The purpose of this Hydrologic Investigations Atlas is to provide a description of the geohydrologic systems in Upper Cambrian through Lower Cretaceous rocks in Kansas. This investigation was made as part of the Central Midwest Regional Aquifer-System Analysis (CMRASA). The CMRASA is one of several major investigations by the U.S. Geological Survey of regional aquifer systems in the United States. These regional investigations are designed to increase knowledge of the flow regime and hydrologic properties of major aquifer systems and to provide quantitative information for the assessment, development, and management of water supplies. The CMRASA study area includes all or parts of 10 Central Midwestern States (Jorgensen and Signor, 1981), as shown on the envelope cover.
","language":"ENGLISH","doi":"10.3133/ha722E","usgsCitation":"Hansen, C.V., Wolf, R.J., and Spinazola, J., 1992, Geohydrologic systems in Kansas; physical framework of the confining unit in the Western Interior Plains aquifer system: U.S. Geological Survey Hydrologic Atlas 722, 2 sheets; Sheet 1, 46 by 40 1/2 inches; sheet 2, 46 by 34 1/2 inches (all in color), https://doi.org/10.3133/ha722E.","productDescription":"2 sheets; Sheet 1, 46 by 40 1/2 inches; sheet 2, 46 by 34 1/2 inches (all in color)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":191629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266335,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/722e/plate-2.pdf"},{"id":266334,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/722e/plate-1.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8dca","contributors":{"authors":[{"text":"Hansen, C. V.","contributorId":74749,"corporation":false,"usgs":true,"family":"Hansen","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":280802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":280800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spinazola, J. M.","contributorId":32574,"corporation":false,"usgs":true,"family":"Spinazola","given":"J. M.","affiliations":[],"preferred":false,"id":280801,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18086,"text":"ofr92501 - 1992 - Geology, hydrology and mechanics of the Alani-Paty Landslide, Manoa Valley, Oahu, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr92501","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-501","title":"Geology, hydrology and mechanics of the Alani-Paty Landslide, Manoa Valley, Oahu, Hawaii","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr92501","usgsCitation":"Baum, R., and Reid, M., 1992, Geology, hydrology and mechanics of the Alani-Paty Landslide, Manoa Valley, Oahu, Hawaii: U.S. Geological Survey Open-File Report 92-501, iv, 87 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr92501.","productDescription":"iv, 87 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0501/report-thumb.jpg"},{"id":47440,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0501/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47441,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0501/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47442,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0501/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47443,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0501/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47444,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0501/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47445,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0501/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47446,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0501/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c658","contributors":{"authors":[{"text":"Baum, R.L.","contributorId":68752,"corporation":false,"usgs":true,"family":"Baum","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":178518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, M.E.","contributorId":108130,"corporation":false,"usgs":true,"family":"Reid","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":178519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20160,"text":"ofr91485 - 1992 - Hydrologic and sedimentologic data collected during three cruises at low water on the Mississippi River and some of its tributaries, July 1987-June 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:38","indexId":"ofr91485","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-485","title":"Hydrologic and sedimentologic data collected during three cruises at low water on the Mississippi River and some of its tributaries, July 1987-June 1988","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr91485","usgsCitation":"Moody, J.A., and Meade, R., 1992, Hydrologic and sedimentologic data collected during three cruises at low water on the Mississippi River and some of its tributaries, July 1987-June 1988: U.S. Geological Survey Open-File Report 91-485, vi, 143 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr91485.","productDescription":"vi, 143 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0485/report-thumb.jpg"},{"id":49702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0485/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117db","contributors":{"authors":[{"text":"Moody, J. A.","contributorId":32930,"corporation":false,"usgs":true,"family":"Moody","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":182170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meade, R.H.","contributorId":27449,"corporation":false,"usgs":true,"family":"Meade","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":182169,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27073,"text":"wri924073 - 1992 - Hydrologic characteristics of abandoned coal mines used as sources of public water supply in McDowell County, West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:08:41","indexId":"wri924073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4073","title":"Hydrologic characteristics of abandoned coal mines used as sources of public water supply in McDowell County, West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924073","usgsCitation":"Ferrell, G., 1992, Hydrologic characteristics of abandoned coal mines used as sources of public water supply in McDowell County, West Virginia: U.S. Geological Survey Water-Resources Investigations Report 92-4073, vi, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924073.","productDescription":"vi, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4073/report-thumb.jpg"},{"id":55943,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611649","contributors":{"authors":[{"text":"Ferrell, G.M.","contributorId":92681,"corporation":false,"usgs":true,"family":"Ferrell","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":197511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44165,"text":"ofr92160 - 1992 - Summary of hydrologic data for the San Gabriel River basin and Edwards Aquifer, Georgetown area, Texas, water year 1990","interactions":[],"lastModifiedDate":"2016-08-15T11:50:10","indexId":"ofr92160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-160","title":"Summary of hydrologic data for the San Gabriel River basin and Edwards Aquifer, Georgetown area, Texas, water year 1990","docAbstract":"The Edwards aquifer is the principal source of freshwater for municipal, domestic, and industrial users in the Georgetown area. Other sources of freshwater are Lake Georgetown and the streams draining the San Gabriel River basin. Lake Georgetown, located on the North Fork San Gabriel River west of Georgetown, is a freshwater supply for some municipalities in the area. Water in the San Gabriel River basin also suppliesa variety of needs east of Georgetown. Because of the importance of the Edwards aquifer and the surface waters as a source of freshwater in the area, the U.S. Geological Survey, in cooperation with the city of Georgetown, established a local streamflow and ground-water monitoring network in principal streams and teh Edwards aquifer, and conducted surveys of the network in water years 1987, 1988, and 1990. The study area was centered on Georgetown and emcompassed an area of about 150 mi2 (fig. 1).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr92160","usgsCitation":"Reeves, W.E., and Land, L.F., 1992, Summary of hydrologic data for the San Gabriel River basin and Edwards Aquifer, Georgetown area, Texas, water year 1990: U.S. Geological Survey Open-File Report 92-160, 39.15 x 30.46 inches, https://doi.org/10.3133/ofr92160.","productDescription":"39.15 x 30.46 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":162901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr92160.PNG"},{"id":81562,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0160/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699170","contributors":{"authors":[{"text":"Reeves, William E.","contributorId":99426,"corporation":false,"usgs":true,"family":"Reeves","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25489,"text":"wri904131 - 1992 - Evaluation of agricultural best-management practices in the Conestoga River headwaters, Pennsylvania; description and water quality of the Little Conestoga Creek headwaters prior to the implementation of nutrient management","interactions":[],"lastModifiedDate":"2017-07-05T11:30:11","indexId":"wri904131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"90-4131","title":"Evaluation of agricultural best-management practices in the Conestoga River headwaters, Pennsylvania; description and water quality of the Little Conestoga Creek headwaters prior to the implementation of nutrient management","docAbstract":"The headwaters of the Conestoga River are being studied to determine the effects of agricultural Best-Management Practices on surface-water and ground-water quality. As part of this study, a 5.82-square-mile area of the Little Conestoga Creek headwaters (Small Watershed) was monitored during 1984-86, prior to implementation of Best-Management Practices. This report describes the land use and hydrology of this study area and characterizes its surface-water and ground-water quality during the pre-Best-Management Practice phase. \r\n\r\nDuring base-flow conditions, median concentrations of dissolved nitrite plus nitrate nitrogen as nitrogen increased from 2.7 to 8.1 milligrams per liter as the stream flowed through the intensively-farmed carbonate valley. Median total phosphorus increased from 0.05 to 0.20 milligram per liter. Concentrations of dissolved nitrate nitrogen as nitrogen measured in ground water in carbonate rocks in the valley were as great as 25 milligrams per liter and consistently exceeded 10 milligrams per liter. \r\n\r\nStatistical analysis showed that it will require substantial reductions in concentrations and discharges of nitrogen and phosphorus in base flow to obtain statistically measurable improvements in water quality. If concentrations and discharges of total nitrogen in base flow at the five sites are reduced by 15 to 33 percent, and by 63 to 70 percent, respectively, then the Wilcoxon Mann-Whitney rank-sum test will be able to detect an improvement in water quality 95 percent of the time. Likewise, if concentrations of total phosphorus are reduced by 36 to 54 percent, or discharges of total phosphorus are reduced by 52 to 69 percent at the five sites, then an improvement in water quality will be able to be detected 95 percent of the time.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904131","usgsCitation":"Fishel, D.K., Brown, M.J., Kostelnik, K.M., and Howse, M., 1992, Evaluation of agricultural best-management practices in the Conestoga River headwaters, Pennsylvania; description and water quality of the Little Conestoga Creek headwaters prior to the implementation of nutrient management: U.S. Geological Survey Water-Resources Investigations Report 90-4131, viii, 68 p. :ill. ;28 cm., https://doi.org/10.3133/wri904131.","productDescription":"viii, 68 p. :ill. ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":54211,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4131/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4131/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c687","contributors":{"authors":[{"text":"Fishel, D. K.","contributorId":72028,"corporation":false,"usgs":true,"family":"Fishel","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":193903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, M. J.","contributorId":106531,"corporation":false,"usgs":true,"family":"Brown","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":193904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kostelnik, K. M.","contributorId":34951,"corporation":false,"usgs":true,"family":"Kostelnik","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193902,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howse, M.A.","contributorId":6893,"corporation":false,"usgs":true,"family":"Howse","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":193901,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20681,"text":"ofr92126 - 1992 - Geologic and hydrologic data collected at test holes NC-4 and NC-14, Manati and Vega Baja, Puerto Rico","interactions":[],"lastModifiedDate":"2018-08-29T13:57:36","indexId":"ofr92126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-126","title":"Geologic and hydrologic data collected at test holes NC-4 and NC-14, Manati and Vega Baja, Puerto Rico","docAbstract":"Test holes NC-4 and NC-14 were drilled in the municipalities of Manati and Vega Baja, respectively, in northern Puerto Rico as part of a study of the ground-water resources in the Northern Coastal Province of Puerto Rico. This study was conducted from 1986 to 1988 by the U.S. Geological Survey in cooperation with the Puerto Rico Department of Natural Resources. Test holes NC-4 and NC-14 were drilled to depths of 1,898 and 1,837 feet below land surface, respectively. Geologic and hydrologic data collected during drilling included continuous core lithology, water-quality measurements, water levels, and estimates of aquifer yields from the water-bearing zones. Detailed petrological and microfaunal analyses of the cores were used to determine the mineralogical content, ages, and paleoenvironments of deposition.
Analysis of the core recovered from test hole NC-4 indicated that four geologic formations of middle Tertiary age were penetrated, these were in descending order: the Aymam6n Limestone, the Los Puertos Limestone, the Cibao Formation, and the Lares Limestone. The Tertiary formations are capped by surficial deposits of Quaternary age. Test hole NC-14 penetrated rocks of middle Tertiary age that included three geologic formations, these were in descending order: the AymamOn Limestone, the Los Puertos Limestone, and the Cibao Formation. These formations are overlain by surficial deposits of Quaternary age. In both test holes the Cibao Formation consisted of the undifferentiated Quebrada Arenas and the Rio Indio Limestone Members of the Cibao Formation and an unnamed mudstone unit.
Test hole NC-4 penetrated three water-bearing units: a water-table aquifer and two artesian aquifers. The specific conductance in the water-table aquifer ranged from 500 to 38,000 microsiemens per centimeter at 25 degrees Celsius. The specific conductance ranged from 740 to 800 microsiemens per centimeter at 25 degrees Celsius in the two artesian aquifers. The relative yield ranged from 120 to 195 gallons per minute in the water-table aquifer and from 60 to 195 gallons per minute in the artesian aquifers. The water level ranged from 81 to 89 feet below land surface in the water-table aquifer. In the artesian aquifers, water levels ranged from 22 feet below land surface to 88 feet above land surface.
Test hole NC-14 penetrated four water-bearing units: a water-table aquifer and three artesian aquifers. The specific conductance in the water-table aquifer ranged from 590 microsiemens per centimeter at 25 degrees Celsius at a depth of 40 feet to 49,500 microsiemens per centimeter at 25 degrees Celsius at 1,010 feet below land surface. In the artesian aquifers specific conductance was about 700 microsiemens per centimeter at 25 degrees Celsius. The relative yield ranged from 58 to 370 gallons per minute in the water-table aquifer, and from 15 to 60 gallons per minute in the artesian aquifers. The water level in the water table aquifer ranged from 20 to 32 feet below land surface. In the artesian aquifers the water levels ranged from 18 feet below land surface to 19 feet above land surface.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr92126","collaboration":"Prepared in cooperation with the Puerto Rico Department of Natural Resources","usgsCitation":"Rodríguez-Martínez, J., Scharlach, R.A., and Torres-Gonzalez, A., 1992, Geologic and hydrologic data collected at test holes NC-4 and NC-14, Manati and Vega Baja, Puerto Rico: U.S. Geological Survey Open-File Report 92-126, v, 32 p., https://doi.org/10.3133/ofr92126.","productDescription":"v, 32 p.","costCenters":[],"links":[{"id":154027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0126/report-thumb.jpg"},{"id":356918,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0126/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"state":"Puerto Rico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108,\n 41\n ],\n [\n -107,\n 41\n ],\n [\n -107,\n 42\n ],\n [\n -108,\n 42\n ],\n [\n -108,\n 41\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a688","contributors":{"authors":[{"text":"Rodríguez-Martínez, Jesús","contributorId":48149,"corporation":false,"usgs":true,"family":"Rodríguez-Martínez","given":"Jesús","affiliations":[],"preferred":false,"id":183056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scharlach, Richard A.","contributorId":59475,"corporation":false,"usgs":true,"family":"Scharlach","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":183057,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Torres-Gonzalez, Arturo","contributorId":70769,"corporation":false,"usgs":true,"family":"Torres-Gonzalez","given":"Arturo","email":"","affiliations":[],"preferred":false,"id":183058,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26142,"text":"wri914193 - 1992 - Simulation of water-table response to management alternatives, central part of the western San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri914193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4193","title":"Simulation of water-table response to management alternatives, central part of the western San Joaquin Valley, California","docAbstract":"The occurrence of selenium in agricultural drainwater in the central pan of the western San Joaquin Valley, California, has focused concern on alternatives other than agricultural drains for managing shallow, poor-quality ground water. A transient, three-dimensional, finite-difference ground-water flow model was developed to assess the response of the water table to various management alternatives. The modeled area is 551 square miles and includes the semiconfined and confined zones above and below the Corcoran Clay Member of the Tulare Formation of Pleistocene age. The model was calibrated using hydrologic data from 1972 to 1988 and was able to reproduce the average change in water-table altitude to within 4 percent. The calibrated model was extended to forecast to the year 2040 for various management alternatives including maintenance of present practices, land retirement, reduced recharge, increased ground-water pumping, combinations of these alternatives, and five alternatives proposed by the U.S. Bureau of Reclamation. The model indicates that if current rates of recharge and pumping (as determined from an analysis of 1980 water-budget data) are maintained, the total area subject to bare-soil evaporation will increase by more than 50 percent and drainflow will increase by 20 percent. Model results indicate that retirement of land will result in a water-table decline beneath the area retired, but the effect on adjacent areas will be small to negligible. The effects of reducing recharge or increasing ground-water pumping vary with the magnitude of the change relative to average conditions and the size of the area managed. The area of land subject to bare-soil evaporation and the amount of drainflow in the model area can be reduced by more than 40 and 50 percent, respectively, if (1) recharge is reduced by 40 percent (about 0.3 foot per year) in areas that currently use only surface water, and by 15 percent (an average of about O. 1 foot per year) in the remainder of the model area; (2) pumping is increased by 0.5 foot per year in areas that currently use surface and ground water.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nFor sale by the USGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri914193","usgsCitation":"Belitz, K., and Phillips, S., 1992, Simulation of water-table response to management alternatives, central part of the western San Joaquin Valley, California: U.S. Geological Survey Water-Resources Investigations Report 91-4193, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914193.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4193/report-thumb.jpg"},{"id":54938,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4193/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1cc3","contributors":{"authors":[{"text":"Belitz, K.R. 0000-0003-4481-2345","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":38992,"corporation":false,"usgs":true,"family":"Belitz","given":"K.R.","affiliations":[],"preferred":false,"id":195889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, S.P.","contributorId":38172,"corporation":false,"usgs":true,"family":"Phillips","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":195888,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29002,"text":"wri924074 - 1992 - Identification of hydraulically conductive fractures intersecting boreholes in fractured gneiss near Ashford, Connecticut","interactions":[],"lastModifiedDate":"2019-12-28T09:51:46","indexId":"wri924074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4074","title":"Identification of hydraulically conductive fractures intersecting boreholes in fractured gneiss near Ashford, Connecticut","docAbstract":"No abstract available.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914085","usgsCitation":"Rinella, F.A., and Schuler, C., 1992, Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Malheur National Wildlife Refuge, Harney County, Oregon, 1988-89: U.S. Geological Survey Water-Resources Investigations Report 91-4085, vii, 106 p., https://doi.org/10.3133/wri914085.","productDescription":"vii, 106 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":159445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4085/report-thumb.jpg"},{"id":58211,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Harney County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-118.229,44.0389],[-118.2286,44.0116],[-118.2288,43.9674],[-118.2286,43.9532],[-118.2289,43.9086],[-118.2287,43.8945],[-118.229,43.8653],[-118.23,43.7792],[-118.2338,43.7798],[-118.2335,43.7675],[-118.2337,43.7242],[-118.2333,43.6978],[-118.2337,43.6295],[-118.2343,43.5744],[-118.2343,43.5357],[-118.2341,43.5211],[-118.2346,43.5065],[-118.2353,43.4487],[-118.2351,43.4346],[-118.2349,43.421],[-118.2354,43.4059],[-118.2352,43.3918],[-118.2357,43.3773],[-118.2362,43.3627],[-118.236,43.3486],[-118.2303,43.349],[-118.2302,43.3335],[-118.2301,43.3185],[-118.2293,43.3039],[-118.2298,43.2893],[-118.2295,43.2616],[-118.2293,43.2461],[-118.2287,43.1888],[-118.2286,43.1733],[-118.228,43.1724],[-118.2279,43.1009],[-118.2277,43.0873],[-118.2274,43.0582],[-118.2272,43.0436],[-118.2277,43.029],[-118.2276,43.0145],[-118.2274,43.0004],[-118.2286,43.0009],[-118.2279,42.9276],[-118.2278,42.9131],[-118.2171,42.9129],[-118.2161,42.8119],[-118.2166,42.7969],[-118.2158,42.7255],[-118.2157,42.7109],[-118.2156,42.6373],[-118.2155,42.6227],[-118.2147,42.5504],[-118.2146,42.5359],[-118.2141,42.4927],[-118.2139,42.4632],[-118.2144,42.4486],[-118.2128,42.3622],[-118.2127,42.3477],[-118.2125,42.3336],[-118.2124,42.319],[-118.2116,42.304],[-118.212,42.2754],[-118.1909,42.275],[-118.1916,42.236],[-118.1914,42.2223],[-118.1926,42.1483],[-118.1918,42.1356],[-118.1936,42.0634],[-118.194,42.0493],[-118.1952,41.9965],[-118.2137,41.9964],[-118.2341,41.9963],[-118.3125,41.9958],[-118.3496,41.9956],[-118.3891,41.9954],[-118.4287,41.9952],[-118.5914,41.9943],[-118.7723,41.993],[-118.7764,41.993],[-118.9076,41.9935],[-119.0478,41.9946],[-119.1449,41.9942],[-119.3244,41.9936],[-119.3569,41.9934],[-119.3585,42.0485],[-119.3589,42.1357],[-119.3632,42.1357],[-119.3643,42.2239],[-119.3641,42.3115],[-119.3639,42.3988],[-119.3643,42.4133],[-119.3647,42.4279],[-119.3644,42.4424],[-119.3642,42.4569],[-119.364,42.4715],[-119.3637,42.486],[-119.3641,42.5742],[-119.364,42.6596],[-119.3644,42.7469],[-119.483,42.747],[-119.5417,42.7465],[-119.6004,42.7465],[-119.6335,42.7463],[-119.7028,42.7453],[-119.7028,42.7426],[-119.7059,42.7426],[-119.7259,42.7423],[-119.8258,42.7419],[-119.8439,42.742],[-119.9419,42.7411],[-119.9418,42.8298],[-119.9417,42.9125],[-119.9348,42.9125],[-119.9379,43.0007],[-119.9384,43.0858],[-119.9389,43.1012],[-119.9396,43.1754],[-119.8981,43.1766],[-119.8988,43.2471],[-119.8987,43.2616],[-119.8991,43.2762],[-119.8989,43.3053],[-119.8991,43.3499],[-119.899,43.364],[-119.8995,43.3786],[-119.8994,43.3931],[-119.8992,43.4077],[-119.8996,43.4364],[-119.8996,43.5092],[-119.8995,43.5233],[-119.8994,43.5378],[-119.8988,43.6084],[-119.8986,43.6248],[-119.8982,43.6689],[-119.898,43.6967],[-119.8796,43.6971],[-119.8594,43.697],[-119.8391,43.6973],[-119.779,43.6979],[-119.7793,43.7854],[-119.7787,43.8427],[-119.7778,43.8719],[-119.7763,43.9575],[-119.6778,43.9574],[-119.6587,43.9577],[-119.5577,43.9589],[-119.5373,43.9587],[-119.4878,43.9593],[-119.416,43.9601],[-119.3982,43.9599],[-119.3569,43.96],[-119.2984,43.9599],[-119.1784,43.9602],[-119.0589,43.9612],[-118.9782,43.9612],[-118.9572,43.961],[-118.9363,43.9612],[-118.9185,43.9614],[-118.8676,43.9617],[-118.8174,43.962],[-118.8159,44.0472],[-118.6944,44.047],[-118.5882,44.0473],[-118.5883,44.0409],[-118.5413,44.0407],[-118.4669,44.0405],[-118.3676,44.0407],[-118.3472,44.0409],[-118.3473,44.0391],[-118.3307,44.0392],[-118.3104,44.0389],[-118.29,44.039],[-118.2697,44.0391],[-118.2493,44.0388],[-118.229,44.0389]]]},\"properties\":{\"name\":\"Harney\",\"state\":\"OR\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63eb31","contributors":{"authors":[{"text":"Rinella, F. A.","contributorId":89120,"corporation":false,"usgs":true,"family":"Rinella","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuler, C.A.","contributorId":42627,"corporation":false,"usgs":true,"family":"Schuler","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":201410,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19357,"text":"ofr92152 - 1992 - Continuous-record networks for collection of hydrologic data in Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr92152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-152","title":"Continuous-record networks for collection of hydrologic data in Ohio","language":"ENGLISH","publisher":"U.S. Geological Survey, Dept. of the Interior,","doi":"10.3133/ofr92152","usgsCitation":"Hindall, S.M., and Eberle, M., 1992, Continuous-record networks for collection of hydrologic data in Ohio: U.S. Geological Survey Open-File Report 92-152, 2 p. ill. ;28 cm., https://doi.org/10.3133/ofr92152.","productDescription":"2 p. ill. ;28 cm.","costCenters":[],"links":[{"id":151713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0152/report-thumb.jpg"},{"id":48834,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dfd","contributors":{"authors":[{"text":"Hindall, S. M.","contributorId":59414,"corporation":false,"usgs":true,"family":"Hindall","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":180741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eberle, Michael","contributorId":39770,"corporation":false,"usgs":true,"family":"Eberle","given":"Michael","email":"","affiliations":[],"preferred":false,"id":180740,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19031,"text":"ofr92629 - 1992 - Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia","interactions":[{"subject":{"id":19031,"text":"ofr92629 - 1992 - Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia","indexId":"ofr92629","publicationYear":"1992","noYear":false,"title":"Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":1414,"text":"wsp2411 - 1997 - Water-supply potential of major streams and the Upper Floridan Aquifer in the vicinity of Savannah, Georgia","indexId":"wsp2411","publicationYear":"1997","noYear":false,"title":"Water-supply potential of major streams and the Upper Floridan Aquifer in the vicinity of Savannah, Georgia"},"id":1}],"supersededBy":{"id":1414,"text":"wsp2411 - 1997 - Water-supply potential of major streams and the Upper Floridan Aquifer in the vicinity of Savannah, Georgia","indexId":"wsp2411","publicationYear":"1997","noYear":false,"title":"Water-supply potential of major streams and the Upper Floridan Aquifer in the vicinity of Savannah, Georgia"},"lastModifiedDate":"2021-03-04T21:16:43.635017","indexId":"ofr92629","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-629","title":"Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia","docAbstract":"Long-term pumping from the Upper Floridan aquifer in the Savannah, Georgia, area has lowered ground-water levels, resulting in increased salinity of ground water by seawater encroachment at Hilton Head Island, S.C., and by saltwater intrusion at Brunswick, Ga. Increased pumpage could cause further salinization of the ground-water resources.
The Savannah and Ogeechee Rivers can be considered potential water-supply sources for the Savannah, Ga., area, on the basis of historic stream flow records and water-quality constituents and properties examined. Analyses of stream-discharge data indicate that the minimum average discharges for 7 consecutive days for a 10-year recurrence interval (7010), was 5,460 cubic feet per second (ft3/s) at Savannah River near Clyo, Ga., and 192 ft3/s at Ogeechee River near Eden, Ga. For example, 90 percent of the time, flows in excess of the 7010 discharges are about 900 and 200 ft3/s, respectively. However, Georgia Department of Natural Resources, Environmental Protection Division, imposes a non-depletable flow criterion; thus, the actual quantity of water available for withdrawal probably would be less than flows in excess of minimum flow criteria, such as the 7Q10.
This report contains hydrologic data for wells finished in sandstone and alluvial aquifers in southeastern San Juan County, Utah, and chemical data for water from selected wells in the Navajo aquifer. Temperature, specific conductance, pH, and discharge data from 1989-91 for water from selected wells in all aquifers are also presented.
Data presented in this report were compiled from previously published reports (Goode, 1958; Sumsion, 1975; Avery, 1986; Kimball, 1987; Howells, 1990); data bases of the U.S. Geological Survey, the Navajo Tribe, the U.S. Bureau of Land Management, the Utah Division of Water Rights, and the Utah Division of Oil, Gas, and Mining; and from information obtained from oil companies in the Greater Aneth Oil Field.
Results of investigations by Avery (1986) during 1982-83 indicated that water from many wells in the Navajo aquifer in the vicinity of the Greater Aneth Oil Field was moderately saline and that in some wells, salinity appeared to increase over time. The purpose of this study is to assess the physical extent and concentration of saline water in the Navajo and other aquifers in this area. The purpose of this report is to present available water-quality data for water from wells in the Navajo aquifer and present records for selected wells in the Navajo and other aquifers.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt lake City, UT","doi":"10.3133/ofr92124","usgsCitation":"Spangler, L.E., 1992, Records of wells in sandstone and alluvial aquifers and chemical data for water from selected wells in the Navajo aquifer in the vicinity of the greater Aneth Oil Field, San Juan County, Utah: U.S. Geological Survey Open-File Report 92-124, v, 44 p., https://doi.org/10.3133/ofr92124.","productDescription":"v, 44 p.","numberOfPages":"49","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":154286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0124/report-thumb.jpg"},{"id":390700,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18236.htm"},{"id":50567,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0124/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Greater Aneth Oil Field, Navajo Aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.5,\n 37\n ],\n [\n -109,\n 37\n ],\n [\n -109,\n 37.5\n ],\n [\n -109.5,\n 37.5\n ],\n [\n -109.5,\n 37\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"This is also Utah Hydrologic-Data Report no. 47","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cb6","contributors":{"authors":[{"text":"Spangler, Lawrence E. 0000-0003-3928-8809 spangler@usgs.gov","orcid":"https://orcid.org/0000-0003-3928-8809","contributorId":973,"corporation":false,"usgs":true,"family":"Spangler","given":"Lawrence","email":"spangler@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":183632,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21095,"text":"ofr92149 - 1992 - Floating sample-collection platform with stage-activated automatic water sampler for streams with large variation in stage","interactions":[],"lastModifiedDate":"2020-04-13T12:33:44.73766","indexId":"ofr92149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-149","title":"Floating sample-collection platform with stage-activated automatic water sampler for streams with large variation in stage","docAbstract":"A floating sample-collection platform is described for stream sites where the vertical or horizontal distance between the stream-sampling point and a safe location for the sampler exceed the suction head of the sampler. 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Information on low-flow magnitude and frequency is essential in hydrologic studies and for optimum development of surface water resources. The report includes analyses of low-flow data and tabulations of computed low-flow magnitude and frequency for 7, 14, 30, 60, and 90 consecutive days with recurrence intervals of 2 and 10 years for continuous-record gaging stations. Low-flow estimates are provided for partial-record stations for 7, 14, and 30 consecutive days with recurrence intervals of 2 and 10 years. Values at partial-record stations were estimated from the relation between concurrent flows at the partial-record stations and nearby continuous-record stations.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924063","usgsCitation":"Santiago-Rivera, L., 1992, Low-flow characteristics at selected sites on streams in eastern Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 92-4063, ix, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924063.","productDescription":"ix, 46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4063/report-thumb.jpg"},{"id":58369,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644b77","contributors":{"authors":[{"text":"Santiago-Rivera, Luis","contributorId":83888,"corporation":false,"usgs":true,"family":"Santiago-Rivera","given":"Luis","email":"","affiliations":[],"preferred":false,"id":201674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21172,"text":"ofr92498 - 1992 - Hydrologic and water-quality data in selected agricultural drainages in Beaufort and Hyde Counties, North Carolina, 1988-90","interactions":[],"lastModifiedDate":"2017-01-04T10:54:06","indexId":"ofr92498","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-498","title":"Hydrologic and water-quality data in selected agricultural drainages in Beaufort and Hyde Counties, North Carolina, 1988-90","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr92498","usgsCitation":"Treece, M., and Bales, J., 1992, Hydrologic and water-quality data in selected agricultural drainages in Beaufort and Hyde Counties, North Carolina, 1988-90: U.S. Geological Survey Open-File Report 92-498, vi, 89 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr92498.","productDescription":"vi, 89 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":153410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0498/report-thumb.jpg"},{"id":50765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0498/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","county":"Beaufort County, Hyde County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.750244140625,\n 34.34570381052938\n ],\n [\n -77.750244140625,\n 35.88014896488361\n ],\n [\n -75.91827392578125,\n 35.88014896488361\n ],\n [\n -75.91827392578125,\n 34.34570381052938\n ],\n [\n -77.750244140625,\n 34.34570381052938\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a368","contributors":{"authors":[{"text":"Treece, M.W.","contributorId":91134,"corporation":false,"usgs":true,"family":"Treece","given":"M.W.","affiliations":[],"preferred":false,"id":183971,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bales, J. D.","contributorId":21569,"corporation":false,"usgs":true,"family":"Bales","given":"J. D.","affiliations":[],"preferred":false,"id":183970,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":67977,"text":"ha722B - 1992 - Geohydrologic systems in Kansas — Physical framework of the Great Plains aquifer system","interactions":[],"lastModifiedDate":"2022-01-24T20:03:31.252351","indexId":"ha722B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"722","chapter":"B","title":"Geohydrologic systems in Kansas — Physical framework of the Great Plains aquifer system","docAbstract":"The purpose of this map report is to provide a description of one of the principal geohydrologic systems in Upper Cambrian through Lower Cretaceous rocks in Kansas. The report is the result of an investigation made as part of the Central Midwest Regional Aquifer-System Analysis (CMRASA). The CMRASA is one of several major investigations by the U.S. Geological Survey of regional aquifer systems in the United States. These regional investigations are designed to increase knowledge of the flow regime and hydrologic properties of major aquifer systems and to provide quantitative information for the assessment, development, and management of water supplies. The CMRASA study area includes all or parts of 10 Central Midwestern States (Jorgensen and Signor, 1981), as shown on the envelope cover.
This Hydrologic Investigations Atlas, which consists of a series of nine chapters, presents a description of the physical framework and the geohydrology of principal aquifer and confining systems in Kansas. Chapter B describes the physical framework of the Great Plains aquifer system and presents maps and a geohydrologic cross section that show the thickness, the areal extent, and the altitude and configuration of the top of the Lower Cretaceous rocks that compose the Great Plains aquifer system. The maps are based on data from selected geophysical and lithologic logs and from published maps of stratigraphically equivalent units. Maps that show the thickness and the altitude and configuration of the top of the Great Plains aquifer system have been prepared as part of a series of interrelated maps that describe the stratigraphic interval from the Precambrian surface through Lower Cretaceous rocks. A concerted effort was made to ensure that maps of each geohydrologic system are consistent with maps of underlying and overlying systems; modifications were made where necessary.
Chapter A of this atlas series (Wolf and others, 1990) describes the relation of geohydrologic systems in Kansas and presents a more detailed discussion of the methods and data used to prepare and ensure consistency among the sets of maps in the series.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha722B","usgsCitation":"Spinazola, J.M., Wolf, R.J., and McGovern, H.E., 1992, Geohydrologic systems in Kansas — Physical framework of the Great Plains aquifer system: U.S. Geological Survey Hydrologic Atlas 722, 2 Plates: 53.86 x 39.87 inches and 51.13 x 34.54 inches, https://doi.org/10.3133/ha722B.","productDescription":"2 Plates: 53.86 x 39.87 inches and 51.13 x 34.54 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":266304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/722b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":360661,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/722b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394772,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16146.htm"}],"scale":"1000000","country":"United States","state":"Kansas","otherGeospatial":"Great Plains aquifer system","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.04,37 ], [ -102.04,40 ], [ -97,40 ], [ -97,37 ], [ -102.04,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e04","contributors":{"authors":[{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":277438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":277437,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGovern, Harold E.","contributorId":9634,"corporation":false,"usgs":true,"family":"McGovern","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277436,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68111,"text":"ha730J - 1992 - Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin","interactions":[{"subject":{"id":68111,"text":"ha730J - 1992 - Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin","indexId":"ha730J","publicationYear":"1992","noYear":false,"chapter":"J","title":"Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin"},"predicate":"IS_PART_OF","object":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"id":1}],"isPartOf":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"lastModifiedDate":"2017-05-30T15:55:08","indexId":"ha730J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"730","chapter":"J","title":"Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin","docAbstract":"Segment 9, which consists of Minnesota, Iowa, Wisconsin, and Michigan, abuts the Canadian border in the upper Midwest and lies adjacent to or surrounds four of the Great Lakes-Superior, Michigan, Huron, and Erie. Thousands of small to large lakes similar to the one shown in figure 1 dot the landscape, which is drained by numerous rivers and streams tributary primarily to the Mississippi River in the west and to the Great Lakes-St. Lawrence River system in the east. These abundant surface-water sources represent an ample supply of water to large users, such as the cities of Milwaukee, Wis., and Detroit, Mich. However, water stored in unconsolidated and consolidated sedimentary-rock aquifers that underlie the four States also is in abundant supply and is an economical source that can be used for nearly any purpose, usually with little or no treatment. In more than 95 percent of the four-State area, these aquifers supply water to a broad spectrum of consumers-from individual households to cities, such as St. Paul, Minn., Madison, Wis., and Lansing, Mich. These aquifers are the subject of this chapter. The geology and the hydrology of each of the principal aquifers are illustrated and discussed insofar as information was available from the literature. Hydrogeology, ground-water flow, availability and quality of water, and freshwater withdrawals from each of the aquifers are the principal subjects of discussion.
Population in the four States is concentrated in the cities and is thinly dispersed in the broad agricultural areas of the States (fig. 2). Minneapolis-St. Paul, Minn., Des Moines, Iowa, Milwaukee and Madison, Wis., and Detroit and Lansing, Mich., are a few of the principal cities. Many of these cities and other large population centers represent areas of concentrated ground-water withdrawals.
Precipitation is the source of all water in Segment 9. Average annual precipitation ranges from about 20 to 40 inches across the segment and generally increases from northwest to southeast (fig. 3). Precipitation is least in the northwestern part of the segment because of the orographic effect of the Rocky Mountains, which are hundreds of miles to the west. Annual precipitation in excess of 36 inches that falls south and east of Lakes Superior and Michigan (fig. 3) is a result of the prevailing westerly winds that evaporate moisture from the lakes; this moisture subsequently condenses and falls as precipitation over the land.
Average annual runoff in rivers and streams (fig. 4) generally reflects average annual precipitation patterns (fig. 3). Runoff generally increases from less than 1 to more than 20 inches. Runoff also tends to be substantial downwind from Lakes Superior and Michigan. However, in no part of the segment does runoff exceed precipitation. Much of the water from precipitation is returned to the atmosphere by evapotranspiration-evaporation from the land and water surfaces, and transpiration by plants. Some of the water is stored in aquifers through ground-water recharge or is stored on the land surface in lakes, marshes, and reservoirs. Runoff represents water from precipitation that runs directly off the land surface to streams and water discharged to streams that was stored in lakes, marshes, reservoirs, or aquifers.
","largerWorkTitle":"Ground Water Atlas of the United States","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha730J","isbn":"0607767588","usgsCitation":"Olcott, P.G., 1992, Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin: U.S. Geological Survey Hydrologic Atlas 730, 31 p., https://doi.org/10.3133/ha730J.","productDescription":"31 p.","startPage":"J1","endPage":"J31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":11487,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ha/ha730/ch_j/index.html","linkFileType":{"id":5,"text":"html"}},{"id":115252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/730j/report.pdf","text":"Report","size":"69.43 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":186516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/730j/report-thumb.jpg"}],"country":"United States","state":"Iowa, Michigan, Minnesota, Wisconsin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-90.640927,42.508302],[-90.161159,42.106372],[-90.172765,41.866149],[-90.364128,41.579633],[-91.050328,41.400049],[-91.113648,41.241401],[-90.955201,40.986805],[-91.448441,40.378914],[-91.785916,40.611488],[-95.746443,40.584935],[-95.852615,40.702262],[-95.929889,41.415155],[-96.096186,41.547192],[-96.077543,41.777824],[-96.628741,42.757532],[-96.448134,43.104452],[-96.598396,43.495074],[-96.453049,43.500415],[-96.452948,45.268925],[-96.835451,45.586129],[-96.587093,45.816445],[-96.559271,46.058272],[-96.789572,46.639079],[-96.851293,47.589264],[-97.139497,48.153108],[-97.108655,48.691484],[-97.238387,48.982631],[-95.153711,48.998903],[-95.153314,49.384358],[-94.974286,49.367738],[-94.555835,48.716207],[-93.741843,48.517347],[-92.984963,48.623731],[-92.634931,48.542873],[-92.698824,48.494892],[-92.341207,48.23248],[-92.066269,48.359602],[-91.542512,48.053268],[-90.88548,48.245784],[-90.703702,48.096009],[-89.489226,48.014528],[-90.86827,47.5569],[-92.058888,46.809938],[-91.942988,46.679939],[-90.880358,46.957661],[-90.78804,46.844886],[-90.920813,46.637432],[-90.398478,46.575832],[-88.982483,46.99883],[-88.400224,47.379551],[-87.816958,47.471998],[-87.730804,47.449112],[-88.349952,47.076377],[-88.462349,46.786711],[-88.167373,46.9588],[-87.915943,46.909508],[-87.619747,46.79821],[-87.366767,46.507303],[-86.850111,46.434114],[-86.188024,46.654008],[-84.964652,46.772845],[-84.969464,46.47629],[-84.177428,46.52692],[-84.097766,46.256512],[-84.247687,46.17989],[-83.931175,46.017871],[-83.63498,46.103953],[-83.49484,45.999541],[-84.345451,45.946569],[-84.656567,46.052654],[-84.820557,45.868293],[-85.047028,46.020603],[-85.528403,46.087121],[-85.663966,45.967013],[-86.278007,45.942057],[-86.687208,45.634253],[-86.532989,45.882665],[-86.92106,45.697868],[-87.018902,45.838886],[-88.027103,44.578992],[-87.943801,44.529693],[-87.428144,44.890738],[-87.021088,45.296541],[-87.73063,43.893862],[-87.910172,43.236634],[-87.800477,42.49192],[-90.640927,42.508302]]],[[[-88.684434,48.115785],[-88.447236,48.182916],[-89.022736,47.858532],[-89.255202,47.876102],[-88.684434,48.115785]]],[[[-83.880387,41.720089],[-86.824828,41.76024],[-86.24971,42.480212],[-86.226305,42.988284],[-86.540916,43.633158],[-86.25395,44.64808],[-86.066745,44.905685],[-85.780439,44.977932],[-85.540497,45.210169],[-85.641652,44.810816],[-85.520205,44.960347],[-85.477423,44.813781],[-85.355478,45.282774],[-84.91585,45.393115],[-85.110884,45.526285],[-84.94565,45.708621],[-85.011433,45.757962],[-84.204218,45.627116],[-84.095905,45.497298],[-83.488826,45.355872],[-83.316118,45.141958],[-83.435822,45.000012],[-83.277213,44.7167],[-83.335248,44.357995],[-83.890145,43.934672],[-83.909479,43.672622],[-83.618602,43.628891],[-83.227093,43.981003],[-82.915976,44.070503],[-82.617955,43.768596],[-82.423086,42.988728],[-82.509935,42.637294],[-82.648776,42.550401],[-82.630922,42.64211],[-82.780817,42.652232],[-83.431103,41.757457],[-83.880387,41.720089]]],[[[-86.880572,45.331467],[-86.956192,45.351179],[-86.82177,45.427602],[-86.880572,45.331467]]]]},\"properties\":{\"name\":\"Iowa\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dd8c","contributors":{"authors":[{"text":"Olcott, Perry G.","contributorId":17249,"corporation":false,"usgs":true,"family":"Olcott","given":"Perry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17248,"text":"ofr92107 - 1992 - Hydrologic research at the Princeton, Minnesota management systems evaluation area","interactions":[],"lastModifiedDate":"2019-12-28T09:53:08","indexId":"ofr92107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-107","title":"Hydrologic research at the Princeton, Minnesota management systems evaluation area","docAbstract":"The Management Systems Evaluation Area (MSEA) program is part of a multi-scale, inter-agency initiative to evaluate the effects of agricultural management systems on water quality. The program resulted from the integration of the U.S. Department of Agriculture (USDA) Research Plan for Water Quality and the U.S Geological Survey (USGS) Mid-Continent Herbicide Initiative and is part of the President's Water Quality Initiative. The mid-continental corn belt was selected for study because it is an area where about 60% of the Nation's pesticides and nitrogen fertilizers are used.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ofr92107","usgsCitation":"Delin, G., Landon, M., Anderson, J.L., and Dowdy, R., 1992, Hydrologic research at the Princeton, Minnesota management systems evaluation area: U.S. Geological Survey Open-File Report 92-107, 2 p., https://doi.org/10.3133/ofr92107.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":46398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0107/report-thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Princeton","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.64797592163086,\n 45.509474756808736\n ],\n [\n -93.64797592163086,\n 45.58304947361755\n ],\n [\n -93.55991363525389,\n 45.58304947361755\n ],\n [\n -93.55991363525389,\n 45.509474756808736\n ],\n [\n -93.64797592163086,\n 45.509474756808736\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6053c6","contributors":{"authors":[{"text":"Delin, G. N.","contributorId":12834,"corporation":false,"usgs":true,"family":"Delin","given":"G. N.","affiliations":[],"preferred":false,"id":175598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landon, M.K. 0000-0002-5766-0494","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":69572,"corporation":false,"usgs":true,"family":"Landon","given":"M.K.","affiliations":[],"preferred":false,"id":175599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, J. L.","contributorId":103240,"corporation":false,"usgs":true,"family":"Anderson","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":175601,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dowdy, R.H.","contributorId":92275,"corporation":false,"usgs":true,"family":"Dowdy","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":175600,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":17746,"text":"ofr92154 - 1992 - A summary of water-resources activities of the U.S. Geological Survey in Iowa, fiscal year 1992","interactions":[],"lastModifiedDate":"2016-03-11T15:52:33","indexId":"ofr92154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-154","title":"A summary of water-resources activities of the U.S. Geological Survey in Iowa, fiscal year 1992","docAbstract":"Water-resources activities of the U.S. Geological Survey in Iowa consist of collecting hydrologic data and conducting interpretive studies. Hydrologic investigations in Iowa are made through three basic types of projects: (1) hydrologic data-collection programs; (2) local or areal studies; and (3) statewide or regional investigations. These projects are funded through cooperative joint-funding agreements with Federal, State, and local agencies and direct Federal funds. The data and the results of the interpretive studies are published or released by either the U.S. Geological Survey or by cooperating agencies. This report describes: (1) the hydrologic data-collection programs; (2) the local or areal hydrologic investigations; and (3) statewide or regional studies conducted by the U.S. Geological Survey in Iowa during fiscal year 1992 and provides a list of selected water-resources references for Iowa.
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confining system","docAbstract":"The purpose of this Hydrologic Investigations Atlas is to provide a description of the principal geohydrologic systems in the Upper Cambrian through Lower Cretaceous rocks in Kansas. 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