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Large parts of four of these sheets cover the waters of the Bay of San Francisco or of the adjacent Pacific Ocean. (See fig. 1.) Within the area mapped are the cities of San Francisco, Oakland, Berkeley, Alameda, Ban Rafael, and San Mateo, and many smaller towns and villages. These cities, which have a population aggregating about 750,000, together form the largest and most important center of commercial and industrial activity on the west coast of the United States. The natural advantages afforded by a great harbor, where the railways from the east meet the ships from all ports of the world, have determined the site of a flourishing cosmopolitan, commercial city on the shores of San Francisco Bay. The bay is encircled by hilly and mountainous country diversified by fertile valley lands and divides the territory mapped into two rather contrasted parts, the western part being again divided by the Golden Gate. It will therefore be convenient to sketch the geographic features under four headings (1) the area east of San Francisco Bay; (2) the San Francisco Peninsula; (3) the Marin Peninsula; (4) San Francisco Bay. (See fig. 2.)
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Geology","linkFileType":{"id":1,"text":"pdf"}},{"id":24075,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gf/193/quad-1_topography.pdf","text":"Tamalpais Quadrangle Topography","linkFileType":{"id":1,"text":"pdf"}},{"id":24074,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gf/193/quad-1_structure.pdf","text":"Tamalpais Quadrangle Structure Sections","linkFileType":{"id":1,"text":"pdf"}},{"id":24072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gf/193/text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":265105,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gf/193/cover-thumb.jpg"}],"scale":"62500","country":"United States","state":"California","city":"San Francisco","otherGeospatial":"Tamalpais, San Francisco, Concord, San Mateo, and Haywards quadrangles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.75,37.5 ], [ -122.75,38 ], [ -122,38 ], [ -122,37.5 ], [ -122.75,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdd83","contributors":{"authors":[{"text":"Lawson, Andrew Cowper","contributorId":101751,"corporation":false,"usgs":true,"family":"Lawson","given":"Andrew","email":"","middleInitial":"Cowper","affiliations":[],"preferred":false,"id":277161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":33918,"text":"b600 - 1914 - The Glacier National Park: A popular guide to its geology and scenery","interactions":[],"lastModifiedDate":"2017-07-06T10:18:54","indexId":"b600","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","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":"600","title":"The Glacier National Park: A popular guide to its geology and scenery","docAbstract":"The Glacier National Park includes that part of the Front Range of the Rocky Mountains lying just south of the Canadian line, in Teton and Flathead counties, Mont. It is bounded on the west by Flathead River (locally called North Fork), on the south by the Middle Fork of Flathead River and the Great Northern Railway, and on the east by the Blackfeet Indian Reservation.
Although this part of the Rocky Mountains has been known since Lewis and Clark crossed the continent in 1805-6, the region later made a park appears not to have been visited by white men until 1853, when Cut Bank Pass was crossed by A. W. Tinkham, one of the Government engineers engaged in exploring a route for the Pacific railroad. Tinkham, who was encamped in the Bitterroot Valley, was ordered to examine Marias Pass, but in traversing Middle Fork of Flathead River along the line of the present railroad he was evidently misled by the large size of the valley of Nyack Creek and ascended that instead of keeping to the right up the main stream. He reported the pass impracticable for railroad construction, and so this region dropped out of public attention for a long time.
The next explorers to enter the region were a group of surveyors who, under the direction of American and British commissioners, established the international boundary line along the forty-ninth parallel from the Pacific coast to the main summit of the Rocky Mountains. This party reached the area now included in the park in the summer of 1861, and the stone monument shown in Plate I, B, which they erected on the Continental Divide west of Waterton Lake, still marks a point on the boundary between the United States and Canada.
The land on the west side of the range formed a part of the public domain which, until the erection of the park, was open to settlement, but the land on the east originally belonged to the Blackfeet Indians and the white men had no rights upon it. About 1890 copper ore was found near the heads of Quartz and Mineral creeks, and a great boom for this region followed. Many prospectors drifted in, expecting to reap rich rewards from the discovery of mineral deposits and the general development of the region. Several of the main trails were built about this time, and considerable money was spent in prospecting, in opening mines, and in providing machinery to handle the large output of copper ore that was expected.
The copper-bearing veins were found to extend through the range to the east side, but prospecting in that part of the mountains was not possible, for the land was included in the Indian reservation. This situation produced a growing discontent among the prospectors, who began to have a strong feeling that the Government should come to their relief by acquiring the coveted land and placing it at their disposal. The urgent demand of the prospectors and promoters was felt in Congress, and a bill was passed providing for the purchase from the Indians of this supposed mineral land for $1,500,000. In accordance with this act, a treaty with the Blackfeet Indians was signed at Browning, Mont., September 26, 1895, and approved by the Senate on June 10, 1896, by which the west line of the reservation was removed from the Continental Divide and was fixed along the eastern points of the spurs of the mountain range, as shown on the accompanying map, and the land so acquired was thrown open to mineral entry only.
Under the stimulus of the new territory acquired, active prospecting was carried on for a time, but copper ore was found only in small quantities, and gradually the prospectors and miners drifted away to newer or more promising fields, and the region reverted to its original condition. For a long time it was visited only by hunters in search of big game and by summer visitors who, in order to escape the heat of the plains, were willing to undergo the privations and discomforts of the rude hotels then to be found in the region.
Although these mountains had ceased to interest prospectors in search of mineral wealth, they still possessed a fascination for the lovers of natural scenery and almost everyone who visited the region was impressed with its alpine beauty. Again it was brought to the attention of Congress, which was urged to secure it for the use of the people by setting it aside as a national park. On May 11, 1910, President Taft signed the bill creating the Glacier National Park, and this most interesting and beautiful region thus became a permanent playground for the American people.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b600","usgsCitation":"Campbell, M., 1914, The Glacier National Park: A popular guide to its geology and scenery: U.S. Geological Survey Bulletin 600, 54 p., https://doi.org/10.3133/b600.","productDescription":"54 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":163348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0600/report-thumb.jpg"},{"id":92485,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0600/report.pdf","text":"Report","size":"9.63 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4ec","contributors":{"authors":[{"text":"Campbell, Marius R.","contributorId":103337,"corporation":false,"usgs":true,"family":"Campbell","given":"Marius R.","affiliations":[],"preferred":false,"id":212169,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":343,"text":"wsp302 - 1913 - Surface water supply of the United States, 1911 : Part 2, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"wsp302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1913","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":"302","title":"Surface water supply of the United States, 1911 : Part 2, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp302","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1913, Surface water supply of the United States, 1911 : Part 2, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 302, 90 p. ;23 cm., https://doi.org/10.3133/wsp302.","productDescription":"90 p. ;23 cm.","costCenters":[],"links":[{"id":136587,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0302/report-thumb.jpg"},{"id":24906,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0302/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697eec","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":527324,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39480,"text":"pp76 - 1913 - The San Franciscan volcanic field, Arizona","interactions":[],"lastModifiedDate":"2017-07-13T08:54:41","indexId":"pp76","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1913","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":"76","title":"The San Franciscan volcanic field, Arizona","docAbstract":"LOCATION OF AREA
The San Franciscan volcanic field, which takes its name from San Francisco Mountain, the largest volcano of the group, covers about 3,000 square miles in the north-central part of Arizona, as shown by the shaded space on the index map forming figure 1. The center of the field lies about 50 miles south of the Grand Canyon of the Colorado and the southern boundary is in part coterminous with that of the San Francisco Plateau, which forms the southwestern division of the great Colorado Plateau.
The region is easily reached, for the main line of the Atchison, Topeka, & Santa Fe Railway traverses it from east to west for more than 60 miles. Flagstaff, a town of 1,500 inhabitants 10 miles south of the summit of San Francisco Mountain, is on the railroad, amid a branch line runs from Williams, 34 miles farther west, to the Grand Canyon. All the more important points of interest in the field may be reached without difficulty by wagon, and outfits may be obtained at Flagstaff.
OUTLINE OF THE REPORT
This report deals primarily with the volcanic phenomena of the region as determined in the field and laboratory. Chapter I contains a brief description of the geography of the field and Chapter II is devoted largely to the sedimentary formations and structure. The rest of the report Chapters III to VI—treats entirely of the various features of the volcanoes and igneous rocks, both individually and collectively. Detailed descriptions of the volcanoes and lava fields are given in Chapter III; the volcanic history of the region and its correlation with the general history of the surrounding country are presented in Chapter IV. These two chapters will presumably suffice for the general reader who may desire to become acquainted with the broader volcanic features of the region. Chapter V (Petrography) is devoted entirely to the detailed description of the individual igneous rocks of the region, as represented by a selected set of type specimens. In Chapter VI (Petrology) is presented a discussion of the igneous rocks considered collectively—that is, as a series of genetically related members. These last two chapters will be more especially interesting to petrologists, although there is considerable matter in the last chapter which may also be of interest to the general reader.
EXTENT OF FIELD WORK
The field work on which the report is based was carried on during the summers of 1901 to 1903, a portion of the time, however, being occupied by side trips to the Grand Canyon of the Colorado, the Verde Valley, and the Moqui Buttes. It was the original intention to study only San Francisco Mountain, but scattered observations made during the first summer at other localities, especially at Elden Mountain and Kendrick Peak, seemed to indicate that the region would repay wider study. The work was accordingly extended so as to embrace all the large cones that lie in the vicinity of San Francisco Mountain and some 2,000 square miles of the surrounding plateau country. The more detailed work was confined to the large cones and the laccoliths, as they presented the greatest variety of phenomena within the smallest space. Reconnaissance work was carried on in the surrounding country more especially for the purpose of determining the limits of the widespread basalt flows, their relation to the underlying sedimentary formations, and the character of those formations.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp76","usgsCitation":"Robinson, H.H., 1913, The San Franciscan volcanic field, Arizona: U.S. Geological Survey Professional Paper 76, 213 p., https://doi.org/10.3133/pp76.","productDescription":"213 p.","costCenters":[],"links":[{"id":343695,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0076/report-thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111,\n 35.9\n ],\n [\n -112.5,\n 35.9\n ],\n [\n -112.5,\n 34.9\n ],\n [\n -111,\n 34.9\n ],\n [\n -111,\n 35.9\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67abbf","contributors":{"authors":[{"text":"Robinson, Henry Hollister","contributorId":193597,"corporation":false,"usgs":true,"family":"Robinson","given":"Henry","email":"","middleInitial":"Hollister","affiliations":[],"preferred":false,"id":221506,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1113,"text":"wsp333 - 1913 - Ground water in Boxelder and Tooele Counties, Utah","interactions":[],"lastModifiedDate":"2022-01-06T21:29:56.152375","indexId":"wsp333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1913","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":"333","title":"Ground water in Boxelder and Tooele Counties, Utah","docAbstract":"The area covered by this report includes Boxelder County, Utah, the eastern part of Tooele County, Utah, and some small tracts in southern Idaho. It comprises about 9,500 square miles, or more than the combined area of Massachusetts and Rhode Island. It lies between 40° and 42° north latitude and 112° and 114° west longitude. (See fig. 1.)
Insufficient rainfall and the rapid settling of the country have created a demand for an investigation to determine the feasibility of irrigating by the use of underground water. In response to this demand and in order to classify the land under the enlarged homestead act, the writer made an investigation covering a period of four months during the summer and fall of 1911. The greater part of this time was spent in Boxelder County, but two weeks at the close of the season were devoted to a reconnaissance in Tooele, Rush, and Skull valleys, in Tooele County. W. B. Heroy, of the United States Geological Survey, collected most of the data presented for southern Idaho.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp333","usgsCitation":"Carpenter, E., 1913, Ground water in Boxelder and Tooele Counties, Utah: U.S. Geological Survey Water Supply Paper 333, Report: 90 p.; 1 Plate: 20.00 x 17.13 inches, https://doi.org/10.3133/wsp333.","productDescription":"Report: 90 p.; 1 Plate: 20.00 x 17.13 inches","numberOfPages":"92","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":393986,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24510.htm"},{"id":138096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0333/report-thumb.jpg"},{"id":25874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0333/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25873,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0333/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Utah","county":"Box Elder County, Tooele County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113,\n 40.767\n ],\n [\n -112,\n 40.767\n ],\n [\n -112,\n 39.917\n ],\n [\n -113,\n 39.917\n ],\n [\n -113,\n 40.767\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db5b","contributors":{"authors":[{"text":"Carpenter, Everett","contributorId":103656,"corporation":false,"usgs":true,"family":"Carpenter","given":"Everett","email":"","affiliations":[],"preferred":false,"id":143199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39482,"text":"pp78 - 1913 - Geology and ore deposits of the Philipsburg quadrangle, Montana","interactions":[],"lastModifiedDate":"2022-03-31T21:11:07.761147","indexId":"pp78","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1913","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":"78","title":"Geology and ore deposits of the Philipsburg quadrangle, Montana","docAbstract":"The Philipsburg quadrangle is bounded by parallels 46° and 46° 30' and meridians 113° and 113° 30'. Its length from north to south is 34.5 miles, its average width east and west 23.8 miles, and its area 827.42 square miles. As shown on the index map (fig. 1), it is not far
from the western border of Montana and nearly midway between the northern and southern boundaries of the State. The nearest large town is Anaconda, the site of the great smelter of the Amalgamated Copper Co., which is on Warm Spring Creek, a mile or two beyond the eastern
boundary of the quadrangle.
Philipsburg lies about midway between the eastern and western limits of the Rocky Mountain system, if the term be used in the broad sense prevailing in the United States. In the general latitude of Montana the system as defined by American usage is bounded on the west by the Columbia River basalt plain and on the east by the Great Plains. The western limit is fairly definite, but on the east there is no very definite line between the plains and mountains; the mountains are fairly continuous west and north of the Philipsburg quadrangle, but to the east and southeast mountains alternate with broad stretches of semiarid lowland. The quadrangle therefore overlaps the line between two physiographic provinces, one characterized by isolated mountain groups, of which the Flint Creek Range is the most westerly, and the other by more continuous elevations, of which the Sapphire Mountains are an example.
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The Glenrock coal field, Wyoming. Coal fields of the northeast side of the Bighorn Basin, Wyoming, and of Bridger, Montana. Coal fields of the southwest side of the Bighorn Basin, Wyoming. The eastern part of the Great Divide Basin coal field, Wyoming. The western part of the Little Snake River coal field, Wyoming. The northern part of the Rock Springs coal field, Sweetwater County, Wyoming","docAbstract":"No abstract available.
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The northern part of the Rock Springs coal field, Sweetwater County, Wyoming: U.S. Geological Survey Bulletin 341, 160 p., https://doi.org/10.3133/b341B.","productDescription":"160 p.","startPage":"123","endPage":"282","costCenters":[],"links":[{"id":483591,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19872.htm","text":"The northern part of the Rock Springs coal field, Sweetwater County, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":483590,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19873.htm","text":"The western part of the Little Snake River coal field, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":483589,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19871.htm","text":"The eastern part of the Great Divide Basin coal field, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":483588,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19858.htm","text":"Coal fields of the southwest side of the Bighorn Basin, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":483587,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19857.htm","text":"Coal fields of the northeast side of the Bighorn Basin, Wyoming, and of Bridger, Montana","linkFileType":{"id":5,"text":"html"}},{"id":483586,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19867.htm","text":"The Sheridan coal field, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":175950,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0341b/report-thumb.jpg"},{"id":114443,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0341b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.08483207959064,\n 45.01372012254623\n ],\n [\n -111.08483207959064,\n 40.96025529580231\n ],\n [\n -104.16562968690882,\n 40.96025529580231\n ],\n [\n -104.16562968690882,\n 45.01372012254623\n ],\n [\n -111.08483207959064,\n 45.01372012254623\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af2e4b07f02db6918bf","contributors":{"authors":[{"text":"Taff, J. A.","contributorId":81467,"corporation":false,"usgs":true,"family":"Taff","given":"J.","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":239422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, E.W.","contributorId":50947,"corporation":false,"usgs":true,"family":"Shaw","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":931446,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Washburne, Chester Wesley","contributorId":16479,"corporation":false,"usgs":true,"family":"Washburne","given":"Chester","email":"","middleInitial":"Wesley","affiliations":[],"preferred":false,"id":931447,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Woodruff, E. G.","contributorId":10770,"corporation":false,"usgs":true,"family":"Woodruff","given":"E.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":931448,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, Edward Eggleston","contributorId":81161,"corporation":false,"usgs":true,"family":"Smith","given":"Edward","email":"","middleInitial":"Eggleston","affiliations":[],"preferred":false,"id":931449,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ball, Max Waite","contributorId":61870,"corporation":false,"usgs":true,"family":"Ball","given":"Max","email":"","middleInitial":"Waite","affiliations":[],"preferred":false,"id":931450,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schultz, A.R.","contributorId":94278,"corporation":false,"usgs":true,"family":"Schultz","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":931451,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":333,"text":"wsp242 - 1909 - Surface water supply of the United States, 1907-8, Part II. South Atlantic Coast and eastern Gulf of Mexico","interactions":[],"lastModifiedDate":"2017-10-02T09:27:37","indexId":"wsp242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1909","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":"242","title":"Surface water supply of the United States, 1907-8, Part II. South Atlantic Coast and eastern Gulf of Mexico","docAbstract":"This volume contains results of flow measurements made on certain streams in the United States. The work was performed by the water-resources branch of the United States Geological Survey, either independently or in cooperation with organizations mentioned herein. These investigations are authorized by the organic law of the Geological Survey (Stat. L., vol. 20, p. 394)...
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp242","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1909, Surface water supply of the United States, 1907-8, Part II. South Atlantic Coast and eastern Gulf of Mexico: U.S. Geological Survey Water Supply Paper 242, 226 p., https://doi.org/10.3133/wsp242.","productDescription":"226 p.","costCenters":[],"links":[{"id":24896,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0242/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0242/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b153b","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":527315,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1280,"text":"wsp236 - 1909 - The quality of surface waters in the United States, Part I, Analyses of waters east of the one hundredth meridian","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp236","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1909","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":"236","title":"The quality of surface waters in the United States, Part I, Analyses of waters east of the one hundredth meridian","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp236","usgsCitation":"Dole, R., 1909, The quality of surface waters in the United States, Part I, Analyses of waters east of the one hundredth meridian: U.S. Geological Survey Water Supply Paper 236, 123 p., https://doi.org/10.3133/wsp236.","productDescription":"123 p.","costCenters":[],"links":[{"id":137545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0236/report-thumb.jpg"},{"id":26243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0236/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641964","contributors":{"authors":[{"text":"Dole, Richard B.","contributorId":21932,"corporation":false,"usgs":true,"family":"Dole","given":"Richard B.","affiliations":[],"preferred":false,"id":143492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2098,"text":"wsp217 - 1908 - Water resources of Beaver Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-12T07:54:00","indexId":"wsp217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1908","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":"217","title":"Water resources of Beaver Valley, Utah","docAbstract":"Location and extent of area examined. Beaver Valley is located in Beaver County, in southwestern Utah, about 175 miles south of Salt Lake. It lies between the Tushar Mountains on the east and the Beaver Mountains on the west. The principal town of the valley is Beaver, which is most conveniently reached from Milford, a station on the San Pedro, Los Angeles and Salt Lake Railroad. The valley, together with its neighboring highlands, occupies the eastern third of Beaver County, an area of about 1,200 square miles. A large part of this area, however, is rocky upland and unproductive desert, the tillable land comprising a comparatively small area in the immediate vicinity of the streams.
Purpose and scope of work. The purpose of this paper is to present information concerning the waters of Beaver Valley and to point out ways and means of increasing their usefulness. The presence of a large amount of water in Beaver Valley results from local topograhic conditions, the water being supplied by precipitation in the highland to the east. Its conservation and distribution result from geologic conditions, the water being held in loose gravel and sand, which are more or less confined between ridges of consolidated rocks. The rock basins were formed partly by erosion and partly by faulting and surface deformation. In order to accomplish the purpose in view it is therefore necessary to describe the geographic and geologic conditions in Beaver Valley and neighboring regions.
The investigation included the determination of the flow of streams and springs, of the manner of occurrence and quantity of the underground waters as shown by the geologic and geographic conditions of the region and by the distribution of springs and wells, and of the chemical character of the waters with reference to their adaptability to domestic use and to irrigation. The chemical data were obtained (a) by field assays, which are approximately correct and probably of sufficient accuracy to be of value in comparing the various waters; (b) by more exact analyses, some of which were made in the laboratory of the United States Geological Survey by W. M. Barr, and others by Herman Harms, State chemist of Utah, for the San Pedro, Los Angeles and Salt Lake Railroad; and (c) by sanitary analyses, made also by Herman Harms.
Cooperation. The work was done during the summer of 1906, the United States Geological Survey cooperating with the State of Utah through Caleb Tanner, State engineer, and with the county of Beaver through the supervisors of the county. In collecting the information the writer was assisted by J. F. Hoyt, of Nephi, Utah.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp217","usgsCitation":"Lee, W.T., 1908, Water resources of Beaver Valley, Utah: U.S. Geological Survey Water Supply Paper 217, 57 p., https://doi.org/10.3133/wsp217.","productDescription":"57 p.","numberOfPages":"60","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":27664,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0217/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0217/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Beaver Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.13034057617188,\n 38.06539235133249\n ],\n [\n -113.13034057617188,\n 38.68014968334624\n ],\n [\n -112.39837646484375,\n 38.68014968334624\n ],\n [\n -112.39837646484375,\n 38.06539235133249\n ],\n [\n -113.13034057617188,\n 38.06539235133249\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b11f2","contributors":{"authors":[{"text":"Lee, Willis Thomas","contributorId":52949,"corporation":false,"usgs":true,"family":"Lee","given":"Willis","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":144670,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2591,"text":"wsp199 - 1907 - Underground water in Sanpete and central Sevier valleys, Utah","interactions":[],"lastModifiedDate":"2017-09-12T07:54:42","indexId":"wsp199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1907","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":"199","title":"Underground water in Sanpete and central Sevier valleys, Utah","docAbstract":"Sanpete and central Sevier valleys are situated at the border of the Basin Range and Plateau provinces in south-central Utah. They are bounded on the east by the Wasatch and Sevier plateaus and on the west by the Gunnison Plateau and the Valley and Pavant ranges, and are drained by Sevier River, which empties into Sevier Lake in the Great Basin. (See fig. 1, p. 6.)
These valleys rank with the richest parts of the State. They were occupied a few years after the Mormon pioneers founded Salt Lake City, in 1847, when settlements, which soon became thriving farming communities, were established where water for irrigation was most available. A variety of crops, especially wheat, are successfully grown, and the valleys are popularly known as the \"granary of Utah.\" Sheep raising is also an important industry, the adjacent highlands being used for summer pastures. The climate is arid, and there is a striking contrast between those areas which in their natural state are covered with sagebrush and grease wood and the fruitful cultivated tracts. (See PI. I, A and B.) Trees are normally absent in the valleys, but they flourish to a limited extent on the adjacent highlands, where there are thin growths of quaking aspen, scrub oak, and stunted conifers. Irrigation is necessary for the production of crops. Canal systems are maintained by San Pitch Creek and Sevier River, and the mountain streams are tapped by ditches near the mouths of the canyons, but this supply is insufficient and attention is being turned to the subterranean store.
This report is a preliminary statement of the general conditions of occurrence of underground water in Sanpete and central Sevier valleys. The field work was carried on in cooperation with Sanpete and Sevier counties through the State engineer, Mr. Caleb Tanner, who detailed Mr. C. S. Jarvis to collect the data embodied in the list of springs and wells on pages 51-60.
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