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       [\n              -80.5078125,\n              39.757879992021756\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688206","contributors":{"authors":[{"text":"Wall, Gary R. grwall@usgs.gov","contributorId":915,"corporation":false,"usgs":true,"family":"Wall","given":"Gary","email":"grwall@usgs.gov","middleInitial":"R.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, Patrick J. pjphilli@usgs.gov","contributorId":856,"corporation":false,"usgs":true,"family":"Phillips","given":"Patrick J.","email":"pjphilli@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":false,"id":153344,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34743,"text":"b2159 - 1997 - Proterozoic geology of the Granite Village area, Albany and Laramie counties, Wyoming, compared with that of the Sierra Madre and Medicine Bow mountains of southeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:43","indexId":"b2159","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2159","title":"Proterozoic geology of the Granite Village area, Albany and Laramie counties, Wyoming, compared with that of the Sierra Madre and Medicine Bow mountains of southeastern Wyoming","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b2159","usgsCitation":"Houston, R.S., and Marlatt, G., 1997, Proterozoic geology of the Granite Village area, Albany and Laramie counties, Wyoming, compared with that of the Sierra Madre and Medicine Bow mountains of southeastern Wyoming: U.S. Geological Survey Bulletin 2159, iv, 25 p. ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/b2159.","productDescription":"iv, 25 p. ill., maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":109830,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22432.htm","linkFileType":{"id":5,"text":"html"},"description":"22432"},{"id":166603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2159/report-thumb.jpg"},{"id":62609,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/2159/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62610,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2159/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656be8","contributors":{"authors":[{"text":"Houston, Robert Stroud","contributorId":73195,"corporation":false,"usgs":true,"family":"Houston","given":"Robert","email":"","middleInitial":"Stroud","affiliations":[],"preferred":false,"id":213502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marlatt, Gordon","contributorId":16485,"corporation":false,"usgs":true,"family":"Marlatt","given":"Gordon","email":"","affiliations":[],"preferred":false,"id":213501,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185299,"text":"70185299 - 1997 - A study of the temporal variability of atrazine in private well water. part ii: analysis of data","interactions":[],"lastModifiedDate":"2017-03-20T11:27:17","indexId":"70185299","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"A study of the temporal variability of atrazine in private well water. part ii: analysis of data","docAbstract":"<p><span>In 1988, the Iowa Department of Natural Resources, along withthe University of Iowa, conducted the Statewide Rural WellWater Survey, commonly known as SWRL. A total of 686private rural drinking water wells was selected by use of aprobability sample and tested for pesticides and nitrate. A subsetof these wells, the 10% repeat wells, were additionally sampledin October, 1990 and June, 1991. Starting in November, 1991,the University of Iowa, with sponsorship from the United StatesEnvironmental Protection Agency, revisited the 10% repeat wellsto begin a study of the temporal variability of atrazine and nitratein wells. Other wells, which had originally tested positive foratrazine in SWRL but were not in the 10% population, wereadded to the study population. Temporal sampling for a year-long period began in February of 1992 and concluded in Januaryof 1993. All wells were sampled monthly, a subset was sampledweekly, and a second subset was sampled for 14 day consecutiveperiods. Of the 67 wells in the 10% population tested monthly,7 (10.4%) tested positive for atrazine at least once during theyear, and 3 (4%) were positive each of the 12 months. Theaverage concentration in the 7 wells was 0.10 µg/L. Fornitrate, 15 (22%) wells in the 10% repeat population monthlysampling were above the Maximum Contaminant Level of 10 mg/L at least once. This paper, the second of two papers on thisstudy, describes the analysis of data from the survey. The firstpaper (Lorber et al., 1997) reviews the study design, theanalytical methodologies, and development of the data base.</span></p>","language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1023/A:1005704920640","usgsCitation":"Pinsky, P., Lorber, M., Johnson, K., Kross, B., Burmeister, L., Wilkins, A., and Hallberg, G., 1997, A study of the temporal variability of atrazine in private well water. part ii: analysis of data: Environmental Monitoring and Assessment, v. 47, no. 2, p. 197-221, https://doi.org/10.1023/A:1005704920640.","productDescription":"25 p. ","startPage":"197","endPage":"221","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337840,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d0ea1be4b0236b68f67379","contributors":{"authors":[{"text":"Pinsky, Paul","contributorId":189527,"corporation":false,"usgs":false,"family":"Pinsky","given":"Paul","email":"","affiliations":[],"preferred":false,"id":685072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorber, Matthew","contributorId":189528,"corporation":false,"usgs":false,"family":"Lorber","given":"Matthew","email":"","affiliations":[],"preferred":false,"id":685073,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Kent","contributorId":189529,"corporation":false,"usgs":false,"family":"Johnson","given":"Kent","email":"","affiliations":[],"preferred":false,"id":685074,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kross, Burton","contributorId":189530,"corporation":false,"usgs":false,"family":"Kross","given":"Burton","email":"","affiliations":[],"preferred":false,"id":685075,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burmeister, Leon","contributorId":189531,"corporation":false,"usgs":false,"family":"Burmeister","given":"Leon","email":"","affiliations":[],"preferred":false,"id":685076,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wilkins, Amina","contributorId":189532,"corporation":false,"usgs":false,"family":"Wilkins","given":"Amina","email":"","affiliations":[],"preferred":false,"id":685077,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hallberg, George","contributorId":16269,"corporation":false,"usgs":true,"family":"Hallberg","given":"George","affiliations":[],"preferred":false,"id":685078,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":26100,"text":"wri964258 - 1997 - Ground-water resources of Catron County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri964258","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"96-4258","title":"Ground-water resources of Catron County, New Mexico","docAbstract":"This report describes the occurrence, availability, and quality \r\nof ground-water and related surface-water resources in Catron \r\nCounty, the largest county in New Mexico. The county is located in \r\nthe Lower Colorado River Basin and the Rio Grande Basin, and the \r\nContinental Divide is the boundary between the two river basins.  \r\nIncreases in water used for mining activities (coal, mineral, and \r\ngeothermal), irrigated agriculture, reservoir construction, or \r\ndomestic purposes could affect the quantity or quality of ground-\r\nwater and surface-water resources in the county.\r\n\r\n     Parts of seven major drainage basins are within the two \r\nregional river basins in the county--Carrizo Wash, North Plains, \r\nRio Salado, San Agustin, Alamosa Creek, Gila, and San Francisco \r\nBasins. The San Francisco, Gila, and Tularosa Rivers typically \r\nflow perennially. During periods of low flow, most streamflow is \r\nderived from baseflow. The stream channels of the Rio Salado and \r\nCarrizo Wash Basins are commonly perennial in their upper reaches \r\nand ephemeral in their lower reaches. Largo Creek in the Carrizo \r\nWash Basin is perennial downstream from Quemado Lake and ephemeral \r\nin the lower reaches.\r\n\r\n     Aquifers in Catron County include Quaternary alluvium and \r\nbolson fill; Quaternary to Tertiary Gila Conglomerate; Tertiary \r\nBearwallow Mountain Andesite, Datil Group, and Baca Formation; \r\nCretaceous Mesaverde Group, Crevasse Canyon Formation, Gallup \r\nSandstone, Mancos Shale, and Dakota Sandstone; Triassic Chinle \r\nFormation; and undifferentiated rocks of Permian age. Water in the \r\naquifers in the county generally is unconfined; however, confined \r\nconditions may exist where the aquifers are overlain by other units \r\nof lower permeability.\r\n\r\n     Yields of ground water from the Quaternary alluvium in the \r\ncounty range from 1 to 375 gallons per minute. Yields of ground \r\nwater from the alluvium in the Carrizo Wash Basin are as much as \r\n250 gallons per minute for short time periods. North of the Plains \r\nof San Agustin, ground-water yields from the alluvium in the San \r\nAgustin Basin range from 1 to 10 gallons per minute.\r\n\r\n     Irrigation wells completed in the Quaternary bolson fill \r\nproduce as much as 975 gallons per minute immediately east of the \r\ncounty. Water from the bolson fill in the Plains of San Agustin has \r\nspecific-conductance values generally ranging from 180 to 3,300 \r\nmicrosiemens per centimeter at 25 degrees Celsius (microsiemens/cm). \r\n\r\n     Yields from the Gila Conglomerate generally range from 2 to 5 \r\ngallons per minute. Water samples from two springs from the Gila \r\nConglomerate have specific conductances of 289 and 381 microsiemens/cm. \r\n\r\n     The Tertiary Datil Group is present in the Carrizo Wash, San \r\nAgustin, San Francisco, and Gila Basins. The Datil Group commonly \r\nis unconfined, but may be confined at depth. Water levels of wells \r\ncompleted in this unit range from 60 to 1,260 feet below land \r\nsurface. Wells completed in the Datil Group typically yield 1 to \r\n15 gallons per minute. Specific conductance of water from the \r\nDatil Group ranges from 210 to 820 microsiemens/cm. The Tertiary Baca \r\nFormation in the Carrizo Wash Basin produces 5 to 20 gallons per \r\nminute in stock wells. Water from wells completed in the Baca \r\nFormation has specific-conductance values ranging from 312 to 752 \r\nmicrosiemens/cm.\r\n\r\n     Aquifers in Cretaceous rocks are present in the Carrizo Wash, \r\nNorth Plains, and Rio Salado Basins. The potential yield from wells \r\ncompleted in Cretaceous rocks in northwestern Catron County is from \r\n1 to 122 gallons per minute. Specific conductance of water from \r\nCretaceous rocks ranges from 210 microsiemens/cm in the Moreno Hill \r\nFormation to 4,490 microsiemens/cm in the Mancos Shale. Yields of ground \r\nwater from Cretaceous rocks in the Carrizo Wash Basin typically \r\nrange from 1 to 100 gallons per minute; in an artesian well, \r\nhowever, the yield in the main body of the Creta","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/wri964258","usgsCitation":"Basabilvazo, G., 1997, Ground-water resources of Catron County, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 96-4258, vii, 141 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri964258.","productDescription":"vii, 141 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4258/report-thumb.jpg"},{"id":54887,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4258/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d865","contributors":{"authors":[{"text":"Basabilvazo, G.T.","contributorId":72832,"corporation":false,"usgs":true,"family":"Basabilvazo","given":"G.T.","email":"","affiliations":[],"preferred":false,"id":195805,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23199,"text":"ofr9739 - 1997 - Construction, geologic log, and aquifer tests of the Puakukui Springs monitor well (State well 2-5626-01), Lihue, Kauai, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:07:58","indexId":"ofr9739","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"97-39","title":"Construction, geologic log, and aquifer tests of the Puakukui Springs monitor well (State well 2-5626-01), Lihue, Kauai, Hawaii","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr9739","issn":"0094-9140","usgsCitation":"Gingerich, S.B., and Izuka, S.K., 1997, Construction, geologic log, and aquifer tests of the Puakukui Springs monitor well (State well 2-5626-01), Lihue, Kauai, Hawaii: U.S. Geological Survey Open-File Report 97-39, iv, 18 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr9739.","productDescription":"iv, 18 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0039/report-thumb.jpg"},{"id":52518,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697ec9","contributors":{"authors":[{"text":"Gingerich, S. B.","contributorId":83958,"corporation":false,"usgs":true,"family":"Gingerich","given":"S.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":189625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Izuka, S. K.","contributorId":39818,"corporation":false,"usgs":true,"family":"Izuka","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":189624,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26582,"text":"wri974094 - 1997 - Geologic framework of the Edwards Aquifer and upper confining unit, and hydrogeologic characteristics of the Edwards Aquifer, south-central Uvalde County, Texas","interactions":[],"lastModifiedDate":"2016-08-17T16:07:27","indexId":"wri974094","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"97-4094","title":"Geologic framework of the Edwards Aquifer and upper confining unit, and hydrogeologic characteristics of the Edwards Aquifer, south-central Uvalde County, Texas","docAbstract":"<p>The stratigraphic units of the Edwards aquifer in south-central Uvalde County generally are porous and permeable. The stratigraphic units that compose the Edwards aquifer in south-central Uvalde County are the Devils River Formation in the Devils River trend; and the West Nueces, McKnight, and Salmon Peak Formations in the Maverick Basin. The Balcones fault zone is the principal structural feature in Uvalde County; however, the displacement along the fault zone is less in Uvalde County than in adjacent Medina and Bexar Counties to the east. The Uvalde Salient is a structural high in south-central Uvalde County, and consists of several closely connected crustal uplifts that bring Edwards aquifer strata to the surface generally forming prominent hills. The crustal uplifts forming this structural high are the remnants of intrusive and extrusive magnatic activity. Six primary faults&mdash;Cooks, Black Mountain, Blue Mountain, Uvalde, Agape, and Connor&mdash;cross the length of the study area from the southwest to the northeast juxtaposing the Lower Cretaceous Salmon Peak Formation at the surface in the northwestern part of the study area against Upper Cretaceous formations in the central part of the study area. In the study area, the porosity of the rocks in the Edwards aquifer is related to depositional or diagenetic elements along specific stratigraphic horizons (fabric selective) and to dissolution and structural elements that can occur in any lithostratigraphic horizon (not fabric selective). Permeability depends on the physical properties of the rock such as size, shape, distribution of pores, and fissuring and dissolution. The middle 185 feet of the lower part of the Devils River Formation, the upper part of the Devils River Formation, and the upper unit of the Salmon Peak Formation probably are the most porous and permeable stratigraphic zones of the Edwards aquifer in south-central Uvalde County.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri974094","collaboration":"In cooperation with the San Antonio Water System","usgsCitation":"Clark, A.K., and Small, T.A., 1997, Geologic framework of the Edwards Aquifer and upper confining unit, and hydrogeologic characteristics of the Edwards Aquifer, south-central Uvalde County, Texas: U.S. Geological Survey Water-Resources Investigations Report 97-4094, Document: iii, 11 p.; Plate: 24.5 x 20.5 inches, https://doi.org/10.3133/wri974094.","productDescription":"Document: iii, 11 p.; Plate: 24.5 x 20.5 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":124831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_97_4094.jpg"},{"id":1983,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri97-4094/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","county":"Uvalde County","otherGeospatial":"Edward Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.875,\n              29.375\n            ],\n            [\n              -99.5,\n              29.375\n            ],\n            [\n              -99.5,\n              29.25\n            ],\n            [\n              -99.5625,\n              29.25\n            ],\n            [\n              -99.633333,\n              29.158333\n            ],\n            [\n              -99.633333,\n              29.125\n            ],\n            [\n              -99.875,\n              29.125\n            ],\n            [\n              -99.875,\n              29.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88a1","contributors":{"authors":[{"text":"Clark, Allan K. 0000-0003-0099-1521 akclark@usgs.gov","orcid":"https://orcid.org/0000-0003-0099-1521","contributorId":1279,"corporation":false,"usgs":true,"family":"Clark","given":"Allan","email":"akclark@usgs.gov","middleInitial":"K.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":196657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Small, Ted A.","contributorId":77533,"corporation":false,"usgs":true,"family":"Small","given":"Ted","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196658,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26591,"text":"wri964282 - 1997 - Metal speciation in the Upper Arkansas River, Colorado, 1990-93","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri964282","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"96-4282","title":"Metal speciation in the Upper Arkansas River, Colorado, 1990-93","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBranch of Information Services [distributor],","doi":"10.3133/wri964282","usgsCitation":"Clark, M.L., and Lewis, M., 1997, Metal speciation in the Upper Arkansas River, Colorado, 1990-93: U.S. Geological Survey Water-Resources Investigations Report 96-4282, iv, 24 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri964282.","productDescription":"iv, 24 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4282/report-thumb.jpg"},{"id":55459,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4282/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db62729d","contributors":{"authors":[{"text":"Clark, M. L.","contributorId":19595,"corporation":false,"usgs":true,"family":"Clark","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, M.E.","contributorId":65504,"corporation":false,"usgs":true,"family":"Lewis","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":196670,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28635,"text":"wri974040 - 1997 - Assessment of the water resources of the Grand Ronde area, Oregon","interactions":[],"lastModifiedDate":"2019-05-16T08:33:34","indexId":"wri974040","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"97-4040","title":"Assessment of the water resources of the Grand Ronde area, Oregon","docAbstract":"Stream hydrographs show that throughout the Grand Ronde area most precipitation follows surface or shallow subsurface pathways to streams, resulting in rapid runoff and little natural water storage within the basin. Limited storage and low aquifer permeability restrict base flow to streams, and streamflows therefore decline rapidly once precipitation ceases. Shallow ground water and springs occur throughout the area, but because of the low permeability of aquifer materials, nearly all wells and springs have low yields. Water quality in streams, wells, and springs is generally good, but saline ground water has been reported on a number of drillers' logs for the study area and in several previous investigations of nearby areas. Further development of water resources in the Grand Ronde area is likely to be constrained by existing downstream water rights, the low permeability of geologic materials throughout the area, and possibly the intrusion of saline water. However, construction of facilities to store available water and thus compensate for low yields could provide a reliable, sustainable water supply for the Grand Ronde area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974040","collaboration":"Prepared in cooperation with the Confederated Tribes of the Grand Ronde Community of Oregon","usgsCitation":"McCarthy, K.A., Risley, J.C., Caldwell, R.R., and McFarland, W.D., 1997, Assessment of the water resources of the Grand Ronde area, Oregon: U.S. Geological Survey Water-Resources Investigations Report 97-4040, Report: v, 27 p.; 1 Plate: 33.33 x 37.16 inches, https://doi.org/10.3133/wri974040.","productDescription":"Report: v, 27 p.; 1 Plate: 33.33 x 37.16 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":120071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4040/report-thumb.jpg"},{"id":57473,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4040/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363940,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1997/4040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Grand Ronde area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.76,\n              44.9\n            ],\n            [\n              -123.48,\n              44.9\n            ],\n            [\n              -123.48,\n              45.25\n            ],\n            [\n              -123.76,\n              45.25\n            ],\n            [\n              -123.76,\n              44.9\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668017","contributors":{"authors":[{"text":"McCarthy, Kathleen A. mccarthy@usgs.gov","contributorId":1159,"corporation":false,"usgs":true,"family":"McCarthy","given":"Kathleen","email":"mccarthy@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":200153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Risley, John C. 0000-0002-8206-5443 jrisley@usgs.gov","orcid":"https://orcid.org/0000-0002-8206-5443","contributorId":2698,"corporation":false,"usgs":true,"family":"Risley","given":"John","email":"jrisley@usgs.gov","middleInitial":"C.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Caldwell, Rodney R. 0000-0002-2588-715X caldwell@usgs.gov","orcid":"https://orcid.org/0000-0002-2588-715X","contributorId":2577,"corporation":false,"usgs":true,"family":"Caldwell","given":"Rodney","email":"caldwell@usgs.gov","middleInitial":"R.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":200152,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McFarland, William D.","contributorId":18738,"corporation":false,"usgs":true,"family":"McFarland","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":200150,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":22645,"text":"ofr97141 - 1997 - Preliminary evaluation of the landslide potential in Capulin Canyon following the Dome fire, Bandelier National Monument, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:57","indexId":"ofr97141","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"97-141","title":"Preliminary evaluation of the landslide potential in Capulin Canyon following the Dome fire, Bandelier National Monument, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr97141","issn":"0094-9140","usgsCitation":"Cannon, S., and Ellis, W., 1997, Preliminary evaluation of the landslide potential in Capulin Canyon following the Dome fire, Bandelier National Monument, New Mexico: U.S. Geological Survey Open-File Report 97-141, 15 p. :ill. (some col.), map ;28 cm., https://doi.org/10.3133/ofr97141.","productDescription":"15 p. :ill. (some col.), map ;28 cm.","costCenters":[],"links":[{"id":155222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0141/report-thumb.jpg"},{"id":52114,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0141/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c397","contributors":{"authors":[{"text":"Cannon, S.H.","contributorId":38154,"corporation":false,"usgs":true,"family":"Cannon","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":188628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellis, W. L.","contributorId":40210,"corporation":false,"usgs":true,"family":"Ellis","given":"W. L.","affiliations":[],"preferred":false,"id":188629,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21868,"text":"ofr9746 - 1997 - Hydrogeologic facies characterization of an alluvial fan near Fresno, California, using geophysical techniques","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr9746","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"97-46","title":"Hydrogeologic facies characterization of an alluvial fan near Fresno, California, using geophysical techniques","docAbstract":"DBCP (1,2-dibromo-3-chloropropane) contamination in the sole source aquifer near Fresno, California, has significantly affected drinking-water supplies. Borehole and surface geophysical data were integrated with borehole textural data to characterize the Kings River alluvial fan sediments and to provide a framework for computer modeling of pesticide transport in ground water. Primary hydrogeologic facies units, such as gravel, coarse sand or gravel, fine sand, and silt and clay, were identified in cores collected from three borings located on a 4.6-kilometer transect of multilevel monitoring wells. Borehole geophysical logs collected from seven wells and surface geophysical surveys were used to extrapolate hydrogeologic facies to depths of about 82meters and to correlate the facies units with neighboring drilling sites. Thickness ranged from 0.3to 13 meters for sand and gravel units, and from 0.3 to 17 meters for silt and clay. The lateral extent of distinct silt and clay layers was mapped using shallow seismic reflection and ground-penetrating radar techniques. About 3.6 kilometers of seismic reflection data were collected; at least three distinct fine-grained layers were mapped. The depth of investigation of the seismic survey ranged from 34 to 107 meters below land surface, and vertical resolution was about 3.5 meters. The ground-penetrating radar survey covered 3.6kilometers and imaged a 1.5-meters thick, continuous fine-grained layer located at a depth of about 8 meters. Integrated results from the borehole sediment descriptions and geophysical surveys provided a detailed characterization over a larger areal extent than traditional hydrogeologic methods alone.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr9746","issn":"0566-8174","usgsCitation":"Burow, K.R., Weissmann, G., Miller, R., and Placzek, G., 1997, Hydrogeologic facies characterization of an alluvial fan near Fresno, California, using geophysical techniques: U.S. Geological Survey Open-File Report 97-46, iv, 15 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr9746.","productDescription":"iv, 15 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153029,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0046/report-thumb.jpg"},{"id":51359,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686340","contributors":{"authors":[{"text":"Burow, Karen R. 0000-0001-6006-6667 krburow@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-6667","contributorId":1504,"corporation":false,"usgs":true,"family":"Burow","given":"Karen","email":"krburow@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":186045,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weissmann, G.S.","contributorId":50927,"corporation":false,"usgs":true,"family":"Weissmann","given":"G.S.","affiliations":[],"preferred":false,"id":186046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, R. D.","contributorId":92693,"corporation":false,"usgs":true,"family":"Miller","given":"R. D.","affiliations":[],"preferred":false,"id":186048,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Placzek, Gary","contributorId":58295,"corporation":false,"usgs":true,"family":"Placzek","given":"Gary","email":"","affiliations":[],"preferred":false,"id":186047,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":35490,"text":"b2094A - 1997 - Regional diagenetic patterns in the St. Peter Sandstone; implications for brine migration in the Illinois Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:09:47","indexId":"b2094A","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2094","chapter":"A","title":"Regional diagenetic patterns in the St. Peter Sandstone; implications for brine migration in the Illinois Basin","docAbstract":"Diagenetic minerals and alteration patterns in the\r\nOrdovician St. Peter Sandstone, Illinois Basin, record varied\r\nhydrologic and chemical conditions during the basin?s long\r\nand complex geologic history. Major diagenetic events modifying\r\nthe St. Peter Sandstone include (1) mechanical compaction,\r\n(2) early K-feldspar overgrowth and dolospar\r\nprecipitation, (3) burial quartz, dolospar, anhydrite, and calcite\r\ncementation, and (4) carbonate-cement and K-feldspar\r\ngrain dissolution. Radiometric age dates of authigenic\r\nK-feldspar and illite in combination with the reconstructed\r\nburial history of the St. Peter reveal that early-diagenetic\r\nK-feldspar and dolospar precipitated at shallow to moderate\r\ndepths in the Devonian, whereas late-diagenetic quartz,\r\ndolospar, anhydrite, and calcite formed during deep burial in\r\nthe Late Pennsylvanian to Early Permian. Stable-isotope\r\ngeochemistry and fluid-inclusion paleothermometry suggest\r\nthat burial cements precipitated from saline fluids over a\r\nwide temperature range. In the southern part of the basin,\r\nburial cements preserve a record of diagenetic effects that\r\nwere in part controlled by fractures and hydrothermal-fluid\r\ncirculation. Baroque dolospar cementation is the most significant\r\nof these effects.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b2094A","usgsCitation":"Pitman, J.K., Goldhaber, M.B., and Spoetl, C., 1997, Regional diagenetic patterns in the St. Peter Sandstone; implications for brine migration in the Illinois Basin: U.S. Geological Survey Bulletin 2094, iii, p. A1-A17, ill., maps ;28 cm., https://doi.org/10.3133/b2094A.","productDescription":"iii, p. A1-A17, ill., maps ;28 cm.","costCenters":[],"links":[{"id":165406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3413,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2094a/b2094a.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c5f5","contributors":{"authors":[{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":214734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":214735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spoetl, Christoph","contributorId":18043,"corporation":false,"usgs":true,"family":"Spoetl","given":"Christoph","email":"","affiliations":[],"preferred":false,"id":214736,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}