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,{"id":1521,"text":"wsp351 - 1915 - Surface water supply of the United States, 1913, Part I, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp351","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":"351","title":"Surface water supply of the United States, 1913, Part I, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp351","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1915, Surface water supply of the United States, 1913, Part I, North Atlantic slope basins: U.S. Geological Survey Water Supply Paper 351, 189 p. :ill. ;23 cm., https://doi.org/10.3133/wsp351.","productDescription":"189 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0351/report-thumb.jpg"},{"id":26587,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0351/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e58","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527887,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33984,"text":"b591 - 1915 - Analyses of rocks and minerals from the laboratory of the United States Geological Survey, 1880 to 1914","interactions":[],"lastModifiedDate":"2017-05-23T12:17:34","indexId":"b591","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1915","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":"591","title":"Analyses of rocks and minerals from the laboratory of the United States Geological Survey, 1880 to 1914","docAbstract":"<p>The present Geological Survey of the United States was organized in 1879. In 1880, in connection with the Colorado work, a chemical laboratory was established at Denver in charge of W. F. Hillebrand, with whom were associated Antony Guyard and, later, L. G. Eakins. In 1882 W. H. Melville was placed in charge of a second laboratory at San Francisco, and in the autumn of 1883 the central laboratory was started in Washington, with myself as chief chemist. In November, 1885, Dr. Hillebrand was transferred to Washington; early in 1888 he was followed by Mr. Eakins, and the Denver laboratory was discontinued. In the spring of 1890 Dr. Melville also was transferred to Washington, and since then the geochemical work of the Survey has been concentrated at headquarters. The special laboratories of the water-resources and technologic branches of the Survey are not included in this statement and their work is not represented in this bulletin.</p><p>Up to January 1, 1914, nearly 8,000 analyses have been made in the laboratory at Washington of rocks, minerals, ores, waters, sediments, coals, metals, and other substances with which geology has to do. Some-hundreds of analyses were also made in the laboratories at Denver and San Francisco. A fair amount of research work upon mineralogical and analytical problems has also been done. In *all of this work the following chemists have been employed: E. T. Allen, R. K. Bailey, Charles Catlett, T. M. Chatard, F. W. Clarke, L. G. Eakins, J. G. Fairchild, F. A. Gooch, Antony Guyard, W. B. Hicks, W. F. Hillebrand, W. F. Hunt, W. H. Melville, H. C. McNeil, Chase Palmer, R. B. Riggs, W. T. Schaller, E. A. Schneider, George Steiger, H. N. Stokes, E. C. Sullivan, William Valentine, R. C. Wells, W. C. Wheeler, and J. E. Whitfield. At present, January 1, 1914, eight of these chemists are employed in the Survey. Other officers of the Survey have been occupied more or less with chemical questions, but the men named in this list were connected directly with the laboratory. Some work for the chemical division has also been done by chemists not regularly on the rolls of the Survey, but their analyses,&nbsp;with the exception of a single group to be noted later, do not fall within the scope of this paper.</p><p><br data-mce-bogus=\"1\"></p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b591","usgsCitation":"Clarke, F.W., 1915, Analyses of rocks and minerals from the laboratory of the United States Geological Survey, 1880 to 1914: U.S. Geological Survey Bulletin 591, 376 p., https://doi.org/10.3133/b591.","productDescription":"376 p.","costCenters":[],"links":[{"id":164147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/591/report-thumb.jpg"},{"id":341575,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/591/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680edf","contributors":{"authors":[{"text":"Clarke, Frank Wigglesworth","contributorId":88798,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank","email":"","middleInitial":"Wigglesworth","affiliations":[],"preferred":false,"id":212280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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G.","contributorId":38547,"corporation":false,"usgs":true,"family":"Hoyt","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":149750,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryan, H.J.","contributorId":21945,"corporation":false,"usgs":true,"family":"Ryan","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":149749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":45195,"text":"b581B - 1915 - Oil and gas in the western part of the Olympic Peninsula, Washington","interactions":[{"subject":{"id":45195,"text":"b581B - 1915 - Oil and gas in the western part of the Olympic Peninsula, Washington","indexId":"b581B","publicationYear":"1915","noYear":false,"chapter":"B","title":"Oil and gas in the western part of the Olympic Peninsula, Washington"},"predicate":"IS_PART_OF","object":{"id":33944,"text":"b581 - 1915 - Contributions to economic geology (short papers and preliminary reports), 1913: Part II - mineral fuels","indexId":"b581","publicationYear":"1915","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1913: Part II - mineral fuels"},"id":1}],"isPartOf":{"id":33944,"text":"b581 - 1915 - Contributions to economic geology (short papers and preliminary reports), 1913: Part II - mineral fuels","indexId":"b581","publicationYear":"1915","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1913: Part II - mineral fuels"},"lastModifiedDate":"2025-03-25T17:19:19.212","indexId":"b581B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1915","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":"581","chapter":"B","title":"Oil and gas in the western part of the Olympic Peninsula, Washington","docAbstract":"High-grade paraffin oil is reported to have been discovered in the western part of the Olympic Peninsula, Wash., as early as 1881. Since then attempts to obtain oil or gas in commercial quantities by drilling have been made from time to time in different localities in this region, but without success. Within the past few years interest has been aroused in oil seeps near the mouth of Hoh River and in gas vents in other parts of the field to such an extent that many persons have been attracted to this country to search for oil and gas. As a result of this interest and on account of the fact that efforts had been made to lease tracts of land for this purpose in the Queniult Indian Reservation, an examination of this region was made by the United States Geological Survey at the request of the Office of Indian Affairs. The results of the investigation, which are enumerated below and which are discussed in detail throughout this report, suggest that certain parts of the field are worthy of careful consideration by oil operators. The following summary includes the most important facts regarding the area examined:\r\n\r\nHigh-grade paraffin oil issues from two seeps near the mouth of Hoh River, and at other localities oil-saturated sandy clay ('smell mud' of the Indians) is exposed. Natural gas containing about 95 per cent methane escapes from a conical mound just north of the mouth of Queniult River and also from an inverted cone-shaped water-filled depression on Hoh River a short distance west of Spruce post office. Other minor gas vents are also known in this field and are described in detail in this report. Three wells - one in the reservation about 1 mile north and slightly west from Taholah, another near the mouth of Hoh River, and the third about 1 mile south of Forks - are being drilled for oil and gas. So far as drilling has progressed none of these wells have encountered oil in paying quantities, but all of them have struck small amounts of gas. A study of the structure and stratigraphy in addition to the examination of oil seeps and gas vents reveals the fact that several anticlines, which may serve as reservoirs for oil and gas, exist in the area examined and that they have apparently a close relationship to the oil seeps and occurrences of 'smell mud'.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1913: Part II - mineral fuels (Bulletin 581)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b581B","usgsCitation":"Lupton, C., 1915, Oil and gas in the western part of the Olympic Peninsula, Washington: U.S. Geological Survey Bulletin 581, 59 p., https://doi.org/10.3133/b581B.","productDescription":"59 p.","startPage":"23","endPage":"81","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":134768,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0581b/report-thumb.jpg"},{"id":113915,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0581b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401948,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20133.htm"}],"country":"United States","state":"Washington","otherGeospatial":"Olympic Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.727783203125,\n              47.204642388766935\n            ],\n            [\n              -123.629150390625,\n              47.204642388766935\n            ],\n            [\n              -123.629150390625,\n              47.96785877999251\n            ],\n            [\n              -124.727783203125,\n              47.96785877999251\n            ],\n            [\n              -124.727783203125,\n              47.204642388766935\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af1e4b07f02db6917bc","contributors":{"authors":[{"text":"Lupton, Charles T.","contributorId":67853,"corporation":false,"usgs":true,"family":"Lupton","given":"Charles T.","affiliations":[],"preferred":false,"id":231246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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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,{"id":70011066,"text":"70011066 - 1915 - Solubility of magnesium carbonate in natural waters","interactions":[],"lastModifiedDate":"2020-11-23T17:22:56.910778","indexId":"70011066","displayToPublicDate":"1915-01-01T00:00:00","publicationYear":"1915","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2519,"text":"Journal of the American Chemical Society","active":true,"publicationSubtype":{"id":10}},"title":"Solubility of magnesium carbonate in natural waters","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ja02172a007","usgsCitation":"Wells, R.C., 1915, Solubility of magnesium carbonate in natural waters: Journal of the American Chemical Society, v. 37, p. 1704-1707, https://doi.org/10.1021/ja02172a007.","productDescription":"4 p.","startPage":"1704","endPage":"1707","costCenters":[],"links":[{"id":480473,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://zenodo.org/record/1566852","text":"External Repository"},{"id":221021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505b9245e4b08c986b319dd9","contributors":{"authors":[{"text":"Wells, R. C.","contributorId":101300,"corporation":false,"usgs":true,"family":"Wells","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":360200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179606,"text":"70179606 - 1914 - Progress report on stream measurement work carried on in cooperation with the United States Geological Survey: Section in <i>Ninth biennial report of the State Engineer to the governor of Utah: 1913-1914</i>","interactions":[],"lastModifiedDate":"2017-01-24T11:07:45","indexId":"70179606","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Progress report on stream measurement work carried on in cooperation with the United States Geological Survey: Section in <i>Ninth biennial report of the State Engineer to the governor of Utah: 1913-1914</i>","docAbstract":"<p>Utah, like other states in the arid region of the United States, points with just pride to her present and future agricultural developments. She proudly boasts, and no doubt justly too, that her fields of green vegetation are inexhaustible and always expanding, and with due vigilance and care on the part of her land holders these fields will bring forth the proper supplies for man for an indefinite period. But, like her neighboring sister states on the east, west, north, and south, she realizes that the precipitation over her lands, as a general rule, is insufficient for the growing and maturing of crops. As a result, her principal lands can only be made to bear crops through the assistance of irrigation. In all irrigation, next to the land itself, the most important factor to be considered is the water supply.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Ninth biennial report of the State Engineer to the governor of Utah: 1913-1914","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"The Arrow Press, Tribune-Reporter Printing Co","publisherLocation":"Salt Lake City UT","usgsCitation":"Porter, E., 1914, Progress report on stream measurement work carried on in cooperation with the United States Geological Survey: Section in <i>Ninth biennial report of the State Engineer to the governor of Utah: 1913-1914</i>: Utah State Engineer Biennial Report 9, 15 p.","productDescription":"15 p.","startPage":"66","endPage":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333768,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-354","text":"Full Text of Biennial Report"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"586f69c3e4b01a71ba0bc925","contributors":{"authors":[{"text":"Porter, E.A.","contributorId":69529,"corporation":false,"usgs":true,"family":"Porter","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":657846,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2211,"text":"wsp350 - 1914 - Profile surveys in Bear River basin, Idaho","interactions":[],"lastModifiedDate":"2016-12-27T13:42:14","indexId":"wsp350","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1914","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":"350","title":"Profile surveys in Bear River basin, Idaho","docAbstract":"Bear River rises on the northern slope of the Uinta Mountains, in\nthe northeastern part of Utah, and after a circuitous course in\nwhich it leaves Utah and enters Wyoming, Utah, and Wyoming in\nturn and makes a long detour in Idaho it returns to Utah and finally\ndischarges its waters into Great Salt Lake. The maximum elevation\nof the upper rim of the basin is 13,000 feet above sea level.\nThe upper part of the basin comprises a rough, broken country,\nwell drained by numerous short streams, most of which are confined\nto steep, narrow canyons. The streams are fed by many small springs\nand by the melting of the snow which forms the greater part of the\nprecipitation. The rocks of the extreme headwater region are chiefly\nsandstones and quartzites and are covered with a thin layer of soil\nthat supports scattered groves of fir and aspen. A few small lakes\nlie near the head of the river.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp350","collaboration":"Prepared under the direction of R. B. Marshall, Chief Geographer","usgsCitation":"Marshall, R.B., 1914, Profile surveys in Bear River basin, Idaho: U.S. Geological Survey Water Supply Paper 350, Report: 7 p.; Plate 1: 19.50 inches x 18.09 inches; Plate 2: 19.50 inches x 18.14 inches; Plate 3: 19.50 inches x 18.15 inches; Plate 4: 19.50 inches x 18.13 inches; Plate 5: 19.50 inches x 18.15 inches; Plate 6: 19.50 inches x 17.99 inches, https://doi.org/10.3133/wsp350.","productDescription":"Report: 7 p.; Plate 1: 19.50 inches x 18.09 inches; Plate 2: 19.50 inches x 18.14 inches; Plate 3: 19.50 inches x 18.15 inches; Plate 4: 19.50 inches x 18.13 inches; Plate 5: 19.50 inches x 18.15 inches; Plate 6: 19.50 inches x 17.99 inches","costCenters":[],"links":[{"id":279589,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/publication/wsp350"},{"id":137826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0350/report-thumb.jpg"},{"id":27905,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0350/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247142,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0350/plate-1_a.pdf","size":"1582","linkFileType":{"id":1,"text":"pdf"}},{"id":247143,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0350/plate-1_b.pdf","size":"1420","linkFileType":{"id":1,"text":"pdf"}},{"id":247144,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0350/plate-1_c.pdf","size":"1741","linkFileType":{"id":1,"text":"pdf"}},{"id":247145,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0350/plate-1_d.pdf","size":"1126","linkFileType":{"id":1,"text":"pdf"}},{"id":247146,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0350/plate-1_e.pdf","size":"1269","linkFileType":{"id":1,"text":"pdf"}},{"id":247147,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0350/plate-1_f.pdf","size":"1069","linkFileType":{"id":1,"text":"pdf"}}],"state":"Idaho","otherGeospatial":"Bear River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.95,41.79 ], [ -111.95,42.27 ], [ -111.75,42.27 ], [ -111.75,41.79 ], [ -111.95,41.79 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a62c","contributors":{"authors":[{"text":"Marshall, Robert Bradford","contributorId":106469,"corporation":false,"usgs":true,"family":"Marshall","given":"Robert","email":"","middleInitial":"Bradford","affiliations":[],"preferred":false,"id":144830,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2214,"text":"wsp347 - 1914 - Profile surveys in Snake River basin, Idaho","interactions":[],"lastModifiedDate":"2013-11-22T12:01:08","indexId":"wsp347","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1914","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":"347","title":"Profile surveys in Snake River basin, Idaho","docAbstract":"Snake River, the largest tributary of the Columbia, rises among\nthe high peaks of the Rocky Mountains in Yellowstone National\nPark, heading in the divide from which streams flow northward and\neastward into the Missouri, southward to the Colorado and the lakes\nof the Great Basin, and westward to the Columbia. From the headwater\nregion, including Shoshone, Lewis, and Heart lakes, in Yellowstone\nNational Park, the river flows southward, broadening into\nJackson Lake (4 miles wide and 18 miles long) and passing through\nJackson Valley (8 miles wide and 40 miles long), beyond which, near\nthe Idaho-Wyoming line, it enters a long canyon. At the south\nedge of Madison County, Idaho, it receives Henrys Fork, below which\nthe Snake flows southward and westward across Idaho to a point\nnear Homedale, near the Oregon-Idaho line, where it turns abruptly\nnorthward and beyond which it forms for about 170 miles the boundary\nbetween Idaho and Oregon and for 30 miles more that between\nIdaho and Washington. It enters Washington at Lewiston, flows\nnorthwest, west, and southwest, and joins the Columbia near Pasco.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp347","collaboration":"Prepared under the direction of R. B. 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