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,{"id":31048,"text":"wsp876 - 1941 - Surface water supply of the United States, 1939, Part VI, Missouri River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:09:15","indexId":"wsp876","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":"876","title":"Surface water supply of the United States, 1939, Part VI, Missouri River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp876","usgsCitation":"Paulsen, C.G., Beckman, H., Follansbee, R., Kasel, R., Newell, T.R., Speer, P.R., Spiegel, J., and Tuttle, A., 1941, Surface water supply of the United States, 1939, Part VI, Missouri River basin: U.S. Geological Survey Water Supply Paper 876, xi, 506 p. :ill. ;24 cm., https://doi.org/10.3133/wsp876.","productDescription":"xi, 506 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":161202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0876/report-thumb.jpg"},{"id":59604,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0876/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6961cd","contributors":{"authors":[{"text":"Paulsen, C. G.","contributorId":96239,"corporation":false,"usgs":true,"family":"Paulsen","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":204697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beckman, H.C.","contributorId":34487,"corporation":false,"usgs":true,"family":"Beckman","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":204694,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Follansbee, Robert","contributorId":51713,"corporation":false,"usgs":true,"family":"Follansbee","given":"Robert","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":204695,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kasel, R.G.","contributorId":32962,"corporation":false,"usgs":true,"family":"Kasel","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":204693,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Newell, Thomas R.","contributorId":106876,"corporation":false,"usgs":true,"family":"Newell","given":"Thomas","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":204699,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Speer, P. R.","contributorId":104948,"corporation":false,"usgs":true,"family":"Speer","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":204698,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Spiegel, J.B.","contributorId":69528,"corporation":false,"usgs":true,"family":"Spiegel","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":204696,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tuttle, A.H.","contributorId":10781,"corporation":false,"usgs":true,"family":"Tuttle","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":204692,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":33768,"text":"b920 - 1941 - Pre-Cambrian geology and mineral resources of the Delaware Water Gap and Easton quadrangles, New Jersey and Pennsylvania","interactions":[],"lastModifiedDate":"2022-03-30T19:23:47.931428","indexId":"b920","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":"920","title":"Pre-Cambrian geology and mineral resources of the Delaware Water Gap and Easton quadrangles, New Jersey and Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b920","usgsCitation":"Bayley, W.S., 1941, Pre-Cambrian geology and mineral resources of the Delaware Water Gap and Easton quadrangles, New Jersey and Pennsylvania: U.S. Geological Survey Bulletin 920, Report: v, 97 p.; 1 Plate: 18.32 × 26.49 inches, https://doi.org/10.3133/b920.","productDescription":"Report: v, 97 p.; 1 Plate: 18.32 × 26.49 inches","costCenters":[],"links":[{"id":397892,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21096.htm"},{"id":163391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0920/report-thumb.jpg"},{"id":92399,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0920/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92398,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0920/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"New Jersey, Pennsylvania","otherGeospatial":"Delaware Water Gap and Easton quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.25,\n              40.547\n            ],\n            [\n              -75,\n              40.547\n            ],\n            [\n              -75,\n              40.872\n            ],\n            [\n              -75.25,\n              40.872\n            ],\n            [\n              -75.25,\n              40.547\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad2e4b07f02db681b19","contributors":{"authors":[{"text":"Bayley, William Shirley","contributorId":66234,"corporation":false,"usgs":true,"family":"Bayley","given":"William","email":"","middleInitial":"Shirley","affiliations":[],"preferred":false,"id":211910,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55546,"text":"ofr4119 - 1941 - Electrical resistivity determinations over the potash area near Carlsbad, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:55","indexId":"ofr4119","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":"41-19","title":"Electrical resistivity determinations over the potash area near Carlsbad, New Mexico","language":"ENGLISH","doi":"10.3133/ofr4119","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Electrical resistivity determinations over the potash area near Carlsbad, New Mexico: U.S. Geological Survey Open-File Report 41-19, 32 p. :ill.; 4 maps, https://doi.org/10.3133/ofr4119.","productDescription":"32 p. :ill.; 4 maps","costCenters":[],"links":[{"id":173842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606ec5","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":532365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55272,"text":"ofr4129 - 1941 - Mining in Alaska in 1940","interactions":[{"subject":{"id":55272,"text":"ofr4129 - 1941 - Mining in Alaska in 1940","indexId":"ofr4129","publicationYear":"1941","noYear":false,"title":"Mining in Alaska in 1940"},"predicate":"SUPERSEDED_BY","object":{"id":35887,"text":"b933A - 1942 - Mineral industry of Alaska in 1940","indexId":"b933A","publicationYear":"1942","noYear":false,"chapter":"A","title":"Mineral industry of Alaska in 1940"},"id":1}],"supersededBy":{"id":35887,"text":"b933A - 1942 - Mineral industry of Alaska in 1940","indexId":"b933A","publicationYear":"1942","noYear":false,"title":"Mineral industry of Alaska in 1940"},"lastModifiedDate":"2012-02-02T00:11:58","indexId":"ofr4129","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":"41-29","title":"Mining in Alaska in 1940","language":"ENGLISH","doi":"10.3133/ofr4129","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Mining in Alaska in 1940 (Superseded by Bulletin 933-A): U.S. Geological Survey Open-File Report 41-29, 5 p., https://doi.org/10.3133/ofr4129.","productDescription":"5 p.","costCenters":[],"links":[{"id":181208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superseded by Bulletin 933-A","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ca4","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":532321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55265,"text":"ofr4130 - 1941 - Chromite deposits of Kenai Peninsula, Alaska","interactions":[{"subject":{"id":55265,"text":"ofr4130 - 1941 - Chromite deposits of Kenai Peninsula, Alaska","indexId":"ofr4130","publicationYear":"1941","noYear":false,"title":"Chromite deposits of Kenai Peninsula, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":45243,"text":"b931G - 1942 - Chromite deposits of Kenai Peninsula, Alaska","indexId":"b931G","publicationYear":"1942","noYear":false,"chapter":"G","title":"Chromite deposits of Kenai Peninsula, Alaska"},"id":1}],"supersededBy":{"id":45243,"text":"b931G - 1942 - Chromite deposits of Kenai Peninsula, Alaska","indexId":"b931G","publicationYear":"1942","noYear":false,"title":"Chromite deposits of Kenai Peninsula, Alaska"},"lastModifiedDate":"2012-02-02T00:11:47","indexId":"ofr4130","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":"41-30","title":"Chromite deposits of Kenai Peninsula, Alaska","language":"ENGLISH","doi":"10.3133/ofr4130","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Chromite deposits of Kenai Peninsula, Alaska (Superseded by Bulletin 931-G): U.S. Geological Survey Open-File Report 41-30, 2 p.; 2 maps, https://doi.org/10.3133/ofr4130.","productDescription":"2 p.; 2 maps","costCenters":[],"links":[{"id":174153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superseded by Bulletin 931-G","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e2465","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":532315,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55301,"text":"ofr438 - 1941 - Map of part of the Blue Wing district, Idaho","interactions":[{"subject":{"id":55301,"text":"ofr438 - 1941 - Map of part of the Blue Wing district, Idaho","indexId":"ofr438","publicationYear":"1941","noYear":false,"title":"Map of part of the Blue Wing district, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":45237,"text":"b931A - 1943 - Tungsten resources of the Blue Wing district, Lemhi County, Idaho","indexId":"b931A","publicationYear":"1943","noYear":false,"chapter":"A","title":"Tungsten resources of the Blue Wing district, Lemhi County, Idaho"},"id":1}],"supersededBy":{"id":45237,"text":"b931A - 1943 - Tungsten resources of the Blue Wing district, Lemhi County, Idaho","indexId":"b931A","publicationYear":"1943","noYear":false,"title":"Tungsten resources of the Blue Wing district, Lemhi County, Idaho"},"lastModifiedDate":"2012-02-02T00:11:55","indexId":"ofr438","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":"43-8","title":"Map of part of the Blue Wing district, Idaho","language":"ENGLISH","doi":"10.3133/ofr438","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Map of part of the Blue Wing district, Idaho (Superseded by Bulletin 931-A): U.S. Geological Survey Open-File Report 43-8, 1 p., https://doi.org/10.3133/ofr438.","productDescription":"1 p.","costCenters":[],"links":[{"id":174885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superseded by Bulletin 931-A","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db658033","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":532330,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55543,"text":"ofr4121 - 1941 - Geology of Markleeville dam site","interactions":[],"lastModifiedDate":"2012-02-02T00:11:55","indexId":"ofr4121","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":"41-21","title":"Geology of Markleeville dam site","language":"ENGLISH","doi":"10.3133/ofr4121","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Geology of Markleeville dam site: U.S. Geological Survey Open-File Report 41-21, 7 p. :ill.; 1 map, https://doi.org/10.3133/ofr4121.","productDescription":"7 p. :ill.; 1 map","costCenters":[],"links":[{"id":173839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683a7f","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":532363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45309,"text":"b883E - 1941 - Spirit leveling in Texas. Part 5, South-central Texas, 1896-1938","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"b883E","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":"883","chapter":"E","title":"Spirit leveling in Texas. Part 5, South-central Texas, 1896-1938","language":"ENGLISH","doi":"10.3133/b883E","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Spirit leveling in Texas. Part 5, South-central Texas, 1896-1938: U.S. Geological Survey Bulletin 883, 561-789 p., https://doi.org/10.3133/b883E.","productDescription":"561-789 p.","costCenters":[],"links":[{"id":93973,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0883e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0883e/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6987c3","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":531584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":"<p>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.</p><p>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.</p><p>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.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Subsurface geology and oil and gas resources of Osage County, Oklahoma","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b900H","usgsCitation":"Kirk, C.T., Dillard, W.R., Leatherock, O., and Jenkins, H.D., 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: U.S. Geological Survey Bulletin 900, 34 p., https://doi.org/10.3133/b900H.","productDescription":"34 p.","startPage":"269","endPage":"302","costCenters":[],"links":[{"id":109540,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21071.htm","linkFileType":{"id":5,"text":"html"},"description":"21071"},{"id":135246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0900h/report-thumb.jpg"},{"id":93939,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0900h/report.pdf","text":"Report","size":"2.65 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oklahoma","county":"Osage 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C. T.","contributorId":26278,"corporation":false,"usgs":true,"family":"Kirk","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":231377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dillard, W. R.","contributorId":25906,"corporation":false,"usgs":true,"family":"Dillard","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":231376,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leatherock, Otto","contributorId":103645,"corporation":false,"usgs":true,"family":"Leatherock","given":"Otto","email":"","affiliations":[],"preferred":false,"id":231379,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jenkins, H. D.","contributorId":91452,"corporation":false,"usgs":true,"family":"Jenkins","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":231378,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":45307,"text":"b883C - 1941 - Spirit leveling in Texas. Part 3, West-central Texas, 1896-1938","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"b883C","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":"883","chapter":"C","title":"Spirit leveling in Texas. Part 3, West-central Texas, 1896-1938","language":"ENGLISH","doi":"10.3133/b883C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Spirit leveling in Texas. Part 3, West-central Texas, 1896-1938: U.S. Geological Survey Bulletin 883, 151-239 p., https://doi.org/10.3133/b883C.","productDescription":"151-239 p.","costCenters":[],"links":[{"id":93971,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0883c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162079,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0883c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a4c","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":531582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45306,"text":"b883B - 1941 - Spirit leveling in Texas. Part 2, Panhandle, 1896-1939","interactions":[],"lastModifiedDate":"2012-02-02T00:04:53","indexId":"b883B","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":"883","chapter":"B","title":"Spirit leveling in Texas. Part 2, Panhandle, 1896-1939","language":"ENGLISH","doi":"10.3133/b883B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Spirit leveling in Texas. Part 2, Panhandle, 1896-1939: U.S. Geological Survey Bulletin 883, 51-149 p., https://doi.org/10.3133/b883B.","productDescription":"51-149 p.","costCenters":[],"links":[{"id":93970,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0883b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135157,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0883b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69660e","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":531581,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53520,"text":"naf57 - 1941 - Attwater's prairie-chicken-its life history and management","interactions":[],"lastModifiedDate":"2017-01-10T15:45:56","indexId":"naf57","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":58,"text":"North American Fauna","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"57","title":"Attwater's prairie-chicken-its life history and management","docAbstract":"<p class=\"first\">Attwater's prairie chicken, a characteristic bird of the Texas coastal prairie, is closely related to the now extinct heath-hen of northeastern North America. Once abundant in an area extending from the coastal tall-grass prairies of southwestern Louisiana and Texas west and south to near Port Isabel, it has decreased in numbers as man has exploited its habitat, until now it is threatened with the same fate as that of the heath-hen.</p><p>Important factors limiting the numbers of the bird include excessive or persistent rainfall during the nesting season, heavy grazing, excessive pasture burning, agricultural operations, and overshooting. Management will usually involve protection from excessive killing, improvement of food and cover, and control of predators and of the kill by hunters. Responsibility for this rests with the landowner.</p><p>Optimum prairie chicken range apparently consists of well-drained grassland, with some weeds or shrubs, the cover varying in density from light to heavy; and with surface water available in summer; diversification within the grassland type is essential. In the absence of ample refuges for the species, probably all other favorable factors together will fail to save Attwater's prairie chicken from extinction.</p><p class=\"last\">This number continues the series of the North American Fauna issued by the Bureau of Biological Survey, of the United States Department of Agriculture, prior to its transfer and consolidation with the Bureau of Fisheries on June 30, 1940, to form the Fish and Wildlife Service, in the Department of the Interior.</p>","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Lehmann, V.W., 1941, Attwater's prairie-chicken-its life history and management: North American Fauna 57, v, 65 p. incl. illus. (incl. map) tables 14 pl. (1 col.) on 11 l. fold. diagr. 23 cm.","productDescription":"v, 65 p. incl. illus. (incl. map) tables 14 pl. (1 col.) on 11 l. fold. diagr. 23 cm.","costCenters":[],"links":[{"id":179433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":22643,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.fwspubs.org/toc/nafa//57","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66933e","contributors":{"authors":[{"text":"Lehmann, Valgene W.","contributorId":62884,"corporation":false,"usgs":true,"family":"Lehmann","given":"Valgene","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":247741,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53291,"text":"ofr4122 - 1941 - Iron ore deposits of the Bull Valley District, Washington County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:11:45","indexId":"ofr4122","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":"41-22","title":"Iron ore deposits of the Bull Valley District, Washington County, Utah","language":"ENGLISH","doi":"10.3133/ofr4122","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Iron ore deposits of the Bull Valley District, Washington County, Utah: U.S. Geological Survey Open-File Report 41-22, 5 p., https://doi.org/10.3133/ofr4122.","productDescription":"5 p.","costCenters":[],"links":[{"id":175004,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1941/0022/report-thumb.jpg"},{"id":87140,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1941/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672e8","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":532177,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213426,"text":"70213426 - 1941 - Ground‐water inventory in the Upper Gila River Valley, New Mexico and Arizona: Scope of investigation and methods used","interactions":[],"lastModifiedDate":"2020-09-17T17:24:58.299364","indexId":"70213426","displayToPublicDate":"1941-09-17T12:14:22","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Ground‐water inventory in the Upper Gila River Valley, New Mexico and Arizona: Scope of investigation and methods used","docAbstract":"<p><span>The Division of Ground Water of the Geological Survey, United States Department of the Interior, has been making an inventory of the water‐resources of the upper Gila River since January 1, 1940. Funds for the project are furnished under a cooperative agreement with the Arizona State Water Commissioner, supplemented by a substantial grant from the United States Engineer Office of the War Department. The State of Arizona wants information regarding the quantity of ground‐water available to supplement surface‐water irrigation. The Army Engineers would like to know the effect that flood‐control structures which may be built on the upper Gila will have on existing relations between river‐flow and ground‐water storage.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00738","usgsCitation":"Turner, S., and Halpenny, L., 1941, Ground‐water inventory in the Upper Gila River Valley, New Mexico and Arizona: Scope of investigation and methods used: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 738-744, https://doi.org/10.1029/TR022i003p00738.","productDescription":"7 p.","startPage":"738","endPage":"744","costCenters":[],"links":[{"id":378523,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Turner, S.F.","contributorId":67914,"corporation":false,"usgs":true,"family":"Turner","given":"S.F.","email":"","affiliations":[],"preferred":false,"id":799093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Halpenny, L.C.","contributorId":40967,"corporation":false,"usgs":true,"family":"Halpenny","given":"L.C.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":799094,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70213419,"text":"70213419 - 1941 - Coefficients of storage and transmissibility obtained from pumping tests in the Houston District, Texas","interactions":[],"lastModifiedDate":"2020-09-17T17:07:17.502537","indexId":"70213419","displayToPublicDate":"1941-09-17T11:57:28","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Coefficients of storage and transmissibility obtained from pumping tests in the Houston District, Texas","docAbstract":"<p><span>An investigation of the ground‐water supply of the Houston District, in Texas, has been in progress since December, 1930, under the general direction of O. E. Meinzer, Geologist‐in‐Charge of the Division of Ground Water of the Geological Survey. The Houston District, as the term is used here, comprises all of Harris County and parts of Montgomery, Waller, and Fort Bend counties, lying between the Trinity and Brazos rivers. The investigation in this area has consisted primarily of inventorying well‐logs and pumpage‐records, of obtaining water‐level data and information regarding the chemical character of the ground‐water, and wherever possible of correlating these data.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00744","usgsCitation":"Jacob, C.E., 1941, Coefficients of storage and transmissibility obtained from pumping tests in the Houston District, Texas: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 744-756, https://doi.org/10.1029/TR022i003p00744.","productDescription":"13 p.","startPage":"744","endPage":"756","costCenters":[],"links":[{"id":378519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.328125,\n              29.372601506681402\n            ],\n            [\n              -94.317626953125,\n              29.372601506681402\n            ],\n            [\n              -94.317626953125,\n              30.230594564932193\n            ],\n            [\n              -96.328125,\n              30.230594564932193\n            ],\n            [\n              -96.328125,\n              29.372601506681402\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":799092,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213281,"text":"70213281 - 1941 - Fluctuations of water‐level in wells in the Los Angeles basin, California, during five strong earthquakes, 1933–1940","interactions":[],"lastModifiedDate":"2020-09-17T13:36:22.732076","indexId":"70213281","displayToPublicDate":"1941-09-16T15:08:27","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Fluctuations of water‐level in wells in the Los Angeles basin, California, during five strong earthquakes, 1933–1940","docAbstract":"<p><span>Numerous ground‐water hydrologists have obtained records of water‐level surges in wells during earthquakes and of heightened or lowered levels after those earthquakes. Many of these surges and changes of level are undoubtedly direct effects of the several earthquake‐waves that are recorded on seismographs. Thus, water‐level recorders on observation‐wells promise to afford a means of extending greatly the scope of seismographic records for local areas.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i002p00374-2","usgsCitation":"LaRocque, G., 1941, Fluctuations of water‐level in wells in the Los Angeles basin, California, during five strong earthquakes, 1933–1940: Eos, Transactions, American Geophysical Union, v. 22, no. 2, p. 374-386, https://doi.org/10.1029/TR022i002p00374-2.","productDescription":"13 p.","startPage":"374","endPage":"386","costCenters":[],"links":[{"id":378478,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Los Angeles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.5809326171875,\n              33.46810795527896\n            ],\n            [\n              -117.3175048828125,\n              33.46810795527896\n            ],\n            [\n              -117.3175048828125,\n              34.298068350990825\n            ],\n            [\n              -118.5809326171875,\n              34.298068350990825\n            ],\n            [\n              -118.5809326171875,\n              33.46810795527896\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"22","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"LaRocque, G.A. Jr.","contributorId":22837,"corporation":false,"usgs":true,"family":"LaRocque","given":"G.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":798939,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213279,"text":"70213279 - 1941 - Report of committee on underground waters, 1940–41","interactions":[],"lastModifiedDate":"2020-09-17T13:37:48.458462","indexId":"70213279","displayToPublicDate":"1941-09-16T15:02:05","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of committee on underground waters, 1940–41","docAbstract":"<p>The membership of the Committee during the past year has continued as it was a year ago [see Trans. Amer. Geophys. Union, p. 433, 1940].</p><p>During a large part of the year, particularly during the last few months, many of the members of the Committee have been engaged in activities more or less closely related to defense. As a consequence it has been necessary to omit or postpone some research studies that might otherwise have been carried on, and the following report is briefer than usual.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00948","usgsCitation":"Thompson, D., 1941, Report of committee on underground waters, 1940–41: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 948-950, https://doi.org/10.1029/TR022i003p00948.","productDescription":"3 p.","startPage":"948","endPage":"950","costCenters":[],"links":[{"id":378499,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David G.","contributorId":8443,"corporation":false,"usgs":true,"family":"Thompson","given":"David G.","affiliations":[],"preferred":false,"id":798938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213278,"text":"70213278 - 1941 - Application of coefficients of transmissibility and storage to regional problems in the Houston District, Texas","interactions":[],"lastModifiedDate":"2020-09-16T20:01:43.241981","indexId":"70213278","displayToPublicDate":"1941-09-16T14:49:37","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Application of coefficients of transmissibility and storage to regional problems in the Houston District, Texas","docAbstract":"<p>The Houston District, as the term is used in this paper, comprises an area between the Trinity and Brazos rivers in Harris County and parts of Montgomery, Waller, and Fort Bend counties, Texas. It consists of a plain of low relief that lies not far above sea‐level, and is a part of the West Gulf Coastal Plain. A part of the District is shown in Figure 1.</p><p>Large quantities of ground‐water are pumped in the Houston District from a succession of beds of sand that occur between 300 and 1,900 feet below the surface. These sands are interbedded with relatively impermeable clays. The formations range in age from Miocene to Recent and were deposited during several cycles of marine and continental deposition. They may be classified into several zones which are predominantly clay or predominantly sand, but in which the individual beds at most horizons can not be traced very far. Most of the beds interfinger and grade into one another laterally and vertically in short distances, the thinner beds in many places changing character or pinching out within a few hundred feet. The formations dip to the southeastward, the dip ranging from about 35 feet to the mile in the older formations to about 20 feet to the mile in the younger. In the outcrop‐areas of the formations, and for considerable distances down the dip, the sediments are in general dominantly sandy. Far to the southeastward, in the direction of the Gulf, clay predominates.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00756","usgsCitation":"Guyton, W., 1941, Application of coefficients of transmissibility and storage to regional problems in the Houston District, Texas: Eos, Transactions, American Geophysical Union, p. 756-770, https://doi.org/10.1029/TR022i003p00756.","productDescription":"15 p.","startPage":"756","endPage":"770","costCenters":[],"links":[{"id":378476,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.328125,\n              29.372601506681402\n            ],\n            [\n              -94.317626953125,\n              29.372601506681402\n            ],\n            [\n              -94.317626953125,\n              30.230594564932193\n            ],\n            [\n              -96.328125,\n              30.230594564932193\n            ],\n            [\n              -96.328125,\n              29.372601506681402\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Guyton, W.F.","contributorId":11688,"corporation":false,"usgs":true,"family":"Guyton","given":"W.F.","affiliations":[],"preferred":false,"id":798937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213276,"text":"70213276 - 1941 - Depth of active solution by ground‐waters in the Pecos Valley, New Mexico","interactions":[],"lastModifiedDate":"2020-09-16T19:44:23.733022","indexId":"70213276","displayToPublicDate":"1941-09-16T14:32:40","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Depth of active solution by ground‐waters in the Pecos Valley, New Mexico","docAbstract":"<p><span>The Pecos River Drainage‐Basin is underlain by a thick series of Permian rocks consisting largely of limestone, gypsum (or anhydrite), and halite. The beds have a regional eastward or southeastward dip of 40 to 80 feet to the mile and successively younger beds are exposed at the surface from west to east across the Basin (Fig, 1). The beds of the San Andres formation and the Chalk Bluff formation or its equivalents crop out over most of the broad western part of the Basin (Fig. 1). Most of the eastern part of the Basin is immediately underlain by the redbeds was sandstone of the Dockum group, of Triassic age, which, south of Acme, are separated from the Chalk Bluff formation by the Salado and Rustler formations. North of Acme the Dockum group overlaps successively older formations ana northwest of Santa Rosa it rests upon beds in the lower part of the San Andres formation.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00779","usgsCitation":"Morgan, A., 1941, Depth of active solution by ground‐waters in the Pecos Valley, New Mexico: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 779-783, https://doi.org/10.1029/TR022i003p00779.","productDescription":"5 p.","startPage":"779","endPage":"783","costCenters":[],"links":[{"id":378470,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Pecos River Drainage Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.10595703125,\n              36.54494944148322\n            ],\n            [\n              -106.23779296875,\n              35.60371874069731\n            ],\n            [\n              -106.36962890624999,\n              34.52466147177172\n            ],\n            [\n              -106.3916015625,\n              32.82421110161336\n            ],\n            [\n              -106.23779296875,\n              32.0639555946604\n            ],\n            [\n              -103.33740234375,\n              32.045332838858506\n            ],\n            [\n              -103.18359375,\n              36.87962060502676\n            ],\n            [\n              -106.06201171875,\n              36.914764288955936\n            ],\n            [\n              -106.10595703125,\n              36.54494944148322\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Morgan, Arthur M.","contributorId":59051,"corporation":false,"usgs":true,"family":"Morgan","given":"Arthur M.","affiliations":[],"preferred":false,"id":798933,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213275,"text":"70213275 - 1941 - Ground‐water dams created by faulting of alluvial sediments in the hurricane fault‐zone, Utah","interactions":[],"lastModifiedDate":"2020-09-17T13:40:55.020762","indexId":"70213275","displayToPublicDate":"1941-09-16T14:09:55","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Ground‐water dams created by faulting of alluvial sediments in the hurricane fault‐zone, Utah","docAbstract":"<p><span>Ground‐water dams are recognized in the unconsolidated sediments of two intermontane valleys in southwestern Utah. Parowan Valley is about 30 miles long and has a general northeasterly trend; Cedar City Valley lies west and south of Parowan Valley, is somewhat larger, and has a more nearly north‐south trend. Great accumulations of boulders, gravel, sand, and clay have been brought into both valleys by the streams that drain the surrounding highlands, and the valleys have become topographic basins whose lowest parts are occupied by lakes or dry alkali flats, rimmed on all sides with the alluvial fans and cones that have been formed by the streams tributary to the valleys. Ground‐water occurs principally in these unconsolidated sediments, and in both valleys a large proportion of the irrigated lands is dependent upon water pumped from wells.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00775","usgsCitation":"Thomas, H.E., 1941, Ground‐water dams created by faulting of alluvial sediments in the hurricane fault‐zone, Utah: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 775-778, https://doi.org/10.1029/TR022i003p00775.","productDescription":"4 p.","startPage":"775","endPage":"778","costCenters":[],"links":[{"id":378469,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.0380859375,\n              36.98500309285596\n            ],\n            [\n              -112.35717773437499,\n              36.98500309285596\n            ],\n            [\n              -112.35717773437499,\n              38.603993275591684\n            ],\n            [\n              -114.0380859375,\n              38.603993275591684\n            ],\n            [\n              -114.0380859375,\n              36.98500309285596\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":798932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213274,"text":"70213274 - 1941 - Report of committee on glaciers, 1940–41","interactions":[],"lastModifiedDate":"2020-09-17T13:42:09.991041","indexId":"70213274","displayToPublicDate":"1941-09-16T13:58:51","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of committee on glaciers, 1940–41","docAbstract":"<p><span>The personnel of the Committee is now as follows: Harry Fielding Reid, Professor Emeritus of Geology, Johns Hopkins University, 608 Cathedral Street, Baltimore, Maryland; William H. Hobbs, Professor Emeritus of Geology, University of Michigan, Ann Arbor, Michigan; Lawrence Martin, Chief of the Division of Maps, Library of Congress, Washington, D.C.; J. E. Church, Professor of Meteorology, Agricultural Experiment Station, University of Nevada, Reno, Nevada; Wm. Osgood Field, Jr., Explorer, 18 West Twelfth Street, New York, New York; Oliver Kehrlein, Chairman, Committee on Glacier Studies of Sierra Club, 1050 Mills Tower, 220 Bush Street, San Francisco, California; Kenneth N. Phillips, Associate Hydraulic Engineer, Water Resources Branch, United States Geological Survey, Chairman, Research Committee of the Mazamas, 606 Post‐Office Building, Portland, Oregon; William S. Cooper, Professor of Botany, University of Minnesota, Minneapolis, Minnesota; Gerald Fitzgerald, Senior Topographic Engineer, Alaska Branch, United States Geological Survey, Washington, D.C.; Laurence M. Gould, Professor of Geology, Carleton College, Northfield, Minnesota; Dr. Max Demorest, Department of Geology, Yale University, New Haven, Connecticut; François E. Matthes (Chairman), Senior Geologist, Section of Glacial Geology, United States Geological Survey, Washington, D.C.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p01006","usgsCitation":"Matthes, F.E., 1941, Report of committee on glaciers, 1940–41: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 1006-1011, https://doi.org/10.1029/TR022i003p01006.","productDescription":"6 p.","startPage":"1006","endPage":"1011","costCenters":[],"links":[{"id":378468,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Matthes, Francois E.","contributorId":97963,"corporation":false,"usgs":true,"family":"Matthes","given":"Francois","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":798931,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213270,"text":"70213270 - 1941 - Factors producing a nine‐year decline in ground‐water levels in Scott County, Kansas","interactions":[],"lastModifiedDate":"2020-09-17T13:48:51.812102","indexId":"70213270","displayToPublicDate":"1941-09-16T13:18:28","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Factors producing a nine‐year decline in ground‐water levels in Scott County, Kansas","docAbstract":"<p><span>In the south‐central part of Scott County, Kansas, there is an area of shallow water‐table in which the ground‐water levels have declined steadily since 1932 (Fig. 1). In this area water has been withdrawn from wells for irrigation in increasing amounts during the last decade and the precipitation has been considerably below normal for the last seven years. Thus, the problem of interpreting the downward trend of the water‐table has been complicated by the presence of two competent causes.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00772","usgsCitation":"Waite, H.A., 1941, Factors producing a nine‐year decline in ground‐water levels in Scott County, Kansas: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 772-775, https://doi.org/10.1029/TR022i003p00772.","productDescription":"4 p.","startPage":"772","endPage":"775","costCenters":[],"links":[{"id":378462,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas","county":"Scott County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-100.6882,38.7037],[-100.6845,38.2627],[-101.1037,38.2636],[-101.1254,38.264],[-101.1293,38.7001],[-100.8168,38.7032],[-100.6882,38.7037]]]},\"properties\":{\"name\":\"Scott\",\"state\":\"KS\"}}]}","volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Waite, H. A.","contributorId":173753,"corporation":false,"usgs":false,"family":"Waite","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":798925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213268,"text":"70213268 - 1941 - Report of committee on the chemistry of natural waters, 1840–41","interactions":[],"lastModifiedDate":"2020-09-17T13:52:06.202075","indexId":"70213268","displayToPublicDate":"1941-09-16T12:17:59","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of committee on the chemistry of natural waters, 1840–41","docAbstract":"<p><span>The membership of the Committee during the past year was as follows: I. A. Dennison. Bureau of Standards; C. S. Scofield, Department of Agriculture; D. G. Thompson, Geological Survey; T. G. Thompson, University of Washington, Seattle, Washington; and C. S. Howard, United States Geological Survey, Washington, D.C. (Chairman).</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00901-1","usgsCitation":"Howard, C.S., 1941, Report of committee on the chemistry of natural waters, 1840–41: Eos, Transactions, American Geophysical Union, v. 22, no. 3, https://doi.org/10.1029/TR022i003p00901-1.","productDescription":"1 p.","startPage":"901","costCenters":[],"links":[{"id":378460,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":798923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213120,"text":"70213120 - 1941 - The quicksilver deposits of the Terlingua region, Texas","interactions":[],"lastModifiedDate":"2020-09-09T20:23:23.184757","indexId":"70213120","displayToPublicDate":"1941-09-09T15:17:34","publicationYear":"1941","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The quicksilver deposits of the Terlingua region, Texas","docAbstract":"<p><span>Texas is second among quicksilver-producing States because of the Terlingua region, in the Big Bend of the Rio Grande. This region contains Cretaceous strata, largely calcareous, which grade upward into Tertiary volcanics, locally without break. The strata are cut by numerous intrusions, largely alkalic, and are extensively folded and faulted.Many of the lodes are near the base of the impervious Del Rio clay, some at higher horizons, and a few in intrusive masses. The solutions penetrated only along open passageways, such as major fractures or joints in zones of tension, and, especially at horizons above the Del Rio, in fractures related to fault zones.The quicksilver is believed to have been brought in by alkali sulphide solutions. Most other constituents that may once have been present in the solutions had been separated earlier. Precipitation resulted largely from mingling with groundwater. The comparatively low temperature and pressure at the shallow levels where groundwater was present aided the precipitation. As the then-existing zone of groundwater circulation has since been partly exposed by erosion, the lodes are necessarily rather close to the present surface. The gangue minerals, particularly the calcite, are believed to have been derived mainly from the sedimentary rocks with some addition of material from deep sources. The relation of the widespread bitumen to genesis is puzzling here, as in many other quicksilver deposits. Weathering is of slight economic importance. Many minerals that resemble supergene products, including the quicksilver chlorides, are thought to have resulted here from original deposition within the zone of vadose water.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.36.2.115","usgsCitation":"Ross, C.P., 1941, The quicksilver deposits of the Terlingua region, Texas: Economic Geology, v. 36, no. 2, p. 115-142, https://doi.org/10.2113/gsecongeo.36.2.115.","productDescription":"28 p.","startPage":"115","endPage":"142","costCenters":[],"links":[{"id":378287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Terlingua Region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.2108154296875,\n              29.463514026304715\n            ],\n            [\n              -104.12841796875,\n              29.38217507514529\n            ],\n            [\n              -104.0130615234375,\n              29.31514119318728\n            ],\n            [\n              -103.7933349609375,\n              29.27202470909843\n            ],\n            [\n              -103.71093749999999,\n              29.19532826709913\n            ],\n            [\n              -103.5736083984375,\n              29.161755515328824\n            ],\n            [\n              -103.46923828124999,\n              29.080175989623203\n            ],\n            [\n              -103.3099365234375,\n              29.017748018496047\n            ],\n            [\n              -103.1231689453125,\n              29.00333620017934\n            ],\n            [\n              -103.0133056640625,\n              29.137768254983335\n            ],\n            [\n              -102.9254150390625,\n              29.23847708592805\n            ],\n            [\n              -102.864990234375,\n              29.3678143847754\n            ],\n            [\n              -102.799072265625,\n              29.544787796199465\n            ],\n            [\n              -102.6947021484375,\n              29.750070930806785\n            ],\n            [\n              -104.2108154296875,\n              29.7453016622136\n            ],\n            [\n              -104.2108154296875,\n              29.463514026304715\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"36","issue":"2","noUsgsAuthors":false,"publicationDate":"1941-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ross, Clyde P.","contributorId":10473,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":798285,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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