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USGS · 70179734

Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data

D. C. Hahl·C.G. Mitchell
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Abstract

This report presents the data collected for a study of the dissolved-mineral load contributed by surficial sources to Great Salt Lake, Utah. The study was conducted by the U.S. Geological Survey in cooperation with the University of Utah during the period from July 1959 through June 1962, and is part of an overall investigation of the Great Salt Lake basin by the University. Financial support for the study was provided by the U.S. Geological Survey and by the University of Utah Research Fund and Uniform School Fund. Some of the data presented in this report were obtained as part of cooperative programs between the Geological Survey and other agencies.

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Utah Geological and Mineralogical Survey Water-Resources BulletinReport
90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 40.59727063442024° to 41.795888098191426° latitude; -113.2305908203125° to -111.81884765624999° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

D. C. Hahl, C.G. Mitchell. 1963. Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data. https://pubs.usgs.gov/publication/70179734

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