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Off.,","doi":"10.3133/b537","usgsCitation":"Smith, G.O., 1913, The classification of the public lands: U.S. Geological Survey Bulletin 537, 197 p. :diagrs. ;24 cm., https://doi.org/10.3133/b537.","productDescription":"197 p. :diagrs. ;24 cm.","costCenters":[],"links":[{"id":93598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0537/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0537/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668f79","contributors":{"authors":[{"text":"Smith, George Otis","contributorId":19538,"corporation":false,"usgs":true,"family":"Smith","given":"George","email":"","middleInitial":"Otis","affiliations":[],"preferred":false,"id":215325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39484,"text":"pp80 - 1913 - Geology and ore deposits of the San Francisco and adjacent districts, Utah","interactions":[],"lastModifiedDate":"2025-09-22T20:16:14.717131","indexId":"pp80","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":"80","title":"Geology and ore deposits of the San Francisco and adjacent districts, Utah","docAbstract":"The San Francisco district was of recognized importance in the early days of mining in Utah, but its output soon declined and thereafter it attracted little attention until about 1903, when the development of the Cactus mine was undertaken.
In August, 1904, S. F. Emmons, then in charge of the division of metalliferous deposits of the Geological Survey, visited the district and determined the area to be covered by a projected topographic map. In 1904 and 1905 Fred McLaughlin completed a topographic map covering the San Francisco and Preuss districts and parts of the Beaver Lake, Rocky, and Star districts, an area of about 175 square miles.
In the spring of 1908 Waldemar Lindgren, in charge of the division of metalliferous deposits, visited the San Francisco district and decided that the Survey should make a study of its geology. The writer was assigned to the work of mapping the surface geology and was occupied in this work during part of July, the whole of August, and part of September, 1908.
Before the geologic work was completed the renewed activity in the Star district made it desirable that all that district should be included in the geologic study and therefore, in the summer of 1909, W. M. Beaman extended the topographic work to include the more active parts of the Star, Rocky, and Beaver Lake districts that were not included in the previous map. The total area mapped is about 200 square miles.
In 1909 the writer was assigned to the study of the ore deposits and spent the greater part of July, the whole of August, and part of September in the district. In 1910 he spent about 10 days in the district and in 1910 and 1911 was engaged in studying other districts in southwestern Utah. Office work on the present report has been in progress since the fall of 1908.
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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":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.
","language":"English","publisher":"Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp78","usgsCitation":"Emmons, W.H., and Calkins, F.C., 1913, Geology and ore deposits of the Philipsburg quadrangle, Montana: U.S. Geological Survey Professional Paper 78, Report: 271 p.; 2 Plates: 17.04 x 24.0 and 16.04 x 19.88 inches, https://doi.org/10.3133/pp78.","productDescription":"Report: 271 p.; 2 Plates: 17.04 x 24.0 and 16.04 x 19.88 inches","numberOfPages":"300","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":104531,"rank":700,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0078/report.pdf","text":"Report","linkFileType":{"id":5,"text":"html"}},{"id":397961,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4657.htm"},{"id":169972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0078/report-thumb.jpg"},{"id":308538,"rank":701,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0078/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":308539,"rank":702,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0078/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Philipsburg quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.5,\n 46\n ],\n [\n -113.5,\n 46.5\n ],\n [\n -113,\n 46.5\n ],\n [\n -113,\n 46\n ],\n [\n -113.5,\n 46\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843ef","contributors":{"authors":[{"text":"Emmons, William Harvey","contributorId":75636,"corporation":false,"usgs":true,"family":"Emmons","given":"William","email":"","middleInitial":"Harvey","affiliations":[],"preferred":false,"id":221509,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Calkins, Frank Cathcart","contributorId":31734,"corporation":false,"usgs":true,"family":"Calkins","given":"Frank","email":"","middleInitial":"Cathcart","affiliations":[],"preferred":false,"id":221510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52746,"text":"b530E - 1913 - Structural materials","interactions":[{"subject":{"id":52746,"text":"b530E - 1913 - Structural materials","indexId":"b530E","publicationYear":"1913","noYear":false,"chapter":"E","title":"Structural materials"},"predicate":"IS_PART_OF","object":{"id":33172,"text":"b530 - 1913 - Contributions to economic geology (short papers and preliminary reports), 1911, Part I, Metals and nonmetals except fuels","indexId":"b530","publicationYear":"1913","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1911, Part I, Metals and nonmetals except fuels"},"id":1}],"isPartOf":{"id":33172,"text":"b530 - 1913 - Contributions to economic geology (short papers and preliminary reports), 1911, Part I, Metals and nonmetals except fuels","indexId":"b530","publicationYear":"1913","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1911, Part I, Metals and nonmetals except fuels"},"lastModifiedDate":"2022-06-07T18:22:03.4832","indexId":"b530E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1913","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":"530","chapter":"E","title":"Structural materials","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1911, Part I, Metals and nonmetals except fuels (Bulletin 530)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b530E","usgsCitation":"Katz, F.J., Lupton, C., Matson, G.C., Miser, H.D., and Stose, G.W., 1913, Structural materials: U.S. Geological Survey Bulletin 530, 84 p., https://doi.org/10.3133/b530E.","productDescription":"84 p.","costCenters":[],"links":[{"id":178001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/530-E/report-thumb.jpg"},{"id":342179,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/530-E/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401862,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20050.htm"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6362","contributors":{"authors":[{"text":"Katz, Frank James","contributorId":60695,"corporation":false,"usgs":true,"family":"Katz","given":"Frank","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":245956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lupton, Charles T.","contributorId":67853,"corporation":false,"usgs":true,"family":"Lupton","given":"Charles T.","affiliations":[],"preferred":false,"id":245957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matson, George Charlton","contributorId":6021,"corporation":false,"usgs":true,"family":"Matson","given":"George","email":"","middleInitial":"Charlton","affiliations":[],"preferred":false,"id":245954,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miser, Hugh Dinsmore","contributorId":95130,"corporation":false,"usgs":true,"family":"Miser","given":"Hugh","email":"","middleInitial":"Dinsmore","affiliations":[],"preferred":false,"id":245958,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stose, George W.","contributorId":46067,"corporation":false,"usgs":true,"family":"Stose","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":245955,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":2279,"text":"wsp320 - 1913 - Geology and water resources of Sulphur Spring Valley, Arizona, with a section on agriculture","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp320","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":"320","title":"Geology and water resources of Sulphur Spring Valley, Arizona, with a section on agriculture","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp320","usgsCitation":"Meinzer, O.E., Kelton, F., and Forbes, R.H., 1913, Geology and water resources of Sulphur Spring Valley, Arizona, with a section on agriculture: U.S. Geological Survey Water Supply Paper 320, 231 p. :illus., XV pl. (on 14 l.) 2 fold. maps (in pocket) diagrs. (part fold.) ;24 cm., https://doi.org/10.3133/wsp320.","productDescription":"231 p. :illus., XV pl. (on 14 l.) 2 fold. maps (in pocket) diagrs. (part fold.) ;24 cm.","costCenters":[],"links":[{"id":137619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0320/report-thumb.jpg"},{"id":28070,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0320/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28071,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0320/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0320/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684104","contributors":{"authors":[{"text":"Meinzer, Oscar Edward","contributorId":12020,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":144945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kelton, F.C.","contributorId":9632,"corporation":false,"usgs":true,"family":"Kelton","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":144944,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forbes, Robert Humphrey","contributorId":103246,"corporation":false,"usgs":true,"family":"Forbes","given":"Robert","email":"","middleInitial":"Humphrey","affiliations":[],"preferred":false,"id":144946,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}