{"pageNumber":"1886","pageRowStart":"47125","pageSize":"25","recordCount":68927,"records":[{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","interactions":[{"subject":{"id":14775,"text":"ofr86532 - 1987 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"ofr86532","publicationYear":"1987","noYear":false,"title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"predicate":"SUPERSEDED_BY","object":{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"wsp2336A","publicationYear":"1988","noYear":false,"chapter":"A","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"id":1}],"lastModifiedDate":"2016-08-05T11:55:09","indexId":"wsp2336A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"2336","chapter":"A","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","docAbstract":"<p>The Edwards aquifer is a complexly faulted, carbonate aquifer lying within the Balcones fault zone of south-central Texas. The aquifer consists of thin- to massive-bedded limestone and dolomite, most of which is in the form of mudstones and wackestones. Well-developed secondary porosity has formed in association with former erosional surfaces within the carbonate rocks, within dolomitized-burrowed tidal and evaporitic deposits, and along inclined fractures to produce an aquifer with transmissivities greater than 100 ft2/s. The aquifer is recharged mainly by streamflow losses in the outcrop area of the Edwards aquifer and is discharged by major springs located at considerable distances, as much as 150 mi, from the areas of recharge and by wells. Ground-water flow within the Edwards aquifer of the San Antonio region was simulated to investigate concepts relating to the storage and flow characteristics. The concepts of major interest were the effects of barrier faults on flow direction, water levels, springflow, and storage within the aquifer. A general-purpose, finite-difference model, modified to provide the capability of representing barrier faults, was used to simulate ground-water flow and storage in the aquifer. The approach in model development was to conduct a series of simulations beginning with a simple representation of the aquifer framework and then proceeding to subsequent representations of increasing complexity. The simulations investigated the effects of complex geologic structures and of significant changes in transmissivity, anisotropy, and storage coefficient. Initial values of transmissivity, anisotropy, and storage coefficient were estimated based on concepts developed in previous studies. Results of the simulations confirmed the original estimates of transmissivity values (greater than 100 square feet/s) in the confined zone of the aquifer between San Antonio and Comal Springs. A storage coefficient of 0.05 in the unconfined zone of the aquifer produced the best simulation of water levels and springflow. A major interpretation resulting from the simulations is that two essentially independent areas of regional flow were identified in the west and central part of the study area. Flows from the two areas converge at Comal Springs. The directions of computed flux vectors reflected the presence of major barrier faults, which locally deflect patterns of ground-water movement. The most noticeable deflection is the convergence of flow through a geologic structural opening, the Knippa gap, in eastern Uvalde County. A second significant interpretation is that ground-water flow in northeastern Bexar, Comal, and Hays Counties is diverted by barrier faults toward San Marcos Springs, a regional discharge point. Simulations showed that several barrier faults in the northwestern part of the San Antonio area had a significant effect on storage, water levels, and springflow within the Edwards aquifer.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2336A","usgsCitation":"Maclay, R.W., and Land, L.F., 1988, Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts: U.S. Geological Survey Water Supply Paper 2336, iv, 48 p., https://doi.org/10.3133/wsp2336A.","productDescription":"iv, 48 p.","endPage":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":27832,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2336a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2336a/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Edwards Aquifer","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2e45","contributors":{"authors":[{"text":"Maclay, Robert W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144799,"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":144800,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26239,"text":"wri874239 - 1988 - A water-resources appraisal of the Mount Shasta area in northern California, 1985","interactions":[],"lastModifiedDate":"2016-09-14T12:35:25","indexId":"wri874239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4239","title":"A water-resources appraisal of the Mount Shasta area in northern California, 1985","docAbstract":"Present Mount Shasta, California, area hydrologic characteristics were documented to compare future changes due to land use or volcanic activity. Lower flanks of Mount Shasta consist of broad aprons of pyroclastic-flow, debris flow, and fluvial deposits, with incised channels on upper parts of the mountain. Data include glacial areas and volumes, streamflow, sediment concentrations, temperature, and water chemistry of groundwater and springs. Many springs issue from fractures in lava and lava tubes around Mount Shasta and serve as sources of water for nearby towns. Groundwater levels fluctuate as much as 27 ft. Water sampled from wells meets U.S. Environmental Protection Agency drinking water standards. Streamflow is affected by snowfield and glacial melt and precipitation, with some streams showing diurnal variations related to daily air temperature changes. Only four streams have sufficient streamflow to travel more than about 6 mi from the summit; differences in low flows are attributed to groundwater stored in materials that compose the mountain and alluvial fans and the rain shadow effect on precipitation in northwest areas of the mountain. Most streamflow is ephemeral and percolates into channel beds on alluvial fans. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874239","usgsCitation":"Blodgett, J.C., Poeschel, K., and Thornton, J., 1988, A water-resources appraisal of the Mount Shasta area in northern California, 1985: U.S. Geological Survey Water-Resources Investigations Report 87-4239, v, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874239.","productDescription":"v, 46 p. :ill., maps ;28 cm.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":55040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4239/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4239/report-thumb.jpg"},{"id":55039,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4239/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d9f","contributors":{"authors":[{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":196040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poeschel, K.R.","contributorId":98715,"corporation":false,"usgs":true,"family":"Poeschel","given":"K.R.","affiliations":[],"preferred":false,"id":196042,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thornton, J.L.","contributorId":41460,"corporation":false,"usgs":true,"family":"Thornton","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":196041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20326,"text":"ofr88137 - 1988 - U.S. Geological Survey ground-water studies in Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr88137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-137","title":"U.S. Geological Survey ground-water studies in Massachusetts","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88137","usgsCitation":"Olimpio, J., 1988, U.S. Geological Survey ground-water studies in Massachusetts: U.S. Geological Survey Open-File Report 88-137, 2 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88137.","productDescription":"2 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0137/report-thumb.jpg"},{"id":49856,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0137/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6128d9","contributors":{"authors":[{"text":"Olimpio, J.C.","contributorId":36137,"corporation":false,"usgs":true,"family":"Olimpio","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":182454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55701,"text":"wdrMO871 - 1988 - Water resources data, Missouri, water year 1987","interactions":[],"lastModifiedDate":"2025-07-18T16:28:01.210194","indexId":"wdrMO871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MO-87-1","title":"Water resources data, Missouri, water year 1987","docAbstract":"<p>Water resources data for the 1987 year for Missouri consist of records of stage, discharge, and water quality of lakes and reservoirs; contains records for water discharge at 105 gaging stations; stage and contents at 10 lakes and reservoirs; water quality at 13 sampling stations (including 2 lakes); and data for 18 crest-stage stations.</p>","language":"English","publisher":"U.S. Geological 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,{"id":13027,"text":"ofr87704 - 1988 - Estimated water use in Iowa, 1985","interactions":[],"lastModifiedDate":"2016-03-09T12:48:39","indexId":"ofr87704","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-704","title":"Estimated water use in Iowa, 1985","docAbstract":"<p>Periodic assessments of water use in Iowa are needed to understand and manage the demands for the available water resources. This report summarizes where, how much, and for what purposes water was used in Iowa during 1985. The data are presented for the following categories: agricultural, self-supplied commercial, self-supplied domestic, self-supplied industrial, irrigation, mining, power generation (excluding hydroelectric plants), and public-water supply. The water-use data are further categorized by county, hydrologic unit subregion, and major aquifer system. During 1985, a total of 1,010,000 million gallons was estimated to have been withdrawn from Iowa's surface- and ground-water resources. Of this, 76 percent was withdrawn from surface-water sources and 24 percent from ground-water sources. Power generation was the largest water-use category, withdrawing 66 percent of the total withdrawals; 99 percent was from surface-water sources. Public-water supply was the second largest water-use category and accounted for 13 percent of total withdrawals; 74 percent was from ground-water sources. Self-supplied industries withdrew 7 percent of the total water use and agricultural withdrawals were 6 percent of the total water use. The remaining 8 percent was accounted for by irrigation (3 percent), self-supplied domestic (2 percent), mining (2 percent), and self-supplied commercial (1 percent) water users. The largest estimated water use occurred in Woodbury County where 201,000 million gallons was withdrawn. Pottawattamie County had the second largest water use with 182,000 million gallons. Other counties with significant withdrawals were Allamakee (74,900 million gallons), Muscatine (63,900 million gallons), and Clinton (62,300 million gallons). Power generation plants are in each of these counties. Surface-water withdrawals were most intensive along the Mississippi and Missouri Rivers. Nearly 80 percent of the surface water used in the State was by power generation plants on the border rivers. Surficial aquifers were the source of 60 percent of the ground-water withdrawals. The remaining 40 percent was withdrawn from the following aquifers: Silurian-Devonian, 14 percent; Cambrian-Ordovician, 13 percent; Dakota, 8 percent; and Mississippian-Pennsylvanian, 5 percent. It was estimated that 17 percent of the total surface water and ground water withdrawn was consumed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr87704","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources","usgsCitation":"Clark, M.L., and Thamke, J., 1988, Estimated water use in Iowa, 1985: U.S. Geological Survey Open-File Report 87-704, iii, 28 p: ill., maps; 22 x 28 cm., https://doi.org/10.3133/ofr87704.","productDescription":"iii, 28 p: ill., maps; 22 x 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":64594,"text":"i1420(NI16) - 1988 - Quaternary geologic map of the Lookout Mountain 4° x 6° quadrangle, United States","interactions":[],"lastModifiedDate":"2022-12-05T19:29:53.594623","indexId":"i1420(NI16)","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1420(NI-16)","subseriesTitle":"GAUS","title":"Quaternary geologic map of the Lookout Mountain 4° x 6° quadrangle, United States","docAbstract":"<p>This map is part of the Quaternary Geologic Atlas of the United States (I–1420). It was first published as a printed edition in 1988. The geologic data have now been captured digitally and are presented here along with images of the printed map sheet and component parts as PDF files.</p>\n<br/>\n<p>The Quaternary Geologic Map of the Lookout Mountain 4° x 6° Quadrangle was mapped as part of the Quaternary Geologic Atlas of the United States.  The atlas was begun as an effort to depict the areal distribution of surficial geologic deposits and other materials that accumulated or formed during the past 2+ million years, the period that includes all activities of the human species.  These materials are at the surface of the Earth.  They make up the \"ground\" on which we walk, the \"dirt\" in which we dig foundations, and the \"soil\" in which we grow crops.  Most of our human activity is related in one way or another to these surface materials that are referred to collectively by many geologists as regolith, the mantle of fragmental and generally unconsolidated material that overlies the bedrock foundation of the continent.  The maps were compiled at 1:1,000,000 scale.</p>\n<br/>\n<p>In recent years, surficial deposits and materials have become the focus of much interest by scientists, environmentalists, governmental agencies, and the general public. They are the foundations of ecosystems, the materials that support plant growth and animal habitat, and the materials through which travels much of the water required for our agriculture, our industry, and our general well being. They also are materials that easily can become contaminated by pesticides, fertilizers, and toxic wastes. In this context, the value of the surficial geologic map is evident.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1420(NI16)","collaboration":"Prepared in cooperation with the Geological Survey of Alabama, the Tennessee Division of Geology, the Georgia Geological Survey, the Mississippi Geological Survey, the Department of Geology, University of North Carolina, and the Arkansas Geological Commission","usgsCitation":"Maher, S.W., Copeland, C.W., Rheams, K.F., Neathery, T.L., Gilliland, W.A., Friddell, M.S., Van Nostrand, A.K., Wheeler, W.H., Holbrook, D.F., Bush, W.V., Fullerton, D.S., and Bush, C.A., 1988, Quaternary geologic map of the Lookout Mountain 4° x 6° quadrangle, United States (Original edition: First published in 1988, paper publication only; Digital edition: Posted online April 2014): U.S. Geological Survey IMAP 1420(NI-16), Report: 15 p.; Map: 58.43 x 30.92 inches; Downloads Directory, https://doi.org/10.3133/i1420(NI16).","productDescription":"Report: 15 p.; Map: 58.43 x 30.92 inches; Downloads Directory","numberOfPages":"15","additionalOnlineFiles":"Y","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":187190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i1420(NI16).jpg"},{"id":106732,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9208.htm","linkFileType":{"id":5,"text":"html"},"description":"9208"},{"id":285393,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/imap/i-1420/ni-16/downloads/DigitalEditionHistory.pdf"},{"id":285390,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/i-1420/ni-16/pdf/i1420_ni-16_map.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":285373,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-1420/ni-16/","linkFileType":{"id":5,"text":"html"}},{"id":285391,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/i-1420/ni-16/downloads/textonly.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":285394,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/imap/i-1420/ni-16/downloads/"}],"scale":"1000000","projection":"Lambert Conformal Conic Projection","country":"United States","state":"Alabama, Arkansas, Georgia, Mississippi, North Carolina, Tennessee","otherGeospatial":"Lookout Mountain 4° x 6° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.0,32.0 ], [ -90.0,36.0 ], [ -84.0,36.0 ], [ -84.0,32.0 ], [ -90.0,32.0 ] ] ] } } ] }","edition":"Original edition: First published in 1988, paper publication only; Digital edition: Posted online April 2014","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8316","contributors":{"compilers":[{"text":"Miller, Robert A.","contributorId":52938,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":749856,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"editors":[{"text":"Richmond, Gerald M.","contributorId":87165,"corporation":false,"usgs":true,"family":"Richmond","given":"Gerald M.","affiliations":[],"preferred":false,"id":749855,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Maher, Stuart W.","contributorId":42134,"corporation":false,"usgs":true,"family":"Maher","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":271631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Copeland, Charles W. Jr.","contributorId":94973,"corporation":false,"usgs":true,"family":"Copeland","given":"Charles","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":271637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rheams, Katherine F.","contributorId":101560,"corporation":false,"usgs":true,"family":"Rheams","given":"Katherine","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":271640,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Neathery, Thorton L.","contributorId":58189,"corporation":false,"usgs":true,"family":"Neathery","given":"Thorton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":271633,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gilliland, William A.","contributorId":61721,"corporation":false,"usgs":true,"family":"Gilliland","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":271635,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Friddell, Michael S.","contributorId":95387,"corporation":false,"usgs":true,"family":"Friddell","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":271638,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Van Nostrand, Arnie K.","contributorId":60130,"corporation":false,"usgs":true,"family":"Van Nostrand","given":"Arnie","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":271634,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wheeler, Walter H.","contributorId":26372,"corporation":false,"usgs":true,"family":"Wheeler","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":271630,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Holbrook, Drew F.","contributorId":50819,"corporation":false,"usgs":true,"family":"Holbrook","given":"Drew","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":271632,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Bush, William V.","contributorId":93536,"corporation":false,"usgs":true,"family":"Bush","given":"William","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":271636,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Fullerton, David S. fullerton@usgs.gov","contributorId":448,"corporation":false,"usgs":true,"family":"Fullerton","given":"David","email":"fullerton@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":271628,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Bush, Charles A.","contributorId":97876,"corporation":false,"usgs":true,"family":"Bush","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":271639,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":55725,"text":"wdrNJ872 - 1988 - Water resources data for New Jersey, water year 1987, volume 2, Delaware River basin and tributaries to Delaware Bay","interactions":[],"lastModifiedDate":"2019-09-24T11:54:11","indexId":"wdrNJ872","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NJ-87-2","title":"Water resources data for New Jersey, water year 1987, volume 2, Delaware River basin and tributaries to Delaware Bay","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNJ872","usgsCitation":"Bauersfeld, W., Moshinsky, E., Pustay, E., and Jones, W., 1988, Water resources data for New Jersey, water year 1987, volume 2, 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,{"id":29613,"text":"wri884001 - 1988 - Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Tulare Lake bed area, southern San Joaquin Valley, California, 1986-87","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri884001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4001","title":"Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Tulare Lake bed area, southern San Joaquin Valley, California, 1986-87","docAbstract":"Concentrations of numerous toxic trace elements and pesticides were measured during 1986 in water, sediment, and biota from three areas near the Tulare Lake Bed, southern San Joaquin Valley, California: Kern National Wildlife Refuge, Pixley National Wildlife Refuge, and Westfarmers evaporation ponds about 5 mi west of Kern National Wildlife Refuge, to determine whether toxic constituents in agricultural-irrigation drainage pose a threat to beneficial uses of water, especially to uses by wildlife. Pesticide residues were found to be low at all three areas. Trace element concentrations were found to be comparatively low at the Kern and Pixley National Wildlife Refuge areas and high at the Westfarmers evaporation ponds. Dissolved selenium concentrations were &lt; 1 micrograms/L (ug/L) in areas on and adjacent to the refuges, but ranged from 110 to 360 ug/L in the saline drainwater impounded in the evaporation ponds. The ratio of mean selenium concentrations in biota from Westfarmers ponds compared to biota from Kesterson National Wildlife Refuge (where adverse effects have been documented) is 5 for waterboatman, 2 for avocet liver, 1 for avocet eggs, and &lt; 1 for widgeongrass. The low concentrations measured at Kern and Pixley National Wildlife Refuges suggest that trace elements and pesticides pose little threat to wildlife there; however, impounded subsurface drainage from agricultural irrigation does pose a threat to wildlife at the nearby Westfarmers ponds. Preliminary results of surveys conducted in 1987 indicated that there are adverse biological effects on shorebirds nesting at the ponds, although interpretation of the magnitude of the effects is premature, pending completion of ongoing studies by the U.S. Fish and Wildlife Service. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884001","usgsCitation":"Schroeder, R.A., Palawski, D.U., and Skorupa, J.P., 1988, Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Tulare Lake bed area, southern San Joaquin Valley, California, 1986-87: U.S. Geological Survey Water-Resources Investigations Report 88-4001, vi, 86 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/wri884001.","productDescription":"vi, 86 p. :ill., maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":110251,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46933.htm","linkFileType":{"id":5,"text":"html"},"description":"46933"},{"id":160409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4001/report-thumb.jpg"},{"id":58436,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4001/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58437,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4001/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625893","contributors":{"authors":[{"text":"Schroeder, R. A.","contributorId":15554,"corporation":false,"usgs":true,"family":"Schroeder","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201814,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palawski, D. U.","contributorId":56240,"corporation":false,"usgs":true,"family":"Palawski","given":"D.","email":"","middleInitial":"U.","affiliations":[],"preferred":false,"id":201815,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Skorupa, J. P.","contributorId":93002,"corporation":false,"usgs":false,"family":"Skorupa","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":201816,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29811,"text":"wri884146 - 1988 - Estimation, analysis, sources, and verification of consumptive water use data in the Great Lakes-St. Lawrence River basin","interactions":[],"lastModifiedDate":"2023-03-07T21:36:16.690138","indexId":"wri884146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4146","title":"Estimation, analysis, sources, and verification of consumptive water use data in the Great Lakes-St. Lawrence River basin","docAbstract":"<p>The Great Lakes-St. Lawrence River basin provides water for many uses and for wildlife habitat; thus many groups have developed strategies to manage the basin 's water resource. The International Joint Commission (IJC) is reviewing and comparing available consumptive-use data to assess the magnitude and effect of consumptive uses under present projected economic and hydraulic conditions on lake levels. As a part of this effort, the U.S. Geological Survey compared its own estimates of consumptive use in the United States with those generated by (1) the International Great Lakes Diversions and (2) the IJC. The U.S. Geological Survey also developed two methods of calculating consumptive-use projections for 1980 through 2000; one method yields an estimate of 6,490 cu ft/s for the year 2000; the other yields an estimate of 8,330 cu ft/s. These two projections could be considered the upper and lower limits for the year 2000. The reasons for the varying estimates are differences in (1) methods by which base year values were developed, and (2) the methods or models that were used to project consumptive-use values for the future. Acquisition of consumptive-use data from water users or governmental agencies or ministries would be desirable to minimize reliance on estimates.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884146","usgsCitation":"Snavely, D.S., 1988, Estimation, analysis, sources, and verification of consumptive water use data in the Great Lakes-St. Lawrence River basin: U.S. Geological Survey Water-Resources Investigations Report 88-4146, iv, 28 p., https://doi.org/10.3133/wri884146.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":122730,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4146/report-thumb.jpg"},{"id":58612,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413791,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47055.htm","linkFileType":{"id":5,"text":"html"}}],"country":"Canada, United States","otherGeospatial":"Great Lakes-St. Lawrence River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -92.34309234262025,\n              49.96207763484773\n            ],\n            [\n              -92.34309234262025,\n              40.684336825120965\n            ],\n            [\n              -70.33475867425648,\n              40.684336825120965\n            ],\n            [\n              -70.33475867425648,\n              49.96207763484773\n            ],\n            [\n              -92.34309234262025,\n              49.96207763484773\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb1be","contributors":{"authors":[{"text":"Snavely, D. S.","contributorId":103692,"corporation":false,"usgs":true,"family":"Snavely","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":202170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55187,"text":"wdrHI872 - 1988 - Water resources data for Hawaii and other Pacific areas, water year 1987: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau, and American Samoa","interactions":[],"lastModifiedDate":"2026-03-06T15:39:20.352396","indexId":"wdrHI872","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"HI-87-2","title":"Water resources data for Hawaii and other Pacific areas, water year 1987: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau, and American Samoa","docAbstract":"<p>Volume 2 of water resources data for the 1987 water year for other Pacific areas consists of records of streamflow and stage of 2 lakes and a reservoir; and water levels and water quality in wells. This report contains discharge records for 26 gaging stations; stage only record for 3 gaging stations; water temperature for 26 gaging stations; and water levels for 36 observations wells and water quality for 64 ground-water sites. Also included are 12 low-flow and 2 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. 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,{"id":55724,"text":"wdrNJ871 - 1988 - Water resources data for New Jersey, water year 1987, volume 1, Atlantic slope basins, Hudson River to Cape May","interactions":[],"lastModifiedDate":"2020-12-22T18:30:32.124531","indexId":"wdrNJ871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NJ-87-1","title":"Water resources data for New Jersey, water year 1987, volume 1, Atlantic slope basins, Hudson River to Cape May","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNJ871","usgsCitation":"Bauersfeld, W., Moshinsky, E., Pustay, E., and Jones, W., 1988, Water resources data for New Jersey, water year 1987, volume 1, 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,{"id":55184,"text":"wdrHI861 - 1988 - Water resources data for Hawaii and other Pacific areas, water year 1986: Volume 1. Hawaii","interactions":[],"lastModifiedDate":"2026-03-06T16:16:30.810542","indexId":"wdrHI861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"HI-86-1","title":"Water resources data for Hawaii and other Pacific areas, water year 1986: Volume 1. Hawaii","docAbstract":"<p>Water resources data for the 1986 water year for Hawaii and other Pacific Areas consist of records of stage, discharge, and water quality of streams and springs; and water levels and water quality in wells. This report, volume 1, contains discharge records for 83 gaging stations; water quality for 13 gaging stations, 73 partial-record flow stations, and 172 wells; and water levels for 40 observations wells. Also included are 107 crest-stage partial-record stations and 10 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, Federal, and other agencies in Hawaii.&nbsp;<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrHI861","collaboration":"Prepared in cooperation with the State of Hawaii Department of Land and Natural Resources, Division of Water and Land Development and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Water resources data for Hawaii and other Pacific areas, water year 1986, volume 1, Hawaii: U.S. Geological Survey Water Data Report HI-86-1, 295 p., https://doi.org/10.3133/wdrHI861.","productDescription":"x, 295 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,{"id":29948,"text":"wri884011 - 1988 - Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the middle Green River basin, Utah, 1986-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri884011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4011","title":"Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the middle Green River basin, Utah, 1986-87","docAbstract":"Reconnaissance of wildlife areas in the middle Green River basin of Utah was conducted during 1986 and 1987 to determine whether irrigation drainage has caused, or has the potential to cause significant harmful effects on human health, fish, and wildlife, or may adversely affect the suitability of water for beneficial uses. Studies at Stewart Lake Waterfowl Management Area and Ouray National Wildlife Refuge indicated that concentrations of boron, selenium, and zinc in water, bottom sediment, and biological tissue were sufficiently large to be harmful to fish and wildlife, and to adversely affect beneficial uses of water. Selenium is the principal element of concern in both areas. Concentrations of dissolved selenium in irrigation drain water entering Stewart Lake Waterfowl Management Area ranged from 14-140 micrograms/L (ug/L) and consistently exceeded Utah standards for wildlife protection in water in two of the four drains. Concentrations of boron and zinc exceeded Utah standards only occasionally in the drain waters. Concentrations of total selenium in sediments collected where the drains discharge into the lake were 10-85 ug/gm. Liver tissue collected from American coots at Stewart Lake Waterfowl Management Area contained concentrations of selenium from 4.9-26 ug/gm (dry weight), and whole body samples of carp contained as much as 31 ug/gm (dry weight). Concentrations of selenium in Potamogeton and blue-green algae ranged from 2.1-27 ug/gm. Concentrations of boron, selenium, and zinc were also measured in water from Ouray National Wildlife Refuge. Liver tissue of American coots from the North Roadside Pond, which receives irrigation tailwater, contained a geometric-mean concentration of selenium of 32 ug/gm (dry weight). Five water-bird eggs collected from the North and South Roadside Ponds contained selenium concentrations of 63-120 ug/gm (dry weight). (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884011","usgsCitation":"Stephens, D.W., Waddell, B., and Miller, J.B., 1988, Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the middle Green River basin, Utah, 1986-87: U.S. Geological Survey Water-Resources Investigations Report 88-4011, vii, 70 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884011.","productDescription":"vii, 70 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4011/report-thumb.jpg"},{"id":58769,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63eaa6","contributors":{"authors":[{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":202410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, Bruce","contributorId":55033,"corporation":false,"usgs":false,"family":"Waddell","given":"Bruce","email":"","affiliations":[{"id":6661,"text":"US Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":202409,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, J. B.","contributorId":70423,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":202411,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":65369,"text":"i1915 - 1988 - Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i1915","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1915","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","language":"ENGLISH","doi":"10.3133/i1915","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars: U.S. Geological Survey IMAP 1915, 1 remote sensing image ;61 x 49 cm., on sheet 95 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1915.","productDescription":"1 remote sensing image ;61 x 49 cm., on sheet 95 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100927,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1915/plate-1.pdf","size":"5988","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f39","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12518,"text":"ofr87552 - 1988 - Water resources publications of the U.S. Geological Survey for Tennessee, 1906-1987","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr87552","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-552","title":"Water resources publications of the U.S. Geological Survey for Tennessee, 1906-1987","docAbstract":"A bibliography of publications has been compiled of the water resources investigations published by the U.S. Geological Survey , Water Resources Division, in Tennessee. The bibliography includes an alphabetical listing by author, as well as listings by general and specific areas in Tennessee. The publications are classified also by discipline and type of report: open-file reports, water supply papers, water resources investigations, professional papers, circulars, hydrologic investigations atlases, miscellaneous investigations maps, journal and symposium articles, water resources bulletin articles, and water resources data reports. (USGS)","language":"ENGLISH","doi":"10.3133/ofr87552","usgsCitation":"Baker, E., and Massingill, R., 1988, Water resources publications of the U.S. Geological Survey for Tennessee, 1906-1987: U.S. Geological Survey Open-File Report 87-552, iii, 34 p. :ill. ;28 cm., https://doi.org/10.3133/ofr87552.","productDescription":"iii, 34 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":146507,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":984,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_87-552","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d15","contributors":{"authors":[{"text":"Baker, E.G.","contributorId":84382,"corporation":false,"usgs":true,"family":"Baker","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":166266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Massingill, R.C.","contributorId":20756,"corporation":false,"usgs":true,"family":"Massingill","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":166265,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29636,"text":"wri884078 - 1988 - Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 12","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri884078","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4078","title":"Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 12","docAbstract":"This report delineates and describes the geohydrology and susceptibility of major aquifers to contamination in Coffee, Dale, Henry, Houston, and Geneva Counties, Alabama. The major aquifers are the Upper Floridan, Lisbon, Nanafalia-Clayton, and Providence-Ripley aquifers. Estimated groundwater withdrawals for public water supplies are about 42 million gal/day. Maximum withdrawals for irrigation are 15 to 20 million gal/day. Withdrawals for self-supplied industrial and domestic uses are estimated to be 3 and 2.5 million gal/day, respectively. Long-term withdrawals of water from the Nanafalia-Clayton aquifer have resulted in significant declines in the potentiometric surface in Coffee, Dale, and Houston Counties. Significant declines in the potentiometric surfaces of the other major aquifers are not apparent. Recharge areas for all major aquifers are susceptible to contamination, but the probability of contamination of the Lisbon, Nanafalia-Clayton, and Providence-Ripley aquifers is low because the recharge areas are remote from areas of withdrawal. The recharge area for the Floridan aquifer, which consists largely of flat, sandy farmland , coincides with the area of use. This area is highly susceptible to contamination from insecticides and herbicides. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884078","usgsCitation":"Scott, J.C., and Cobb, R., 1988, Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 12: U.S. Geological Survey Water-Resources Investigations Report 88-4078, v, 51 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wri884078.","productDescription":"v, 51 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":122224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4078/report-thumb.jpg"},{"id":58457,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4078/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58458,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8bed","contributors":{"authors":[{"text":"Scott, J. C.","contributorId":75901,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobb, R.H.","contributorId":31027,"corporation":false,"usgs":true,"family":"Cobb","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":201855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65245,"text":"i2008 - 1988 - Controlled photomosaic and revised shaded relief map of the Elysium Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i2008","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2008","subseriesTitle":"NONE","title":"Controlled photomosaic and revised shaded relief map of the Elysium Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i2008","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Controlled photomosaic and revised shaded relief map of the Elysium Quadrangle of Mars (Rev.): U.S. Geological Survey IMAP 2008, 2 remote-sensing images :1 col. ;37 x 53 cm., on sheets 67 x 67 cm. and 59 x 61 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2008.","productDescription":"2 remote-sensing images :1 col. ;37 x 53 cm., on sheets 67 x 67 cm. and 59 x 61 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260748,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2008/plate-1.pdf"},{"id":260749,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2008/plate-2.pdf"}],"scale":"5000000","edition":"Rev.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68af99","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533649,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30613,"text":"wri874066 - 1988 - Simulated effects of ground-water management alternatives for the Salinas Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:59","indexId":"wri874066","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4066","title":"Simulated effects of ground-water management alternatives for the Salinas Valley, California","docAbstract":"A two-dimensional digital groundwater flow model was developed to analyze the geohydrology of the groundwater basin in the Salinas Valley. The model was calibrated for steady-state and transient simulations by comparing simulated with measured or estimated inflows, outflows, and water levels for 1970-81. Preliminary estimates of hydraulic properties and some inflows and outflows were adjusted during model calibration. The simulated mean annual water budget for the basin was 559,500 acre-ft/yr each of outflow and inflow. Inflow components consisted of Salinas River recharge (38.3%), percolation of irrigation water (34.0%), small stream and Arroyo Seco recharge (20.9%), seawater intrusion (3.4%), and other sources (3.4%). Outflow components consisted of agricultural pumpage (91.5%), municipal pumpage (4.0%), and riparian phreatophyte evapotranspiration (4.5%). For the steady-state calibration, 70% of the simulated water levels were within 9 ft of measured water levels for 1970-81. A sensitivity analysis determined the overall stability of the model results. The model input variable that probably contributes most to the uncertainty of the results is the quantity of groundwater recharge contributed by irrigation-return flow to the unconfined aquifer. A 15% change in the estimate of this variable causes an 11% change in the simulated river-seepage rate and a 6% change in the simulated seawater intrusion rate. The calibrated model was used to investigate several water resources management alternatives. Projected pumpage increase at a rate of 1%/yr for 20 yr caused declines in mean annual water levels of 10 to 20 ft in some areas and an increase in seawater intrusion from 18,900 to 23 ,600 acre-ft/yr. Pumpage decreases in the coastal area decreased seawater intrusion more effectively than pumpage decreases farther inland. When pumpage was decreased uniformly throughout the valley, the decrease in seawater intrusion was only one-fourteenth the decrease in pumpage. Simulations indicated that replacement of groundwater pumpage with imported surface water in a 9,000 acre service area near the coast would result in a decrease in seawater intrusion equaling nearly one-half the quantity of imported water. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874066","usgsCitation":"Yates, E., 1988, Simulated effects of ground-water management alternatives for the Salinas Valley, California: U.S. Geological Survey Water-Resources Investigations Report 87-4066, vii, 79 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874066.","productDescription":"vii, 79 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":160150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4066/report-thumb.jpg"},{"id":59380,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4066/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f54","contributors":{"authors":[{"text":"Yates, E.B.","contributorId":77973,"corporation":false,"usgs":true,"family":"Yates","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":203542,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66542,"text":"i1875 - 1988 - Subsurface geology of Paleozoic, Mesozoic, and Cenozoic units in southeast Missouri","interactions":[],"lastModifiedDate":"2016-08-23T09:34:53","indexId":"i1875","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1875","title":"Subsurface geology of Paleozoic, Mesozoic, and Cenozoic units in southeast Missouri","docAbstract":"<p>The U.S. Geological Survey is conducting a regional water-resources investigation of the Gulf Costal Plain, which includes all of the Mississippi Alluvial Plain of southeastern Missouri, locally known as the southeast lowlands. The purpose of the regional study is to describe and evaluate the major aquifer systems in sediments of Tertiary and younger age in parts of 10 states (Grubb, 1984). In the southeast lowlands of Missouri, the sub-surface stratigraphy and structural configuration of geologic units need to be described in detail to define the major aquifer syustems in the area. The purpose of this report is to describe the subsurface geologic framework for Paleozoic, Mesozoic, and Cenozoic units in the southeast lowlands of Missouri and to correlate these units to those in adjecent States using geophysical and geologic methods (index map). Geophysical logs of wells were used to determine which units are aquifers or confining beds. The drilling of the U.S. Geological Survey test well 1-X in New Madrid County, Missouri, and the subsequent interpretation of geohydrologic data from the well have provided valuable information used in the preparation of this report.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1875","usgsCitation":"Mesko, T.O., 1988, Subsurface geology of Paleozoic, Mesozoic, and Cenozoic units in southeast Missouri: U.S. Geological Survey IMAP 1875, 2 Plates: 40.79 x 54.10 inches and 36.42 x 18.93 inches, https://doi.org/10.3133/i1875.","productDescription":"2 Plates: 40.79 x 54.10 inches and 36.42 x 18.93 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":187893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i1875.GIF"},{"id":327511,"rank":701,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1875/plate-1.pdf"},{"id":327512,"rank":702,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1875/plate-2.pdf"},{"id":107160,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9963.htm","linkFileType":{"id":5,"text":"html"},"description":"9963"}],"scale":"500000","country":"United States","state":"Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.50561523437499,\n              37.309014074275915\n            ],\n            [\n              -89.36279296875,\n              37.00255267215955\n            ],\n            [\n              -89.329833984375,\n              37.142803443716836\n            ],\n            [\n              -89.12109375,\n              37.06394430056685\n            ],\n            [\n              -88.978271484375,\n              36.87962060502676\n            ],\n            [\n              -88.978271484375,\n              36.641977814705946\n            ],\n            [\n              -89.066162109375,\n              36.421282443649496\n            ],\n            [\n              -89.329833984375,\n              36.25313319699069\n            ],\n            [\n              -89.50561523437499,\n              35.96022296929667\n            ],\n            [\n              -89.6044921875,\n              35.85343961959182\n            ],\n            [\n              -89.80224609374999,\n              35.7286770448517\n            ],\n            [\n              -90.5712890625,\n              35.71975793933433\n            ],\n            [\n              -90.59326171875,\n              36.491973470593685\n            ],\n            [\n              -90.37353515625,\n              36.69485094156225\n            ],\n            [\n              -90.19775390625,\n              36.730079507078415\n            ],\n            [\n              -90.02197265625,\n              37.03763967977139\n            ],\n            [\n              -89.98901367187499,\n              37.16031654673677\n            ],\n            [\n              -89.835205078125,\n              37.26530995561875\n            ],\n            [\n              -89.593505859375,\n              37.32648861334206\n            ],\n            [\n              -89.50561523437499,\n              37.309014074275915\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a12","contributors":{"authors":[{"text":"Mesko, T. 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,{"id":29843,"text":"wri874048 - 1988 - Geologic and geohydrologic reconnaissance of Staten Island, New York","interactions":[],"lastModifiedDate":"2022-03-28T18:58:50.802783","indexId":"wri874048","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4048","title":"Geologic and geohydrologic reconnaissance of Staten Island, New York","docAbstract":"The public water supply for about 350,000 people on Staten Island (Richmond County)--a mainly suburban 60-sq mi borough of the City of New York is provided by the City from reservoirs in upstate New York. Since 1962, many individuals and businesses have used groundwater for supplemental supply as a result of the City 's ban on the use of public supply water for irrigation, swimming pools, and automobile washing during protracted droughts that depleted the reservoirs. Hundreds of wells were installed on the island during droughts of 1962-66 and 1983-85. Bedrock of Late Proterozoic to Jurassic age and unconsolidated deposits of the Upper Cretaceous and late Pleistocene age contain groundwater that is generally suitable for the city prohibited purposes. The groundwater of the island receives sufficient recharge to meet the current demands and could sustain considerably greater withdrawals. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874048","usgsCitation":"Soren, J., 1988, Geologic and geohydrologic reconnaissance of Staten Island, New York: U.S. Geological Survey Water-Resources Investigations Report 87-4048, Report: v, 22 p.; 4 Plates: 18.07 × 19.67 inches or smaller, https://doi.org/10.3133/wri874048.","productDescription":"Report: v, 22 p.; 4 Plates: 18.07 × 19.67 inches or smaller","costCenters":[],"links":[{"id":58651,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4048/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58650,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4048/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58654,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4048/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397734,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46730.htm"},{"id":124181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4048/report-thumb.jpg"},{"id":58653,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4048/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58652,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4048/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"41700","country":"United States","state":"New York","otherGeospatial":"Staten Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.24491882324219,\n              40.49395938772784\n            ],\n            [\n              -74.19204711914062,\n              40.50753459933616\n            ],\n            [\n              -74.12200927734375,\n              40.534676780615406\n            ],\n            [\n              -74.04098510742188,\n              40.60456943720527\n            ],\n            [\n              -74.080810546875,\n              40.65355504328839\n            ],\n            [\n              -74.12956237792969,\n              40.64157252400389\n            ],\n            [\n              -74.18655395507812,\n              40.64730356252251\n            ],\n            [\n              -74.20440673828125,\n              40.6306300839918\n            ],\n            [\n              -74.19960021972656,\n              40.60978237983301\n            ],\n            [\n              -74.20578002929688,\n              40.58475654701271\n            ],\n            [\n              -74.21195983886719,\n              40.56911064456484\n            ],\n            [\n              -74.2181396484375,\n              40.558156335842106\n            ],\n            [\n              -74.23805236816406,\n              40.558156335842106\n            ],\n            [\n              -74.25247192382812,\n              40.545634930725775\n            ],\n            [\n              -74.24697875976562,\n              40.522150985623796\n            ],\n            [\n              -74.25453186035156,\n              40.51171103483292\n            ],\n            [\n              -74.25315856933594,\n              40.49918094806632\n            ],\n            [\n              -74.24491882324219,\n              40.49395938772784\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a56f5","contributors":{"authors":[{"text":"Soren, Julian","contributorId":54184,"corporation":false,"usgs":true,"family":"Soren","given":"Julian","email":"","affiliations":[],"preferred":false,"id":202227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65370,"text":"i1916 - 1988 - Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i1916","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1916","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","language":"ENGLISH","doi":"10.3133/i1916","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars: U.S. Geological Survey IMAP 1916, 1 remote sensing image ;62 x 49 cm., on sheet 96 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1916.","productDescription":"1 remote sensing image ;62 x 49 cm., on sheet 96 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100928,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1916/plate-1.pdf","size":"5075","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f3c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12726,"text":"ofr88129 - 1988 - U.S. Geological Survey ground-water studies in Oregon","interactions":[],"lastModifiedDate":"2017-02-07T09:36:01","indexId":"ofr88129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-129","title":"U.S. Geological Survey ground-water studies in Oregon","docAbstract":"The use of groundwater in Oregon is expected to increase owing to continued population growth and to surface water supplies that are inadequate to meet present or future demand. The major groundwater issues in Oregon are: conjunctive use of surface and groundwater; contamination from hazardous wastes, leakage from underground gasoline and diesel tanks, naturally occurring brackish water, and high concentrations of dissolved iron; groundwater availability; and Indian water rights. Before 1987, the Oregon Water Resources Department, in cooperation with the U.S. Geological Survey (USGS), maintained a network of about 400 observation wells in Oregon to monitor fluctuations in groundwater levels. Water levels currently are measured cooperatively only in active project areas. The USGS has conducted more than 120 hydrologic investigations in Oregon. During fiscal year 1987, the USGS entered into cooperative agreements with 23 local, State, and Federal agencies to conduct hydrologic investigations in Oregon; six investigations included quantitative studies of groundwater. Examples of these groundwater studies are: groundwater hydrology of the Portland basin; groundwater hydrology in the Umatilla Plateau; and iron geochemistry of a sand dune aquifer near Coos Bay. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88129","usgsCitation":"Bolke, E., 1988, U.S. Geological Survey ground-water studies in Oregon: U.S. Geological Survey Open-File Report 88-129, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr88129.","productDescription":"2 p. :map ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":145765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0129/report-thumb.jpg"},{"id":41136,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6124ec","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":166606,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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