No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884155","usgsCitation":"Casey, G.D., and Reynolds, R.J., 1989, Hydrogeology of the stratified-drift aquifers in the Rome area, Oneida County, New York: U.S. Geological Survey Water-Resources Investigations Report 88-4155, 8 Plates: 41.00 × 33.00 inches or smaller, https://doi.org/10.3133/wri884155.","productDescription":"8 Plates: 41.00 × 33.00 inches or smaller","costCenters":[],"links":[{"id":171837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398254,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45785.htm","linkFileType":{"id":5,"text":"html"}},{"id":82180,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4155/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82187,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4155/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82186,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4155/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82185,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4155/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82184,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4155/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82183,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4155/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82182,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4155/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82181,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4155/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New York","county":"Oneida County","otherGeospatial":"Rome area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.535,\n 43.164\n ],\n [\n -75.25,\n 43.164\n ],\n [\n -75.25,\n 43.3\n ],\n [\n -75.535,\n 43.3\n ],\n [\n -75.535,\n 43.164\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68434a","contributors":{"authors":[{"text":"Casey, George D.","contributorId":105689,"corporation":false,"usgs":true,"family":"Casey","given":"George","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":230511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard J. 0000-0001-5032-6613 rjreynol@usgs.gov","orcid":"https://orcid.org/0000-0001-5032-6613","contributorId":1082,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rjreynol@usgs.gov","middleInitial":"J.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12575,"text":"ofr8939 - 1989 - Geographic information system index for the State of Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:06:50","indexId":"ofr8939","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-39","title":"Geographic information system index for the State of Tennessee","docAbstract":"Recently the use of Geographical Information Systems (GIS) has increased within Tennessee. As a result, the U.S. Geological Survey, the Tennessee State Planning Office, and the Tennessee Comptroller of the Treasury entered into an agreement to conduct a survey of GIS users within the State. Two hundred and sixty three agencies were contacted. One hundred and thirty-nine agencies maintained one or more computer system (including personal computers). Twenty-five agencies used GIS software. The number of coverages or layers that exist upon completion of the survey as computerized digital data for Tennessee was 4,741. One hundred and twenty location-specific data bases were available. The U.S. Geological Survey, National Mapping Division map accuracy standards and digital cartographic data standards were included as minimum guidelines for GIS users. General data sharing techniques were described. The most common one was the use of magnetic tapes. A GIS index data base containing the survey data was built for inquiries. A 7.5 minute quadrangle coverage of Tennessee was created to allow for identification on a quadrangle basis of existing coverages contained in the GIS data base. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8939","usgsCitation":"Barron, W.R., and Norris, P.G., 1989, Geographic information system index for the State of Tennessee: U.S. Geological Survey Open-File Report 89-39, vi, 53 p. ill. ;28 cm., https://doi.org/10.3133/ofr8939.","productDescription":"vi, 53 p. ill. ;28 cm.","costCenters":[],"links":[{"id":145888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":985,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_89-39","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9081","contributors":{"authors":[{"text":"Barron, William R.","contributorId":41435,"corporation":false,"usgs":true,"family":"Barron","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":166363,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norris, Pamela G.","contributorId":10434,"corporation":false,"usgs":true,"family":"Norris","given":"Pamela","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":166362,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14902,"text":"ofr89493 - 1989 - Black and white photographic catalog of geologic/geomorphologic phenomena","interactions":[],"lastModifiedDate":"2021-03-18T21:11:18.228856","indexId":"ofr89493","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-493","title":"Black and white photographic catalog of geologic/geomorphologic phenomena","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr89493","usgsCitation":"McGregor, J., 1989, Black and white photographic catalog of geologic/geomorphologic phenomena: U.S. Geological Survey Open-File Report 89-493, 351 p., https://doi.org/10.3133/ofr89493.","productDescription":"351 p.","costCenters":[],"links":[{"id":384466,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0493/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0493/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db60848f","contributors":{"authors":[{"text":"McGregor, J.K. Jr.","contributorId":61831,"corporation":false,"usgs":true,"family":"McGregor","given":"J.K.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":170204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":59508,"text":"mf2061 - 1989 - Geologic map of the North Stansbury Mountains Wilderness Study Area, Tooele County, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:12","indexId":"mf2061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2061","title":"Geologic map of the North Stansbury Mountains Wilderness Study Area, Tooele County, Utah","language":"ENGLISH","doi":"10.3133/mf2061","usgsCitation":"Foose, M.P., 1989, Geologic map of the North Stansbury Mountains Wilderness Study Area, Tooele County, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2061, 1 map ;58 x 41 cm., on sheet 89 x 78 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2061.","productDescription":"1 map ;58 x 41 cm., on sheet 89 x 78 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105214,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5659.htm","linkFileType":{"id":5,"text":"html"},"description":"5659"},{"id":184959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.66666666666667,40.583333333333336 ], [ -112.66666666666667,40.700833333333335 ], [ -112.58333333333333,40.700833333333335 ], [ -112.58333333333333,40.583333333333336 ], [ -112.66666666666667,40.583333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6960f2","contributors":{"authors":[{"text":"Foose, M. P.","contributorId":97075,"corporation":false,"usgs":true,"family":"Foose","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":262136,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27978,"text":"wri894073 - 1989 - Water-level changes in the High Plains aquifer underlying parts of South Dakota, Wyoming, Nebraska, Colorado, Kansas, New Mexico, Oklahoma, and Texas: Predevelopment through nonirrigation season 1987-88","interactions":[],"lastModifiedDate":"2022-07-06T18:33:36.473025","indexId":"wri894073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4073","title":"Water-level changes in the High Plains aquifer underlying parts of South Dakota, Wyoming, Nebraska, Colorado, Kansas, New Mexico, Oklahoma, and Texas: Predevelopment through nonirrigation season 1987-88","docAbstract":"The changes in water levels in the High Plains aquifer from the nonirrigation season 1986-87 through the nonirrigation season 1987-88 and from the nonirrigation season 1979-80 through the nonirrigation season 1987-88 are presented in maps for the entire High Plains aquifer area. Water level changes are caused by interacting changes in precipitation, land use, and annual pumpage. Water levels declined from conditions prior to development until 1980 through parts of the High Plains of Nebraska, Colorado, New Mexico, Oklahoma, and Texas. From 1980 through 1987 water level changes were mixed, with declines of more than 10 ft in the highly developed areas of Kansas, New Mexico, Oklahoma, and Texas and relatively stable to rising water tables throughout the remaining aquifer area. The net change was a rise of 0.8 ft. The 1981-87 period was generally wetter than normal and pumping for irrigated agriculture was therefore reduced. Water level changes were mixed during 1987. Declines continued in some highly developed areas, but water levels generally rose throughout most of the aquifer. The average area-weighted change was a rise of 0.28 ft. This rise was due to the generally greater than normal precipitation, decreased acreage under irrigation, and decreased pumpage for those areas irrigated. At the end of the growing season, the drought in the Midwest in 1988 affected only limited areas of the High Plains. The effects of the drought on water levels can not be assessed until the water-level measurements for the nonirrigation season of 1988-89 are compiled.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894073","usgsCitation":"Kastner, W.M., Schild, D.E., and Spahr, D.S., 1989, Water-level changes in the High Plains aquifer underlying parts of South Dakota, Wyoming, Nebraska, Colorado, Kansas, New Mexico, Oklahoma, and Texas: Predevelopment through nonirrigation season 1987-88: U.S. Geological Survey Water-Resources Investigations Report 89-4073, vi, 61 p., https://doi.org/10.3133/wri894073.","productDescription":"vi, 61 p.","costCenters":[],"links":[{"id":403084,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47183.htm","linkFileType":{"id":5,"text":"html"}},{"id":56794,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4073/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4073/report-thumb.jpg"}],"country":"United States","state":"Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, Wyoming","otherGeospatial":"High Plains aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.5,\n 32\n ],\n [\n -97,\n 32\n ],\n [\n -97,\n 43.5\n ],\n [\n -105.5,\n 43.5\n ],\n [\n -105.5,\n 32\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e75a6","contributors":{"authors":[{"text":"Kastner, W. M.","contributorId":67921,"corporation":false,"usgs":true,"family":"Kastner","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":198999,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schild, D. E.","contributorId":77559,"corporation":false,"usgs":true,"family":"Schild","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":199000,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spahr, D. S.","contributorId":88783,"corporation":false,"usgs":true,"family":"Spahr","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":199001,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1816,"text":"wsp2327 - 1989 - Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","interactions":[{"subject":{"id":14055,"text":"ofr86301 - 1987 - Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","indexId":"ofr86301","publicationYear":"1987","noYear":false,"title":"Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois"},"predicate":"SUPERSEDED_BY","object":{"id":1816,"text":"wsp2327 - 1989 - Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","indexId":"wsp2327","publicationYear":"1989","noYear":false,"title":"Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp2327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2327","title":"Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","docAbstract":"From July 1982 through June 1984, a study was made of the evapotranspiration and microclimate at a low-level radioactive-waste disposal site near Sheffield, Bureau County, Illinois. Vegetation at the site consists of mixed pasture grasses, primarily awnless brome (Bromus inermis) and red clover (Trifoleum pratense). Three methods were used to estimate evapotranspiration: (1) an energy budget with the Bowen ratio, (2) an aerodynamic profile, and (3) a soil-based water budget. For the aerodynamic-profile method, sensible-heat flux was estimated by a profile equation and evapotranspiration was then calculated as the residual in the energy-balance equation. Estimates by the energy-budget and aerodynamic-profile methods were computed from hourly data and then summed by days and months. Yearly estimates (for March through November) by these methods were in close agreement: 648 and 626 millimeters, respectively. Daily estimates reach a maximum of about 6 millimeters. The water-budget method produced only monthly estimates based on weekly or biweekly soil-moisture content measurements. The yearly evapotranspiration estimated by this method (which actually included only the months of April through October) was 655 millimeters. The March-through-November average for the three methods of 657 millimeters was equivalent to 70 percent of total precipitation. \r\n\r\nContinuous measurements were made of incoming and reflected shortwave radiation, incoming and emitted longwave radiation, net radiation, soil-heat flux, soil temperature, horizontal windspeed, and wet- and dry-bulb air temperature. Windspeed and air temperature were measured at heights of 0.5 and 2.0 meters (and also at 1.0 meter after September 1983). Soilmoisture content of the soil zone was measured with a gamma-attenuation gage. \r\n\r\nAnnual precipitation (938 millimeters) and average temperature (10.8 degrees Celsius) at the Sheffield site were virtually identical to long-term averages from nearby National Weather Service stations. Solar radiation averaged 65 percent of that normally expected under clear skies. Net radiation averaged 70.1 watts per square meter and was highest in July and negative during some winter months. Wind direction varied but was predominately south-southeasterly. Wind speed at the 2-meter height averaged 3.5 meters per second and was slightly higher in winter months than the rest of the year. The amount of water stored within the soil zone was greatest in early spring and least in late summer.\r\n\r\nSeasonal and diurnal trends of evapotranspiration rates mirrored those of net radiation; July was usually the month with the highest evapotranspiration rate. The ratio of sensible- to latentheat fluxes (commonly called the Bowen ratio) for the 2-year study period was 0.38, as averaged from the three methods. Monthly Bowen ratios fluctuated somewhat but averaged about 0.35 for late spring through summer. In fall, the ratio declined to zero or to slightly negative values. When the ratio was negative, the latent-heat flux was slightly greater than the net radiation because of additional energy supplied by' the cooling soil and air. \r\n\r\nEvapotranspiration calculated by the three methods averaged 75 percent of potential evapotranspiration, as estimated by the Penman equation. There was no apparent seasonal trend in the relation between actual and potential evapotranspiration rates.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nBooks and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/wsp2327","usgsCitation":"Healy, R.W., DeVries, M., and Sturrock, A.M., 1989, Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois: U.S. Geological Survey Water Supply Paper 2327, v, 44 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2327.","productDescription":"v, 44 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":137215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2327/report-thumb.jpg"},{"id":27012,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2327/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9bba","contributors":{"authors":[{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeVries, M.P.","contributorId":39760,"corporation":false,"usgs":true,"family":"DeVries","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":144201,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sturrock, Alex M. Jr.","contributorId":62191,"corporation":false,"usgs":true,"family":"Sturrock","given":"Alex","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":144202,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44623,"text":"wri884067 - 1989 - Water-level maps of the Mississippi River Valley alluvial aquifer in eastern Arkansas, 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:11:00","indexId":"wri884067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4067","title":"Water-level maps of the Mississippi River Valley alluvial aquifer in eastern Arkansas, 1986","docAbstract":"The Mississippi River Valley alluvial aquifer is a major source of water for irrigation in much of eastern Arkansas. Maps of the potentiometric surface, water level change, and depth to water illustrate the effects of large withdrawals for irrigation on water levels in the aquifer. The Mississippi River Valley alluvial aquifer is composed of Quaternary Flood plain and terrace deposits. Water in the aquifer generally is confined by an upper silt and clay layer. The regional direction of groundwater flow is south and southeast, except where affected by large withdrawals for irrigation by stream reaches that are hydraulically connected with the alluvial aquifer. The largest well yields range from 1,000 to 3,000 gal/min. Recharge to the aquifer principally is by infiltration of precipitation and water for surface water bodies. Both the spring and fall potentiometric surface maps show extensive cones of depression that result from large withdrawals for irrigation-one centered beneath Arkansas County, and another beneath western Poinsett and Cross Counties. Average water level differences between the spring and fall indicate a general decline of about 3 ft. The largest declines in water levels between 1981 and 1986 and the deepest water levels in 1986 occurred in areas most affected by large withdrawals for irrigation, as shown by the water level change map and depth to water map. The largest water level declines mainly occurred in central Lonoke County and in western Poinsett County. (USGS)","language":"ENGLISH","doi":"10.3133/wri884067","usgsCitation":"Plafcan, M., and Remsing, L.M., 1989, Water-level maps of the Mississippi River Valley alluvial aquifer in eastern Arkansas, 1986: U.S. Geological Survey Water-Resources Investigations Report 88-4067, 4 maps on 1 sheet ; sheet 94 x 132 cm. folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri884067.","productDescription":"4 maps on 1 sheet ; sheet 94 x 132 cm. folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":168815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81953,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4067/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db54539f","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":230135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remsing, Larry M.","contributorId":32221,"corporation":false,"usgs":true,"family":"Remsing","given":"Larry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":230136,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28903,"text":"wri894130 - 1989 - Effects of limestone quarrying and cement-plant operations on runoff and sediment yields in the Upper Permanente Creek basin, Santa Clara County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri894130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4130","title":"Effects of limestone quarrying and cement-plant operations on runoff and sediment yields in the Upper Permanente Creek basin, Santa Clara County, California","docAbstract":"High sediment loads below headwater areas of the Permanente Creek drainage basin, Santa Clara County, California, have caused flood-control problems in downstream lowland areas. Measured sediment yields in Permanente Creek, which drains areas affected by limestone quarrying and cement-plant operations, were 14 times greater than yields from the West Fork Permanente Creek, which primarily drains parkland. Part of this large disparity in yields is the result of higher runoff/unit of drainage area in the Permanente Creek Basin. Results of rainfall-runoff modeling indicate that the tendency for higher runoff from Permanente Creek results from natural differences in basin physiography. Runoff during periods of high streamflow (when most sediment is transported) is dominated by subsurface flow, which is not affected by human activities. Although artificial features created by human activities seem to have had only minor effects on runoff, they apparently have had major effects on sediment availability. Artificial features accounted for 273 acres (89%) of the 307 acres of active erosional landforms mapped in 1984. Increased availability of sediment in the Permanente Creek basin appears to be indicated by elevated intercepts of sediment-transport curves. A comparison of sediment-transport curves for the West Fork Permanente Creek with similar curves for the Permanente Creek basin under natural conditions suggests that the sediment yield from Permanente Creek is about 3.5 times higher than it would be under natural basin conditions. The increased yield apparently is due to an increase in sediment availability rather than an increase in runoff. 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The potentiometric-surface map for this aquifer, compiled from wastewater level measurements made during spring 1986, indicates a generally eastward and southward hydraulic gradient. The potentiometric surface also shows three major cones of depression resulting from groundwater withdrawals for industrial and public supplies; one centered in Columbia County, one in Union County, and one in Jefferson County. The water level change maps for the Sparta-Memphis aquifer for the period between spring 1981 and spring 1986 show large areas of both rise and decline in water levels across the study area. Largest rises occurred in parts of Jefferson, Columbia, and Phillips Counties, whereas largest declines occurred in parts of Union County. 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