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B.","contributorId":50867,"corporation":false,"usgs":true,"family":"Goodrich","given":"H.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":231382,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":45288,"text":"b900H - 1941 - Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 8, Parts of township 20 north, ranges 9 and 10 east, and township 21 north, ranges 8 and 9 east and all of township 21 north, range 10 east","interactions":[{"subject":{"id":45288,"text":"b900H - 1941 - Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 8, Parts of township 20 north, ranges 9 and 10 east, and township 21 north, ranges 8 and 9 east and all of township 21 north, range 10 east","indexId":"b900H","publicationYear":"1941","noYear":false,"chapter":"H","title":"Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 8, Parts of township 20 north, ranges 9 and 10 east, and township 21 north, ranges 8 and 9 east and all of township 21 north, range 10 east"},"predicate":"IS_PART_OF","object":{"id":33723,"text":"b900 - 1942 - Subsurface geology and oil and gas resources of Osage county, Oklahoma","indexId":"b900","publicationYear":"1942","noYear":false,"title":"Subsurface geology and oil and gas resources of Osage county, Oklahoma"},"id":1}],"isPartOf":{"id":33723,"text":"b900 - 1942 - Subsurface geology and oil and gas resources of Osage county, Oklahoma","indexId":"b900","publicationYear":"1942","noYear":false,"title":"Subsurface geology and oil and gas resources of Osage county, Oklahoma"},"lastModifiedDate":"2022-04-28T18:50:30.576715","indexId":"b900H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"900","chapter":"H","title":"Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 8, Parts of township 20 north, ranges 9 and 10 east, and township 21 north, ranges 8 and 9 east and all of township 21 north, range 10 east","docAbstract":"The area whose subsurface geology and oil and gas resources are described in this report lies along the southern border of Osage County, Okla., and includes parts of T. 20 N., Rs. 9 and 10 E., and of T. 21 N., Rs. 8 and 9 E., and all of T. 21 N., R. 10 E. The towns of Osage and Prue are within the area; Cleveland, which is a mile south of the Arkansas River, is not far beyond its southwestern limit; and Tulsa is 10 miles east of its southeast corner. The production of oil and gas from the many fields in the five townships began as early as 1905, and drilling has continued up to the present. Oil or gas is produced from 13 zones at depths ranging from 250 to 2,600 feet. Of these zones, one is in the Ordovician system, one is at the contact of the Mississippian and the Pennsylvanian series, and all others are in the Pennsylvanian series. The five townships lie within a region that contains many oil and gas fields in the Bartlesville sand; the Red Fork sand is oil-bearing in a narrow belt in T. 21 N., R. 8 E.; and oil and gas are produced in small areas from the Taneha, Skinner, Squirrel, Cleveland, Jones, and Layton sands, the Mussehem and Peoples sand zone, the Okesa, Torpedo, and Clem Creek sand zone, and the Big lime and Peru sand zone.
The rocks dip westward across the five townships at an average rate of about 38 feet to the mile as measured on the top of the Oswego lime. This regional dip is interrupted, however, by many anticlines, domes, synclines, and structural basins. The subsurface crests of most of the domes and anticlines are not directly under the crests as determined on the exposed rocks, and the dips of the deeper rocks are steeper and the structural closures greater in the buried rocks than in the exposed rocks. The exposed rocks are cut by several faults that trend northwest, but the data are insufficient to determine whether the deeply buried rocks, also, are displaced along the faults.
This investigation has shown that there are a few localities not yet completely tested in this part of Osage County that may produce oil and gas and that a few producing oil fields have areas within or adjacent to them that have not been thoroughly prospected. It is pointed out that yields of oil and gas from limy reservoir rocks may be increased by acid treatment and that additional oil may be produced from some of the reservoir sands by repressuring them with gas or flooding them with water.
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","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Strategic minerals investigations, 1940, part 2: L-T","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b922L","usgsCitation":"Ross, C.P., 1941, Quicksilver deposits of the Mayacmas and Sulphur Bank districts, California, a preliminary report: U.S. Geological Survey Bulletin 922, Report: iii, 27 p.; 3 Plates: 20.51 × 14.78 inches or smaller, https://doi.org/10.3133/b922L.","productDescription":"Report: iii, 27 p.; 3 Plates: 20.51 × 14.78 inches or smaller","costCenters":[],"links":[{"id":109554,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21110.htm","linkFileType":{"id":5,"text":"html"},"description":"21110"},{"id":163146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0922l/report-thumb.jpg"},{"id":97017,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0922l/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":97020,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0922l/plate-53.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":97019,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0922l/plate-52.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":97018,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0922l/plate-50.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Mayacmas and Sulphur Bank districts","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.8830,\n 38.6\n ],\n [\n -122.433,\n 38.6\n ],\n [\n -122.433,\n 39.05\n ],\n [\n -122.8830,\n 39.05\n ],\n [\n -122.8830,\n 38.6\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a112","contributors":{"authors":[{"text":"Ross, Clyde Polhemus","contributorId":71954,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"Polhemus","affiliations":[],"preferred":false,"id":215057,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3182,"text":"wsp866A - 1941 - Geology of dam sites on the upper tributaries of the Columbia river in Idaho and Montana: Part 1. Katka, Tunnel no. 8 and Kootenai Falls dam sites, Kootenai River Idaho and Montana","interactions":[],"lastModifiedDate":"2024-02-01T23:11:46.67183","indexId":"wsp866A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"866","chapter":"A","title":"Geology of dam sites on the upper tributaries of the Columbia river in Idaho and Montana: Part 1. Katka, Tunnel no. 8 and Kootenai Falls dam sites, Kootenai River Idaho and Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp866A","usgsCitation":"Erdmann, C.E., 1941, Geology of dam sites on the upper tributaries of the Columbia river in Idaho and Montana: Part 1. Katka, Tunnel no. 8 and Kootenai Falls dam sites, Kootenai River Idaho and Montana: U.S. Geological Survey Water Supply Paper 866, v, 36 p., https://doi.org/10.3133/wsp866A.","productDescription":"v, 36 p.","costCenters":[],"links":[{"id":30140,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0866a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139031,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0866a/report-thumb.jpg"},{"id":394778,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24664.htm","text":"Katka Dam site","linkFileType":{"id":5,"text":"html"}},{"id":425262,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24665.htm","text":"Kootenai Falls Dam site","linkFileType":{"id":5,"text":"html"}},{"id":425263,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24666.htm","text":"Tunnel No. 8 Dam site","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho","otherGeospatial":"Kootenai River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.129,\n 48.869\n ],\n [\n -116.129,\n 48.596\n ],\n [\n -115.72,\n 48.596\n ],\n [\n -115.72,\n 48.869\n ],\n [\n -116.129,\n 48.869\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68397d","contributors":{"authors":[{"text":"Erdmann, C. E.","contributorId":87122,"corporation":false,"usgs":true,"family":"Erdmann","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2976,"text":"wsp849C - 1941 - Geology and ground-water resources of the Balmorhea area, western Texas","interactions":[],"lastModifiedDate":"2016-08-19T14:48:55","indexId":"wsp849C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"849","chapter":"C","title":"Geology and ground-water resources of the Balmorhea area, western Texas","docAbstract":"Balmorhea is the center of a thriving farming community, the lands of which are irrigated with water derived chiefly from large springs but partly from the storm flow of Toyah Creek. The storm flow of the creek and a part of the winter flow of the springs is stored in a reservoir near Balmorhea and used later to supplement the flow of the springs. The present investigation was made to determine the geologic and hydrologic relations of the springs, whether additional water can be obtained from wells, and what effect the withdrawal of large amounts of water from wells would have upon the discharge of the springs. Balmorhea is situated near the foot of the Davis and Barrilla Mountains and along the southwestern margin of the Toyah Basin. The mountains and adjacent basin are drained by Toyah and Limpia Creeks. The group of springs around Balmorhea occur in the floor of the valley of Toyah Creek. They have been divided into artesian springs--Phantom Lake, Giffin and San Solomon Springs; and gravity springs--Toyah Creek, Saragosa, East Sandia and West Sandia Springs. The combined discharge of the springs during dry years is about 23,000 gallons a minute, of which amount the artesian springs supply more than 90 percent. The underground reservoir which supplies the artesian springs is the fractured and cavernous Lower Cretaceous limestone. This limestone, about 500 feet thick, is underlain by impermeable rocks, probably of Permian age, and is overlain by impermeable Upper Cretaceous strata that have a maximum thickness of about 500 feet. These are in turn overlain in the mountains by Tertiary lava and on the plains by gravel and other surficial deposits. The Lower Cretaceous limestone is at the surface or covered by a thin layer of gravel in a belt that lies athwart the stream channels and extends from Gomez Peak southeastward along the foothills of the Davis Mountains. In this belt all the streams suffer heavy seepage losses. From this belt the limestone dips gently northeastward to the axis of a northwestward-trending syncline and then rises to the surface in the vicinity of Phantom Lake, where a part of the water is discharged. About 1,000 feet northeast of this lake is a northwestward-trending fault of small displacement, on the northeast side of which the limestone is downthrown, northeastward from this fault the limestone rises gently and appears at the surface about a mile to the northeast, where it is again downfaulted, but the throw is not sufficient to affect the movement of the water. For several miles to the north the water-bearing Lower Cretaceous limestone is covered by 400 to 500 feet of impermeable Upper Cretaceous strata. It is believed that the Lower Cretaceous rocks are again near the surface and covered by only a thin mantle of gravel and other surficial deposits at San Solomon and Giffin Springs and that just northeast of the springs a fault crosses the valley along which the impermeable Upper Cretaceous rocks are faulted into a position opposite the Lower Cretaceous rocks, thus obstructing further northward movement of the water in the Lower Cretaceous limestone and forcing it to issue as large springs. Between this fault and Brogada the Lower Cretaceous rocks are believed to lie at a depth of about 500 feet and are overlain by Upper Cretaceous strata and a blanket of gravel and other surficial deposits, which are the source of the water of Toyah Creek, Sandia, and Saragosa Springs. Northeast of Brogada the Lower Cretaceous lies at a greater depth, and the mantle of gravel is much thicker. Wells put down to the limestone in the vicinity of San Solomon and Giffin Springs would decrease the flow of the springs. The effect of wells in limestone between the fault near these springs and the Brogado Hills on the flow of the springs would depend on the completeness with which the fault cuts off northward movement of ground water in the limestone. If the movement of water across the fault has been prev
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp849C","isbn":"pbk","usgsCitation":"White, W.N., Gale, H.S., and Nye, S.S., 1941, Geology and ground-water resources of the Balmorhea area, western Texas: U.S. Geological Survey Water Supply Paper 849, 69 p., https://doi.org/10.3133/wsp849C.","productDescription":"69 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":138908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0849c/report-thumb.jpg"},{"id":29732,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0849c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6857ca","contributors":{"authors":[{"text":"White, Walter N.","contributorId":99124,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":146080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gale, H. S.","contributorId":102040,"corporation":false,"usgs":true,"family":"Gale","given":"H.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":146081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nye, S. Spencer","contributorId":26570,"corporation":false,"usgs":true,"family":"Nye","given":"S.","email":"","middleInitial":"Spencer","affiliations":[],"preferred":false,"id":146079,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":35478,"text":"b921B - 1941 - Geology and oil and coal resources of the region south of Cody, Park County, Wyoming","interactions":[],"lastModifiedDate":"2022-02-02T19:53:13.712051","indexId":"b921B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"921","chapter":"B","title":"Geology and oil and coal resources of the region south of Cody, Park County, Wyoming","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1940","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b921B","usgsCitation":"Pierce, W.G., and Andrews, D.A., 1941, Geology and oil and coal resources of the region south of Cody, Park County, Wyoming: U.S. Geological Survey Bulletin 921, Report: v, 82 p.; 2 Plates: 23.00 × 46.75 inches and 22.50 × 46.75 inches, https://doi.org/10.3133/b921B.","productDescription":"Report: v, 82 p.; 2 Plates: 23.00 × 46.75 inches and 22.50 × 46.75 inches","costCenters":[],"links":[{"id":96939,"rank":301,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0921b/report.pdf","size":"9058","linkFileType":{"id":1,"text":"pdf"}},{"id":166824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0921b/report-thumb.jpg"},{"id":109550,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21098.htm","linkFileType":{"id":5,"text":"html"},"description":"21098"},{"id":63378,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0921b/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63377,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0921b/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","county":"Park County","city":"Cody","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.3420,\n 44.536\n ],\n [\n -108.944,\n 44.536\n ],\n [\n -108.944,\n 43.9290\n ],\n [\n -109.3420,\n 43.9290\n ],\n [\n -109.3420,\n 44.536\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68484a","contributors":{"authors":[{"text":"Pierce, William Gamewell","contributorId":105361,"corporation":false,"usgs":true,"family":"Pierce","given":"William","email":"","middleInitial":"Gamewell","affiliations":[],"preferred":false,"id":214712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, Douglas A.","contributorId":92923,"corporation":false,"usgs":true,"family":"Andrews","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":214711,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55391,"text":"ofr4124 - 1941 - Manganese deposits near Dunseith, North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:11:38","indexId":"ofr4124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"41-24","title":"Manganese deposits near Dunseith, North Dakota","language":"ENGLISH","doi":"10.3133/ofr4124","usgsCitation":"Hendricks, T.A., 1941, Manganese deposits near Dunseith, North Dakota: U.S. Geological Survey Open-File Report 41-24, 2 p., https://doi.org/10.3133/ofr4124.","productDescription":"2 p.","costCenters":[],"links":[{"id":177042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64acf5","contributors":{"authors":[{"text":"Hendricks, T. A.","contributorId":77494,"corporation":false,"usgs":true,"family":"Hendricks","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":253355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3031,"text":"wsp869 - 1941 - Flood of August 1935 in the Muskingum River Basin, Ohio, with sections on the associated meteorology and hydrology","interactions":[],"lastModifiedDate":"2022-01-03T19:55:27.641624","indexId":"wsp869","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"869","title":"Flood of August 1935 in the Muskingum River Basin, Ohio, with sections on the associated meteorology and hydrology","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp869","usgsCitation":"Youngquist, C.V., Langbein, W.B., Smith, W.E., and Showalter, A.K., 1941, Flood of August 1935 in the Muskingum River Basin, Ohio, with sections on the associated meteorology and hydrology: U.S. Geological Survey Water Supply Paper 869, vi, 118 p., https://doi.org/10.3133/wsp869.","productDescription":"vi, 118 p.","costCenters":[],"links":[{"id":393777,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24676.htm"},{"id":29862,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0869/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0869/report-thumb.jpg"}],"country":"United States","state":"Ohio","otherGeospatial":"Muskingum River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.779,\n 39.377\n ],\n [\n -80.9070,\n 39.377\n ],\n [\n -80.9070,\n 41.158\n ],\n [\n -82.779,\n 41.158\n ],\n [\n -82.779,\n 39.377\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eef0a","contributors":{"authors":[{"text":"Youngquist, C. V.","contributorId":28230,"corporation":false,"usgs":true,"family":"Youngquist","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":146178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Waldo E.","contributorId":15188,"corporation":false,"usgs":true,"family":"Smith","given":"Waldo","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146176,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Showalter, A. K.","contributorId":15600,"corporation":false,"usgs":true,"family":"Showalter","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":146177,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}