true,"family":"Healy","given":"Henry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":199525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24511,"text":"ofr801057 - 1980 - Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado","interactions":[{"subject":{"id":24511,"text":"ofr801057 - 1980 - Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado","indexId":"ofr801057","publicationYear":"1980","noYear":false,"title":"Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":60855,"text":"mf1483A - 1983 - Mineral resource potential and geologic map of the Powderhorn Wilderness study area and Cannibal Plateau Roadless Area, Gunnison and Hinsdale counties, Colorado","indexId":"mf1483A","publicationYear":"1983","noYear":false,"chapter":"A","title":"Mineral resource potential and geologic map of the Powderhorn Wilderness study area and Cannibal Plateau Roadless Area, Gunnison and Hinsdale counties, Colorado"},"id":1}],"supersededBy":{"id":60855,"text":"mf1483A - 1983 - Mineral resource potential and geologic map of the Powderhorn Wilderness study area and Cannibal Plateau Roadless Area, Gunnison and Hinsdale counties, Colorado","indexId":"mf1483A","publicationYear":"1983","noYear":false,"title":"Mineral resource potential and geologic map of the Powderhorn Wilderness study area and Cannibal Plateau Roadless Area, Gunnison and Hinsdale counties, Colorado"},"lastModifiedDate":"2023-06-05T19:52:40.220456","indexId":"ofr801057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1057","title":"Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado","docAbstract":"The Powderhorn Instant Study Area covers approximately 51,000 acres of land under BLM administration located about 80 km (50 mi) southwest of Gunnison, Colorado. A mineral resource survey, made in 1979 by the U.S. Geological Survey and the U.S. Bureau of Mines, indicates that both the mineral potential and the energy potential for the Powderhorn Instant Study Area are low. This report is based on geologic and geochemical investigations, examination of prospects, and an aeromagnetic survey. Spectrographic analyses were made of approximately 120 stream-sediment and rock samples. No mining districts are located within the study area.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801057","issn":"0094-9140","usgsCitation":"Sharp, W.N., Martin, R., and Lane, M., 1980, Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado: U.S. Geological Survey Open-File Report 80-1057, Report: ii, 4 p.; 3 Plates: 35.83 x 51.26 inches or smaller, https://doi.org/10.3133/ofr801057.","productDescription":"Report: ii, 4 p.; 3 Plates: 35.83 x 51.26 inches or smaller","costCenters":[],"links":[{"id":417771,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1057/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417770,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1057/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417769,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1057/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417768,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1057/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156570,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1057/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Gunnison County, Hinsdale County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.3,37.916666666666664 ], [ -107.3,38.333333333333336 ], [ -107,38.333333333333336 ], [ -107,37.916666666666664 ], [ -107.3,37.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c7ef","contributors":{"authors":[{"text":"Sharp, William N.","contributorId":18751,"corporation":false,"usgs":true,"family":"Sharp","given":"William","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":192055,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":874635,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, Michael","contributorId":39756,"corporation":false,"usgs":true,"family":"Lane","given":"Michael","affiliations":[],"preferred":false,"id":192056,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10728,"text":"ofr801265 - 1980 - Single-channel seismic-reflection profiles collected on the northern Blake Plateau, 29 September to 19 October 1978","interactions":[],"lastModifiedDate":"2018-06-18T15:12:53","indexId":"ofr801265","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1265","title":"Single-channel seismic-reflection profiles collected on the northern Blake Plateau, 29 September to 19 October 1978","docAbstract":"During 29 September to 19 October 1978, the U.S. Geological Survey (USGS ) collected 3,570 km of single-channel airgun, 3,487 km of minisparker, and 3,565 km of 3.5-kHz echo-sounder seismic-reflection profiles from the Research Vessel COLUMBUS ISELIN in the area of the northern Blake Plateau. These data were acquired in cooperation with the U.S. Bureau of Land Management (BLM) as part of a study to determine potential geologic hazards or limitations to petroleum exploration or development on the northern Blake Plateau area. Fourteen lines were acquired perpendicular to the margin and were spaced about 25 km apart; two converging tie lines parallel the margin. The seismic-reflection profiles were placed to intersect similar seismic lines acquired in 1976 to 1977 on the Florida-Hatteras Shelf and inner Blake Plateau and to be tied to the offshore drill holes JOIDES 4 and 6 and ASP3. All acquired seismic-reflection data are of excellent quality, and for airgun data, penetration is to a depth equivalent to a two-way travel time of as much as 2.0 seconds.
Three acoustical energy sources were utilized simultaneously throughout the survey: two Bolt 40-in3 airguns were fired simultaneously at
10-s intervals at a pressure of 2,000 psi; a Teledyne sparker unit of 600 joules was activated at a repetition rate of 1.5 s; and a ORE 3.5-kHz-tuned transducer was used in an overside fish. Return signals from the airguns were gathered by a 300-m-long hydrophone array consisting of 200 elements, and a shorter 20-element array received the sparker signal. Towing speeds were maintained between 5 and 6 knots and the hydrophones were streamed at a depth of 4 to 5 m. Analog signals were recorded on magnetic tape and graphically on EPI recorders after passing through band-pass filters set for 150/300 Hz for the sparker system and 65/150 Hz for the airgun unit. Sweep rates were 0.5 s for the sparker and 1.0 and 2.0 s for airgun.
Navigation was by Loran-C (5-minute fix interval) and satellite.
The original data may be inspected at the offices of the U.S. Geological Survey in Woods Hole, MA 02 543. Microfilm copies of the data are available for purchase from the National Geophysical and Solar-Terrestrial Data Center (NGSDC), Boulder, CO 80303.
","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr801265","usgsCitation":"Popenoe, P., 1980, Single-channel seismic-reflection profiles collected on the northern Blake Plateau, 29 September to 19 October 1978: U.S. Geological Survey Open-File Report 80-1265, 4 p. :map ;28 cm., https://doi.org/10.3133/ofr801265.","productDescription":"4 p. :map ;28 cm.","costCenters":[],"links":[{"id":143506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr801265.PNG"},{"id":259869,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1265/ofr19801265.pdf","text":"Report","size":"110 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1980-1265"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1801","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":161866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21827,"text":"ofr80837 - 1980 - Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","interactions":[{"subject":{"id":21827,"text":"ofr80837 - 1980 - Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","indexId":"ofr80837","publicationYear":"1980","noYear":false,"title":"Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan"},"predicate":"SUPERSEDED_BY","object":{"id":24989,"text":"pp716G - 1981 - Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","indexId":"pp716G","publicationYear":"1981","noYear":false,"chapter":"G","title":"Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan"},"id":1}],"supersededBy":{"id":24989,"text":"pp716G - 1981 - Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","indexId":"pp716G","publicationYear":"1981","noYear":false,"title":"Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan"},"lastModifiedDate":"2022-10-31T19:34:21.934107","indexId":"ofr80837","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-837","title":"Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","docAbstract":"This report is based upon field investigations covering an area of about 1,400 square miles (3,626 sq km) in the Hindu Rush Mountains of Chitral State in northern Pakistan and also includes a discussion of geological questions relating to an area of about 8,000 square miles (20,720 sq km) in the Chitral-Gilgit area. The area is extremely rugged; local relief exceeds more than 8,000 feet (2,438 meters) over most of the area and commonly reaches 14,000 feet (3,048 meters). Many peaks are higher than 17,000 feet (5,182 meters), and Tirich Mir, 8 miles (12.9 km) north of the mapped area, is 25,263 feet (7,700 meters) high.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80837","collaboration":"Prepared in cooperation with the Geological Survey of Pakistan, under the auspices of the U.S. Department of State and the Government of Pakistan","usgsCitation":"Calkins, J.A., Jamiluddin, S., Bhuyan, K., and Hussain, A., 1980, Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan: U.S. Geological Survey Open-File Report 80-837, Report: viii, 86 p.; 2 Plates: 26.69 x 50.62 inches and 44.04 x 36.53 inches, https://doi.org/10.3133/ofr80837.","productDescription":"Report: viii, 86 p.; 2 Plates: 26.69 x 50.62 inches and 44.04 x 36.53 inches","costCenters":[],"links":[{"id":408920,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0837/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":408919,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0837/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0837/report-thumb.jpg"},{"id":408918,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0837/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Pakistan","otherGeospatial":"Chitral-Partsan area, Hindu Kush Range, northern Pakistan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 70.13671875,\n 33.063924198120645\n ],\n [\n 76.46484375,\n 33.063924198120645\n ],\n [\n 76.46484375,\n 36.914764288955936\n ],\n [\n 70.13671875,\n 36.914764288955936\n ],\n [\n 70.13671875,\n 33.063924198120645\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b470b","contributors":{"authors":[{"text":"Calkins, James Alfred","contributorId":75504,"corporation":false,"usgs":true,"family":"Calkins","given":"James","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":185853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jamiluddin, S.","contributorId":29009,"corporation":false,"usgs":true,"family":"Jamiluddin","given":"S.","email":"","affiliations":[],"preferred":false,"id":185852,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bhuyan, K.","contributorId":91895,"corporation":false,"usgs":true,"family":"Bhuyan","given":"K.","affiliations":[],"preferred":false,"id":185854,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hussain, A.","contributorId":6886,"corporation":false,"usgs":true,"family":"Hussain","given":"A.","email":"","affiliations":[],"preferred":false,"id":185851,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":10191,"text":"ofr801238 - 1980 - Heat flow from the western arm of the Black Rock Desert, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr801238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1238","title":"Heat flow from the western arm of the Black Rock Desert, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801238","usgsCitation":"Mase, C., and Sass, J., 1980, Heat flow from the western arm of the Black Rock Desert, Nevada: U.S. Geological Survey Open-File Report 80-1238, 38 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801238.","productDescription":"38 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1238/report-thumb.jpg"},{"id":38053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1238/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ae4b07f02db63cfb8","contributors":{"authors":[{"text":"Mase, C. W.","contributorId":106893,"corporation":false,"usgs":true,"family":"Mase","given":"C. W.","affiliations":[],"preferred":false,"id":160975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":160974,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10975,"text":"ofr80188 - 1980 - Lithologic and geophysical logs of drill holes BCR-4 and BCR-3 and coal analysis of a 1978 drill hole BCR-1 in the southern part of the Wasatch Plateau coal field, Emery West, Flagstaff Peak, and Acord Lakes quadrangles, Sevier County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr80188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-188","title":"Lithologic and geophysical logs of drill holes BCR-4 and BCR-3 and coal analysis of a 1978 drill hole BCR-1 in the southern part of the Wasatch Plateau coal field, Emery West, Flagstaff Peak, and Acord Lakes quadrangles, Sevier County, Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80188","usgsCitation":"Sanchez, J.D., 1980, Lithologic and geophysical logs of drill holes BCR-4 and BCR-3 and coal analysis of a 1978 drill hole BCR-1 in the southern part of the Wasatch Plateau coal field, Emery West, Flagstaff Peak, and Acord Lakes quadrangles, Sevier County, Utah: U.S. Geological Survey Open-File Report 80-188, 34 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr80188.","productDescription":"34 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0188/report-thumb.jpg"},{"id":38744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0188/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b476e","contributors":{"authors":[{"text":"Sanchez, Joseph D.","contributorId":100847,"corporation":false,"usgs":true,"family":"Sanchez","given":"Joseph","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":162308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4708,"text":"twri03B3 - 1980 - Type curves for selected problems of flow to wells in confined aquifers","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri03B3","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-B3","title":"Type curves for selected problems of flow to wells in confined aquifers","docAbstract":"This report presents type curves and related material for\r\n11 conditions of flow to wells m confined aquifers. These\r\nsolutions, compiled from hydrologic literature, span an\r\ninterval of time from Theis (1935) to Papadopulos, Bredehoeft,\r\nand Cooper (1973). Solutions are presented for\r\nconstant discharge, constant drawdown, and variable discharge\r\nfor pumping wells that fully penetrate leaky and\r\nnonleaky aquifers. Solutions for wells that partially penetrate\r\nleaky and nonleaky aquifers are included. Also, solutions\r\nare included for the effect of finite well radius and\r\nthe sudden injection of a volume of water for nonleaky\r\naquifers. Each problem includes the partial differential\r\nequation, boundary and initial conditions, and solutions.\r\nPrograms in FORTRAN for calculating additional function\r\nvalues are included for most of the solutions.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri03B3","issn":"0565-596X","usgsCitation":"Reed, J., 1980, Type curves for selected problems of flow to wells in confined aquifers: U.S. Geological Survey Techniques of Water-Resources Investigations 03-B3, ix, 106 p. :ill. ;26 cm., https://doi.org/10.3133/twri03B3.","productDescription":"ix, 106 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":139146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":297,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-b3/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6237d2","contributors":{"authors":[{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":149655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24486,"text":"ofr801026 - 1980 - Geophysical logs of five coal test holes drilled in the Kemmerer coal field, Uinta and Lincoln counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr801026","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1026","title":"Geophysical logs of five coal test holes drilled in the Kemmerer coal field, Uinta and Lincoln counties, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801026","issn":"0094-9140","usgsCitation":"Schroeder, M.L., 1980, Geophysical logs of five coal test holes drilled in the Kemmerer coal field, Uinta and Lincoln counties, Wyoming: U.S. Geological Survey Open-File Report 80-1026, 15 p. :chiefly ill., maps ;28 cm., https://doi.org/10.3133/ofr801026.","productDescription":"15 p. :chiefly ill., maps ;28 cm.","costCenters":[],"links":[{"id":155712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1026/report-thumb.jpg"},{"id":53555,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b7c1","contributors":{"authors":[{"text":"Schroeder, Marvin L.","contributorId":91104,"corporation":false,"usgs":true,"family":"Schroeder","given":"Marvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":192013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}