{"pageNumber":"7259","pageRowStart":"181450","pageSize":"25","recordCount":185244,"records":[{"id":45320,"text":"b846A - 1933 - Some mining districts of eastern Oregon","interactions":[{"subject":{"id":45320,"text":"b846A - 1933 - Some mining districts of eastern Oregon","indexId":"b846A","publicationYear":"1933","noYear":false,"chapter":"A","title":"Some mining districts of eastern Oregon"},"predicate":"IS_PART_OF","object":{"id":34988,"text":"b846 - 1934 - Contributions to economic geology (short papers and preliminary reports), 1933","indexId":"b846","publicationYear":"1934","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1933"},"id":1}],"isPartOf":{"id":34988,"text":"b846 - 1934 - Contributions to economic geology (short papers and preliminary reports), 1933","indexId":"b846","publicationYear":"1934","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1933"},"lastModifiedDate":"2022-04-27T21:20:34.123389","indexId":"b846A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"846","chapter":"A","title":"Some mining districts of eastern Oregon","docAbstract":"<p>This report presents the results of a reconnaissance of most of the mining districts of Oregon east of the Cascade Range, with the exception of the districts in the Sumpter quadrangle. The districts described are distributed through an area roughly coincident with the Blue Mountains, which extend over much of the northeast quarter of the State. </p><p>The geology of the Blue Mountains, except for certain small areas, is known only in its most general outlines. The most widespread rocks are the Tertiary volcanic rocks, which extend over a very large part of the State. They are separated by a profound angular and erosional unconformity from the pre-Tertiary rocks. </p><p>The pre-Tertiary rocks include representatives of all the geologic periods from Carboniferous to Cretaceous, and earlier periods may also be represented. </p><p>The known Carboniferous rocks include argillite, chert, greenstone, and subordinate limestone of uncertain age and a thick series of Permian greenstone, tuff, and limestone. The Triassic rocks include shale, slate, and limestone; the Jurassic rocks are shale and slate; and the Cretaceous are conglomerate and sandstone. Schist and phyllite with some limestone and greenstone of uncertain age occur along the Burnt River west of Durkee and in the Mormon Basin. </p><p>Intrusive rocks of at least two magmatic cycles are widespread in the Blue Mountains, and the stratigraphy suggests that several cycles may be represented. The older intrusive rocks include gabbro, pyroxenite, norite, dunite, hornblende-quartz diorite, and albite granite and are characterized by a considerable degree of shearing and both cataclastic and metasomatic metamorphism. The age of some of these rocks in the Canyon Range has been fixed as Lower or Middle Triassic, and others are known to be post-Triassic. Younger biotite-quartz diorite and granodiorite of post-Triassic (possibly post-Jurassic) age are widespread, arid the ore deposits of pre-Tertiary age are believed to be genetically related to these rocks. </p><p>Representatives of the Tertiary period include Eocene volcanic rocks and sediments, Oligocene fluviatile deposits, Miocene basic lavas and fluviatile and lacustrine sediments, and Pliocene tuff and gravel. The Quaternary deposits include glacial moraines in the higher mountains, stream gravel, and volcanic ash. </p><p>The structure of the pre-Tertiary rocks is complex. Folds are characteristically close or isoclinal and strike eastward. The post-Permian rocks appear to be less metamorphosed and less strongly deformed than the earlier rocks, and the Jurassic less than the Triassic. More than one epoch of diastrophism is therefore involved.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology (short papers and preliminary reports), 1933","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b846A","usgsCitation":"Gilluly, J., Reed, J., and Park, C.F., 1933, Some mining districts of eastern Oregon: U.S. Geological Survey Bulletin 846, viii, 140 p., https://doi.org/10.3133/b846A.","productDescription":"viii, 140 p.","costCenters":[],"links":[{"id":399784,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20512.htm"},{"id":93981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0846a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0846a/report-thumb.jpg"}],"country":"United States","state":"Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.6290,\n              44.4129\n            ],\n            [\n              -117.548,\n              44.4129\n            ],\n            [\n              -117.548,\n              44.4519\n            ],\n            [\n              -117.6290,\n              44.4519\n            ],\n            [\n              -117.6290,\n              44.4129\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db6914de","contributors":{"authors":[{"text":"Gilluly, James","contributorId":51743,"corporation":false,"usgs":true,"family":"Gilluly","given":"James","email":"","affiliations":[],"preferred":false,"id":231417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, J. C.","contributorId":75589,"corporation":false,"usgs":true,"family":"Reed","given":"J. C.","affiliations":[],"preferred":false,"id":231418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Park, C. F. Jr.","contributorId":90277,"corporation":false,"usgs":true,"family":"Park","given":"C.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":231419,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45317,"text":"b836C - 1933 - Mineral resources of Alaska, report on progress of investigations in 1930. Surface water supply of southeastern Alaska, 1909-1930","interactions":[],"lastModifiedDate":"2012-02-02T00:10:13","indexId":"b836C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"836","chapter":"C","title":"Mineral resources of Alaska, report on progress of investigations in 1930. Surface water supply of southeastern Alaska, 1909-1930","language":"ENGLISH","doi":"10.3133/b836C","usgsCitation":"Henshaw, F., 1933, Mineral resources of Alaska, report on progress of investigations in 1930. Surface water supply of southeastern Alaska, 1909-1930: U.S. Geological Survey Bulletin 836, 137-218 p., https://doi.org/10.3133/b836C.","productDescription":"137-218 p.","costCenters":[],"links":[{"id":113975,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0836c/report.pdf","size":"7223","linkFileType":{"id":1,"text":"pdf"}},{"id":170328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0836c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b7b2","contributors":{"authors":[{"text":"Henshaw, F.F.","contributorId":41805,"corporation":false,"usgs":true,"family":"Henshaw","given":"F.F.","email":"","affiliations":[],"preferred":false,"id":231414,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45321,"text":"b846B - 1933 - Geology and ore deposits of the Takilma-Waldo district, Oregon, including the Blue Creek district","interactions":[{"subject":{"id":45321,"text":"b846B - 1933 - Geology and ore deposits of the Takilma-Waldo district, Oregon, including the Blue Creek district","indexId":"b846B","publicationYear":"1933","noYear":false,"chapter":"B","title":"Geology and ore deposits of the Takilma-Waldo district, Oregon, including the Blue Creek district"},"predicate":"IS_PART_OF","object":{"id":34988,"text":"b846 - 1934 - Contributions to economic geology (short papers and preliminary reports), 1933","indexId":"b846","publicationYear":"1934","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1933"},"id":1}],"isPartOf":{"id":34988,"text":"b846 - 1934 - Contributions to economic geology (short papers and preliminary reports), 1933","indexId":"b846","publicationYear":"1934","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1933"},"lastModifiedDate":"2021-08-17T21:20:07.800384","indexId":"b846B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"846","chapter":"B","title":"Geology and ore deposits of the Takilma-Waldo district, Oregon, including the Blue Creek district","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b846B","usgsCitation":"Shenon, P., 1933, Geology and ore deposits of the Takilma-Waldo district, Oregon, including the Blue Creek district: U.S. Geological Survey Bulletin 846, 54 p., https://doi.org/10.3133/b846B.","productDescription":"54 p.","startPage":"141","endPage":"194","costCenters":[],"links":[{"id":388067,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20513.htm"},{"id":93982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0846b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0846b/report-thumb.jpg"}],"country":"United States","state":"Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.7810,\n              42.0\n            ],\n            [\n              -123.5730,\n              42.0\n            ],\n            [\n              -123.5730,\n              42.10\n            ],\n            [\n              -123.7810,\n              42.10\n            ],\n            [\n              -123.7810,\n              42.0\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db691658","contributors":{"authors":[{"text":"Shenon, P. J.","contributorId":38540,"corporation":false,"usgs":true,"family":"Shenon","given":"P. J.","affiliations":[],"preferred":false,"id":231420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45322,"text":"b846C - 1933 - The Climax molybdenum deposit, Colorado, with a section on history, production, metallurgy, and development","interactions":[{"subject":{"id":45322,"text":"b846C - 1933 - The Climax molybdenum deposit, Colorado, with a section on history, production, metallurgy, and development","indexId":"b846C","publicationYear":"1933","noYear":false,"chapter":"C","title":"The Climax molybdenum deposit, Colorado, with a section on history, production, metallurgy, and development"},"predicate":"IS_PART_OF","object":{"id":34988,"text":"b846 - 1934 - Contributions to economic geology (short papers and preliminary reports), 1933","indexId":"b846","publicationYear":"1934","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1933"},"id":1}],"isPartOf":{"id":34988,"text":"b846 - 1934 - Contributions to economic geology (short papers and preliminary reports), 1933","indexId":"b846","publicationYear":"1934","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1933"},"lastModifiedDate":"2022-06-09T20:19:30.667308","indexId":"b846C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"846","chapter":"C","title":"The Climax molybdenum deposit, Colorado, with a section on history, production, metallurgy, and development","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology (short papers and preliminary reports), 1933 (Bulletin 846)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b846C","usgsCitation":"Butler, B.S., and Vanderwilt, J., 1933, The Climax molybdenum deposit, Colorado, with a section on history, production, metallurgy, and development: U.S. Geological Survey Bulletin 846, 43 p., https://doi.org/10.3133/b846C.","productDescription":"43 p.","startPage":"195","endPage":"237","costCenters":[],"links":[{"id":402028,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20514.htm","linkFileType":{"id":5,"text":"html"}},{"id":170333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0846c/report-thumb.jpg"},{"id":93983,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0846c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113982,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0846c/plate-37.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113981,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0846c/plate-36.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113980,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0846c/plate-35.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113979,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0846c/plate-34.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113978,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0846c/plate-33.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113977,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0846c/plate-32.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113976,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0846c/plate-23.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.186,\n              39.35\n            ],\n            [\n              -106.133,\n              39.35\n            ],\n            [\n              -106.133,\n              39.392\n            ],\n            [\n              -106.186,\n              39.392\n            ],\n            [\n              -106.186,\n              39.35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e60","contributors":{"authors":[{"text":"Butler, B. 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,{"id":4603,"text":"wsp714 - 1933 - Surface water supply of the United States, 1931, Part IV, St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"wsp714","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"714","title":"Surface water supply of the United States, 1931, Part IV, St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp714","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1933, Surface water supply of the United States, 1931, Part IV, St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 714, v, 160 p. ;23 cm., https://doi.org/10.3133/wsp714.","productDescription":"v, 160 p. ;23 cm.","costCenters":[],"links":[{"id":139591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0714/report-thumb.jpg"},{"id":31660,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0714/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697895","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":528297,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4534,"text":"wsp735 - 1933 - Surface water supply of the United States, 1932 : Part 10, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"wsp735","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"735","title":"Surface water supply of the United States, 1932 : Part 10, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp735","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1933, Surface water supply of the United States, 1932 : Part 10, The Great Basin: U.S. Geological Survey Water Supply Paper 735, v, 107 p. ;23 cm., https://doi.org/10.3133/wsp735.","productDescription":"v, 107 p. ;23 cm.","costCenters":[],"links":[{"id":139701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0735/report-thumb.jpg"},{"id":31591,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0735/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697a3d","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":528232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1587,"text":"wsp724 - 1933 - Surface water supply of the United States, 1931 : Part 12. North Pacific slope drainage basins : C. Pacific slope basins in Oregon and lower Columbia River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp724","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"724","title":"Surface water supply of the United States, 1931 : Part 12. North Pacific slope drainage basins : C. Pacific slope basins in Oregon and lower Columbia River Basin","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp724","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1933, Surface water supply of the United States, 1931 : Part 12. North Pacific slope drainage basins : C. Pacific slope basins in Oregon and lower Columbia River Basin: U.S. Geological Survey Water Supply Paper 724, vi, 166 p. :ill. ;23 cm., https://doi.org/10.3133/wsp724.","productDescription":"vi, 166 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":138356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0724/report-thumb.jpg"},{"id":26652,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0724/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69626f","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":527950,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3597,"text":"cir3 - 1933 - The bleaching clays","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"cir3","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3","title":"The bleaching clays","docAbstract":"Groundwater is one of Utah 's most extensive and valuable natural resources. Because of its widespread occurrence in both wet and dry areas, groundwater has been, and is a major factor affecting economic growth and development of the State. In some areas, groundwater is used to supplement streamflow for irrigation, public supply, and other uses. In other areas, it is the only water available for use. The U.S. Geological Survey, under cooperative programs with the Utah Department of Natural Resources and other Federal, State, and local agencies has been studying Utah 's groundwater resources since 1987. Much information has been gained during those studies about the occurrence, availability, and quality of groundwater; the withdrawal and use of the water; and the effects of withdrawal. This report summarizes that information in nontechnical language , which is designed for all readers. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir3","usgsCitation":"Nutting, P.G., 1933, The bleaching clays: U.S. Geological Survey Circular 3, 51 p.; ill. ;27 cm., https://doi.org/10.3133/cir3.","productDescription":"51 p.; ill. ;27 cm.","costCenters":[],"links":[{"id":123711,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1933/0003/report-thumb.jpg"},{"id":30630,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1933/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836d2","contributors":{"authors":[{"text":"Nutting, P. G.","contributorId":89121,"corporation":false,"usgs":true,"family":"Nutting","given":"P.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":147231,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1506,"text":"wsp725 - 1933 - Surface water supply of Hawaii : July 1, 1930 to June 30, 1931","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp725","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"725","title":"Surface water supply of Hawaii : July 1, 1930 to June 30, 1931","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp725","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1933, Surface water supply of Hawaii : July 1, 1930 to June 30, 1931: U.S. Geological Survey Water Supply Paper 725, iv, 99 p. ;23 cm., https://doi.org/10.3133/wsp725.","productDescription":"iv, 99 p. ;23 cm.","costCenters":[],"links":[{"id":136946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0725/report-thumb.jpg"},{"id":26567,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0725/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6978aa","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":527874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1588,"text":"wsp736 - 1933 - Surface water supply of the United States, 1932 : Part 11. Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp736","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"736","title":"Surface water supply of the United States, 1932 : Part 11. Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp736","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1933, Surface water supply of the United States, 1932 : Part 11. Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 736, xi, 415 p. :ill. ;23 cm., https://doi.org/10.3133/wsp736.","productDescription":"xi, 415 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0736/report-thumb.jpg"},{"id":26653,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0736/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69788d","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":527951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34167,"text":"b845 - 1933 - Guidebook of the western United States: Part F - The Southern Pacific lines, New Orleans to Los Angeles","interactions":[],"lastModifiedDate":"2023-07-14T18:33:24.56548","indexId":"b845","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","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":"845","title":"Guidebook of the western United States: Part F - The Southern Pacific lines, New Orleans to Los Angeles","docAbstract":"The Southern Pacific Railroad from New Orleans to Los Angeles, a distance of about 2,000 miles, passes through a region exhibiting a great variety of geographic and industrial conditions. The climate, especially the amount of precipitation, is the most influential factor in causing this variety.\r\n\r\nThe low Coastal Plain of southern Louisiana and eastern Texas, with ample rainfall and thick rich soils, is a province distinct in configuration, human occupations, and products. There are extensive swamps, prairies, and wooded areas, but a large part of the land is under cultivation, with sugarcane, cotton, and rice as the principal crops. The streams are wide and slow, the winter climate is mild, and the summer heat is tempered by breezes from the Gulf of Mexico. Flourishing towns occur at short intervals, and some of them are growing rapidly. The entire region is underlain by a great thickness of sand and clay of alluvial origin.\r\n\r\nIn central-eastern Texas the Coastal Plain is higher, the soil conditions are materially different, the streams run more swiftly, swamps become rare, and although much land is under cultivation, many areas are either in pasture or not cleared. The vegetation changes with change of soil and increase of altitude, and the crops are more diversified than in the lower parts of the Coastal Plain. The region is underlain by sandstone, shale, and other formations, which rise toward the west, cropping out in regular succession as they are crossed from east to west. Some of these formations are hard enough to make ridges and knobs, and there is general terracing at various levels. Parts of the highest lands are remnants of an old plain of former wide extent.\r\n\r\nBeyond San Antonio the traveler observes several changes in the general aspect of the country, for although the Coastal Plain extends west to Del Rio, there is both a gradual increase in elevation to about 1,000 feet and a marked diminution of rainfall to the west, which greatly affect landscape and industries. Cacti become larger and more abundant, and many special trees and plants are prevalent, notably the mesquite; forests diminish in density, and far to the west trees occur only in the bottom lands. Agriculture here depends largely on irrigation, and the raising of cattle, sheep, and goats is the dominant industry. The principal underlying rocks are shale, soft sandstone, and chalk, which do not make strong relief but produce hills and ridges of moderate height separated by wide valleys, which along the larger streams are bordered by bottom lands. Northwest of San Antonio the Coastal Plain gives place rather abruptly to the Edwards Plateau, owing to the rapid rise of hard limestones; from San Antonio to Del Rio this feature lies north of the railroad but is visible at many places.\r\n\r\nFor many miles west from Del Rio the railroad is on the plateau, which is floored by hard limestone and deeply trenched by the drainageways, notably by the canyons of the Devils River, the Rio Grande, and the Pecos River. In this district, where semiarid conditions prevail, vegetation is sparse and trees are mostly confined to valley bottoms except where the limestone supports a growth of juniper or live oak. The soil is thin, but it sustains grass and shrubs which afford good pasturage for many goats, sheep, and cattle. Owing to the gradual general rise of the strata to the west the land increases in elevation, and much of the plateau in south-central Texas is 2,000 feet above sea level in its eastern part and 3,000 feet in its western part. Near Sanderson this rise develops into the great dome of the Marathon uplift. The central part of this uplift is truncated, revealing a large area of closely folded Paleozoic rocks, making sharp ridges of the Appalachian type. The Edwards Plateau ends on the east side of this uplift. To the west is the Davis Mountain region, a wide province of volcanic rocks, characterized by rugged peaks and irregularly disposed ridges in great va","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Guidebook of the western United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b845","usgsCitation":"Darton, N.H., 1933, Guidebook of the western United States: Part F - The Southern Pacific lines, New Orleans to Los Angeles: U.S. Geological Survey Bulletin 845, 304 p., https://doi.org/10.3133/b845.","productDescription":"304 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":418962,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_114929.htm","linkFileType":{"id":5,"text":"html"}},{"id":164020,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0845/report-thumb.jpg"},{"id":92611,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0845/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.3,\n              34.34\n            ],\n            [\n              -118.3,\n              29.1\n            ],\n            [\n              -90,\n              29.1\n            ],\n            [\n              -90,\n              34.34\n            ],\n            [\n              -118.3,\n              34.34\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ac2b","contributors":{"authors":[{"text":"Darton, Nelson Horatio","contributorId":78307,"corporation":false,"usgs":true,"family":"Darton","given":"Nelson","email":"","middleInitial":"Horatio","affiliations":[],"preferred":false,"id":212555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159033,"text":"ar54 - 1933 - Fifty-fourth annual report of the Director of the Geological Survey","interactions":[],"lastModifiedDate":"2015-10-14T10:25:36","indexId":"ar54","displayToPublicDate":"1940-01-01T00:00:00","publicationYear":"1933","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":304,"text":"Annual Report","code":"AR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"54","title":"Fifty-fourth annual report of the Director of the Geological Survey","docAbstract":"<p>The appropriations made directly for the work of the Geological Survey for the fiscal year 1933 included 12 items, amounting, to&nbsp;$2,181,000. Of the balance remaining in the 1932 appropriation for&nbsp;topographic surveys, $150,000 was continued available for expenditure&nbsp;during the fiscal year 1933, and the sum of $284,400 was transferred&nbsp;to the Geological Survey under the provisions of section 317 of the&nbsp;legislative appropriation act of June 30, 1932, making a total of&nbsp;$2,615,400 available for expenditure. In addition, $12,424.50 for&nbsp;miscellaneous supplies was allotted from appropriations for the&nbsp;Interior Department.</p>","language":"English","publisher":"U.S. Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/ar54","usgsCitation":"Mendenhall, W.C., 1933, Fifty-fourth annual report of the Director of the Geological Survey: U.S. Geological Survey Annual Report 54, 33 p., https://doi.org/10.3133/ar54.","productDescription":"33 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309876,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ar/54/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":309868,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ar54.jpg"}],"country":"United 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,{"id":70207448,"text":"70207448 - 1933 - Classification and nomenclature of rock units","interactions":[],"lastModifiedDate":"2019-12-20T07:19:20","indexId":"70207448","displayToPublicDate":"1933-12-31T12:36:49","publicationYear":"1933","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":"Classification and nomenclature of rock units","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/GSAB-44-423","issn":"00167606","usgsCitation":"Ashley, G.H., Cheney, M., Galloway, J., Gould, C., Hares, C., Howell, B., Levorsen, A., Miser, H., Moore, R., Reeside, J., Rubey, W., Stanton, T.W., Stose, G.W., and Twenhofel, W., 1933, Classification and nomenclature of rock units: Economic Geology, v. 44, no. 2, p. 423-459, https://doi.org/10.1130/GSAB-44-423.","productDescription":"37 p. ","startPage":"423","endPage":"459","costCenters":[],"links":[{"id":370493,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"2","noUsgsAuthors":false,"publicationDate":"1933-04-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Ashley, G. H.","contributorId":106857,"corporation":false,"usgs":true,"family":"Ashley","given":"G.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":778089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cheney, M.G.","contributorId":221411,"corporation":false,"usgs":false,"family":"Cheney","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":778090,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, J.J.","contributorId":221412,"corporation":false,"usgs":false,"family":"Galloway","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":778091,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gould, C.N.","contributorId":221413,"corporation":false,"usgs":false,"family":"Gould","given":"C.N.","email":"","affiliations":[],"preferred":false,"id":778092,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hares, C.J.","contributorId":15251,"corporation":false,"usgs":true,"family":"Hares","given":"C.J.","affiliations":[],"preferred":false,"id":778093,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Howell, B.F.","contributorId":221414,"corporation":false,"usgs":false,"family":"Howell","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":778094,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Levorsen, A.I.","contributorId":221415,"corporation":false,"usgs":false,"family":"Levorsen","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":778095,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Miser, H. D.","contributorId":121305,"corporation":false,"usgs":true,"family":"Miser","given":"H. D.","affiliations":[],"preferred":false,"id":778096,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Moore, R.C.","contributorId":77180,"corporation":false,"usgs":true,"family":"Moore","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":778097,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Reeside, J.B. Jr.","contributorId":29787,"corporation":false,"usgs":true,"family":"Reeside","given":"J.B.","suffix":"Jr.","affiliations":[],"preferred":false,"id":778098,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Rubey, W.W.","contributorId":6426,"corporation":false,"usgs":true,"family":"Rubey","given":"W.W.","affiliations":[],"preferred":false,"id":778099,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Stanton, T. W.","contributorId":42997,"corporation":false,"usgs":true,"family":"Stanton","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":778100,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Stose, G. W.","contributorId":75892,"corporation":false,"usgs":true,"family":"Stose","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":778101,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Twenhofel, W.H.","contributorId":221416,"corporation":false,"usgs":false,"family":"Twenhofel","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":778102,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70221748,"text":"70221748 - 1933 - A new lepidolite deposit in Colorado","interactions":[],"lastModifiedDate":"2021-06-30T18:16:44.868768","indexId":"70221748","displayToPublicDate":"1933-12-01T13:09:11","publicationYear":"1933","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7141,"text":"Journal of the American Ceramic Society","active":true,"publicationSubtype":{"id":10}},"title":"A new lepidolite deposit in Colorado","docAbstract":"<p>A<span>&nbsp;newly discovered pegmatite&nbsp;</span>deposit<span>&nbsp;near Ohio City,&nbsp;</span>Colorado<span>, is chiefly&nbsp;</span>lepidolite<span>, massive topaz, beryl, and albite, with some samarskite and columbitc. Three parallel pegmatite dikes, cach about 11 fect thick and 300 feet long, cut black schist. The minerals arc banded parallel to walls, with the following succession from walls to center; fine‐grained albite and quartz, large plates of lcpidolite with crystals of topaz and beryl, fine‐grained lcpidolitc, and lamellar albite. An estimate of the bulk percentage of the various constituents heads to the belief that at least several thousand tons of each of the commercially vdluahle minerals await mining.&nbsp;</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1151-2916.1933.tb19223.x","usgsCitation":"Eckel, E., 1933, A new lepidolite deposit in Colorado: Journal of the American Ceramic Society, v. 16, no. 1-12, p. 239-245, https://doi.org/10.1111/j.1151-2916.1933.tb19223.x.","productDescription":"7 p.","startPage":"239","endPage":"245","costCenters":[],"links":[{"id":386908,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Colorado","city":"Ohio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.64154052734374,\n              38.56212645363985\n            ],\n            [\n              -106.56875610351562,\n              38.56212645363985\n            ],\n            [\n              -106.56875610351562,\n              38.581989399203906\n            ],\n            [\n              -106.64154052734374,\n              38.581989399203906\n            ],\n            [\n              -106.64154052734374,\n              38.56212645363985\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"16","issue":"1-12","noUsgsAuthors":false,"publicationDate":"2006-10-17","publicationStatus":"PW","contributors":{"authors":[{"text":"Eckel, E.B.","contributorId":22825,"corporation":false,"usgs":true,"family":"Eckel","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":818607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221690,"text":"70221690 - 1933 - Rôle of water conditions in the formation and differentiation of common (banded) coals","interactions":[],"lastModifiedDate":"2021-06-28T18:48:05.110726","indexId":"70221690","displayToPublicDate":"1933-09-01T13:38:11","publicationYear":"1933","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":"Rôle of water conditions in the formation and differentiation of common (banded) coals","docAbstract":"<p>No abstract available,&nbsp;</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.28.6.556","usgsCitation":"White, D., 1933, Rôle of water conditions in the formation and differentiation of common (banded) coals: Economic Geology, v. 28, no. 6, p. 556-570, https://doi.org/10.2113/gsecongeo.28.6.556.","productDescription":"15 p.","startPage":"556","endPage":"570","costCenters":[],"links":[{"id":386820,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"6","noUsgsAuthors":false,"publicationDate":"1933-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"White, D.","contributorId":39103,"corporation":false,"usgs":true,"family":"White","given":"D.","affiliations":[],"preferred":false,"id":818432,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70241236,"text":"70241236 - 1933 - Origin and structure of the Pensauken gravel","interactions":[],"lastModifiedDate":"2023-03-15T16:32:30.31428","indexId":"70241236","displayToPublicDate":"1933-09-01T11:29:13","publicationYear":"1933","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Origin and structure of the Pensauken gravel","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.2475/ajs.s5-26.153.300","usgsCitation":"Campbell, M.R., and Bascom, F., 1933, Origin and structure of the Pensauken gravel: American Journal of Science, v. 26, no. 153, p. 300-318, https://doi.org/10.2475/ajs.s5-26.153.300.","productDescription":"19 p.","startPage":"300","endPage":"318","costCenters":[],"links":[{"id":414235,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"153","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Campbell, Marius Robinson","contributorId":21202,"corporation":false,"usgs":true,"family":"Campbell","given":"Marius","email":"","middleInitial":"Robinson","affiliations":[],"preferred":false,"id":866610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bascom, Florence","contributorId":107668,"corporation":false,"usgs":true,"family":"Bascom","given":"Florence","email":"","affiliations":[],"preferred":false,"id":866611,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221691,"text":"70221691 - 1933 - Chloride and sulfate in rain water","interactions":[],"lastModifiedDate":"2021-06-28T18:54:11.390653","indexId":"70221691","displayToPublicDate":"1933-08-01T13:50:05","publicationYear":"1933","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1986,"text":"Industrial and Engineering Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Chloride and sulfate in rain water","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"American  Chemical Society","doi":"10.1021/ie50284a027","usgsCitation":"Collins, W.D., and Williams, K., 1933, Chloride and sulfate in rain water: Industrial and Engineering Chemistry, v. 25, no. 8, p. 944-945, https://doi.org/10.1021/ie50284a027.","productDescription":"2 p.","startPage":"944","endPage":"945","costCenters":[],"links":[{"id":386821,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"8","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Collins, W. D.","contributorId":37713,"corporation":false,"usgs":true,"family":"Collins","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":818433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, K.T.","contributorId":260663,"corporation":false,"usgs":false,"family":"Williams","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":818434,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221693,"text":"70221693 - 1933 - The lode deposits in the Boise Basin, Idaho","interactions":[],"lastModifiedDate":"2021-06-28T19:04:22.813601","indexId":"70221693","displayToPublicDate":"1933-06-01T14:01:17","publicationYear":"1933","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 lode deposits in the Boise Basin, Idaho","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.28.4.329","usgsCitation":"Ross, C.P., 1933, The lode deposits in the Boise Basin, Idaho: Economic Geology, v. 28, no. 4, p. 329-343, https://doi.org/10.2113/gsecongeo.28.4.329.","productDescription":"15 p.","startPage":"329","endPage":"343","costCenters":[],"links":[{"id":386825,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Idaho","city":"Boise","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.5869140625,\n              43.45291889355465\n            ],\n            [\n              -115.8837890625,\n              43.45291889355465\n            ],\n            [\n              -115.8837890625,\n              43.96119063892024\n            ],\n            [\n              -116.5869140625,\n              43.96119063892024\n            ],\n            [\n              -116.5869140625,\n              43.45291889355465\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"28","issue":"4","noUsgsAuthors":false,"publicationDate":"1933-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ross, C. P.","contributorId":91545,"corporation":false,"usgs":true,"family":"Ross","given":"C.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":818443,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221749,"text":"70221749 - 1933 - Specific yield determined from a Thiem's Pumping‐Test","interactions":[],"lastModifiedDate":"2021-06-30T18:55:53.005509","indexId":"70221749","displayToPublicDate":"1933-06-01T13:52:40","publicationYear":"1933","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":"Specific yield determined from a Thiem's Pumping‐Test","docAbstract":"<p>The specific yield of a water-bearing formation is defined as the ratio of (1) the volume of water, which after being saturated, it will yield by gravity to (2) its own volume (O. E. Meinzer, Outline of ground-water hydrology, U.S. Geol. Sur. Water-Supply Paper 494, p. 28, 1923). It is a measure of the quantity of water that a formation will yield when it is drained by lowering of the water-table. The determination of the specific yield is essential in many quantitative ground-water investigations.</p><p>In 1931 a pumping-test was made in the Platte River Valley, in Nebraska, to determine by Thiem's method the permeability of the water-bearing sand and gravel that underlie the Valley. This test, which constitutes a part of a cooperative investigation by the Conservation and Survey Department of the University of Nebraska and the United States Geological Survey, was briefly described in the 1932 Transactions of the American Geophysical Union (p. 393). The well was pumped continuously for 48 hours, and measurements of the discharge were made every 30 minutes. During the period of pumping and after pumping stopped about 5,000 measurements were made of the depths to the water-surfaces in 80 observation-wells, which were located on lines radiating from the pumped well to distances up to 1,200 feet. Instrumental levels were run to the measuring points on each of the wells so that the altitudes of the water-surfaces could be determined for any time. From the data obtained in this test the average coefficient of permeability was computed to be about 700. In the present paper a method is presented for determining the specific yield of the water-bearing material from the data collected in this test, and the results of the computations are given. This method for determining specific yield was suggested by Meinzer (O. E. Meinzer, Outline of methods for estimating ground-water supplies, U.S. Geol. Sur. water-Supply Paper 638-c, p. 136, 1932).</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00475","usgsCitation":"Wenzel, L., 1933, Specific yield determined from a Thiem's Pumping‐Test: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 475-477, https://doi.org/10.1029/TR014i001p00475.","productDescription":"3 p.","startPage":"475","endPage":"477","costCenters":[],"links":[{"id":386909,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, L.K.","contributorId":18733,"corporation":false,"usgs":true,"family":"Wenzel","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":818608,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221747,"text":"70221747 - 1933 - Further remarks on the Cripple Creek Volcano, Colorado","interactions":[],"lastModifiedDate":"2021-06-30T18:02:56.774297","indexId":"70221747","displayToPublicDate":"1933-06-01T12:58:44","publicationYear":"1933","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":"Further remarks on the Cripple Creek Volcano, Colorado","docAbstract":"<p><span>Structural evidence, particularly in the deeper mine‐workings, indicates that the&nbsp;</span>volcano<span>, which is of Tertiary age, was developed by explosive eruptions at a number of points along intersecting fissure‐systems that had been formed in pre‐Cambrian granite by east‐west compression, probably during the Laramide revolution. The volcanic breccia, which consists principally of phonolitic material, appears to fill several elongate or elliptical funnel‐shaped openings that coalesce upward and taper downward into roots. Local adjustments that followed the principal explosive eruptions developed fissure‐systems in the breccia parallel and transverse to the older fissure‐systems and permitted the intrusion of dikes and irregular masses of latite‐phonolite and syenite within the breccia mass. Mild regional readjustment, caused by compression in a nearly north‐south direction, ensued and reopened these fissure‐systems within and around the breccia mass. It was followed by the relatively widespread intrusion of dikes and irregular masses of phonolite. Local readjustment then recurred repeatedly, mainly along the master fissure‐systems, and was followed by three successive intrusions of alkaline basaltic dikes and finally by the formation of mineral veins.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00243-1","usgsCitation":"Loughlin, G.F., 1933, Further remarks on the Cripple Creek Volcano, Colorado: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 243-243, https://doi.org/10.1029/TR014i001p00243-1.","productDescription":"1 p.","startPage":"243","endPage":"243","costCenters":[],"links":[{"id":386907,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Colorado","city":"Cripple Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.31219482421875,\n              38.70480271154007\n            ],\n            [\n              -105.00732421875,\n              38.70480271154007\n            ],\n            [\n              -105.00732421875,\n              38.78620445725866\n            ],\n            [\n              -105.31219482421875,\n              38.78620445725866\n            ],\n            [\n              -105.31219482421875,\n              38.70480271154007\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Loughlin, G. F.","contributorId":8428,"corporation":false,"usgs":true,"family":"Loughlin","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":818606,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221746,"text":"70221746 - 1933 - Volcanic history of the Magdalena District, New Mexico","interactions":[],"lastModifiedDate":"2021-06-30T17:53:58.785368","indexId":"70221746","displayToPublicDate":"1933-06-01T12:46:43","publicationYear":"1933","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":"Volcanic history of the Magdalena District, New Mexico","docAbstract":"<p>The Magdalena District in central New Mexico comprises the Magdalena Range and Granite Mountain which are block mountains of the Basin Range type. They consist of Carboniferous sedimentary formations on a pre-Cambrian basement and are covered by Tertiary volcanic rocks.</p><p>Volcanism in the District was preceded by considerable faulting, tilting, and uplifting very probably in early Tertiary time. The initial volcanic extrusion consisted of latite flows and tuffs now resting unconformably on the Granite Mountain fault-block in the northern part of the District. Subsequent extrusions consisted of alternations of andesites, rhyolites, and latites, and have a minimum thickness of approximately 4,000 feet. Graben faulting, probably in compensation for the effusion of the large volumes of lava, followed and some of the major faults were subsequently the sites of the intrusion of monzonitic and granitic stocks. Late lamprophyre and white rhyolite dikes in large numbers intruded the intrusive as well as earlier extrusive and sedimentary rocks.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00250","usgsCitation":"Koschmann, A.H., 1933, Volcanic history of the Magdalena District, New Mexico: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 250-250, https://doi.org/10.1029/TR014i001p00250.","productDescription":"1 p.","startPage":"250","endPage":"250","costCenters":[],"links":[{"id":386906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"New Mexico","city":"Magdalena","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.5341796875,\n              34.02990029603907\n            ],\n            [\n              -107.0013427734375,\n              34.02990029603907\n            ],\n            [\n              -107.0013427734375,\n              34.31168124115256\n            ],\n            [\n              -107.5341796875,\n              34.31168124115256\n            ],\n            [\n              -107.5341796875,\n              34.02990029603907\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Koschmann, A. H.","contributorId":55455,"corporation":false,"usgs":true,"family":"Koschmann","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":818605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221745,"text":"70221745 - 1933 - Geophysical interpretation of ground‐water levels","interactions":[],"lastModifiedDate":"2021-06-30T16:31:51.062153","indexId":"70221745","displayToPublicDate":"1933-06-01T11:28:11","publicationYear":"1933","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":"Geophysical interpretation of ground‐water levels","docAbstract":"<p><span>The theory of rock‐pressure as a cause of artesian‐head dates back at least to early Grecian times. Thus the philosopher Thales, about 600 B.C., taught that the springs derive their&nbsp;</span>water<span>&nbsp;from the ocean through subterranean channels and that the&nbsp;</span>water<span>&nbsp;is lifted to the springs by rook‐pressure. The theory of rock‐pressure has had a number of recent advocates, chief among whom was the British geologist, J. W. Gregory, but apparently no effective attempt was made by any of them to apply critical data to the problem. In general, geologists and hydrologists have rejected rock‐pressure as a vague heresy and have assumed that the artesian formations function as perfectly rigid and inert containers, not recognizing the fact that the data in regard to the performance of wells appear to conflict with such an&nbsp;</span>interpretation<span>.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00036","usgsCitation":"Meinzer, O.E., 1933, Geophysical interpretation of ground‐water levels: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 36-37, https://doi.org/10.1029/TR014i001p00036.","productDescription":"2 p.","startPage":"36","endPage":"37","costCenters":[],"links":[{"id":386904,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221744,"text":"70221744 - 1933 - Some relations between ground‐water hydrology and oceanography","interactions":[],"lastModifiedDate":"2021-06-30T16:23:44.914113","indexId":"70221744","displayToPublicDate":"1933-06-01T11:19:31","publicationYear":"1933","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":"Some relations between ground‐water hydrology and oceanography","docAbstract":"<p>In many areas along the sea-coasts of the world the water-supply for human use is derived largely, and in some areas wholly, from underground sources. Because of the proximity to the ocean in these areas, in some respects the geologic and hydrologic conditions that govern the occurrence and movement of ground-water are quite different from those in inland areas, and to properly interpret them the ground-water hydrologist must avail himself of facts developed by the oceanographer.</p><p>These conditions are encountered in a marginal zone that in different localities may extend only a few feet or many miles inland from the coast, and presumably for greater or less distances out beneath the ocean. These special conditions have been recognized and extensively studied for many years, for example, in the lowland-area of Holland that lies between the Zuider Zee and the North Sea, and on Long Island, New York. Within recent years more or less attention has been given to these conditions in many of the coastal states of the United States, and in the Hawaiian Islands and Cuba. It is the purpose of this statement to indicate some of the problems of groundwater hydrology that are related to oceanography.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00030","usgsCitation":"Thompson, D., 1933, Some relations between ground‐water hydrology and oceanography: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 30-33, https://doi.org/10.1029/TR014i001p00030.","productDescription":"4 p.","startPage":"30","endPage":"33","costCenters":[],"links":[{"id":386903,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","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":818603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221743,"text":"70221743 - 1933 - Deep‐well salinity‐exploration","interactions":[],"lastModifiedDate":"2021-06-30T16:05:47.249003","indexId":"70221743","displayToPublicDate":"1933-06-01T11:00:20","publicationYear":"1933","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":"Deep‐well salinity‐exploration","docAbstract":"<p><span>One of the outstanding accomplishments of recent years in connection with the study of the geologic source of groundwater and the quality of water yielded by different formations has been the development of methods and equipment for the&nbsp;</span>exploration<span>&nbsp;of wells. The description and use of the&nbsp;</span>deep<span>‐</span>well<span>&nbsp;current‐meter on&nbsp;</span>well<span>‐</span>exploration<span>&nbsp;work in Hawaii and New Mexico has already appeared in published literature (John McCombs and A. G. Fiedler, Methods of exploring and repairing leaky artesian wells, U.S. Geol. Sur. Water‐Supply Paper 596, pp. 1–32, 1928) on hydrology but recent developments in the application of electrical conductivity‐measurements for determining the&nbsp;</span>salinity<span>&nbsp;of water in wells have not heretofore been presented. In addition to being of considerable scientific importance in connection with problems of ground‐water hydrology, the practical value of locating the place at which salt water is entering a&nbsp;</span>well<span>&nbsp;and contaminating a potable water‐supply is great. Such information may be the means of preventing the loss of large investments in industries, irrigation‐projects, and cities that are dependent upon&nbsp;</span>well<span>‐water supplies that may at some time become contaminated by salty or other highly mineralized water.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00478","usgsCitation":"Fiedler, A., 1933, Deep‐well salinity‐exploration: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 478-480, https://doi.org/10.1029/TR014i001p00478.","productDescription":"3 p.","startPage":"478","endPage":"480","costCenters":[],"links":[{"id":386902,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Nevada, Hawaii","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.984375,\n              31.42866311735861\n            ],\n            [\n              -103.22753906249999,\n              31.42866311735861\n            ],\n            [\n              -103.22753906249999,\n              37.09023980307208\n            ],\n            [\n              -108.984375,\n              37.09023980307208\n            ],\n            [\n              -108.984375,\n              31.42866311735861\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -161.54296875,\n              18.396230138028827\n            ],\n            [\n              -151.875,\n              18.396230138028827\n            ],\n            [\n              -151.875,\n              23.483400654325642\n            ],\n            [\n              -161.54296875,\n              23.483400654325642\n            ],\n            [\n              -161.54296875,\n              18.396230138028827\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Fiedler, A.G.","contributorId":11272,"corporation":false,"usgs":true,"family":"Fiedler","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":818602,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220434,"text":"70220434 - 1933 - Appendix B—investigations of underground‐water problems in California, New Mexico, and Oregon","interactions":[],"lastModifiedDate":"2021-05-13T13:15:14.949049","indexId":"70220434","displayToPublicDate":"1933-05-13T08:11:31","publicationYear":"1933","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":"Appendix B—investigations of underground‐water problems in California, New Mexico, and Oregon","docAbstract":"<div id=\"article__content\" class=\"col-sm-12 col-md-8 col-lg-8 article__content article-row-left\"><div class=\"article__body \"><div class=\"article-section__content en main\"><p><span>Investigations by the California Department of Public Works, Division of Water Resources</span><span>&nbsp;</span>(based on written communication from Harold Conkling, Deputy State Engineer)—the Division of Water Resources, California Department of Public Works, has in the past year conducted investigations of ground‐water problems in the great central valley of the State (California Trough); in the Salinas and Santa Clara Valleys of the central part of the State; also in the South Coastal Basin and in Ventura County, in southern California. In these investigations the Bureau of Agricultural Engineering of the United States Department of Agriculture, the Geological Survey of the United States Department of the Interior, and many local agencies have cooperated. In large part, the activities of the past year are continuations of investigations summarized in an earlier statement (A. M. Piper, Investigations of underground‐water problems in Arizona, California, New Mexico, and Oregon, National Research Council, Trans. Amer. Geophys. Union, 13th annual meeting, 308–309, 1932). Progress in 1932–35 is summarized in the following paragraphs.</p></div></div></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00374","usgsCitation":"Piper, A., 1933, Appendix B—investigations of underground‐water problems in California, New Mexico, and Oregon: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 374-377, https://doi.org/10.1029/TR014i001p00374.","productDescription":"9 p.","startPage":"374","endPage":"377","costCenters":[],"links":[{"id":385605,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, New Mexico, 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