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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr88305","usgsCitation":"Frenzel, P.F., Kaehler, C., and Anderholm, S., 1990, Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas: U.S. Geological Survey Open-File Report 88-305, Report: xii, 179 p.; 5 Plates: 17.29 x 20.97 inches or smaller, https://doi.org/10.3133/ofr88305.","productDescription":"Report: xii, 179 p.; 5 Plates: 17.29 x 20.97 inches or smaller","costCenters":[],"links":[{"id":383000,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382999,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382998,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382997,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382996,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382995,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0305/report-thumb.jpg"}],"country":"United States","state":"New Mexico, Texas","county":"Dona Ana County, New Mexico, El Paso County, Texas","otherGeospatial":"Mesilla Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.85302734374999,\n 31.53640812943961\n ],\n [\n -105.7159423828125,\n 31.53640812943961\n ],\n [\n -105.7159423828125,\n 32.368363067704706\n ],\n [\n -106.85302734374999,\n 32.368363067704706\n ],\n [\n -106.85302734374999,\n 31.53640812943961\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c5b","contributors":{"authors":[{"text":"Frenzel, P. F.","contributorId":98726,"corporation":false,"usgs":true,"family":"Frenzel","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":180088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaehler, C. A.","contributorId":59469,"corporation":false,"usgs":true,"family":"Kaehler","given":"C. A.","affiliations":[],"preferred":false,"id":180086,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderholm, S. K.","contributorId":69149,"corporation":false,"usgs":true,"family":"Anderholm","given":"S. K.","affiliations":[],"preferred":false,"id":180087,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68577,"text":"ha715 - 1990 - Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States","interactions":[{"subject":{"id":12617,"text":"ofr86402W - 1986 - Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States","indexId":"ofr86402W","publicationYear":"1986","noYear":false,"chapter":"W","title":"Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States"},"predicate":"SUPERSEDED_BY","object":{"id":68577,"text":"ha715 - 1990 - Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States","indexId":"ha715","publicationYear":"1990","noYear":false,"title":"Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States"},"id":1}],"lastModifiedDate":"2015-10-28T12:04:10","indexId":"ha715","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"715","title":"Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States","docAbstract":"In 1984, the U.S. Geological Survey began a study of the geologic and hydrologic characteristics of the unsaturated zone in the western conterminous United States. The study area extends from the eastern edge of the Rocky Mountains westward and includes all or parts of the 12 westernmost conterminous States. The goal of the study is to characterize unsaturated flow systems to aid in identifying environments in the western United States that may merit further study for isolation of hazardous waste, including high- and low-level radioactive waste and other toxic waste.
The major physiographic areas discussed in this report (see index map below thickness map) are: (1) Rocky Mountain System consisting of the Southern, Middle, and Northern Rocky Mountains, and the Wyoming Basin; (2) Intermontane Plateaus consisting of the Basin and Range province, and the Colorado and Columbia Plateaus; and (3) Pacific Mountain System (Fenneman, 1946). Two of these areas, the Colorado and Columbia plateaus, exhibit a variety of geohydrologic conditions, and therefore are further subdivided in the discussions that follow.
Outstanding features peculiar to the mountainous area of the Rocky Mountain and the Pacific Mountain Systems are the high rugged mountains and steep relief. These mountains receive greater precipitation than do the lower parts of the otherwise dry western United States. Generally moisture-laden air masses move eastward across the continent, and the mountains force them to higher, cooler altitudes. As the air cools, moisture condenses and precipitates. As a result, the Rocky Mountain and Pacific Mountain Systems have annual precipitation in excess of 30 in.
The Wyoming Basin of the Rocky Mountain System and the Basin and Range province, Colorado Plateaus, and Columbia Plateaus of the Intermontane Plateaus generally have lower altitudes and less relief than do the mountainous areas. The climate throughout most of these provinces generally is semiarid to arid. Annual precipitation is generally less than 16 in. throughout most of the area, and is less than 4 in. in some parts. The mean annual free-water-surface evaporation ranges from 20 to 100in. A large part of the study area is subject to a water deficit because potential evapotranspiration exceeds precipitation. As a consequence of the large water deficit, ground-water recharge generally is small, surface runoff is small, perennial streams and lakes are few, and the depth to ground water commonly is large. The generalized thickness of the unsaturated zone (the depth to ground water), in the western conterminous United States is presented on the map.
Water-quality and streamflow data were collected in the Coteau des Prairies region of southwestern Minnesota and eastern South Dakota to document the water-quality characteristics of streams and impoundments in the Coteau, and to predict the effect of proposed impoundments on the quality of water in Coteau streams.
\nReconnaissance data collection at 66 stream and 24 impoundment sites plus 21 inlets and outlets during 1979, and intensive data collection at 4 stream and 4 impoundment plus 9 inlet and outlet sites during 1980-84, showed that major ions, nutrients, and suspended-sediment concentrations and suspendedsediment discharge differed widely in unimpounded streams, but that maximum and median suspended-sediment concentrations were significantly reduced in impounded streams. Peak daily suspended-sediment discharges were reduced at impoundment outlets relative to the sediment discharge at their inlets. The impoundments were found to have little or no effect on stream temperature and concentrations of dissolved oxygen, dissolved solids, and major ions.
\nElevated concentrations of fecal bacteria were found in unimpounded streams throughout the study area and the impoundments did not substantially reduce the number of bacteria transported in the impounded streams. During summer, elevated concentrations of nitrate, ammonia, and phosphorus were present in all the impoundments. Levels of productivity were not significantly related to concentrations of total phosphorus in the euphotic zone. Real levels of productivity differed among the impoundments however, and seemed to be affected by the occurrence and duration of thermal stratification.
\nPeriods of summer stratification and accumulation of late winter snow on pool ice were frequently accompanied by near total depletion of dissolved oxygen. During summer stratification the concentration of ammonia increased with time in the lower part of the water column in some impoundments.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri904033","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers, U.S. Soil Conservation Service","usgsCitation":"Smith, C., Payne, G.A., and Tornes, L., 1990, Effects of impoundments on water quality of streams in the Coteau des Prairies: Upper Minnesota River basin: U.S. Geological Survey Water-Resources Investigations Report 90-4033, v, 67 p., https://doi.org/10.3133/wri904033.","productDescription":"v, 67 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":424445,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47314.htm","linkFileType":{"id":5,"text":"html"}},{"id":58604,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119195,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4033/report-thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Coteau des Prairies, Upper Minnesota River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -96.4168351830468,\n 44.3725159102313\n ],\n [\n -94.08390124893188,\n 43.74328462942049\n ],\n [\n -93.49425103823344,\n 44.47261188200261\n ],\n [\n -96.50438766963126,\n 45.98318805592024\n ],\n [\n -96.8237861277608,\n 45.58082116993637\n ],\n [\n -96.46250839082896,\n 45.352494618169715\n ],\n [\n -96.4168351830468,\n 44.3725159102313\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611ec8","contributors":{"authors":[{"text":"Smith, C.J.","contributorId":69141,"corporation":false,"usgs":true,"family":"Smith","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":202152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Payne, G. A.","contributorId":62190,"corporation":false,"usgs":true,"family":"Payne","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tornes, L. H.","contributorId":103675,"corporation":false,"usgs":true,"family":"Tornes","given":"L. H.","affiliations":[],"preferred":false,"id":202153,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18796,"text":"ofr90565 - 1990 - Nutrients, pesticides, surfactants, and trace metals in ground water from the Howe and Mud Lake areas upgradient from the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr90565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-565","title":"Nutrients, pesticides, surfactants, and trace metals in ground water from the Howe and Mud Lake areas upgradient from the Idaho National Engineering Laboratory, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr90565","usgsCitation":"Edwards, D., Bartholomay, R.C., and Bennett, C.M., 1990, Nutrients, pesticides, surfactants, and trace metals in ground water from the Howe and Mud Lake areas upgradient from the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Open-File Report 90-565, iv, 19 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90565.","productDescription":"iv, 19 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0565/report-thumb.jpg"},{"id":48165,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0565/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6966ac","contributors":{"authors":[{"text":"Edwards, D.D.","contributorId":52980,"corporation":false,"usgs":true,"family":"Edwards","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":179755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartholomay, R. C.","contributorId":66271,"corporation":false,"usgs":true,"family":"Bartholomay","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":179756,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, C. 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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrSD891","usgsCitation":"Burr, M., Benson, R., and Hansen, D.S., 1990, Water resources data, South Dakota, water year 1989: U.S. Geological Survey Water Data Report SD-89-1, ix, 383 p., https://doi.org/10.3133/wdrSD891.","productDescription":"ix, 383 p.","costCenters":[],"links":[{"id":380133,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1989/sd-89-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1989/sd-89-1/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faade","contributors":{"authors":[{"text":"Burr, M.J.","contributorId":34541,"corporation":false,"usgs":true,"family":"Burr","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":252202,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benson, R.D.","contributorId":23955,"corporation":false,"usgs":true,"family":"Benson","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":252201,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hansen, D. S.","contributorId":70003,"corporation":false,"usgs":true,"family":"Hansen","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":252203,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":54384,"text":"wdrAR891 - 1990 - Water resources data, Arkansas, water year 1989","interactions":[],"lastModifiedDate":"2020-10-01T22:40:03.831535","indexId":"wdrAR891","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-89-1","title":"Water resources data, Arkansas, water year 1989","docAbstract":"No abstract available.
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This report contains discharge records for 160 streamflow gaging stations, 12 partial-record or miscellaneous streamflow stations, and 5 crest-stage, partial-record streamflow stations; stage and contents records for 11 lakes and reservoirs; water-quality records for 38 streamflow stations, 8 ungaged stream-sites, and 159 wells; and water-level records for 55 observation wells. These data represent that part of the National Water-Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Nebraska.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f1084","contributors":{"authors":[{"text":"Boohar, J.A.","contributorId":24821,"corporation":false,"usgs":true,"family":"Boohar","given":"J.A.","affiliations":[],"preferred":false,"id":252802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoy, C.G.","contributorId":50958,"corporation":false,"usgs":true,"family":"Hoy","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":252804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, M. J.","contributorId":27840,"corporation":false,"usgs":true,"family":"Ellis","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":252803,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29897,"text":"wri894190 - 1990 - Preliminary evaluation of the effects of an abandoned oil refinery on chemical quality of water in the Arkansas River valley, Arkansas City, Kansas, 1985-86","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri894190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4190","title":"Preliminary evaluation of the effects of an abandoned oil refinery on chemical quality of water in the Arkansas River valley, Arkansas City, Kansas, 1985-86","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri894190","usgsCitation":"Spruill, T., 1990, Preliminary evaluation of the effects of an abandoned oil refinery on chemical quality of water in the Arkansas River valley, Arkansas City, Kansas, 1985-86: U.S. Geological Survey Water-Resources Investigations Report 89-4190, vi, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri894190.","productDescription":"vi, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159480,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4190/report-thumb.jpg"},{"id":58712,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4190/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58713,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4190/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c3d6","contributors":{"authors":[{"text":"Spruill, T.B.","contributorId":76747,"corporation":false,"usgs":true,"family":"Spruill","given":"T.B.","affiliations":[],"preferred":false,"id":202317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2553,"text":"wsp2366 - 1990 - A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming","interactions":[{"subject":{"id":15559,"text":"ofr88337 - 1989 - A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming","indexId":"ofr88337","publicationYear":"1989","noYear":false,"title":"A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":2553,"text":"wsp2366 - 1990 - A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming","indexId":"wsp2366","publicationYear":"1990","noYear":false,"title":"A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp2366","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"2366","title":"A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming","docAbstract":"A physically based point-infiltration model was developed for computing infiltration of rainfall into soils and the resulting runoff from small basins in Wyoming. The user describes a 'design storm' in terms of average rainfall intensity and storm duration. Information required to compute runoff for the design storm by using the model include (1) soil type and description, and (2) two infiltration parameters and a surface-retention storage parameter. Parameter values are tabulated in the report. Rainfall and runoff data for three ephemeral-stream basins that contain only one type of soil were used to develop the model. Two assumptions were necessary: antecedent soil moisture is some long-term average, and storm rainfall is uniform in both time and space. The infiltration and surface-retention storage parameters were determined for the soil of each basin. Observed rainstorm and runoff data were used to develop a separation curve, or incipient-runoff curve, which distinguishes between runoff and nonrunoff rainfall data. The position of this curve defines the infiltration and surface-retention storage parameters. \r\n\r\nA procedure for applying the model to basins that contain more than one type of soil was developed using data from 7 of the 10 study basins. For these multiple-soil basins, the incipient-runoff curve defines the infiltration and retention-storage parameters for the soil having the highest runoff potential. Parameters were defined by ranking the soils according to their relative permeabilities and optimizing the position of the incipient-runoff curve by using measured runoff as a control for the fit. Analyses of runoff from multiple-soil basins indicate that the effective contributing area of runoff is less than the drainage area of the basin. In this study, the effective drainage area ranged from 41.6 to 71.1 percent of the total drainage area. Information on effective drainage area is useful in evaluating drainage area as an independent variable in statistical analyses of hydrologic data, such as annual peak frequency distributions and sediment yield.A comparison was made of the sum of the simulated runoff and the sum of the measured runoff for all available records of runoff-producing storms in the 10 study basins. The sums of the simulated runoff ranged from 12.0 percent less than to 23.4 percent more than the sums of the measured runoff. A measure of the standard error of estimate was computed for each data set. These values ranged from 20 to 70 percent of the mean value of the measured runoff. \r\n\r\nRainfall-simulator infiltrometer tests were made in two small basins. The amount of water uptake measured by the test in Dugout Creek tributary basin averaged about three times greater than the amount of water uptake computed from rainfall and runoff data. Therefore, infiltrometer data were not used to determine infiltration rates for this study.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2366","usgsCitation":"Rankl, J.G., 1990, A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming: U.S. Geological Survey Water Supply Paper 2366, v, 29 p. :ill., maps ; 28 cm., https://doi.org/10.3133/wsp2366.","productDescription":"v, 29 p. :ill., maps ; 28 cm.","costCenters":[],"links":[{"id":138619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2366/report-thumb.jpg"},{"id":28801,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2366/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91fd","contributors":{"authors":[{"text":"Rankl, James G.","contributorId":93026,"corporation":false,"usgs":true,"family":"Rankl","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38596,"text":"pp1200US - 1990 - The National Gazetteer of the United States of America; United States concise 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp1200US","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1200","chapter":"US","title":"The National Gazetteer of the United States of America; United States concise 1990","language":"ENGLISH","doi":"10.3133/pp1200US","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, The National Gazetteer of the United States of America; United States concise 1990: U.S. Geological Survey Professional Paper 1200, 526 p., https://doi.org/10.3133/pp1200US.","productDescription":"526 p.","costCenters":[],"links":[{"id":119150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1200us/report-thumb.jpg"},{"id":65408,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1200us/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b19d","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":529868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41077,"text":"ofr90188 - 1990 - Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, September 1989","interactions":[],"lastModifiedDate":"2022-10-26T18:13:16.040466","indexId":"ofr90188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-188","title":"Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, September 1989","docAbstract":"No abstract available.
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