No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp218","usgsCitation":"Henshaw, F.F., and Covert, C.C., 1908, Water-supply investigations in Alaska, 1906-1907: Nome and Kougarok regions, Seward Peninsula; Fairbanks district, Yukon-Tanana region: U.S. Geological Survey Water Supply Paper 218, 156, v p., https://doi.org/10.3133/wsp218.","productDescription":"156, v p.","costCenters":[],"links":[{"id":425047,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24473.htm","text":"Nome region","linkFileType":{"id":5,"text":"html"}},{"id":425046,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24472.htm","text":"Kougarok region","linkFileType":{"id":5,"text":"html"}},{"id":402164,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24471.htm","text":"Fairbanks region","linkFileType":{"id":5,"text":"html"}},{"id":27086,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0218/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138370,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0218/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Fairbanks, Kougarok, Nome","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -147.667,\n 65.5\n ],\n [\n -147.667,\n 64.833\n ],\n [\n -146,\n 64.833\n ],\n [\n -146,\n 65.5\n ],\n [\n -147.667,\n 65.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -165.667,\n 65.25\n ],\n [\n -164,\n 65.25\n ],\n [\n -164,\n 65.833\n ],\n [\n -165.667,\n 65.833\n ],\n [\n -165.667,\n 65.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -166.333,\n 65.083\n ],\n [\n -166.333,\n 64.5\n ],\n [\n -164.333,\n 64.5\n ],\n [\n -164.333,\n 65.083\n ],\n [\n -166.333,\n 65.083\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d80","contributors":{"authors":[{"text":"Henshaw, Fred Forbes","contributorId":12452,"corporation":false,"usgs":true,"family":"Henshaw","given":"Fred","email":"","middleInitial":"Forbes","affiliations":[],"preferred":false,"id":144280,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Covert, Clermont Calvert","contributorId":26284,"corporation":false,"usgs":true,"family":"Covert","given":"Clermont","email":"","middleInitial":"Calvert","affiliations":[],"preferred":false,"id":144281,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":39532,"text":"pp60 - 1908 - The interpretation of topographic maps","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp60","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1908","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":"60","title":"The interpretation of topographic maps","language":"ENGLISH","doi":"10.3133/pp60","usgsCitation":"Salisbury, R.D., and Atwood, W.W., 1908, The interpretation of topographic maps: U.S. Geological Survey Professional Paper 60, 84 p. illus, clxx pl., https://doi.org/10.3133/pp60.","productDescription":"84 p. illus, clxx pl.","costCenters":[],"links":[{"id":120312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0060/report-thumb.jpg"},{"id":67138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d355","contributors":{"authors":[{"text":"Salisbury, Rollin D.","contributorId":71241,"corporation":false,"usgs":true,"family":"Salisbury","given":"Rollin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":221582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atwood, Wallace Walter","contributorId":85635,"corporation":false,"usgs":true,"family":"Atwood","given":"Wallace","email":"","middleInitial":"Walter","affiliations":[],"preferred":false,"id":221583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":39531,"text":"pp58 - 1908 - The Guadalupian Fauna","interactions":[],"lastModifiedDate":"2016-12-27T13:40:19","indexId":"pp58","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1908","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":"58","title":"The Guadalupian Fauna","docAbstract":"The first descriptions of the Guadalupian fauna were published nearly fifty years ago. This early account of Shumard's was meager enough, but gave promise of a facies interesting and novel among the known Carboniferous faunas of North America. The following pages add largely to our knowledge of Guadalupian life, and I believe more than make good any promise contained in the previous account. Nevertheless, even the collections of the Guadalupian fauna here described fail to do justice to its richness and diversity, and the present report is completed with the hope of returning to the subject after another visit to the Guadalupe Mountains.\r\n\r\nAlthough a description of this range and the adjacent region can be found elsewhere, a repetition of the more important facts will conduce to a better understanding of the geologic relations of the fauna described herein and will serve to illustrate the references to localities and horizons necessarily involved in the paleontologic discussion.\r\n\r\nThe Guadalupe Mountains are situated chiefly in southeastern New Mexico, but extend across the border for a short distance into the trans-Pecos region of Texas. Save only for this southern extreme both their geology and their topography are practically unknown, and it should be understood that anything hereafter said of them relates only to that portion.\r\n\r\nThese mountains form a north-south range of considerable height, which rises abruptly from an arid and treeless plain, stretching westward to more mountainous elevations, the Cornudas Mountains and the Sierra Tinaja Pinta. This plain is locally known as Crow Flats and forms a part of the Salt Basin (Pl. I). It is now used as cattle ranges, water being raised by windmills. The only permanent surface water consists of salt lakes - broad, shallow pools incrusted with saline deposits, which in the early days were extensively sought for domestic use. This water is of course unfit for consumption, but cattle seem as a rule not to mind the less highly impregnated waters brought up by the pumps. These vary considerably in the amount and character of their saline contents, but even the best is unsatisfactory for human use.\r\n\r\nOn the east side, from the foot of the mountains the land slopes gradually eastward and merges with the plains of Texas. There are springs of sweet water and perennial streams on this side of the range, such streams being in this region, as a rule, associated only with the highest mountains. Usually the canyons and sandy channels serve merely to carry off the occasional torrential rains, and this is the case for the most part even with the perennial streams, which almost immediately on striking into the plain are drunk up by the soil. Beyond their debouchure from the mountains their course is merely a dry sandy channel. There are, however, flowing streams east of the Guadalupes, one such being Delaware River. In seasons of rain this watercourse is formed by the confluence of numerous small tributaries - some leading back into the mountains - which pour their sudden waters through channels usually dry; but the source of the perennial stream seems to be a very definite point situated some distance east of the Guadalupes and generally referred to as the 'headwaters of the Delaware.' This expression would naturally be taken to have a more general significance, but Shumard uses it, I believe, in this local sense, and as it is often difficult to fix references to local geography it seems desirable to make the present record of the fact. At this point, which is also known as Huhling's ranch, three springs, one of them strongly charged with sulphur, break out close together in the bed of the Delaware, which below this point is a permanent watercourse.\r\n\r\nThe Guadalupe Mountains are formed by uplifted strata, consisting of a thick limestone series above and a thick sandstone series below. The abrupt termination of the limestone in an almost sheer precipice of practically its entire thickness","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp58","usgsCitation":"Girty, G., 1908, The Guadalupian Fauna: U.S. Geological Survey Professional Paper 58, 651 p., https://doi.org/10.3133/pp58.","productDescription":"651 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":67137,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0058/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0058/report-thumb.jpg"},{"id":12485,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/58/index.htm","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.25,31 ], [ -105.25,32 ], [ -104.25,32 ], [ -104.25,31 ], [ -105.25,31 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c388","contributors":{"authors":[{"text":"Girty, George H.","contributorId":22419,"corporation":false,"usgs":true,"family":"Girty","given":"George H.","affiliations":[],"preferred":false,"id":221581,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39534,"text":"pp63 - 1908 - Economic geology of the Georgetown quadrangle (together with the Empire district), Colorado","interactions":[],"lastModifiedDate":"2022-02-15T19:44:20.261866","indexId":"pp63","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1908","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":"63","title":"Economic geology of the Georgetown quadrangle (together with the Empire district), Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp63","usgsCitation":"Spurr, J., Garrey, G.H., and Ball, S., 1908, Economic geology of the Georgetown quadrangle (together with the Empire district), Colorado: U.S. Geological Survey Professional Paper 63, Report: 422 p.; 4 Plates: 16.88 × 27.82 inches or smaller, https://doi.org/10.3133/pp63.","productDescription":"Report: 422 p.; 4 Plates: 16.88 × 27.82 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":395978,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4644.htm"},{"id":67140,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0063/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264266,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0063/plate-44.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264265,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0063/plate-25.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264264,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0063/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264263,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0063/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0063/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Georgetown quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.75,\n 39.5\n ],\n [\n -105.5,\n 39.5\n ],\n [\n -105.5,\n 39.75\n ],\n [\n -105.75,\n 39.75\n ],\n [\n -105.75,\n 39.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625c04","contributors":{"authors":[{"text":"Spurr, Josiah E.","contributorId":55502,"corporation":false,"usgs":true,"family":"Spurr","given":"Josiah E.","affiliations":[],"preferred":false,"id":221586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrey, George H.","contributorId":39435,"corporation":false,"usgs":true,"family":"Garrey","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":221585,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ball, Sydney H.","contributorId":86413,"corporation":false,"usgs":true,"family":"Ball","given":"Sydney H.","affiliations":[],"preferred":false,"id":221587,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":36329,"text":"b347 - 1908 - The Ketchikan and Wrangell mining districts, Alaska","interactions":[],"lastModifiedDate":"2017-06-10T11:52:22","indexId":"b347","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1908","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":"347","title":"The Ketchikan and Wrangell mining districts, Alaska","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b347","usgsCitation":"Wright, F., and Wright, C.W., 1908, The Ketchikan and Wrangell mining districts, Alaska: U.S. Geological Survey Bulletin 347, 210, v p. :illus., xii pl. (incl. maps, part fold.) diagrs. ;24 cm., https://doi.org/10.3133/b347.","productDescription":"210, v p. :illus., xii pl. 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