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,{"id":66549,"text":"i419 - 1965 - Geology of the Elkmont quadrangle, Alabama-Tennessee","interactions":[],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i419","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"419","subseriesTitle":"NONE","title":"Geology of the Elkmont quadrangle, Alabama-Tennessee","language":"ENGLISH","doi":"10.3133/i419","usgsCitation":"McMaster, W., 1965, Geology of the Elkmont quadrangle, Alabama-Tennessee: U.S. Geological Survey IMAP 419, 1 map., https://doi.org/10.3133/i419.","productDescription":"1 map.","costCenters":[],"links":[{"id":102904,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1371.htm","linkFileType":{"id":5,"text":"html"},"description":"1371"},{"id":188559,"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\": [ [ [ -87,34.8675 ], [ -87,35 ], [ -86.86749999999999,35 ], [ -86.86749999999999,34.8675 ], [ -87,34.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db68077b","contributors":{"authors":[{"text":"McMaster, W.M.","contributorId":89227,"corporation":false,"usgs":true,"family":"McMaster","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":274703,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52493,"text":"ofr65130 - 1965 - Floods of December 1964 in Redwood areas of north coastal California","interactions":[],"lastModifiedDate":"2025-07-01T15:16:07.355746","indexId":"ofr65130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-130","title":"Floods of December 1964 in Redwood areas of north coastal California","docAbstract":"<p>The flood of December 1964 in the redwood areas of north coastal California was the most damaging in the history of the area. The flood resulted from a series of storms in late December, but primarily from the warm torrential rainfall of December 21-23. This rainfall reflected the combined effect of moist unstable airmasses, strong west-southwest winds, and mountain ranges oriented nearly at right angles to the flow of air. The magnitude of the rainfall over much of the mountainous area was equal to or greater than that estimated to have an average return period of 100 years. Precipitation totals in excess of 10 inches in 24 hours and 15 inches in 48 hours were commonplace in the mountains and interior valleys. The peak discharge of streams draining these drenched areas was extremely high and also had a return period estimated to be greater than 100 years. By contrast, some of the areas immediately adjacent to the Pacific Ocean had maximum 24-hour rainfalls of only 2 inches and the small streams draining these low-altitude basins experienced rises that were little greater than those that occur during the usual winter storms.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65130","usgsCitation":"Rantz, S., 1965, Floods of December 1964 in Redwood areas of north coastal California: U.S. Geological Survey Open-File Report 65-130, 39 p., https://doi.org/10.3133/ofr65130.","productDescription":"39 p.","costCenters":[],"links":[{"id":491599,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0130/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179423,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0130/report-thumb.jpg"}],"country":"United 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,{"id":52472,"text":"ofr6578 - 1965 - Low-flow summary at stream-gaging stations on Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:11:23","indexId":"ofr6578","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-78","title":"Low-flow summary at stream-gaging stations on Long Island, New York","language":"ENGLISH","doi":"10.3133/ofr6578","usgsCitation":"Hunt, O.P., 1965, Low-flow summary at stream-gaging stations on Long Island, New York: U.S. Geological Survey Open-File Report 65-78, 20 p., https://doi.org/10.3133/ofr6578.","productDescription":"20 p.","costCenters":[],"links":[{"id":179269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6487d8","contributors":{"authors":[{"text":"Hunt, O. P.","contributorId":69116,"corporation":false,"usgs":true,"family":"Hunt","given":"O.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":245397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39026,"text":"pp392A - 1965 - Stratigraphy of the Pierre Shale, Valley City and Pembina Mountain areas, North Dakota","interactions":[{"subject":{"id":39026,"text":"pp392A - 1965 - Stratigraphy of the Pierre Shale, Valley City and Pembina Mountain areas, North Dakota","indexId":"pp392A","publicationYear":"1965","noYear":false,"chapter":"A","title":"Stratigraphy of the Pierre Shale, Valley City and Pembina Mountain areas, North Dakota"},"predicate":"IS_PART_OF","object":{"id":5635,"text":"pp392 - 1976 - Studies of the Pierre Shale in the Northern Great Plains","indexId":"pp392","publicationYear":"1976","noYear":false,"title":"Studies of the Pierre Shale in the Northern Great Plains"},"id":1}],"isPartOf":{"id":5635,"text":"pp392 - 1976 - Studies of the Pierre Shale in the Northern Great Plains","indexId":"pp392","publicationYear":"1976","noYear":false,"title":"Studies of the Pierre Shale in the Northern Great Plains"},"lastModifiedDate":"2017-08-09T14:34:55","indexId":"pp392A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"392","chapter":"A","title":"Stratigraphy of the Pierre Shale, Valley City and Pembina Mountain areas, North Dakota","language":"ENGLISH","doi":"10.3133/pp392A","usgsCitation":"Gill, J.R., and Cobban, W.A., 1965, Stratigraphy of the Pierre Shale, Valley City and Pembina Mountain areas, North Dakota: U.S. Geological Survey Professional Paper 392, p. A1-A20, https://doi.org/10.3133/pp392A.","productDescription":"p. A1-A20","costCenters":[],"links":[{"id":66168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0392a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126717,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0392a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5fc1","contributors":{"authors":[{"text":"Gill, J. R.","contributorId":8125,"corporation":false,"usgs":true,"family":"Gill","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":220823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobban, W. A.","contributorId":21577,"corporation":false,"usgs":true,"family":"Cobban","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":220824,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34085,"text":"b1221A - 1965 - Rockfalls and Avalanches from Little Tahoma Peak on Mount Rainier, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"b1221A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1221","chapter":"A","title":"Rockfalls and Avalanches from Little Tahoma Peak on Mount Rainier, Washington","docAbstract":"In December 1963 rockfalls from Little Tahoma Peak on the east side of Mount Rainier volcano fell onto Emmons Glacier and formed avalanches of rock debris that traveled about 4 miles down the glacier and the White River valley. In this distance, the rock debris descended as much as 6,200 feet in altitude. Minor lithologic differences and crosscutting relations indicate that the rockfalls caused at least seven separate avalanches, having an estimated total volume of 14 million cubic yards. The initial rockfall may have been caused by a small steam explosion near the base of Little Tahoma Peak.\r\n\r\nDuring movement, some of the avalanches were deflected from one side of the valley to the other. Calculations based on the height to which the avalanches rose on the valley walls suggest that their velocity reached at least 80 or 90 miles per hour. The unusually long distance some of the avalanches were transported is attributed to a cushion of trapped and compressed air at their base, which buoyed them up amid reduced friction.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/b1221A","usgsCitation":"Crandell, D.R., and Fahnestock, R.K., 1965, Rockfalls and Avalanches from Little Tahoma Peak on Mount Rainier, Washington: U.S. Geological Survey Bulletin 1221, p. A1-A30, https://doi.org/10.3133/b1221A.","productDescription":"p. A1-A30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":96251,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1221a/report.pdf","size":"5958","linkFileType":{"id":1,"text":"pdf"}},{"id":163980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1221a/report-thumb.jpg"},{"id":12498,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/bul/1221-A/index.htm","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.83333333333333,46.75 ], [ -121.83333333333333,46.916666666666664 ], [ -121.58333333333333,46.916666666666664 ], [ -121.58333333333333,46.75 ], [ -121.83333333333333,46.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe45d","contributors":{"authors":[{"text":"Crandell, Dwight Raymond","contributorId":6440,"corporation":false,"usgs":true,"family":"Crandell","given":"Dwight","email":"","middleInitial":"Raymond","affiliations":[],"preferred":false,"id":212434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fahnestock, Robert K.","contributorId":100381,"corporation":false,"usgs":true,"family":"Fahnestock","given":"Robert","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":212435,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52444,"text":"ofr6521 - 1965 - Hydrologic effects of ground-water pumping in northwest Hillsborough County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:11:29","indexId":"ofr6521","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-21","title":"Hydrologic effects of ground-water pumping in northwest Hillsborough County, Florida","language":"ENGLISH","doi":"10.3133/ofr6521","usgsCitation":"Bredehoeft, J., Papadopulos, I., and Stewart, J.W., 1965, Hydrologic effects of ground-water pumping in northwest Hillsborough County, Florida: U.S. Geological Survey Open-File Report 65-21, 23 p., https://doi.org/10.3133/ofr6521.","productDescription":"23 p.","costCenters":[],"links":[{"id":178984,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606f8f","contributors":{"authors":[{"text":"Bredehoeft, J.D.","contributorId":12836,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"J.D.","affiliations":[],"preferred":false,"id":245352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Papadopulos, I.S.","contributorId":37379,"corporation":false,"usgs":true,"family":"Papadopulos","given":"I.S.","email":"","affiliations":[],"preferred":false,"id":245353,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stewart, J. W.","contributorId":72774,"corporation":false,"usgs":true,"family":"Stewart","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":245354,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66747,"text":"i413 - 1965 - Geologic map of the crystalline rocks of South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:13:30","indexId":"i413","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"413","subseriesTitle":"NONE","title":"Geologic map of the crystalline rocks of South Carolina","language":"ENGLISH","doi":"10.3133/i413","usgsCitation":"Overstreet, W., and Bell, H., 1965, Geologic map of the crystalline rocks of South Carolina: U.S. Geological Survey IMAP 413, 1 map :col. ;92 x 138 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i413.","productDescription":"1 map :col. ;92 x 138 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":108295,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12969.htm","linkFileType":{"id":5,"text":"html"},"description":"12969"},{"id":188587,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b5b","contributors":{"authors":[{"text":"Overstreet, W.C.","contributorId":105294,"corporation":false,"usgs":true,"family":"Overstreet","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":275010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, Henry III","contributorId":37710,"corporation":false,"usgs":true,"family":"Bell","given":"Henry","suffix":"III","email":"","affiliations":[],"preferred":false,"id":275009,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34936,"text":"b1199J - 1965 - Bauxite and Kaolin Deposits of the Irwinton district, Georgia","interactions":[{"subject":{"id":55287,"text":"ofr4478 - 1944 - Kaolin deposits of Twiggs, Washington, and Wilkinson Counties, Georgia","indexId":"ofr4478","publicationYear":"1944","noYear":false,"title":"Kaolin deposits of Twiggs, Washington, and Wilkinson Counties, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":34936,"text":"b1199J - 1965 - Bauxite and Kaolin Deposits of the Irwinton district, Georgia","indexId":"b1199J","publicationYear":"1965","noYear":false,"chapter":"J","title":"Bauxite and Kaolin Deposits of the Irwinton district, Georgia"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"b1199J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1199","chapter":"J","title":"Bauxite and Kaolin Deposits of the Irwinton district, Georgia","docAbstract":"The Irwinton district is in the central part of Georgia at the inner margin \r\nof the Coastal Plain province. The oldest rocks exposed in the district are \r\ncrystalline rocks of the Piedmont province. They are unconformably overlain \r\nby nonmarine sedimentary strata of Late Cretaceous age, including gravel, \r\nmicaceous sand, and lenses of kaolin.\r\n\r\nBauxite has been found in a few of the kaolin lenses near the top of the \r\nsequence of these strata. During a long period prior to deposition of the over- \r\nlying marine beds of the Claiborne and Jackson Groups (middle and upper \r\nEocene), the Upper Cretaceous strata were subjected to subaerial erosion. \r\nThe bauxite deposits are considered to have formed during this period. They \r\nrange in thickness from a few inches to more than 10 feet and occupy areas \r\nranging from a few square feet to more than 5 acres. Most of the known \r\nbauxite deposits lie along the valleys of Commissioners Creek and Big Sandy \r\nCreek in Wilkinson County. The kaolin lenses are much larger than the \r\nbauxite deposits; some of the lenses underlie more than 200 acres and are \r\nmore than 20 feet thick.\r\n\r\nBauxite was discovered in the district in 1907 and was mined from 1910 to \r\n1928. A few additional carloads of ore were shipped in 1941 and 1942, but \r\nno ore has been mined since that time. Reserves of high-grade bauxite are \r\nvery small. Reserves of all grades of bauxite plus bauxitic clay may be about \r\n400,000 long tons.\r\n\r\nThe Irwinton district is the principal source of high-grade kaolin in the \r\nUnited States. The presence of kaolin here has been known since early colo- \r\nnial time, and it has been mined continuously since 1897. Production in 1959 \r\nwas 1,940,279 short tons. The reserves of kaolin are very large but have never \r\nbeen adequately measured. Reserves of first and second grade kaolin may be \r\n67 to 84 million short tons. Kaolin of lower grade is present in larger quantity.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Distribution, occurrence, and resources of bauxite and kaolin","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/b1199J","usgsCitation":"Lang, W., Warren, W., Thompson, R.M., and Overstreet, E.F., 1965, Bauxite and Kaolin Deposits of the Irwinton district, Georgia: U.S. Geological Survey Bulletin 1199, p. J1-J26, ill., map (1 fold. col.in pocket) ;24 cm., https://doi.org/10.3133/b1199J.","productDescription":"p. J1-J26, ill., map (1 fold. col.in pocket) ;24 cm.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":162961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1199j/report-thumb.jpg"},{"id":62889,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62890,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1199j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.58333333333333,32.666666666666664 ], [ -83.58333333333333,33.083333333333336 ], [ -82.83333333333333,33.083333333333336 ], [ -82.83333333333333,32.666666666666664 ], [ -83.58333333333333,32.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e14b","contributors":{"authors":[{"text":"Lang, Walter B.","contributorId":27507,"corporation":false,"usgs":true,"family":"Lang","given":"Walter B.","affiliations":[],"preferred":false,"id":213837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warren, Walter C.","contributorId":18425,"corporation":false,"usgs":true,"family":"Warren","given":"Walter C.","affiliations":[],"preferred":false,"id":213836,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, Raymond M.","contributorId":82760,"corporation":false,"usgs":true,"family":"Thompson","given":"Raymond","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":213839,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Overstreet, Elizabeth F.","contributorId":67942,"corporation":false,"usgs":true,"family":"Overstreet","given":"Elizabeth","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":213838,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":62711,"text":"gq376 - 1965 - Geology of the Honey Grove quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:47","indexId":"gq376","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"376","title":"Geology of the Honey Grove quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq376","usgsCitation":"Klemic, H., 1965, Geology of the Honey Grove quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 376, 1 map :col. ;c72 x 86 cm., https://doi.org/10.3133/gq376.","productDescription":"1 map :col. ;c72 x 86 cm.","costCenters":[],"links":[{"id":102390,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_839.htm","linkFileType":{"id":5,"text":"html"},"description":"839"},{"id":248867,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0376/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":254343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0376/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.36749999999999,36.8675 ], [ -87.36749999999999,37 ], [ -87.25,37 ], [ -87.25,36.8675 ], [ -87.36749999999999,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67ff38","contributors":{"authors":[{"text":"Klemic, Harry","contributorId":49767,"corporation":false,"usgs":true,"family":"Klemic","given":"Harry","email":"","affiliations":[],"preferred":false,"id":267764,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62405,"text":"gq407 - 1965 - Geologic map of the Black Diamond quadrangle, King County, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:41","indexId":"gq407","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"407","title":"Geologic map of the Black Diamond quadrangle, King County, Washington","language":"ENGLISH","doi":"10.3133/gq407","usgsCitation":"Mullineaux, D.R., 1965, Geologic map of the Black Diamond quadrangle, King County, Washington: U.S. Geological Survey Geologic Quadrangle 407, 1 map :col. ;57 x 38 cm., on sheet 79 x 76 cm., folded in envelope 31 x 24 cm., https://doi.org/10.3133/gq407.","productDescription":"1 map :col. ;57 x 38 cm., on sheet 79 x 76 cm., folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":102425,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_874.htm","linkFileType":{"id":5,"text":"html"},"description":"874"},{"id":180549,"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\": [ [ [ -122.11749999999999,47.25 ], [ -122.11749999999999,47.3675 ], [ -122,47.3675 ], [ -122,47.25 ], [ -122.11749999999999,47.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0de4b07f02db69f1e1","contributors":{"authors":[{"text":"Mullineaux, Donal Ray","contributorId":31759,"corporation":false,"usgs":true,"family":"Mullineaux","given":"Donal","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":267340,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":34847,"text":"b1201A - 1965 - Petrography of evaporites from the Wellington Formation near Hutchinson, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:29","indexId":"b1201A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1201","chapter":"A","title":"Petrography of evaporites from the Wellington Formation near Hutchinson, Kansas","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1201A","usgsCitation":"Jones, C., 1965, Petrography of evaporites from the Wellington Formation near Hutchinson, Kansas: U.S. Geological Survey Bulletin 1201, p. A1-A70, ill., map, diagrs. ;24 cm., https://doi.org/10.3133/b1201A.","productDescription":"p. A1-A70, ill., map, diagrs. ;24 cm.","costCenters":[],"links":[{"id":167633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1201a/report-thumb.jpg"},{"id":62804,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1201a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62805,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1201a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fa6","contributors":{"authors":[{"text":"Jones, C.L.","contributorId":60218,"corporation":false,"usgs":true,"family":"Jones","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":213686,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":42540,"text":"ofr652 - 1965 - Preliminary geologic map of the Poker Peak and Palisades Reservoir quadrangles, Bonneville County, Idaho, and Lincoln County, Wyoming","interactions":[],"lastModifiedDate":"2022-12-28T20:15:15.825011","indexId":"ofr652","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-2","title":"Preliminary geologic map of the Poker Peak and Palisades Reservoir quadrangles, Bonneville County, Idaho, and Lincoln County, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr652","usgsCitation":"Albee, H., and Cullins, H.L., 1965, Preliminary geologic map of the Poker Peak and Palisades Reservoir quadrangles, Bonneville County, Idaho, and Lincoln County, Wyoming: U.S. Geological Survey Open-File Report 65-2, 1 Plate: 47.20 x 31.86 inches, https://doi.org/10.3133/ofr652.","productDescription":"1 Plate: 47.20 x 31.86 inches","costCenters":[],"links":[{"id":106358,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8100.htm","linkFileType":{"id":5,"text":"html"},"description":"8100"},{"id":80315,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175636,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Idaho, Wyoming","county":"Bonneville County, Lincoln County","otherGeospatial":"Poker Peak and Palisades Reservoir quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111,\n              43.25\n            ],\n            [\n              -111.25,\n              43.25\n            ],\n            [\n              -111.25,\n              43.125\n            ],\n            [\n              -111,\n              43.125\n            ],\n            [\n              -111,\n              43.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ada4","contributors":{"authors":[{"text":"Albee, Howard F.","contributorId":64252,"corporation":false,"usgs":true,"family":"Albee","given":"Howard F.","affiliations":[],"preferred":false,"id":226678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cullins, Henry L.","contributorId":23149,"corporation":false,"usgs":true,"family":"Cullins","given":"Henry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":226677,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1196,"text":"wsp1759D - 1965 - Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota","interactions":[{"subject":{"id":52312,"text":"ofr6320 - 1963 - Water resources in the vicinity of municipalities on the Central Mesabi Iron Range, northeastern Minnesota","indexId":"ofr6320","publicationYear":"1963","noYear":false,"title":"Water resources in the vicinity of municipalities on the Central Mesabi Iron Range, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1196,"text":"wsp1759D - 1965 - Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota","indexId":"wsp1759D","publicationYear":"1965","noYear":false,"chapter":"D","title":"Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2018-03-05T12:35:10","indexId":"wsp1759D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1759","chapter":"D","title":"Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota","docAbstract":"<p>Additional supplies of water are available near the municipalities on the central Mesabi Iron Range. Ground water presents the greatest potential yield, and most of the productive aquifers are in the Biwabik Iron-Formation and the stratified glacial drift. /k single body of ice-contact stratified drift underlies parts of all but one of the five municipality areas mapped. Surface-water supplies are generally inadequate. The Two River system in the eastern part of the area of this report offers some possibilities. Flow data from one discharge station and one miscellaneous gaging site are presented.</p>\n<p>Analyses of water from many sources are presented as are data from many wells and test holes. Ground water commonly has a concentration of high iron and manganese and is hard. Surface water generally has a high concentration of iron and is colored.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/wsp1759D","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Cotter, R.D., Young, H.L., Petri, L.R., and Prior, C.H., 1965, Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 1759, Document: iv, 20 p.; Plate: 28.5 x 29.5 inches, https://doi.org/10.3133/wsp1759D.","productDescription":"Document: iv, 20 p.; Plate: 28.5 x 29.5 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":137955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1759d/report-thumb.jpg"},{"id":26066,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1759d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26067,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1759d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.925,\n              47.516667\n            ],\n            [\n              -92.925,\n              47.452778\n            ],\n            [\n              -92.833333,\n              47.452778\n            ],\n            [\n              -92.833333,\n              47.425\n            ],\n            [\n              -92.741667,\n              47.425\n            ],\n            [\n              -92.741667,\n              47.46\n            ],\n            [\n              -92.675,\n              47.46\n            ],\n            [\n              -92.675,\n              47.383333\n            ],\n            [\n              -92.583333,\n              47.383333\n            ],\n            [\n              -92.583333,\n              47.566667\n            ],\n            [\n              -92.675,\n              47.566667\n            ],\n            [\n              -92.675,\n              47.53\n            ],\n            [\n              -92.741667,\n              47.53\n            ],\n            [\n              -92.741667,\n              47.516667\n            ],\n            [\n              -92.925,\n              47.516667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025b6","contributors":{"authors":[{"text":"Cotter, R. 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,{"id":1195,"text":"wsp1759B - 1965 - Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota","interactions":[{"subject":{"id":52316,"text":"ofr6324 - 1963 - Water resources in the vicinity of municipalities on the Western Mesabi Iron Range, northeastern Minnesota","indexId":"ofr6324","publicationYear":"1963","noYear":false,"title":"Water resources in the vicinity of municipalities on the Western Mesabi Iron Range, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1195,"text":"wsp1759B - 1965 - Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota","indexId":"wsp1759B","publicationYear":"1965","noYear":false,"chapter":"B","title":"Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2016-05-06T10:48:02","indexId":"wsp1759B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1759","chapter":"B","title":"Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota","docAbstract":"<p>Additional supplies of water are available near the municipalities on the western Mesabi Iron Range. Potential yields from both ground-water and surface-water sources are good. The most productive aquifers for ground-water supplies are the Biwabik Iron-Formation and the stratified glacial drift. Areas of stratified drift believed to have good water potential have been outlined. The most abundant surface-water supplies in the area of this report are from the Mississippi River and its tributaries.</p>\n<p>The ground water is generally hard and has a high concentration of iron and manganese. The surface water is generally high in iron and is colored. Analyses of water from many sources are included.</p>\n<p>Data from many wells and test holes are given as are flow data for two discharge stations.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1759B","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Cotter, R.D., Young, H.L., Petri, L.R., and Prior, C.H., 1965, Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 1759, Document: iv, 24 p.; Plate: 23 x 23 inches, https://doi.org/10.3133/wsp1759B.","productDescription":"Document: iv, 24 p.; Plate: 23 x 23 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":137954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1759b/report-thumb.jpg"},{"id":26064,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1759b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1759b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.591667,\n              47.279167\n            ],\n            [\n              -93.591667,\n              47.175\n            ],\n            [\n              -93.5,\n              47.175\n            ],\n            [\n              -93.5,\n              47.279167\n            ],\n            [\n              -93.591667,\n              47.279167\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.45,\n              47.341667\n            ],\n            [\n              -93.358333,\n              47.341667\n            ],\n            [\n              -93.358333,\n              47.33333333\n            ],\n            [\n              -93.216667,\n              47.33333333\n            ],\n            [\n              -93.216667,\n              47.275\n            ],\n            [\n              -93.358333,\n              47.275\n            ],\n            [\n              -93.358333,\n              47.25\n            ],\n            [\n              -93.45,\n              47.25\n            ],\n            [\n              -93.45,\n              47.341667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648597","contributors":{"authors":[{"text":"Cotter, R. 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,{"id":1193,"text":"wsp1759F - 1965 - Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","interactions":[{"subject":{"id":52314,"text":"ofr6322 - 1963 - Water resources in the vicinity of municipalities on the Eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","indexId":"ofr6322","publicationYear":"1963","noYear":false,"title":"Water resources in the vicinity of municipalities on the Eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1193,"text":"wsp1759F - 1965 - Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","indexId":"wsp1759F","publicationYear":"1965","noYear":false,"chapter":"F","title":"Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2021-11-02T21:27:50.468028","indexId":"wsp1759F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1759","chapter":"F","title":"Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","docAbstract":"<p>Additional supplies of water are available near the municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range. On the eastern Mesabi Range the potential for additional development of both ground-water and surface-water supplies are good, and on the Vermilion Range the best potential for development is from surface-water resources.</p>\n<p>The most productive aquifers in the area of this report are the Biwabik Iron-Formation and the stratified glacial drift; Bast of Colby Lake the Biwabik Iron-Formation is not an important aquifer, and it is entirely absent on the Vermilion Range. Also, on the Vermilion Range the glacial drift is generally too thin to yield the quantities of water found on the Mesabi Range.</p>\n<p>Surface-water supplies in the area of this report are good. An extensive network of river systems and many lakes form a large untapped potential supply. Records of flow from eight gaging stations are presented as are data from many wells and test holes.</p>\n<p>Ground water commonly has a high concentration of iron and manganese and is hard. Surface water generally has a high concentration of iron and is colored. Analyses of water from many sources are included.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water resources of the Mesabi and Vermilion Iron Ranges","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1759F","usgsCitation":"Cotter, R.D., Young, H.L., Petri, L.R., and Prior, C.H., 1965, Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 1759, Report: iv, 27 p.; 1 Plate: 31.18 x 23.60 inches, https://doi.org/10.3133/wsp1759F.","productDescription":"Report: iv, 27 p.; 1 Plate: 31.18 x 23.60 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":137952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1759f/report-thumb.jpg"},{"id":26061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1759f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":278838,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1759f/plate-1.pdf"},{"id":391292,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24938.htm"}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.62548828125,\n              47.09630525444073\n            ],\n            [\n              -91.99676513671875,\n              47.09630525444073\n            ],\n            [\n              -91.99676513671875,\n              47.945786463687185\n            ],\n            [\n              -93.62548828125,\n              47.945786463687185\n            ],\n            [\n              -93.62548828125,\n              47.09630525444073\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f08d4","contributors":{"authors":[{"text":"Cotter, R. 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