{"pageNumber":"4134","pageRowStart":"103325","pageSize":"25","recordCount":166022,"records":[{"id":35392,"text":"b1845 - 1989 - Geomorphic, seismic, and geotechnical evaluation of sand and gravel deposits in the Sheridan, Wyoming, area","interactions":[],"lastModifiedDate":"2012-02-02T00:09:47","indexId":"b1845","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1845","title":"Geomorphic, seismic, and geotechnical evaluation of sand and gravel deposits in the Sheridan, Wyoming, area","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1845","usgsCitation":"Odum, J.K., and Miller, C., 1989, Geomorphic, seismic, and geotechnical evaluation of sand and gravel deposits in the Sheridan, Wyoming, area: U.S. Geological Survey Bulletin 1845, v, 32 p. ill., map ;28 cm., https://doi.org/10.3133/b1845.","productDescription":"v, 32 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":165242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1845/report-thumb.jpg"},{"id":247560,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1845/plate-1.pdf","size":"2871","linkFileType":{"id":1,"text":"pdf"}},{"id":63254,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1845/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4fc","contributors":{"authors":[{"text":"Odum, Jack K. 0000-0002-3162-0355","orcid":"https://orcid.org/0000-0002-3162-0355","contributorId":97900,"corporation":false,"usgs":true,"family":"Odum","given":"Jack","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":214557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, C.H.","contributorId":19148,"corporation":false,"usgs":true,"family":"Miller","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":214556,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33133,"text":"b1794 - 1989 - Anhydrite deposits of the United States and characteristics of anhydrite important for storage of radioactive wastes","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"b1794","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1794","title":"Anhydrite deposits of the United States and characteristics of anhydrite important for storage of radioactive wastes","language":"ENGLISH","publisher":"U.S. G.P.O. ; For sale by the Books and Open-File Reports Section, Federal Center,","doi":"10.3133/b1794","usgsCitation":"Dean, W.E., and Johnson, K.S., 1989, Anhydrite deposits of the United States and characteristics of anhydrite important for storage of radioactive wastes: U.S. Geological Survey Bulletin 1794, ix, 132 p. ill. ;28 cm., https://doi.org/10.3133/b1794.","productDescription":"ix, 132 p. ill. ;28 cm.","costCenters":[],"links":[{"id":161359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1794/report-thumb.jpg"},{"id":60945,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1794/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c15e","contributors":{"authors":[{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":209994,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Kenneth Sutherland","contributorId":81151,"corporation":false,"usgs":true,"family":"Johnson","given":"Kenneth","email":"","middleInitial":"Sutherland","affiliations":[],"preferred":false,"id":209995,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28709,"text":"wri874272 - 1989 - Hydrology of the Castle Lake blockage, Mount St. Helens, Washington","interactions":[],"lastModifiedDate":"2022-02-03T21:40:12.647391","indexId":"wri874272","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4272","title":"Hydrology of the Castle Lake blockage, Mount St. Helens, Washington","docAbstract":"<p>The debris avalanche that occurred during the May 19, 1980, eruption of Mount St. Helens blocked South Fork Castle Creek and created Castle Lake. Stability of the blockage was of concern, and a digital model that simulates three-dimensional groundwater movement in the blockage was constructed as part of the analysis used in a follow-up study that assessed the blockage 's stability. Slug test results in the debris avalanche deposits and model results indicate that the average horizontal hydraulic conductivity of the blockage material is approximately 2.5 ft/day, whereas the ratio of horizontal to vertical hydraulic conductivity is approximately 10 to 1. The model was calibrated to seasonally high groundwater levels and groundwater discharge. Model-predicted recharge rates for this time period were 0.97 cu ft/sec. Most of the recharge (81%) results from the infiltration of precipitation, whereas discharge by seeps through the blockage accounts for 81% of the total discharge. Because water levels under the crest of the blockage are higher than lake level, the movement of groundwater is toward the lake and the toe of the blockage. The model allows the water levels to be estimated at any location in the blockage. This information is required for making estimates of the stability of the blockage against failure by gravitational-induced or earthquake-induced slope failure, liquefaction, the process of seepage erosion, or by erosion.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874272","usgsCitation":"Meyer, W., and Sabol, M.A., 1989, Hydrology of the Castle Lake blockage, Mount St. Helens, Washington: U.S. Geological Survey Water-Resources Investigations Report 87-4272, iv, 25 p., https://doi.org/10.3133/wri874272.","productDescription":"iv, 25 p.","costCenters":[],"links":[{"id":395412,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46917.htm"},{"id":124043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4272/report-thumb.jpg"},{"id":57545,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4272/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Castle Lake blockage, Mount St, Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.31285095214842,\n              46.24884345903478\n            ],\n            [\n              -122.26221084594725,\n              46.24884345903478\n            ],\n            [\n              -122.26221084594725,\n              46.275190434531005\n            ],\n            [\n              -122.31285095214842,\n              46.275190434531005\n            ],\n            [\n              -122.31285095214842,\n              46.24884345903478\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a24a6","contributors":{"authors":[{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":200268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sabol, M. A.","contributorId":36178,"corporation":false,"usgs":true,"family":"Sabol","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3626,"text":"cir1030 - 1989 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","interactions":[{"subject":{"id":15090,"text":"ofr88472 - 1988 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","indexId":"ofr88472","publicationYear":"1988","noYear":false,"title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty"},"predicate":"SUPERSEDED_BY","object":{"id":3626,"text":"cir1030 - 1989 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","indexId":"cir1030","publicationYear":"1989","noYear":false,"title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir1030","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1030","title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty","docAbstract":"The interactions of the water resources on and within the surface of the Earth with the atmosphere that surrounds it are exceedingly complex. Increased uncertainty can be attached to the availability of water of usable quality in the 21st century, therefore, because of potential anthropogenic changes in the global climate system. For the U.S. Geological Survey to continue to fulfill its mission with respect to assessing the Nation's water resources, an expanded program to study the hydrologic implications of climate uncertainty will be required. The goal for this program is to develop knowledge and information concerning the potential water-resources implications for the United States of uncertainties in climate that may result from both anthropogenic and natural changes of the Earth's atmosphere. Like most past and current water-resources programs of the Geological Survey, the climate-uncertainty program should be composed of three elements: (1) research, (2) data collection, and (3) interpretive studies. However, unlike most other programs, the climate-uncertainty program necessarily will be dominated by its research component during its early years. \r\n\r\nCritical new concerns to be addressed by the research component are (1) areal estimates of evapotranspiration, (2) hydrologic resolution within atmospheric (climatic) models at the global scale and at mesoscales, (3) linkages between hydrology and climatology, and (4) methodology for the design of data networks that will help to track the impacts of climate change on water resources. Other ongoing activities in U.S. Geological Survey research programs will be enhanced to make them more compatible with climate-uncertainty research needs. \r\n\r\nThe existing hydrologic data base of the Geological Survey serves as a key element in assessing hydrologic and climatologic change. However, this data base has evolved in response to other needs for hydrologic information and probably is not as sensitive to climate change as is desirable. Therefore, as measurement and network-design methodologies are improved to account for climate-change potential, new data-collection activities will be added to the existing programs. One particular area of data-collection concern pertains to the phenomenon of evapotranspiration. \r\n\r\nInterpretive studies of the hydrologic implications of climate uncertainty will be initiated by establishing several studies at the river-basin scale in diverse hydroclimatic and demographic settings. These studies will serve as tests of the existing methodologies for studying the impacts of climate change and also will help to define subsequent research priorities. A prototype for these studies was initiated in early 1988 in the Delaware River basin.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir1030","usgsCitation":"Moss, M.E., and Lins, H.F., 1989, Water resources in the twenty-first century; a study of the implications of climate uncertainty: U.S. Geological Survey Circular 1030, vi, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1030.","productDescription":"vi, 25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1989/1030/report-thumb.jpg"},{"id":30669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1989/1030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0951","contributors":{"authors":[{"text":"Moss, Marshall E.","contributorId":6830,"corporation":false,"usgs":true,"family":"Moss","given":"Marshall","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":147282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":147281,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28993,"text":"wri894211 - 1989 - Analysis of geophysical well logs and flowmeter measurements in boreholes penetrating subhorizontal fracture zones, Lac de Bonnet Batholith, Manitoba, Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri894211","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4211","title":"Analysis of geophysical well logs and flowmeter measurements in boreholes penetrating subhorizontal fracture zones, Lac de Bonnet Batholith, Manitoba, Canada","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Books and Open-File Reports Section,","doi":"10.3133/wri894211","usgsCitation":"Paillet, F.L., 1989, Analysis of geophysical well logs and flowmeter measurements in boreholes penetrating subhorizontal fracture zones, Lac de Bonnet Batholith, Manitoba, Canada: U.S. Geological Survey Water-Resources Investigations Report 89-4211, 30 p. :ill. ;28 cm., https://doi.org/10.3133/wri894211.","productDescription":"30 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4211/report-thumb.jpg"},{"id":57861,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4211/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680437","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200750,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38453,"text":"pp1409E - 1989 - Ground-water hydrology and simulated effects of development in Smith Creek valley, a hydrologically closed basin in Lander County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:02","indexId":"pp1409E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1409","chapter":"E","title":"Ground-water hydrology and simulated effects of development in Smith Creek valley, a hydrologically closed basin in Lander County, Nevada","language":"ENGLISH","doi":"10.3133/pp1409E","usgsCitation":"Thomas, J.M., Carlton, S., and Hines, L., 1989, Ground-water hydrology and simulated effects of development in Smith Creek valley, a hydrologically closed basin in Lander County, Nevada: U.S. Geological Survey Professional Paper 1409, p. E1-E57, 2 plates in pocket, https://doi.org/10.3133/pp1409E.","productDescription":"p. E1-E57, 2 plates in pocket","costCenters":[],"links":[{"id":104637,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4862.htm","linkFileType":{"id":5,"text":"html"},"description":"4862"},{"id":122090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1409e/report-thumb.jpg"},{"id":64944,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1409e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64945,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1409e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64946,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1409e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d86","contributors":{"authors":[{"text":"Thomas, J. M.","contributorId":62217,"corporation":false,"usgs":true,"family":"Thomas","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":219849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlton, S.M.","contributorId":18036,"corporation":false,"usgs":true,"family":"Carlton","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":219847,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hines, L.B.","contributorId":49406,"corporation":false,"usgs":true,"family":"Hines","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":219848,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28406,"text":"wri884101 - 1989 - Estimated use of water in Colorado, 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri884101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4101","title":"Estimated use of water in Colorado, 1985","docAbstract":"Water-use data was collected for the State of Colorado as part of the U.S. Geological Survey 's National Water-Use Information Program. An estimated 20,800 million gal/day of water were used in Colorado during 1985. 89% came from surface water sources and 11% came from groundwater sources. Public supply systems provided 4% of all water used in Colorado during 1985, but provided 80% of all commercial, domestic, and industrial water used. An estimated 4,840 million gal/day of water were consumed during 1985; return flows amounted to 16,000 million gallons per day. Of all water used, 60% was used for irrigation, 35% for hydroelectric power generation, and the remaining 5% for commercial, domestic, industrial, livestock, mining, and other uses. The most water was used in Montrose (3,260 million gal/day), Mesa (1,950 million gal/day), and Gunnison (1,520 million gal/day) Counties. The predominant water uses in these counties were hydroelectric power and irrigation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884101","usgsCitation":"Litke, D.W., and Appel, C.L., 1989, Estimated use of water in Colorado, 1985: U.S. Geological Survey Water-Resources Investigations Report 88-4101, xi, 157 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884101.","productDescription":"xi, 157 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124029,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4101/report-thumb.jpg"},{"id":57211,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4101/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a044","contributors":{"authors":[{"text":"Litke, D. W.","contributorId":94346,"corporation":false,"usgs":true,"family":"Litke","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Appel, C. L.","contributorId":62212,"corporation":false,"usgs":true,"family":"Appel","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":199744,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67097,"text":"i1894 - 1989 - Historic trail maps of the Sterling 1° x 2° quadrangle, northeastern Colorado","interactions":[],"lastModifiedDate":"2021-10-22T21:55:20.903255","indexId":"i1894","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1894","title":"Historic trail maps of the Sterling 1° x 2° quadrangle, northeastern Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1894","usgsCitation":"Scott, G., 1989, Historic trail maps of the Sterling 1° x 2° quadrangle, northeastern Colorado: U.S. Geological Survey IMAP 1894, Report: 23 p.; 2 Plates: 29.22 x 22.68 inches and 28.25 x 22.20 inches, https://doi.org/10.3133/i1894.","productDescription":"Report: 23 p.; 2 Plates: 29.22 x 22.68 inches and 28.25 x 22.20 inches","costCenters":[],"links":[{"id":390877,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9973.htm"},{"id":189385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1894/report-thumb.jpg"},{"id":91646,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1894/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256451,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1894/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256452,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1894/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Colorado","otherGeospatial":"Sterling 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,40 ], [ -104,41 ], [ -102,41 ], [ -102,40 ], [ -104,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885ac","contributors":{"authors":[{"text":"Scott, G. R.","contributorId":61398,"corporation":false,"usgs":true,"family":"Scott","given":"G. R.","affiliations":[],"preferred":false,"id":275595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67188,"text":"i1939 - 1989 - Geologic map of the Montrose 30' x 60' Quadrangle, southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"i1939","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1939","subseriesTitle":"NONE","title":"Geologic map of the Montrose 30' x 60' Quadrangle, southwestern Colorado","language":"ENGLISH","doi":"10.3133/i1939","usgsCitation":"Steven, T.A., and Hail, W., 1989, Geologic map of the Montrose 30' x 60' Quadrangle, southwestern Colorado: U.S. Geological Survey IMAP 1939, 1 map :col. ;88 x 55 cm., on sheet 86 x 137 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1939.","productDescription":"1 map :col. ;88 x 55 cm., on sheet 86 x 137 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107193,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10013.htm","linkFileType":{"id":5,"text":"html"},"description":"10013"},{"id":188850,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108,38 ], [ -108,38.5 ], [ -107,38.5 ], [ -107,38 ], [ -108,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696841","contributors":{"authors":[{"text":"Steven, T. A.","contributorId":42575,"corporation":false,"usgs":true,"family":"Steven","given":"T.","middleInitial":"A.","affiliations":[],"preferred":false,"id":275738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hail, W. J. Jr.","contributorId":35332,"corporation":false,"usgs":true,"family":"Hail","given":"W. J.","suffix":"Jr.","affiliations":[],"preferred":false,"id":275737,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61406,"text":"mf2110 - 1989 - Correlation of the Charleston Sandstone of the proposed Pennsylvanian stratotype with strata in eastern Kentucky, western West Virginia, and southern Ohio","interactions":[],"lastModifiedDate":"2025-05-29T20:29:54.706374","indexId":"mf2110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2110","title":"Correlation of the Charleston Sandstone of the proposed Pennsylvanian stratotype with strata in eastern Kentucky, western West Virginia, and southern Ohio","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2110","isbn":"0607820357","usgsCitation":"Outerbridge, W., 1989, Correlation of the Charleston Sandstone of the proposed Pennsylvanian stratotype with strata in eastern Kentucky, western West Virginia, and southern Ohio: U.S. Geological Survey Miscellaneous Field Studies Map 2110, 1 Plate: 40.95 x 32.40 inches, https://doi.org/10.3133/mf2110.","productDescription":"1 Plate: 40.95 x 32.40 inches","costCenters":[],"links":[{"id":282203,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2110/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183668,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":487852,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5710.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"1000000","country":"United States","state":"Kentucky, Ohio, West Virginia","otherGeospatial":"Charleston Sandstone","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -83.5,\n              38.5\n            ],\n            [\n              -83.5,\n              37.1333\n            ],\n            [\n              -81.3333,\n              37.1333\n            ],\n            [\n              -81.3333,\n              38.5\n            ],\n            [\n              -83.5,\n              38.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684578","contributors":{"authors":[{"text":"Outerbridge, W.F.","contributorId":58646,"corporation":false,"usgs":true,"family":"Outerbridge","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":265593,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63442,"text":"gq1632 - 1989 - Geologic map of the Inferno Cone quadrangle, Butte County, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq1632","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1632","title":"Geologic map of the Inferno Cone quadrangle, Butte County, Idaho","language":"ENGLISH","doi":"10.3133/gq1632","usgsCitation":"Kuntz, M., Lefebvre, R., Champion, D., and Skipp, B., 1989, Geologic map of the Inferno Cone quadrangle, Butte County, Idaho: U.S. Geological Survey Geologic Quadrangle 1632, 1 map :col. ;58 x 42 cm., on sheet 70 x 127 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1632.","productDescription":"1 map :col. ;58 x 42 cm., on sheet 70 x 127 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102705,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1155.htm","linkFileType":{"id":5,"text":"html"},"description":"1155"},{"id":179785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.61749999999999,43.3675 ], [ -113.61749999999999,43.5 ], [ -113.5,43.5 ], [ -113.5,43.3675 ], [ -113.61749999999999,43.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697b88","contributors":{"authors":[{"text":"Kuntz, Mel A. 0000-0001-8828-5474","orcid":"https://orcid.org/0000-0001-8828-5474","contributorId":6446,"corporation":false,"usgs":true,"family":"Kuntz","given":"Mel A.","affiliations":[],"preferred":false,"id":268858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lefebvre, R.H.","contributorId":85656,"corporation":false,"usgs":true,"family":"Lefebvre","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":268861,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Champion, D.E.","contributorId":70402,"corporation":false,"usgs":true,"family":"Champion","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":268860,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Skipp, Betty","contributorId":51268,"corporation":false,"usgs":true,"family":"Skipp","given":"Betty","affiliations":[],"preferred":false,"id":268859,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38425,"text":"pp1496 - 1989 - Topographic and structural conditions in areas of gravitational spreading of ridges in the Western United States","interactions":[],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"pp1496","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1496","title":"Topographic and structural conditions in areas of gravitational spreading of ridges in the Western United States","language":"ENGLISH","doi":"10.3133/pp1496","usgsCitation":"Varnes, D.J., Hall-Radbruch, D.H., and Savage, W.Z., 1989, Topographic and structural conditions in areas of gravitational spreading of ridges in the Western United States: U.S. Geological Survey Professional Paper 1496, 28 p., https://doi.org/10.3133/pp1496.","productDescription":"28 p.","costCenters":[],"links":[{"id":113184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1496/report.pdf","size":"10665","linkFileType":{"id":1,"text":"pdf"}},{"id":164810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1496/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a129","contributors":{"authors":[{"text":"Varnes, D. J.","contributorId":85201,"corporation":false,"usgs":true,"family":"Varnes","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":219801,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall-Radbruch, D. H.","contributorId":54268,"corporation":false,"usgs":true,"family":"Hall-Radbruch","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":219800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Savage, W. Z.","contributorId":106481,"corporation":false,"usgs":true,"family":"Savage","given":"W.","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":219802,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28592,"text":"wri884156 - 1989 - Hydrology of the Prospector Square area, Summit County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri884156","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4156","title":"Hydrology of the Prospector Square area, Summit County, Utah","docAbstract":"The Silver Creek tailings site is in Prospector Square, a commercial development and residential community in Summit County, Utah. This study assessed the presence of metals and the movement of groundwater in the unconsolidated valley-fill and consolidated-rock aquifers underlying the tailings. The unconsolidated valley fill is a poorly sorted mixture of clay, silt, sand, and gravel, with intermittent layers of clay. The hydraulic conductivity, estimated on the basis of slug tests, ranged from 1 to 14 ft/day. An aquifer-interference test indicated that water in the valley fill underlying the tailings site did not move toward the pumped municipal well completed in the consolidated-rock aquifer. Concentrations of dissolved and suspended cadmium, manganese, and zinc were greater than background in surface water only during low-flow conditions. Concentrations of suspended iron and lead were greater than background concentrations upstream from the tailings site, but concentrations decreased progressively downstream and during later sampling rounds. Concentrations of dissolved cadmium, managanese, and zinc were greater than background concentrations in water from six wells and one drain. Dissolved arsenic and lead were detected in water from a well downgradient from Prospector Square, but were not detected in water from any of the other wells. Concentrations of all selected metals detected in stream-sediment samples, were detected in similar concentrations in tailings samples. Concentrations of metals in surface and groundwater could increase if the pH of the water decreases substantially from the present (1988) values of about 7 (neutral). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884156","usgsCitation":"Mason, J.L., 1989, Hydrology of the Prospector Square area, Summit County, Utah: U.S. Geological Survey Water-Resources Investigations Report 88-4156, v, 75 p. :ill. ;28 cm., https://doi.org/10.3133/wri884156.","productDescription":"v, 75 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123537,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4156/report-thumb.jpg"},{"id":57421,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4156/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdbad","contributors":{"authors":[{"text":"Mason, J. L.","contributorId":24389,"corporation":false,"usgs":true,"family":"Mason","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200079,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27661,"text":"wri894037 - 1989 - Trend analysis of Lake Parker stage and relation to various hydrologic factors, 1950-86, Lakeland, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri894037","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4037","title":"Trend analysis of Lake Parker stage and relation to various hydrologic factors, 1950-86, Lakeland, Florida","docAbstract":"Kendall tau test and regression analysis were used to determine if statistically significant long-term trends exist for Lake Parker, Florida stage data or for four other area lakes, four groundwater sites, four rainfall sites, Lakeland public-supply pumpage, and pan evaporation. A 10% significance level was used for criterion of an existing trend. Findings were consistent between the two analytical methods. There were no long-term trends indicated for seasonal or annual stage data at Lake Parker. Statistically significant Kendall tau slope estimators were detected for pan evaporation (+0.45 in/yr), Lakeland well-field pumpage (+0.56 million gal/day/yr), and one groundwater site (+0.48 ft/year). Decreasing trends were indicated for three other lakes (-0.03 to -0.27 ft/year) and one groundwater site (-0.25 ft/year). Kendall tau tests of four annual rainfall records indicated no long-term trends. Change in Lake Parker stage from November to May was related by multiple linear regression to change in groundwater level, rainfall, and pumpage for the same time period. The regression coefficient of determination was 0.90, and the standard error was 0.24 ft. Monthly change in lake stage for November through May was related to evaporation, rainfall, and groundwater levels with a coefficient of determination of 0.67 and a standard error of 0.14 ft. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports [distributor],","doi":"10.3133/wri894037","usgsCitation":"Henderson, S., and Lopez, M.A., 1989, Trend analysis of Lake Parker stage and relation to various hydrologic factors, 1950-86, Lakeland, Florida: U.S. Geological Survey Water-Resources Investigations Report 89-4037, iii, 19 p. :ill. ;28 cm., https://doi.org/10.3133/wri894037.","productDescription":"iii, 19 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4037/report-thumb.jpg"},{"id":56515,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db6267a1","contributors":{"authors":[{"text":"Henderson, S.E.","contributorId":70806,"corporation":false,"usgs":true,"family":"Henderson","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":198488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lopez, M. A.","contributorId":12493,"corporation":false,"usgs":true,"family":"Lopez","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198487,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27988,"text":"wri894081 - 1989 - Hydrogeology and results of aquifer tests in the vicinity of a hazardous-waste disposal site near Byron, Illinois","interactions":[],"lastModifiedDate":"2023-03-14T18:25:34.408189","indexId":"wri894081","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4081","title":"Hydrogeology and results of aquifer tests in the vicinity of a hazardous-waste disposal site near Byron, Illinois","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the U.S. Environmental Protection Agency, conducted an investigation of a Superfund Site near Byron, Illinois. The purpose of the investigation was to determine the hydrogeologic properties of the Galena-Platteville and St. Peter aquifers, the primary water-supply aquifers for domestic supply in the area. The Galena and Platteville Groups and older St. Peter Sandstone are separated by the Harmony Hill Shale Member of the Glenwood Formation. The Harmony Hill Shale Member is a semiconfining unit. Groundwater flow in the study area is from the site northwestward to the Rock River. Movement of groundwater in the dolomites is mainly through joints, fractures, and solution openings. Analysis of the Galena-Platteville aquifer-test data indicates that the calculated aquifer transmissivity ranges from 490 to 670 sq ft/day, and the calculated specific yield ranges from 0.017 to 0.140. Aquifer test data also indicate that the Galena-Platteville aquifer is heterogeneous and anisotropic. Analysis of the St. Peter aquifer-test data indicates that the calculated transmissivity of the aquifer ranges from 1,200 to 1 ,305 sq ft/day, storativity ranges from 0.000528 to 0.00128, horizontal hydraulic conductivity ranges from 2.9 to 3.1 ft/day, and leakage through the Harmony Hill Shale Member ranges from .000123 to .000217 ft/day/ft.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894081","usgsCitation":"Kay, R.T., Olson, D.N., and Ryan, B.J., 1989, Hydrogeology and results of aquifer tests in the vicinity of a hazardous-waste disposal site near Byron, Illinois: U.S. Geological Survey Water-Resources Investigations Report 89-4081, vi, 56 p., https://doi.org/10.3133/wri894081.","productDescription":"vi, 56 p.","costCenters":[],"links":[{"id":414114,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47189.htm","linkFileType":{"id":5,"text":"html"}},{"id":56811,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4081/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119982,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4081/report-thumb.jpg"}],"country":"United States","state":"Illinois","city":"Byron","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.3333,\n              42.1083\n            ],\n            [\n              -89.3333,\n              42.0625\n            ],\n            [\n              -89.2917,\n              42.0625\n            ],\n            [\n              -89.2917,\n              42.1083\n            ],\n            [\n              -89.3333,\n              42.1083\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6254b5","contributors":{"authors":[{"text":"Kay, Robert T. 0000-0002-6281-8997 rtkay@usgs.gov","orcid":"https://orcid.org/0000-0002-6281-8997","contributorId":1122,"corporation":false,"usgs":true,"family":"Kay","given":"Robert","email":"rtkay@usgs.gov","middleInitial":"T.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":199019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, David N.","contributorId":66305,"corporation":false,"usgs":true,"family":"Olson","given":"David","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":199021,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ryan, Barbara J.","contributorId":62989,"corporation":false,"usgs":true,"family":"Ryan","given":"Barbara","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199020,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61418,"text":"mf2103 - 1989 - Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations along the western margins of the greater Green River Basin in southwest Wyoming","interactions":[],"lastModifiedDate":"2025-05-29T20:03:45.8047","indexId":"mf2103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2103","title":"Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations along the western margins of the greater Green River Basin in southwest Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2103","isbn":"0607820284","usgsCitation":"Roehler, H.W., 1989, Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations along the western margins of the greater Green River Basin in southwest Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 2103, 1 Plate: 28.67 x 31.19 inches, https://doi.org/10.3133/mf2103.","productDescription":"1 Plate: 28.67 x 31.19 inches","costCenters":[],"links":[{"id":487568,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5703.htm","linkFileType":{"id":5,"text":"html"}},{"id":186857,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/2103/report-thumb.jpg"},{"id":282198,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2103/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"666700","country":"United States","state":"Wyoming","otherGeospatial":"greater Green River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111,\n              42.667\n            ],\n            [\n              -111,\n              41\n            ],\n            [\n              -109.7942,\n              41\n            ],\n            [\n              -109.7942,\n              42.667\n            ],\n            [\n              -111,\n              42.667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6846a5","contributors":{"authors":[{"text":"Roehler, H. W.","contributorId":16072,"corporation":false,"usgs":true,"family":"Roehler","given":"H.","middleInitial":"W.","affiliations":[],"preferred":false,"id":265613,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67108,"text":"i1803A - 1989 - Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i1803A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1803","subseriesTitle":"NONE","chapter":"A","title":"Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana","language":"ENGLISH","doi":"10.3133/i1803A","usgsCitation":"Segal, D.B., and Rowan, L.C., 1989, Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana: U.S. Geological Survey IMAP 1803, 1 map :col. ;45 x 63 cm., on sheet 59 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1803A.","productDescription":"1 map :col. ;45 x 63 cm., on sheet 59 x 104 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107132,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9924.htm","linkFileType":{"id":5,"text":"html"},"description":"9924"},{"id":188041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,45 ], [ -114,46 ], [ -112,46 ], [ -112,45 ], [ -114,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c869","contributors":{"authors":[{"text":"Segal, D. B.","contributorId":60236,"corporation":false,"usgs":true,"family":"Segal","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":275616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowan, L. C.","contributorId":40584,"corporation":false,"usgs":true,"family":"Rowan","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":275615,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61419,"text":"mf2105 - 1989 - Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations along the western margins of the Sand Wash Basin, northwest Colorado, and Washakie Basin, southwest Wyoming","interactions":[],"lastModifiedDate":"2025-05-29T20:16:41.202035","indexId":"mf2105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2105","title":"Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations along the western margins of the Sand Wash Basin, northwest Colorado, and Washakie Basin, southwest Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2105","isbn":"0607820306","usgsCitation":"Roehler, H.W., 1989, Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations along the western margins of the Sand Wash Basin, northwest Colorado, and Washakie Basin, southwest Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 2105, 1 Plate: 55.04 x 41.71 inches, https://doi.org/10.3133/mf2105.","productDescription":"1 Plate: 55.04 x 41.71 inches","costCenters":[],"links":[{"id":282194,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2105/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/2105/report-thumb.jpg"},{"id":487713,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5705.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"666700","country":"United States","state":"Colorado, Wyoming","otherGeospatial":"Sand Wash Basin, Washakie Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.8536,\n              41.667\n            ],\n            [\n              -108.8536,\n              40.6789\n            ],\n            [\n              -108.1464,\n              40.6789\n            ],\n            [\n              -108.1464,\n              41.667\n            ],\n            [\n              -108.8536,\n              41.667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684696","contributors":{"authors":[{"text":"Roehler, H. W.","contributorId":16072,"corporation":false,"usgs":true,"family":"Roehler","given":"H.","middleInitial":"W.","affiliations":[],"preferred":false,"id":265614,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61420,"text":"mf2102 - 1989 - Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations, Great Divide Basin, southwest Wyoming","interactions":[],"lastModifiedDate":"2025-05-29T19:54:04.059262","indexId":"mf2102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2102","title":"Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations, Great Divide Basin, southwest Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2102","isbn":"0607820276","usgsCitation":"Roehler, H.W., 1989, Correlation of surface sections of the intertongued Eocene Wasatch and Green River formations, Great Divide Basin, southwest Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 2102, 1 Plate: 35.78 x 27.21 inches, https://doi.org/10.3133/mf2102.","productDescription":"1 Plate: 35.78 x 27.21 inches","costCenters":[],"links":[{"id":487502,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5702.htm","linkFileType":{"id":5,"text":"html"}},{"id":282199,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2102/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186894,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/2102/report-thumb.jpg"}],"scale":"666700","country":"United States","state":"Wyoming","otherGeospatial":"Great Divide Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.2397,\n              42.3333\n            ],\n            [\n              -109.2397,\n              41.5456\n            ],\n            [\n              -107.8861,\n              41.5456\n            ],\n            [\n              -107.8861,\n              42.3333\n            ],\n            [\n              -109.2397,\n              42.3333\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684572","contributors":{"authors":[{"text":"Roehler, H. W.","contributorId":16072,"corporation":false,"usgs":true,"family":"Roehler","given":"H.","middleInitial":"W.","affiliations":[],"preferred":false,"id":265615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28626,"text":"wri874124 - 1989 - Estimation of the recharge area of a pumped, stratified-drift aquifer in Connecticut by simulation modeling","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri874124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4124","title":"Estimation of the recharge area of a pumped, stratified-drift aquifer in Connecticut by simulation modeling","docAbstract":"Groundwater quality management plans in Connecticut require information about the size and shape of recharge areas that contribute flow to pumping centers in extensive, stratified-drift aquifers. Flow models of a hypothetical aquifer , and a stratified-drift aquifer in Farmington are used to evaluate how contributing areas change in response to variations in recharge and hydraulic conductivity. A series of simulations of a hypothetical aquifer model were made during which average annual recharge rates of 0, 15, 25, and 35 inches were combined with aquifer hydraulic conductivity values of 25, 75, and 225 ft/day. Under steady-state conditions, and a withdrawal rate of 1.2 million gal/day, the size of the contributing recharge area ranges from 0.16 to 0.75 sq mi as recharge from precipitation and average aquifer hydraulic conductivity range from highest to lowest values. Three simulations of the Farmington aquifer model were made: they assumed steady-state conditions, a withdrawal rate of 2.8 million gal/day, and combinations of recharge and aquifer hydraulic conductivity that represented highest, average and lowest rates. The size of the contributing recharge area, under these conditions, ranges from 0.89 to 1.94 sq mi. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri874124","usgsCitation":"Mazzaferro, D., 1989, Estimation of the recharge area of a pumped, stratified-drift aquifer in Connecticut by simulation modeling: U.S. Geological Survey Water-Resources Investigations Report 87-4124, vi, 100 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874124.","productDescription":"vi, 100 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124022,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4124/report-thumb.jpg"},{"id":57456,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4124/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57457,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4124/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57458,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4124/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57459,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4124/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4124/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb1bf","contributors":{"authors":[{"text":"Mazzaferro, D. L.","contributorId":75579,"corporation":false,"usgs":true,"family":"Mazzaferro","given":"D. L.","affiliations":[],"preferred":false,"id":200138,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28438,"text":"wri884095 - 1989 - Withdrawals and consumptive use of water in Pennsylvania, 1984","interactions":[],"lastModifiedDate":"2022-12-02T22:36:58.350085","indexId":"wri884095","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4095","title":"Withdrawals and consumptive use of water in Pennsylvania, 1984","docAbstract":"Total accountable water withdrawals in Pennsylvania during 1984 were 14,033.66 Mga/d (million gallons per day); of that total, 5.2 percent (729.53 Mgal/d) was supplied from ground-water sources in 94.8 percent (13,302.12 Mgal/d) was supplied from surface-water sources. Thermoelectric power generation accounted for 71 percent of the total withdrawals (10,010.60 Mgal/d); this was followed by self-supplied industry, 15 percent (2,055.63 Mgal/d); public supply, 11 percent (1,600.02 Mgal/d); mining (147.73 Mgal/d), self- supplied domestic use (131.63 Mgal/d), livestock and poultry (83.52 Mgal/d) and irrigation (4.52 Mgal/d) collectively made up 3 percent. Total consumptive use of water was 615.22 Mgal/d; self-supplied industry is responsible for the greatest consumptive use--185.53 Mgal/d.\r\n\r\n      Trends in water withdrawals from 1950 to 1984 were examined for public supply, thermoelectric power generation and self-supplied industry. Total population and water withdrawals for public supply gradual increased in those years, whereas withdrawals for self-supplied industry and power generation increased until 1970 and then decreased.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884095","usgsCitation":"Loper, C.A., Lent, S.D., and Wetzel, K.L., 1989, Withdrawals and consumptive use of water in Pennsylvania, 1984: U.S. Geological Survey Water-Resources Investigations Report 88-4095, iv, 50 p., https://doi.org/10.3133/wri884095.","productDescription":"iv, 50 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":410028,"rank":2,"type":{"id":36,"text":"NGMDB Index 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,{"id":27653,"text":"wri884140 - 1989 - Application of the precipitation-runoff modeling system to the Ah-Shi-Sle-Pah Wash watershed, San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2022-02-10T22:53:19.002925","indexId":"wri884140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4140","title":"Application of the precipitation-runoff modeling system to the Ah-Shi-Sle-Pah Wash watershed, San Juan County, New Mexico","docAbstract":"<p>The precipitation-runoff modeling system was applied to the 8.21 sq-mi drainage area of the Ah-shi-sle-pah Wash watershed in northwestern New Mexico. The calibration periods were May to September of 1981 and 1982, and the verification period was May to September 1983. Twelve storms were available for calibration and 8 storms were available for verification. For calibration A (hydraulic conductivity estimated from onsite data and other storm-mode parameters optimized), the computed standard error of estimate was 50% for runoff volumes and 72% of peak discharges. Calibration B included hydraulic conductivity in the optimization, which reduced the standard error of estimate to 28 % for runoff volumes and 50% for peak discharges. Optimized values for hydraulic conductivity resulted in reductions from 1.00 to 0.26 in/h and 0.20 to 0.03 in/h for the 2 general soils groups in the calibrations. Simulated runoff volumes using 7 of 8 storms occurring during the verification period had a standard error of estimate of 40% for verification A and 38% for verification B. Simulated peak discharge had a standard error of estimate of 120% for verification A and 56% for verification B. Including the eighth storm which had a relatively small magnitude in the verification analysis more than doubled the standard error of estimating volumes and peaks.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884140","usgsCitation":"Hejl, H.R., 1989, Application of the precipitation-runoff modeling system to the Ah-Shi-Sle-Pah Wash watershed, San Juan County, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 88-4140, iv, 36 p., https://doi.org/10.3133/wri884140.","productDescription":"iv, 36 p.","costCenters":[],"links":[{"id":395827,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47049.htm"},{"id":56509,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4140/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"San Juan County","otherGeospatial":"Ah-Shi-Sle-Pah Wash watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.97431945800781,\n              36.134547437460064\n            ],\n            [\n              -107.87406921386717,\n              36.134547437460064\n            ],\n            [\n              -107.87406921386717,\n              36.18942952802744\n            ],\n            [\n              -107.97431945800781,\n              36.18942952802744\n            ],\n            [\n              -107.97431945800781,\n              36.134547437460064\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a96a","contributors":{"authors":[{"text":"Hejl, H. R. Jr.","contributorId":69555,"corporation":false,"usgs":true,"family":"Hejl","given":"H.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198474,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61426,"text":"mf2077 - 1989 - Surface and subsurface correlations showing depositional environments of the upper Cretaceous Mesaverde Group and associated formations, Cow Creek in southwest Wyoming to Mount Harris in northwest Colorado","interactions":[],"lastModifiedDate":"2025-05-29T17:47:54.377646","indexId":"mf2077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2077","title":"Surface and subsurface correlations showing depositional environments of the upper Cretaceous Mesaverde Group and associated formations, Cow Creek in southwest Wyoming to Mount Harris in northwest Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2077","isbn":"0607819898","usgsCitation":"Roehler, H.W., and Hansen, D., 1989, Surface and subsurface correlations showing depositional environments of the upper Cretaceous Mesaverde Group and associated formations, Cow Creek in southwest Wyoming to Mount Harris in northwest Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 2077, 1 Plate: 37.83 × 25.11 inches, https://doi.org/10.3133/mf2077.","productDescription":"1 Plate: 37.83 × 25.11 inches","costCenters":[],"links":[{"id":392105,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5678.htm"},{"id":281768,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2077/plate-1.pdf"},{"id":180413,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/2077/report-thumb.jpg"}],"country":"United States","state":"Colorado, Wyoming","otherGeospatial":"Cow Creek, Mount Harris","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.6767,\n              41.4083\n            ],\n            [\n              -107.075,\n              41.4083\n            ],\n            [\n              -107.075,\n              40.4647\n            ],\n            [\n              -107.6767,\n              40.4647\n            ],\n            [\n              -107.6767,\n              41.4083\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6983ba","contributors":{"authors":[{"text":"Roehler, H. W.","contributorId":16072,"corporation":false,"usgs":true,"family":"Roehler","given":"H.","middleInitial":"W.","affiliations":[],"preferred":false,"id":265621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, D. E.","contributorId":73609,"corporation":false,"usgs":true,"family":"Hansen","given":"D. E.","affiliations":[],"preferred":false,"id":265622,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28352,"text":"wri884152 - 1989 - The hydrothermal system in central Twin Falls County, Idaho","interactions":[],"lastModifiedDate":"2013-11-21T14:29:18","indexId":"wri884152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4152","title":"The hydrothermal system in central Twin Falls County, Idaho","docAbstract":"Thermal water in Twin Fall County has been used for space heating, large-scale greenhouse operations, and aquaculture since the mid-1970's. More recently, increased utilization of the thermal water has caused aquifer pressures to decline. Near the city of Twin Falls, water levels in some formerly flowing thermal wells have declined to below land surface. The thermal water is principally in the silicic volcanic rocks of the Idavada Volcanics. Electrical resistivity soundings indicate that thickness of the rocks ranges from about 700 to 3,000 ft and averages about 2,000 ft. Temperatures of water sampled range from 26 C to nearly 50 C in wells completed in the upper part of the reservoir near Twin Falls. Water from deeper parts of the reservoir may be warmer than 50 C. Most of the thermal water is a sodium bicarbonate type. The maximum fluoride concentration was 22 mg/L. Chloride concentrations between about 50 and 150 mg/L are the result of mixing of deep water with shallower, cooler water that has been affected by percolation of irrigation water. Carbon-14 concentrations in selected thermal water samples indicate ages of 1,000 to 15,000 years. The water becomes progressively older northward along proposed groundwater flowpaths. On the basis of transit times in the system of 10,000 to 15,000 years and the reservoir volume, recharge is estimated to be about 5 to 7 cu ft/sec. Net heat flux in the area is about 2.2 heat flow units.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884152","collaboration":"Prepared in cooperation with Idaho Department of Water Resources","usgsCitation":"Lewis, R., and Young, H., 1989, The hydrothermal system in central Twin Falls County, Idaho: U.S. Geological Survey Water-Resources Investigations Report 88-4152, iii, 44 p.,, https://doi.org/10.3133/wri884152.","productDescription":"iii, 44 p.,","numberOfPages":"50","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":158329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4152/report-thumb.jpg"},{"id":57157,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Twin Falls County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.0396,42.9195 ], [ -115.0396,41.9942 ], [ -114.0099,41.9942 ], [ -114.0099,42.9195 ], [ -115.0396,42.9195 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d5a8","contributors":{"authors":[{"text":"Lewis, R.E.","contributorId":31735,"corporation":false,"usgs":true,"family":"Lewis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":199647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":199648,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28711,"text":"wri894072 - 1989 - Tritium deposition in the continental United States, 1953-83","interactions":[],"lastModifiedDate":"2021-11-26T22:18:08.328543","indexId":"wri894072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4072","title":"Tritium deposition in the continental United States, 1953-83","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894072","usgsCitation":"Michel, R.L., 1989, Tritium deposition in the continental United States, 1953-83: U.S. Geological Survey Water-Resources Investigations Report 89-4072, iv, 46 p., https://doi.org/10.3133/wri894072.","productDescription":"iv, 46 p.","costCenters":[],"links":[{"id":392159,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49230.htm"},{"id":57546,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4072/report-thumb.jpg"}],"country":"United States","otherGeospatial":"continental United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        \"type\": \"MultiPolygon\",\n        \"coordinates\": [\n          [\n            [\n              [\n                -94.81758,\n                49.38905\n              ],\n              [\n                -94.64,\n                48.84\n              ],\n              [\n                -94.32914,\n                48.67074\n              ],\n          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