This report contains hydrologic data for wells collected in the East Shore area of the Great Salt Lake, Utah. It includes water-quality data, discharge measurements, water levels, and drillers* logs. The East Shore area (plate 1) includes about 430 square miles, bounded by the Wasatch Range on the east and the Great Salt Lake on the west. The first section line north of the town of Willard is the northern boundary, whereas the Davis-Salt Lake County line is the southern boundary.
Most of the data in this report were collected from 1983 to 1985 by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights. Some of the data were previously published by Smith (1961) or Bolke and Waddell (1972).
The purpose of this report is to provide ground-water data for use by officials managing water resources and the general public and to supplement an interpretive report for the area that will be published later. From tables 1- 5 of this report, determinations can be made for the depth to water-bearing units, water levels in wells, well yields, or chemical quality of ground water at the sites shown on plate 1.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr86139","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Plantz, G.G., Appel, C.L., Clark, D.W., Lambert, P.M., and Puryear, R.L., 1985, Selected hydrologic data from wells in the East Shore area of the Great Salt Lake, Utah, 1985: U.S. Geological Survey Open-File Report 86-139, Report: iv, 75 p.; Plate: 20.16 in. x 30.48 in., https://doi.org/10.3133/ofr86139.","productDescription":"Report: iv, 75 p.; Plate: 20.16 in. x 30.48 in.","numberOfPages":"79","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":143678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0139/report-thumb.jpg"},{"id":40511,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0139/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f89e4","contributors":{"authors":[{"text":"Plantz, Gerald G.","contributorId":96149,"corporation":false,"usgs":true,"family":"Plantz","given":"Gerald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":165793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Appel, Cynthia L.","contributorId":34509,"corporation":false,"usgs":true,"family":"Appel","given":"Cynthia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":165791,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":165790,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lambert, Patrick M. 0000-0001-6808-2303 plambert@usgs.gov","orcid":"https://orcid.org/0000-0001-6808-2303","contributorId":349,"corporation":false,"usgs":true,"family":"Lambert","given":"Patrick","email":"plambert@usgs.gov","middleInitial":"M.","affiliations":[{"id":38131,"text":"WMA - Office of Planning and Programming","active":true,"usgs":true}],"preferred":true,"id":165792,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Puryear, Robert L.","contributorId":85191,"corporation":false,"usgs":true,"family":"Puryear","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":165794,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":12464,"text":"ofr84249 - 1985 - Chemical and biological quality of selected lakes in Ohio, 1978 and 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr84249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-249","title":"Chemical and biological quality of selected lakes in Ohio, 1978 and 1979","docAbstract":"Twenty-eight Ohio lakes were sampled by the U.S. Geological Survey and the Ohio Environmental Protection Agency for water-quality characteristics during the spring and summer of 1978 and 1979. This report is the third in a series covering a lake-sampling program that began in 1975. Data include water-column profiles of temperature, dissolved oxygen, pH, and specific conductance. Chemical, physical, and biological properties were measured at specific points in the water column, and selected physical and chemical properties also were measured in the principal inflows.\r\n\r\nThe lakes were predominatly hard (120 180 milligrams per liter) to very hard water, although several soft-water lakes were found in southeastern Ohio. Calcium, bicarbonate, and sulfate were the principal dissolved constituents. Specific conductance ranged from 103 micromhos per centimeter (at 25 degrees Celsius) at Tycoon Lake, 1978, to 2,550 micromhos per centimeter at West Fork Mill Creek Lake, 1978. Thirteen lakes had trace-element concentrations that were above the limits for exceptional warm-water habitat recammended by the Ohio Environmental Protection Agency.\r\n\r\nSeasonal thermal gradients developed in most lakes deeper than 17 feet. Oxygen concentrations were zero or near zero during the summer sampling of the bottom water of all lakes having definite thermal gradients. Most anaerobic zones contained hydrogen sulfide and high concentrations of ammonia.\r\n\r\nAll lakes were evaluated and classified by Carlson's trophic state index. Most of the lakes were classified as eutrophic. Blue-green algae (CyanophytaJ) dominated the summer algal communities. Fecal colifrom counts were within Ohio standards, although high (more than 1,000 colonies per 100 milliliters) fecal colifrom and fecal streptococcus counts were observed in West Fork Mill Creek Lake after significant runoff.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84249","usgsCitation":"Angelo, C., and Youger, J.D., 1985, Chemical and biological quality of selected lakes in Ohio, 1978 and 1979: U.S. Geological Survey Open-File Report 84-249, xii, 306 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84249.","productDescription":"xii, 306 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0249/report-thumb.jpg"},{"id":40720,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0249/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e48d3","contributors":{"authors":[{"text":"Angelo, C.G.","contributorId":27434,"corporation":false,"usgs":true,"family":"Angelo","given":"C.G.","affiliations":[],"preferred":false,"id":166181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Youger, John D.","contributorId":46961,"corporation":false,"usgs":true,"family":"Youger","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":166182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8082,"text":"ofr84802 - 1985 - Hydrogeologic data from a test well in east-central Duval County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr84802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-802","title":"Hydrogeologic data from a test well in east-central Duval County, Florida","docAbstract":"A 2,112-foot test well was drilled in east-central Duval County, Florida, to obtain geologic, hydrologic, and water chemistry data. Drill cuttings and water samples were collected, and water-level measurements and lithologic and geophysical logs were made. Deposits to a depth of 575 feet consist of sand, clayey sand, phosphatic sandy clay, coquina, sandy limestone, and dolostone. Below 575 feet, the deposits consist of fragmented and granular limestone, dolomitic limestone, and massive to finely crystalline dolostone, which comprise the Floridan aquifer system in the area. Water levels were measured near or at the bottom of the drill hole through the drill stem and in the annular space between the drilled hole and drill stem at the well head as drilling progressed from 770 to 2,112 feet in depth. Water levels measured through the drill stem ranged from 1.17 feet above land surface at a depth of 2,107 feet to 15.0 feet above land surface at a depth of 1,574 feet. Water levels measured in the annular space ranged from 7.5 feet above land surface at a depth of 770 feet to 14.9 feet at various depths from 1,574 to 1,721 feet. Chloride concentrations of water sampled through the drill stem from a depth of 711 to 1 ,616 feet ranged from 22 to 150 milligrams per liter at 1,648 feet. Chloride concentrations then ranged from 345 to about 800 milligrams per liter to a depth of 2,071 feet and then increased to a maximum of 5,450 milligrams per liter at 2,107 feet. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84802","usgsCitation":"Brown, D., Johnson, R., and Broxton, R., 1985, Hydrogeologic data from a test well in east-central Duval County, Florida: U.S. Geological Survey Open-File Report 84-802, iv, 67 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84802.","productDescription":"iv, 67 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0802/report-thumb.jpg"},{"id":35686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0802/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6273e5","contributors":{"authors":[{"text":"Brown, D.P.","contributorId":95881,"corporation":false,"usgs":true,"family":"Brown","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":157113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, R.A.","contributorId":93864,"corporation":false,"usgs":true,"family":"Johnson","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":157112,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Broxton, R.A.","contributorId":36934,"corporation":false,"usgs":true,"family":"Broxton","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":157111,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":15236,"text":"ofr85187 - 1985 - Sediment and water-quality data for the West Branch Shade and East Branch Shade River basins, Ohio, 1983 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr85187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-187","title":"Sediment and water-quality data for the West Branch Shade and East Branch Shade River basins, Ohio, 1983 water year","docAbstract":"Sedimentation in and flooding of the West Branch Shade River and its tributaries have been major concerns of residents and State and local officials. The area was extensively surface mined for coal between the mid-1940's and the early 1960's. Reclamation efforts immediately after mining were unsuccessful. The results have been elevated sediment loads and the subsequent loss of channel conveyance.\r\n\r\nTwo sediment and stream-gaging stations were established on the West Branch Shade River and one station was established on the East Branch Shade River. These three stations will provide data to evalute the effectiveness of current reclamation activties on reducing sediment loads.\r\n\r\nFrom June Through September 1983, suspended-sediment yield was 18 times higher in West Branch (218 tons/mi2) than East Branch (12 tons/mi2) Shade River. In addition, acidity is higher, pH is lower, and concentrations of dissolved sulfate and metals are higher in the West Branch Shade River basin than in the East Branch Shade river basins.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85187","usgsCitation":"Childress, C., and Jones, R., 1985, Sediment and water-quality data for the West Branch Shade and East Branch Shade River basins, Ohio, 1983 water year: U.S. Geological Survey Open-File Report 85-187, iv, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85187.","productDescription":"iv, 20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0187/report-thumb.jpg"},{"id":44184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc108","contributors":{"authors":[{"text":"Childress, C.J.","contributorId":88734,"corporation":false,"usgs":true,"family":"Childress","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":170793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, R.L.","contributorId":39785,"corporation":false,"usgs":true,"family":"Jones","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":170792,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12269,"text":"ofr85304 - 1985 - Research, investigations, and technical developments; National Mapping Program 1983-84","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr85304","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-304","title":"Research, investigations, and technical developments; National Mapping Program 1983-84","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85304","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Research, investigations, and technical developments; National Mapping Program 1983-84: U.S. Geological Survey Open-File Report 85-304, xiii, 118 p. :ill. (some col.), maps ;1985., https://doi.org/10.3133/ofr85304.","productDescription":"xiii, 118 p. :ill. (some col.), maps ;1985.","costCenters":[],"links":[{"id":144619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0304/report-thumb.jpg"},{"id":40444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0304/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bd23","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528933,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38516,"text":"pp1345 - 1985 - The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","interactions":[{"subject":{"id":30815,"text":"ofr84624 - 1984 - The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","indexId":"ofr84624","publicationYear":"1984","noYear":false,"title":"The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":38516,"text":"pp1345 - 1985 - The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","indexId":"pp1345","publicationYear":"1985","noYear":false,"title":"The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington"},"id":1}],"lastModifiedDate":"2022-10-06T18:27:09.748698","indexId":"pp1345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1345","title":"The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","docAbstract":"A slope stability analysis on the South Fork Castle Creek debris avalanche blockage, near Mount St. Helens, Washington, was conducted to determine the likelihood of mass failure of the blockage and resultant breakout of South Fork Castle Creek Lake. On the basis of material properties, groundwater levels, and seismic history of the blockage, slope stability with and without earthquake-induced forces was determined. Results indicated that the blockage will not fail from gravitational forces at September 1983 groundwater levels. An increase of 25 feet or more in water levels could cause local failures, but massive failure of the blockage is improbable. Blockage slopes are potentially unstable for present and higher water levels if an earthquake with magnitude greater than 6.0 should occur. Retrogressive slope failures are possible, but lowering of the blockage crest below lake level and consequent lake breakout are considered remote. Significant earthquake shaking could cause cracks in the blockage that might facilitate piping.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1345","usgsCitation":"Meyer, W., Sabol, M.A., Glicken, H., and Voight, B., 1985, The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington: U.S. Geological Survey Professional Paper 1345, iv, 42 p., https://doi.org/10.3133/pp1345.","productDescription":"iv, 42 p.","costCenters":[],"links":[{"id":408049,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74275.htm","linkFileType":{"id":5,"text":"html"}},{"id":65253,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1345/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1345/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens area, South Fork Castle Creek blockage","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.2861,\n 46.2569\n ],\n [\n -122.2736,\n 46.2569\n ],\n [\n -122.2736,\n 46.2667\n ],\n [\n -122.2861,\n 46.2667\n ],\n [\n -122.2861,\n 46.2569\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65def4","contributors":{"authors":[{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":219978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sabol, M. A.","contributorId":36178,"corporation":false,"usgs":true,"family":"Sabol","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":219976,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Glicken, H. X.","contributorId":8902,"corporation":false,"usgs":true,"family":"Glicken","given":"H. X.","affiliations":[],"preferred":false,"id":219975,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Voight, Barry","contributorId":73653,"corporation":false,"usgs":true,"family":"Voight","given":"Barry","email":"","affiliations":[],"preferred":false,"id":219977,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":29863,"text":"wri854244 - 1985 - Estimation of evaporation from Ned Wilson Lake, Flat Tops Wilderness Area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:59","indexId":"wri854244","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4244","title":"Estimation of evaporation from Ned Wilson Lake, Flat Tops Wilderness Area, Colorado","docAbstract":"As part of an effort to define the hydrology and water quality of Ned Wilson Lake, evaporation rates were estimated for the summer periods of 1983 and 1984. Mass-transfer and energy-budget techniques and the Morton model were used to estimate evaporation using data collected at the lake and data collected at a meteorological station 0.1 mile from the lake. The estimate of evaporation for July 29 through September 27, 1983, using the mass-transfer technique, was 9.50 inches; the estimate using the energy-budget technique was 8.10 inches; the estimate using the Morton model was 9.90 inches. The evaporation estimate for July 18 through September 25, 1984, using the mass-transfer technique was 8.71 inches; the estimate using the energy-budget technique was 7.88 inches; the estimate using the Moron model was 10.49 inches. These estimates will provide values to be used in future analyses of the interaction of lake and groundwater; however, refinement of data collection will be necessary to determine specifically the rate of evaporation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854244","usgsCitation":"Spahr, N., and Turk, J., 1985, Estimation of evaporation from Ned Wilson Lake, Flat Tops Wilderness Area, Colorado: U.S. Geological Survey Water-Resources Investigations Report 85-4244, iv, 13 p. :ill., map ;28 cm., https://doi.org/10.3133/wri854244.","productDescription":"iv, 13 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":126593,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4244/report-thumb.jpg"},{"id":58674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4244/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fba16","contributors":{"authors":[{"text":"Spahr, N.E.","contributorId":79476,"corporation":false,"usgs":true,"family":"Spahr","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":202259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turk, J.T.","contributorId":94259,"corporation":false,"usgs":true,"family":"Turk","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":202260,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29936,"text":"wri854048 - 1985 - Controls on ground-water chemistry in the Horse Heaven Hills, south-central Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri854048","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4048","title":"Controls on ground-water chemistry in the Horse Heaven Hills, south-central Washington","docAbstract":"Miocene basaltic aquifers are the source of domestic and municipal water, and about 20,000 acre-feet of irrigation water annually, in the Horse Heaven Hills in south-central Washington State. Groundwater chemical variations derive from the hydraulic characteristics is of the geohydrologic system, from groundwater basalt reactions, and from irrigation. Some dissolved species concentrations increase with residence time; others decrease. Recharge area groundwaters are calcium magnesium sodium bicarbonate waters with sodium-adsorption ratios (SAR's) less than 1.0. They evolve to sodium potassium bicarbonate waters with SAR 's as high as 17. Glassy and cryptocrystalline phases of the basalt are the main sources of dissolved sodium. They dissolve by silicate hydrolysis in carbon dioxide charged waters that recharge the aquifer system. Dissolved silicon, iron, and aluminum concentrations are controlled by the solubilities of amorphous secondary alteration products, which order to silica phases, oxyhydroxides, and smectite. Carbonate mineral precipitation is induced by increasing pH from the hydrolysis reaction. Sodium and potassium concentrations increase until clinoptilolite saturation is reached and precipitation begins. Deviations from the general variation patterns are due to localized geologic structures which distort the groundwater flow system, and to the irrigation use of Columbia River water. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854048","usgsCitation":"Steinkampf, W., Bortleson, G.C., and Packard, F.A., 1985, Controls on ground-water chemistry in the Horse Heaven Hills, south-central Washington: U.S. Geological Survey Water-Resources Investigations Report 85-4048, v, 26 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854048.","productDescription":"v, 26 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4048/report-thumb.jpg"},{"id":58751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4048/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686525","contributors":{"authors":[{"text":"Steinkampf, W.C.","contributorId":8137,"corporation":false,"usgs":true,"family":"Steinkampf","given":"W.C.","affiliations":[],"preferred":false,"id":202386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bortleson, Gilbert C.","contributorId":57472,"corporation":false,"usgs":true,"family":"Bortleson","given":"Gilbert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":202387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Packard, F. A.","contributorId":71164,"corporation":false,"usgs":true,"family":"Packard","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202388,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29931,"text":"wri844290 - 1985 - Harmonic analyses of stream temperatures in the Upper Colorado River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri844290","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4290","title":"Harmonic analyses of stream temperatures in the Upper Colorado River Basin","docAbstract":"Harmonic analyses were made for available daily water-temperature records for 36 measurement sites on major streams in the Upper Colorado River Basin and for 14 measurement sites on streams in the Piceance structural basin. Generally (88 percent of the station years analyzed), more than 80 percent of the annual variability of temperatures of streams in the Upper Colorado River Basin was explained by the simple-harmonic function. Significant trends were determined for 6 of the 26 site records having 8 years or more record. In most cases, these trends resulted from construction and operation of upstream surface-water impoundments occurring during the period of record. Regional analysis of water-temperature characteristics at the 14 streamflow sites in the Piceance structural basin indicated similarities in water-temperature characteristics for a small range of measurement-site elevations. Evaluation of information content of the daily records indicated that less-than-daily measurement intervals should be considered, resulting in substantial savings in measurement and data-processing costs. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844290","usgsCitation":"Steele, T., 1985, Harmonic analyses of stream temperatures in the Upper Colorado River Basin: U.S. Geological Survey Water-Resources Investigations Report 84-4290, iv, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844290.","productDescription":"iv, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4290/report-thumb.jpg"},{"id":58747,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4290/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db640ff6","contributors":{"authors":[{"text":"Steele, T.D.","contributorId":38976,"corporation":false,"usgs":true,"family":"Steele","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":202377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41177,"text":"ofr85681 - 1985 - Potentiometric surface of the upper Floridan Aquifer in central Sumter County, Florida, September 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr85681","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-681","title":"Potentiometric surface of the upper Floridan Aquifer in central Sumter County, Florida, September 1985","docAbstract":"The map presents the potentiometric surface of the Upper Floridan aquifer in central Sumter County, Florida, for September 1985. The Upper Floridan aquifer is the principal source of potable water in the area. The focus of the map is the potentiometric surface in the Jumper Creek Canal area. Water level measurements were made on approximately 60 wells. The potentiometric surface ranged in altitude from more than 90 feet in the southeastern part of the county to less than 40 feet northwest of Lake Panasoffkee in the west-central area. (USGS)","language":"ENGLISH","doi":"10.3133/ofr85681","usgsCitation":"Bradner, L.A., 1985, Potentiometric surface of the upper Floridan Aquifer in central Sumter County, Florida, September 1985: U.S. Geological Survey Open-File Report 85-681, 1 map :photocopy ;73 x 64 cm., on sheet 87 x 77 cm., https://doi.org/10.3133/ofr85681.","productDescription":"1 map :photocopy ;73 x 64 cm., on sheet 87 x 77 cm.","costCenters":[],"links":[{"id":175455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79009,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0681/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682dd8","contributors":{"authors":[{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":224610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11357,"text":"ofr84603 - 1985 - Effects of storm-water runoff on an urban lake, Lake Ellyn at Glen Ellyn, Illinois","interactions":[],"lastModifiedDate":"2018-01-30T20:58:00","indexId":"ofr84603","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-603","title":"Effects of storm-water runoff on an urban lake, Lake Ellyn at Glen Ellyn, Illinois","docAbstract":"Detention of urban runoff was observed to have physical, chemical, and biological effects on a small lake located near Chicago, Illinois. Accumulated bottom sediments reduce lake storage and have comparatively high concentrations of metals and organic compounds. Concentrations of many constituents dissolved in the lake water are seasonally cyclic, with annual concentration peaks occurring during the winter. Maintenance of desirable benthic invertebrate and fish communities, and development of undesirable phytoplankton blooms appear to be inhibited by sediments deposited on the lake bottom and suspended in the lake water. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84603","usgsCitation":"Striegl, R.G., 1985, Effects of storm-water runoff on an urban lake, Lake Ellyn at Glen Ellyn, Illinois: U.S. Geological Survey Open-File Report 84-603, iv, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84603.","productDescription":"iv, 30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0603/report-thumb.jpg"},{"id":39184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0603/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610a81","contributors":{"authors":[{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":162992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30163,"text":"wri844261 - 1985 - Water-quality characteristics of streams in the Piceance Creek and Yellow Creek drainage basins, northwestern Colorado, water years 1977-81","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri844261","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4261","title":"Water-quality characteristics of streams in the Piceance Creek and Yellow Creek drainage basins, northwestern Colorado, water years 1977-81","docAbstract":"Physical and chemical data for streams in the Piceance Creek and Yellow Creek drainage basins, Colorado collected during the 1977-81 water years are summarized. Stream temperatures ranged from -0.5 to 35.0 degrees Celsius and were warmest near the downstream reaches of Piceance and Yellow Creeks. Minimum concentrations of dissolved oxygen were greater than 3.0 milligrams per liter in Piceance and Yellow Creeks, and concentrations of dissolved oxygen exceeded saturation during periods of active photosynthesis. Values of pH in streams ranged from 6.9 to 9.0 and were least during snowmelt runoff and greatest in low flows in the lower reaches of Piceance and Yellow Creeks. Concentrations of suspended sediment exceeded 100 ,000 milligrams per liter in localized runoff. Specific conductance varied inversely with discharge. Sodium, magnesium, bicarbonate, and sulfate ions and concentration ranges of dissolved solids between 400 and 1,700 milligrams per liter were characteristic of the water quality of the perennial streams. Calcium and bicarbonate dominated the major ions, and concentrations of dissolved solids normally were less than 600 milligrams per liter in the intermittent streams during storm and snowmelt runoff. Augmentation to Piceance and Yellow Creeks from ground-water sources in the lower reaches of both streams increased concentrations of dissolved solids several thousand milligrams per liter during medium and low flows and caused a change in water-quality type from sodium magnesium bicarbonate to a high-percentage sodium bicarbonate. Increases in dissolved concentrations of arsenic, boron, fluoride, lithium, strontium, and sulfate were related to ground-water sources or discharges from areas of energy resource development. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844261","usgsCitation":"Tobin, R., Stranathan, H., and Covay, K., 1985, Water-quality characteristics of streams in the Piceance Creek and Yellow Creek drainage basins, northwestern Colorado, water years 1977-81: U.S. Geological Survey Water-Resources Investigations Report 84-4261, vii, 80 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844261.","productDescription":"vii, 80 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4261/report-thumb.jpg"},{"id":58964,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4261/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f58ad","contributors":{"authors":[{"text":"Tobin, R.L.","contributorId":34143,"corporation":false,"usgs":true,"family":"Tobin","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":202792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stranathan, H.E.","contributorId":96698,"corporation":false,"usgs":true,"family":"Stranathan","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":202794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Covay, K.J.","contributorId":44948,"corporation":false,"usgs":true,"family":"Covay","given":"K.J.","affiliations":[],"preferred":false,"id":202793,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28863,"text":"wri854114 - 1985 - Results of test drilling and hydrogeology of Capps Coal Field, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri854114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4114","title":"Results of test drilling and hydrogeology of Capps Coal Field, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri854114","usgsCitation":"Nelson, G.L., 1985, Results of test drilling and hydrogeology of Capps Coal Field, Alaska: U.S. Geological Survey Water-Resources Investigations Report 85-4114, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854114.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4114/report-thumb.jpg"},{"id":57741,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4114/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60560f","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200524,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8908,"text":"ofr85159 - 1985 - Water-quality data for Marsh Creek, Rock Creek, and Cedar Draw, southern Idaho, 1979-81","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr85159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-159","title":"Water-quality data for Marsh Creek, Rock Creek, and Cedar Draw, southern Idaho, 1979-81","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85159","usgsCitation":"Frenzel, S., and Jones, M., 1985, Water-quality data for Marsh Creek, Rock Creek, and Cedar Draw, southern Idaho, 1979-81: U.S. Geological Survey Open-File Report 85-159, iv, 43 p. :maps ;28 cm., https://doi.org/10.3133/ofr85159.","productDescription":"iv, 43 p. :maps ;28 cm.","costCenters":[],"links":[{"id":141748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0159/report-thumb.jpg"},{"id":36516,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0159/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fad47","contributors":{"authors":[{"text":"Frenzel, S.A.","contributorId":9246,"corporation":false,"usgs":true,"family":"Frenzel","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":158529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, M.L.","contributorId":88731,"corporation":false,"usgs":true,"family":"Jones","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":158530,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27125,"text":"wri854077 - 1985 - Cost effectiveness of the stream-gaging program in Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:22:12","indexId":"wri854077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4077","title":"Cost effectiveness of the stream-gaging program in Pennsylvania","docAbstract":"This report documents a cost-effectiveness study of the stream-gaging program in Pennsylvania. Data uses and funding were identified for 223 continuous-record stream gages operated in 1983; four are planned for discontinuance at the close of water-year 1985; two are suggested for conversion, at the beginning of the 1985 water year, for the collection of only continuous stage records. Two of 11 special-purpose short-term gages are recommended for continuation when the supporting project ends; eight of these gages are to be discontinued and the other will be converted to a partial-record type. Current operation costs for the 212 stations recommended for continued operation is $1,199,000 per year in 1983. The average standard error of estimation for instantaneous streamflow is 15.2%. An overall average standard error of 9.8% could be attained on a budget of $1,271,000, which is 6% greater than the 1983 budget, by adopted cost-effective stream-gaging operations. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854077","usgsCitation":"Flippo, H., and Behrendt, T., 1985, Cost effectiveness of the stream-gaging program in Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 85-4077, v, 108 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854077.","productDescription":"v, 108 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":158720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4077/report-thumb.jpg"},{"id":55987,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4077/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686633","contributors":{"authors":[{"text":"Flippo, H.N.","contributorId":97948,"corporation":false,"usgs":true,"family":"Flippo","given":"H.N.","affiliations":[],"preferred":false,"id":197597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behrendt, T.E.","contributorId":27887,"corporation":false,"usgs":true,"family":"Behrendt","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":197596,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28593,"text":"wri854036 - 1985 - Cost-effectiveness of the stream-gaging program in North Carolina","interactions":[],"lastModifiedDate":"2017-01-24T10:22:00","indexId":"wri854036","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4036","title":"Cost-effectiveness of the stream-gaging program in North Carolina","docAbstract":"This report documents the results of a study of the cost-effectiveness of the stream-gaging program in North Carolina. Data uses and funding sources are identified for the 146 gaging stations currently operated in North Carolina with a budget of $777,600 (1984). As a result of the study, eleven stations are nominated for discontinuance and five for conversion from recording to partial-record status. Large parts of North Carolina 's Coastal Plain are identified as having sparse streamflow data. This sparsity should be remedied as funds become available. Efforts should also be directed toward defining the efforts of drainage improvements on local hydrology and streamflow characteristics. The average standard error of streamflow records in North Carolina is 18.6 percent. This level of accuracy could be improved without increasing cost by increasing the frequency of field visits and streamflow measurements at stations with high standard errors and reducing the frequency at stations with low standard errors. A minimum budget of $762,000 is required to operate the 146-gage program. A budget less than this does not permit proper service and maintenance of the gages and recorders. At the minimum budget, and with the optimum allocation of field visits, the average standard error is 17.6 percent.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854036","usgsCitation":"Mason, R., and Jackson, N., 1985, Cost-effectiveness of the stream-gaging program in North Carolina: U.S. Geological Survey Water-Resources Investigations Report 85-4036, vi, 109 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854036.","productDescription":"vi, 109 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":57422,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4036/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4036/report-thumb.jpg"}],"country":"United States","state":"North 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Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68460d","contributors":{"authors":[{"text":"Mason, R.R.","contributorId":34520,"corporation":false,"usgs":true,"family":"Mason","given":"R.R.","affiliations":[],"preferred":false,"id":200080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackson, N.M.","contributorId":47375,"corporation":false,"usgs":true,"family":"Jackson","given":"N.M.","affiliations":[],"preferred":false,"id":200081,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26913,"text":"wri844093 - 1985 - The quality of water in the principal aquifers of southwestern Washington","interactions":[],"lastModifiedDate":"2021-11-19T22:52:59.066708","indexId":"wri844093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4093","title":"The quality of water in the principal aquifers of southwestern Washington","docAbstract":"The quality of water in major aquifers in southwestern Washington was addressed in terms of inorganic-constituent, trace-metal, and fecal-coliform concentrations. Results of this assessment indicate that the groundwater in southwestern Washington can be characterized as soft to moderately hard with a low concentration of dissolved solids. Nitrate was the only constituent found at concentrations above maximum contaminant levels specified by the U.S. Environmental Protection Agency primary drinking water regulations. The most prevalent detriment to the otherwise good quality of groundwater in the region was concentrations of iron and manganese that exceeds limits recommended by the U.S. Environmental Protection Agency secondary standards. Although these limits were exceeded in less than one half of the samples, high concentrations of iron and manganese were common throughout the entire region.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844093","usgsCitation":"Ebbert, J., and Payne, K.L., 1985, The quality of water in the principal aquifers of southwestern Washington: U.S. Geological Survey Water-Resources Investigations Report 84-4093, Report: v, 59 p.; 5 Plates: 32.60 × 25.46 inches or smaller, https://doi.org/10.3133/wri844093.","productDescription":"Report: v, 59 p.; 5 Plates: 32.60 × 25.46 inches or smaller","costCenters":[],"links":[{"id":55794,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4093/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55793,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4093/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391965,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35984.htm"},{"id":55795,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4093/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55792,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4093/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55791,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4093/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55790,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4093/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4093/report-thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.25,\n 45.531\n ],\n [\n -122.467,\n 45.531\n ],\n [\n -122.467,\n 47.25\n ],\n [\n -124.25,\n 47.25\n ],\n [\n -124.25,\n 45.531\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db64105a","contributors":{"authors":[{"text":"Ebbert, J.C.","contributorId":57451,"corporation":false,"usgs":true,"family":"Ebbert","given":"J.C.","affiliations":[],"preferred":false,"id":197235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Payne, K. L.","contributorId":31771,"corporation":false,"usgs":true,"family":"Payne","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197234,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27494,"text":"wri844299 - 1985 - Low-flow frequency analyses for streams in west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri844299","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4299","title":"Low-flow frequency analyses for streams in west-central Florida","docAbstract":"The log-Pearson type III distribution was used for defining low-flow frequency at 116 continuous-record streamflow stations in west-central Florida. Frequency distributions were calculated for 1, 3, 7, 14, 30, 60, 90, 120, and 183 consecutive-day periods for recurrence intervals of 2, 5, 10, and 20 years. Discharge measurements at more than 100 low-flow partial-record stations and miscellaneous discharge-measurement stations were correlated with concurrent daily mean discharge at continuous-record stations. Estimates of the 7-day, 2-year; 7-day, 10-year; 30-day, 2-year; and 30-day, 10-year discharges were made for most of the low-flow partial-record and miscellaneous discharge-measurement stations based on those correlations. Multiple linear-regression analysis was used in an attempt to mathematically relate low-flow frequency data to basin characteristics. The resulting equations showed an apparent bias and were considered unsatisfactory for use in estimating low-flow characteristics. Maps of the 7-day, 10-year and 30-day, 10-year low flows are presented. Techniques that can be used to estimate low-flow characteristics at an ungaged site are also provided. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844299","usgsCitation":"Hammett, K., 1985, Low-flow frequency analyses for streams in west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4299, iv, 116 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844299.","productDescription":"iv, 116 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4299/report-thumb.jpg"},{"id":56344,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4299/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56345,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4299/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56346,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4299/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648731","contributors":{"authors":[{"text":"Hammett, K.M.","contributorId":59006,"corporation":false,"usgs":true,"family":"Hammett","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":198212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28424,"text":"wri854146 - 1985 - Summary of northern Atlantic Coastal Plain hydrology and its relation to disposal of high-level radioactive waste in buried crystalline rock – A preliminary appraisal","interactions":[],"lastModifiedDate":"2021-12-14T22:25:16.309266","indexId":"wri854146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4146","title":"Summary of northern Atlantic Coastal Plain hydrology and its relation to disposal of high-level radioactive waste in buried crystalline rock – A preliminary appraisal","docAbstract":"Interpretation of available hydrologic data suggests that some areas beneath the Coastal Plain in the States of Delaware, Maryland, New Jersey, North Carolina, and Virginia might have some potential for the disposal of nuclear waste in crystalline rock that is buried beneath the Coastal Plain sediments. The areas of major interest occur where the top of the basement rock lies between 1,000 and 4,000 feet below sea level, the aquifer(s) immediately above the basement rock are saturated with saline water, confining material overlies the saline water bearing aquifer(s), and groundwater flow in the saline water aquifer(s) can be established. Preliminary data on (1) the distribution and thickness of the lowermost aquifers and confining beds, (2) the distribution of hydraulic conductivity in the lowermost aquifers, (3) estimated hydraulic heads and inferred direction of lateral groundwater flow for 1980, and (4) the distribution of saline water and brine, indicate eastern parts of the study area relatively best meet most of the criteria proposed for sediments that would overlie any potential buried crystalline-rock disposal site.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854146","usgsCitation":"Lloyd, O., Larson, J.D., and Davis, R.W., 1985, Summary of northern Atlantic Coastal Plain hydrology and its relation to disposal of high-level radioactive waste in buried crystalline rock – A preliminary appraisal: U.S. Geological Survey Water-Resources Investigations Report 85-4146, vi, 132 p., https://doi.org/10.3133/wri854146.","productDescription":"vi, 132 p.","costCenters":[],"links":[{"id":392912,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36309.htm"},{"id":57227,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4146/report-thumb.jpg"}],"country":"United States","state":"Delaware, Maryland, New Jersey, North Carolina, Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.5,\n 33.833\n ],\n [\n -74,\n 33.833\n ],\n [\n -74,\n 40.5\n ],\n [\n -79.5,\n 40.5\n ],\n [\n -79.5,\n 33.833\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a55ea","contributors":{"authors":[{"text":"Lloyd, O. B.","contributorId":75189,"corporation":false,"usgs":true,"family":"Lloyd","given":"O. B.","affiliations":[],"preferred":false,"id":199771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larson, J. D.","contributorId":83084,"corporation":false,"usgs":true,"family":"Larson","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":199772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199773,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":65267,"text":"i1733 - 1985 - Controlled photomosaic of part of the Alba Patera Region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:09","indexId":"i1733","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1733","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Alba Patera Region of Mars","language":"ENGLISH","doi":"10.3133/i1733","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Controlled photomosaic of part of the Alba Patera Region of Mars: U.S. Geological Survey IMAP 1733, 1 remote-sensing image ;62 x 59 cm., on sheet 96 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1733.","productDescription":"1 remote-sensing image ;62 x 59 cm., on sheet 96 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260753,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1733/plate-1.pdf"}],"scale":"502000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68aace","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57246,"text":"wdrAR841 - 1985 - Water resources data, Arkansas, water year 1984","interactions":[],"lastModifiedDate":"2019-10-01T16:04:25","indexId":"wdrAR841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-84-1","title":"Water resources data, Arkansas, water year 1984","docAbstract":"No abstract available.
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Geological Survey, in cooperation with the Santa Clara Valley Water District, has completed a study of ground-water recharge by injection in the Palo Alto baylands along San Francisco Bay, California. Selected wells within the Water District 's injection-extraction network were monitored to determine hydraulic and chemical interactions affecting well-field operation. The well field was installed to prevent and eliminate saline contamination in the local shallow aquifer system. The primary focus of this study is on factors that affect injection efficiency, specifically well and aquifer clogging. Mixing and break-through curves for major chemical constituents indicate ion exchange, adsorption, and dissolution reactions. Freshwater breakthrough was detected in water-level data, which reflected fluid-density change as well as head buildup. Dissolution of calcium carbonate caused by dilution of saline ground water probably accounts for an apparent increase in specific capacity possibly related to improved aquifer permeability. Adsorption evidently removed trace elements during passage of injected water through the aquifer. In terms of hydraulic and chemical compatibility, the well field is a viable system for ground-water recharge. Aquifer heterogeneity and operational constraints reduce the efficiency of the system. Efficiency may be maximized by careful attention to extraction distribution and quantity and to injection distribution, quantity, and water quality. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844152","usgsCitation":"Hamlin, S.N., 1985, An investigation of ground-water recharge by injection in the Palo Alto Baylands, California: Hydraulic and chemical interactions — Final report: U.S. Geological Survey Water-Resources Investigations Report 84-4152, vi, 61 p., https://doi.org/10.3133/wri844152.","productDescription":"vi, 61 p.","costCenters":[],"links":[{"id":394365,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36025.htm"},{"id":56341,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4152/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158584,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4152/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Palo Alto Baylands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.1298599243164,\n 37.42852418375166\n ],\n [\n -122.09999084472658,\n 37.42852418375166\n ],\n [\n -122.09999084472658,\n 37.45823569268173\n ],\n [\n -122.1298599243164,\n 37.45823569268173\n ],\n [\n -122.1298599243164,\n 37.42852418375166\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68429c","contributors":{"authors":[{"text":"Hamlin, S. N.","contributorId":46560,"corporation":false,"usgs":true,"family":"Hamlin","given":"S.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":198208,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47716,"text":"wri854112 - 1985 - Maps of the Bonsall area of the San Luis Rey River valley, San Diego County, California, showing geology, hydrology, and ground-water quality","interactions":[],"lastModifiedDate":"2015-09-24T15:20:56","indexId":"wri854112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4112","title":"Maps of the Bonsall area of the San Luis Rey River valley, San Diego County, California, showing geology, hydrology, and ground-water quality","docAbstract":"In November 1984, 84 wells and 1 spring in the Bonsall area of the San Luis Rey River valley were inventoried by U.S. Geological Survey personnel. Depth to water in 38 wells ranged from 1.3 to 38 ft and 23 wells had depths to water less than 10 feet. Dissolved solids concentration of water from 29 wells and 1 spring sampled in autumn 1983 and spring 1984 ranged from 574 to 2,370 mgs/L. Groundwater with a dissolved solids concentration less than 1,000 mgs/L was generally restricted to the eastern part of the aquifer. The total volume of alluvial fill in the Bonsall area is 113,000 acre-feet; the amount of groundwater storage available in the alluvial aquifer is 18,000 acre-feet. The alluvial aquifer is, in part, surrounded and underlain by colluvium and weathered crystalline rock that add some additional groundwater storage capacity to the system. Data in this report are presented on five maps showing well locations , thickness of alluvial fill, water level contours in November 1983 and hydrographs of selected wells, groundwater quality in spring 1960 and graphs showing changes in dissolved solids concentrations of water from selected wells with time, and groundwater quality in spring 1984. This report is part of a larger cooperative project between the Rainbow Municipal Irrigation District and the U.S. Geological Survey. The purpose of the larger project is to develop an appropriate groundwater management plan for the Bonsall area of the San Luis Rey River valley. (USGS)
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