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,{"id":65516,"text":"i2249 - 1992 - Controlled photomosaic of the MTM 00112 Quadrangle, Pavonis Mons region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2249","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 00112 Quadrangle, Pavonis Mons region of Mars","language":"ENGLISH","doi":"10.3133/i2249","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Controlled photomosaic of the MTM 00112 Quadrangle, Pavonis Mons region of Mars: U.S. Geological Survey IMAP 2249, 1 remote-sensing image ;61 x 62 cm., on sheet 97 x 68 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2249.","productDescription":"1 remote-sensing image ;61 x 62 cm., on sheet 97 x 68 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100973,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2249/plate-1.pdf","size":"17725","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50200","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115,-2.5 ], [ -115,2.5 ], [ -110,2.5 ], [ -110,-2.5 ], [ -115,-2.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688ae0","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":533903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30211,"text":"wri914181 - 1992 - Effects of effluent spray irrigation and sludge disposal on ground water in a karst region, northwest Pinellas County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri914181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4181","title":"Effects of effluent spray irrigation and sludge disposal on ground water in a karst region, northwest Pinellas County, Florida","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914181","usgsCitation":"Trommer, J., 1992, Effects of effluent spray irrigation and sludge disposal on ground water in a karst region, northwest Pinellas County, Florida: U.S. Geological Survey Water-Resources Investigations Report 91-4181, v, 32 p. :ill. ;28 cm., https://doi.org/10.3133/wri914181.","productDescription":"v, 32 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4181/report-thumb.jpg"},{"id":58999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4181/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615cc1","contributors":{"authors":[{"text":"Trommer, J.T.","contributorId":28248,"corporation":false,"usgs":true,"family":"Trommer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":202864,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65517,"text":"i2248 - 1992 - Controlled photomosaic of the MTM 00117 Quadrangle, Pavonis Mons region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2248","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 00117 Quadrangle, Pavonis Mons region of Mars","language":"ENGLISH","doi":"10.3133/i2248","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Controlled photomosaic of the MTM 00117 Quadrangle, Pavonis Mons region of Mars: U.S. Geological Survey IMAP 2248, 1 remote-sensing image ;61 x 62 cm., on sheet 97 x 68 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2248.","productDescription":"1 remote-sensing image ;61 x 62 cm., on sheet 97 x 68 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100974,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2248/plate-1.pdf","size":"18056","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,-2.5 ], [ -120,2.5 ], [ -115,2.5 ], [ -115,-2.5 ], [ -120,-2.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b7f","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":533904,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65519,"text":"i2251 - 1992 - Controlled photomosaic of the MTM 05112 Quadrangle, Pavonis Mons region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2251","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2251","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 05112 Quadrangle, Pavonis Mons region of Mars","language":"ENGLISH","doi":"10.3133/i2251","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Controlled photomosaic of the MTM 05112 Quadrangle, Pavonis Mons region of Mars: U.S. Geological Survey IMAP 2251, 1 remote-sensing image ;61 x 61 cm., on sheet 96 x 69 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2251.","productDescription":"1 remote-sensing image ;61 x 61 cm., on sheet 96 x 69 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100976,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2251/plate-1.pdf","size":"14429","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 110,2.5 ], [ 110,7.5 ], [ 115,7.5 ], [ 115,2.5 ], [ 110,2.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b93","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":533906,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38443,"text":"pp1405A - 1992 - Summary of ground-water hydrology of the Cambrian-Ordovician aquifer system in the northern Midwest, United States","interactions":[],"lastModifiedDate":"2021-08-27T19:52:44.287101","indexId":"pp1405A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"1405","chapter":"A","title":"Summary of ground-water hydrology of the Cambrian-Ordovician aquifer system in the northern Midwest, United States","docAbstract":"<p>The Cambrian-Ordovician aquifer system contains very productive aquifers throughout an area of about 161,000 square miles in the northern Midwest. The aquifer system is used extensively for industrial and rural water supplies and is the primary source of water for many municipalities in most of its area of occurrence, except in Indiana, central and southern Illinois, and western Iowa, where the aquifer system contains saline water. About 680 million gallons per day was withdrawn from drilled wells in the aquifer system in 1980.</p>\n<p>Rocks of Cambrian and Ordovician age, mainly marine sandstones and carbonate rocks, constitute most of the bedrock and subcrop beneath glacial drift in southeastern Minnesota, northeastern Iowa, Wisconsin, northern Illinois, and extreme northwestern Indiana. These strata dip generally to the south and east off the Transcontinental arch in Minnesota and the Wisconsin arch, which are structurally high areas of the Precambrian basement, into the structural lows of the Forest City basin of southwestern Iowa, the Illinois basin, and the Michigan basin.</p>\n<p>The Cambrian and Ordovician rocks are buried by younger rocks in the remainder of Iowa, Illinois, and Indiana and in most of northern Missouri. Silurian and Devonian carbonate rocks immediately overlie the Cambrian and Ordovician rocks in those areas and are termed the \"Silurian-Devonian aquifer\" in this study. The balance of the Devonian rocks and the overlying Mississippian and Pennsylvanian rocks generally are fine-grained sediment or dense carbonate rocks and collectively are considered to be a regional confining unit. Most of the area is covered by a veneer of glacial drift, which, along with Cretaceous sandstone in northwestern Iowa, is treated as a regional water-table aquifer.</p>\n<p>The Cambrian-Ordovician aquifer system is composed of six hydrogeologic units, which are, in descending order, the Maquoketa confining unit, St. Peter-Prairie du Chien-Jordan aquifer, St. Lawrence- Franconia confining unit, Ironton-Galesville aquifer, Eau Claire confining unit, and Mount Simon aquifer. The uppermost confining unit is the least permeable; it consists primarily of the Maquoketa Shale but includes the dense carbonate rocks of the Galena Dolomite and the Decorah, Platteville, and Glenwood Formations where they are overlain by the Maquoketa Shale. The presence of the Maquoketa in Iowa, eastern Wisconsin, northeastern Illinois, and Indiana effectively confines the entire aquifer system below.</p>\n<p>The aquifer system is a leaky-artesian system in which movement of ground water is controlled partly by the internal confining units. In the northern outcrop area, unconfined conditions prevail in shallow parts of the aquifer system and where the system is thin. Much of the recharge in upland areas discharges to streams through local flow systems, which are no more than a few miles in length. The remainder of the recharge moves slowly downward to deeper formations and downgradient to form or join the regional flow system.</p>\n<p>Computer simulations of regional ground-water flow improve understanding of the regional character of the Cambrian-Ordovician aquifer system. Ground-water flow in the confined part of the aquifer system is mainly horizontal, away from the structural highs in the north, toward the structural basins in the south and east. The rate of ground-water movement is very slow, and the flux along flow paths into the basins decreases because of a progressive loss of head and small but widespread upward leakage. Saline water in the basins restricts movement of freshwater into the deeper parts of the basins, thereby forcing flow upward through confining units. Principal regional discharge areas are the Mississippi and Missouri Rivers, the Illinois and Michigan structural basins, and Lake Michigan. However, the lake is not in direct hydraulic connection with the Cambrian-Ordovician aquifer system and receives flow primarily from the Silurian-Devonian aquifer, which it directly overlies. The longest regional flow paths originate in recharge areas in northwestern Iowa and extend southeastward as much as 400 miles toward the Illinois basin.</p>\n<p>Simulated predevelopment recharge and discharge for the Cambrian- Ordovician aquifer system balance at 351 million gallons per day.</p>\n<p>Development of the aquifer system began in various parts of the northern Midwest in the 1860's and 1870's with the drilling of deep, generally flowing artesian wells near Lake Michigan in eastern Wisconsin and northeastern Illinois and along the valleys of the Mississippi River and its tributaries. Initial heads of 186 and 130 feet above Lake Michigan at Milwaukee and Chicago, respectively, have been reported. Large-scale pumping has produced cones of depression in these two areas, with respective head declines of as much as 375 and 900 feet. Other major pumping centers generally have had much smaller declines. The largest withdrawals from the aquifer system were about 180 million gallons per day in each of the major metropolitan areas of Chicago and Minneapolis-St. Paul (Twin Cities). However, the total decline in head in the St. Peter-Prairie du Chien-Jordan aquifer in the Twin Cities by 1980 was only 90 feet because the aquifer is unconfined. Most of the eastern two-thirds of Iowa, where the aquifer system is tightly confined, is characterized by more than 50 feet of head decline, with 200 feet or more at Mason City and the Quad Cities. Pumpage from the Cambrian-Ordovician aquifer system throughout the study area averaged 683 million gallons per day for the period 1976-80. Results of a transient-model simulation show that recharge increased over predevelopment recharge by 447 million gallons per day. Natural discharge decreased by 99 million gallons per day, and 137 million gallons per day was released from aquifer storage. Mineralization of ground water in the aquifer system increases from slightly mineralized calcium magnesium bicarbonate water in the northern recharge areas, through more mineralized, mixed water types with increased sodium and sulfate, to highly mineralized sodium chloride brines in the deeper parts of the structural basins.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Regional aquifer-system analysis - northern Midwest","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1405A","usgsCitation":"Young, H.L., 1992, Summary of ground-water hydrology of the Cambrian-Ordovician aquifer system in the northern Midwest, United States: U.S. Geological Survey Professional Paper 1405, 55 p., https://doi.org/10.3133/pp1405A.","productDescription":"55 p.","numberOfPages":"67","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":388615,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4851.htm"},{"id":119767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1405a/report-thumb.jpg"},{"id":64918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1405a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa, Illinois, Indiana, Michigan, Minnesota, Missouri, Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.044921875,\n              45.9511496866914\n            ],\n            [\n              -88.330078125,\n              46.042735653846506\n            ],\n            [\n              -90.3955078125,\n              46.31658418182218\n            ],\n            [\n              -92.59277343749999,\n              46.34692761055676\n            ],\n            [\n              -93.603515625,\n              46.13417004624326\n            ],\n            [\n              -94.7021484375,\n              45.24395342262324\n            ],\n            [\n              -95.8447265625,\n              43.644025847699496\n            ],\n            [\n              -96.6796875,\n              42.553080288955826\n            ],\n            [\n              -96.7236328125,\n              41.83682786072714\n            ],\n            [\n              -96.328125,\n              40.78054143186031\n            ],\n            [\n              -95.2734375,\n              39.16414104768742\n            ],\n            [\n              -94.8779296875,\n              38.37611542403604\n            ],\n            [\n              -93.8232421875,\n              37.996162679728116\n            ],\n            [\n              -90.7470703125,\n              37.54457732085582\n            ],\n            [\n              -89.69238281249999,\n              37.71859032558816\n            ],\n            [\n              -88.1982421875,\n              38.03078569382294\n            ],\n            [\n              -87.01171875,\n              38.685509760012\n            ],\n            [\n              -85.78125,\n              39.16414104768742\n            ],\n            [\n              -86.4404296875,\n              42.45588764197166\n            ],\n            [\n              -86.8798828125,\n              43.29320031385282\n            ],\n            [\n              -87.099609375,\n              44.15068115978091\n            ],\n            [\n              -86.044921875,\n              45.9511496866914\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991cc","contributors":{"authors":[{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":219832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30035,"text":"wri914144 - 1992 - Effects of a wetland on quality of Natty Pond Brook, Massachusetts, 1985-86","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri914144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4144","title":"Effects of a wetland on quality of Natty Pond Brook, Massachusetts, 1985-86","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri914144","usgsCitation":"Suurballe, N., 1992, Effects of a wetland on quality of Natty Pond Brook, Massachusetts, 1985-86: U.S. Geological Survey Water-Resources Investigations Report 91-4144, v, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914144.","productDescription":"v, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4144/report-thumb.jpg"},{"id":58838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4144/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624d1e","contributors":{"authors":[{"text":"Suurballe, N.C.","contributorId":37779,"corporation":false,"usgs":true,"family":"Suurballe","given":"N.C.","email":"","affiliations":[],"preferred":false,"id":202571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42670,"text":"ofr92257 - 1992 - Regional stratigraphic cross sections of upper Cretaceous rocks across the San Juan Basin, northwestern New Mexico and southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr92257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"92-257","title":"Regional stratigraphic cross sections of upper Cretaceous rocks across the San Juan Basin, northwestern New Mexico and southwestern Colorado","language":"ENGLISH","doi":"10.3133/ofr92257","usgsCitation":"Molenaar, C.M., and Baird, J.K., 1992, Regional stratigraphic cross sections of upper Cretaceous rocks across the San Juan Basin, northwestern New Mexico and southwestern Colorado: U.S. Geological Survey Open-File Report 92-257, 3 sections :photocopy ;sheets 67 x 88 cm. and smaller., https://doi.org/10.3133/ofr92257.","productDescription":"3 sections :photocopy ;sheets 67 x 88 cm. and smaller.","costCenters":[],"links":[{"id":175560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80461,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0257/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80462,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0257/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80463,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0257/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4b7","contributors":{"authors":[{"text":"Molenaar, C. M.","contributorId":77904,"corporation":false,"usgs":false,"family":"Molenaar","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":226913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baird, J. K.","contributorId":27873,"corporation":false,"usgs":true,"family":"Baird","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":226912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66269,"text":"i2273 - 1992 - Geologic map of the Harris Quadrangle and parts of the Waverly SE, Williamsburg, and Waverly quadrangles, Anderson County, Kansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:19","indexId":"i2273","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2273","subseriesTitle":"NONE","title":"Geologic map of the Harris Quadrangle and parts of the Waverly SE, Williamsburg, and Waverly quadrangles, Anderson County, Kansas","language":"ENGLISH","doi":"10.3133/i2273","isbn":"0607794402","usgsCitation":"Johnson, W., 1992, Geologic map of the Harris Quadrangle and parts of the Waverly SE, Williamsburg, and Waverly quadrangles, Anderson County, Kansas: U.S. Geological Survey IMAP 2273, 1 map :col. ;65 x 52 cm., on sheet 81 x 81 cm., folded in envelope 31 x 24 cm., https://doi.org/10.3133/i2273.","productDescription":"1 map :col. ;65 x 52 cm., on sheet 81 x 81 cm., folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":107357,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10207.htm","linkFileType":{"id":5,"text":"html"},"description":"10207"},{"id":188487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.5,38.25 ], [ -95.5,38.38388888888889 ], [ -95.36749999999999,38.38388888888889 ], [ -95.36749999999999,38.25 ], [ -95.5,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980ee","contributors":{"authors":[{"text":"Johnson, W.D. Jr.","contributorId":33689,"corporation":false,"usgs":true,"family":"Johnson","given":"W.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":274274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29940,"text":"wri914025 - 1992 - Geohydrology and water quality of stratified-drift aquifers in the lower Merrimack and coastal river basins, southeastern New Hampshire","interactions":[],"lastModifiedDate":"2013-01-24T14:56:42","indexId":"wri914025","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4025","title":"Geohydrology and water quality of stratified-drift aquifers in the lower Merrimack and coastal river basins, southeastern New Hampshire","docAbstract":"Communities in the lower Merrimack River basin and coastal river basins of southeastern New Hampshire are experiencing increased demands for water because of a rapid increase in population. The population in 1987 was 225,495 and is expected to increase by 30 percent during the next decade. As of 1987, five towns used the stratified-drift aquifers for municipal supply and withdrew an estimated 6 million gallons per day. Four towns used the bedrock aquifer for municipal supply and withdrew an average of 1 .6 million gallons per day. Stratified-drift deposits cover 78 of the 327 square miles of the study area. These deposits are generally less than 10 square miles in areal extent, and their saturated thickness ranges front less than 20 feet to as much as 100 feet . Transinissivity exceeds 4,000 square feet per day in several locations. Stratified-drift aquifers in the eastern part are predominantly small ice-contact deposits surrounded by marine sediments or till of low hydraulic conductivity. Stratified-drift aquifers in the western part consist of ice-contact and proglacial deposits that are large in areal extent and are commonly in contact with surface-water bodies. Five stratified-drift aquifers, in the towns of Derry, Windham, Kingston, North Hampton, and Greenland, have the greatest potential to supply additional amounts of water. Potential yields and contributing areas of hypothetical supply wells were estimated for an aquifer in Windham near Cobbetts Pond and for an aquifer in Kingston along the Powwow River by use of a method analogous to superposition in conjunction with a numerical ground-waterflow model. The potential yield is estimated to be 0 .6 million gallons per day for the Windham-Cobbetts Pond aquifer and 4 .0 million gallons per day for the Kingston-Powwow River aquifer. Contributing recharge area for supply wells is estimated to be 1.6 square miles in the Windham-Cobbetts Pond aquifer and 4.9 square miles in the Kingston-Powwow River aquifer. Analyses of water samples from 30 wells indicate that the water quality in the basins studied is generally suitable for drinking and other domestic purposes. Concentrations of iron and manganese exceeded the U.S . Environmental Protection Agency's (USEPA) and the New Hampshire Water Supply Engineering Bureau's secondary maximum contaminant levels for drinking water in 20 samples. With one exception, concentrations of volatile organic compounds at all wells sampled met New Hampshire Water Supply and Engineering Bureau's drinking-water standards. At one well, trichloroethylene was detected at a concentration of 5.7 micrograms per liter. Ground-water contamination has been detected at several hazardous-waste sites in the study area. Currently, 5 sites are on the USEPA's National Priority List of superfund sites, 10 sites are Resource Conservation and Recovery Act of 1976 sites, and 1 site is a Department of Defense hazardous-waste site of stratigraphic layers is a product of a material's density and the velocity at which sound travels through that material . The reflected signals return to the hydrophones at the water surface and are then filtered, amplified, and displayed graphically on the chart recorder to allow interpretation of aquifer stratigraphy and bedrock depths. Lithologic data from nearby wells and test holes were used as control points to check the interpretation of the reflection profiles. Test drilling was done at 66 locations (pls . 1-3) to determine sediment grain size, stratigraphy, depth to water table, depth to bedrock, and ground water quality . A 6-inch-diameter, hollow-stem auger was used for test drilling . Split-spoon samples of subsurface materials collected at specific depths were used to evaluate the grain-size characteristics and identify the stratigraphic sequence of materials comprising the aquifers . Thirty-eight test holes cased with a 2-inch-diameter polyvinyl-chloride (PVC) pipe and slotted screens were used to make ground-water-level measurements and collect ground-water-quality samples. Surface-water-discharge measurements were made at 16 sites during low flow when the surface water is primarily ground-water discharge . These low-flow measurements indicate quantities of ground water potentially available from aquifers. Hydraulic conductivities of aquifer materials were estimated from grain-size-distribution data from 61 samples of stratified drift . Transmissivity was estimated from well logs by assigning hydraulic conductivity to specific well-log intervals, multiplying by the saturated thickness of the interval, and summing the results . Additional transmissivity values were obtained from an analysis of specific capacity and aquifer-test data. Long-term aquifer yields and contributing areas to hypothetical supply wells were estimated by application of a method that is analogous to super position and incorporates a ground-water-flow model developed by McDonald and Harbaugh (1988) . This method was applied to two aquifers judged to have the best potential for providing additional ground-water supplies. Samples of ground water from 26 test wells and 4 municipal wells were collected in March and August 1987 for analysis of common inorganic, organic, and volatile organic constituents. Methods for collecting and analyzing the samples are described by Fishman and Freidman (1989) . The water-quality results from the well samples were used to characterize background water quality in the stratified-drift aquifers.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Bow, NH","doi":"10.3133/wri914025","collaboration":"Prepared in cooperation with the New Hampshire Department of Environmental Services, Water Resources Division","usgsCitation":"Stekl, P.J., and Flanagan, S., 1992, Geohydrology and water quality of stratified-drift aquifers in the lower Merrimack and coastal river basins, southeastern New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 91-4025, Report: vii, 75, A-18 p.; 7 Plates: 42.02 x 53.15 inches or smaller, https://doi.org/10.3133/wri914025.","productDescription":"Report: vii, 75, A-18 p.; 7 Plates: 42.02 x 53.15 inches or smaller","numberOfPages":"101","costCenters":[{"id":637,"text":"Water Resources of New Hampshire and Vermont","active":false,"usgs":true}],"links":[{"id":2420,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri914025/","linkFileType":{"id":5,"text":"html"}},{"id":119450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_91_4025.jpg"},{"id":266398,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4025/plate-1.pdf"},{"id":266399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4025/plate-2.pdf"},{"id":266400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4025/plate-3.pdf"},{"id":266401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4025/plate-4.pdf"},{"id":266402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4025/plate-5.pdf"},{"id":266403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4025/plate-6.pdf"},{"id":266404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4025/plate-7.pdf"},{"id":266397,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4025/report.pdf"}],"country":"United States","state":"New Hampshire","otherGeospatial":"Merrimack River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.5,42.5 ], [ -71.5,43.25 ], [ -70.5,43.25 ], [ -70.5,42.5 ], [ -71.5,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b81","contributors":{"authors":[{"text":"Stekl, Peter J.","contributorId":63415,"corporation":false,"usgs":true,"family":"Stekl","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flanagan, Sarah M.","contributorId":8492,"corporation":false,"usgs":true,"family":"Flanagan","given":"Sarah M.","affiliations":[],"preferred":false,"id":202393,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66184,"text":"i2304 - 1992 - Geologic map of the MTM 90000 area, Planum Australe region of Mars","interactions":[],"lastModifiedDate":"2023-07-05T11:14:02.108453","indexId":"i2304","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2304","title":"Geologic map of the MTM 90000 area, Planum Australe region of Mars","docAbstract":"<p><span class=\"TextRun SCXW236379580 BCX8\" lang=\"EN-US\" xml:lang=\"EN-US\" data-contrast=\"auto\"><span class=\"NormalTextRun SCXW236379580 BCX8\">Published geologic maps of the south polar region of Mars, made using either </span><span class=\"NormalTextRun SCXW236379580 BCX8\">Mariner</span><span class=\"NormalTextRun SCXW236379580 BCX8\"> 9 (</span><span class=\"NormalTextRun SCXW236379580 BCX8\">Condit and </span><span class=\"SpellingError SCXW236379580 BCX8\">Soderbloom</span><span class=\"NormalTextRun SCXW236379580 BCX8\">, 1978) or Viking Orbiter (Tanaka and Scott, 1987) images, identified only layered deposits of </span><span class=\"NormalTextRun SCXW236379580 BCX8\">polar ice </span><span class=\"NormalTextRun SCXW236379580 BCX8\">within this map area. Layered deposits probably </span><span class=\"NormalTextRun SCXW236379580 BCX8\">underlie </span><span class=\"AdvancedProofingIssue SCXW236379580 BCX8\">all of</span><span class=\"NormalTextRun SCXW236379580 BCX8\"> the </span><span class=\"NormalTextRun SCXW236379580 BCX8\">other</span><span class=\"NormalTextRun SCXW236379580 BCX8\"> units shown in the map. The residual polar ice cap, partial frost cover, and two low-albedo units are also mapped </span><span class=\"NormalTextRun SCXW236379580 BCX8\">here. These </span><span class=\"NormalTextRun SCXW236379580 BCX8\">u</span><span class=\"NormalTextRun SCXW236379580 BCX8\">nits were first recognized and mapped by Herkenhoff and Murray (1990a) at 1:2,000,000 scale</span><span class=\"NormalTextRun SCXW236379580 BCX8\"> using a color mosaic of Viking Orbiter images. This mosaic and an additional Viking color mosaic were used to confirm the identification of the five mapped color/albedo units. The colors and albedos of these units were presented in table 1 and figure 1. Because the resolution of the color mosaics is not sufficient to map </span><span class=\"NormalTextRun SCXW236379580 BCX8\">these</span> <span class=\"NormalTextRun SCXW236379580 BCX8\">units in </span><span class=\"ContextualSpellingAndGrammarError SCXW236379580 BCX8\">details</span><span class=\"NormalTextRun SCXW236379580 BCX8\"> at 1:500,000 scale, contacts between them were recognized and mapped using higher resolution black and white Viking and Mariner 9 images</span><span class=\"NormalTextRun SCXW236379580 BCX8\">.</span></span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2304","usgsCitation":"Herkenhoff, K., and Murray, B.C., 1992, Geologic map of the MTM 90000 area, Planum Australe region of Mars: U.S. Geological Survey IMAP 2304, 1 Plate: 48.00 × 42.67 inches, https://doi.org/10.3133/i2304.","productDescription":"1 Plate: 48.00 × 42.67 inches","costCenters":[],"links":[{"id":438933,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9HDKTG2","text":"USGS data release","linkHelpText":"Geologic map of the MTM 90000 area, Planum Australe region of Mars"},{"id":188391,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101324,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2304/plate-1.pdf","size":"10906","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d32","contributors":{"authors":[{"text":"Herkenhoff, Ken","contributorId":51385,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"Ken","email":"","affiliations":[],"preferred":false,"id":274122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murray, B. C.","contributorId":49870,"corporation":false,"usgs":false,"family":"Murray","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":274121,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30126,"text":"wri924123 - 1992 - Data encapsulation using FORTRAN-77 modules; a first step toward object-oriented programming in water resources","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri924123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"92-4123","title":"Data encapsulation using FORTRAN-77 modules; a first step toward object-oriented programming in water resources","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924123","usgsCitation":"Thompson, D., DeLong, L.L., and Fulford, J., 1992, Data encapsulation using FORTRAN-77 modules; a first step toward object-oriented programming in water resources: U.S. Geological Survey Water-Resources Investigations Report 92-4123, iii, 67 p. :ill. ;28 cm., https://doi.org/10.3133/wri924123.","productDescription":"iii, 67 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4123/report-thumb.jpg"},{"id":58931,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c978","contributors":{"authors":[{"text":"Thompson, D.B.","contributorId":74418,"corporation":false,"usgs":true,"family":"Thompson","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":202726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeLong, L. L.","contributorId":44530,"corporation":false,"usgs":true,"family":"DeLong","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fulford, J.M.","contributorId":27473,"corporation":false,"usgs":true,"family":"Fulford","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":202724,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30208,"text":"wri914129 - 1992 - Quality of water from public-supply wells in Massachusetts, 1975-86","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"wri914129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4129","title":"Quality of water from public-supply wells in Massachusetts, 1975-86","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports [distributor],","doi":"10.3133/wri914129","usgsCitation":"Trombley, T.J., 1992, Quality of water from public-supply wells in Massachusetts, 1975-86: U.S. Geological Survey Water-Resources Investigations Report 91-4129, v, 63 p. :ill. ;28 cm., https://doi.org/10.3133/wri914129.","productDescription":"v, 63 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":160438,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4129/report-thumb.jpg"},{"id":58997,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6517ad","contributors":{"authors":[{"text":"Trombley, T. J.","contributorId":75161,"corporation":false,"usgs":true,"family":"Trombley","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30314,"text":"wri914104 - 1992 - Hydrogeology and ground-water quality near a hazardous-waste landfill near Pinewood, South Carolina","interactions":[],"lastModifiedDate":"2017-01-25T12:53:20","indexId":"wri914104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4104","title":"Hydrogeology and ground-water quality near a hazardous-waste landfill near Pinewood, South Carolina","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri914104","usgsCitation":"Vroblesky, D., 1992, Hydrogeology and ground-water quality near a hazardous-waste landfill near Pinewood, South Carolina: U.S. Geological Survey Water-Resources Investigations Report 91-4104, v, 87 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914104.","productDescription":"v, 87 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":59106,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4104/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4104/report-thumb.jpg"},{"id":59107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4104/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","city":"Pinewood","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.958251953125,\n              32.95797741405952\n            ],\n            [\n              -80.958251953125,\n              33.83848275599514\n            ],\n            [\n              -79.9310302734375,\n              33.83848275599514\n            ],\n            [\n              -79.9310302734375,\n              32.95797741405952\n            ],\n            [\n              -80.958251953125,\n              32.95797741405952\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627562","contributors":{"authors":[{"text":"Vroblesky, D.A.","contributorId":101691,"corporation":false,"usgs":true,"family":"Vroblesky","given":"D.A.","affiliations":[],"preferred":false,"id":203039,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25499,"text":"wri914159 - 1992 - Evapotranspiration measurements of native vegetation, Owens Valley, California, June 1986","interactions":[],"lastModifiedDate":"2018-10-25T19:14:04","indexId":"wri914159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4159","title":"Evapotranspiration measurements of native vegetation, Owens Valley, California, June 1986","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914159","usgsCitation":"Reginato, R.J., and Hollett, K., 1992, Evapotranspiration measurements of native vegetation, Owens Valley, California, June 1986: U.S. Geological Survey Water-Resources Investigations Report 91-4159, viii, 83 p. :ill. ;28 cm., https://doi.org/10.3133/wri914159.","productDescription":"viii, 83 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4159/report-thumb.jpg"},{"id":54218,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4159/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c18","contributors":{"editors":[{"text":"Wilson, D.H.","contributorId":72654,"corporation":false,"usgs":true,"family":"Wilson","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":749932,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Reginato, R. J.","contributorId":20082,"corporation":false,"usgs":false,"family":"Reginato","given":"R.","email":"","middleInitial":"J.","affiliations":[{"id":6622,"text":"US Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":193944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hollett, K.J.","contributorId":23570,"corporation":false,"usgs":true,"family":"Hollett","given":"K.J.","affiliations":[],"preferred":false,"id":193945,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21074,"text":"ofr9247 - 1992 - Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89","interactions":[{"subject":{"id":21074,"text":"ofr9247 - 1992 - Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89","indexId":"ofr9247","publicationYear":"1992","noYear":false,"title":"Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89"},"predicate":"SUPERSEDED_BY","object":{"id":2777,"text":"wsp2409 - 1995 - Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89","indexId":"wsp2409","publicationYear":"1995","noYear":false,"title":"Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89"},"id":1}],"supersededBy":{"id":2777,"text":"wsp2409 - 1995 - Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89","indexId":"wsp2409","publicationYear":"1995","noYear":false,"title":"Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89"},"lastModifiedDate":"2013-08-01T15:20:40","indexId":"ofr9247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"92-47","title":"Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89","language":"ENGLISH","publisher":"U.S. Geological Survey ;Books and Open-File Reports Section [distributor],","doi":"10.3133/ofr9247","usgsCitation":"Swancar, A., and Hutchinson, C.B., 1992, Chemical and isotopic composition and potential for contamination of water in the upper Floridan Aquifer, west-central Florida, 1986-89: U.S. Geological Survey Open-File Report 92-47, iv, 48 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr9247.","productDescription":"iv, 48 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":153878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0047/report-thumb.jpg"},{"id":275869,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0047/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e493d","contributors":{"authors":[{"text":"Swancar, Amy aswancar@usgs.gov","contributorId":450,"corporation":false,"usgs":true,"family":"Swancar","given":"Amy","email":"aswancar@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":183797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, C. B.","contributorId":94655,"corporation":false,"usgs":true,"family":"Hutchinson","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":183798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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