This report contains hydrologic data on water-level measurements in observation wells in western and south-central Kansas. The measurements were made in mid-winter, mostly in January, when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also provides basic hydrologic data for relating water-level changes from a \"base-reference year\" (pre-development year), a year of abnormally high rainfall and minimum pumpage (1966), and the previous year (1979). The \"base-reference year\" i s designated as 1950 for the northwestern and west-central areas, 1940 for the southwestern area, and 1944 for the south-central area. Water-level data in the south-central area also are compared with data for 1974. \"Base-reference-year\" water levels are based on measurements made during that year and on interpretation of water-table-contour maps.
Tables in the report show the depths to water level in 1940, 1944, or 1950 (pre-development years), 1966, 1974, 1979, and 1980; water-level changes from 1940-80,1944-80,1950-80,1966-80,1974-80, and 1979-80; and the average annual changes from 1940-80, 1944-80, 1950-80, 1966-80, and 1974-80. Also shown are saturated thicknesses of the deposits in 1940, 1944, or 1950, and in 1980, as well as the percentage change in saturated thickness from 1940-80, 1944-80, or 1950-80.
Maps in the report, drawn by digital plotter, show the location of observation wells where water-level measurements are made. The water-level rise or decline, 1979-80, is given to the nearest 0.01 foot; two values at the same location indicate separate wells in the same 10-acre tract.
The annual water-level measurements are made by personnel of the Division of Water Resources of the Kansas State Board of Agriculture and of the U.S. Geological Survey. State-agency support for this program is provided through the Kansas Geological Survey.
Wells in this report are numbered according to the Bureau of Land Manage- ment's system of land subdivision. In this system, the first set of digits of a well number indicates the township; the second set, the range east or west of the sixth principal meridian; and the third set, the section in which the well is situated. The first letter denotes the 160-acre tract within the section; the second, the 40-acre tract, and the third, the 10-acre tract. The letters, A, B, C, or D, are designated in a counterclockwise direction beginning in the northeast quadrant. Because there may be more than one well in a 10-acre tract, consecutive numbers, beginning with \"1\", are added in the order in which the data from the wells are collect.
Explanation of geologic units in tables 1 and 2 are: QA, Quaternary alluvium; QU, undifferentiated Quaternary deposits; TO, Ogallala Formation; KN, Niobrara Formation; KU, undifferentiated Lower Cretaceous rocks; KJ, undiffer-rentiated Lower Cretaceous and Upper Jurassic rocks.
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showing electric log correlation section E-E' of some Upper Cretaceous and Tertiary rocks, Cherokee Ridge, Wyoming","language":"ENGLISH","doi":"10.3133/ofr80191","usgsCitation":"Tyler, T.F., 1980, Preliminary chart showing electric log correlation section E-E' of some Upper Cretaceous and Tertiary rocks, Cherokee Ridge, Wyoming: U.S. Geological Survey Open-File Report 80-191, 4 sheets ;220 x 107 cm. or smaller., https://doi.org/10.3133/ofr80191.","productDescription":"4 sheets ;220 x 107 cm. or 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F.","contributorId":103648,"corporation":false,"usgs":true,"family":"Tyler","given":"Theodore","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":224349,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24411,"text":"ofr80571 - 1980 - Cape Cod Aquifer, Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2022-08-02T18:38:18.517501","indexId":"ofr80571","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":"80-571","title":"Cape Cod Aquifer, Cape Cod, Massachusetts","docAbstract":"Ground water was the major source of drinking water on Cape Cod, Massachusetts in 1978. Withdrawals from over 100 municipal wells averaged 17.5 million gallons per day in 1978. Private wells on Cape Cod are estimated to number 15,000. Ground water occurs primarily under unconfined or water-table conditions. Artesian conditions exist where fine silt and clay beds have been deposited along Cape Cod's north shore from Bourne to Brewster, locally along the south shore, and in parts of Chatham and Orleans. Natural recharge to the aquifer is entirely from precipitation. Discharge is by pumping; evapotranspiration; direct evaporation from the water table; and seepage to rivers, marshes, and the ocean. Ground-water quality is generally suitable for domestic uses, although some public and private water wells have been contaminated. Contaminants can enter the ground water by infiltration from land surface, ponds, streams, and swamps. Infiltration from sewage lagoons, sand filter beds, septic tanks, cesspools, recharge pits, wells, or intrusion of saline water may also contaminate the aquifer. Alternative sources of drinking water, including desalination, transport from the mainland, and rainwater cisterns, are many times more expensive.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80571","issn":"0094-9140","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Ryan, B.J., 1980, Cape Cod Aquifer, Cape Cod, Massachusetts: U.S. Geological Survey Open-File Report 80-571, Report: v, 23 p.; 3 Plates: 25.36 x 25.67 inches or smaller, https://doi.org/10.3133/ofr80571.","productDescription":"Report: v, 23 p.; 3 Plates: 25.36 x 25.67 inches or smaller","costCenters":[],"links":[{"id":404686,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0571/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404685,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0571/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404684,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0571/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404683,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0571/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0571/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.64208984375,\n 41.50034959128928\n ],\n [\n -69.873046875,\n 41.50034959128928\n ],\n [\n -69.873046875,\n 42.15525946577863\n ],\n [\n -70.64208984375,\n 42.15525946577863\n ],\n [\n -70.64208984375,\n 41.50034959128928\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f692a","contributors":{"authors":[{"text":"Ryan, Barbara J.","contributorId":62989,"corporation":false,"usgs":true,"family":"Ryan","given":"Barbara","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":191878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24404,"text":"ofr80560 - 1980 - Hydrologic data for runoff studies on small drainage areas, West Virginia Department of Highways Research Project 16","interactions":[],"lastModifiedDate":"2022-10-25T19:44:33.681433","indexId":"ofr80560","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":"80-560","title":"Hydrologic data for runoff studies on small drainage areas, West Virginia Department of Highways Research Project 16","docAbstract":"Station listings, basin and flow characteristics tables, and annual maximum discharges are presented for stations in West Virginia, Maryland, and Virginia that were used to develop flood-frequency relations for West Virginia. Also presented are figures showing approximate station location and areal coverage for both longterm and short-term stations that were used in the frequency analysis.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80560","collaboration":"Prepared in cooperation with the West Virginia Department of Highways and Federal Highway Administration","usgsCitation":"Runner, G.S., 1980, Hydrologic data for runoff studies on small drainage areas, West Virginia Department of Highways Research Project 16: U.S. Geological Survey Open-File Report 80-560, 169 p., https://doi.org/10.3133/ofr80560.","productDescription":"169 p.","costCenters":[],"links":[{"id":408715,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0560/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0560/report-thumb.jpg"}],"country":"United States","state":"West 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Virginia\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ed0f","contributors":{"authors":[{"text":"Runner, Gerald S.","contributorId":90297,"corporation":false,"usgs":true,"family":"Runner","given":"Gerald","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":191866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24394,"text":"ofr80931 - 1980 - Preliminary map showing distribution of altered rocks and limonitic unaltered rocks in the Walker Lake 1° by 2° quadrangle, Nevada-California","interactions":[],"lastModifiedDate":"2022-05-04T21:28:42.747395","indexId":"ofr80931","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":"80-931","title":"Preliminary map showing distribution of altered rocks and limonitic unaltered rocks in the Walker Lake 1° by 2° quadrangle, Nevada-California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80931","issn":"0094-9140","usgsCitation":"Rowan, L.C., and Purdy, T.L., 1980, Preliminary map showing distribution of altered rocks and limonitic unaltered rocks in the Walker Lake 1° by 2° quadrangle, Nevada-California: U.S. Geological Survey Open-File Report 80-931, 1 Plate: 44.56 × 22.54 inches, https://doi.org/10.3133/ofr80931.","productDescription":"1 Plate: 44.56 × 22.54 inches","costCenters":[],"links":[{"id":53490,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0931/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Walker Lake 1° by 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120,\n 38\n ],\n [\n -118,\n 38\n ],\n [\n -118,\n 39\n ],\n [\n -120,\n 39\n ],\n [\n -120,\n 38\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968d6","contributors":{"authors":[{"text":"Rowan, Lawrence C.","contributorId":58629,"corporation":false,"usgs":true,"family":"Rowan","given":"Lawrence","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":191844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purdy, Terri L.","contributorId":87950,"corporation":false,"usgs":true,"family":"Purdy","given":"Terri","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191845,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11698,"text":"ofr791271 - 1980 - Simulated effects of ground-water development on potentiometric surface of the Floridan Aquifer, west-central Florida","interactions":[{"subject":{"id":11698,"text":"ofr791271 - 1980 - Simulated effects of ground-water development on potentiometric surface of the Floridan Aquifer, west-central Florida","indexId":"ofr791271","publicationYear":"1980","noYear":false,"title":"Simulated effects of ground-water development on potentiometric surface of the Floridan Aquifer, west-central Florida"},"predicate":"SUPERSEDED_BY","object":{"id":38602,"text":"pp1217 - 1982 - Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida","indexId":"pp1217","publicationYear":"1982","noYear":false,"title":"Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida"},"id":1}],"supersededBy":{"id":38602,"text":"pp1217 - 1982 - Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida","indexId":"pp1217","publicationYear":"1982","noYear":false,"title":"Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida"},"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr791271","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":"79-1271","title":"Simulated effects of ground-water development on potentiometric surface of the Floridan Aquifer, west-central Florida","docAbstract":"A digital model of two-dimensional ground-water flow was used to predict changes in the potentiometric surface of the Floridan aquifer, 1976-2000, in a 5,938-square-mile area of west-central Florida. In 1975, ground water withdrawn from the Floridan aquifer for irrigation, phosphate mines, other industries, and municipal supplies averaged about 649 million gallons per day. Rates are projected to increase to about 840 million gallons per day by 2000. The model was calibrated under steady-state and transient conditions. Input parameters included transmissivity and storage coefficient of the Floridan aquifer; thickness, vertical hydraulic conductivity, and storage coefficient of the upper confining bed; altitudes of the water table and potentiometric surface; and ground-water withdrawals. Simulation of May 1976 to May 2000, using projected combined pumping rates for municipal supplies, irrigation, and industry (including existing and proposed phosphate mines), resulted in a rise in the potentiometric surface of about 10 feet in Polk County, and a decline of about 35 feet in parts of Manatee and Hardee Counties. The lowest predicted potentiometric level was about 30 feet below sea level. Predicted declines for November 1976 to October 2000 were generally 5 to 10 feet less than those for May 1976 to May 2000. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791271","usgsCitation":"Wilson, W.E., and Gerhart, J.M., 1980, Simulated effects of ground-water development on potentiometric surface of the Floridan Aquifer, west-central Florida: U.S. Geological Survey Open-File Report 79-1271, 128 p. :ill., maps (2 fold. in pocket) ;28 cm., https://doi.org/10.3133/ofr791271.","productDescription":"128 p. :ill., maps (2 fold. in pocket) ;28 cm.","costCenters":[],"links":[{"id":145060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1271/report-thumb.jpg"},{"id":39579,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1271/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39580,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1271/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39581,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1271/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3922","contributors":{"authors":[{"text":"Wilson, William Edward","contributorId":82321,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":163587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gerhart, James M.","contributorId":35717,"corporation":false,"usgs":true,"family":"Gerhart","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":47195,"text":"ofr80788 - 1980 - Geologic map and sections of the Sonsela Butte 4 SE Quadrangle, Apache County, Arizona, and San Juan and McKinley counties, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:04:54","indexId":"ofr80788","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":"80-788","title":"Geologic map and sections of the Sonsela Butte 4 SE Quadrangle, Apache County, Arizona, and San Juan and McKinley counties, New Mexico","language":"ENGLISH","doi":"10.3133/ofr80788","usgsCitation":"Byers, V.P., 1980, Geologic map and sections of the Sonsela Butte 4 SE Quadrangle, Apache County, Arizona, and San Juan and McKinley counties, New Mexico: U.S. Geological Survey Open-File Report 80-788, 1 map ;58 x 47 cm. on sheet 89 x 113 cm., https://doi.org/10.3133/ofr80788.","productDescription":"1 map ;58 x 47 cm. on sheet 89 x 113 cm.","costCenters":[],"links":[{"id":108069,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11765.htm","linkFileType":{"id":5,"text":"html"},"description":"11765"},{"id":134900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84170,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0788/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea16","contributors":{"authors":[{"text":"Byers, Virginia P.","contributorId":71147,"corporation":false,"usgs":true,"family":"Byers","given":"Virginia","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":234802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41110,"text":"ofr80723 - 1980 - Preliminary bedrock map of the Chiwaukum 4 SE Quadrangle, Chiwaukum Graben, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:11:10","indexId":"ofr80723","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":"80-723","title":"Preliminary bedrock map of the Chiwaukum 4 SE Quadrangle, Chiwaukum Graben, Washington","language":"ENGLISH","doi":"10.3133/ofr80723","usgsCitation":"Whetten, J.T., 1980, Preliminary bedrock map of the Chiwaukum 4 SE Quadrangle, Chiwaukum Graben, Washington: U.S. Geological Survey Open-File Report 80-723, 1 map ;58 x 40 cm.; 6 p., https://doi.org/10.3133/ofr80723.","productDescription":"1 map ;58 x 40 cm.; 6 p.","costCenters":[],"links":[{"id":108067,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11748.htm","linkFileType":{"id":5,"text":"html"},"description":"11748"},{"id":175333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0723/report-thumb.jpg"},{"id":78964,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0723/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78965,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0723/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c8c0","contributors":{"authors":[{"text":"Whetten, John T.","contributorId":102444,"corporation":false,"usgs":true,"family":"Whetten","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":224517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23686,"text":"ofr80322 - 1980 - Feldspar from hybrid granitoid rocks of the southern Snake Range, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"ofr80322","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":"80-322","title":"Feldspar from hybrid granitoid rocks of the southern Snake Range, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80322","issn":"0094-9140","usgsCitation":"Lee, D.E., Van Loenen, R.E., and Brandt, E., 1980, Feldspar from hybrid granitoid rocks of the southern Snake Range, Nevada: U.S. Geological Survey Open-File Report 80-322, 11 p. ill. ;27 cm., https://doi.org/10.3133/ofr80322.","productDescription":"11 p. ill. ;27 cm.","costCenters":[],"links":[{"id":156702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5d14","contributors":{"authors":[{"text":"Lee, Donald Edward","contributorId":101660,"corporation":false,"usgs":true,"family":"Lee","given":"Donald","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":190549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Loenen, Richard E.","contributorId":13951,"corporation":false,"usgs":true,"family":"Van Loenen","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190547,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brandt, Elaine L.","contributorId":83157,"corporation":false,"usgs":true,"family":"Brandt","given":"Elaine L.","affiliations":[],"preferred":false,"id":190548,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23691,"text":"ofr80336 - 1980 - Geochemistry of water in the Fort Union Formation of the northern Powder River basin, southeastern Montana","interactions":[{"subject":{"id":23691,"text":"ofr80336 - 1980 - Geochemistry of water in the Fort Union Formation of the northern Powder River basin, southeastern Montana","indexId":"ofr80336","publicationYear":"1980","noYear":false,"title":"Geochemistry of water in the Fort Union Formation of the northern Powder River basin, southeastern Montana"},"predicate":"SUPERSEDED_BY","object":{"id":2092,"text":"wsp2076 - 1981 - Geochemistry of water in the Fort Union formation of the northern Powder River basin, southeastern Montana","indexId":"wsp2076","publicationYear":"1981","noYear":false,"title":"Geochemistry of water in the Fort Union formation of the northern Powder River basin, southeastern Montana"},"id":1}],"supersededBy":{"id":2092,"text":"wsp2076 - 1981 - Geochemistry of water in the Fort Union formation of the northern Powder River basin, southeastern Montana","indexId":"wsp2076","publicationYear":"1981","noYear":false,"title":"Geochemistry of water in the Fort Union formation of the northern Powder River basin, southeastern Montana"},"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr80336","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":"80-336","title":"Geochemistry of water in the Fort Union Formation of the northern Powder River basin, southeastern Montana","docAbstract":"Shallow water in the coal-bearing Fort Union Formation of southeastern Montana was investigated to provide a better understanding of the geochemistry. Springs, wells less than 200 feet deep, and wells greater then 200 feet deep were observed to have different water qualities. Overall, the ground water exists as two systems: a mosaic of shallow, chemically dynamic, and localized recharge-discharge cells superimposed on a deeper, chemically static regional system. Water chemistry is highly variable in the shallow system, whereas sodium and bicarbonate waters characterize the deeper system. Within the shallow system , springs, and wells less than 200 feet deep show predominantly sodium and sulfate enrichment processes from recharge to discharge. These processes are consistent with the observed aquifer mineralogy and aqueous chemistry. However, intermittent mixing with downward moving recharge waters or upward moving deeper waters, and bacterially catalyzed sulfate reduction, may cause apparent reversals in these processes. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80336","issn":"0094-9140","usgsCitation":"Lee, R.W., 1980, Geochemistry of water in the Fort Union Formation of the northern Powder River basin, southeastern Montana: U.S. Geological Survey Open-File Report 80-336, iv, 21 p. ill., maps ;26 cm., https://doi.org/10.3133/ofr80336.","productDescription":"iv, 21 p. ill., maps ;26 cm.","costCenters":[],"links":[{"id":157086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a28e6","contributors":{"authors":[{"text":"Lee, Roger W.","contributorId":105273,"corporation":false,"usgs":true,"family":"Lee","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":190555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24342,"text":"ofr80934 - 1980 - High-resolution seismic-reflection profiles collected by the R/V James M. Gilliss, cruise GS 7903-4, in the Baltimore Canyon outer continental shelf area, offshore New Jersey","interactions":[],"lastModifiedDate":"2018-06-19T08:26:08","indexId":"ofr80934","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":"80-934","title":"High-resolution seismic-reflection profiles collected by the R/V James M. Gilliss, cruise GS 7903-4, in the Baltimore Canyon outer continental shelf area, offshore New Jersey","docAbstract":"High-resolution seismic-reflection profiles were collected by the U.S. Geological Survey (USGS) aboard R/V JAMES M. GILLIS (cruise GS 7903-4) from 27 June to 11 July 1979 over the Continental Slope of the Eastern United States between Lindenkohl and Hudson Canyons. These data were acquired as part of a study to determine potential geologic hazards to petroleum development of the Baltimore Canyon trough area. On this cruise, the Continental Slope between Carteret and South Toms Canyons was surveyed along lines spaced one-half nautical mile apart to study the size and distribution of mass-wasting features as a guide to assess the importance of mass-wasting processes on the Continental Slope. The seimsic-reflection profiles were placed to complement other data gathered previously by the USGS and to continue a survey grid begun in 1978 aboard the R/V COLUMBUS !SELIN, cruise CI 7807-1.
Track-line distances totaled 1,555 km of 40-in3 air-gun (with wave shaper) profiles, 1, 750 km of 800-J sparker data, and 1,780 km of 3 .5-kHz data. All data are of high quality. A side-scan sonar system was operated briefly along the uppermost Continental Slope to acquire data over 70 km of ship's track. In addition, experimental profiling data were collected from a hydrophone towed at depth over the midslope on the end of the side-scan cable; the surface-towed sparker was used as a sound source. High-resolution profiles were collected by this method over 105 km of track.
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, Massachusetts 02543. Microfilm copies of the data from this cruise are available for purchase from the National Geophysical and Solar-Terrestrial Data Center (NGSDC), Boulder, Colorado 80303.
","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80934","issn":"0094-9140","usgsCitation":"Robb, J.M., 1980, High-resolution seismic-reflection profiles collected by the R/V James M. Gilliss, cruise GS 7903-4, in the Baltimore Canyon outer continental shelf area, offshore New Jersey: U.S. Geological Survey Open-File Report 80-934, 3 p. :map ;28 cm., https://doi.org/10.3133/ofr80934.","productDescription":"3 p. :map ;28 cm.","costCenters":[],"links":[{"id":259880,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0934/ofr1980934.pdf","text":"Report","size":"67 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1980-934"},{"id":157437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr80934.PNG"}],"contact":"Coastal and Marine Geology Program
U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
Thermal water (30.0 to 72.0 degrees Celsius) is produced from 26 wells and 2 springs in the vicinity of Banbury Hot Springs near Buhl, Idaho. Thermal water is used for space heating of private residences, catfish and tropical fish production, greenhouse operation, swimming pools, and therapeutic baths. In 1979, 10 ,300 acre-feet of thermal water was utilized; heat discharged convectively from the geothermal system was about 1.1 x 107 calories per second. Decline in artesian head and discharge apparent in recorder charts from two wells may represent seasonal fluctuations or may reflect aquifer response to development of the resource. Thermal waters sampled are sodium bicarbonate in character and slightly alkaline. Mixing of a hot (72 degrees Celsius) water with local, cooler ground water can be shown from various relations between stable isotopes, chloride, and enthalpy. On the basis of concentration of trituim, age of the waters sampled is at least 100 years an perhaps more than 1,000 years. One water (33 degress Celsius) may be as young as 29 years. On the basis of silica, sodium-potassium-calcium, and sulfate-water geothermometers, best estimate of the maximum reservoir temperature for the thermal waters is between about 70 and 100 degrees Celsius.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80563","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Lewis, R., and Young, H., 1980, Geothermal resources in the Banbury Hot Springs area, Twin Falls County, Idaho: U.S. Geological Survey Open-File Report 80-563, Report: iv, 35 p.; 2 Plates: 20.55 x 12.53 inches and 20.45 x 12.50 inches, https://doi.org/10.3133/ofr80563.","productDescription":"Report: iv, 35 p.; 2 Plates: 20.55 x 12.53 inches and 20.45 x 12.50 inches","costCenters":[],"links":[{"id":156132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0563/report-thumb.jpg"},{"id":404689,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0563/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404688,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0563/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404687,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0563/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Twin Falls County","otherGeospatial":"Banbury Hot Springs area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.84695434570311,\n 42.65012181368022\n ],\n [\n -114.7906494140625,\n 42.65012181368022\n ],\n [\n -114.7906494140625,\n 42.69959515809203\n ],\n [\n -114.84695434570311,\n 42.69959515809203\n ],\n [\n -114.84695434570311,\n 42.65012181368022\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aece","contributors":{"authors":[{"text":"Lewis, R.E.","contributorId":31735,"corporation":false,"usgs":true,"family":"Lewis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":190588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":190589,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24341,"text":"ofr80935 - 1980 - High-resolution seismic-reflection profiles collected by the R/V Columbus Iselin, cruise CI 7807-1, in the Baltimore Canyon outer continental shelf area, offshore New Jersey","interactions":[],"lastModifiedDate":"2018-06-19T08:24:20","indexId":"ofr80935","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":"80-935","title":"High-resolution seismic-reflection profiles collected by the R/V Columbus Iselin, cruise CI 7807-1, in the Baltimore Canyon outer continental shelf area, offshore New Jersey","docAbstract":"High-resolution seismic-reflection profiles were collected by the U.S. Geological Survey (USGS) aboard R/V COLUMBUS ISELIN, cruise 7807-1, from 18 August to 4 September 1978 over the Continental Slope of the Eastern United States between Wilmington and Hudson Canyons. These data were acquired as part of a study to determine potential geologic hazards to petroleum development of the Baltimore Canyon trough area. On this cruise, the Continental Slope between Lindenkohl and Carteret Canyons was surveyed along lines spaced one-half nautical mile apart to study the size and distribution of mass-wasting features as a guide to assess the importance of mass wasting processes on the Continental Slope. The seismic-reflection profiles were placed to complement other data gathered previously by the USGS.
Track-line distances totaled 2,050 km of 40-in3 air-gun (with wave shaper) profiles, 2,100 km of 800-J sparker data, and 2,100 km of 3 .5-kHz data. The air-gun and sparker profiles are of high quality, but the 3.5-kHz system did not function well and achieved no subbottom penetration. The side-scan sonar system was operated along the uppermost Continental Slope to investigate its potential for use in this environment. Data were acquired over 22 km of ship's track.
Navigation was by Loran-C (5-minute fix interval).
The original records can be examined at the U.S. Geological Survey offices in Woods Hole, Massachusetts 02543. Microfilm copies of the data are available for purchase from the National Geophysical and Solar-Terrestrial Data Center (NGSDC), Boulder, Colorado 80303.
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U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
The Red River alluvial aquifer of Louisiana underlies approximately 2,000 square miles in the Red River Valley of Louisiana. The aquifer is Pleistocene in age and consists of clay, silt, sand, and gravel deposited by the Red River. Sand and gravel constitute the lower two-thirds of the deposit, the most productive part of the aquifer. The aquifer ranges from 40 to 150 feet in thickness and reaches its maximum thickness in Avoyelles and Catahoula Parishes. Fine sand, silt, and clay of Holocene age overlie and generally confine the aquifer. These fine-grained deposits generally do not exceed 50 feet in thickness.
The aquifer is recharged by downward seepage of rainfall in the valley, by lateral movement of water from adjacent Pleistocene and Tertiary formations, and by upward movement of water from underlying formations of Tertiary age. When large quantities of seepage occur locally within short periods of time, a temporary reduction in mineralization takes place in the upper part of the aquifer. Lateral recharge from Pleistocene and Tertiary formations generally upgrades water in the alluvial aquifer near the edge of the valley. Recharge from underlying aquifers may upgrade or downgrade the quality of water in the lower part of the alluvial aquifer.
The Red River and its major tributaries recharge the Red River alluvial aquifer in local zones near the river during high stream stages, but noticeable water-quality changes occur only following periods of prolonged high stages.
Ground water in the alluvium generally moves toward the streams and down the valley. Water levels fluctuate seasonally and are generally less than 30 feet below land surface. Annual water-level fluctuations have a maximum range of about 30 feet near the Red River, and a minimum range of only a few feet in some interstream areas.
The Red River alluvial aquifer can yield 2,000 gallons per minute or more of water to individual wells where thick beds of coarse sand and gravel occur in the southern part of the study area. Aquifer tests indicate that the transmissivity ranges from 2,000 to 27,000 feet squared per day. The hydraulic conductivity ranges from 100 to 300 feet per day. Storage coefficients range from 6.0x10-4 to 1.0x10-3.
Water in the aquifer typically is of the calcium magnesium bicarbonate type. The water is hard to very hard, ranging in hardness from about 100 to 2,300 mg/L (milligrams per liter). However, hardness generally is in the 200- to 600-mg/L range. The ions that appear to be most variable in occurrence and sensitive to change with time are calcium, magnesium, iron, sulfate, and chloride. Iron concentrations range from less than 0.3 mg/L to as high as 49 mg/L but generally are 1 to 10 mg/L. In areas where rapid recharge occurs, shallow wells may have iron concentrations of less than 0.3 mg/L. Sulfate concentrations generally range from 0.5 to 50 mg/L but locally exceed 250 mg/L. The highest concentration detected was 1,900 mg/L. Chloride concentrations typically are less than 50 Mg/L. However, concentrations of chloride exceed 250 mg/L locally and are as high as 4,400 mg/L in a few areas. For this report, water with chloride concentrations greater than 250 mg/L is considered salty.
The base of freshwater in the Red River Valley generally coincides with the base of the alluvium at depths of 80 to 150 feet. However, locally, the aquifer contains salty water, and the base of freshwater occurs within the aquifer; in parts of Rapides, Caddo, and Natchitoches Parishes, the base of freshwater extends below the alluvium. The largest occurrence of salty water is in Natchitoches Parish, with other smaller bodies occurring in Red River, Caddo, and Bossier Parishes.
Water quality in the aquifer varies both areally and with depth; the quality also varies with time, depending on the quantity and chemical character of the recharge water.
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Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80372","issn":"0094-9140","usgsCitation":"Repetski, J.E., and Perry, W., 1980, Early Ordovician conodonts from the Bane Dome, Giles County, Virginia: U.S. Geological Survey Open-File Report 80-372, 14 p. ill. ;28 cm., https://doi.org/10.3133/ofr80372.","productDescription":"14 p. ill. ;28 cm.","costCenters":[],"links":[{"id":156273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0372/report-thumb.jpg"},{"id":53423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0372/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c29e","contributors":{"authors":[{"text":"Repetski, John E. 0000-0002-2298-7120 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1979","interactions":[],"lastModifiedDate":"2016-06-22T08:33:43","indexId":"ofr80970","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":"80-970","title":"Quality of surface water in the coal-mining region, southwestern Indiana, March and May 1979","docAbstract":"On August 3, 1977, the Surface Mine Control and Reclamation Act, Public Law 95-87 (the Act) was enacted by the 95th Congress. Under Section 507(b)(11) of the Act, an appropriate Federal or State agency must provide applicants for coal-mining permits hydrologic and water-quality information for the general use of proposed mining. To help meet the goals of the Act, the U.S. Geological Survey is designing a data-collection network in the coal-mining region of southwestern Indiana. The purpose of the network is to provide hydrologic and water-quality data on the ' general area ' for coal-mining permits. Because of the large size of the study area and the lack of hydrologic and water-quality data, a preliminary assessment is being done to determine the factors that affect water quality in the coal-mining region. This information will be used in designing a data network that will (1) provide the hydrologic and water-quality data needed by applicants for coal-mining permits and (2) determine the major factors that affect water quality. Reconnaissance data were collected at 293 sites in March, and hydrologic and water-quality data were collected at 84 synoptic sampling sites in May. (Synoptic sampling is the virtually simultaneous collection of data at specific sites.) In the reconnaissance, pH, specific conductance, dissolved-oxygen concentration, temperature, and Eh of streams were measured on site to provide general water-quality data. In the synoptic sampling, the preceding characteristics, as well as concentrations of various dissolved and suspended constituents of stream water and concentrations of heavy metals on streambed materials, were determined.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr80970","issn":"0094-9140","usgsCitation":"Renn, D.E., Ragone, S.E., and Wilber, W.G., 1980, Quality of surface water in the coal-mining region, southwestern Indiana, March and May 1979: U.S. Geological Survey Open-File Report 80-970, v, 69 p. :maps ;28 cm., https://doi.org/10.3133/ofr80970.","productDescription":"v, 69 p. :maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":156272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635d26","contributors":{"authors":[{"text":"Renn, Danny E.","contributorId":14808,"corporation":false,"usgs":true,"family":"Renn","given":"Danny","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ragone, Stephen E.","contributorId":74374,"corporation":false,"usgs":true,"family":"Ragone","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191678,"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":191676,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11643,"text":"ofr801232 - 1980 - Depositional environment of the middle Proterozoic Spokane Formation; Empire Formation transition zone, west-central Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr801232","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":"80-1232","title":"Depositional environment of the middle Proterozoic Spokane Formation; Empire Formation transition zone, west-central Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801232","usgsCitation":"Whipple, J., 1980, Depositional environment of the middle Proterozoic Spokane Formation; Empire Formation transition zone, west-central Montana: U.S. Geological Survey Open-File Report 80-1232, iv, 103 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801232.","productDescription":"iv, 103 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1232/report-thumb.jpg"},{"id":39499,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1232/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab1e4b07f02db66e944","contributors":{"authors":[{"text":"Whipple, James W.","contributorId":90736,"corporation":false,"usgs":true,"family":"Whipple","given":"James W.","affiliations":[],"preferred":false,"id":163493,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24310,"text":"ofr80360 - 1980 - Dinkum Sands","interactions":[],"lastModifiedDate":"2023-06-05T19:54:40.185229","indexId":"ofr80360","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":"80-360","title":"Dinkum Sands","docAbstract":"The State/Federal Beaufort Sea lease sale in December 1979 attracted over one billion dollars in bids. Tracts with the highest bids, and apparently with the highest oil potential, lie in the area south of Dinkum Sands, and within a three-mile radius of the shoal (Fig. 1). Jurisdiction over the tracts within the three-mile radius depends on whether Dinkum Sands is an island, as shown by published charts and claimed by the State, or a mainly submerged shoal or bar as claimed by the U.S.G.S. If Dinkum Sands were an island, even the tracts halfway between the mainland and the island chain might be disputed as they then would be considered to form an enclave totally surrounded by State lands. Thus Dinkum Sands holds a strategic position within the lease sale area and, for the production life of the oil field, will be monitored at 5-minute intervals to provide a basis for division of the income from future oil production in that lease sale area.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80360","issn":"0094-9140","usgsCitation":"Reimnitz, E., Ross, R., and Barnes, P.W., 1980, Dinkum Sands: U.S. Geological Survey Open-File Report 80-360, 11 p., https://doi.org/10.3133/ofr80360.","productDescription":"11 p.","costCenters":[],"links":[{"id":417772,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0360/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156252,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0360/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Dinkum Sands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -148.3102976268423,\n 70.39082100908053\n ],\n [\n -148.3102976268423,\n 70.22987259684805\n ],\n [\n -147.54158447661962,\n 70.22987259684805\n ],\n [\n -147.54158447661962,\n 70.39082100908053\n ],\n [\n -148.3102976268423,\n 70.39082100908053\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ac4a","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":191671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, Robin","contributorId":36547,"corporation":false,"usgs":true,"family":"Ross","given":"Robin","email":"","affiliations":[],"preferred":false,"id":191672,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barnes, Peter W.","contributorId":6042,"corporation":false,"usgs":true,"family":"Barnes","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":191670,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24297,"text":"ofr80446 - 1980 - Digital-computer model of ground-water flow in Tooele Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-02T14:02:18","indexId":"ofr80446","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":"80-446","title":"Digital-computer model of ground-water flow in Tooele Valley, Utah","docAbstract":"A two-dimensional, finite-difference digital-computer model was used to simulate the ground-water flow in the principal artesian aquifer in Tooele Valley, Utah. The parameters used in the model were obtained through field measurements and tests, from historical records, and by trial-and-error adjustments. The model was calibrated against observed water-level changes that occurred during 1941-50, 1951-60, 1961-66, 1967-73, and 1974-78. The reliability of the predictions is good in most parts of the valley, as is shown by the ability of the model to match historical water-level changes.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, Utah","doi":"10.3133/ofr80446","issn":"0094-9140","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Razem, A.C., and Bartholoma, S.D., 1980, Digital-computer model of ground-water flow in Tooele Valley, Utah: U.S. Geological Survey Open-File Report 80-446, iv, 55 p., https://doi.org/10.3133/ofr80446.","productDescription":"iv, 55 p.","numberOfPages":"58","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":155065,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0446/report-thumb.jpg"},{"id":53413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0446/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Tooele Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae83","contributors":{"authors":[{"text":"Razem, Allan C.","contributorId":72390,"corporation":false,"usgs":true,"family":"Razem","given":"Allan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":191649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartholoma, Scott D.","contributorId":39408,"corporation":false,"usgs":true,"family":"Bartholoma","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":191648,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24296,"text":"ofr80833 - 1980 - Data on some stratabound Precambrian deposits containing zinc, copper, lead, silver, and gold in the Royal Gorge 15-minute quadrangle, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr80833","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":"80-833","title":"Data on some stratabound Precambrian deposits containing zinc, copper, lead, silver, and gold in the Royal Gorge 15-minute quadrangle, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80833","issn":"0094-9140","usgsCitation":"Raymond, W.H., and Sheridan, D.M., 1980, Data on some stratabound Precambrian deposits containing zinc, copper, lead, silver, and gold in the Royal Gorge 15-minute quadrangle, Colorado: U.S. Geological Survey Open-File Report 80-833, 9 p. :map ;28 cm., https://doi.org/10.3133/ofr80833.","productDescription":"9 p. :map ;28 cm.","costCenters":[],"links":[{"id":155064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0833/report-thumb.jpg"},{"id":53412,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0833/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7fb","contributors":{"authors":[{"text":"Raymond, William H.","contributorId":48555,"corporation":false,"usgs":true,"family":"Raymond","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":191647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheridan, Douglas M.","contributorId":13966,"corporation":false,"usgs":true,"family":"Sheridan","given":"Douglas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":191646,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24295,"text":"ofr80969 - 1980 - Land-surface subsidence in the Texas coastal region","interactions":[],"lastModifiedDate":"2016-08-11T12:10:35","indexId":"ofr80969","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":"80-969","title":"Land-surface subsidence in the Texas coastal region","docAbstract":"Land-surface subsidence has been mapped in the Houston-Galveston area and is known to have occurred in other areas within the Texas coastal region. Most of the subsidence has been caused by both the withdrawal of ground water and by the production of oil, gas, and associated ground water.
\nLand-surface subsidence was determined by comparing adjusted elevations of bench marks for various periods of releveling and by comparing topographic maps of the same areas for different years. In general, most of the Texas coastal region has subsided less than 0.5 foot (0.15 meter). The largest amount of subsidence measured in the region is in the Pasadena-Houston Ship Channel area, where the land surface subsided between 8.5 and 9.0 feet (2.6 and 2.7 meters) during 1906-73. The cause of the subsidence in this area was ground-water withdrawals. Local subsidence caused by sulfur mining in the Moss Bluff Salt Dome area has been reported to exceed 15 feet (4.6 meters).
\nIn Jefferson County, the Spindletop Dome area subsided approximately 5 feet (1.5 meters) during 1925-77, and the Port Acres area subsided about 3 feet (0.9 meter) during 1959-77, mainly from the withdrawal of oil or gas and associated ground water. Local subsidence caused by sulfur mining in the Spindletop Dome area has been estimated to exceed 10 feet (3.0 meters).
\nIn southeastern Jackson County and northwestern Matagorda County, the land surface subsided more than 1.5 feet (0.46 meter) during 1943-73 as a result of ground-water withdrawals. Withdrawals of oil, gas, and associated ground water caused more than 5 feet (1.5 meters) of subsidence during 1942-75 in the western part of Corpus Christi in Nueces County.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr80969","issn":"0094-9140","usgsCitation":"Ratzlaff, K.W., 1980, Land-surface subsidence in the Texas coastal region: U.S. Geological Survey Open-File Report 80-969, Report: iv, 16 p.; 5 Plates: 14.10 x 12.82 inches or smaller, https://doi.org/10.3133/ofr80969.","productDescription":"Report: iv, 16 p.; 5 Plates: 14.10 x 12.82 inches or smaller","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":155050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0969/report-thumb.jpg"},{"id":53406,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0969/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53407,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0969/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53408,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0969/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53409,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0969/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53410,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0969/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0969/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adede","contributors":{"authors":[{"text":"Ratzlaff, Karl W.","contributorId":99177,"corporation":false,"usgs":true,"family":"Ratzlaff","given":"Karl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":191645,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":45899,"text":"ofr80195 - 1980 - Oblique map of the northern California continental margin","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr80195","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":"80-195","title":"Oblique map of the northern California continental margin","language":"ENGLISH","doi":"10.3133/ofr80195","usgsCitation":"Alpha, T.R., and Gerin, M., 1980, Oblique map of the northern California continental margin: U.S. Geological Survey Open-File Report 80-195, 1 map ;81 x 108 cm., https://doi.org/10.3133/ofr80195.","productDescription":"1 map ;81 x 108 cm.","costCenters":[],"links":[{"id":135699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82911,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0195/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696557","contributors":{"authors":[{"text":"Alpha, Tau Rho","contributorId":63371,"corporation":false,"usgs":true,"family":"Alpha","given":"Tau","email":"","middleInitial":"Rho","affiliations":[],"preferred":false,"id":232253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gerin, Marybeth","contributorId":20718,"corporation":false,"usgs":true,"family":"Gerin","given":"Marybeth","email":"","affiliations":[],"preferred":false,"id":232252,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23498,"text":"ofr80639 - 1980 - Irrigated cropland, 1978, Kit Carson, Phillips, and Yuma Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr80639","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":"80-639","title":"Irrigated cropland, 1978, Kit Carson, Phillips, and Yuma Counties, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80639","issn":"0094-9140","usgsCitation":"Johnson, T., 1980, Irrigated cropland, 1978, Kit Carson, Phillips, and Yuma Counties, Colorado: U.S. Geological Survey Open-File Report 80-639, 1 map ;80 x 43 cm., https://doi.org/10.3133/ofr80639.","productDescription":"1 map ;80 x 43 cm.","costCenters":[],"links":[{"id":156677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667270","contributors":{"authors":[{"text":"Johnson, Thomas","contributorId":46566,"corporation":false,"usgs":true,"family":"Johnson","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":190206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}