{"pageNumber":"545","pageRowStart":"13600","pageSize":"25","recordCount":16449,"records":[{"id":10394,"text":"ofr82240 - 1982 - Ground-water applications of remote sensing","interactions":[],"lastModifiedDate":"2017-03-28T13:17:48","indexId":"ofr82240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-240","title":"Ground-water applications of remote sensing","docAbstract":"<p>Remote sensing can be used as a tool to inventory springs and seeps and to interpret lithology, structure, and ground-water occurrence and quality. Thermograms are the best images for inventory of seeps and springs. The steps in aquifer mapping are image analysis and interpretation and ground-water interpretation. A ground-water interpretation is derived from a conceptual geologic model by inferring aquifer characteristics and water salinity. The image selection process is very important for obtaining maximum geologic and hydrologic information from remotely sensed data. Remote sensing can contribute an image base map or geologic and hydrologic parameters, derived from the image, to the multiple data sets in a hydrologic information system. Various merging and integration techniques may then be used to obtain information from these data sets.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82240","usgsCitation":"Moore, G.K., 1982, Ground-water applications of remote sensing: U.S. Geological Survey Open-File Report 82-240, iv, 55 p., https://doi.org/10.3133/ofr82240.","productDescription":"iv, 55 p.","numberOfPages":"61","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":38226,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0240/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0240/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d3dc","contributors":{"authors":[{"text":"Moore, Gerald K.","contributorId":14377,"corporation":false,"usgs":true,"family":"Moore","given":"Gerald","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":161314,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10336,"text":"ofr8231 - 1982 - Water for western oil shale development: Potential local supplies","interactions":[],"lastModifiedDate":"2022-09-23T20:26:58.565482","indexId":"ofr8231","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-31","title":"Water for western oil shale development: Potential local supplies","docAbstract":"<p>Commercial-scale development of western oil shale resources will require a supply of water for both extraction and reclamation purposes. This paper summarizes some of the information on the occurrence of potential local supplies of water in the Piceance Creek Basin-Uinta Basin areas of northwest Colorado and northeast Utah. The discussion is somewhat hypothetical in that it is restricted to the physical occurrence of water with emphasis on water resources in each basin. Of course, the many potential constraints on water use (including economics, water quality, legal and other institutional factors) are necessarily secondary to the ultimate constraint, its physical occurrence. Perhaps the most obvious constraint is that of water rights and water laws. For example, \"mining\" of some of the ground water is herein assumed to be necessary for technically sound management and utilization of the water resource, but the hydrologic effects of such \"mining\" would require accommodation under water laws and agreements.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8231","usgsCitation":"Miller, G., 1982, Water for western oil shale development: Potential local supplies: U.S. Geological Survey Open-File Report 82-31, 6 p., https://doi.org/10.3133/ofr8231.","productDescription":"6 p.","costCenters":[],"links":[{"id":143503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0031/report-thumb.jpg"},{"id":407297,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Piceance Creek Basin, Uinta Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.9893798828125,\n              40.17047886718109\n            ],\n            [\n              -108.2537841796875,\n              40.17047886718109\n            ],\n            [\n              -108.2537841796875,\n              40.925964939514294\n            ],\n            [\n              -110.9893798828125,\n              40.925964939514294\n            ],\n            [\n              -110.9893798828125,\n              40.17047886718109\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa1f2","contributors":{"authors":[{"text":"Miller, G.A.","contributorId":107671,"corporation":false,"usgs":true,"family":"Miller","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":161215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10339,"text":"ofr82774 - 1982 - Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","interactions":[{"subject":{"id":10339,"text":"ofr82774 - 1982 - Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","indexId":"ofr82774","publicationYear":"1982","noYear":false,"title":"Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":2314,"text":"wsp2243 - 1984 - Changes in flood response of the Red River of the North basin, North Dakota-Minnesota","indexId":"wsp2243","publicationYear":"1984","noYear":false,"title":"Changes in flood response of the Red River of the North basin, North Dakota-Minnesota"},"id":1}],"supersededBy":{"id":2314,"text":"wsp2243 - 1984 - Changes in flood response of the Red River of the North basin, North Dakota-Minnesota","indexId":"wsp2243","publicationYear":"1984","noYear":false,"title":"Changes in flood response of the Red River of the North basin, North Dakota-Minnesota"},"lastModifiedDate":"2018-03-09T13:58:25","indexId":"ofr82774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-774","title":"Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","docAbstract":"<p>The magnitude and frequency of large floods that have occurred in recent years in the basin of the Red River of the North have caused concern that land-use changes and manmade drainage have increased flooding. This study was undertaken to determine if any changes in flood response of the Red River basin can be documented. A review of the hydrologic setting, previous floods, flood-control measures, and probable effects of land-use changes shows that the flooding problem of the Red River basin is complex hydrologically, highly variable historically, and follows a regional pattern. Therefore, a change in flood response of the basin is difficult to identify. The flood-frequency, regression, normalized-hydrograph, and double-mass analyses show little indication of significant change in flood response of the Red River basin at locations on the main stem. However, the large variation in flood discharges may mask or dwarf small changes in response of the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82774","usgsCitation":"Miller, J.E., and Frink, D.L., 1982, Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota: U.S. Geological Survey Open-File Report 82-774, viii, 166 p., https://doi.org/10.3133/ofr82774.","productDescription":"viii, 166 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":94967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0774/report.pdf","size":"8340","linkFileType":{"id":1,"text":"pdf"}},{"id":143661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0774/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6cdb","contributors":{"authors":[{"text":"Miller, Jeffrey E.","contributorId":76717,"corporation":false,"usgs":true,"family":"Miller","given":"Jeffrey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frink, Dale L.","contributorId":59421,"corporation":false,"usgs":true,"family":"Frink","given":"Dale","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7412,"text":"ofr82758 - 1982 - A plan for hydrologic investigations of in situ, oil-shale retorting near Rock Springs, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr82758","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-758","title":"A plan for hydrologic investigations of in situ, oil-shale retorting near Rock Springs, Wyoming","docAbstract":"The recovery of shale oil by the in-situ retort process may cause hydrologic impacts, the most significant being ground-water contamination and possible transport of contaminants into surrounding areas. Although these impacts are site-specific, many of the techniques used to investigate each retort operation commonly will be the same. The U.S. Geological Survey has begun a study of hydrologic impacts in the area of an in-situ retort near Rock Springs, Wyoming, as a means of refining and demonstrating these techniques. Geological investigations include determining the areal extent and thickness of aquifers. Emphasis will be placed on determining lithologic variations from geophysical logging. Hydrologic investigations include mapping of potentiometric surfaces, determining rates of ground-water discharge, and estimating aquifer properties by analytical techniques. Water-quality investigations include monitoring solute migration from the retort site and evaluating sampling techniques by standard statistical procedures. A ground-water-flow and solute-transport model will be developed to predict future movement of the water plume away from the retort. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82758","usgsCitation":"Glover, K.C., Zimmerman, E.A., Larson, L.R., and Wallace, J., 1982, A plan for hydrologic investigations of in situ, oil-shale retorting near Rock Springs, Wyoming: U.S. Geological Survey Open-File Report 82-758, iv, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82758.","productDescription":"iv, 30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0758/report-thumb.jpg"},{"id":34812,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0758/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab7a3","contributors":{"authors":[{"text":"Glover, Kent C.","contributorId":53766,"corporation":false,"usgs":true,"family":"Glover","given":"Kent","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":155508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zimmerman, E. A.","contributorId":75533,"corporation":false,"usgs":true,"family":"Zimmerman","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, L. R.","contributorId":41421,"corporation":false,"usgs":true,"family":"Larson","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":155507,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wallace, J.C.","contributorId":25944,"corporation":false,"usgs":true,"family":"Wallace","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":155506,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7490,"text":"ofr82346 - 1982 - Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah","interactions":[],"lastModifiedDate":"2017-09-02T09:55:54","indexId":"ofr82346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-346","title":"Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah","docAbstract":"<p>Six exploratory wells were drilled into the cap rock underlying Salt Valley, Utah, for geologic, geophysical, and hydrologic data to augment information obtained from three previous test wells. Drilling of three other test holes was abandoned due to caving and loss of drilling tools, Before reaching the zone of saturation; the upper 100 meters of cap rock is unsaturated. Within the saturated part of the cap rock, hydraulic heads generally decrease with depth and to the northwest in this part of the valley.</p><p>Hydraulic conductivity of the cap rock, as determined from pumping tests, ranged from 9.3 X 10<sup>-5</sup> to 2.06 X 10<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>-1</sup></span> meters per day; as a result, groundwater flow rates in the cap rock are low. Water ranges from a calcium bicarbonate sulfate type on the western edge of the valley to a calcium magnesium sodium bicarbonate, sulfate, chloride type near the center of the valley. Carbon-14 specific activity for cap-rock water yielded an uncorrected age of about 17,000 to 26,000 years before present near the western edge of the valley and about 41,000 years before present near the center of the valley.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr82346","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Wollitz, L.E., Thordarson, W., Whitfield, M.S., and Weir, J.E., 1982, Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah: U.S. Geological Survey Open-File Report 82-346, vii, 71 p., https://doi.org/10.3133/ofr82346.","productDescription":"vii, 71 p.","numberOfPages":"78","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":140454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0346/report-thumb.jpg"},{"id":34934,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","county":"Grand County","otherGeospatial":"Salt Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e092","contributors":{"authors":[{"text":"Wollitz, Leonard E.","contributorId":22340,"corporation":false,"usgs":true,"family":"Wollitz","given":"Leonard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":155858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whitfield, Merrick S. Jr.","contributorId":67911,"corporation":false,"usgs":true,"family":"Whitfield","given":"Merrick","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155859,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weir, James E. Jr.","contributorId":47419,"corporation":false,"usgs":true,"family":"Weir","given":"James","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155860,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7503,"text":"ofr82916 - 1982 - Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980","interactions":[],"lastModifiedDate":"2017-09-01T14:57:41","indexId":"ofr82916","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-916","title":"Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980","docAbstract":"<p>The Price River basin in east-central Utah includes a significant part of the Wasatch Plateau and Book Cliffs coal-fields area (pi. 1) and currently (1980) is part of the most active coal-mining areas in the State.</p><p>This report presents data gathered by the U.S. Geological Survey as part of a hydrologic study carried out during the water years 1979 and 1980 in cooperation with the U.S. Bureau of Land Management. The data were obtained in the field or from private, State, and other Federal agencies. The purpose of this report is to make the data available to those engaged in coal mining, to those assessing water resources that may possibly be affected by coal mining, and to supplement two interpretive reports that will be published at a later date. Other sources of hydrologic data in the Price River basin include Waddell and others, 1978 and Sumsion, 1979.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr82916","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Waddell, K., Dodge, J., Darby, D., and Theobald, S., 1982, Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980: U.S. Geological Survey Open-File Report 82-916, Report: iv, 73 p.; Plate: 23.85 in. x 22.64 in., https://doi.org/10.3133/ofr82916.","productDescription":"Report: iv, 73 p.; Plate: 23.85 in. x 22.64 in.","numberOfPages":"77","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":34957,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0916/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0916/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0916/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f8830","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":155918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dodge, J.E.","contributorId":21133,"corporation":false,"usgs":true,"family":"Dodge","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":155915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darby, D.W.","contributorId":49333,"corporation":false,"usgs":true,"family":"Darby","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":155916,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Theobald, S.M.","contributorId":51270,"corporation":false,"usgs":true,"family":"Theobald","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":155917,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":6513,"text":"pp1044J - 1982 - Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada","interactions":[{"subject":{"id":53044,"text":"ofr802043 - 1980 - Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada","indexId":"ofr802043","publicationYear":"1980","noYear":false,"title":"Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":6513,"text":"pp1044J - 1982 - Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada","indexId":"pp1044J","publicationYear":"1982","noYear":false,"chapter":"J","title":"Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada"},"id":1}],"lastModifiedDate":"2025-04-17T17:04:29.694949","indexId":"pp1044J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1044","chapter":"J","title":"Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044J","usgsCitation":"Young, H., and Lewis, R., 1982, Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada: U.S. Geological Survey Professional Paper 1044, Report: 20 p.;  2 Plates: 20.50 x 25.00 inches and 21.00 x 25.00 inches, https://doi.org/10.3133/pp1044J.","productDescription":"Report: 20 p.;  2 Plates: 20.50 x 25.00 inches and 21.00 x 25.00 inches","costCenters":[],"links":[{"id":33978,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044j/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33977,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33979,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":484685,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4699.htm","linkFileType":{"id":5,"text":"html"}},{"id":118022,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044j/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605128","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":152850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, R.E.","contributorId":31735,"corporation":false,"usgs":true,"family":"Lewis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":152849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7694,"text":"ofr82374 - 1982 - Hydrologic data-verification management program plan","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82374","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-374","title":"Hydrologic data-verification management program plan","docAbstract":"Data verification refers to the performance of quality control on hydrologic data that have been retrieved from the field and are being prepared for dissemination to water-data users. Water-data users now have access to computerized data files containing unpublished, unverified hydrologic data. Therefore, it is necessary to develop techniques and systems whereby the computer can perform some data-verification functions before the data are stored in user-accessible files. Computerized data-verification routines can be developed for this purpose. A single, unified concept describing master data-verification program using multiple special-purpose subroutines, and a screen file containing verification criteria, can probably be adapted to any type and size of computer-processing system. Some traditional manual-verification procedures can be adapted for computerized verification, but new procedures can also be developed that would take advantage of the powerful statistical tools and data-handling procedures available to the computer. Prototype data-verification systems should be developed for all three data-processing environments as soon as possible. The WATSTORE system probably affords the greatest opportunity for long-range research and testing of new verification subroutines. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82374","usgsCitation":"Alexander, C., 1982, Hydrologic data-verification management program plan: U.S. Geological Survey Open-File Report 82-374, iv, 25 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82374.","productDescription":"iv, 25 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0374/report-thumb.jpg"},{"id":35158,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0374/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6072a5","contributors":{"authors":[{"text":"Alexander, C.W.","contributorId":76745,"corporation":false,"usgs":true,"family":"Alexander","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":156451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7738,"text":"ofr821023 - 1982 - Selected hydrologic data for northern Utah Valley, Utah, 1935-82","interactions":[],"lastModifiedDate":"2022-09-19T22:17:45.843729","indexId":"ofr821023","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1023","title":"Selected hydrologic data for northern Utah Valley, Utah, 1935-82","docAbstract":"<p>This report contains hydrologic data collected in northern Utah Valley from 1935 to 1982. Northern Utah Valley is approximately the northern half of an alluvial-filled basin partly occupied by Utah Lake in north-central Utah. The report area is bounded by the Wasatch Range on the east, the Lake Mountains on the west, and the Traverse Mountains on the north. Its southern boundary is the boundary between Townships 7 and 8 south, Salt Lake Base Line and Meridian.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821023","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Appel, C.L., Clark, D.W., and Fairbanks, P.E., 1982, Selected hydrologic data for northern Utah Valley, Utah, 1935-82: U.S. Geological Survey Open-File Report 82-1023, Report: iv, 97 p.; 1 Plate: 19.07 x 23.94 inches, https://doi.org/10.3133/ofr821023.","productDescription":"Report: iv, 97 p.; 1 Plate: 19.07 x 23.94 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":407017,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407016,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1023/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1023/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Utah Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.96441650390625,\n              40.054949943999496\n            ],\n            [\n              -111.62384033203124,\n              40.054949943999496\n            ],\n            [\n              -111.62384033203124,\n              40.44276659332215\n            ],\n            [\n              -111.96441650390625,\n              40.44276659332215\n            ],\n            [\n              -111.96441650390625,\n              40.054949943999496\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"This report was also published as Utah Hydrologic Data Report 39","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a144","contributors":{"authors":[{"text":"Appel, Cynthia L.","contributorId":34509,"corporation":false,"usgs":true,"family":"Appel","given":"Cynthia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":156517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":156519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fairbanks, Paul E.","contributorId":66254,"corporation":false,"usgs":true,"family":"Fairbanks","given":"Paul","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":156518,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7747,"text":"ofr82698 - 1982 - Evaluation of the hydrologic system in the New Leipzig coal area, Grant and Hettinger counties, North Dakota","interactions":[],"lastModifiedDate":"2018-05-23T12:06:02","indexId":"ofr82698","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-698","title":"Evaluation of the hydrologic system in the New Leipzig coal area, Grant and Hettinger counties, North Dakota","docAbstract":"Aquifers in the New Leipzig coal area consist of sandstone beds in the Fox Hills Sandstone, the Hell Creek Formation, the Cannonball and Ludlow Members of the Fort Union Formation, and the basal part of the Tongue River Member of the Fort Union Formation. Aquifers also occur in sandstone and lignite beds in the upper part of the Tongue River Member and Sentinel Butte Member of the Fort Union Formation. Potential well yields from each of the aquifers are variable, but are less than 100 gallons per minute. Water in the Fox Hills, Hell Creek, Cannonball, and Ludlow is soft and of the sodium bicarbonate type. Water in basal Tongue River aquifer is either soft or very hard and generally is of the sodium bicarbonate type. Water in the upper Tongue River and Sentinel Butte aquifer system is very hard and generally is either of the calcium bicarbonate or sodium bicarbonate type. There is little or no contribution of ground water to Thirty Mile Creek or the Cannonball River from the area of minable coal. Coal mining will expose sulfide minerals to oxidation, and result in an increase in dissolved solids and sulfate in water in the basal Tongue River aquifer. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82698","usgsCitation":"Armstrong, C.A., 1982, Evaluation of the hydrologic system in the New Leipzig coal area, Grant and Hettinger counties, North Dakota: U.S. Geological Survey Open-File Report 82-698, 46 p., 3 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82698.","productDescription":"46 p., 3 over-size sheets, ill., maps ;28 cm.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":35212,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0698/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35208,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0698/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35209,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0698/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0698/report-thumb.jpg"},{"id":35210,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0698/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35211,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0698/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa27e","contributors":{"authors":[{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156532,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7758,"text":"ofr82326 - 1982 - Background hydrologic information in potential lignite mining areas in Mississippi, August 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82326","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-326","title":"Background hydrologic information in potential lignite mining areas in Mississippi, August 1981","docAbstract":"The U.S. Geological Survey in cooperation with the Mississippi Bureau of Geology is conducting a hydrologic data-collection program in potential lignite-producing areas in Mississippi. During the period August 24-31, 1981, hydrologic data consisting of channel characteristics and stream discharge were collected at 18 sites, and water and channel bottom material samples were collected at 15 sites on small streams draining potential lignite mining areas in east-central Mississippi. Main channel widths ranged from 100 feet on Mill Creek near Louisville to 30 feet on Spring Creek near Bond. Maximum water depths varied from 12.5 feet on Pawticfaw Creek to 0.2 foot on Beasha Creek. Three sites had no discharge. Specific conductance ranged from 100 micromhos on Lonsilocher Canal near Philadelphia to 24 micromhos on Jofuska Creek near Arlington. Water temperatures varied from 22.5 to 26 degrees Celsius. The highest pH was 7.6 on Fulton and Lonsilocher Canals. The dissolved oxygen concentration was 3.8 milligrams per liter or higher at all sites. Channel bottom-material samples commonly contained iron, manganese, and zinc. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82326","usgsCitation":"Arthur, J.K., 1982, Background hydrologic information in potential lignite mining areas in Mississippi, August 1981: U.S. Geological Survey Open-File Report 82-326, iii, 19 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82326.","productDescription":"iii, 19 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0326/report-thumb.jpg"},{"id":35233,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0326/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67afe0","contributors":{"authors":[{"text":"Arthur, J. K.","contributorId":56223,"corporation":false,"usgs":true,"family":"Arthur","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":156549,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11489,"text":"ofr811007 - 1982 - Surface-water-quality data from selected sites in Washington affected by Mount St. Helens eruptions; March 27 - September 30, 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr811007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1007","title":"Surface-water-quality data from selected sites in Washington affected by Mount St. Helens eruptions; March 27 - September 30, 1980","docAbstract":"The volcanic eruptions of Mount St. Helens have resulted in the collection of many forms of hydrologic data. Chemical data collected from March 27 to September 30, 1980, to document the effects of the various volcanic events (mudflows, pyroclastic flows, deposition of ash) on the quality of surface water at selected sites in the State of Washington are presented in the report. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811007","usgsCitation":"Turney, G.L., and Klein, J., 1982, Surface-water-quality data from selected sites in Washington affected by Mount St. Helens eruptions; March 27 - September 30, 1980: U.S. Geological Survey Open-File Report 81-1007, iii, 158 p. :map ;28 cm., https://doi.org/10.3133/ofr811007.","productDescription":"iii, 158 p. :map ;28 cm.","costCenters":[],"links":[{"id":146578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1007/report-thumb.jpg"},{"id":39360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a551","contributors":{"authors":[{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klein, J.M.","contributorId":44550,"corporation":false,"usgs":true,"family":"Klein","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":163229,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7926,"text":"ofr82152 - 1982 - Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-152","title":"Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year","docAbstract":"This report contains data on the physical and chemical properties measured in the Tidal Potomac River and Estuary during the 1980 Water Year. Data were collected routinely at five stations, and periodically at 17 stations including three stations near the mouth of the Potomac River in Chesapeake Bay. Each of the five stations represent a cross section through which the transport of selected dissolved and suspended materials can be computed. The remaining stations represent locations at which data were collected for special synoptic studies such as salt water migration, and dissolved oxygen dynamics. Routinely, samples were analyzed for silica, nitrogen, phosphorus, chlorophyll-a, pheophytin, and suspended sediment. Additional samples were analyzed for organic carbon, calcium, manganese, magnesium, sodium, alkalinity, sulfate, iron, potassium, chloride, fluoride, seston, algal growth potential, adenosine triphosphate, nitrifying bacteria and dissolved-solids residue. In addition, solar radiation measurements and in-situ measurements of dissolved oxygen, specific conductance, pH, temperature, and Secchi disk transparency are reported. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82152","usgsCitation":"Blanchard, S., Coupe, R., and Woodward, J., 1982, Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year: U.S. Geological Survey Open-File Report 82-152, i, 335 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82152.","productDescription":"i, 335 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0152/report-thumb.jpg"},{"id":35490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8882","contributors":{"authors":[{"text":"Blanchard, Stephen","contributorId":6852,"corporation":false,"usgs":true,"family":"Blanchard","given":"Stephen","affiliations":[],"preferred":false,"id":156845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coupe, R.H. Jr.","contributorId":84755,"corporation":false,"usgs":true,"family":"Coupe","given":"R.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":156847,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodward, J.C.","contributorId":62590,"corporation":false,"usgs":true,"family":"Woodward","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":156846,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20415,"text":"ofr82696 - 1982 - Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr82696","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-696","title":"Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79","docAbstract":"This report summarizes data collected by the U.S. Geological Survey for the U.S. Department of Energy, Naval Petroleum, and Oil Shale Reserves in the Parachute Creek drainage basin of western Colorado. It includes data from five surface-water gages, two automatic sediment samplers and two water-quality monitors. Instantaneous streamflow measurements were made at 63 sites on Parachute Creek tributaries to determine gain or loss of flow. Thirteen springs and nine surface-water sites were sampled and chemical analyses of these sites are included. From 1975 to 1979, 88 spring sites were inventoried; conductivity, temperature, pH, and discharge were measured. Climate data include maximum, minimum, and total daily solar radiation. Daily total precipitation is reported for three stations and snow-course data is reported for one site.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82696","usgsCitation":"Patt, R.O., Adams, D.B., and Collins, D.L., 1982, Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79: U.S. Geological Survey Open-File Report 82-696, v, 134 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82696.","productDescription":"v, 134 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0696/report-thumb.jpg"},{"id":49957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0696/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6077cc","contributors":{"authors":[{"text":"Patt, Ralph O.","contributorId":61450,"corporation":false,"usgs":true,"family":"Patt","given":"Ralph","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":182611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, D. Briane","contributorId":35707,"corporation":false,"usgs":true,"family":"Adams","given":"D.","email":"","middleInitial":"Briane","affiliations":[],"preferred":false,"id":182610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, Dannie L.","contributorId":77925,"corporation":false,"usgs":true,"family":"Collins","given":"Dannie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182612,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7961,"text":"ofr82639 - 1982 - Hydrologic data collected in and around a surface coal mine, Clay and Vigo counties, Indiana, 1977-80","interactions":[],"lastModifiedDate":"2016-05-06T14:39:43","indexId":"ofr82639","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-639","title":"Hydrologic data collected in and around a surface coal mine, Clay and Vigo counties, Indiana, 1977-80","docAbstract":"<p>Few data are available for evaluating water-quality and other hydrologic properties in and around surface coal mines, particularly in areas where material having a high potential for acid-production is selectively buried. This report contains hydrologic data collected in an active coal mining area in Clay and Vigo Counties, Indiana, from September 1977 through February 1980. Methods of sampling and analysis used in collecting the data also are summarized. The data include field and laboratory measurements of water at 41 wells and 24 stream sites. Variables measured in the field include water temperature, specific conductance, pH, Eh, dissolved oxygen, ground-water levels, and streamflow; and in the laboratory, concentrations of major ions, alkalinity, hardness, trace elementsl, organic carbon, phosphorus, and dissolved solids. Other variables measured in the laboratory include ferrous iron concentration of water samples from selected wells, percent sulfur by weight and the potential acidity of core samples of reclaimed cast overburden, concentrations of elements absorbed on streambed materials, concentrations and particle size of suspended sediment in water, and populations and Shannon diversity indices of phytoplankton in water. Dissolved-solids concentrations and pH of ground water ranged from 173 to 5,130 milligrams per liter and from 6.1 to 8.9, respectively, and of surface water, from 120 to 4,100 milligrams per liter and from 6.1 to 8.8 respectively.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82639","usgsCitation":"Bobo, L.L., and Eikenberry, S.E., 1982, Hydrologic data collected in and around a surface coal mine, Clay and Vigo counties, Indiana, 1977-80: U.S. Geological Survey Open-File Report 82-639, vii, 123 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82639.","productDescription":"vii, 123 p. :ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":140240,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0639/report-thumb.jpg"},{"id":35533,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0639/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Clay, Vigo","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.1992,39.6082],[-87.1233,39.6063],[-87.011,39.6041],[-87.0116,39.5176],[-87.0125,39.4736],[-86.9404,39.4734],[-86.9426,39.3424],[-87.014,39.3426],[-87.0532,39.3433],[-87.0549,39.1701],[-87.1267,39.1702],[-87.2383,39.1728],[-87.238,39.2607],[-87.3485,39.2605],[-87.4578,39.2606],[-87.572,39.261],[-87.6011,39.2612],[-87.6023,39.2626],[-87.6032,39.2638],[-87.6031,39.267],[-87.603,39.2694],[-87.6018,39.2724],[-87.6012,39.2744],[-87.602,39.2768],[-87.6034,39.2783],[-87.6048,39.28],[-87.6057,39.2811],[-87.6062,39.2838],[-87.6068,39.2852],[-87.6068,39.2874],[-87.6049,39.2901],[-87.6031,39.2924],[-87.6006,39.2946],[-87.5988,39.2968],[-87.5981,39.2991],[-87.5987,39.3011],[-87.599,39.3016],[-87.5999,39.3034],[-87.6023,39.3047],[-87.6047,39.3052],[-87.6089,39.3047],[-87.6118,39.3042],[-87.6148,39.3042],[-87.616,39.3044],[-87.617,39.3048],[-87.6182,39.3061],[-87.6181,39.308],[-87.6169,39.3089],[-87.6149,39.3096],[-87.6141,39.3098],[-87.6107,39.3106],[-87.6078,39.3116],[-87.6061,39.3128],[-87.6036,39.3155],[-87.5993,39.3218],[-87.595,39.3267],[-87.5941,39.328],[-87.5925,39.3303],[-87.5901,39.3334],[-87.5876,39.3361],[-87.585,39.3385],[-87.5826,39.3402],[-87.582,39.3405],[-87.5803,39.3412],[-87.5767,39.3426],[-87.5726,39.3431],[-87.5666,39.3426],[-87.5645,39.3424],[-87.5595,39.342],[-87.5588,39.342],[-87.5565,39.3423],[-87.5547,39.3428],[-87.5518,39.3437],[-87.55,39.3451],[-87.5482,39.3474],[-87.5479,39.3479],[-87.5471,39.3492],[-87.5465,39.3509],[-87.5455,39.3522],[-87.5449,39.3529],[-87.5442,39.3533],[-87.5418,39.3542],[-87.5411,39.3544],[-87.5401,39.3544],[-87.539,39.354],[-87.537,39.3529],[-87.5348,39.3517],[-87.5322,39.3507],[-87.5304,39.3516],[-87.5308,39.4178],[-87.5307,39.4388],[-87.5309,39.4767],[-87.5309,39.5615],[-87.531,39.5988],[-87.5311,39.6091],[-87.4607,39.6096],[-87.3819,39.6093],[-87.349,39.6091],[-87.2356,39.6089],[-87.1992,39.6082]]]},\"properties\":{\"name\":\"Clay\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f7c1","contributors":{"authors":[{"text":"Bobo, Linda L.","contributorId":104053,"corporation":false,"usgs":true,"family":"Bobo","given":"Linda","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":156893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eikenberry, Stephen E.","contributorId":35309,"corporation":false,"usgs":true,"family":"Eikenberry","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":156892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8149,"text":"ofr82863 - 1982 - Hydrology of the low-level radioactive solid waste burial site and vicinity near Barnwell, South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T13:04:30","indexId":"ofr82863","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-863","title":"Hydrology of the low-level radioactive solid waste burial site and vicinity near Barnwell, South Carolina","docAbstract":"Geologic and hydrologic conditions at a burial site for low-level radioactive waste were studied, and migration of leachates from the buried waste into surrounding unconsolidated sediments were evaluated. The burial site and vicinity are underlain by a sequence of unconsolidated sediments of Late Cretaceous, Tertiary, and Quaternary age. These sediments are deposited over a graben which has been filled with sedimentary rocks of Triassic age. \r\n\r\nHydraulic properties of the sediments beneath the burial site were determined by laboratory and field tests. Laboratory hydraulic conductivity values ranged from about 10^-7 to 10^-1 feet per day for the clayey sediments to nearly 22 feet per day for aquifer sands. Field aquifer tests indicate a transmissivity of about 22,000 feet squared per day for Cretaceous sediments and about 6,000 feet squared per day for Tertiary sediments. Aquifer tests indicate heterogeneity in the upper 200 feet of the Tertiary sediments. \r\n\r\nWater samples were analyzed from 51 wells, 5 streams, a Carolina bay, and rainfall at the burial site. The total dissolved solids of the ground water ranged from about 7 to 40 milligrams per liter in the upper clayey sediments to about 150 milligrams per liter in the water in the deeper calcareous sediments. The pH of the ground water ranges from 4.8 to 6.5. This slightly acidic water is corrosive to buried metal. \r\n\r\nTritium activity greater than background was detected in sediment cores taken from drill holes adjacent to the burial trenches. High tritium activity occurred at depths above the trench floor. This indicates upward movement of water or vapor to the land surface. Tritium and organic constituents greater than background concentrations were observed in a monitoring well about 10 feet from a trench, indicating lateral migration of radionuclides from the buried waste. Traces of cobalt-60 and tritium greater than background activity were observed in sediment cores collected 5.8 feet beneath the trench floor at one site.\r\n\r\nA hydrologic model was used to simulate ground-water flow in the study area. Based on the model results the minimum time of travel for ground water to move from the burial site to the nearest stream, Marys Branch Creek, is about 50 years. Radionuclides will move more slowly than the water, and will diminish in activity, because of dispersion and radioactive decay.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82863","usgsCitation":"Cahill, J.M., 1982, Hydrology of the low-level radioactive solid waste burial site and vicinity near Barnwell, South Carolina: U.S. Geological Survey Open-File Report 82-863, viii, 109 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82863.","productDescription":"viii, 109 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":141469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0863/report-thumb.jpg"},{"id":35757,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0863/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","city":"Barnwell","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-81.2198,33.4393],[-81.2148,33.3902],[-81.2215,33.2295],[-81.2176,33.2209],[-81.224,33.1581],[-81.2119,33.1476],[-81.2069,33.1344],[-81.1943,33.1231],[-81.2304,33.1176],[-81.2442,33.1189],[-81.2589,33.1134],[-81.2836,33.1083],[-81.3652,33.1081],[-81.4354,33.1297],[-81.4519,33.1346],[-81.5123,33.1503],[-81.5419,33.1579],[-81.5708,33.1332],[-81.6142,33.0953],[-81.6187,33.0952],[-81.6241,33.0946],[-81.6268,33.0941],[-81.6323,33.0928],[-81.6362,33.0924],[-81.6395,33.0923],[-81.6428,33.0928],[-81.6466,33.0937],[-81.6494,33.0949],[-81.6532,33.0973],[-81.6536,33.0977],[-81.6569,33.1009],[-81.6611,33.1041],[-81.6621,33.1046],[-81.667,33.1072],[-81.6752,33.1099],[-81.6851,33.1135],[-81.6961,33.1161],[-81.6993,33.1166],[-81.7016,33.117],[-81.7025,33.1172],[-81.7053,33.1183],[-81.7076,33.1188],[-81.7098,33.1207],[-81.7126,33.1224],[-81.7162,33.1243],[-81.7189,33.1252],[-81.7211,33.1257],[-81.7236,33.1278],[-81.7263,33.13],[-81.7297,33.1332],[-81.7352,33.1368],[-81.7407,33.1409],[-81.7428,33.1424],[-81.7479,33.1463],[-81.7545,33.1517],[-81.759,33.1557],[-81.7622,33.1599],[-81.7648,33.1649],[-81.767,33.1708],[-81.7673,33.1716],[-81.7691,33.1758],[-81.7701,33.1777],[-81.7701,33.1795],[-81.7689,33.1808],[-81.7674,33.1817],[-81.7669,33.183],[-81.7669,33.1839],[-81.7673,33.1864],[-81.7662,33.1877],[-81.7655,33.1881],[-81.7636,33.1894],[-81.762,33.1903],[-81.7615,33.1907],[-81.7609,33.1913],[-81.7588,33.1931],[-81.7577,33.1949],[-81.7573,33.1972],[-81.7575,33.1982],[-81.5165,33.3824],[-81.373,33.4907],[-81.3399,33.4831],[-81.3251,33.485],[-81.3047,33.48],[-81.2738,33.4637],[-81.2463,33.4442],[-81.2198,33.4393]]]},\"properties\":{\"name\":\"Barnwell\",\"state\":\"SC\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697917","contributors":{"authors":[{"text":"Cahill, James M.","contributorId":55432,"corporation":false,"usgs":true,"family":"Cahill","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":157229,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":250,"text":"wsp2180 - 1982 - Summary of hydrologic testing in Tertiary limestone aquifer, Tenneco offshore exploratory well--Atlantic OCS, lease-block 427 (Jacksonville NH 17-5)","interactions":[{"subject":{"id":12324,"text":"ofr80558 - 1980 - Summary of hydrologic testing in Tertiary limestone aquifer, Tenneco offshore exploratory well-Atlantic OCS, lease block 427 (Jacksonville NH-17-5)","indexId":"ofr80558","publicationYear":"1980","noYear":false,"title":"Summary of hydrologic testing in Tertiary limestone aquifer, Tenneco offshore exploratory well-Atlantic OCS, lease block 427 (Jacksonville NH-17-5)"},"predicate":"SUPERSEDED_BY","object":{"id":250,"text":"wsp2180 - 1982 - Summary of hydrologic testing in Tertiary limestone aquifer, Tenneco offshore exploratory well--Atlantic OCS, lease-block 427 (Jacksonville NH 17-5)","indexId":"wsp2180","publicationYear":"1982","noYear":false,"title":"Summary of hydrologic testing in Tertiary limestone aquifer, Tenneco offshore exploratory well--Atlantic OCS, lease-block 427 (Jacksonville NH 17-5)"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"wsp2180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2180","title":"Summary of hydrologic testing in Tertiary limestone aquifer, Tenneco offshore exploratory well--Atlantic OCS, lease-block 427 (Jacksonville NH 17-5)","docAbstract":"A summary of hydrologic testing in an offshore oil-test well (LB427) drilled for Tenneco, Inc., 55 miles east of Fernandina Beach, Florida, is presented. The interval tested (1,050 to 1,070 feet below sea level) is in a calcarenite that is equivalent to the Ocala Limestone (late Eocene) of onshore Florida and South Georgia. At this site the Ocala forms the highly productive Tertiary limestone aquifer system of the southeastern United States. Pressure-head measurements indicate an equivalent freshwater head of 24 to 29 feet above sea level. These pressure-head measurements and an earlier one made in the nearby JOIDES J- I hole are the only hydraulic head determinations to date in the offshore extensions of any of the aquifers underlying the Atlantic coastal plain. \r\n\r\nA drill-stem test recovered water samples containing about 7,000 milligrams per liter chloride. However, seawater used in the drilling process apparently contaminated the samples and the formation water is considered slightly fresher. \r\n\r\nThe head and salinity data from the Tenneco well suggest that the sampled interval lies in the transition zone between fresh and seawater in the limestone aquifer. These data, when viewed with similar data from JOIDES J-I, show the transition zone to slope very slightly landward. The interface position is probably intermediate between a position compatible with present-day heads and a position compatible with predevelopment heads.","language":"ENGLISH","doi":"10.3133/wsp2180","usgsCitation":"Johnston, R.H., Bush, P.W., Krause, R.E., Miller, J.A., and Sprinkle, C.L., 1982, Summary of hydrologic testing in Tertiary limestone aquifer, Tenneco offshore exploratory well--Atlantic OCS, lease-block 427 (Jacksonville NH 17-5): U.S. Geological Survey Water Supply Paper 2180, iii, 15 p. : ill., map ; 28 cm., https://doi.org/10.3133/wsp2180.","productDescription":"iii, 15 p. : ill., map ; 28 cm.","costCenters":[],"links":[{"id":136616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2180/report-thumb.jpg"},{"id":24856,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699034","contributors":{"authors":[{"text":"Johnston, Richard H.","contributorId":95860,"corporation":false,"usgs":true,"family":"Johnston","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":142148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":142147,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krause, Richard E.","contributorId":40185,"corporation":false,"usgs":true,"family":"Krause","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":142144,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, James A.","contributorId":49772,"corporation":false,"usgs":true,"family":"Miller","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":142146,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sprinkle, Craig L.","contributorId":41802,"corporation":false,"usgs":true,"family":"Sprinkle","given":"Craig","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142145,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":8193,"text":"ofr82681 - 1982 - Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82681","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-681","title":"Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana","docAbstract":"The Cook Creek area of the Ashland coal field contains large reserves of Federally owned coal that have been identified for potential lease sale. A hydrologic study has been conducted in the potential lease area to describe existing hydrologic systems and to assess potential impacts of surface coal mining on local water resources. Hydrogeologic data collected from wells, springs, and drill holes indicate that shallow aquifers exist within the Tongue River Member of the Fort Union Formation (Paleocene age) and within valley alluvium (Pleistocene and Holocene age). Shallow aquifers within the Tonge River Member include coal beds, clinker, and lenses of sandstone and siltstone. The Knobloch coal bed, a principal shallow aquifer used for livestock watering in the area, averages about 55 feet in thickness and is completely saturated throughout most of its extent. Coarse alluvial deposits are the most productive aquifers and are a major source of stock water in the Cook Creek basin. Surface-water resources are limited to the upstream reach part of Cook Creek, which flows intermittently. The downstream reach part of Cook Creek, plus all other small drainages that originate in the study area, are ephemeral. Mining of the Knoblock and Sawyer coal beds would remove two alluvial springs, one bedrock spring, and two wells, which are all used for watering of livestock. The potentiometric surface within the Knobloch coal aquifer and the alluvial aquifer in the downstream part of the Cook Creek basin would be lowered during mining. Lowered water levels in these aquifers might substantially affect water levels in five wells outside the mine boundary. After mining, the alluvial aquifer downgradient from the mine area might show a long-term degradation in water quality as a result of leaching of soluble salts from overburden materials used to backfill mine pits. Although mining would alter the existing hydrologic systems and remove several springs and shallow wells, alternative ground-water supplies are available that could be developed to replace those lost by mining. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82681","usgsCitation":"Cannon, M.R., 1982, Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana: U.S. Geological Survey Open-File Report 82-681, 34 p., 2 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82681.","productDescription":"34 p., 2 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0681/report-thumb.jpg"},{"id":35805,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0681/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35806,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0681/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0681/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683848","contributors":{"authors":[{"text":"Cannon, M. R.","contributorId":99140,"corporation":false,"usgs":true,"family":"Cannon","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11720,"text":"ofr811180 - 1982 - Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr811180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1180","title":"Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida","docAbstract":"This report provides results of reliability and cost-effective studies of the goes satellite data-collection system used to operate a small hydrologic data network in west-central Florida. The GOES system, in its present state of development, was found to be about as reliable as conventional methods of data collection. Benefits of using the GOES system include some cost and manpower reduction, improved data accuracy, near real-time data availability, and direct computer storage and analysis of data. The GOES system could allow annual manpower reductions of 19 to 23 percent with reduction in cost for some and increase in cost for other single-parameter sites, such as streamflow, rainfall, and ground-water monitoring stations. Manpower reductions of 46 percent or more appear possible for multiple-parameter sites. Implementation of expected improvements in instrumentation and data handling procedures should further reduce costs. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811180","usgsCitation":"Woodham, W.M., 1982, Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida: U.S. Geological Survey Open-File Report 81-1180, iv, 27 p., map ;28 cm., https://doi.org/10.3133/ofr811180.","productDescription":"iv, 27 p., map ;28 cm.","costCenters":[],"links":[{"id":143920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1180/report-thumb.jpg"},{"id":39606,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3a6","contributors":{"authors":[{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8220,"text":"ofr82457 - 1982 - Volcano-tectonic history of Crater Flat, southwestern Nevada, as suggested by new evidence from drill hole USW-VH-1 and vicinity","interactions":[],"lastModifiedDate":"2021-10-13T18:08:27.092236","indexId":"ofr82457","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-457","title":"Volcano-tectonic history of Crater Flat, southwestern Nevada, as suggested by new evidence from drill hole USW-VH-1 and vicinity","docAbstract":"New evidence for a possible resurgent dome in the caldera related to eruption of the Bullfrog Member of the Crater Flat Tuff has been provided by recent drilling of a 762-meter (2,501-foot) hole in central Crater Flat. Although no new volcanic units were penetrated by the drill hole (USW-VH-1), the positive aeromagnetic anomaly in the vicinity of the drill hole appears to result in part from the unusually thick, densely welded tuff of the Bullfrog. Major units penetrated include alluvium, basalt of Crater Flat, Tiva Canyon and Topopah Spring Members of the Paintbrush Tuff, and Prow Pass and Bullfrog Members of the Crater Flat Tuff. \r\n\r\nIn addition, the drill hole provided the first subsurface hydrologic information for the area. The water table in the hole is at about 180 meters (600 feet), and the temperature gradient appears slightly higher than normal for the region.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82457","usgsCitation":"Carr, W.J., 1982, Volcano-tectonic history of Crater Flat, southwestern Nevada, as suggested by new evidence from drill hole USW-VH-1 and vicinity: U.S. Geological Survey Open-File Report 82-457, ii, 25 p., https://doi.org/10.3133/ofr82457.","productDescription":"ii, 25 p.","costCenters":[],"links":[{"id":35850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0457/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390476,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13731.htm"},{"id":141328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0457/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Crater Flat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.6340,\n              36.667\n            ],\n            [\n              -116.4780,\n              36.667\n            ],\n            [\n              -116.4780,\n              36.871\n            ],\n            [\n              -116.6340,\n              36.871\n            ],\n            [\n              -116.6340,\n              36.667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd71b","contributors":{"authors":[{"text":"Carr, W. J.","contributorId":9245,"corporation":false,"usgs":true,"family":"Carr","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8235,"text":"ofr82273 - 1982 - Selected hydrologic and climatologic data from the Prairie Dog Creek basin, southeastern Montana, water year 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr82273","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-273","title":"Selected hydrologic and climatologic data from the Prairie Dog Creek basin, southeastern Montana, water year 1980","docAbstract":"Hydrologic and climatologic data are being collected in a 25-square-mile (65-square-kilometer) basin in southeastern Montana to provide a base for development, calibration, and verification of a precipitation-runoff model. The study area and data-collection stations within the area are shown on a map. A summary of data collected at each station during the second year , beginning in October 1979, is provided in tables. The data include precipitation, snow depth and water content, air temperature, relative humidity, wind speed and direction, solar radiation, soil temperature and moisture, stream discharge, chemical analyses of water, and suspended sediment. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82273","usgsCitation":"Cary, L.E., and Johnson, J., 1982, Selected hydrologic and climatologic data from the Prairie Dog Creek basin, southeastern Montana, water year 1980: U.S. Geological Survey Open-File Report 82-273, iv, 78 p. :maps ;28 cm., https://doi.org/10.3133/ofr82273.","productDescription":"iv, 78 p. :maps ;28 cm.","costCenters":[],"links":[{"id":141309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0273/report-thumb.jpg"},{"id":35854,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0273/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f925e","contributors":{"authors":[{"text":"Cary, L. E.","contributorId":47369,"corporation":false,"usgs":true,"family":"Cary","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, J.D.","contributorId":71166,"corporation":false,"usgs":true,"family":"Johnson","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":157396,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8252,"text":"ofr8340 - 1982 - Activities in Idaho; status of projects, fiscal years 1982-83","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr8340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-40","title":"Activities in Idaho; status of projects, fiscal years 1982-83","docAbstract":"Twenty-three projects were conducted by the Water Resources Division of the U.S. Geological Survey in Idaho during FY 's (fiscal year) 1982-83. These projects were done in cooperation with seven State and local and nine federal agencies. State and local cooperative funding amounted to $566,123 in FY 1982 and $570,000 (projected monies) in FY 1983; Federal funding amounted to $2,083,748 in FY 1982 and $1,656,494 (projected monies) in FY 1983. Eighty-three persons were employed as of September, FY 1982--40 full time and 43 other than full time. Sixty-five persons were employed as of October, FY 1983--35 full time and 30 other than full time. In addition, the Water Resources Division maintains a project office at the Idaho National Engineering Laboratory. Work there is done in cooperation with the U.S. Department of Energy, which provides most of the funding. Some Federal funds are provided for special projects. Projects other than continuing programs for collection of hydrologic data included flood-mapping studies, geothermal-resource investigations, groundwater-quality assessments, basin-and region-wide water-resource investigations , river quality-of-water monitoring studies, volcanic-ash-related studies, groundwater trends and stream gaging-program evaluations, river erosion and sediment-transport studies, water-budget and groundwater-use determinations, and a sole-source aquifer appraisal. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8340","usgsCitation":"Channel, L.K., 1982, Activities in Idaho; status of projects, fiscal years 1982-83: U.S. Geological Survey Open-File Report 83-40, 48 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr8340.","productDescription":"48 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0040/report-thumb.jpg"},{"id":35868,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0040/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544759","contributors":{"authors":[{"text":"Channel, Linda K. (compiler)","contributorId":35734,"corporation":false,"usgs":true,"family":"Channel","given":"Linda","suffix":"(compiler)","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":157427,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8363,"text":"ofr82361 - 1982 - Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr82361","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-361","title":"Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida","docAbstract":"Hydrologic, geologic, and water-quality data collected in Escambia County, Florida, October 1962 through September 1980 are presented. The data were collected by the U.S. Geological Survey as part of a cooperative investigation with the city of Pensacola and Escambia County to provide information on the quality and quantity of water available from the sand-and-gravel aquifer and selected surface-water sites in Escambia County. Ground-water data include records of 440 wells, chemical and physical analyses of water quality for 325 wells, 6 long-term hydrographs, and 19 lithologic logs. Surface-water data include streamflow measurements and analyses of water collected at 9 sites. Maps of the county show the locations of the data-collection sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82361","usgsCitation":"Coffin, J., 1982, Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida: U.S. Geological Survey Open-File Report 82-361, 136 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82361.","productDescription":"136 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0361/report-thumb.jpg"},{"id":35935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0361/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980e9","contributors":{"authors":[{"text":"Coffin, J.E.","contributorId":75913,"corporation":false,"usgs":true,"family":"Coffin","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":157598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8404,"text":"ofr82680 - 1982 - Support by the U.S. Geological Survey for adjudications, compacts, and treaties","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr82680","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-680","title":"Support by the U.S. Geological Survey for adjudications, compacts, and treaties","docAbstract":"The U.S. Geological Survey supports interstate compacts, treaties, and court decrees by providing hydrologic data and analysis needed in their administration and by providing Federal representation on compact commissions. As part of this program, in fiscal year 1982 the Geological Survey operated 171 streamflow stations, 3 sediment stations, and 13 water-quality stations, and conducted ground-water studies at a cost of $1,014,000. Funding for Federal representation to i0 interstate compacts is presently budgeted at $56,000.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82680","usgsCitation":"Condes de la Torre, A., 1982, Support by the U.S. Geological Survey for adjudications, compacts, and treaties: U.S. Geological Survey Open-File Report 82-680, iv, 28 p. :maps ;28 cm., https://doi.org/10.3133/ofr82680.","productDescription":"iv, 28 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0680/report-thumb.jpg"},{"id":35968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0680/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697cbd","contributors":{"authors":[{"text":"Condes de la Torre, Alberto","contributorId":73570,"corporation":false,"usgs":true,"family":"Condes de la Torre","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":157662,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11043,"text":"ofr82509 - 1982 - U.S. Geological Survey research in radioactive waste disposal; fiscal year 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82509","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-509","title":"U.S. Geological Survey research in radioactive waste disposal; fiscal year 1980","docAbstract":"The report summarizes progress on geologic and hydrologic research related to the disposal of radioactive wastes. The research is described according to whether it is related most directly to: (1) High-level and transuranic wastes; (2) Low-level wastes, or (3) Uranium mill tailings. Included is research applicable to the identification and geohydrologic characterization of waste-disposal sites, to investigations of specific sites where wastes have been stored, and to studies of regions or environments where waste-disposal sites might be located. A significant part of the activity is concerned with techniques and methods for characterizing disposal sites and studies of geologic and hydrologic processes related to the transport and (or) retention of waste radionuclides.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82509","usgsCitation":"Schneider, R., and Trask, N., 1982, U.S. Geological Survey research in radioactive waste disposal; fiscal year 1980: U.S. Geological Survey Open-File Report 82-509, 115 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr82509.","productDescription":"115 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0509/report-thumb.jpg"},{"id":38813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0509/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4fde","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":162430,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":162429,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}