This paper is the result of field work done during the seasons of 1904 and 1905 It is designed mainly to furnish information regarding geologic structure and the prospects for underground water. The description of the formations of the Bighorn Mountain area is chiefly the work of N. H. Darton, under whose direction the exploration ·was made.
\nA general account of the surface waters is given, including a statement of their present and proposed uses for irrigation, and the economic products of a geologic nature are also described. The region considered comprises the Bighorn basin, a part of the Clark Fork basin, and the slopes of the adjoining mountain ranges, the entire area comprising 8,500 square miles. As shown on fig. 1, it is situated mainly in Bighorn County, in the northwestern part of Wyoming, and includes the greater portion of the area lying between meridians 107° 15' and 109° 15' and parallels 43° 40' and 45°. It is bounded on the north by Montana, on the east by the Bighorn Mountains, on the south by Bighorn and Owl Creek mountains, and on the west by Shoshone, Absaroka, and Beartooth mountains.
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The lofty Wasatch Range (Pl. I), the westernmost of the Rocky Mountain system, limits the valleys on the east, and relatively low basin ranges - the Oquirrh, Lake, and East Tintic mountains - determine them on the west. The valleys trend north and south, and are almost separated by the low east-west Traverse Range, the slopes of which constitute a dam for Utah Lake, which drains through Jordan River to Great Salt Lake.
The area under consideration is the most populous and flourishing part of the State, Salt Lake City and Provo, the first and third cities in the State, and many other thriving settlements are there located. At Bingham Junction and Murray a number of smelters treat the ores from near-by mines, but agriculture is the main industry. Water for irrigation is supplied by mountain streams, and intensive farming is successfully pursued. The practice of irrigation was begun by the Mormon pioneers in 1847, and has been discussed in several publications; little attention, however, has been given to the underground water resources, and, so far as the writer is aware, they have not before been described. The present paper outlines conditions of occurrence of the subterranean waters and describes their development in the valleys of Utah Lake and Jordan River.
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B.","contributorId":70356,"corporation":false,"usgs":true,"family":"Richardson","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":287519,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, David T.","contributorId":43730,"corporation":false,"usgs":true,"family":"Day","given":"David","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":287518,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richards, R.H.","contributorId":99653,"corporation":false,"usgs":true,"family":"Richards","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":287520,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":76652,"text":"b285B - 1906 - Contributions to economic geology, 1905: Copper","interactions":[],"lastModifiedDate":"2012-02-02T00:14:17","indexId":"b285B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"285","chapter":"B","title":"Contributions to economic geology, 1905: Copper","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1905","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/b285B","usgsCitation":"Weed, W.H., Emmons, W.H., Collier, A.J., and Phalen, W.C., 1906, Contributions to economic geology, 1905: Copper: U.S. Geological Survey Bulletin 285, p. 93-145, https://doi.org/10.3133/b285B.","productDescription":"p. 93-145","costCenters":[],"links":[{"id":115643,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0285b/report.pdf","size":"4759","linkFileType":{"id":1,"text":"pdf"}},{"id":194623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0285b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697bb6","contributors":{"authors":[{"text":"Weed, W. H.","contributorId":75208,"corporation":false,"usgs":true,"family":"Weed","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":287515,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmons, W. H.","contributorId":38623,"corporation":false,"usgs":true,"family":"Emmons","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":287514,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collier, A. J.","contributorId":98286,"corporation":false,"usgs":true,"family":"Collier","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":287517,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phalen, W. C.","contributorId":90358,"corporation":false,"usgs":true,"family":"Phalen","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":287516,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":2116,"text":"wsp182 - 1906 - Flowing wells and municipal water supplies in the southern portion of the southern peninsula of Michigan","interactions":[],"lastModifiedDate":"2017-01-11T14:35:15","indexId":"wsp182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"182","title":"Flowing wells and municipal water supplies in the southern portion of the southern peninsula of Michigan","docAbstract":"A large amount of data on water supplies was collected by the writer in the course of glacial investigations made under the direction of Prof. T. C. Chamberlin in the last five years in the Southern Peninsula of Michigan. These investigations resulted in a partial acquaintance with conditions in about 200 separate flowing-well districts and brought out matters of such exceptional importance that arrangements were made to extend them by examining each of the flowing-well districts in the State sufficiently to determine its essential characteristics, present state of development, and probable capacity for future development. It was arranged also that the quality of various classes of waters, both surface and underground, as well as water supplies of the cities and villages, should be given attention. As the mineral waters of the State had already been discussed in some detail by the State geologist, Dr. A. C. Lane, in Water-Supply Paper No. 31 of the United States Geological Survey, it was deemed unnecessary to prepare another report on that subject, but arrangements were made with Doctor Lane for embodying in this report the large amount of material which had accumulated at his office relative to other classes of water supply, and also for furnishing reports on certain counties in which special investigations had been carried on by the State survey. The results of all these studies, so far as they apply to the southern counties (see fig. 1), are embodied in the present report; the remainder will appear in a companion report on the middle and northern counties of the Southern Peninsula of Michigan.
","language":"English","publisher":"Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp182","usgsCitation":"Leverett, F., 1906, Flowing wells and municipal water supplies in the southern portion of the southern peninsula of Michigan: U.S. Geological Survey Water Supply Paper 182, xi, 292, iii p., https://doi.org/10.3133/wsp182.","productDescription":"xi, 292, iii p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":27704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0182/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0182/report-thumb.jpg"}],"country":"United 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Frank","contributorId":77512,"corporation":false,"usgs":true,"family":"Leverett","given":"Frank","email":"","affiliations":[],"preferred":false,"id":144696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2120,"text":"wsp161 - 1906 - Quality of water in the upper Ohio River basin and at Erie, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-22T08:30:20","indexId":"wsp161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"161","title":"Quality of water in the upper Ohio River basin and at Erie, Pennsylvania","docAbstract":"This paper discusses the quality of water on the most important tributaries of Ohio River in Pennsylvania, New York, West Virginia, and Maryland, and the nature of the water supply at Erie, Pa. The amount and character of the pollution is described and the results of drinking contaminated water as shown by typhoid statistics are indicated. The conditions on the tributaries of Ohio River in Ohio are discussed in Water-Supply and Irrigation Paper No. 79, United States Geological Survey, pages 129-187. The water supplies and sewerage of small towns high up toward the head of a large drainage system do not in many cases receive the attention they should. Epidemics of a waterborne disease which affect large municipalities near the mouth of the river and therefore attract attention must necessarily have their origin in the pollution of the watershed above. It is evident, therefore, that adequate sanitation of the small towns and a water supply as carefully guarded as that of a large city would prevent disease at its very source and be far less expensive than the costly battles which are waged against epidemics in huge centers of population after disease has broken out. Typhoid fever statistics for small towns in this section are seldom available and are more or less unreliable at best. The few figures given show the existence of virulent typhoid fever in most towns of the drainage areas in certain years, and as these towns drain into the streams the liability ofthe water to infection is evident. The significance of typhoid fever death rates will be better understood from the statistics presented below, which have been collated from a number of cities having excellent water supplies.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp161","usgsCitation":"Lewis, S.J., 1906, Quality of water in the upper Ohio River basin and at Erie, Pennsylvania: U.S. Geological Survey Water Supply Paper 161, 114 p., 1 l. :illus., VI pl. (incl. fold. diagr.) ;23 cm., https://doi.org/10.3133/wsp161.","productDescription":"114 p., 1 l. :illus., VI pl. (incl. fold. diagr.) ;23 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":27708,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0161/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0161/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651686","contributors":{"authors":[{"text":"Lewis, Samuel James","contributorId":93882,"corporation":false,"usgs":true,"family":"Lewis","given":"Samuel","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":144701,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}