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,{"id":44533,"text":"wri77136 - 1978 - Floods of November 11-13, 1974, in St. Croix, U.S. Virgin Islands","interactions":[],"lastModifiedDate":"2019-08-05T09:09:10","indexId":"wri77136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"77-136","title":"Floods of November 11-13, 1974, in St. Croix, U.S. Virgin Islands","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri77136","usgsCitation":"Haire, W., and Johnson, K., 1978, Floods of November 11-13, 1974, in St. Croix, U.S. Virgin Islands: U.S. Geological Survey Water-Resources Investigations Report 77-136, 11 Plates: 22.87 x 17.26 inches or smaller, https://doi.org/10.3133/wri77136.","productDescription":"11 Plates: 22.87 x 17.26 inches or smaller","costCenters":[],"links":[{"id":366125,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":134821,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0136/report-thumb.jpg"},{"id":366126,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-8.pdf"},{"id":366127,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366128,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366129,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366130,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366131,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366132,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366133,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366134,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366135,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0136/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","country":"United States","otherGeospatial":"St. Croix","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -65,17.5 ], [ -65,18 ], [ -64.5,18 ], [ -64.5,17.5 ], [ -65,17.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df932","contributors":{"authors":[{"text":"Haire, W.J.","contributorId":47341,"corporation":false,"usgs":true,"family":"Haire","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":229953,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, K. G.","contributorId":29381,"corporation":false,"usgs":true,"family":"Johnson","given":"K. G.","affiliations":[],"preferred":false,"id":229952,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42807,"text":"ofr78951 - 1978 - Preliminary reconnaissance bedrock geologic map of the Shrewsbury quadrangle, Worcester County, Massachusetts","interactions":[],"lastModifiedDate":"2022-04-05T19:27:54.703242","indexId":"ofr78951","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-951","title":"Preliminary reconnaissance bedrock geologic map of the Shrewsbury quadrangle, Worcester County, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78951","usgsCitation":"Hepburn, J.C., 1978, Preliminary reconnaissance bedrock geologic map of the Shrewsbury quadrangle, Worcester County, Massachusetts: U.S. Geological Survey Open-File Report 78-951, Report: 14 p.; 1 Plate: 19.19 × 28.07 inches, https://doi.org/10.3133/ofr78951.","productDescription":"Report: 14 p.; 1 Plate: 19.19 × 28.07 inches","costCenters":[],"links":[{"id":80622,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0951/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80621,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0951/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0951/report-thumb.jpg"},{"id":398139,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74949.htm"}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Worcester County","otherGeospatial":"Shrewsbury quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.75,\n              42.25\n            ],\n            [\n              -71.625,\n              42.25\n            ],\n            [\n              -71.625,\n              42.375\n            ],\n            [\n              -71.75,\n              42.375\n            ],\n            [\n              -71.75,\n              42.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc89","contributors":{"authors":[{"text":"Hepburn, J. Christopher","contributorId":60305,"corporation":false,"usgs":true,"family":"Hepburn","given":"J.","email":"","middleInitial":"Christopher","affiliations":[],"preferred":false,"id":227164,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42813,"text":"ofr78518 - 1978 - Preliminary reconnaissance geologic map of the Glendale Quadrangle, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:11:08","indexId":"ofr78518","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-518","title":"Preliminary reconnaissance geologic map of the Glendale Quadrangle, Oregon","language":"ENGLISH","doi":"10.3133/ofr78518","usgsCitation":"Page, N.J., Johnson, M.G., Moring, B., Blair, W., Gray, F., and Cannon, J., 1978, Preliminary reconnaissance geologic map of the Glendale Quadrangle, Oregon: U.S. Geological Survey Open-File Report 78-518, 1 map., https://doi.org/10.3133/ofr78518.","productDescription":"1 map.","costCenters":[],"links":[{"id":176196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108554,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14754.htm","linkFileType":{"id":5,"text":"html"},"description":"14754"},{"id":80628,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0518/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc90","contributors":{"authors":[{"text":"Page, Norman J.","contributorId":46492,"corporation":false,"usgs":true,"family":"Page","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":227177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, M. G.","contributorId":22831,"corporation":false,"usgs":true,"family":"Johnson","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":227176,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moring, Barry","contributorId":80692,"corporation":false,"usgs":true,"family":"Moring","given":"Barry","affiliations":[],"preferred":false,"id":227179,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blair, W.N.","contributorId":49033,"corporation":false,"usgs":true,"family":"Blair","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":227178,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gray, Floyd 0000-0002-0223-8966 fgray@usgs.gov","orcid":"https://orcid.org/0000-0002-0223-8966","contributorId":603,"corporation":false,"usgs":true,"family":"Gray","given":"Floyd","email":"fgray@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":227175,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cannon, J.K.","contributorId":106965,"corporation":false,"usgs":true,"family":"Cannon","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":227180,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":42816,"text":"ofr78418 - 1978 - Preliminary reconnaissance geologic maps of the Garnet Range, western Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:11:08","indexId":"ofr78418","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-418","title":"Preliminary reconnaissance geologic maps of the Garnet Range, western Montana","language":"ENGLISH","doi":"10.3133/ofr78418","usgsCitation":"Wallace, C.A., Klepper, M.R., and French, A., 1978, Preliminary reconnaissance geologic maps of the Garnet Range, western Montana: U.S. Geological Survey Open-File Report 78-418, 1 map. +1 text (6 p., mounted on 1 sheet), https://doi.org/10.3133/ofr78418.","productDescription":"1 map. +1 text (6 p., mounted on 1 sheet)","costCenters":[],"links":[{"id":175753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0418/report-thumb.jpg"},{"id":80640,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0418/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80641,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0418/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc6e","contributors":{"authors":[{"text":"Wallace, C. A.","contributorId":15596,"corporation":false,"usgs":true,"family":"Wallace","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":227190,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klepper, M. R.","contributorId":64278,"corporation":false,"usgs":true,"family":"Klepper","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":227191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"French, A. B.","contributorId":10479,"corporation":false,"usgs":true,"family":"French","given":"A. B.","affiliations":[],"preferred":false,"id":227189,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9964,"text":"ofr78144 - 1978 - Hydrogeology of the observation well site at the United States Geological Survey National Center, Reston, Virginia","interactions":[],"lastModifiedDate":"2022-10-04T21:14:02.622659","indexId":"ofr78144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-144","title":"Hydrogeology of the observation well site at the United States Geological Survey National Center, Reston, Virginia","docAbstract":"<p>The U. S. Geological Survey's National Center is on a 105-acre tract straddling rocks of two distinct types. These are pelitic schists of late Precambrian and early Paleozoic age; and sandstone, shale, siltstone, and conglomerate of Triassic age. Within the Triassic part is a diabase dike and an associated contact metamorphic zone.</p><p>Two observation wells and two core holes were drilled on the part of the property underlain by Triassic rocks. The wells are 10-inch and 8-inch diameter and were drilled to depths of 165 feet and 205 feet. The wells were drilled to monitor water levels, for equipment testing, and to determine the hydraulic properties of the Triassic rocks. Geophysical logs were run, and good correlations were found between the electric and caliper logs and the lithologic logs prepared from drill cuttings and cores.</p><p>An aquifer test was made and was analyzed by the Theis method which considers nonleaky artesian conditions and the Streltsova method which considers flow in fractured rocks. The test results suggest that transmissivity of the sandstone aquifer is about 40 ft2/day. Flowmeter surveys showed that the water comes from two thin zones parallel to the bedding. The flowmeter surveys, core samples, and geophysical logs suggest that the Triassic sandstone is a fractured-rock aquifer. Water is probably derived from partings and joints parallel to bedding which in turn are fed by vertical joints and fractures.</p><p>A water sample taken at the close of the aquifer test indicates that the water has a low dissolved solids content, is soft, and is generally of excellent quality.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78144","usgsCitation":"Larson, J.D., 1978, Hydrogeology of the observation well site at the United States Geological Survey National Center, Reston, Virginia: U.S. Geological Survey Open-File Report 78-144, 35 p., https://doi.org/10.3133/ofr78144.","productDescription":"35 p.","costCenters":[],"links":[{"id":407898,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0144/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142423,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0144/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Reston","otherGeospatial":"United States Geological Survey National Center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.37044334411621,\n              38.94393982589585\n            ],\n            [\n              -77.36407041549683,\n              38.94393982589585\n            ],\n            [\n              -77.36407041549683,\n              38.948212067795126\n            ],\n            [\n              -77.37044334411621,\n              38.948212067795126\n            ],\n            [\n              -77.37044334411621,\n              38.94393982589585\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684702","contributors":{"authors":[{"text":"Larson, J. D.","contributorId":83084,"corporation":false,"usgs":true,"family":"Larson","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":160583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9965,"text":"ofr79202 - 1978 - Direct solution algorithm for the two-dimensional ground-water flow model","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr79202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"79-202","title":"Direct solution algorithm for the two-dimensional ground-water flow model","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79202","usgsCitation":"Larson, S.P., 1978, Direct solution algorithm for the two-dimensional ground-water flow model: U.S. Geological Survey Open-File Report 79-202, 25 p. :ill. ;27 cm. --, https://doi.org/10.3133/ofr79202.","productDescription":"25 p. :ill. ;27 cm. --","costCenters":[],"links":[{"id":142424,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0202/report-thumb.jpg"},{"id":37766,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0202/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64abdc","contributors":{"authors":[{"text":"Larson, S. P.","contributorId":34903,"corporation":false,"usgs":true,"family":"Larson","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":160584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27846,"text":"wri791 - 1978 - Water-quality assessment of runoff from a rural highway bridge near Tallahassee, Florida","interactions":[],"lastModifiedDate":"2019-07-15T10:11:32","indexId":"wri791","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"79-1","title":"Water-quality assessment of runoff from a rural highway bridge near Tallahassee, Florida","docAbstract":"Runoff from a rural highway bridge on U.S. 27 near Tallahassee, Florida, was found to have an insignificant water-quality loading impact on the Ochlockonee River. Potential annual-runoff loads on the bridge surface for virtually all constituents studied were less than one percent of those transported by the river at the study site. The loading rates for some parameters were significantly related to traffic counts, but the regression equations were limited to traffic ranges between 3,800 to 4,200 vehicles per day in 1977-78. Precipitation samples indicated that a significant percentage of the constituent loading to the bridge surface is from atmospheric deposition. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri791","usgsCitation":"Irwin, G.A., and Losey, G.T., 1978, Water-quality assessment of runoff from a rural highway bridge near Tallahassee, Florida: U.S. Geological Survey Water-Resources Investigations Report 79-1, v, 27 p. , https://doi.org/10.3133/wri791.","productDescription":"v, 27 p. ","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":158603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0001/report-thumb.jpg"},{"id":365505,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0001/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","city":"Tallahassee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.4134521484375,\n              30.344435586368462\n            ],\n            [\n              -84.144287109375,\n              30.344435586368462\n            ],\n            [\n              -84.144287109375,\n              30.526779182105784\n            ],\n            [\n              -84.4134521484375,\n              30.526779182105784\n            ],\n            [\n              -84.4134521484375,\n              30.344435586368462\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e715e","contributors":{"authors":[{"text":"Irwin, G. A.","contributorId":35733,"corporation":false,"usgs":true,"family":"Irwin","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Losey, Gerald T.","contributorId":97150,"corporation":false,"usgs":true,"family":"Losey","given":"Gerald","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":198773,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23139,"text":"ofr78752 - 1978 - Land use and land cover maps for Mindego Hill, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr78752","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-752","title":"Land use and land cover maps for Mindego Hill, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78752","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for Mindego Hill, California: U.S. Geological Survey Open-File Report 78-752, 1 map., https://doi.org/10.3133/ofr78752.","productDescription":"1 map.","costCenters":[],"links":[{"id":155581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae465","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":529115,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18100,"text":"ofr78908 - 1978 - Quality of water and dye-dispersion characteristics in the Back Bay of Biloxi, Harrison County, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr78908","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-908","title":"Quality of water and dye-dispersion characteristics in the Back Bay of Biloxi, Harrison County, Mississippi","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78908","usgsCitation":"Bednar, G.A., 1978, Quality of water and dye-dispersion characteristics in the Back Bay of Biloxi, Harrison County, Mississippi: U.S. Geological Survey Open-File Report 78-908, iv, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr78908.","productDescription":"iv, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db65187b","contributors":{"authors":[{"text":"Bednar, Gene A.","contributorId":81881,"corporation":false,"usgs":true,"family":"Bednar","given":"Gene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":178544,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18203,"text":"ofr78239 - 1978 - Water-resources investigations of the U.S. Geological Survey in Wyoming, fiscal year 1978","interactions":[],"lastModifiedDate":"2017-01-09T10:18:08","indexId":"ofr78239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-239","title":"Water-resources investigations of the U.S. Geological Survey in Wyoming, fiscal year 1978","docAbstract":"<p>This report contains lists of streamflow and reservoir stations, peak-flow partial-record stations, chemical-quality stations, sediment stations, and observation wells where water levels are measured in Wyoming. The locations of the basic-data sites are shown on maps. Thirty-two water-resources appraisal projects in Wyoming are also described, including many that are related to the development of energy resources. The general locations of the projects are shown on maps. The report serves as an annual progress report to cooperators and the public.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Cheyenne, WY","doi":"10.3133/ofr78239","usgsCitation":"Boner, F.C., 1978, Water-resources investigations of the U.S. Geological Survey in Wyoming, fiscal year 1978: U.S. Geological Survey Open-File Report 78-239, v, 106 p., https://doi.org/10.3133/ofr78239.","productDescription":"v, 106 p.","numberOfPages":"112","costCenters":[],"links":[{"id":47568,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0239/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0239/report-thumb.jpg"}],"country":"United States","state":"Wyoming","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c1a","contributors":{"authors":[{"text":"Boner, F. C.","contributorId":32136,"corporation":false,"usgs":true,"family":"Boner","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":178698,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46990,"text":"ofr78286 - 1978 - Equal area base map of Norton Sound and the Northern Bering Sea","interactions":[],"lastModifiedDate":"2012-02-02T00:10:39","indexId":"ofr78286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-286","title":"Equal area base map of Norton Sound and the Northern Bering Sea","language":"ENGLISH","doi":"10.3133/ofr78286","usgsCitation":"Gerin, M., 1978, Equal area base map of Norton Sound and the Northern Bering Sea: U.S. Geological Survey Open-File Report 78-286, 1 map., https://doi.org/10.3133/ofr78286.","productDescription":"1 map.","costCenters":[],"links":[{"id":172699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr78286.JPG"},{"id":99853,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0286/plate-1.pdf","size":"3941","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6020c2","contributors":{"authors":[{"text":"Gerin, Marybeth","contributorId":20718,"corporation":false,"usgs":true,"family":"Gerin","given":"Marybeth","email":"","affiliations":[],"preferred":false,"id":234448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38697,"text":"pp813I - 1978 - Summary appraisals of the nation's ground-water resources – Mid-Atlantic region","interactions":[],"lastModifiedDate":"2021-12-14T21:53:16.272671","indexId":"pp813I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"813","chapter":"I","title":"Summary appraisals of the nation's ground-water resources – Mid-Atlantic region","docAbstract":"<p>The Mid-Atlantic Region covers a total area of about 108,000 square miles. It includes parts of Vermont, Massachusetts, New York, Pennsylvania, Maryland, West Virginia, and Virginia, the entire States of New Jersey and Delaware, and the District of Columbia. It encompasses the entire drainage basins (within the United States) of the Hudson, Delaware, Susquehanna, Potomac, and the James River and includes Long Island and the coastal drainage of New Jersey, Delaware, Maryland, and Virginia.</p>\n<p>Ground water in the region occurs in three broad types of geologic terrane: (1) unconsolidated deposits in the Coastal Plain seaward of the Fall Line; (2) hard, consolidated sedimentary rocks and crystalline igneous and metamorphic rocks in the remainder of the region; and (3) unconsolidated sand, gravel, and other deposits of glacial origin that overlie the older rocks extensively in the glaciated northern part of the region.</p>\n<p>Ground water is derived primarily from precipitation; it can be intercepted for use by pumping from wells before it reaches the streams or before it drains into coastal wetlands or the ocean.</p>\n<p>The natural discharge from the aquifers in the region is estimated to be at about 38.6 billion gallons per day; in addition, at least 140-350 trillion gallons is stored in the rocks.</p>\n<p>About 949 billion gallons of fresh ground water was withdrawn in 1970. This quantity represents about 9 percent of the total freshwater use of 10,220 billion gallons. Available ground-water reserves indicate that a considerable part of the additional supplies needed for the anticipated increase in economic activity in the region could be developed from ground water.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813I","usgsCitation":"Sinnott, A., and Cushing, E.M., 1978, Summary appraisals of the nation's ground-water resources – Mid-Atlantic region: U.S. Geological Survey Professional Paper 813, iv, 32 p., https://doi.org/10.3133/pp813I.","productDescription":"iv, 32 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":392895,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5064.htm"},{"id":119916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813i/report-thumb.jpg"},{"id":65551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813i/report.pdf","text":"Report","size":"8.19 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Delaware, Maryland, Massachusetts, New Jersey, New York, Pennsylvania, Vermont, Virginia, West Virginia","otherGeospatial":"District of Columbia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.77294921875,\n              45.02695045318546\n            ],\n            [\n              -71.4990234375,\n              45.058001435398296\n            ],\n      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Survey","active":false,"usgs":true}],"preferred":false,"id":220304,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, Elliot Morse","contributorId":14390,"corporation":false,"usgs":true,"family":"Cushing","given":"Elliot","email":"","middleInitial":"Morse","affiliations":[],"preferred":false,"id":220305,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10599,"text":"ofr78140 - 1978 - Distribution of organic carbon and petroleum source rock potential of Cretaceous and lower Tertiary carbonates, south Florida basin: Preliminary results","interactions":[],"lastModifiedDate":"2022-09-16T18:24:27.785516","indexId":"ofr78140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-140","title":"Distribution of organic carbon and petroleum source rock potential of Cretaceous and lower Tertiary carbonates, south Florida basin: Preliminary results","docAbstract":"Analyses of 134 core samples from the South Florida Basin show that the carbonates of Comanchean age are relatively richer in average organic carbon (0.41 percent) than those of Coahuilan age (0.28 percent), Gulfian age (0.18 percent) and Paleocene age (0.20 percent). They are also nearly twice as rich as the average world, wide carbonate (average 0.24 percent). The majority of carbonates have organic carbons less than 0.30 percent but the presence of many relatively organic rich beds composed of highly bituminous, argillaceous, highly stylolitic, and algal-bearing limestones and dolomites accounts for the higher percentage of organic carbon in some of the stratigraphic \r\nunits. \r\n\r\nCarbonate rocks that contain greater than 0.4 percent organic carbon and that might be considered as possible petroleum sources were noted in almost each subdivision of the Coahuilan and Comanchean Series but particularly the units of Fredericksburg 'B', Trinity 'A', Trinity 'F', and Upper Sunniland. Possible source rocks have been ascribed by others to the Lower Sunniland, but lack of sufficient samples precluded any firm assessment in this initial report. \r\n\r\nIn the shallower section of the basin, organic-rich carbonates containing as much as 3.2 percent organic carbon were observed in the lowermost part of the Gulfian Series and carbonate rocks with oil staining or 'dead' and 'live oil' were noted by others in the uppermost Gulfian and upper Cedar Keys Formation. It is questionable whether these shallower rocks are of sufficient thermal maturity to have generated commercial oil.\r\n\r\nThe South Florida basin is still sparsely drilled and produces only from the Sunniland Limestone at an average depth of 11,500 feet (3500 m). Because the Sunniland contains good reservoir rocks and apparently adequate source rocks, and because the success rate of new oil field discoveries has increased in recent years, the chances of finding additional oil reserves in the Sunniland are promising. Furthermore, the presence of possible source rocks in many of the other stratigraphic units, in particular, the Fredericksburg, should give further impetus to exploring for other productive horizons.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78140","usgsCitation":"Palacas, J.G., 1978, Distribution of organic carbon and petroleum source rock potential of Cretaceous and lower Tertiary carbonates, south Florida basin: Preliminary results: U.S. Geological Survey Open-File Report 78-140, Report: 43 p.; 6 Plates: 11.32 × 57.82 inches or smaller, https://doi.org/10.3133/ofr78140.","productDescription":"Report: 43 p.; 6 Plates: 11.32 × 57.82 inches or smaller","costCenters":[],"links":[{"id":406869,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74835.htm","linkFileType":{"id":5,"text":"html"}},{"id":38435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38434,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0140/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38433,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0140/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38432,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0140/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38431,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0140/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38430,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0140/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38429,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0140/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"south Florida basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86,\n              24.5\n            ],\n            [\n              -80,\n              24.5\n            ],\n            [\n              -80,\n              28\n            ],\n            [\n              -86,\n              28\n            ],\n            [\n              -86,\n              24.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640834","contributors":{"authors":[{"text":"Palacas, James George","contributorId":72791,"corporation":false,"usgs":true,"family":"Palacas","given":"James","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":161656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","interactions":[{"subject":{"id":10803,"text":"ofr77565 - 1977 - Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","indexId":"ofr77565","publicationYear":"1977","noYear":false,"title":"Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region"},"predicate":"SUPERSEDED_BY","object":{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","indexId":"pp813K","publicationYear":"1978","noYear":false,"chapter":"K","title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region"},"id":1}],"lastModifiedDate":"2021-12-14T22:08:19.164288","indexId":"pp813K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"813","chapter":"K","title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","docAbstract":"<p>A broad-perspective analysis of the ground-water resources and present and possible future water development and management in the Souris-Red-Rainy Region is presented. The region includes the basins of the Souris River within Montana and North Dakota; the Red River of the North in South Dakota, North Dakota, and Minnesota; and the Rainy River within Minnesota. The region includes 59,645 square miles, mostly in North Dakota and Minnesota.</p>\n<p>The terrain is relatively flat, but ranges in altitude from 2,541 to 750 feet. Annual average precipitation ranges from 14 inches in the west to 28 inches in the east and about 75 percent of it is rain. The mean annual snowfall ranges from 32 inches in the west to 64 inches in the east. Temperatures range from -55&deg; to 118&deg; F (-48.3&deg; to 47.8&deg; C). Irrigation is needed at least part of the time to assure crop production, particularly in the western part of the region.</p>\n<p>Sand and gravel deposits in the drift form the most important freshwater aquifers. Other aquifers are found in at least parts of the region in the Precambrian, Paleozoic, Cretaceous, and Tertiary rocks. The potentiometric surface in the bedrock aquifers generally decreases in altitude toward the Red River of the North, indicating that the general direction of ground-water movement is toward the river. Ground water with less than 3,000 milligrams per liter dissolved solids is available throughout the region. Ground water with less than 1,000 milligrams per liter occurs in most of the region east of the Red River of the North and in most of the shallow aquifers west of the river. The total volume of water available from storage having less than 3,000 milligrams per liter dissolved solids is estimated to be 5x10<sup>8</sup> acre-feet. In addition to the fresh and slightly saline water, the region has abundant highly mineralized water that can be considered as a resource. Yields of wells in individual bedrock aquifers are generally less than 100 gallons per minute but locally yields may be as much as 500 gallons per minute and more. Yields in drift aquifers are frequently less than 100 gallons per minute but range from 5 to 1,000 gallons per minute. In a few places outwash yields more than 1,000 gallons per minute.</p>\n<p>Ground water is the sole or a primary source of water supply in much of the region, including supplies for irrigation, domestic and livestock, municipal, and industrial needs. Reportedly, the potential irrigation development is 1,550,000 acres, as compared with 50,200 acres in 1975. Both ground- and surface-water supplies would be required to meet these demands. Rural domestic and livestock water supplies are derived almost entirely from ground-water sources. Smaller communities and towns generally rely on ground water, and the cities and industries use ground water, surface water, or both. The municipalities using surface water generally depend upon reservoir storage. Water quality rather than quantity is the greater water-supply problem for many communities in the region.</p>\n<p>Increased demands on both ground-water and surface-water supplies likely will be made in the future. Storage of surface water in the ground-water reservoirs during times of surplus for withdrawal during times of scarcity would aid in meeting these demands. The surplus (flood) water is of better chemical quality than underlying ground water in parts of the western half of the region. Freshwater could be stored in saline- or freshwater aquifers, and pumped out later, as needed. Thus, the ground-water reservoirs have a definite present and potential role in water management.</p>\n<p>To understand the hydrologic system for management purposes there is a need to determine more adequately the geologic and hydrologic characteristics of existing aquifers and the location of new aquifers. Also, as pumping and other stresses on any part of the hydrologic system affect other parts of the system, monitoring programs ideally should be started and maintained to detect changes and determine effects of the stresses.</p>\n<p>Many alternatives are available for managing water in the region. Some of these are operational and others are undergoing research. Adequate hydrologic information is needed to aid in solving problems of water supply, use, and pollution.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813K","usgsCitation":"Reeder, H.O., 1978, Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region: U.S. Geological Survey Professional Paper 813, vi, 25 p., https://doi.org/10.3133/pp813K.","productDescription":"vi, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"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":392905,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5066.htm"},{"id":122128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813k/report-thumb.jpg"},{"id":65552,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813k/report.pdf","text":"Report","size":"8.83 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Minnesota, Montana, North Dakota, South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ],\n            [\n              -95.185546875,\n              49.06666839558117\n            ],\n            [\n              -95.1416015625,\n              49.52520834197442\n            ],\n            [\n              -94.74609375,\n              49.32512199104001\n            ],\n            [\n              -94.482421875,\n              48.864714761802794\n            ],\n            [\n              -93.69140625,\n              48.69096039092549\n            ],\n            [\n              -93.0322265625,\n              48.719961222646276\n            ],\n            [\n              -92.28515625,\n              48.516604348867475\n            ],\n            [\n              -91.845703125,\n              48.40003249610685\n            ],\n            [\n              -91.3623046875,\n              48.19538740833338\n            ],\n            [\n              -90.7470703125,\n              48.28319289548349\n            ],\n            [\n              -89.384765625,\n              48.1367666796927\n            ],\n            [\n              -90,\n              47.724544549099676\n            ],\n            [\n              -91.2744140625,\n              47.15984001304432\n            ],\n            [\n              -92.373046875,\n              46.70973594407157\n            ],\n            [\n              -94.5703125,\n              45.73685954736049\n            ],\n            [\n              -95.712890625,\n              45.398449976304086\n            ],\n            [\n              -97.0751953125,\n              45.30580259943578\n            ],\n            [\n              -98.525390625,\n              45.82879925192134\n            ],\n            [\n              -99.5361328125,\n              46.10370875598026\n            ],\n            [\n              -100.81054687499999,\n              46.89023157359399\n            ],\n            [\n              -101.953125,\n              47.07012182383309\n            ],\n            [\n              -103.3154296875,\n              47.54687159892238\n            ],\n            [\n              -104.150390625,\n              47.84265762816538\n            ],\n            [\n              -105.2490234375,\n              48.3416461723746\n            ],\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6996cc","contributors":{"authors":[{"text":"Reeder, Harold O.","contributorId":14381,"corporation":false,"usgs":true,"family":"Reeder","given":"Harold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":220306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16728,"text":"ofr78842 - 1978 - 1979 water quality laboratory services catalog","interactions":[],"lastModifiedDate":"2018-09-18T19:53:52","indexId":"ofr78842","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-842","title":"1979 water quality laboratory services catalog","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78842","usgsCitation":"1978, 1979 water quality laboratory services catalog: U.S. Geological Survey Open-File Report 78-842, 1 v. (various pagings) ;28 cm.; (499 p. - PGS), https://doi.org/10.3133/ofr78842.","productDescription":"1 v. (various pagings) ;28 cm.; (499 p. - PGS)","costCenters":[],"links":[{"id":147449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4912e4b0b290850eedc1","contributors":{"editors":[{"text":"Friedman, Linda C.","contributorId":98702,"corporation":false,"usgs":true,"family":"Friedman","given":"Linda C.","affiliations":[],"preferred":false,"id":745452,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":38702,"text":"pp813Q - 1978 - Summary appraisals of the nation's ground-water resources – Missouri basin region","interactions":[],"lastModifiedDate":"2021-12-14T21:56:38.395429","indexId":"pp813Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"813","chapter":"Q","title":"Summary appraisals of the nation's ground-water resources – Missouri basin region","docAbstract":"<p>The Missouri Basin Region lies in the north-central part of the United States and southern Canada. It includes parts of Alberta and Saskatchewan in Canada; parts of Montana, Wyoming, North Dakota, South Dakota, Minnesota, Iowa, Colorado, Kansas, and Missouri, and all of Nebraska in the United States. The region includes about one-sixth of the contiguous United States and requires large water supplies for irrigation, industrial, public, and rural uses. Climate ranges from semiarid to subhumid. Normal annual precipitation increases generally eastward in the downstream direction, but precipitation is not a dependable source of supply. The Missouri River and its tributaries furnish water to many users, but surface water is often inadequate to meet large demands. Numerous surface reservoirs help to regulate streamflow and provide storage, but they also allow an increase in evapotranspiration, which in some areas exceeds normal precipitation. Ground water occurs in aquifers classified as alluvial deposits of sand and gravel, glacial deposits, dune-sand deposits, basin-fill deposits of sand and gravel, sandstone, siltstone, fractured sandy clay, limestone, and dolomite. Ground water can be developed and managed in an orderly manner provided adequate geologic and hydrologic data are available to determine aquifer characteristics and response to pumping and other hydraulic stresses. These data and determinations are essential to design, testing, and implementation of water management plans.</p>\n<p>Unconsolidated and semiconsolidated aquifers include valley-fill alluvium, areally extensive alluvium, glacial deposits, and basin-fill deposits. The aquifers normally consist of alluvial sand and gravel that contain unconfined ground water that lies near the land surface. Many wells completed in the alluvial aquifers have high yields of good-quality water because most alluvial aquifers are highly transmissive and hydraulically connected to streams. Aquifers in glacial deposits may be difficult to locate and in some areas contain saline water; nevertheless, these aquifers are sources of water supply for many users. Basin-fill aquifers are as much as several thousand feet thick, and many contain large ground-water supplies. Ground-water mining has occurred in semiconsolidated aquifers because of withdrawals from wells.&nbsp;Unconsolidated and semiconsolidated aquifers have potential for conjunctive use with surface water, recycling to reuse available supplies, artificial recharge, and salvage of evapotranspired water.</p>\n<p>Sandstone aquifers lie near the land surface and in structural basins. Interbasin movement of ground water occurs in the Virgelle (Milk River aquifer), Fox Hills-basal Hell Creek, and Dakota aquifers. Sandstone aquifers are less transmissive than unconsolidated and semiconsolidated aquifers in general. Confined sandstone aquifers are common, and flowing wells are obtained in many areas. However, flowing wells may cause large declines in water levels if uncontrolled. Water quality is variable in sandstone aquifers but is adequate for most needs.&nbsp;Sandstone aquifers have potential for artificial recharge, induced interaquifer leakage, conjunctive use with surface water, and mining of ground water.</p>\n<p>Limestone and dolomite aquifers are extensive in the region, but in some areas they lie deep below the land surface. The occurrence of ground water in small pores, fractures, or large caverns causes yields from wells to range widely. Large flows through cavern systems in the aquifers are indicated by large springs in some areas. Water quality is extremely variable and must be considered in any water-development plan.&nbsp;Limestone and dolomite aquifers have potential for development of large water supplies in some areas. The development may be aided by induced recharge and interaquifer leakage.</p>\n<p>Saline ground water occurs throughout the Missouri Basin Region. Dissolved-solids concentration as much as 30,000 milligrams per liter has been measured in aquifers in glacial deposits in Montana. Saline water is common in sandstone aquifers in Wyoming, North Dakota, and South Dakota; maximum reported concentration is 280,000 milligrams per liter in water from the Tensleep Sandstone in Wyoming. Limestone contains saline water in many areas; maximum dissolved-solids concentration is about 350,000 milligrams per liter for the Madison Group in the Williston Basin in North Dakota.</p>\n<p>Comprehensive water-management planning in the Missouri Basin Region will require periodic or continuing inventory of precipitation, streamflow, surface-water storage, and ground water. Water demands for irrigation, industrial, public supply, and rural use are increasing rapidly. Reliance on ground-water supplies is increasing even though in many areas the ground water is still mostly undeveloped. Optimal use of water supplies will require the establishment of realistic goals and carefully conceived water-management plans, each of which will necessarily be based on an adequate baseline of hydrologic data and knowledge of the highly variable hydrologic systems in the region.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813Q","usgsCitation":"Taylor, O., 1978, Summary appraisals of the nation's ground-water resources – Missouri basin region: U.S. Geological Survey Professional Paper 813, Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller, https://doi.org/10.3133/pp813Q.","productDescription":"Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","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":392897,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5071.htm"},{"id":123063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813q/report-thumb.jpg"},{"id":65559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813q/report.pdf","text":"Report","size":"15.58 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":65558,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813q/plate-3.pdf","text":"Plate 3","size":"7.46 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":65557,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813q/plate-2.pdf","text":"Plate 2","size":"7.25 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 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,{"id":20762,"text":"ofr78176 - 1978 - Recent and projected changes in Dead Sea level and effects on mineral production from the sea","interactions":[],"lastModifiedDate":"2022-09-23T20:25:47.485204","indexId":"ofr78176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-176","title":"Recent and projected changes in Dead Sea level and effects on mineral production from the sea","docAbstract":"<p>Hydrologic data for the Dead Sea area were reviewed to assess the probable magnitude and rate of change of the water level of the Dead Sea. Historical average annual Dead Sea levels range from a minimum of 399.4 meters below sea level in about 1818 to a maximum of 388.6 meters below in 1896. Present levels are rapidly approaching the historical low. There is a close correlation between Dead Sea level and accumulated departure from the mean of long-term rainfall except for the most recent period since 1964. During that period rainfall has been near the long-term average but water levels have continued to decline, in part due to abstractions for irrigation in the Jordan River basin.</p><p>The dissolved-solids concentration of Dead Sea water presently is approximately 322,000 milligrams per liter and is generally well mixed throughout. This concentration is at the saturation level, resulting in continuous precipitation of some salts. The increase in dissolved solids to the present high concentration has resulted in an evaporation rate less than that estimated in previous reports. Evaporation rate from the North Basin is estimated at 1,310 millimeters per year at present. The evaporation rate from the South Basin was not estimated due to extensive existing or planned modifications for mineral production facilities.</p><p>Water budget computations were performed at various inflow rates in order to project water-level changes for 50 years. Computations assumed closure of the South Basin by existing and proposed mineral extraction facilities. The projected 50-year changes ranged from a decline of 51 meters with no inflow from any sources to a rise of 10.2 meters when average annual inflow from the Jordan River was 750 cubic hectometers. An average annual inflow to the Sea of 900 cubic hectometers from all sources is required to stabilize the Sea at the present level. Principal impact of declining water levels on proposed potash production facilities in Jordan would be an increase in power requirements.</p><p>A cursory review of a proposed plan to divert water from the Mediterranean Sea into the Dead Sea to generate electric power and stabilize water levels indicates a very limited impact on chemical, physical, and ecological characteristics of the Dead Sea in the near future. Water-budget computations indicate that if all but 200 cubic hectometers of tributaries' waters were utilized for irrigation and other purposes, a maximum diversion of 700 cubic hectometers per year into the Dead Sea would be possible without significantly raising long-term average water levels.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78176","collaboration":"Prepared in cooperation with the U.S. Agency for International Development","usgsCitation":"Sauer, S.P., 1978, Recent and projected changes in Dead Sea level and effects on mineral production from the sea: U.S. Geological Survey Open-File Report 78-176, iv, 43 p., https://doi.org/10.3133/ofr78176.","productDescription":"iv, 43 p.","costCenters":[],"links":[{"id":407296,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0176/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0176/report-thumb.jpg"}],"country":"Israel, Jordan, West Bank","otherGeospatial":"Dead Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              35.36773681640625,\n              30.954057859276126\n            ],\n            [\n              35.6011962890625,\n              30.954057859276126\n            ],\n            [\n              35.6011962890625,\n              31.826231907142883\n            ],\n            [\n              35.36773681640625,\n              31.826231907142883\n            ],\n            [\n              35.36773681640625,\n              30.954057859276126\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485a7","contributors":{"authors":[{"text":"Sauer, Stanley P.","contributorId":38966,"corporation":false,"usgs":true,"family":"Sauer","given":"Stanley","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":183201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39570,"text":"pp712D - 1978 - Hydrologic processes and radionuclide distribution in a cavity and chimney produced by the Cannikin nuclear explosion, Amchitka Island, Alaska","interactions":[],"lastModifiedDate":"2025-04-15T20:26:16.195733","indexId":"pp712D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"712","chapter":"D","title":"Hydrologic processes and radionuclide distribution in a cavity and chimney produced by the Cannikin nuclear explosion, Amchitka Island, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp712D","usgsCitation":"Claassen, H., 1978, Hydrologic processes and radionuclide distribution in a cavity and chimney produced by the Cannikin nuclear explosion, Amchitka Island, Alaska: U.S. Geological Survey Professional Paper 712, Report: 27 p.; 1 Plate: 34.50 x 22.50 inches, https://doi.org/10.3133/pp712D.","productDescription":"Report: 27 p.; 1 Plate: 34.50 x 22.50 inches","costCenters":[],"links":[{"id":484616,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_113900.htm","linkFileType":{"id":5,"text":"html"}},{"id":67152,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0712d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67151,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0712d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122231,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0712d/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              179.25275267331563,\n              51.33956315534962\n            ],\n            [\n              179.49112175917583,\n              51.36223420066128\n            ],\n            [\n              179.39553212575987,\n              51.421126430176\n            ],\n            [\n              178.84982421853886,\n              51.64392567497552\n            ],\n            [\n              178.6150851187565,\n              51.677701728838\n            ],\n            [\n              178.59814518372121,\n              51.63266139516509\n            ],\n            [\n              178.76996452479904,\n              51.5620081900241\n            ],\n            [\n              179.2261327754033,\n              51.341074907368835\n            ],\n            [\n              179.25275267331563,\n              51.33956315534962\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056d6","contributors":{"authors":[{"text":"Claassen, H.C.","contributorId":74028,"corporation":false,"usgs":true,"family":"Claassen","given":"H.C.","affiliations":[],"preferred":false,"id":221686,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10056,"text":"ofr78125 - 1978 - A laboratory control system using the PDP 1103 microprocessor","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr78125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-125","title":"A laboratory control system using the PDP 1103 microprocessor","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78125","usgsCitation":"Lockner, D.A., Weeks, J.D., and Byerlee, J., 1978, A laboratory control system using the PDP 1103 microprocessor: U.S. Geological Survey Open-File Report 78-125, 18, [19] leaves :ill. ;28 cm.; (32 p. - PGS), https://doi.org/10.3133/ofr78125.","productDescription":"18, [19] leaves :ill. ;28 cm.; (32 p. - PGS)","costCenters":[],"links":[{"id":144406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0125/report-thumb.jpg"},{"id":37905,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3e8","contributors":{"authors":[{"text":"Lockner, David A. 0000-0001-8630-6833 dlockner@usgs.gov","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":567,"corporation":false,"usgs":true,"family":"Lockner","given":"David","email":"dlockner@usgs.gov","middleInitial":"A.","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":160741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weeks, John D.","contributorId":104067,"corporation":false,"usgs":true,"family":"Weeks","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":160742,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10003,"text":"ofr78438 - 1978 - Selected data from thermal-spring areas, southwestern Montana","interactions":[],"lastModifiedDate":"2023-02-14T22:44:26.668776","indexId":"ofr78438","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-438","title":"Selected data from thermal-spring areas, southwestern Montana","docAbstract":"<p>During 1975-77 the Montana district of the U.S. Geological Survey collected and assembled data describing the flow, temperature, and chemical characteristics of thermal and related waters. The work was part of an assessment of the geothermal resources of southwestern Montana, excluding Yellowstone Park. The purpose of this report is to present representative data from 24 thermal springs and 3 deep wells where water temperatures exceed 38°C (100°F).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78438","usgsCitation":"Leonard, R., Brosten, T.M., and Midtlyng, N.A., 1978, Selected data from thermal-spring areas, southwestern Montana: U.S. Geological Survey Open-File Report 78-438, v, 71 p., https://doi.org/10.3133/ofr78438.","productDescription":"v, 71 p.","costCenters":[],"links":[{"id":413059,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0438/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142581,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0438/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"southwestern Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.5305701130645,\n              46.95115677390058\n            ],\n            [\n              -114.5305701130645,\n              44.45354114928685\n            ],\n            [\n              -110.43088341514704,\n              44.45354114928685\n            ],\n            [\n              -110.43088341514704,\n              46.95115677390058\n            ],\n            [\n              -114.5305701130645,\n              46.95115677390058\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2f2b","contributors":{"authors":[{"text":"Leonard, Robert B.","contributorId":14407,"corporation":false,"usgs":true,"family":"Leonard","given":"Robert B.","affiliations":[],"preferred":false,"id":160657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brosten, Tordis M.","contributorId":72790,"corporation":false,"usgs":true,"family":"Brosten","given":"Tordis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Midtlyng, Norman A. nmidtlyn@usgs.gov","contributorId":4442,"corporation":false,"usgs":true,"family":"Midtlyng","given":"Norman","email":"nmidtlyn@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":160656,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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