In December 1980, the U.S. Geological Survey (USGS), in cooperation with the U.S. Army Corps of Engineers (COE), conducted a seismic survey of the Mississippi River in the vicinity of Alton, Illinois, near St. Louis, Missouri (fig. 1). Seismic lines were run from the mouth of the Missouri River up the Mississippi River to a point approximately seven miles upriver from Lock and Dam No. 26 at Alton, Illinois (fig. 2a,b). Additional lines were run upriver from Lock and Dam No. 25 between the dam and River Mile 244, but these data are not reported because of mechanical problems with the larger sound-source equipment and inexact navigational control.
The objective of the cooperative study was to utilize marine common-depth-point (CDP), digital, and multichannel techniques to locate a monoclinal flexure of the Cap au Gres Fault that earlier had been interpreted from land seismic data to be in the vicinity of Lock and Dam No 26 (Shannon and Wilson, 1980). A second objective was to demonstrate that the marine seismic system could be used for making relatively deep penetration seismic-reflection surveys on shallow (less than 10-m water depth) inland waterways that have organic sediment floors.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8482","usgsCitation":"Winget, E.A., and Tirey, G.B., 1984, U.S. Geological Survey common-depth-point seismic-reflection survey between Mississippi River miles 195 and 210 (R/V NEECHO cruise NE-80-3): U.S. Geological Survey Open-File Report 84-82, 5 p., https://doi.org/10.3133/ofr8482.","productDescription":"5 p.","costCenters":[],"links":[{"id":391454,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13576.htm"},{"id":39583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0082/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":145062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0082/report-thumb.jpg"}],"country":"United States","state":"Illinois, Missouri","otherGeospatial":"Mississippi River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.333,\n 38.9350\n ],\n [\n -90.333,\n 38.7960\n ],\n [\n -90.083,\n 38.7960\n ],\n [\n -90.083,\n 38.9350\n ],\n [\n -90.333,\n 38.9350\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db612e27","contributors":{"authors":[{"text":"Winget, E. A.","contributorId":78748,"corporation":false,"usgs":true,"family":"Winget","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":163589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tirey, G. B.","contributorId":95891,"corporation":false,"usgs":true,"family":"Tirey","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":163590,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18561,"text":"ofr84132 - 1984 - Water quality of the tidal Potomac River and Estuary; hydrologic data report supplement, 1979 through 1981 water years","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr84132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-132","title":"Water quality of the tidal Potomac River and Estuary; hydrologic data report supplement, 1979 through 1981 water years","docAbstract":"This report is a companion report to the U.S. Geological Survey 1979, 1980, and 1981 Hydrologic Data Reports of the tidal Potomac River and Estuary. It contains values of biochemical oxygen demand and specific rate constants, incident light and light attenuation measurements; numbers of phytoplankton, fecal coliform and fecal streptococci, cross-sectional averages from field measurements of dissolved oxygen, pH, specific conductance , and temperature data; and cross-sectional averages of chlorophyll data. Sewage treatment plant loads are also included. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey :\r\nOpen-File Services Section, Western Distribution Branch,","doi":"10.3133/ofr84132","usgsCitation":"Coupe, R., and Webb, W., 1984, Water quality of the tidal Potomac River and Estuary; hydrologic data report supplement, 1979 through 1981 water years: U.S. Geological Survey Open-File Report 84-132, iii, 360 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84132.","productDescription":"iii, 360 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0132/report-thumb.jpg"},{"id":47913,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9817","contributors":{"authors":[{"text":"Coupe, R.H.","contributorId":84778,"corporation":false,"usgs":true,"family":"Coupe","given":"R.H.","affiliations":[],"preferred":false,"id":179340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Webb, W.E.","contributorId":85247,"corporation":false,"usgs":true,"family":"Webb","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":179341,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15627,"text":"ofr84713 - 1984 - Ground-water resources of Limestone County, Texas","interactions":[],"lastModifiedDate":"2016-08-11T16:35:01","indexId":"ofr84713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-713","title":"Ground-water resources of Limestone County, Texas","docAbstract":"Limestone County, located in east-central Texas, has small to plentiful ground-water supplies available, depending upon the location within the county. The Wilcox Group in the eastern part of the county has adequate supplies to meet the expected water demands in the foreseeable future. The thicker zones of the Wilcox Group can supply yields in excess of 500 gallons per minute. The Midway Group can supply yields in excess of 100 gallons per minute from the Tehuacana Member of the Kincaid Formation. This represents the largest well yields from the Midway Group in Texas. The Midway Group elsewhere in the State is mostly a poor water producer and is not considered an aquifer. The Taylor Marl and Navarro Group furnish only small quantities of ground water to wells in the western part of the county where these units crop out. The Hosston and Travis Peak Formations are present at depths in excess of 2,000 feet. These formations, which contain slightly saline water in the western part of the county, could be expected to produce water with a temperature of about 150°F that might be used for heating purposes.
\nAbout 0.9 million gallons per day of ground water was used for all purposes in 1980. This use has declined since 1955 but is expected to increase as additional public-supply and industrial wells are being developed. The Wilcox Group is capable of annually yielding at least 14,000 acre-feet or 11.6 million gallons per day of water to wells on a long-term basis.
\nGenerally, the ground water is of acceptable quality for most uses. Relatively high dissolved-solids and iron concentrations are the major water-quality problems. Water-quality problems that may be the result of man's activities are limited to a small oilfield area near Mexia.
\nLignite mining from the Wilcox Group is expected to take place in the foreseeable future. The collection of additional hydrologic data on the Wilcox would be desirable before, during, and after mining.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Ausitn, TX","doi":"10.3133/ofr84713","usgsCitation":"Rettman, P., 1984, Ground-water resources of Limestone County, Texas: U.S. Geological Survey Open-File Report 84-713, vi, 92 p., https://doi.org/10.3133/ofr84713.","productDescription":"vi, 92 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":147309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0713/report-thumb.jpg"},{"id":44590,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0713/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Limestone County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.4998,31.8005],[-96.4298,31.7011],[-96.2333,31.4115],[-96.3228,31.3661],[-96.3236,31.3593],[-96.5948,31.2235],[-96.8,31.5192],[-96.9329,31.7114],[-96.7184,31.8195],[-96.4998,31.8005]]]},\"properties\":{\"name\":\"Limestone\",\"state\":\"TX\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d38","contributors":{"authors":[{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":171457,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17031,"text":"ofr84146 - 1984 - Data from pumping and injection tests and chemical sampling in the geothermal aquifer at Klamath Falls, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr84146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-146","title":"Data from pumping and injection tests and chemical sampling in the geothermal aquifer at Klamath Falls, Oregon","docAbstract":"A seven-week pumping and injection tests in the geothermal aquifer at Klamath Falls, Oregon, in 1983 provided new information on hydraulic properties of the aquifer. The Open-File Data Report on the tests includes graphs of water levels measured in 50 wells, temperature measurement in 17 wells , daily air-temperatures in relation to discharge of thermal water from more than 70 pumped and artesian wells, tables of monthly mean air temperatures and estimates of discharges of thermal water during a normal year, and tables of chemical and isotopic analyses on samples from 12 wells. The water-level measurements reflect the effects of pumping, injection, and recovery over about 1.7 square miles of the hot-well area of Klamath Falls. The pumped well, City Well No 1, and the injection well at the Klamath County Museum are components of a proposed District Heating Plan. The study was funded principally under contracts from the U.S. Department of Energy to the Lawrence Berkeley Laboratory, Stanford University, and the Oregon Institute of Technology, with coordination and chemical sampling provided under the Geothermal Research Program, U.S. Geological Survey. Support was received from the City of Klamath Falls, Klamath County Chamber of Commerce, Citizens for Responsible Geothermal Development, and many citizen volunteers. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84146","usgsCitation":"Benson, S., Janik, C.J., Long, D., Solbau, R., and Lienau, P., 1984, Data from pumping and injection tests and chemical sampling in the geothermal aquifer at Klamath Falls, Oregon: U.S. Geological Survey Open-File Report 84-146, viii, 114 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84146.","productDescription":"viii, 114 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":147869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0146/report-thumb.jpg"},{"id":46163,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0146/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c936","contributors":{"authors":[{"text":"Benson, S.M.","contributorId":102901,"corporation":false,"usgs":true,"family":"Benson","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":174658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Janik, C. J.","contributorId":10795,"corporation":false,"usgs":true,"family":"Janik","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":174654,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Long, D.C.","contributorId":26702,"corporation":false,"usgs":true,"family":"Long","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":174655,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Solbau, R.D.","contributorId":48985,"corporation":false,"usgs":true,"family":"Solbau","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":174657,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lienau, P.J.","contributorId":30643,"corporation":false,"usgs":true,"family":"Lienau","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":174656,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":18620,"text":"ofr82320 - 1984 - Hole-to-surface resistivity measurements at Gibson Dome (drill hole GD-1) Paradox basin, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr82320","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-320","title":"Hole-to-surface resistivity measurements at Gibson Dome (drill hole GD-1) Paradox basin, Utah","docAbstract":"Hole-to-surface resistivity measurements were made in a deep drill hole (GD-1), in San Juan County, Utah, which penetrated a sequence of sandstone, shale, and evaporite. These measurements were made as part of a larger investigation to study the suitability of an area centered around the Gibson Dome structure for nuclear waste disposal. The magnitude and direction of the total electric field resulting from a current source placed in a drill hole is calculated from potential difference measurements for a grid of closely-spaced stations. A contour map of these data provides a detailed map of the distribution of the electric field away from the drill hole. Computation of the apparent resistivity from the total electric field helps to interpret the data with respect to the ideal situation of a layered earth. Repeating the surface measurements for different source depths gives an indication of variations in the geoelectric section with depth. \r\n\r\nThe quantitative interpretation of the field data at Gibson Dome was hindered by the pressure of a conductive borehole fluid. However, a qualitative interpretation of the field data indicates the geoelectric section around drill hole GD-1 is not perfectly layered. The geoelectric section appears to dip to the northwest, and contains anomalies in the resistivity distribution that may be representative of localized thickening or folding of the salt layers.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82320","usgsCitation":"Daniels, J., 1984, Hole-to-surface resistivity measurements at Gibson Dome (drill hole GD-1) Paradox basin, Utah: U.S. Geological Survey Open-File Report 82-320, 28 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82320.","productDescription":"28 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0320/report-thumb.jpg"},{"id":47960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0320/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bf9b","contributors":{"authors":[{"text":"Daniels, J.J.","contributorId":75929,"corporation":false,"usgs":true,"family":"Daniels","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":179442,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10730,"text":"ofr84750 - 1984 - Relation of urban land-use and dry-weather, storm, and snowmelt flow characteristics to stream-water quality, Shunganunga Creek basin, Topeka, Kansas","interactions":[],"lastModifiedDate":"2017-09-29T16:00:28","indexId":"ofr84750","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-750","title":"Relation of urban land-use and dry-weather, storm, and snowmelt flow characteristics to stream-water quality, Shunganunga Creek basin, Topeka, Kansas","docAbstract":"Overland runoff from urban areas can cause concentrations of some water-quality constituents in local receiving streams to increase. The U.S. Geological Survey in cooperation with the Kansas Department of Health and Environment investigated the water-quality characteristics of streams draining Topeka, Kansas, and adjacent parts of the Shunganunga Creek basin from October 1979 through November 1981. The purpose of this investigation was to provide the data and interpretation necessary to determine the effects of runoff from urban areas on the water-quality characteristics of receiving streams.
Water-quality characteristics for three streamflow conditions were determined: (1) dry-weather streamflow--a combination of base flow and point-source contributions, (2) storm streamflow--mainly provided by overland runoff from storms, and (3) snowmelt streamflow- mainly provided by overland runoff from snowmelt.
Median concentrations of trace metals and nutrients were larger in storm streamflow than in dry-weather streamflow. Median concentrations of total lead and zinc were largest in storm streamflow from the more urban basins. Regression equations were developed to estimate median concentrations of total lead and zinc in storm streamflow from the percentage of drainage area in residential plus commercial land-use areas (correlation coefficients were 0.98 for total lead and 0.88 for total zinc); and from street density in lane miles per square mile (correlation coefficients were 0.89 for total lead and 0.84 for total zinc). Median concentrations of dissolved nitrite plus nitrate nitrogen and total phosphorus averaged, respectively, 76-percent and 70-percent larger during storm streamflow than during dry-weather streamflow and were largest in storm streamflow from the more agricultural basins.
Median concentrations of dissolved sodium, chloride, and solids in snowmelt streamflow at all study sites averaged 218-percent larger for dissolved sodium, 296-percent larger for dissolved chloride, and 71-percent larger for dissolved solids relative to median concentrations in dry-weather streamflow. Regression equations also were developed to estimate median concentrations of dissolved sodium, chloride, and solids in snowmelt streamflow from the summation of percentages of the drainage area in residential, commercial, and industrial land-use areas (correlation coefficients were 0.97 for each of the three relationships) and from street density in lane miles per square mile (correlation coefficients were 0.93 for dissolved sodium and 0.94 for both dissolved chloride and dissolved solids).
Multiple-correlation and regression analysis relating storm-runoff volumes and average constituent concentrations to land-use and storm characteristics produced significant relations (0.05 level of significance) for storm-runoff volume (0.81 coefficient of determination), total lead (0.71 coefficient of determination), total zinc (0.50 coefficient of determination), and suspended sediment (0.58 coefficient of determination).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84750","collaboration":"Prepared in cooperation with the Kansas Department of Health and Environment","usgsCitation":"Pope, L.M., and Bevans, H.E., 1984, Relation of urban land-use and dry-weather, storm, and snowmelt flow characteristics to stream-water quality, Shunganunga Creek basin, Topeka, Kansas: U.S. Geological Survey Open-File Report 84-750, vi, 64 p., https://doi.org/10.3133/ofr84750.","productDescription":"vi, 64 p.","costCenters":[],"links":[{"id":143526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0750/report-thumb.jpg"},{"id":346272,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0750/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","city":"Topeka","otherGeospatial":"Shunganunga Creek basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.84747314453125,\n 38.96154447940714\n ],\n [\n -95.53985595703124,\n 38.96154447940714\n ],\n [\n -95.53985595703124,\n 39.131125517089906\n ],\n [\n -95.84747314453125,\n 39.131125517089906\n ],\n [\n -95.84747314453125,\n 38.96154447940714\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6349e1","contributors":{"authors":[{"text":"Pope, Larry M.","contributorId":93455,"corporation":false,"usgs":true,"family":"Pope","given":"Larry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":161868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bevans, Hugh E.","contributorId":11589,"corporation":false,"usgs":true,"family":"Bevans","given":"Hugh","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18673,"text":"ofr8499 - 1984 - Geologic bibliography for selected onshore sedimentary basins of central and southern Alaska stressing basin analysis and including an index of publicly available well and subsurface data","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr8499","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-99","title":"Geologic bibliography for selected onshore sedimentary basins of central and southern Alaska stressing basin analysis and including an index of publicly available well and subsurface data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8499","usgsCitation":"DiBona, P., and Kirschner, C., 1984, Geologic bibliography for selected onshore sedimentary basins of central and southern Alaska stressing basin analysis and including an index of publicly available well and subsurface data: U.S. Geological Survey Open-File Report 84-99, i, 72 p. :map ;28 cm., https://doi.org/10.3133/ofr8499.","productDescription":"i, 72 p. :map ;28 cm.","costCenters":[],"links":[{"id":151443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0099/report-thumb.jpg"},{"id":48011,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0099/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a64db","contributors":{"authors":[{"text":"DiBona, P.A.","contributorId":98583,"corporation":false,"usgs":true,"family":"DiBona","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":179540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirschner, C.E.","contributorId":81107,"corporation":false,"usgs":true,"family":"Kirschner","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":179539,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10543,"text":"ofr84619 - 1984 - Literature review and need for additional study of surface-water quality in the Cuyahoga Valley National Recreation Area, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr84619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-619","title":"Literature review and need for additional study of surface-water quality in the Cuyahoga Valley National Recreation Area, Ohio","docAbstract":"The Cuyahoga Valley National Recreation Area encompasses about 24 miles of the middle reach of the Cuyahoga River and parts of four major tributaries -- Furnace Run, Brandywine Creek, Chippewa Creek, and TInkers Creek. Water quality in this reach does not meet Ohio water-quality standards for dissolved oxygen, fecal bacteria, ammonia, and lead. Point sources of effluent contribute contaminants. \r\n\r\nOn the basis of a review of scientific and technical literature, National Park Service management goals, and water-quality data collected by the U.S. Geological Survey, three subject areas for future study are suggested: (1) The dissolved oxygen regime, (2) chemical quality of base flow, and (3) quality of storm-water runoff.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84619","usgsCitation":"Childress, C., 1984, Literature review and need for additional study of surface-water quality in the Cuyahoga Valley National Recreation Area, Ohio: U.S. Geological Survey Open-File Report 84-619, iv, 58 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84619.","productDescription":"iv, 58 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0619/report-thumb.jpg"},{"id":38386,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0619/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eb9","contributors":{"authors":[{"text":"Childress, C.J.","contributorId":88734,"corporation":false,"usgs":true,"family":"Childress","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":161570,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16064,"text":"ofr87194 - 1984 - Upper Cretaceous (Maestrichtian) larger invertebrates from the Haustator bilira assemblage zone in the Atlantic Coastal Plain with further data for the East Gulf","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr87194","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"87-194","title":"Upper Cretaceous (Maestrichtian) larger invertebrates from the Haustator bilira assemblage zone in the Atlantic Coastal Plain with further data for the East Gulf","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87194","usgsCitation":"Sohl, N.F., and Koch, C., 1984, Upper Cretaceous (Maestrichtian) larger invertebrates from the Haustator bilira assemblage zone in the Atlantic Coastal Plain with further data for the East Gulf: U.S. Geological Survey Open-File Report 87-194, 172 p. :maps ;28 cm., https://doi.org/10.3133/ofr87194.","productDescription":"172 p. :maps ;28 cm.","costCenters":[],"links":[{"id":150321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0194/report-thumb.jpg"},{"id":44995,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0194/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a24e4b07f02db60e5bd","contributors":{"authors":[{"text":"Sohl, N. F.","contributorId":70029,"corporation":false,"usgs":true,"family":"Sohl","given":"N.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":172177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koch, C.F.","contributorId":48436,"corporation":false,"usgs":true,"family":"Koch","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":172176,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28640,"text":"wri834260 - 1984 - Potential effects of surface coal mining on the hydrology of the Corral Creek area, Hanging Woman Creek coal field, southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:39","indexId":"wri834260","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4260","title":"Potential effects of surface coal mining on the hydrology of the Corral Creek area, Hanging Woman Creek coal field, southeastern Montana","docAbstract":"The Corral Creek area of the Hanging Woman Creek coal field, 9 miles east of the Decker coal mines near the Tongue River, contains large reserves of Federal coal that have been identified for potential lease sale. A hydrologic study was conducted in the area to describe existing hydrologic systems and to study assess potential impacts of surface coal mining on local water resources. Hydrogeologic data collected indicate that aquifers are coal and sandstone beds within the Tongue River Member of the Fort Union Formation (Paleocene age) and sand and gravel in valley alluvium (Pleistocene and Holocene age). Surface-water resources are limited to a few spring-fed stock ponds in the higher parts of the area and the intermittent flow of Corral Creek near the mouth. Most of the stock ponds in the area become dry by midsummer. Mining of the Anderson coal bed would remove three stock wells and would lower the potentiometric surface within the coal and sandstone aquifers. The alluvial aquifer beneath Corral Creek and South Fork would be removed. Although mining would alter the existing hydrologic systems and remove several shallow wells, alternative ground-water supplies are available that could be developed to replace those lost by mining. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834260","usgsCitation":"McClymonds, N.E., 1984, Potential effects of surface coal mining on the hydrology of the Corral Creek area, Hanging Woman Creek coal field, southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 83-4260, v, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834260.","productDescription":"v, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4260/report-thumb.jpg"},{"id":57475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4260/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a628f","contributors":{"authors":[{"text":"McClymonds, N. E.","contributorId":94653,"corporation":false,"usgs":true,"family":"McClymonds","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30138,"text":"wri834121C - 1984 - Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Texas","interactions":[],"lastModifiedDate":"2021-12-21T20:19:56.28278","indexId":"wri834121C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4121","chapter":"C","title":"Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Texas","docAbstract":"This map report is one of a series of geologic and hydrologic maps of States in the Basin and Range Province. These map reports contain information on ground-water hydrology, ground-water quality, surface distribution of selected rock types, data on tectonic conditions, areal geophysical data, Pleistocene lakes and marshes and natural resources. This information is the basis for a summary report that characterizes the Basin and Range Province. The geologic and hydrologic characterization will be used to evaluate the Province for prospective regions for further study relative to isolation of high-level radioactive waste. (Bedinger, Sargent and Reed, 1984).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834121C","collaboration":"Prepared in cooperation with the Texas Bureau of Economic Geology","usgsCitation":"Thompson, T., and Nuter, J., 1984, Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4121, Report: 5 p.; 1 Plate: 39.13 x 54.99 inches, https://doi.org/10.3133/wri834121C.","productDescription":"Report: 5 p.; 1 Plate: 39.13 x 54.99 inches","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":58948,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4121c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393240,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4121c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4121c/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Basin and Range Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.6552734375,\n 28.844673680771795\n ],\n [\n -101.7333984375,\n 28.844673680771795\n ],\n [\n -101.7333984375,\n 31.87755764334002\n ],\n [\n -106.6552734375,\n 31.87755764334002\n ],\n [\n -106.6552734375,\n 28.844673680771795\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60575d","contributors":{"authors":[{"text":"Thompson, Thomas H.","contributorId":20748,"corporation":false,"usgs":true,"family":"Thompson","given":"Thomas H.","affiliations":[],"preferred":false,"id":202746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nuter, Janet","contributorId":89003,"corporation":false,"usgs":true,"family":"Nuter","given":"Janet","email":"","affiliations":[],"preferred":false,"id":202747,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30139,"text":"wri834122C - 1984 - Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range province, Utah","interactions":[],"lastModifiedDate":"2021-12-21T20:42:31.465357","indexId":"wri834122C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4122","chapter":"C","title":"Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range province, Utah","docAbstract":"This map report is one of a series of geologic and hydrologic maps of States in the Basin and Range Province. These map reports contain information on ground-water hydrology, ground-water quality, surface distribution of selected rock types, data on tectonic conditions, areal geophysical data, Pleistocene lakes and marshes and natural resources. This information is the basis for a summary report that characterizes the Basin and Range Province. The geologic and hydrologic characterization will be used to evaluate the Province for prospective regions for further study relative to isolation of high-level radioactive waste. (Bedinger, Sargent and Reed, 1984).