Salt Lake County Progress Report
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Salt Lake City Progress Report
Author | : Salt Lake City (Utah) |
Publisher | : |
Total Pages | : 332 |
Release | : 1932 |
Genre | : Corporate minutes |
ISBN | : |
Salt Lake City Progress Report
Author | : Salt Lake City (Utah) |
Publisher | : |
Total Pages | : 290 |
Release | : 1918 |
Genre | : Corporate minutes |
ISBN | : |
Report to the People of Salt Lake County
Author | : Salt Lake County Government Study Commission |
Publisher | : |
Total Pages | : |
Release | : 1974 |
Genre | : Salt Lake County (Utah) |
ISBN | : |
Report of the Survey of the Public School System of Salt Lake City, Utah
Author | : Salt Lake City (Utah). Survey committee |
Publisher | : |
Total Pages | : 350 |
Release | : 1915 |
Genre | : Education |
ISBN | : |
Report to the People of Salt Lake County
Author | : Salt Lake County Government Study Commission |
Publisher | : |
Total Pages | : 63 |
Release | : 1974 |
Genre | : Local government |
ISBN | : |
Monthly Catalog of United States Government Publications
Author | : United States. Superintendent of Documents |
Publisher | : |
Total Pages | : |
Release | : 1985 |
Genre | : Government publications |
ISBN | : |
February issue includes Appendix entitled Directory of United States Government periodicals and subscription publications; September issue includes List of depository libraries; June and December issues include semiannual index
Engineering Geology of the Salt Lake City Metropolitan Area, Utah
Author | : William R. Lund |
Publisher | : Utah Geological Survey |
Total Pages | : 77 |
Release | : 1990 |
Genre | : Engineering geology |
ISBN | : 1557910936 |
Geologic exposures in the Salt Lake City region record a long history of sedimentation and tectonic activity extending back to the Precambrian Era. Today, the city lies above a deep, sediment-filled basin flanked by two uplifted range blocks, the Wasatch Range and the Oquirrh Mountains. The Wasatch Range is the easternmost expression of major Basin and Range extension in north-central Utah and is bounded on the west by the Wasatch fault zone (WFZ), a major zone of active normal faulting. During the late Pleistocene Epoch, the Salt Lake City region was dominated by a succession of inter-basin lakes. Lake Bonneville was the last and probably the largest of these lakes. By 11,000 yr BP, Lake Bonneville had receded to approximately the size of the present Great Salt Lake.