{"pageNumber":"1871","pageRowStart":"46750","pageSize":"25","recordCount":46826,"records":[{"id":45365,"text":"b795F - 1927 - The Gilbert district, Nevada","interactions":[{"subject":{"id":45365,"text":"b795F - 1927 - The Gilbert district, Nevada","indexId":"b795F","publicationYear":"1927","noYear":false,"chapter":"F","title":"The Gilbert district, Nevada"},"predicate":"IS_PART_OF","object":{"id":34986,"text":"b795 - 1927 - Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels","indexId":"b795","publicationYear":"1927","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels"},"id":1}],"isPartOf":{"id":34986,"text":"b795 - 1927 - Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels","indexId":"b795","publicationYear":"1927","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels"},"lastModifiedDate":"2025-05-07T21:14:45.582495","indexId":"b795F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1927","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":"795","chapter":"F","title":"The Gilbert district, Nevada","docAbstract":"<p>The eastern part of the Monte Cristo Range, in Esmeralda County, Nev., has been prospected for many years, and one mine, the Carrie, was developed as early as 1890. The discovery of high-grade ore by the Gilbert brothers on the Last Hope claim in 1924 led to a boom during which the region was extensively prospected and claims were staked out covering not only the Gilbert district but another area from which the barren later andesite has been eroded, known as South Gilbert. The total production for the years 1917-1925, according to data furnished by Mr. V. C. Heikes, U. S. Bureau of Mines, amounted to $24,807, about two-thirds of which was from gold.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels (Bulletin 795)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b795F","usgsCitation":"Ferguson, H.G., 1927, The Gilbert district, Nevada: U.S. Geological Survey Bulletin 795, 21 p., https://doi.org/10.3133/b795F.","productDescription":"21 p.","startPage":"125","endPage":"145","numberOfPages":"23","costCenters":[],"links":[{"id":485534,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20447.htm","linkFileType":{"id":5,"text":"html"}},{"id":168312,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0795f/report-thumb.jpg"},{"id":94026,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0795f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Gilbert district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.23211669921876,\n              37.88352498087131\n            ],\n            [\n              -118.23211669921876,\n              38.53527591154413\n            ],\n            [\n              -117.13623046874999,\n              38.53527591154413\n            ],\n            [\n              -117.13623046874999,\n              37.88352498087131\n            ],\n            [\n              -118.23211669921876,\n              37.88352498087131\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698440","contributors":{"authors":[{"text":"Ferguson, Henry Gardiner","contributorId":72041,"corporation":false,"usgs":true,"family":"Ferguson","given":"Henry","email":"","middleInitial":"Gardiner","affiliations":[],"preferred":false,"id":231471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39384,"text":"pp147C - 1927 - American Tertiary mollusks of the genus Clementia","interactions":[],"lastModifiedDate":"2013-09-13T12:48:46","indexId":"pp147C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1927","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"147","chapter":"C","title":"American Tertiary mollusks of the genus Clementia","docAbstract":"Aside from its value as an aid in determining the age of Tertiary beds, the chief interest of the genus Clementia lies in the anomalous features of its present \nand former distribution. An attempt is made in this paper to trace its geologic history, to point out its paleobiologic significance, and to describe all the known American Tertiary species. The fossils from Colombia used in preparing this report were collected during explorations made under the direction of Dr. 0. B. Hopkins, chief geologist of the Imperial Oil Co. (Ltd.), who kindly donated them to the United States National Museum. Dr. T. Wayland Vaughan, of the Scripps Institution of Oceanography, furnished information relating to specimens collected by him in Mexico. Dr. Bruce L. Clark, of the University of California; Dr. G. Dallas Hanna, of the California Academy of Sciences; Dr. H. A. Pilsbry, of the Philadelphia Academy of Natural Sciences; and Dr. W. D. Matthew, of the American Museum of Natural History, generously loaned type specimens and other material. Doctor Clark and Doctor Hanna also gave information concerning the Tertiary species from California. Mr. Ralph B. Stewart, of the University of California, read the manuscript, and I have taken advantage of his suggestions. I am also indebted to Mr. L. R. Cox, of the British Museum, for information relating to the fossil species from Persia, Zanzibar, and Burma, and to Dr. Axel A. Olsson, of the International Petroleum Co., for data concerning undescribed Tertiary species from Peru.","language":"English","doi":"10.3133/pp147C","usgsCitation":"Woodring, W., 1927, American Tertiary mollusks of the genus Clementia: U.S. Geological Survey Professional Paper 147, 23 p., https://doi.org/10.3133/pp147C.","productDescription":"23 p.","startPage":"25","endPage":"47","numberOfPages":"27","costCenters":[],"links":[{"id":120094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0147c/report-thumb.jpg"},{"id":67092,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0147c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6868f7","contributors":{"authors":[{"text":"Woodring, W. P.","contributorId":48230,"corporation":false,"usgs":true,"family":"Woodring","given":"W. P.","affiliations":[],"preferred":false,"id":221390,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32869,"text":"pp148 - 1927 - Geology and ore deposits of the Leadville mining district, Colorado","interactions":[],"lastModifiedDate":"2016-01-14T15:47:07","indexId":"pp148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1927","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"148","title":"Geology and ore deposits of the Leadville mining district, Colorado","docAbstract":"<p>Adequate treatment of so large and so extensively developed a district as that of Leadville necessitates a voluminous report, in which the practical questions of prime interest to the commercial world can not be systematically answered until the data on which they depend are discussed. Many readers will no doubt wish to turn at once to the chapter on ore reserves, which will give them an appraisal of the district, without bothering with geologic detail. For those who wish a brief general account, a summary of the principal chapters of the report is presented below.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp148","usgsCitation":"Emmons, S.F., Irving, J., and Loughlin, G.F., 1927, Geology and ore deposits of the Leadville mining district, Colorado: U.S. Geological Survey Professional Paper 148, xvi, 368 p., https://doi.org/10.3133/pp148.","productDescription":"xvi, 368 p.","numberOfPages":"452","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":314383,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-15.pdf","text":"Plate 15","linkFileType":{"id":1,"text":"pdf"}},{"id":314384,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-16.pdf","text":"Plate 16","linkFileType":{"id":1,"text":"pdf"}},{"id":287224,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0148/report.pdf"},{"id":287225,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0148/report-thumb.jpg"},{"id":314378,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-07.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"}},{"id":314379,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-11.pdf","text":"Plate 11","linkFileType":{"id":1,"text":"pdf"}},{"id":314380,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-12.pdf","text":"Plate 12","linkFileType":{"id":1,"text":"pdf"}},{"id":314381,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-13.pdf","text":"Plate 13","linkFileType":{"id":1,"text":"pdf"}},{"id":314382,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-14.pdf","text":"Plate 14","linkFileType":{"id":1,"text":"pdf"}},{"id":314385,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-17.pdf","text":"Plate 17","linkFileType":{"id":1,"text":"pdf"}},{"id":314386,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-22.pdf","text":"Plate 22","linkFileType":{"id":1,"text":"pdf"}},{"id":314387,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-23.pdf","text":"Plate 23","linkFileType":{"id":1,"text":"pdf"}},{"id":314388,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-24.pdf","text":"Plate 24","linkFileType":{"id":1,"text":"pdf"}},{"id":314389,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-25.pdf","text":"Plate 25","linkFileType":{"id":1,"text":"pdf"}},{"id":314390,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-26.pdf","text":"Plate 26","linkFileType":{"id":1,"text":"pdf"}},{"id":314391,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-27.pdf","text":"Plate 27","linkFileType":{"id":1,"text":"pdf"}},{"id":314392,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-28.pdf","text":"Plate 28","linkFileType":{"id":1,"text":"pdf"}},{"id":314393,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-45.pdf","text":"Plate 45","linkFileType":{"id":1,"text":"pdf"}},{"id":314394,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-56.pdf","text":"Plate 56","linkFileType":{"id":1,"text":"pdf"}},{"id":314395,"rank":20,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0148/plate-57.pdf","text":"Plate 57","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Leadville","otherGeospatial":"Leadville Mining District","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.31,39.24 ], [ -106.31,39.25 ], [ -106.28,39.25 ], [ -106.28,39.24 ], [ -106.31,39.24 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684469","contributors":{"authors":[{"text":"Emmons, S. F.","contributorId":44593,"corporation":false,"usgs":true,"family":"Emmons","given":"S.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irving, J.D.","contributorId":70043,"corporation":false,"usgs":true,"family":"Irving","given":"J.D.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":209313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loughlin, G. F.","contributorId":8428,"corporation":false,"usgs":true,"family":"Loughlin","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209311,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45364,"text":"b795E - 1927 - Quicksilver deposits of the Pilot Mountains, Mineral County, Nevada","interactions":[{"subject":{"id":45364,"text":"b795E - 1927 - Quicksilver deposits of the Pilot Mountains, Mineral County, Nevada","indexId":"b795E","publicationYear":"1927","noYear":false,"chapter":"E","title":"Quicksilver deposits of the Pilot Mountains, Mineral County, Nevada"},"predicate":"IS_PART_OF","object":{"id":34986,"text":"b795 - 1927 - Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels","indexId":"b795","publicationYear":"1927","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels"},"id":1}],"isPartOf":{"id":34986,"text":"b795 - 1927 - Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels","indexId":"b795","publicationYear":"1927","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels"},"lastModifiedDate":"2025-05-07T21:12:13.566809","indexId":"b795E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1927","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":"795","chapter":"E","title":"Quicksilver deposits of the Pilot Mountains, Mineral County, Nevada","docAbstract":"<p>In the course of general geologic mapping of the Hawthorne quadrangle, in western Nevada, the writer undertook a short study of the quicksilver deposits of the Pilot Mountains. The work was. done under the supervision of Henry G. Ferguson, in charge of the field work in the Hawthorne quadrangle, and the writer was accompanied by L. B. Spencer, mining engineer, of Mina, Nev., whose intimate knowledge of the district greatly facilitated the study and to whom the writer is indebted for much valuable information. Data on the general geology of the district, collected by Messrs. Ferguson and Cathcart, were freely drawn upon.</p><p>The deposits of the Pilot Mountains were first described by Knopf* and later briefly by Ransome.<sup>2</sup></p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels (Bulletin 795)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b795E","usgsCitation":"Foshag, W.F., 1927, Quicksilver deposits of the Pilot Mountains, Mineral County, Nevada: U.S. Geological Survey Bulletin 795, 6 p., https://doi.org/10.3133/b795E.","productDescription":"6 p.","startPage":"118","endPage":"123","numberOfPages":"14","costCenters":[],"links":[{"id":485533,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20446.htm","linkFileType":{"id":5,"text":"html"}},{"id":94025,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0795e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168311,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0795e/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Mineral County","otherGeospatial":"Pilot Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.1414794921875,\n              38.18692647809604\n            ],\n            [\n              -118.1414794921875,\n              38.45412642738129\n            ],\n            [\n              -117.78579711914062,\n              38.45412642738129\n            ],\n            [\n              -117.78579711914062,\n              38.18692647809604\n            ],\n            [\n              -118.1414794921875,\n              38.18692647809604\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e74","contributors":{"authors":[{"text":"Foshag, William F.","contributorId":65130,"corporation":false,"usgs":true,"family":"Foshag","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":231470,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45363,"text":"b795D - 1927 - The brown iron ores of west-middle Tennessee","interactions":[{"subject":{"id":45363,"text":"b795D - 1927 - The brown iron ores of west-middle Tennessee","indexId":"b795D","publicationYear":"1927","noYear":false,"chapter":"D","title":"The brown iron ores of west-middle Tennessee"},"predicate":"IS_PART_OF","object":{"id":34986,"text":"b795 - 1927 - Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels","indexId":"b795","publicationYear":"1927","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels"},"id":1}],"isPartOf":{"id":34986,"text":"b795 - 1927 - Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels","indexId":"b795","publicationYear":"1927","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels"},"lastModifiedDate":"2025-05-07T21:10:10.903103","indexId":"b795D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1927","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":"795","chapter":"D","title":"The brown iron ores of west-middle Tennessee","docAbstract":"<p>A study of the brown iron ore deposits of west-middle Tennessee has been carried on recently under a cooperative agreement between the Tennessee State Geological Survey and the United States Geological Survey. A detailed report on the subject was submitted in the spring of 1925 to the State Survey for publication as a bulletin, and the writing of the present report was completed in March, 1926. The field work was done mainly between October 22 and November 2, 1921, and April 26 and July 18, 1923; but in October, 1924, a visit was made to the mine at Napier. The writer was assisted in the field in 1921 by. R. W. Smith, assistant geologist, and in 1923 by C. C. Anderson, topographer, both of the Tennessee Survey. Mr. Wilbur A. Nelson, State geologist at the time the work was in progress, visited several mines with the writer and on these occasions as well as many times during the preparation of the report rendered helpful suggestions and guidance. Mr. H. D. Miser, of the United States Geological Survey, State geologist from September 1, 1925, to July 1, 1926, who is especially familiar with the southern part of this area, also cooperated heartily in the preparation of this report; and Mr. H. W. Davis, of the United States Bureau of Mines, compiled the statistical data on iron ore and pig iron. To all these gentlemen the writer desires to express his appreciation. Acknowledgments are also due to the officials and employees of the iron mining and manufacturing companies and to people living in the vicinity of inactive mining properties for their courteous attention and for the large amount of information furnished.</p><p>In the present paper the general features of the region and of the iron-ore deposits are delineated, but only a few typical ore deposits in each county are described, as the State bulletin will contain detailed descriptions of all properties.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology (short papers and preliminary reports), 1927: Part I - Metals and nonmetals except fuels (Bulletin 795)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/b795D","usgsCitation":"Burchard, E.F., 1927, The brown iron ores of west-middle Tennessee: U.S. Geological Survey Bulletin 795, iv, 60 p., https://doi.org/10.3133/b795D.","productDescription":"iv, 60 p.","startPage":"53","endPage":"112","numberOfPages":"69","costCenters":[],"links":[{"id":485532,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20448.htm","linkFileType":{"id":5,"text":"html"}},{"id":94024,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0795d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168310,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0795d/report-thumb.jpg"}],"country":"United States","state":"Tennessee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.3740234375,\n              36.50301312197295\n            ],\n            [\n              -88.3740234375,\n              34.994003757575776\n            ],\n            [\n              -86.6876220703125,\n              34.994003757575776\n            ],\n            [\n              -86.6876220703125,\n              36.65079252503471\n            ],\n            [\n              -87.85491943359375,\n              36.63757008123925\n            ],\n            [\n              -87.85491943359375,\n              36.66180949419195\n            ],\n            [\n              -88.077392578125,\n              36.672824886786564\n            ],\n            [\n              -88.04443359375,\n              36.61332303966068\n            ],\n            [\n              -88.03070068359375,\n              36.54715598643371\n            ],\n            [\n              -88.04443359375,\n              36.50301312197295\n            ],\n            [\n              -88.3740234375,\n              36.50301312197295\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69844c","contributors":{"authors":[{"text":"Burchard, E. F.","contributorId":104020,"corporation":false,"usgs":true,"family":"Burchard","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":231469,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39358,"text":"pp132C - 1925 - Notes on the geology of Green River Valley between Green River, Wyoming, and Green River, Utah","interactions":[],"lastModifiedDate":"2013-09-13T14:32:30","indexId":"pp132C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"132","chapter":"C","title":"Notes on the geology of Green River Valley between Green River, Wyoming, and Green River, Utah","docAbstract":"During July, August, and part of September, 1922, I had the privilege of accompanying a party sent out jointly by the Utah Power & Light Co. and the United States Geological Survey to gather such data as were still needed to complete a study of the power resources of Green River between Green River, Wyo., and Green River, Utah. The chief deficiency to be supplied was a continuous topographic map of the valley in sufficient detail to permit calculation of the storage capacity of any reservoir site that might be used, the stream gradient, and similar features. Maps on a satisfactory scale of a number of isolated \nstretches of the river had already been made by public or private agencies, and it was necessary to verify them and connect them on a uniform datum. Inasmuch as it was deemed unlikely that a dam higher than 300 feet would be constructed anywhere on the part of the river to be examined, a plane 300 feet above the water surface was made the upper limit of mapping. Over such parts of the valley as had been mapped already the progress of the party was naturally very rapid, and even where no mapping had previously been done, the 300-foot limit set upon the work and the usual narrowness of the valley combined to reduce the extent of the area to be mapped, so that the speed maintained was relatively high. Under this condition of rapid movement it was seldom possible to make more than the most cursory examination of the rocks, though occasionally circumstances permitted more or less detailed observation. The notes here recorded are therefore mostly of a rather generalized character, but as they pertain in part to localities that are difficult of access and not often visited by geologists, and that are at the same time classic in the history of American geology, I venture to to record them for whatever value they may \nhave to other geologists.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter Contributions to General Geology, 1923-24","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","doi":"10.3133/pp132C","usgsCitation":"Reeside, J., 1925, Notes on the geology of Green River Valley between Green River, Wyoming, and Green River, Utah: U.S. Geological Survey Professional Paper 132, 16 p., https://doi.org/10.3133/pp132C.","productDescription":"16 p.","startPage":"35","endPage":"50","costCenters":[],"links":[{"id":172964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132c/report-thumb.jpg"},{"id":271209,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132c/report.pdf"}],"country":"United States","state":"Utah;Wyoming","otherGeospatial":"Green River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.13,37.75 ], [ -112.13,42.57 ], [ -109.43,42.57 ], [ -109.43,37.75 ], [ -112.13,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969b2","contributors":{"authors":[{"text":"Reeside, J.B. Jr.","contributorId":29787,"corporation":false,"usgs":true,"family":"Reeside","given":"J.B.","suffix":"Jr.","affiliations":[],"preferred":false,"id":221353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25059,"text":"wsp520A - 1925 - Variation in annual run-off in the Rocky Mountain region: Chapter A in <i>Contributions to the hydrology of the United States, 1923-1924</i>","interactions":[],"lastModifiedDate":"2013-12-13T12:45:32","indexId":"wsp520A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"520","chapter":"A","title":"Variation in annual run-off in the Rocky Mountain region: Chapter A in <i>Contributions to the hydrology of the United States, 1923-1924</i>","docAbstract":"<p>Records of run-off in the Rocky Mountain States since the nineties and for a few stations since the eighties afford a means of studying the variation in the annual run-off in this region. The data presented in this report show that the variation in annual run-off differs in different areas in the Rocky Mountain region, owing to the differences in the sources of the precipitation in these areas. Except in the drainage basins of streams in northern Montana the year of lowest run-off shown by the records was 1902, when the run-ff at one station was only 36 per cent of the mean run-ff for the periods covered by the several records available. The percentage variation of run-ff for streams in different parts of Colorado is less for any one year than that for streams in the mountain region as a whole, and for streams in the same major drainage basin the annual variation is markedly similar. The influence of topography upon variation in annual run-ff for streams in Colorado is marked, the streams that rise in the central mountain region having a smaller range in variation than the streams that rise on the eastern or western edges of the central mountain mass. The streams that rise on the plains just east of the mountains have a greater variation than those of any of the mountain groups.</p>\n<br/>\n<p>The ratio of any 10-year mean to the mean for the entire period covered by the records ranges from 72 to 133 per cent. For the South Platte, Arkansas, and Rio Grande the run-off during the nineties was below the normal, but since about 1903 it has been above normal. For the Cache la Poudre low-water periods occurred during the eighties and from 1905 to 1922, but during the nineties the run-off was above the normal.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1923-1924 (Water Supply Paper 520)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp520A","collaboration":"This report is Chapter A in <i>Contributions to the hydrology of the United States, 1923-1924</i>. For more information, see <a href=\"http://pubs.er.usgs.gov/publication/wsp520\" target=\"_blank\">Water Supply Paper 520</a>.","usgsCitation":"Follansbee, R., 1925, Variation in annual run-off in the Rocky Mountain region: Chapter A in <i>Contributions to the hydrology of the United States, 1923-1924</i>: U.S. Geological Survey Water Supply Paper 520, iv, 14 p., https://doi.org/10.3133/wsp520A.","productDescription":"iv, 14 p.","startPage":"1","endPage":"14","numberOfPages":"20","costCenters":[],"links":[{"id":156694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520a/report-thumb.jpg"},{"id":279500,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520a/report.pdf"}],"country":"United States","state":"Colorado;Montana;Wyoming","otherGeospatial":"Arkansas River Basin;Big Horn River Basin;Colorado River Basin;Green River Basin;Rocky Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,36.98 ], [ -116.05,49.0 ], [ -102.02,49.0 ], [ -102.02,36.98 ], [ -116.05,36.98 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602b56","contributors":{"authors":[{"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":193146,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25064,"text":"wsp520F - 1925 - Temperature of water available for industrial use in the United States: Chapter F in <i>Contributions to the hydrology of the United States, 1923-1924</i>","interactions":[{"subject":{"id":25064,"text":"wsp520F - 1925 - Temperature of water available for industrial use in the United States: Chapter F in <i>Contributions to the hydrology of the United States, 1923-1924</i>","indexId":"wsp520F","publicationYear":"1925","noYear":false,"chapter":"F","title":"Temperature of water available for industrial use in the United States: Chapter F in <i>Contributions to the hydrology of the United States, 1923-1924</i>"},"predicate":"IS_PART_OF","object":{"id":1737,"text":"wsp520 - 1925 - Contributions to the hydrology of the United States, 1923-1924","indexId":"wsp520","publicationYear":"1925","noYear":false,"title":"Contributions to the hydrology of the United States, 1923-1924"},"id":1}],"isPartOf":{"id":1737,"text":"wsp520 - 1925 - Contributions to the hydrology of the United States, 1923-1924","indexId":"wsp520","publicationYear":"1925","noYear":false,"title":"Contributions to the hydrology of the United States, 1923-1924"},"lastModifiedDate":"2017-09-11T19:06:02","indexId":"wsp520F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"520","chapter":"F","title":"Temperature of water available for industrial use in the United States: Chapter F in <i>Contributions to the hydrology of the United States, 1923-1924</i>","docAbstract":"<p>The importance of water supply as a limiting factor in industrial development is becoming more evident each year. The limitation in a particular instance may be the quantity of water available, the quality determined by the mineral matter in solution or in suspension or by organic pollution, or the temperature of the water. Generally it is a combination of two or more of these factors.</p><p>Many publications of the Geological Survey give data in regard to the quantity of surface water and ground water obtainable at different points. Other publications of this Survey and of other organizations give data on the quality of waters available for industrial use. The temperature of these waters is discussed in the present report.</p><p>Data in regard to ground water have been obtained from Geological Survey water-supply papers, from the publications indicated in footnotes, and from an unpublished compilation of temperature records prepared by C. E. Van Orstrand, of the Geological Survey, in connection with studies of deep earth temperature. Data on temperature of surface water have been obtained mainly from officials of waterworks, as noted in the accompanying table. Data on air temperature have been obtained from reports of the United States Weather Bureau. The maps showing temperature of ground water and surface water (Pls. VIII and IX) are taken directly from Weather Bureau charts of temperature distribution.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1923-1924 (Water Supply Paper 520)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp520F","collaboration":"This report is Chapter F in <i>Contributions to the hydrology of the United States, 1923-1924</i>. For more information, see <a href=\"http://pubs.er.usgs.gov/publication/wsp520\" target=\"_blank\">Water Supply Paper 520</a>.","usgsCitation":"Collins, W.D., 1925, Temperature of water available for industrial use in the United States: Chapter F in <i>Contributions to the hydrology of the United States, 1923-1924</i>: U.S. Geological Survey Water Supply Paper 520, iv, 8 p., https://doi.org/10.3133/wsp520F.","productDescription":"iv, 8 p.","startPage":"97","endPage":"104","numberOfPages":"16","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":157222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520f/report-thumb.jpg"},{"id":279497,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520f/report.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685812","contributors":{"authors":[{"text":"Collins, W. D.","contributorId":37713,"corporation":false,"usgs":true,"family":"Collins","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":193152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25063,"text":"wsp520E - 1925 - The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle","interactions":[{"subject":{"id":25063,"text":"wsp520E - 1925 - The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle","indexId":"wsp520E","publicationYear":"1925","noYear":false,"chapter":"E","title":"The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle"},"predicate":"IS_PART_OF","object":{"id":1737,"text":"wsp520 - 1925 - Contributions to the hydrology of the United States, 1923-1924","indexId":"wsp520","publicationYear":"1925","noYear":false,"title":"Contributions to the hydrology of the United States, 1923-1924"},"id":1}],"isPartOf":{"id":1737,"text":"wsp520 - 1925 - Contributions to the hydrology of the United States, 1923-1924","indexId":"wsp520","publicationYear":"1925","noYear":false,"title":"Contributions to the hydrology of the United States, 1923-1924"},"lastModifiedDate":"2021-08-30T21:13:52.498817","indexId":"wsp520E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"520","chapter":"E","title":"The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle","docAbstract":"<p>The Dakota sandstone and the overlying dense plastic shales form the most remarkable artesian basin in the United States with respect to its great extent, the long distances through which its water has percolated from the outcrops of the sandstone in the western mountains to the areas of artesian flow, and especially the tremendous pressure under which the water in the sandstone was originally by thick and continuous cover of impermeable shales. In 1882 a well was drilled to the Dakota sandstone at Aberdeen, S. Dak., by the Chicago, Milwaukee & St. Paul Railway Co. This well was reported by Nettleton<sup>1</sup> to have been \"the first bore put down which reached the artesian basin of the Dakotas.\" In 1896 Darton<sup>2</sup> estimated that about 400 artesian wells had been drilled to the Dakota sandstone, presumably in South Dakota and adjacent parts of the artesian basin in North Dakota which he investigated.<sup>3</sup> The strongest of these wells had pressures ranging from 100 to more than 200 pounds to the square inch and flows ranging from 1,000 to more than 4,000 gallons a minute.</p>\n<br/>\n<p>The present brief paper is based chiefly on the data that have been obtained in the successive surveys in regard to about 230 artesian wells in or near the Edgeley quadrangle. A table of these well data is on file in the United States Geological Survey and is to be published in the detailed report on the geology and hydrology of the Edgeley and La Moure quadrangles that has been prepared by Mr. Hard. The well data obtained by Mr. Hard have already been published in a report prepared by him in his capacity as State flood-control engineer.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1923-1924 (Water Supply Paper 520)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp520E","usgsCitation":"Meinzer, O.E., and Hard, H.A., 1925, The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle: U.S. Geological Survey Water Supply Paper 520, iv, 23 p., https://doi.org/10.3133/wsp520E.","productDescription":"iv, 23 p.","startPage":"73","endPage":"95","numberOfPages":"31","costCenters":[],"links":[{"id":388207,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24584.htm"},{"id":156698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520e/report-thumb.jpg"},{"id":279498,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520e/report.pdf"}],"country":"United States","state":"North Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -99.0,46.0 ], [ -99.0,46.5 ], [ -98.5,46.5 ], [ -98.5,46.0 ], [ -99.0,46.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6697cb","contributors":{"authors":[{"text":"Meinzer, Oscar E.","contributorId":83436,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hard, Herbert A.","contributorId":88205,"corporation":false,"usgs":true,"family":"Hard","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193151,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34042,"text":"b770 - 1924 - The data of geochemistry","interactions":[],"lastModifiedDate":"2018-02-19T21:34:48","indexId":"b770","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1924","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":"770","title":"The data of geochemistry","docAbstract":"<p><span>Upon the subject of geochemistry a vast literature exists, but it is widely scattered and portions of it are difficult of access. The general treatises, like the classical works of Bischof and of Koth, are not recent, and great masses of modern data are as yet uncorrelated. The American material alone is singularly rich, but most of it has been accumulated since Roth's treatise was published. The science of chemistry, moreover, has undergone great changes during the last 25 years, and many subjects now appear under new and generally unfamiliar aspects. The methods and principles of physical chemistry are being more and more applied to the solution of geochemical problems,</span><sup>1</sup><span> as is shown by the well-known researches of Van't Hoff upon the Stassfurt salts and the magmatic studies of Vogt, Doelter, and others. The great work in progress at the geophysical laboratory of the Carnegie Institution is another illustration of the change now taking place in geochemical investigation. To bring some of the data together, to formulate a few of the problems and to present certain general conclusions in their modern form are the purposes of this memoir. It is not an exhaustive monograph upon geochemistry, but rather a critical summary of what is now known, and a guide to the more important literature of the subject. If it does no more than to make existing data available to the reader, its preparation will be justified.</span></p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b770","usgsCitation":"Clarke, F.W., 1924, The data of geochemistry (5th ed.): U.S. Geological Survey Bulletin 770, 841 p., https://doi.org/10.3133/b770.","productDescription":"841 p.","numberOfPages":"841","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":92558,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0770/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0770/report-thumb.jpg"}],"edition":"5th ed.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668895","contributors":{"authors":[{"text":"Clarke, Frank Wigglesworth","contributorId":88798,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank","email":"","middleInitial":"Wigglesworth","affiliations":[],"preferred":false,"id":212362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39365,"text":"pp135 - 1924 - The composition of the river and lake waters of the United States","interactions":[],"lastModifiedDate":"2017-09-11T19:21:06","indexId":"pp135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1924","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"135","title":"The composition of the river and lake waters of the United States","docAbstract":"<p>In the summer of 1903 the late Richard B. Dole, chemist of the water-resources branch of the United States Geological Survey, began a systematic investigation of the composition of the river and lake waters of the United States. His plan, which developed gradually, was to have analyses made of the different waters in such a manner as to give the average composition of each one for an entire year. For a few waters, such completeness was impracticable, the analyses covered only part of a year, but even in these waters the data obtained were of much value. As a rule, samples of each water were collected day by day. They were then mixed in sets of ten and analyzed, so that for each river or lake from 34 to 37 analyses were made. For the Mississippi above New Orleans composite analyses were made in sets of seven, giving 52 analyses from which to compute the average. For the Great Lakes, however, only monthly samples were taken, for the reason that their waters vary so little in composition that greater elaboration was not necessary. Some of the larger rivers were treated even more thoroughly; their average composition was determined at more than one point – the Mississippi at six points. For some rivers the analyses cover two years of collection, and for the data, received from a contributor not connected with the Geological Survey, three years.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp135","usgsCitation":"Clarke, F.W., 1924, The composition of the river and lake waters of the United States: U.S. Geological Survey Professional Paper 135, iv, 199 p., https://doi.org/10.3133/pp135.","productDescription":"iv, 199 p.","numberOfPages":"203","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science 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,{"id":2434,"text":"wsp492 - 1923 - Summary of hydrometric data in Washington, 1878-1919","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp492","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1923","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":"492","title":"Summary of hydrometric data in Washington, 1878-1919","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp492","usgsCitation":"Parker, G.L., and Lee, L., 1923, Summary of hydrometric data in Washington, 1878-1919: U.S. Geological Survey Water Supply Paper 492, vii, [1], 363 p. :VIII pl., fold. map, tables. ;23 cm., https://doi.org/10.3133/wsp492.","productDescription":"vii, [1], 363 p. :VIII pl., fold. map, tables. ;23 cm.","costCenters":[],"links":[{"id":139061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0492/report-thumb.jpg"},{"id":247214,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0492/plate-9.pdf","size":"5149","linkFileType":{"id":1,"text":"pdf"}},{"id":28504,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0492/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699135","contributors":{"authors":[{"text":"Parker, Glenn Lane","contributorId":66661,"corporation":false,"usgs":true,"family":"Parker","given":"Glenn","email":"","middleInitial":"Lane","affiliations":[],"preferred":false,"id":145193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Lasley","contributorId":35711,"corporation":false,"usgs":true,"family":"Lee","given":"Lasley","email":"","affiliations":[],"preferred":false,"id":145192,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2283,"text":"wsp489 - 1923 - The occurrence of ground water in the United States, with a discussion of principles","interactions":[],"lastModifiedDate":"2017-09-11T19:31:20","indexId":"wsp489","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1923","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":"489","title":"The occurrence of ground water in the United States, with a discussion of principles","docAbstract":"<p>The writer has planned and partly prepared a series of six papers on ground water in the United States. These papers are to deal with (1) occurrence, (2) origin, discharge, and quantity, (3) movement and head, (4) quality, (5) recovery and use, and (6) ground-water provinces. The present paper is the first of the series.</p><p>The writer is indebted to many colaborers for assistance in preparing this paper, especially to the following members of the United States Geological Survey: M. R. Campbell, who read the entire paper; E. W. Shaw, C. E. Van Orstrand, A. F. Melcher, and C. K. Wentworth, who examined Chapter I; W. C. Alden, who examined Chapters II and IV with special reference to their statements regarding glacial geology; E. S. Larsen, who examined a part of Chapter II; G. W. Stosfi, who examined Chapter III; T. W. Stanton, who examined Chapter IV; L. W. Stephenson, who examined the parts of Chapter IV that relate to the Coastal Plain; C. W. Cooke, who furnished many unpublished data on the geology of the Coastal Plain; Miss M. G. Wilmarth, who gave valuable help in compiling the geologic sections; D. G. Thompson and Miss Norah E. Dowell, who furnished original data on the mechanical composition and porosity of various sedimentary materials; B. H. Lane, who made valuable criticisms of the text; and Martin Solem, who had charge of the preparation of the illustrations. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/wsp489","usgsCitation":"Meinzer, O.E., 1923, The occurrence of ground water in the United States, with a discussion of principles: U.S. Geological Survey Water Supply Paper 489, xi, 321 p., https://doi.org/10.3133/wsp489.","productDescription":"xi, 321 p.","numberOfPages":"373","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":137634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0489/report-thumb.jpg"},{"id":28082,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0489/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6494d9","contributors":{"authors":[{"text":"Meinzer, Oscar Edward","contributorId":12020,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":144951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33920,"text":"b707 - 1922 - Guidebook of the western United States: Part E - The Denver & Rio Grande Western route","interactions":[],"lastModifiedDate":"2023-07-14T18:30:15.331703","indexId":"b707","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1922","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":"707","title":"Guidebook of the western United States: Part E - The Denver & Rio Grande Western route","docAbstract":"The United States of America comprise an area so vast in extent and so diverse in natural features as well as in characters due to human agency that the American citizen who knows thoroughly his own country must have traveled widely and observed wisely. To 'know America first' is a patriotic obligation, but to meet this obligation the railroad traveler needs to have his eyes directed toward the more important or essential things within his field of vision and then to have much that he sees explained by what is unseen in the swift passage of the train. Indeed, many things that attract his attention are inexplicable except as the story of the past is available to enable him to interpret the present. Herein lie the value and the charm of history, whether human or geologic.\r\n\r\nThe present stimulus given to travel in the home country will encourage many thousands of Americans to study geography at first hand. To make this study most profitable the traveler needs a handbook that will answer the questions that come to his mind so readily along the way. Furthermore, the aim of such a guide should be to stimulate the eye in the selection of the essentials in the scene that so rapidly unfolds itself in the crossing of the continent. In recognition of the opportunity to render service of this kind to an unusually large number of American citizens, as well as to visitors from other countries, the United States Geological Survey has published a series of guidebooks covering four of the older railroad routes west of the Mississippi. The present volume is an addition to this series and covers one of the finest scenic routes of the continent.\r\n\r\nThese books are educational in purpose, but the method adopted is to entertain the traveler by making more interesting what he sees from the car window. The plan of the series is to present authoritative information that may enable the reader to realize adequately the scenic and material resources of the region he is traversing, to comprehend correctly the basis of its development, and above all to appreciate keenly the real value of the country he looks out upon, not as so many square miles of territory represented on the map in a railroad folder by meaningless spaces, but rather as land - real estate, if you please - varying widely in present appearance because differing largely in its history, and characterized by even greater variation in values because possessing diversified natural resources. One region may be such as to afford a livelihood for only a pastoral people; another may present opportunity for intensive agriculture; still another may contain hidden stores of mineral wealth that may attract large industrial development; and, taken together, these varied resources afford, the promise of long-continued prosperity for this or that State.\r\n\r\nItems of interest in civic development or references to significant epochs in the record of discovery and settlement may be interspersed. with explanations of mountain and valley or statements of geologic history. In a broad way the story of the West is a unit, and every chapter should be told in order to meet fully the needs of the tourist who aims to understand all that he sees. To such a traveler-reader this series of guidebooks is addressed.\r\n\r\nTo this interpretation of our own country the United States Geological Survey brings the accumulated data of decades of pioneering investigation, and the present contribution is only one type of return to the public which has supported this scientific work under the Federal Government - a by-product of research.\r\n\r\nIn the preparation of the description of the country traversed by the Denver & Rio Grande Western Route the geographic and geologic information already published as well as unpublished material in the possession of the Geological Survey has been utilized, but to supplement this material Mr. Campbell made a field examination of the entire route in 1915-1916. Information has been furnished by others,","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/b707","usgsCitation":"Campbell, M., 1922, Guidebook of the western United States: Part E - The Denver & Rio Grande Western route: U.S. Geological Survey Bulletin 707, viii, 266 p., https://doi.org/10.3133/b707.","productDescription":"viii, 266 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":163438,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0707/report-thumb.jpg"},{"id":92487,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0707/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":418961,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_114928.htm","linkFileType":{"id":5,"text":"html"}}],"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              -112.3,\n              41\n            ],\n            [\n              -112.3,\n              38.15\n            ],\n            [\n              -104.5,\n              38.15\n            ],\n            [\n              -104.5,\n              41\n            ],\n            [\n              -112.3,\n             41\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64af11","contributors":{"authors":[{"text":"Campbell, Marius R.","contributorId":103337,"corporation":false,"usgs":true,"family":"Campbell","given":"Marius R.","affiliations":[],"preferred":false,"id":212172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174800,"text":"70174800 - 1921 - Surface waters of Kansas, 1895-1919","interactions":[],"lastModifiedDate":"2016-07-15T14:34:19","indexId":"70174800","displayToPublicDate":"1999-06-16T14:30:00","publicationYear":"1921","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Surface waters of Kansas, 1895-1919","docAbstract":"<p>Kansas is preeminently an agricultural state. According to the United States census of 1910, the area in farms was 43,384,799 acres, or 67,789 square miles, 83 per cent of the total area of the state &mdash;82,158 square miles.</p>\n<p>The products of these farms rank high in value among those of farms in other states, as shown by comparative statistics compiled by the United States Department of Agriculture, Bureau of Crop Estimates. For the period from 1913 to 1917 Kansas ranked ninth of the states of the United States in the value of all crops raised, exclusive of livestock; in 1919 Kansas ranked fifth. In livestock Kansas ranked sixth in 1918 and eighth in 1919.</p>\n<p>Climatic conditions have largely dominated agricultural development in Kansas. Early ventures in dry farming in western Kansas, encouraged by a succession of rainy seasons, resulted in disheartening disasters, due to the dry seasons that followed. Throughout that region the farmers have gradually utilized the surface and underground waters for irrigation to provide against this deficiency of rainfall.</p>\n<p>The floods that have occurred in the valleys of eastern\" Kansas at frequent intervals during the past twenty years have been the subject of much investigation by state and Federal organizations. In 1844 and 1903 exceptionally disastrous floods occurred in the Kansas (Kaw) valley. Floods that were of lesser magnitude, but that caused widespread loss and injury to property, have occurred in other years, the most recent being the flood of 1915. Much of the cultivated land in these valleys lies along fertile river bottoms that are annually liable to overflow, and the control of the flood waters on these rivers and their tributaries is therefore one of the problems arising from unfavorable climate that demand early solution.</p>\n<p>In view of the increasing demand for water for domestic service and fire protection, the need of determining whether the supply is adequate for rapidly growing centers of population throughout the state has recently been impressed very strongly upon a great many communities. The dependability of available sources of water supply during seasons of drought is fully as important as investigations of flood problems.</p>\n<p>Practical solutions of the many local and statewide water problems, such as flood protection, flood prevention, domestic water supply, drainage, irrigation, and water power, depend largely on a thorough knowledge of certain physical data relating to water resources.</p>\n<p>Hydrologic conditions differ widely in the different drainage basins, so that long-time investigations of stream-flow phenomena in each basin, as well as long-time investigations of meteorologic conditions over the state, are essential in the formulation of comprehensive plans to meet specific water problems.</p>\n<p>The collection of long-time records of stream-flow in Kansas which is published in this volume has been prepared for the use of those who are concerned with the different phases of the utilization of water in the state.</p>","language":"English","publisher":"Kansas Water Commission, Printed by Kansas state printing plant, B. P. 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,{"id":34165,"text":"b701 - 1920 - Geothermal data of the United States, including many original determinations of underground temperature","interactions":[],"lastModifiedDate":"2017-09-11T19:34:12","indexId":"b701","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1920","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":"701","title":"Geothermal data of the United States, including many original determinations of underground temperature","docAbstract":"<p>The purpose of this report is to present all available published data bearing on the rate of increase of underground temperature with increasing depth in the United States, together with several hundred original observations by myself and my associates. A canvass of the governmental, State, and serial publications has yielded many records of temperature of flowing wells and also a few observations made with thermometers in borings and deep mines. Additional data on temperature of flows have been given by correspondents. Some of the data, especially those relating to flows from wells, may not be reliable, and as a rule these could not be discriminated. Many records are omitted because no facts are available as to the source of flow. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b701","usgsCitation":"Darton, N.H., 1920, Geothermal data of the United States, including many original determinations of underground temperature: U.S. Geological Survey Bulletin 701, 97 p., https://doi.org/10.3133/b701.","productDescription":"97 p.","numberOfPages":"98","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":163499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0701/report-thumb.jpg"},{"id":92604,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0701/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b06f","contributors":{"authors":[{"text":"Darton, Nelson Horatio","contributorId":78307,"corporation":false,"usgs":true,"family":"Darton","given":"Nelson","email":"","middleInitial":"Horatio","affiliations":[],"preferred":false,"id":212553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34041,"text":"b695 - 1920 - The data of geochemistry (fourth edition)","interactions":[],"lastModifiedDate":"2012-02-02T00:09:31","indexId":"b695","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1920","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":"695","title":"The data of geochemistry (fourth edition)","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/b695","usgsCitation":"Clarke, F.W., 1920, The data of geochemistry (fourth edition): U.S. Geological Survey Bulletin 695, 832 p., https://doi.org/10.3133/b695.","productDescription":"832 p.","costCenters":[],"links":[{"id":92557,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0695/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0695/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6688f9","contributors":{"authors":[{"text":"Clarke, Frank Wigglesworth","contributorId":88798,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank","email":"","middleInitial":"Wigglesworth","affiliations":[],"preferred":false,"id":212361,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35797,"text":"b688 - 1919 - The oil fields of Allen County, Kentucky, with notes on the oil geology of adjoining counties","interactions":[],"lastModifiedDate":"2017-06-06T10:28:41","indexId":"b688","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1919","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":"688","title":"The oil fields of Allen County, Kentucky, with notes on the oil geology of adjoining counties","docAbstract":"<p>This report is based on a reconnaissance investigation of the oil field of Allen County, Ky., which was part of a broader study of the oil and gas fields of Kentucky, Tennessee, and Alabama, on which a general report is planned. Most of the field work was done by Mr. Mather, who spent three and a half weeks in and around the county. Mr. Shaw visited Scottsville, the county seat of Allen County, a few years ago and spent a few days in that vicinity at the beginning of the recent field work, which extended from the middle of April to the middle of May, 1917 He prepared also the first draft of the report and reviewed the literature, including reports in oil and gas journals.</p><p>The purpose of the field work was to investigate the geology of the county, particularly the structure or lay of the oil-bearing strata and the results of drilling to date. Structural conditions in the producing fields were determined by running level lines to the wells and correlating the data recorded in the well logs generously furnished by the operators. Traverses were made of outcrops, and observations of the dip and strike were made in different parts of the county. Lack of a topographic base map and of time and funds for making an accurate topographic survey render the results of the work somewhat incomplete, but it is hoped they will form a valuable contribution to the knowledge of the geology of this relatively little known region, for little detailed geologic work has been done heretofore within 50 miles of Scottsville.</p><p>The dips are generally too low to be read by the clinometer, but in some localities unmistakable dips can be observed in extensive outcrops along creek banks and can be measured with a level or hand transit. Few of the beds of this region can be followed any considerable distance, though by means of fossils the stratigraphic position of beds outcropping many miles apart can be determined&nbsp;within a few feet. The black shale is the best horizon marker, but it outcrops in only a few places and is reached in only a few wells outside the oil fields.</p><p>The field work thus consisted largely in observations on out-<br>, cropping beds in different localities and in estimating the altitude of those identified, in collecting fossils for use in future detailed work, and in obtaining from oil operators data concerning the wells and their output. It included the determination of the general lay of the rocks in the county and surrounding territory and details of structure in certain areas. The rocks lie so nearly flat that without topographic data only the general dip could be made out for a large part of the area examined. A complete set of logs of wildcat wells in the region would have thrown much light on the structure and oil possibilities, but little is known of many of the earlier wells drilled in the region, especially of those altogether unsuccessful. An unsuccessful test is soon forgotten, though the data thus obtained concerning the depth at which different beds were found and the yield of porous strata, whether water, oil, or gas, is of great value to the geologist and oil prospector.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b688","usgsCitation":"Shaw, E.W., and Mather, K., 1919, The oil fields of Allen County, Kentucky, with notes on the oil geology of adjoining counties: U.S. Geological Survey Bulletin 688, 126 p., https://doi.org/10.3133/b688.","productDescription":"126 p.","costCenters":[],"links":[{"id":342141,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/688/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/688/b688.jpg"}],"country":"United States","state":"Kentucky","county":"Allen County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-86.4054,36.7763],[-86.2633,36.873],[-86.2651,36.8757],[-86.2623,36.8848],[-86.2675,36.8866],[-86.2681,36.892],[-86.2653,36.8938],[-86.2612,36.892],[-86.2595,36.8939],[-86.256,36.8912],[-86.2514,36.8916],[-86.2492,36.8966],[-86.24,36.8944],[-86.2394,36.899],[-86.2348,36.8981],[-86.2343,36.9067],[-86.2291,36.9072],[-86.2257,36.9122],[-86.2194,36.9113],[-86.2153,36.9046],[-86.2124,36.9037],[-86.2067,36.9073],[-86.2033,36.9132],[-86.2039,36.9169],[-86.2079,36.9187],[-86.2103,36.9259],[-86.2058,36.9327],[-86.1989,36.9355],[-86.1983,36.9314],[-86.1954,36.9273],[-86.1913,36.9233],[-86.1878,36.9215],[-86.1815,36.9243],[-86.1707,36.9347],[-86.1661,36.9343],[-86.1609,36.9298],[-86.1602,36.9248],[-86.1631,36.9234],[-86.1659,36.9198],[-86.1728,36.9184],[-86.1763,36.9143],[-86.1687,36.9085],[-86.163,36.9067],[-86.1572,36.9067],[-86.1497,36.9104],[-86.1492,36.9135],[-86.1521,36.9163],[-86.1522,36.9226],[-86.1505,36.9271],[-86.1476,36.9294],[-86.1453,36.9294],[-86.1361,36.9322],[-86.135,36.9304],[-86.1372,36.9254],[-86.1417,36.9145],[-86.1342,36.9037],[-86.1422,36.9009],[-86.1468,36.8968],[-86.1415,36.8923],[-86.1306,36.896],[-86.1243,36.8951],[-86.115,36.8806],[-86.1138,36.8752],[-86.1097,36.872],[-86.1097,36.868],[-86.1051,36.8643],[-86.1016,36.8639],[-86.0993,36.8648],[-86.0976,36.8694],[-86.1081,36.8802],[-86.1087,36.8838],[-86.1058,36.8893],[-86.0979,36.9002],[-86.0875,36.8998],[-86.0766,36.9026],[-86.0691,36.9017],[-86.0651,36.8981],[-86.0645,36.894],[-86.0667,36.8908],[-86.0685,36.8908],[-86.0673,36.8945],[-86.0771,36.8926],[-86.0782,36.8912],[-86.077,36.8817],[-86.0701,36.8777],[-86.0723,36.8718],[-86.0746,36.8736],[-86.0764,36.8731],[-86.078,36.8672],[-86.0752,36.8645],[-86.078,36.8554],[-86.0715,36.8437],[-86.0617,36.8378],[-86.0559,36.8292],[-86.0656,36.8233],[-86.0684,36.8119],[-86.0707,36.811],[-86.0718,36.8078],[-86.0701,36.8056],[-86.054,36.8093],[-86.0465,36.8075],[-86.0477,36.8039],[-86.0505,36.8034],[-86.0516,36.7943],[-86.0499,36.7934],[-86.0459,36.7953],[-86.043,36.7921],[-86.0395,36.7908],[-86.0401,36.7876],[-86.036,36.7853],[-86.0349,36.7803],[-86.04,36.7781],[-86.0486,36.7789],[-86.0526,36.7753],[-86.0509,36.7721],[-86.0411,36.7676],[-86.0393,36.7645],[-86.0376,36.7599],[-86.0347,36.7599],[-86.0336,36.7618],[-86.0296,36.764],[-86.0066,36.7601],[-86.002,36.7587],[-85.9927,36.7501],[-85.9829,36.7411],[-85.977,36.7225],[-85.977,36.7158],[-85.9636,36.6909],[-85.9555,36.6696],[-85.9491,36.6619],[-85.9502,36.651],[-85.9548,36.6501],[-85.9599,36.646],[-85.9736,36.6292],[-86,36.6305],[-86.207,36.6412],[-86.2077,36.6412],[-86.3401,36.65],[-86.4119,36.6516],[-86.4138,36.6611],[-86.4191,36.6764],[-86.4191,36.6787],[-86.4147,36.6933],[-86.4132,36.7137],[-86.4097,36.7477],[-86.4054,36.7763]]]},\"properties\":{\"name\":\"Allen\",\"state\":\"KY\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b463c","contributors":{"authors":[{"text":"Shaw, Eugene Wesley","contributorId":53867,"corporation":false,"usgs":true,"family":"Shaw","given":"Eugene","email":"","middleInitial":"Wesley","affiliations":[],"preferred":false,"id":215242,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mather, Kirtley F.","contributorId":32036,"corporation":false,"usgs":true,"family":"Mather","given":"Kirtley F.","affiliations":[],"preferred":false,"id":215241,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39444,"text":"pp108K - 1917 - The Helderberg limestone of central Pennsylvania","interactions":[],"lastModifiedDate":"2022-11-09T17:40:20.56823","indexId":"pp108K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1917","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"108","chapter":"K","title":"The Helderberg limestone of central Pennsylvania","docAbstract":"<p>This paper presents the results of a study made during 1913, 1914, and 1915, while the writer was a student at Johns Hopkins University. The formations discussed have been studies in Maryland, New Jersey, and New York, and described with more or less detail, but concerning their occurrence in the intervening area in Pennsylvania little exact information has been available. The conflict in opinion as to the proper position and correlation of the Keyser limestone and as to the interpretation of some of the standard New York sections has made further data very desirable, and the present paper is an attempt to meet a part of the deficiency.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp108K","usgsCitation":"Reeside, J.B., 1917, The Helderberg limestone of central Pennsylvania: U.S. Geological Survey Professional Paper 108, 43 p., https://doi.org/10.3133/pp108K.","productDescription":"43 p.","startPage":"185","endPage":"225","numberOfPages":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":120264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_108_k.jpg"},{"id":271229,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0108k/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.5630789887784,\n              40.9269920564185\n            ],\n            [\n              -77.07853929891903,\n              41.17577198684302\n            ],\n            [\n              -78.17956252137813,\n              40.6272152654912\n            ],\n            [\n              -78.6785281015939,\n              39.75149515933953\n            ],\n            [\n              -78.29914931333096,\n              39.75466547716687\n            ],\n            [\n              -77.99399680972797,\n              40.514450368441175\n            ],\n            [\n              -77.52389700687974,\n              40.53325771324711\n            ],\n            [\n              -77.57338119665323,\n              40.297786768837796\n            ],\n            [\n              -77.41255757988957,\n              40.508180080845165\n            ],\n            [\n              -76.5630789887784,\n              40.9269920564185\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c307","contributors":{"authors":[{"text":"Reeside, John B. Jr.","contributorId":98299,"corporation":false,"usgs":true,"family":"Reeside","given":"John","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":221463,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39486,"text":"pp98P - 1916 - Contributions to the geology and paleontology of San Juan County, New Mexico: 1. Stratigraphy of a part of the Chaco River valley","interactions":[{"subject":{"id":39486,"text":"pp98P - 1916 - Contributions to the geology and paleontology of San Juan County, New Mexico: 1. Stratigraphy of a part of the Chaco River valley","indexId":"pp98P","publicationYear":"1916","noYear":false,"chapter":"P","title":"Contributions to the geology and paleontology of San Juan County, New Mexico: 1. Stratigraphy of a part of the Chaco River valley"},"predicate":"IS_PART_OF","object":{"id":39465,"text":"pp98 - 1917 - Shorter contributions to general geology, 1916","indexId":"pp98","publicationYear":"1917","noYear":false,"title":"Shorter contributions to general geology, 1916"},"id":1}],"isPartOf":{"id":39465,"text":"pp98 - 1917 - Shorter contributions to general geology, 1916","indexId":"pp98","publicationYear":"1917","noYear":false,"title":"Shorter contributions to general geology, 1916"},"lastModifiedDate":"2024-01-09T21:04:49.284733","indexId":"pp98P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1916","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"98","chapter":"P","title":"Contributions to the geology and paleontology of San Juan County, New Mexico: 1. Stratigraphy of a part of the Chaco River valley","docAbstract":"<p>This preliminary paper is an attempt to set forth the principal features of the stratigraphy in a part of the San Juan Basin-to describe the succession of strata irrespective of possible correlations and thereby to establish a type section for the formations exposed and to bring out their relations to the strata immediately above and below. The paper presents only a part of the data collected by a field party of the United States Geological Survey in the season of 1915, in charge of the writer, and does not describe the economic resources of the area, such as coal, nor the general geologic problems.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp98P","usgsCitation":"Bauer, C., 1916, Contributions to the geology and paleontology of San Juan County, New Mexico: 1. Stratigraphy of a part of the Chaco River valley: U.S. Geological Survey Professional Paper 98, 19 p., https://doi.org/10.3133/pp98P.","productDescription":"19 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":271170,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0098p/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424236,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93338.htm","linkFileType":{"id":5,"text":"html"}},{"id":170053,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0098p/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"San Juan County","otherGeospatial":"Chaco River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.8522,\n              36.7611\n            ],\n            [\n              -108.6978,\n              36.7611\n            ],\n            [\n              -108.6978,\n              36.0903\n            ],\n            [\n              -107.8522,\n              36.0903\n            ],\n            [\n              -107.8522,\n              36.7611\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af0e4b07f02db691764","contributors":{"authors":[{"text":"Bauer, Clyde Max","contributorId":66525,"corporation":false,"usgs":true,"family":"Bauer","given":"Clyde Max","affiliations":[],"preferred":false,"id":221514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34168,"text":"b613 - 1916 - Guidebook of the western United States: Part C - The Santa Fe route, with a side trip to Grand Canyon of the Colorado","interactions":[],"lastModifiedDate":"2023-07-14T18:15:36.725642","indexId":"b613","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1916","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":"613","title":"Guidebook of the western United States: Part C - The Santa Fe route, with a side trip to Grand Canyon of the Colorado","docAbstract":"<p>The United States of America comprise an area so vast in extent and so diverse in natural features as well as in characters due to human agency that the American citizen who knows thoroughly his own country must have traveled widely and observed wisely. To 'know America first' is a patriotic obligation, but to meet this obligation the railroad traveler needs to have his eyes directed toward the more important or essential things within his field of vision and then to have much that he sees explained by what is unseen in the swift passage of the train. Indeed, many things that attract his attention are inexplicable except as the story of the past is available to enable him to interpret the present. Herein lie the value and the charm of history, whether human or geologic. </p><p>The present stimulus given to travel in the home country will encourage many thousands of Americans to study geography at first hand. To make this study most profitable the traveler needs a handbook that will answer the questions that come to his mind so readily along the way. Furthermore, the aim of such a guide should be to stimulate the eye in the selection of the essentials in the scene that so rapidly unfolds itself in the crossing of the continent. In recognition of the opportunity afforded in 1915 to render service of this kind to an unusually large number of American citizens, as well as to visitors from other countries, the United States Geological Survey has prepared a series of guidebooks covering four of the older railroad routes west of the Mississippi. </p><p>These books are educational in purpose, but the method adopted is to entertain the traveler by making more interesting what he sees from the car window. The plan of the series is to present authoritative information that may enable the reader to realize adequately the scenic and material resources of the region he is traversing, to comprehend correctly the basis of its development, and above all to appreciate keenly the real value of the country he looks out upon, not as so many square miles of territory represented on the map in a railroad folder by meaningless spaces, but rather as land - real estate, if you please - varying widely in present appearance because differing largely in its history and characterized by even greater variation in values because possessing diversified natural resources. One region may be such as to afford a livelihood for only a pastoral people; another may present opportunity for intensive agriculture; still another may contain hidden stores of mineral wealth that may attract large industrial development; and taken together these varied resources afford the promise of long-continued prosperity for this or that State. </p><p>Items of interest in civic development or references to significant epochs in the record of discovery and settlement may be interspersed with explanations of mountain and valley or statements of geologic history. In a broad way, the story of the West is a unit, and every chapter should be told in order to meet fully the needs of the tourist who aims to understand all that he sees. To such a traveler-reader this series of guidebooks is addressed. </p><p>To this interpretation of our own country the United States Geological Survey brings the accumulated data of decades of pioneering investigation, and the present contribution is only one type of return to the public which has supported this scientific work under the Federal Government. </p><p>In preparing the description of the country traversed by the Santa Fe Route the geographic and geologic information already published as well as unpublished material in the possession of the Geological Survey has been utilized, but to supplement this material Mr. Darton made a field examination of the entire route in 1914. Information has been furnished by Erasmus Haworth, J. E. Todd, and R. T. Hill, as well as by others whose writings are listed in the bibliography at the end of the text. Cooperation has been rendered by the United States Reclamation Service and by bureaus of the Department of Agriculture. Railroad officials and other citizens have also generously given their aid, and other members of the Survey have freely cooperated in the work.</p><p>For the purpose of furnishing the traveler with a graphic presentation of each part of his route, the accompanying maps, 25 sheets in all, have been prepared, with a degree of accuracy probably never bsfore attained in a guidebook, aiid their arrangement has been planned to meet the convenience of the reader. The special topographic surveys necessary to complete these maps of the route were made by W. O. Tufts. </p>","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/b613","usgsCitation":"Darton, N.H., 1916, Guidebook of the western United States: Part C - The Santa Fe route, with a side trip to Grand Canyon of the Colorado: U.S. Geological Survey Bulletin 613, iv, 194 p., https://doi.org/10.3133/b613.","productDescription":"iv, 194 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":164021,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0613/report-thumb.jpg"},{"id":92612,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0613/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":418959,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_114926.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.5,\n              39.25\n            ],\n            [\n              -119,\n              39.25\n            ],\n            [\n              -119,\n              33.5\n            ],\n            [\n              -94.5,\n              33.5\n            ],\n            [\n              -94.5,\n              39.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db6920e9","contributors":{"authors":[{"text":"Darton, Nelson Horatio","contributorId":78307,"corporation":false,"usgs":true,"family":"Darton","given":"Nelson","email":"","middleInitial":"Horatio","affiliations":[],"preferred":false,"id":212557,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34044,"text":"b616 - 1916 - The data of geochemistry (third edition)","interactions":[],"lastModifiedDate":"2012-02-02T00:09:31","indexId":"b616","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1916","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":"616","title":"The data of geochemistry (third edition)","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/b616","usgsCitation":"Clarke, F.W., 1916, The data of geochemistry (third edition): U.S. Geological Survey Bulletin 616, 821 p. ;24 cm., https://doi.org/10.3133/b616.","productDescription":"821 p. ;24 cm.","costCenters":[],"links":[{"id":92560,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0616/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0616/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668861","contributors":{"authors":[{"text":"Clarke, Frank Wigglesworth","contributorId":88798,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank","email":"","middleInitial":"Wigglesworth","affiliations":[],"preferred":false,"id":212364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1736,"text":"wsp400D - 1916 - Accuracy of stream-flow data","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp400D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1916","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":"400","chapter":"D","title":"Accuracy of stream-flow data","language":"ENGLISH","publisher":"G.P.O.,","doi":"10.3133/wsp400D","usgsCitation":"Grover, N.C., and Hoyt, J.C., 1916, Accuracy of stream-flow data: U.S. Geological Survey Water Supply Paper 400, p. 53-59 ;24 cm., https://doi.org/10.3133/wsp400D.","productDescription":"p. 53-59 ;24 cm.","costCenters":[],"links":[{"id":264373,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0400d/report.pdf","size":"895","linkFileType":{"id":1,"text":"pdf"}},{"id":264374,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0400d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2b70","contributors":{"authors":[{"text":"Grover, Nathan Clifford","contributorId":66660,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan","email":"","middleInitial":"Clifford","affiliations":[],"preferred":false,"id":144047,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoyt, John Clayton","contributorId":10399,"corporation":false,"usgs":true,"family":"Hoyt","given":"John","email":"","middleInitial":"Clayton","affiliations":[],"preferred":false,"id":144046,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2888,"text":"wsp338 - 1915 - Springs of California","interactions":[],"lastModifiedDate":"2019-03-11T13:22:28","indexId":"wsp338","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1915","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":"338","title":"Springs of California","docAbstract":"<p>In 1903 the United States Geological Survey began an investigation of the underground water of California, generally with financial cooperation on the part of the State. Since that year ten papers on the underground water of the State have been issued by the Survey, each representing an investigation that has been completed. The field work which is to serve as the basis for two additional papers has also been done and the reports are in preparation. Investigations have been begun in two other areas in the State and their results will eventually be assembled and published.</p><p>Since a period soon after the inception of the California work those responsible for its conduct have realized the desirability of a special study of the springs, particularly those which yield mineral waters and which are utilized to a greater or less extent by citizens of the State and by tourists as recreation and health resorts. It did not become practicable to begin this work until the summer of 1908, when Mr. G. A. Waring, who had assisted in some of the earlier California studies and had investigated for the Survey certain areas in southern Oregon and Washington, was assigned to the task of collecting and assembling the necessary data.</p><p>California, with an area of 158,000 square miles, is the second largest State in the Union. It exhibits wide geographic diversity, since it includes the lowest area in the United States Death Valley, 276 feet below sea level and the highest Mount Whitney, 14,501 feet above the sea; and accompanying this geographic diversity there is a corresponding range in scenic effects, climate, and vegetation. The records obtained at meteorological stations in the Salton Sink indicate a maximum temperature of 130° in the shade, the highest of record within the continental United States. It is probable that minimum temperatures on the higher peaks, like Mount Whitney and Mount Shasta, approach the minimum within our boundaries. Rainfall records in the most arid sections of the southern deserts of the State represent the extreme of aridity in the United States, with averages of less than 3 inches per annum and periods of 12 months or more with only traces of rain, whereas the precipitation&nbsp;in northwestern California is very heavy, an annual average of close to 100 inches being recorded at a few stations in Mendocino and Del Norte counties.</p><p>The immensity of the area of the State has made the collection of the field data required for the report a task of considerable magnitude, though its diversity has added greatly to the interest of the work. In the original plan it was estimated that two years of field studies would prove sufficient. Mr. Waring succeeded in visiting the more important localities during this period, although some of his examinations were, of necessity, rather cursory. In midsummer, 1910, after the completion of the field work and the assembling of the greater portion of his data in manuscript form he was called by the Government of Brazil to take charge of general water supply investigations in the northeastern arid portion of that South American republic. The task of reviewing, editing, and supplementing in some respects, the results of his studies was thus unavoidably left to others. This task was rendered light by the systematic form in which Mr. Waring's material was left.</p><p>It was a matter of regret to Mr. Waring, as it has been to those associated with him, that the financial limitations which controlled his work made it impracticable to procure the large number of new analyses which are particularly important in a paper of this type, in which waters of unusual chemical characteristics are discussed. Such analyses as are available have been assembled from all possible sources and combined with those which were prepared especially in connection with this investigation. The result, although it is in some respects unsatisfactory, furnishes a basis for a general view of the characteristics of the spring waters and serves to permit, their classification in a general way. Mr. Herman Stabler has reviewed the chemical data and rearranged and interpreted the available analyses.</p><p>It is hoped that the report, setting forth as it does the results of impartial observations upon one of the important present and more important prospective resources of the State, will prove of value to its citizens as well as to its visitors, and that the assembled material will not be without interest to physicians, chemists, geologists, and teachers who may have especial need for the information contained in the volume.</p>","language":"English","publisher":"Government Printing Office","doi":"10.3133/wsp338","usgsCitation":"Waring, G.A., 1915, Springs of California: U.S. Geological Survey Water Supply Paper 338, Report: 410 p.; 3 Plates: 20.66 x 24.79 inches or smaller, https://doi.org/10.3133/wsp338.","productDescription":"Report: 410 p.; 3 Plates: 20.66 x 24.79 inches or 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