{"pageNumber":"1620","pageRowStart":"40475","pageSize":"25","recordCount":68937,"records":[{"id":21395,"text":"ofr94547 - 1995 - Analytical results from an environmental investigation of six sites on Kirtland Air Force Base, New Mexico, 1993-94","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr94547","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"94-547","title":"Analytical results from an environmental investigation of six sites on Kirtland Air Force Base, New Mexico, 1993-94","docAbstract":"The six sites investigated include silver recovery units; a buried caustic drain line; a neutralization pit; an evaporation/infiltration pond; the Manzano fire training area; and a waste oil underground storage tank. Environmental samples of soil, pond sediment, soil gas, and water and gas in floor drains were collected and analyzed. Field quality-control samples were also collected and analyzed in association with the environmental samples. The six sites were investigated because past or current activities could have resulted in contamination of soil, pond sediment, or water and sediment in drains.","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division, [New Mexico District] ;\r\nCan be purchased from U.S. Geological Survey, Earth Science Information Center, Open-file Reports Section,","doi":"10.3133/ofr94547","usgsCitation":"Wilcox, R., 1995, Analytical results from an environmental investigation of six sites on Kirtland Air Force Base, New Mexico, 1993-94: U.S. Geological Survey Open-File Report 94-547, iv, 55 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94547.","productDescription":"iv, 55 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0547/report-thumb.jpg"},{"id":50964,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0547/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9d1","contributors":{"authors":[{"text":"Wilcox, Ralph","contributorId":9679,"corporation":false,"usgs":true,"family":"Wilcox","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":184353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30104,"text":"wri944079 - 1995 - Hydrogeologic setting and ground-water quality of areas tributary to Lake Tahoe in Douglas County and Carson City, Nevada, through 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri944079","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"94-4079","title":"Hydrogeologic setting and ground-water quality of areas tributary to Lake Tahoe in Douglas County and Carson City, Nevada, through 1987","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/wri944079","usgsCitation":"Thodal, C.E., 1995, Hydrogeologic setting and ground-water quality of areas tributary to Lake Tahoe in Douglas County and Carson City, Nevada, through 1987: U.S. Geological Survey Water-Resources Investigations Report 94-4079, iv, 31 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944079.","productDescription":"iv, 31 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4079/report-thumb.jpg"},{"id":58921,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6278fa","contributors":{"authors":[{"text":"Thodal, C. E.","contributorId":8136,"corporation":false,"usgs":true,"family":"Thodal","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17997,"text":"ofr95107 - 1995 - Irrigated croplands, estimated pumpage, and water-level changes in Diamond Valley, Eureka and Elko counties, Nevada, through 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:07:20","indexId":"ofr95107","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"95-107","title":"Irrigated croplands, estimated pumpage, and water-level changes in Diamond Valley, Eureka and Elko counties, Nevada, through 1990","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95107","usgsCitation":"Arteaga, F.E., Smith, J.L., and Harrill, J.R., 1995, Irrigated croplands, estimated pumpage, and water-level changes in Diamond Valley, Eureka and Elko counties, Nevada, through 1990: U.S. Geological Survey Open-File Report 95-107, iv, 68 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr95107.","productDescription":"iv, 68 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":149918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0107/report-thumb.jpg"},{"id":19345,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0107/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47237,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66727d","contributors":{"authors":[{"text":"Arteaga, Freddy E.","contributorId":73601,"corporation":false,"usgs":true,"family":"Arteaga","given":"Freddy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":178351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, J. LaRue jlsmith@usgs.gov","contributorId":1863,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"jlsmith@usgs.gov","middleInitial":"LaRue","affiliations":[],"preferred":true,"id":178350,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harrill, James R.","contributorId":99533,"corporation":false,"usgs":true,"family":"Harrill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":178352,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17887,"text":"ofr95105 - 1995 - Water-resources activities, North Dakota District, fiscal year 1994-95","interactions":[],"lastModifiedDate":"2018-03-12T15:42:08","indexId":"ofr95105","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"95-105","title":"Water-resources activities, North Dakota District, fiscal year 1994-95","docAbstract":"<p>The mission of the U.S. Geological Survey, Water Resources Division, is to provide the hydrologic information and understanding needed for the optimum utilization and management of the Nation's water resources for the overall benefit of the people of the United States. This report describes water-resources activities of the Water Resources Division in North Dakota in fiscal year 1994. Information on each project includes objectives, approach, progress, plans for fiscal year 1995, and completed and planned report products.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95105","usgsCitation":"1995, Water-resources activities, North Dakota District, fiscal year 1994-95: U.S. Geological Survey Open-File Report 95-105, vi, 55 p., https://doi.org/10.3133/ofr95105.","productDescription":"vi, 55 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":47126,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0105/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150602,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0105/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ada7","contributors":{"compilers":[{"text":"Martin, Cathy R.","contributorId":87951,"corporation":false,"usgs":true,"family":"Martin","given":"Cathy R.","affiliations":[],"preferred":false,"id":730817,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":70205368,"text":"70205368 - 1995 - Wind shear stress measurements in a coastal marsh during Hurricane Andrew","interactions":[],"lastModifiedDate":"2019-09-17T08:31:34","indexId":"70205368","displayToPublicDate":"1995-06-30T11:15:51","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Wind shear stress measurements in a coastal marsh during Hurricane Andrew","docAbstract":"<p><span>Hurricane Andrew produced changes to the Louisiana wetlands not normally observed after lesser, more common storms. For example, the &lt;25 m/s wind speeds generated by cold fronts and winter storms, and any accompanying storm surge, do not cause substantial, wide-spread alteration of marsh vegetation. During Hurricane Andrew, however, the wind, the wind-driven storm surge, or both produced severe, wide-spread wetland alteration, especially in areas that primarily consisted of densely vegetated floating mats. In a few hours, vegetated brackish marsh was severely torn and large areas were converted to open water, a process that takes decades when driven by geologic subsidence, human intervention, and lesser storms. During the passage of Hurricane Andrew, wind measurements were taken inside an impoundment within a brackish part of Louisiana's coastal wetlands system. At its closest point, the site lay 50 km to the right of the north-trending storm track, placing it in or near the zone of maximum wind (the eye wall). As the hurricane approached, the wind blew from the north; after it passed, the wind direction swung around to the southeast. Several hours after the eye passed, the southeasterly wind drove a 1.5-m storm surge through the area, causing the collapse of the meteorology tower. Wind shear stress calculations, based on data from two vertically stacked sensors, showed a direct correlation between wind shear stress and wind speed. The greatest increase in wind shear stress occurred when wind speed exceeded 20 m/s. Overall, wind shear stress increased more than three orders of magnitude — from approximately 0.01 N/m² at a wind speed of 6 m/s through 1 N/m² at 20 m/s to 18 N/m² at the maximum sustained speed of 43 m/s. Drag-coefficient calculations show that the open-ocean CD formulations, such as the popular WAMDI model, cannot be employed for wetland use because it overestimates CD for velocities less than approximately 20 m/s and underestimates it for higher velocities.</span></p>","language":"English","publisher":"Coastal Education and Research Foundation Inc","usgsCitation":"Dingler, J.R., Hsu, S., and Foote, A.L., 1995, Wind shear stress measurements in a coastal marsh during Hurricane Andrew: Journal of Coastal Research, p. 295-305.","productDescription":"11 p.","startPage":"295","endPage":"305","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":367434,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":367447,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/25736016"}],"country":"United States","state":"Louisiana","otherGeospatial":"Jug Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.0081672668457,\n              29.34582065193874\n            ],\n            [\n              -90.90568542480469,\n              29.34582065193874\n            ],\n            [\n              -90.90568542480469,\n              29.397131972809856\n            ],\n            [\n              -91.0081672668457,\n              29.397131972809856\n            ],\n            [\n              -91.0081672668457,\n              29.34582065193874\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dingler, J. R.","contributorId":79043,"corporation":false,"usgs":true,"family":"Dingler","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":770951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hsu, S.A.","contributorId":94161,"corporation":false,"usgs":true,"family":"Hsu","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":770952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foote, A. Lee","contributorId":216145,"corporation":false,"usgs":false,"family":"Foote","given":"A.","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":770953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70201973,"text":"70201973 - 1995 - Structural impact of hurricane Andrew on the forested wetlands of the Atchaflaya Basin in South Louisiana","interactions":[],"lastModifiedDate":"2019-02-05T09:40:54","indexId":"70201973","displayToPublicDate":"1995-06-22T09:23:08","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Structural impact of hurricane Andrew on the forested wetlands of the Atchaflaya Basin in South Louisiana","docAbstract":"<p>On August 26, 1992, Hurricane Andrew hit the Louisiana coast and traversed a large portion of the lower Atchafalaya Basin, bounding the largest remaining tract of cypress-tupelo and bottomland hardwood swamp in the United States. Permanent field sites were established following the hurricane to assess the extent of forest damage and to monitor the rate and process of forest recovery. Bottomland hardwood forests had significantly greater damage and mortality than did cypress-tupelo communities. Canopy trees suffered the greatest direct damage, particularly in sites within the storm's eyewall and right quadrant. The type and extent of damage (windthrow, branch loss, and defoliation) generally decreased as distance from the storm path increased. Azimuths of downed trees were strongly correlated with predicted wind vectors derived from a hurricane simulation model of Andrew. Species differences were readily apparent, indicating a high degree of tolerance to windthrow by baldcypress and water tupelo, and intolerance by many common hardwood species. Bottomland hardwood forests are particularly susceptible to catastrophic disturbance by hurricanes such as Andrew, which have significant impact on forest structure and dynamics. </p>","language":"English","publisher":"Coastal Education & Research Foundation, Inc.","publisherLocation":"Fort Lauderdale, Florida","usgsCitation":"Doyle, T.W., Keeland, B.D., Gorham, L.E., and Johnson, D.J., 1995, Structural impact of hurricane Andrew on the forested wetlands of the Atchaflaya Basin in South Louisiana: Journal of Coastal Research, no. Special Issue 21, p. 354-364.","productDescription":"11 p.","startPage":"354","endPage":"364","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":360951,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":361005,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/25736020?seq=1#metadata_info_tab_contents"}],"country":"United States","state":"Louisiana","otherGeospatial":"Atchafalaya Basin","issue":"Special Issue 21","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Doyle, Thomas W. 0000-0001-5754-0671 doylet@usgs.gov","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":703,"corporation":false,"usgs":true,"family":"Doyle","given":"Thomas","email":"doylet@usgs.gov","middleInitial":"W.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":756388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keeland, Bobby D.","contributorId":103506,"corporation":false,"usgs":true,"family":"Keeland","given":"Bobby","email":"","middleInitial":"D.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":756389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gorham, Lance E.","contributorId":212704,"corporation":false,"usgs":false,"family":"Gorham","given":"Lance","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":756390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Darrin J.","contributorId":212705,"corporation":false,"usgs":false,"family":"Johnson","given":"Darrin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":756391,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25140,"text":"25140 - 1995 - Cartographic catalog (CC) on CD-ROM","interactions":[],"lastModifiedDate":"2014-07-14T13:17:04","indexId":"25140","displayToPublicDate":"1995-06-01T13:16:21","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Cartographic catalog (CC) on CD-ROM","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/25140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Cartographic catalog (CC) on CD-ROM, computer laser optical discs, https://doi.org/10.3133/25140.","productDescription":"computer laser optical discs","costCenters":[],"links":[{"id":289916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fbf7e4b0b58d96eeb55f","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":529181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65583,"text":"i2418 - 1995 - Controlled photomosaic of the MTM 40002 Quadrangle, Acidalia Planitia region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2418","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2418","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 40002 Quadrangle, Acidalia Planitia region of Mars","language":"ENGLISH","doi":"10.3133/i2418","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 40002 Quadrangle, Acidalia Planitia region of Mars: U.S. Geological Survey IMAP 2418, 1 remote-sensing image ;62 x 48 cm., on sheet 97 x 57 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2418.","productDescription":"1 remote-sensing image ;62 x 48 cm., on sheet 97 x 57 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101034,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2418/plate-1.pdf","size":"6521","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 0,37.5 ], [ 0,42.5 ], [ 5,42.5 ], [ 5,37.5 ], [ 0,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6882c5","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":533970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18836,"text":"ofr9543 - 1995 - Impact of the lower Alamosa River water on alfalfa, southwestern San Luis Valley, Colorado: 1994 follow-up study","interactions":[],"lastModifiedDate":"2019-12-07T11:30:31","indexId":"ofr9543","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"95-43","title":"Impact of the lower Alamosa River water on alfalfa, southwestern San Luis Valley, Colorado: 1994 follow-up study","docAbstract":"<p>No abstract available.</p>","language":"English ","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr9543","usgsCitation":"Erdman, J.A., and Smith, K.S., 1995, Impact of the lower Alamosa River water on alfalfa, 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,{"id":18653,"text":"ofr9549 - 1995 - Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr9549","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"95-49","title":"Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9549","usgsCitation":"Desborough, G.A., 1995, Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado: U.S. Geological Survey Open-File Report 95-49, i, 10 p. ill. ;28 cm., https://doi.org/10.3133/ofr9549.","productDescription":"i, 10 p. ill. ;28 cm.","costCenters":[],"links":[{"id":151723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0049/report-thumb.jpg"},{"id":47990,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3552","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65524,"text":"i2425 - 1995 - Controlled photomosaic of the MTM 05142 Quadrangle, Gordii Dorsum region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2425","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2425","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 05142 Quadrangle, Gordii Dorsum region of Mars","language":"ENGLISH","doi":"10.3133/i2425","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 05142 Quadrangle, Gordii Dorsum region of Mars: U.S. Geological Survey IMAP 2425, 1 remote-sensing image ;61 x 62 cm., on sheet 96 x 69 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2425.","productDescription":"1 remote-sensing image ;61 x 62 cm., on sheet 96 x 69 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100981,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2425/plate-1.pdf","size":"14098","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 140,2.5 ], [ 140,7.5 ], [ 145,7.5 ], [ 145,2.5 ], [ 140,2.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b0c","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":533911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29384,"text":"wri944003 - 1995 - Factors affecting water quality and net flux of solutes in two stream basins in the Quabbin Reservoir drainage basin, central Massachusetts, 1983-85","interactions":[],"lastModifiedDate":"2022-02-16T21:40:08.31276","indexId":"wri944003","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"94-4003","title":"Factors affecting water quality and net flux of solutes in two stream basins in the Quabbin Reservoir drainage basin, central Massachusetts, 1983-85","docAbstract":"The factors that affect stream-water quality were studied at West Branch Swift River (Swift River), and East Branch Fever Brook (Fever Brook), two forested watersheds that drain into the Quabbin Reservoir, central Massachusetts, from December 1983 through August 1985. Spatial and temporal variations of chemistry of precipitation, surface water; and ground water and the linkages between chemical changes and hydrologic processes were used to identify the mechanisms that control stream chemistry. Precipitation chemistry was dominated by hydrogen ion (composite p.H 4.23), sulfate, and nitrate. Inputs of hydrogen and nitrate from pre- cipitation were almost entirely retained in the basins, whereas input of sulfate was approximately balanced by export by streamflow draining the basins. Both streams were poorly buffered, with mean pH near 5.7, mean alkalinity less than 30 microequivalents per liter, and sulfate concen- trations greater than 130 microequivalents per liter. Sodium and chloride, derived primarily from highway deicing salts, were the dominant solutes at Fever Brook. After adjustments for deicing salts, fluxes of base cations during the 21-month study were 2,014 and 1,429 equivalents per hectare in Swift River and Fever Brook, respectively. Base cation fluxes were controlled primarily by weathering of hornblende (Fever Brook) and plagioclase (Swift River). The overall weathering rate was greater in the Swift River Basin because easily weathered gabbro underlies one subbasin which comprises 11.2 percent of the total basin area but contributed about 77 percent of the total alkalinity. Alkalinity export was nearly equal in the two basins, however, because some alkalinity was generated in wetlands in the Fever Brook Basin through bacterial sulfate reduction coupled with organic-carbon oxidation.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944003","usgsCitation":"Rittmaster, R., and Shanley, J.B., 1995, Factors affecting water quality and net flux of solutes in two stream basins in the Quabbin Reservoir drainage basin, central Massachusetts, 1983-85: U.S. Geological Survey Water-Resources Investigations Report 94-4003, v, 66 p., https://doi.org/10.3133/wri944003.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":58230,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4003/report-thumb.jpg"},{"id":396050,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47918.htm"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Quabbin Reservoir drainage basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.4167,\n              42.4583\n            ],\n            [\n              -72.1833,\n              42.4583\n            ],\n            [\n              -72.1833,\n              42.5458\n            ],\n            [\n              -72.4167,\n              42.5458\n            ],\n            [\n              -72.4167,\n              42.4583\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f879b","contributors":{"authors":[{"text":"Rittmaster, R. L.","contributorId":55861,"corporation":false,"usgs":true,"family":"Rittmaster","given":"R. L.","affiliations":[],"preferred":false,"id":201444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shanley, J. B.","contributorId":52226,"corporation":false,"usgs":true,"family":"Shanley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":201443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65548,"text":"i2428 - 1995 - Controlled photomosaic of the MTM-10117 Quadrangle (revised), Arsia Mons Region of Mars","interactions":[{"subject":{"id":65549,"text":"i2221 - 1991 - Controlled photomosaic of the MTM 10117 Quadrangle, Arsia Mons region of Mars","indexId":"i2221","publicationYear":"1991","noYear":false,"title":"Controlled photomosaic of the MTM 10117 Quadrangle, Arsia Mons region of Mars"},"predicate":"SUPERSEDED_BY","object":{"id":65548,"text":"i2428 - 1995 - Controlled photomosaic of the MTM-10117 Quadrangle (revised), Arsia Mons Region of Mars","indexId":"i2428","publicationYear":"1995","noYear":false,"title":"Controlled photomosaic of the MTM-10117 Quadrangle (revised), Arsia Mons Region of Mars"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:05","indexId":"i2428","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2428","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM-10117 Quadrangle (revised), Arsia Mons Region of Mars","language":"ENGLISH","doi":"10.3133/i2428","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM-10117 Quadrangle (revised), Arsia Mons Region of Mars (Supersedes I-2221): U.S. Geological Survey IMAP 2428, 1 remote-sensing image ;61 x 61 cm., on sheet 97 x 69 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2428.","productDescription":"1 remote-sensing image ;61 x 61 cm., on sheet 97 x 69 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101001,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2428/plate-1.pdf","size":"11862","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 115,-12.5 ], [ 115,-7.5 ], [ 120,-7.5 ], [ 120,-12.5 ], [ 115,-12.5 ] ] ] } } ] }","edition":"Supersedes I-2221","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6866db","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":533935,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185359,"text":"70185359 - 1995 - Chemical evolution of groundwater near a sinkhole lake, northern Florida: 1. Flow patterns, age of groundwater, and influence of lakewater leakage","interactions":[],"lastModifiedDate":"2018-03-21T15:06:56","indexId":"70185359","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Chemical evolution of groundwater near a sinkhole lake, northern Florida: 1. Flow patterns, age of groundwater, and influence of lakewater leakage","docAbstract":"<p><span>Leakage from sinkhole lakes significantly influences recharge to the Upper Floridan aquifer in poorly confined sediments in northern Florida. Environmental isotopes (oxygen 18, deuterium, and tritium), chlorofluorocarbons (CFCs: CFC-11, CCl</span><sub>3</sub><span>F; CFC-12, CCl</span><sub>2</sub><span>F</span><sub>2</sub><span>; and CFC-113, C</span><sub>2</sub><span>Cl</span><sub>3</sub><span>F</span><sub>3</sub><span>), and solute tracers were used to investigate groundwater flow patterns near Lake Barco, a seepage lake in a mantled karst setting in northern Florida. Stable isotope data indicated that the groundwater downgradient from the lake contained 11–67% lake water leakage, with a limit of detection of lake water in groundwater of 4.3%. The mixing fractions of lake water leakage, which passed through organic-rich sediments in the lake bottom, were directly proportional to the observed methane concentrations and increased with depth in the groundwater flow system. In aerobic groundwater upgradient from Lake Barco, CFC-modeled recharge dates ranged from 1987 near the water table to the mid 1970s for water collected at a depth of 30 m below the water table. CFC-modeled recharge dates (based on CFC-12) for anaerobic groundwater downgradient from the lake ranged from the late 1950s to the mid 1970s and were consistent with tritium data. CFC-modeled recharge dates based on CFC-11 indicated preferential microbial degradation in anoxic waters. Vertical hydraulic conductivities, calculated using CFC-12 modeled recharge dates and Darcy's law, were 0.17, 0.033, and 0.019 m/d for the surficial aquifer, intermediate confining unit, and lake sediments, respectively. These conductivities agreed closely with those used in the calibration of a three-dimensional groundwater flow model for transient and steady state flow conditions.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR00221","usgsCitation":"Katz, B.G., Lee, T.M., Plummer, N., and Busenberg, E., 1995, Chemical evolution of groundwater near a sinkhole lake, northern Florida: 1. Flow patterns, age of groundwater, and influence of lakewater leakage: Water Resources Research, v. 31, no. 6, p. 1549-1564, https://doi.org/10.1029/95WR00221.","productDescription":"16 p. ","startPage":"1549","endPage":"1564","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337921,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Lake Barco","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.00907707214355,\n              29.67850809103362\n            ],\n            [\n              -82.01105117797852,\n              29.675599772669415\n            ],\n            [\n              -82.00924873352051,\n              29.674182869145277\n            ],\n            [\n              -82.00693130493164,\n              29.674257443512726\n            ],\n            [\n              -82.00590133666992,\n              29.675823492453357\n            ],\n            [\n              -82.00624465942383,\n              29.67761323280481\n            ],\n            [\n              -82.00761795043945,\n              29.67835894854861\n            ],\n            [\n              -82.00907707214355,\n              29.67850809103362\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b94e4b0236b68f8291c","contributors":{"authors":[{"text":"Katz, Brian G. bkatz@usgs.gov","contributorId":1093,"corporation":false,"usgs":true,"family":"Katz","given":"Brian","email":"bkatz@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":685316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Terrie M. tmlee@usgs.gov","contributorId":2461,"corporation":false,"usgs":true,"family":"Lee","given":"Terrie","email":"tmlee@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":685317,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685318,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685319,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70185361,"text":"70185361 - 1995 - Chemical evolution of groundwater near a sinkhole lake, northern Florida: 2. Chemical patterns, mass-transfer modeling, and rates of chemical reactions","interactions":[],"lastModifiedDate":"2018-03-21T15:06:46","indexId":"70185361","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Chemical evolution of groundwater near a sinkhole lake, northern Florida: 2. Chemical patterns, mass-transfer modeling, and rates of chemical reactions","docAbstract":"<p><span>Chemical patterns along evolutionary groundwater flow paths in silicate and carbonate aquifers were interpreted using solute tracers, carbon and sulfur isotopes, and mass balance reaction modeling for a complex hydrologic system involving groundwater inflow to and outflow from a sinkhole lake in northern Florida. Rates of dominant reactions along defined flow paths were estimated from modeled mass transfer and ages obtained from CFC-modeled recharge dates. Groundwater upgradient from Lake Barco remains oxic as it moves downward, reacting with silicate minerals in a system open to carbon dioxide (CO</span><sub>2</sub><span>), producing only small increases in dissolved species. Beneath and downgradient of Lake Barco the oxic groundwater mixes with lake water leakage in a highly reducing, silicate-carbonate mineral environment. A mixing model, developed for anoxic groundwater downgradient from the lake, accounted for the observed chemical and isotopic composition by combining different proportions of lake water leakage and infiltrating meteoric water. The evolution of major ion chemistry and the<span>&nbsp;</span></span><sup>13</sup><span>C isotopic composition of dissolved carbon species in groundwater downgradient from the lake can be explained by the aerobic oxidation of organic matter in the lake, anaerobic microbial oxidation of organic carbon, and incongruent dissolution of smectite minerals to kaolinite. The dominant process for the generation of methane was by the CO</span><sub>2</sub><span><span>&nbsp;</span>reduction pathway based on the isotopic composition of hydrogen (δ</span><sup>2</sup><span>H(CH</span><sub>4</sub><span>) = −186 to −234‰) and carbon (δ</span><sup>13</sup><span>C(CH</span><sub>4</sub><span>) = −65.7 to −72.3‰). Rates of microbial metabolism of organic matter, estimated from the mass transfer reaction models, ranged from 0.0047 to 0.039 mmol L</span><sup>−1</sup><span><span>&nbsp;</span>yr</span><sup>−1</sup><span><span>&nbsp;</span>for groundwater downgradient from the lake.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR00220","usgsCitation":"Katz, B.G., Plummer, N., Busenberg, E., Revesz, K.M., Jones, B.F., and Lee, T.M., 1995, Chemical evolution of groundwater near a sinkhole lake, northern Florida: 2. Chemical patterns, mass-transfer modeling, and rates of chemical reactions: Water Resources Research, v. 31, no. 6, p. 1565-1584, https://doi.org/10.1029/95WR00220.","productDescription":"20 p. ","startPage":"1565","endPage":"1584","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337922,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b93e4b0236b68f8291a","contributors":{"authors":[{"text":"Katz, Brian G. bkatz@usgs.gov","contributorId":1093,"corporation":false,"usgs":true,"family":"Katz","given":"Brian","email":"bkatz@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":685329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685331,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Revesz, Kinga M. krevesz@usgs.gov","contributorId":506,"corporation":false,"usgs":true,"family":"Revesz","given":"Kinga","email":"krevesz@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":685332,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jones, Blair F. bfjones@usgs.gov","contributorId":2784,"corporation":false,"usgs":true,"family":"Jones","given":"Blair","email":"bfjones@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685333,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lee, Terrie M. tmlee@usgs.gov","contributorId":2461,"corporation":false,"usgs":true,"family":"Lee","given":"Terrie","email":"tmlee@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":685334,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":5157,"text":"fs11895 - 1995 - The Lake Pontchartrain watershed; a unique resource of the Louisiana coast","interactions":[],"lastModifiedDate":"2012-02-02T00:05:46","indexId":"fs11895","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"118-95","title":"The Lake Pontchartrain watershed; a unique resource of the Louisiana coast","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs11895","usgsCitation":"Demcheck, D.K., 1995, The Lake Pontchartrain watershed; a unique resource of the Louisiana coast: U.S. Geological Survey Fact Sheet 118-95, 1 sheet : col. ill. ; 28 cm. col. ill. ;, https://doi.org/10.3133/fs11895.","productDescription":"1 sheet : col. ill. ; 28 cm. col. ill. ;","costCenters":[],"links":[{"id":125250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0118/report-thumb.jpg"},{"id":31917,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0118/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf58","contributors":{"authors":[{"text":"Demcheck, Dennis K. 0000-0003-2981-078X ddemchec@usgs.gov","orcid":"https://orcid.org/0000-0003-2981-078X","contributorId":3273,"corporation":false,"usgs":true,"family":"Demcheck","given":"Dennis","email":"ddemchec@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":150515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65584,"text":"i2421 - 1995 - Controlled photomosaic of the MTM 40007 Quadrangle, Acidalia Planitia region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2421","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2421","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 40007 Quadrangle, Acidalia Planitia region of Mars","language":"ENGLISH","doi":"10.3133/i2421","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 40007 Quadrangle, Acidalia Planitia region of Mars: U.S. Geological Survey IMAP 2421, 1 remote-sensing image ;61 x 48 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2421.","productDescription":"1 remote-sensing image ;61 x 48 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101035,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2421/plate-1.pdf","size":"10863","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 5,37.5 ], [ 5,42.5 ], [ 10,42.5 ], [ 10,37.5 ], [ 5,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688290","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":533971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65585,"text":"i2419 - 1995 - Controlled photomosaic of the MTM 40012 Quadrangle, Acidalia Planitia region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2419","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2419","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 40012 Quadrangle, Acidalia Planitia region of Mars","language":"ENGLISH","doi":"10.3133/i2419","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 40012 Quadrangle, Acidalia Planitia region of Mars: U.S. Geological Survey IMAP 2419, 1 remote-sensing image ;62 x 48 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2419.","productDescription":"1 remote-sensing image ;62 x 48 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101036,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2419/plate-1.pdf","size":"11655","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 10,37.5 ], [ 10,42.5 ], [ 15,42.5 ], [ 15,37.5 ], [ 10,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688299","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":533972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30452,"text":"wri944210 - 1995 - Dissolved-solids contribution to the Colorado River from public lands in southeastern Nevada, through September 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri944210","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"94-4210","title":"Dissolved-solids contribution to the Colorado River from public lands in southeastern Nevada, through September 1993","docAbstract":"The Bureau of Land Management administers about 9,300 square miles of public lands in southeastern Nevada that are part of the Colorado River Basin. The U.S. Geological Survey, in cooperation with the Bureau of Land Management, began a 5-year program in October 1988 to assess the contribution of dissolved solids to the fiver from those lands. About 6,200 square miles of public lands are in the Muddy River subbasin in Nevada. The estimated average dissolved-solids load contributed to the Colorado River from those lands was 28,000 tons per year from October 1988 through September 1993. Subsurface flow contributed about 86 percent (24,000 tons per year) of that load. About 730 square miles of public lands in the Las Vegas Wash subbasin contribute dissolved-solids load to the Colorado River. (About 120 square miles of public lands do not contribute to the river.) The estimated average dissolved-solids load contributed to the river from those lands was about 1,300 tons per year from October 1988 through September 1993. Subsurface flow contributed almost all of that load. About 1,100 square miles of public lands are in the Virgin River subbasin in Nevada. The estimated average dissolved- solids load contributed to the  Colorado River from Nevada public lands in the subbasin was 8,700 tons per year. Subsurface flow contributed almost the entire load. About 1,200 square miles of Nevada public lands are in ephemeral tributaries that drain direcfly to the Colorado River or its impoundments (Lake Mead and Lake Mobave). The estimated average dissolved-solids load contributed to the river from those lands was 50 tons per year from surface runoff; however, the dissolved-solids load contributed by subsurface flow was not estimated. From October 1992 to September 1993, the Colorado River carried about 6,600,000 tons of dissolved solids past a streamflow gaging station 0.3 mile downstream from Hoover Dam. In contrast, surface runoff and subsurface flow contribute an estimated average dissolved-solids load of 38,000 tons per year from public lands in southeastern Nevada to the Colorado River. Land-management practices probably would not substantially reduce this contribution.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Services [distributor],","doi":"10.3133/wri944210","usgsCitation":"Westenburg, C., 1995, Dissolved-solids contribution to the Colorado River from public lands in southeastern Nevada, through September 1993: U.S. Geological Survey Water-Resources Investigations Report 94-4210, iv, 25 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri944210.","productDescription":"iv, 25 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":123953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4210/report-thumb.jpg"},{"id":59234,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4883e4b07f02db5181ba","contributors":{"authors":[{"text":"Westenburg, C.L.","contributorId":102511,"corporation":false,"usgs":true,"family":"Westenburg","given":"C.L.","affiliations":[],"preferred":false,"id":203276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38211,"text":"pp1547 - 1995 - Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington","interactions":[{"subject":{"id":20836,"text":"ofr90385 - 1992 - Sedimentology, behavior, and hazards of debris flows at Mount Rainier, Washington","indexId":"ofr90385","publicationYear":"1992","noYear":false,"title":"Sedimentology, behavior, and hazards of debris flows at Mount Rainier, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":38211,"text":"pp1547 - 1995 - Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington","indexId":"pp1547","publicationYear":"1995","noYear":false,"title":"Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"pp1547","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"1547","title":"Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington","docAbstract":"Mount Rainier is potentially the most dangerous volcano in the Cascade Range because of its great height, frequent earthquakes, active hydrothermal system, and extensive glacier mantle. Many debris flows and their distal phases have inundated areas far from the volcano during postglacial time. Two types of debris flows, cohesive and noncohesive, have radically different origins and behavior that relate empirically to clay content. The two types are the major subpopulations of debris flows at Mount Rainier. The behavior of cohesive flows is affected by the cohesion and adhesion of particles; noncohesive flows are dominated by particle collisions to the extent that particle cataclasis becomes common during near-boundary shear.\r\n\r\nCohesive debris flows contain more than 3 to 5 percent of clay-size sediment. The composition of these flows changed little as they traveled more than 100 kilometers from Mount Rainier to inundate parts of the now-populated Puget Sound lowland. They originate as deep-seated failures of sectors of the volcanic edifice, and such failures are sufficiently frequent that they are the major destructional process of Mount Rainier's morphologic evolution. In several deposits of large cohesive flows, a lateral, megaclast-bearing facies (with a mounded or hummocky surface) contrasts with a more clay-rich facies in the center of valleys and downstream. Cohesive flows at Mount Rainier do not correlate strongly with volcanic activity and thus can recur without warning, possibly triggered by non-magmatic earthquakes or by changes in the hydrothermal system.\r\n\r\nNoncohesive debris flows contain less than 3 to 5 percent clay-size sediment. They form most commonly by bulking of sediment in water surges, but some originate directly or indirectly from shallow slope failures that do not penetrate the hydrothermally altered core of the volcano. In contrast with cohesive flows, most noncohesive flows transform both from and to other flow types and are, therefore, the middle segments of flow waves that begin and end as flood surges. Proximally, through the bulking of poorly sorted volcaniclastic debris on the flanks of the volcano, flow waves expand rapidly in volume by transforming from water surges through hyperconcentrated stream flow (20 to 60 percent sediment by volume) to debris flow. Distally, the transformations occur more slowly in reverse order - from debris flow, to hyperconcentrated flow, and finally to normal streamflow with less than 20 percent sediment by volume. During runout of the largest noncohesive flows, hyperconcentrated flow has continued for as much as 40 to 70 kilometers.\r\n\r\nLahars (volcanic debris flows and their deposits) have occurred frequently at Mount Rainier over the past several thousand years, and generally they have not clustered within discrete eruptive periods as at Mount St. Helens. An exception is a period of large noncohesive flows during and after construction of the modern summit cone. Deposits from lahar-runout flows, the hyperconcentrated distal phases of lahars, document the frequency and extent of noncohesive lahars. These deposits also record the following transformations of debris flows: (1) the direct, progressive dilution of debris flow to hyperconcentrated flow, (2) deposition of successively finer grained lobes of debris until only the hyperconcentrated tail of the flow remains to continue downstream, and (3) dewatering of coarse debris flow deposits to yield fine-grained debris flow or hyperconcentrated flow.\r\n\r\nThree planning or design case histories represent different lengths of postglacial time. Case I is representative of large, infrequent (500 to 1,000 years on average) cohesive debris flows. These flows need to be considered in long-term planning in valleys around the volcano. Case II generalizes the noncohesive debris flows of intermediate size and recurrence (100 to 500 years). This case is appropriate for consideration in some structural design. Case III flows are ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp1547","usgsCitation":"Scott, K.M., Vallance, J., and Pringle, P.T., 1995, Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington: U.S. Geological Survey Professional Paper 1547, 56 p., https://doi.org/10.3133/pp1547.","productDescription":"56 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":104677,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4926.htm","linkFileType":{"id":5,"text":"html"},"description":"4926"},{"id":122086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1547/report-thumb.jpg"},{"id":12502,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/1547/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":64514,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1547/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64515,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1547/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,46 ], [ -123,47.75 ], [ -121,47.75 ], [ -121,46 ], [ -123,46 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb3c0","contributors":{"authors":[{"text":"Scott, K. M.","contributorId":8119,"corporation":false,"usgs":true,"family":"Scott","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":219341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vallance, J.W.","contributorId":45336,"corporation":false,"usgs":true,"family":"Vallance","given":"J.W.","affiliations":[],"preferred":false,"id":219343,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pringle, P. T.","contributorId":39806,"corporation":false,"usgs":true,"family":"Pringle","given":"P.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":219342,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68217,"text":"ha730K - 1995 - Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee","interactions":[{"subject":{"id":68217,"text":"ha730K - 1995 - Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee","indexId":"ha730K","publicationYear":"1995","noYear":false,"chapter":"K","title":"Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee"},"predicate":"IS_PART_OF","object":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"id":1}],"isPartOf":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"lastModifiedDate":"2017-05-30T16:01:32","indexId":"ha730K","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"730","chapter":"K","title":"Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee","docAbstract":"<p>This report provides a summary of ground-water conditions and problems in Illinois, Indiana, Kentucky, Ohio, and Tennessee, which compose Segment 10 of the Ground Water Atlas of the United States, an area of about 217,000 square miles. The definition, distribution, thickness, water-yielding, and water-quality characteristics of the principal aquifers in the segment are the primary topics of this chapter. Ground-water source, occurrence, movement, use, and problems also are discussed where appropriate. </p><p>Segment 10 consists of parts of seven physiographic provinces (fig. 1)- the Coastal Plain, Blue Ridge, Valley and Ridge, Appalachian Plateaus, Interior Low Plateaus, Central Lowland, and Ozark Plateaus. The provinces have unique hydrogeologic characteristics that make it convenient to describe the principal aquifers in each province.</p>","largerWorkTitle":"Ground Water Atlas of the United States","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha730K","isbn":"0607767596","usgsCitation":"Lloyd, O., and Lyke, W.L., 1995, Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee: U.S. Geological Survey Hydrologic Atlas 730, 30 p., https://doi.org/10.3133/ha730K.","productDescription":"30 p.","startPage":"K1","endPage":"K30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":115255,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/730k/report.pdf","text":"Report","size":"65.53 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":11488,"rank":100,"type":{"id":15,"text":"Index 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,{"id":27595,"text":"wri944164 - 1995 - Use of fathometers and electrical-conductivity probes to monitor riverbed scour at bridge piers","interactions":[],"lastModifiedDate":"2012-02-02T00:08:39","indexId":"wri944164","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"94-4164","title":"Use of fathometers and electrical-conductivity probes to monitor riverbed scour at bridge piers","docAbstract":"Two methods, a fathometer system and an electrical- conductivity probe system, were developed to monitor scour at bridge piers. The scour-monitoring systems consisted of a sensor (fathometer or electrical- conductivity probe), power supply, data logger, relay, and system program. The fathometer system was installed and tested at a bridge over the Leipsic River at Leipsic, Delaware, and at a bridge over Sinepuxent Bay near Ocean City. Maryland. Field data collected indicate that fathometers can be used to identify and monitor the riverbed elevation if post processing of the data and trends in the data are used to determine the riverbed location in relation to the transducer. The accuracy of the system is approximately the same as the resolution of the fathometer. Signal scatter can be a major source of error in the data. The electrical- conductivity probe system was installed and tested at a bridge over the Pamunkey River near Hanover, Virginia. The approximate elevation of the riverbed is determined by comparing conductivities of the surface-water flow with conductivities of submerged bed material from sensors located in each. Field data collected indicate that an electrical- conductivity probe, as tested, has limited usefulness in identifying and monitoring the riverbed elevation during high flows. As the discharge increases, the concentration of sediment in the surface-water flow increases, especially near the riverbed. Conductivities, measured at the sensors in the surface-water flow could not be distinguished from conductivities measured at the shallowest sensor in the submerged bed material.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944164","usgsCitation":"Hayes, D.C., and Drummond, F., 1995, Use of fathometers and electrical-conductivity probes to monitor riverbed scour at bridge piers: U.S. Geological Survey Water-Resources Investigations Report 94-4164, iv, 17 p. :ill., map ;28 cm., https://doi.org/10.3133/wri944164.","productDescription":"iv, 17 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":158814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4164/report-thumb.jpg"},{"id":56466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4882e4b07f02db516b6d","contributors":{"authors":[{"text":"Hayes, Donald C.","contributorId":14000,"corporation":false,"usgs":true,"family":"Hayes","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drummond, F.E.","contributorId":63057,"corporation":false,"usgs":true,"family":"Drummond","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":198385,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65518,"text":"i2422 - 1995 - Controlled photomosaic of the MTM 00142 Quadrangle, Gordii Dorsum region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2422","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2422","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 00142 Quadrangle, Gordii Dorsum region of Mars","language":"ENGLISH","doi":"10.3133/i2422","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 00142 Quadrangle, Gordii Dorsum region of Mars: U.S. Geological Survey IMAP 2422, 1 remote-sensing image ;61 x 62 cm., on sheet 97 x 69 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2422.","productDescription":"1 remote-sensing image ;61 x 62 cm., on sheet 97 x 69 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100975,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2422/plate-1.pdf","size":"13307","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 140,-2.5 ], [ 140,2.5 ], [ 145,2.5 ], [ 145,-2.5 ], [ 140,-2.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b8e","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":533905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65604,"text":"i2417 - 1995 - Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:06","indexId":"i2417","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2417","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars","language":"ENGLISH","doi":"10.3133/i2417","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars: U.S. Geological Survey IMAP 2417, 1 remote-sensing image ;62 x 45 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2417.","productDescription":"1 remote-sensing image ;62 x 45 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101054,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2417/plate-1.pdf","size":"9679","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 20,42.5 ], [ 20,47.5 ], [ 25,47.5 ], [ 25,42.5 ], [ 20,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688256","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":533992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65536,"text":"i2403 - 1995 - Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars","interactions":[],"lastModifiedDate":"2019-12-23T12:38:24","indexId":"i2403","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2403","title":"Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2403","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars: U.S. Geological Survey IMAP 2403, Plate: 26 x 38 inches, https://doi.org/10.3133/i2403.","productDescription":"Plate: 26 x 38 inches","costCenters":[],"links":[{"id":189936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100989,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2403/plate-1.pdf","size":"18749","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688425","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":533923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}