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":24681,"text":"ofr80774 - 1980 - Ground-water resources investigation in the Amran Valley, Yeman Arab Republic","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"ofr80774","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":"80-774","title":"Ground-water resources investigation in the Amran Valley, Yeman Arab Republic","docAbstract":"A program of hydrologic studies and exploratory drilling was conducted intermittently between 1974 and 1978 to evaluate the water-bearing properties of the unconsolidated alluvial sediments and associated rocks in the semi-arid Amran Valley basin, an 800-square-kilometer area in north-central Yemen Arab Republic. Inventory data from 395 wells were compiled, observation well and rain-gage networks were established and 16 standard complete chemical analyses were made for samples from selected wells. The water resources of the area were overexploited. The chemical quality of the water is generally good. Four aquifer tests were run to determine transmissivity and storage characteristics. The pumping tests show that groundwater occurs under semi-confined leaky-aquifer conditions in the valley fill. Wells drilled in the alluvial fill of the south-central part of the valley have the highest yields. Wells penetrating the limestone and volcanic rocks generally have little or no yield except in fracture zones. Basalt flows occur interbedded with the wadi alluvium at several depths. Cropping out rocks in the Amran Valley range in age from late Jurassic to Holocene. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80774","issn":"0094-9140","usgsCitation":"Tibbitts, G., and Aubel, J., 1980, Ground-water resources investigation in the Amran Valley, Yeman Arab Republic: U.S. Geological Survey Open-File Report 80-774, vi, 144 p. ill., maps ;26 cm., https://doi.org/10.3133/ofr80774.","productDescription":"vi, 144 p. ill., maps ;26 cm.","costCenters":[],"links":[{"id":157703,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0774/report-thumb.jpg"},{"id":53704,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0774/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53705,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0774/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e3e","contributors":{"authors":[{"text":"Tibbitts, G. Chase","contributorId":79453,"corporation":false,"usgs":true,"family":"Tibbitts","given":"G. Chase","affiliations":[],"preferred":false,"id":192377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aubel, James","contributorId":19597,"corporation":false,"usgs":true,"family":"Aubel","given":"James","email":"","affiliations":[],"preferred":false,"id":192376,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23752,"text":"ofr80755 - 1980 - Iowa observation well network; past, present, and future","interactions":[],"lastModifiedDate":"2016-03-02T13:40:29","indexId":"ofr80755","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":"80-755","title":"Iowa observation well network; past, present, and future","docAbstract":"Water-level measurements in wells were started by the USGS in Iowa in 1935.
\nSince then a total of about 450 different wells have been measured. The present network consists of about 70 wells. The measurement of these water levels aids in evaluating the present and future water resources of the State.
\nMany factors influence water-level fluctuations. These factors include atmospheric pressure, withdrawals by pumping, earthquakes, earth tides, change in surface loading, discharge to streams, evapotranspiration, and precipitation. Fluctuations produced by artificial discharge through pumping is a common phenomena but unlike the other factors can be regulated and controlled.
\nAll present and past USGS observation wells for the State of Iowa since 1935 are listed and located on maps. It is recommended that improvement of the observation-well network by the addition of wells in specific areas should be undertaken as soon as possible.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr80755","issn":"0094-9140","collaboration":"Prepared in cooperation with the Iowa Natural Resources Council and the Iowa Geological Survey","usgsCitation":"Logel, J.D., 1980, Iowa observation well network; past, present, and future: U.S. Geological Survey Open-File Report 80-755, v, 45 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr80755.","productDescription":"v, 45 p., ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":156135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0755/report-thumb.jpg"},{"id":52985,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0755/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52986,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0755/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667320","contributors":{"authors":[{"text":"Logel, John D.","contributorId":59835,"corporation":false,"usgs":true,"family":"Logel","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":190655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23784,"text":"ofr80645 - 1980 - Outer continental shelf oil and gas activities in the Pacific (Southern California) and their onshore impacts: a summary report, May 1980","interactions":[],"lastModifiedDate":"2013-12-13T14:15:10","indexId":"ofr80645","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":"80-645","title":"Outer continental shelf oil and gas activities in the Pacific (Southern California) and their onshore impacts: a summary report, May 1980","docAbstract":"Outer Continental Shelf (OCS) oil and gas exploration and development have been under way in the Pacific (Southern California) Region since 1966. During that time, there have been four Federal lease sales: in 1966, 1968, 1975 (Sale 35), and 1979 (Sale 48). Oil and gas production from three leases has been going on since 1968. It peaked in 1971 and now averages around 31,400 barrels of oil and 15.4 million cubic feet of gas per day. Discoveries on areas leased in the 1968 and 1975 sales have led to plans for eight new platforms to begin production in the early 1980's. Five platforms are in the eastern end of Santa Barbara Channel, one is in the western Channel, and two are in San Pedro Bay, south of Long Beach. Three rigs are doing exploratory drilling in the Region.
\nThe most recent estimates by the U.S. Geological Survey of remaining reserves for all identified fields in the Southern California Region are 695 million barrels of oil and 1,575 billion cubic feet of gas (January 1979). The USGS has also made risked estimates of economically recoverable oil and gas resources for all the leased tracts in the Region (March 1980). These risked estimates of economically recoverable resources are 394 billion barrels of oil and 1,295 billion cubic feet of gas. The USGS estimates of undiscovered recoverable resources for the entire Southern California OCS Region (January 1980) are 3,200 million barrels of oil and 3,400 billion cubic feet of gas.
\nBecause of the long history of oil and gas production in Southern California from wells onshore and in State waters, there are many existing facilities for the transportation, processing, and refining of oil and gas. Some of the expected new OCS production can be accommodated in these facilities. Four new onshore projects will be required. Two of these are under construction: (1) a 9.6-km (6-mi) onshore oil pipeline (capacity: 60,000 bpd) between Carpinteria (Santa Barbara County) and the existing Mobil-Rincon separation and treatment facility (Ventura County), and (2) a small supply base and dock (upgrade of existing facility) and a 0.4-hectare (1-acre) crude oil distribution facility in Long Beach (Los Angeles County), connected to landfall by a 3-km (1.8-mi) onshore pipeline. The two other facilities are awaiting permit approval: (1) a gas treatment plant at Las Flores Canyon (Santa Barbara County) and (2) a separation and treatment plant at Mandalay Beach (Ventura County) with 4 km (2.5 mi) of onshore pipeline on the same right-of-way from landfall to the plant and from the plant to an existing gas transmission line.
","language":"English","publisher":"Rogers, Golden & Halpern, Inc.","publisherLocation":"Philadelphia, PA","doi":"10.3133/ofr80645","issn":"0094-9140","collaboration":"Prepared for the U.S. Department of the Interior, Geological Survey, in cooperation with the Bureau of Land Management and the Council of Environmental Quality under Contract No. EQ9AC006, by Rogers, Golden & Halpern, Inc.","usgsCitation":"Macpherson, G.S., and Bernstein, J., 1980, Outer continental shelf oil and gas activities in the Pacific (Southern California) and their onshore impacts: a summary report, May 1980: U.S. Geological Survey Open-File Report 80-645, xi, 134 p., https://doi.org/10.3133/ofr80645.","productDescription":"xi, 134 p.","numberOfPages":"148","costCenters":[],"links":[{"id":157162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0645/report-thumb.jpg"},{"id":279459,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0645/report.pdf"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.0748,30.7489 ], [ -121.0748,34.5156 ], [ -116.9879,34.5156 ], [ -116.9879,30.7489 ], [ -121.0748,30.7489 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a3ce","contributors":{"authors":[{"text":"Macpherson, George S.","contributorId":75538,"corporation":false,"usgs":true,"family":"Macpherson","given":"George","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":190720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernstein, Janis","contributorId":71207,"corporation":false,"usgs":true,"family":"Bernstein","given":"Janis","email":"","affiliations":[],"preferred":false,"id":190719,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23209,"text":"ofr801204 - 1980 - Floods in Indiana, June-August 1979","interactions":[],"lastModifiedDate":"2020-02-05T15:31:05","indexId":"ofr801204","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":"80-1204","title":"Floods in Indiana, June-August 1979","docAbstract":"This report documents rainstorms and resultant floods in central and southern Indiana during the summer of 1979. Major flooding was caused by three storms, one in June and two in July 1979, centered primarily in central and southern Indiana. Peak discharge exceeded the 100-year recurrence interval at 16 sites in this area. State Civil Defense officials estimated that almost 50-million dollars damage was attributable to the July floods. Hydrologic data have been tabulated for streamflow sites in the areas of flooding. Reservoir storage volumes, observation-well data, rainfall totals, and discharge hydrographs are presented to show the intensity and time of the storms and resultant floods. (USGS)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr801204","issn":"0094-9140","usgsCitation":"Gold, R., and Wolcott, S.W., 1980, Floods in Indiana, June-August 1979: U.S. Geological Survey Open-File Report 80-1204, v, 32 p. , https://doi.org/10.3133/ofr801204.","productDescription":"v, 32 p. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e70cb","contributors":{"authors":[{"text":"Gold, Robert L.","contributorId":78324,"corporation":false,"usgs":true,"family":"Gold","given":"Robert L.","affiliations":[],"preferred":false,"id":189636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolcott, Stephen W.","contributorId":93458,"corporation":false,"usgs":true,"family":"Wolcott","given":"Stephen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":189637,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24712,"text":"ofr80419 - 1980 - Ground-water data for the Riley and Andrews Resource Areas, southeastern Oregon","interactions":[],"lastModifiedDate":"2016-07-08T09:22:09","indexId":"ofr80419","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":"80-419","title":"Ground-water data for the Riley and Andrews Resource Areas, southeastern Oregon","docAbstract":"Appraisals of the resources of selected management areas in eastern Oregon are being made by the U.S. Bureau of Land Mangement. To provide needed hydrologic information, the Bureau of Land Management requested the U.S. Geological Survey to inventory ground-water data for the Riley and Andrews Resource Areas. The inventory included field location of selected wells and springs; measurement of ground-water levels, temperatures, specific conductance, and pH; and the collection of ground-water samples from selected sources to determine dissolved chemical constituents.
\nIncluded in this report are well data, drillers ' lithologic logs, hydrographs of observation wells, a summary of observation-well data, and chemical analyses of ground water.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr80419","issn":"0094-9140","usgsCitation":"Townley, P.J., Soja, C.M., and Sidle, W., 1980, Ground-water data for the Riley and Andrews Resource Areas, southeastern Oregon: U.S. Geological Survey Open-File Report 80-419, Report: v, 32 p.; Plate: 41.03 x 45.85 inches, https://doi.org/10.3133/ofr80419.","productDescription":"Report: v, 32 p.; Plate: 41.03 x 45.85 inches","numberOfPages":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":157520,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr80419.jpg"},{"id":324874,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0419/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":324875,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0419/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120,\n 42\n ],\n [\n -120,\n 44\n ],\n [\n -118,\n 44\n ],\n [\n -118,\n 42\n ],\n [\n -120,\n 42\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf3b","contributors":{"authors":[{"text":"Townley, Paul J.","contributorId":106157,"corporation":false,"usgs":true,"family":"Townley","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":192419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soja, Constance M.","contributorId":89566,"corporation":false,"usgs":true,"family":"Soja","given":"Constance","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":192417,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sidle, W.C.","contributorId":93911,"corporation":false,"usgs":true,"family":"Sidle","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":192418,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23282,"text":"ofr801120 - 1980 - Reconnaissance of the effect of landfill leachate on the water quality of Marshall Brook, Southwest Harbor, Hancock County, Maine","interactions":[],"lastModifiedDate":"2019-06-20T11:29:47","indexId":"ofr801120","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":"80-1120","title":"Reconnaissance of the effect of landfill leachate on the water quality of Marshall Brook, Southwest Harbor, Hancock County, Maine","docAbstract":"A small stream (2.2 square miles drainage area) receiving leachate from a landfill was studied from August through November 1979 to determine the impact of the leachate on water quality. The presence of un-ionized ammonia, considered toxic to some aquatic vertebrates, was indicated in samples taken from sections of the stream affected by leachate. Some dissolved oxygen values did not meet the criteria for the protection of aquatic life. Many other dissolved constituents were present in elevated concentrations in the leachate-influenced reaches of the stream. Flow-data comparisons indicate that streamflow less than that observed will occur approximately 20 percent of the time. Leachate-affected stream conditions may deteriorate further during such low streamflow. Several areas with the potential for large sediment yields are present in the basin.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801120","issn":"0094-9140","collaboration":"Prepared in cooperation with the Water Resources Program, Office of Scientific Studies, National Park Service, North Atlantic Region","usgsCitation":"Hansen, B.P., 1980, Reconnaissance of the effect of landfill leachate on the water quality of Marshall Brook, Southwest Harbor, Hancock County, Maine: U.S. Geological Survey Open-File Report 80-1120, iv, 13 p., https://doi.org/10.3133/ofr801120.","productDescription":"iv, 13 p.","costCenters":[],"links":[{"id":364833,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1120/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1120/report-thumb.jpg"}],"scale":"62500","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"Maine","county":"Hancock County","otherGeospatial":"Marshall Brook","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -68.41684341430664,\n 44.21924632442265\n ],\n [\n -68.29341888427734,\n 44.21924632442265\n ],\n [\n -68.29341888427734,\n 44.3170933048524\n ],\n [\n -68.41684341430664,\n 44.3170933048524\n ],\n [\n -68.41684341430664,\n 44.21924632442265\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a63e4b07f02db636f93","contributors":{"authors":[{"text":"Hansen, Bruce P.","contributorId":90727,"corporation":false,"usgs":true,"family":"Hansen","given":"Bruce","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":189807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24003,"text":"ofr80574 - 1980 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","interactions":[{"subject":{"id":24003,"text":"ofr80574 - 1980 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"ofr80574","publicationYear":"1980","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043690,"text":"70043690 - 1982 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"70043690","publicationYear":"1982","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"id":1}],"supersededBy":{"id":70043690,"text":"70043690 - 1982 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"70043690","publicationYear":"1982","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"lastModifiedDate":"2016-12-17T12:51:17","indexId":"ofr80574","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":"80-574","title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80574","issn":"0094-9140","usgsCitation":"Mundorff, J.C., and Thompson, K.R., 1980, Reconnaissance of the quality of surface water in the San Rafael River basin, Utah: U.S. Geological Survey Open-File Report 80-574, https://doi.org/10.3133/ofr80574.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":157494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"San Rafael River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.5,\n 38.4\n ],\n [\n -111.5,\n 39.75\n ],\n [\n -110,\n 39.75\n ],\n [\n -110,\n 38.4\n ],\n [\n -111.5,\n 38.4\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636a58","contributors":{"authors":[{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":191128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Kendall R.","contributorId":100854,"corporation":false,"usgs":true,"family":"Thompson","given":"Kendall","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":191129,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23361,"text":"ofr80697 - 1980 - Feasibility of using an acoustic velocity meter to measure flow in the Chipps Island channel, Suisun Bay, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"ofr80697","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":"80-697","title":"Feasibility of using an acoustic velocity meter to measure flow in the Chipps Island channel, Suisun Bay, California","docAbstract":"Tests were conducted in 1978 to determine the feasibility of using an acoustic velocity meter to measure the Sacramento-San Joaquin Delta outflow in the Chipps Island Channel, Suisun Bay, Calif. Three parts of transducers with frequencies of 100, 40, and 24 kilohertz were installed on a cross-channel test path and operated at three elevations, 15.5, 8.0, and 4.0 feet below mean lower low water, to test signal transmission at varying depths. Transmission was most reliable at the lowest depth, and the 24-kilohertz transducers at the 7-millivolt threshold of signal strength met the study 's criterion of no persistent signal loss of more than one hour 's duration in any phase of the tidal cycle. Signal strength was statistically correlated with the environmental factors of wind velocity, wind direction, solar insolation, electrical conductivity, water temperature, water velocity, stage, rate of change in stage, and the acceleration of the rate of change in stage. All correlations were weak. Signal strength is apparently a function of the interaction of several environmental factors. A 32-day test to observe if aquatic growth on the transducers would affect signal transmission showed no reduction in signal strength. Suspended-sediment samples indicated that both the size and concentration of particles are greater than presumed in earlier studies. According to the results of this study, chances are good for reliable transmission of acoustic velocity meter signals. Usually some signals were much stronger than the average 20-second signal strength at 15-minute intervals used for correlation and the frequency analysis. Superior equipment is now being developed specifically for the Chipps Island site to transmit signals several times stronger than the signals analyzed in these tests. (USGS)","language":"ENGLISH","publisher":"Water Resources Division, U.S. Geological Survey,","doi":"10.3133/ofr80697","issn":"0094-9140","usgsCitation":"Hoffard, S.H., 1980, Feasibility of using an acoustic velocity meter to measure flow in the Chipps Island channel, Suisun Bay, California: U.S. Geological Survey Open-File Report 80-697, v, 33 p. ill., map ;28 cm., https://doi.org/10.3133/ofr80697.","productDescription":"v, 33 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":157355,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6f3b","contributors":{"authors":[{"text":"Hoffard, Stuart H.","contributorId":46568,"corporation":false,"usgs":true,"family":"Hoffard","given":"Stuart","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":189974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24156,"text":"ofr80743 - 1980 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1977","interactions":[],"lastModifiedDate":"2022-12-27T21:41:38.499586","indexId":"ofr80743","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":"80-743","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1977","docAbstract":"Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Dallas, Dallas County, Fort Worth, Houston, and San Antonio.
The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing gaging-station network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data.
The operation and maintenance of stations 08178000, San Antonio River at San Antonio; 08178700, Salado Creek (upper station) at San Antonio; and 08178800, Salado Creek (lower station) at San Antonio are funded by the San Antonio River Authority in cooperation with the Texas Department of Water Resources and the U.S. Geological Survey.
The operation and maintenance and collection of water-quality data at station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio are funded by the Edwards Underground Water District in cooperation with the Texas Department of Water Resources and the U.S. Geological Survey. These stations will provide hydrologic data on similar and adjacent drainage basins. One drainage basin is undergoing extensive urbanization while the other is undeveloped.
The objective of the San Antonio urban-hydrology study are:
Heliothermic lakes contain a sun-heated layer of warm, saline water beneath a surface layer of cooler, less saline water. The two layers are separated by a chemocline, a stratum in which salinity increases progressively with depth. The chemocline, the position of which varies from lake to lake, functions as a heat trap. Most sunlight that penetrates this stratum is transformed into heat, which cannot escape by radiation because water is opaque to infrared light, and which cannot escape by convection because the specific gravity of the dense water below the chemocline is not significantly decreased by the increasing temperature. Heat can escape only by conduction through the chemocline, and water or brine is a very poor conductor. As a result, the temperature within and commonly below the chemocline rises. Under ideal conditions of a clear solution, high isolation, and a suitable salinity distribution, the temperature of the chemocline will increase to the boiling point. The lower part of the chemocline in a shallow (0.8-m) manmade heliothermic lake at Sedom, Israel, for example, reached a temperature of 96°C (205°F) in spite of a brine with poor light transmissibility.
About 30 natural heliothermic lakes have been reported. The best known, Lake Ursului, occurs in Transylvania, Romania (latitude, 46°35'N). During four consecutive summers, 1899 to 1902, this lake had temperatures of 60-70°C (140-158°F) at a depth of 1-2 m. Heliothermic conditions have persisted in this lake for at least 28 and probably for more than 77 years. The most unusual, Lake Vanda, Victoria Land, Antarctica (latitude, 77°35'S), has a temperature of 26°C near the base of the chemocline at a depth of 61 despite a mean atmospheric temperature of -20°C. Sunlight penetrates into the chemocline through 5 m of remarkably clear ice.
Maintenance of the chemocline is the chief problem preventing commercial use of manmade heliothermic lakes for the collection and storage of solar energy. The most effective means of preserving this stratum from destruction by diffusion and wind mixing may be the use of salts, such as sodium sulfate and sodium borate, whose solubilities are markedly influenced by temperature. The chemoclines of ponds constructed with such salts, in theory, would persist indefinitely and could be of great size.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80807","issn":"0094-9140","usgsCitation":"Kirkland, D.W., Bradbury, J.P., and Dean, W.E., 1980, The heliothermic lake: a direct method of collecting and storing solar energy: U.S. Geological Survey Open-File Report 80-807, vi, 126 p., https://doi.org/10.3133/ofr80807.","productDescription":"vi, 126 p.","costCenters":[],"links":[{"id":156442,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0807/report-thumb.jpg"},{"id":350863,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0807/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655576","contributors":{"authors":[{"text":"Kirkland, Douglas W.","contributorId":10067,"corporation":false,"usgs":true,"family":"Kirkland","given":"Douglas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":190355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradbury, J. Platt","contributorId":91106,"corporation":false,"usgs":true,"family":"Bradbury","given":"J.","email":"","middleInitial":"Platt","affiliations":[],"preferred":false,"id":190356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":190354,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23566,"text":"ofr80417 - 1980 - Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":23566,"text":"ofr80417 - 1980 - Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado","indexId":"ofr80417","publicationYear":"1980","noYear":false,"title":"Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":2028,"text":"wsp2074 - 1981 - Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado","indexId":"wsp2074","publicationYear":"1981","noYear":false,"title":"Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado"},"id":1}],"supersededBy":{"id":2028,"text":"wsp2074 - 1981 - Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado","indexId":"wsp2074","publicationYear":"1981","noYear":false,"title":"Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado"},"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr80417","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":"80-417","title":"Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr80417","issn":"0094-9140","usgsCitation":"Kimball, B.A., 1980, Geochemistry of spring water, southeastern Uinta Basin, Utah and Colorado: U.S. Geological Survey Open-File Report 80-417, 68 p. ill., map ;28 cm., https://doi.org/10.3133/ofr80417.","productDescription":"68 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":156622,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa6c9","contributors":{"authors":[{"text":"Kimball, Briant A. bkimball@usgs.gov","contributorId":533,"corporation":false,"usgs":true,"family":"Kimball","given":"Briant","email":"bkimball@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":190328,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25020,"text":"pp1107 - 1980 - Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality","interactions":[{"subject":{"id":21771,"text":"ofr78576 - 1978 - Erosion, sediment discharge, and channel morphology in the Upper Chattahoochee River basin, Georgia","indexId":"ofr78576","publicationYear":"1978","noYear":false,"title":"Erosion, sediment discharge, and channel morphology in the Upper Chattahoochee River basin, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":25020,"text":"pp1107 - 1980 - Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality","indexId":"pp1107","publicationYear":"1980","noYear":false,"title":"Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality"},"id":1}],"lastModifiedDate":"2017-01-05T12:28:04","indexId":"pp1107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1107","title":"Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality","docAbstract":"The 3,550 square miles of the Upper Chattahoochee River basin is an area of diverse physiographic and land-use characteristics. The headwater areas are mountainous with steep, relatively narrow channels. Land in the headwater areas is heavily forested, but small towns and farms are common in the valleys of large streams. Downstream, the basin is characterized by low hills and wider stream channels. Land in this part of the basin is also predominantly forested; however, large agricultural and urban areas are common. Urban land use is particularly intensive within the Atlanta Metropolitan Area. ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1107","usgsCitation":"Faye, R.E., Carey, W.P., Stamer, J., and Kleckner, R., 1980, Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality: U.S. Geological Survey Professional Paper 1107, 85 p., https://doi.org/10.3133/pp1107.","productDescription":"85 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":122566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1107/report-thumb.jpg"},{"id":54022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","otherGeospatial":"Upper Chattahoochee River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.21295166015629,\n 34.24245948736849\n ],\n [\n -84.13604736328122,\n 34.56764471968292\n ],\n [\n -83.98223876953124,\n 34.768691457552706\n ],\n [\n -83.726806640625,\n 34.75740963726004\n ],\n [\n -83.50982666015624,\n 34.70775131553933\n ],\n [\n -83.47412109374999,\n 34.54954921593403\n ],\n [\n -83.47137451171875,\n 34.51334640147576\n ],\n [\n -84.00009155273438,\n 33.970697997361654\n ],\n [\n -84.36538696289062,\n 33.87041555094183\n ],\n [\n -84.4793701171875,\n 33.73804486328907\n ],\n [\n -84.53430175781247,\n 33.6031820405205\n ],\n [\n -84.70733642578124,\n 33.447484889088855\n ],\n [\n -84.6551513671875,\n 33.351179088043494\n ],\n [\n -84.7540283203125,\n 33.284619968887675\n ],\n [\n -84.76226806640624,\n 33.18353672893615\n ],\n [\n -84.84191894531249,\n 33.100745405144245\n ],\n [\n -84.8583984375,\n 32.9372338139709\n ],\n [\n -85.02044677734375,\n 32.858825196463854\n ],\n [\n -85.177001953125,\n 32.857671610787456\n ],\n [\n -85.27313232421878,\n 32.88996633815203\n ],\n [\n -85.30746459960939,\n 33.04781007347206\n ],\n [\n -85.26214599609375,\n 33.167444534375925\n ],\n [\n -85.1708221435547,\n 33.23983613293645\n ],\n [\n -85.16738891601562,\n 33.31905344502012\n ],\n [\n -85.07812500000003,\n 33.46810795527894\n ],\n [\n -84.99092102050781,\n 33.49445251114961\n ],\n [\n -84.83230590820312,\n 33.67063988581374\n ],\n [\n -84.70184326171875,\n 33.7597402884442\n ],\n [\n -84.55490112304689,\n 33.91487347147951\n ],\n [\n -84.43130493164067,\n 34.025347738147936\n ],\n [\n -84.35302734375003,\n 34.07882486401267\n ],\n [\n -84.21295166015629,\n 34.24245948736849\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdf58","contributors":{"authors":[{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carey, W. P.","contributorId":105749,"corporation":false,"usgs":true,"family":"Carey","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":193064,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stamer, J. K.","contributorId":47753,"corporation":false,"usgs":true,"family":"Stamer","given":"J. K.","affiliations":[],"preferred":false,"id":193061,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kleckner, R.L.","contributorId":70744,"corporation":false,"usgs":true,"family":"Kleckner","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":193062,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":26006,"text":"wri8071 - 1980 - Effects of urbanization on the water quality of lakes in Eagan, Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T10:54:22","indexId":"wri8071","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"80-71","title":"Effects of urbanization on the water quality of lakes in Eagan, Minnesota","docAbstract":"Water-quality characteristics of 17 lakes and ponds in the city of Eagan were described from data collected from 1972 through 1978. The data showed that differences in water quality between lakes were related to differences in the percentage of urbanization. However, water-quality variations within each lake were affected more by climatic variations than by land-use changes during that period.
\nDissolved solids, alkalinity, and chloride concentrations varied most in lakes with urbanized watersheds, in lakes with outlets, and in lakes less than 6 feet deep. Certain lakes without outlets showed an increase in chloride during the study, caused in part by urbanization but intensified by drought conditions of 1976-77.
\nFifteen of the lakes studied are less than 10 feet deep and frequently mix during open water. These lakes are highly eutrophic, primarily because of high nutrient loading and recycling of nutrients.
\nHolland and Fish Lakes, with depths of 52 and 30 feet, respectively, were the least eutrophic. These lakes limit continuous recycling of nutrients from bottom materials to water surface by thermal stratification and entrapment of nutrients in the hypolimnion.
\nThree phosphorus-prediction models developed during the study are applicable to shallow (less than about 12 feet), nonstratifying lakes and ponds. The data base was not sufficient to select an appropriate model to predict the effects of future loading from continuing urbanization on the deeper lakes.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri8071","collaboration":"Prepared in cooperation with the city of Eagan","usgsCitation":"Ayers, M.A., Payne, G.A., and Have, M.A., 1980, Effects of urbanization on the water quality of lakes in Eagan, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 80-71, iv, 42 p., https://doi.org/10.3133/wri8071.","productDescription":"iv, 42 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":157627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0071/report-thumb.jpg"},{"id":95573,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0071/report.pdf","size":"3285","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fcfc","contributors":{"authors":[{"text":"Ayers, M. A.","contributorId":41417,"corporation":false,"usgs":true,"family":"Ayers","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195629,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Payne, G. A.","contributorId":62190,"corporation":false,"usgs":true,"family":"Payne","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195630,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Have, Mark A.","contributorId":16867,"corporation":false,"usgs":true,"family":"Have","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195628,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23381,"text":"ofr80696 - 1980 - Low-flow characteristics of streams in the St. Croix River basin, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-20T09:39:30","indexId":"ofr80696","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":"80-696","title":"Low-flow characteristics of streams in the St. Croix River basin, Wisconsin","docAbstract":"Low-flow characteristics of streams in the St. Croix River basin , Wisconsin, are presented. Included are estimates of low-flow frequency and flow duration at 7 gaging stations, low-flow frequency characteristics at 23 low-flow partial-record stations and 78 miscellaneous sites, and a list of base-flow discharge measurements at 29 miscellaneous sites. Equations are provided to estimate low-flow characteristics at ungaged sites and at sites where one base-flow discharge measurement is available. The equations were determined from multiple-regression analyses that related low-flow characteristics at gaging stations and low-flow partial-record stations to basin characteristics. The standard error of estimate is provided for each method of estimating the annual minimum 7-day mean flow below which the flow will fall on the average of once in 2 years and once in 10 years. Standard error provides the user with the expected degree of accuracy for each method. (USGS)
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80696","issn":"0094-9140","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Holmstrom, B.K., 1980, Low-flow characteristics of streams in the St. Croix River basin, Wisconsin: U.S. Geological Survey Open-File Report 80-696, Report: iv, 62 p.; 2 Plates: 14.00 x 21.00 inches, https://doi.org/10.3133/ofr80696.","productDescription":"Report: iv, 62 p.; 2 Plates: 14.00 x 21.00 inches","numberOfPages":"66","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":52680,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0696/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52681,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0696/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52682,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0696/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0696/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"St. Croix River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.85693359375,\n 46.44542749723387\n ],\n [\n -92.61474609375,\n 46.475699386607516\n ],\n [\n -92.94433593749999,\n 45.10454630976873\n ],\n [\n -92.933349609375,\n 44.77013681219717\n ],\n [\n -92.823486328125,\n 44.55916341529184\n ],\n [\n -92.197265625,\n 44.33170718680922\n ],\n [\n -91.527099609375,\n 44.33170718680922\n ],\n [\n -91.724853515625,\n 44.91813929958515\n ],\n [\n -91.768798828125,\n 45.44471679159555\n ],\n [\n -91.62597656249999,\n 45.5679096098613\n ],\n [\n -91.19750976562499,\n 45.82114340079471\n ],\n [\n -90.845947265625,\n 46.14939437647686\n ],\n [\n -90.85693359375,\n 46.44542749723387\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486f0","contributors":{"authors":[{"text":"Holmstrom, B. K.","contributorId":90728,"corporation":false,"usgs":true,"family":"Holmstrom","given":"B.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":190008,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23933,"text":"ofr801195 - 1980 - Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978","interactions":[],"lastModifiedDate":"2013-08-02T08:00:06","indexId":"ofr801195","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":"80-1195","title":"Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978","docAbstract":"This report describes the observation-well network in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough Counties, Florida. Data obtained in 1978 from the network in and adjacent to the two well fields, as well as rainfall and pumpage records, are presented. The Southwest Florida Water Management District has established regulatory water-level limits in four observation wells and water-quality limits in three observation wells. Water levels dropped below regulatory limits in the spring of 1978 in three wells. Chloride concentrations in 1978 remained above regulatory limits for the entire year in one well and exceeded the limit during the late spring in the other two deep wells, both west of Eldridge-Wilde well field. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr801195","issn":"0094-9140","usgsCitation":"Mills, L.R., 1980, Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978: U.S. Geological Survey Open-File Report 80-1195, iv, 27 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801195.","productDescription":"iv, 27 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":156575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1195/report-thumb.jpg"},{"id":275925,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1195/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606973","contributors":{"authors":[{"text":"Mills, L. R.","contributorId":26281,"corporation":false,"usgs":true,"family":"Mills","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23380,"text":"ofr80749 - 1980 - Low-flow characteristics of streams in the Menominee-Oconto-Peshtigo River basin, Wisconsin","interactions":[],"lastModifiedDate":"2022-10-03T21:23:58.758817","indexId":"ofr80749","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":"80-749","title":"Low-flow characteristics of streams in the Menominee-Oconto-Peshtigo River basin, Wisconsin","docAbstract":"Low-flow characteristics of streams in the Menominee-Oconto-Peshtigo River basin, Wisconsin, are presented. Included are estimates of low-flow frequency at 12 gaging stations, flow duration at 10 gaging stations, and low-flow frequency characteristics at 23 low-flow partial-record stations and 137 miscellaneous sites. Equations are provided to estimate low-flow characteristics at ungaged sites and at sites where one base-flow discharge measurement is available. The equations were determined from multiple-regression analyses that related low-flow characteristics at gaging stations and low-flow partial-record stations to basin characteristics. The standard error of estimate is provided for each method of estimating the annual minimum 7-day mean flow below which the flow will fall on the average of once in 2 years and once in 10 years. The standard error of estimate for the 7-day 10-year low flow ranged from 6% to 76% depending on the type of data available. Standard error provides the user with the expected degree of accuracy for each method.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80749","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Holmstrom, B.K., 1980, Low-flow characteristics of streams in the Menominee-Oconto-Peshtigo River basin, Wisconsin: U.S. Geological Survey Open-File Report 80-749, Report: iv, 82 p.; 2 Plates: 12.00 x 18.00 inches, https://doi.org/10.3133/ofr80749.","productDescription":"Report: iv, 82 p.; 2 Plates: 12.00 x 18.00 inches","numberOfPages":"87","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":52679,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0749/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52678,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0749/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52677,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0749/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0749/report-thumb.jpg"},{"id":407825,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11756.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"500000","country":"United States","state":"Wisconsin","county":"Brown County, Florence County, Forest County Langlade County, Marinette County, Menominee County, Oconto County, Outagamie County, Shawano County, Vilas County","otherGeospatial":"Menominee River, Oconto River, Peshtigo River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.593505859375,\n 44.166444664458595\n ],\n [\n -89.593505859375,\n 46.263442671779885\n ],\n [\n -87.47314453125,\n 46.263442671779885\n ],\n [\n -87.47314453125,\n 44.166444664458595\n ],\n [\n -89.593505859375,\n 44.166444664458595\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486de","contributors":{"authors":[{"text":"Holmstrom, B. K.","contributorId":90728,"corporation":false,"usgs":true,"family":"Holmstrom","given":"B.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":190007,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24802,"text":"ofr80598 - 1980 - Potentiometric map of the Winona-Tallahatta aquifer in northwestern Mississippi, fall 1979","interactions":[],"lastModifiedDate":"2022-08-09T19:34:37.336296","indexId":"ofr80598","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":"80-598","title":"Potentiometric map of the Winona-Tallahatta aquifer in northwestern Mississippi, fall 1979","docAbstract":"The potentiometric map of the Winona-Tallahatta aquifer is one of a series of maps, prepared by the U.S. Geological Survey in cooperation with the Mississippi Department of Natural Resources , Bureau of Land and Water Resources, delineating the potentiometric surfaces of the major aquifers in Mississippi. In the outcrop area of the Winona-Tallahatta aquifer the potentiometric surface is strongly affected by recharge from precipitation, by topography, and by drainage of the aquifer by streams. The potentiometric surface slopes downward generally to the west away from the area of outcrop and is strongly affected by recharge from precipitation, by topography, and by drainage of the aquifer by streams. The potentiometric surface slopes downward generally to the west away from the area of outcrop and is strongly affected by pumpage from wells in Leflore, Sunflower , and Bolivar Counties, Historically, water levels in or near the outcrop of the Winona-Tallahatta have shown little or no long-term changes, but the heavy withdrawals in the confined part of the aquifer have caused long-term water-level declines of 1 to 2 feet per year. (USGS)","language":"English","publisher":"U.S Geological Survey","doi":"10.3133/ofr80598","usgsCitation":"Wasson, B.E., 1980, Potentiometric map of the Winona-Tallahatta aquifer in northwestern Mississippi, fall 1979 (WRI/OFR): U.S. Geological Survey Open-File Report 80-598, 1 Plate: 34.50 × 20.53 inches or smaller, https://doi.org/10.3133/ofr80598.","productDescription":"1 Plate: 34.50 × 20.53 inches or smaller","costCenters":[],"links":[{"id":157424,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":405045,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11704.htm","linkFileType":{"id":5,"text":"html"}},{"id":53816,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0598/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Mississippi","otherGeospatial":"Winona-Tallahatta aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.1070,\n 32.57\n ],\n [\n -89.335,\n 32.57\n ],\n [\n -89.335,\n 34.665\n ],\n [\n -91.1070,\n 34.665\n ],\n [\n -91.1070,\n 32.57\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db6831f9","contributors":{"authors":[{"text":"Wasson, B. 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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.
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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":24624,"text":"ofr80551 - 1980 - Index of streamflow and water quality records to September 30, 1978, Southwest Alaska","interactions":[],"lastModifiedDate":"2018-10-31T13:59:29","indexId":"ofr80551","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":"80-551","title":"Index of streamflow and water quality records to September 30, 1978, Southwest Alaska","docAbstract":"This report, which is one of a series of reports for Alaska, lists stations in southwest Alaska (fig. 1) at which streamflow and water-quality data have been collected by the U.S. Geological Survey.
Most of the data referred to in this report have been published in reports of the Geological Survey. Water-quality data which were not included in those reports have been placed in the Survey's national computer storage system and are available through data-retrieval programs. Some of the older streamflow data have not been entered into the computer system. Geological Survey Water-Supply Paper (WSP) 1372 contains a summary of previously published records of monthly and annual discharges through September 1945, as well as records of daily and monthly discharges for the water years 1946-50 that had not yet been published. Water-Supply Paper 1372 also contains other stream chemical quality records collected between September 1948 and September 1950 and also some earlier records for the Yukon River at Anvik. Since 1950 data have been published in water-supply papers and a series of annual reports...
Data have been published in the annual series of reports, \"Water Resources Data for Alaska,\" since 1961 for streamflow records and 1964 for water-quality records.
This index lists: continuous-record streamgaging stations, crest-stage gage and low-flow partial-record stations; daily chemical, sediment, and temperature stations; and stations where some chemical, sediment, and biological data have been collected on an intermittent basis.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80551","issn":"0094-9140","usgsCitation":"Still, P.J., 1980, Index of streamflow and water quality records to September 30, 1978, Southwest Alaska: U.S. Geological Survey Open-File Report 80-551, iii, 13 p., https://doi.org/10.3133/ofr80551.","productDescription":"iii, 13 p.","costCenters":[],"links":[{"id":359036,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0551/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":111907,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/11301","linkFileType":{"id":5,"text":"html"}},{"id":157864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0551/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -188.7890625,\n 51.069016659603896\n ],\n [\n -152,\n 51.069016659603896\n ],\n [\n -152,\n 64\n ],\n [\n -188.7890625,\n 64\n ],\n [\n -188.7890625,\n 51.069016659603896\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48e9e4b07f02db553ad5","contributors":{"authors":[{"text":"Still, Patsy J.","contributorId":27077,"corporation":false,"usgs":true,"family":"Still","given":"Patsy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":192275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23714,"text":"ofr801020 - 1980 - Thermal springs in the Payette River basin, west-central Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"ofr801020","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":"80-1020","title":"Thermal springs in the Payette River basin, west-central Idaho","docAbstract":"The Payette River basin, characterized by steep, rugged mountains and narrow river valleys, occupies an area of about 3 ,300 square miles in west-central Idaho. Predominant rock types in the basin include granitic rocks of the Idaho batholith and basalt flows of the Columbia River Basalt Group. Waters from thermal springs in the basin, temperatures of which range from 34 to 86 degrees Celsius, are sodium bicarbonate types and are slightly alkaline. Dissolved-solids concentrations range from 173 to 470 milligrams per liter. Reservoir temperatures determined from the sodium-potassium-calcium and silicic acid-corrected silica geothermometers range from 53 to 143 degrees Celsius. Tritium, present in concentrations between 0 and 2 tritium units, indicate sampled thermal waters are at least 100 years old and possibly more than 1,000 years old. Stable isotope data indicate it is unlikely any of the nonthermal waters sampled are representative of precipitation that recharges the thermal springs in the basin. Thermal springs discharged about 5,700 acre-feet of water in 1979. Associated convective heat flux is 1.1x10 to the 7th power calories per second. 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