Mineral occurrences of the Tooele 1o x 2o quadrangle, west-central Utah (OFR-153) Topographic Map Strata in the region were

Strata in the region were deformed by Late Cretaceous to early Tertiary contractional folding and faulting of the Sevier orogeny

the native peoples who in the eleventh century converged on Chaco Canyon (in today's southwestern New Mexico) and built what has been called the Las Vegas of its day

and (3) an up-to-date reference for all who are interested in Great Salt Lake

geotourism locations

No coal resources in the Ferron Sandstone and Muley Canyon Sandstone members of the Mancos are known to lie below 2

Mineral occurrences of the Tooele 1o x 2o quadrangle, west-central Utah (OFR-153) Topographic Map Strata in the region wereBy: B. T. Tripp, M. A. Shubat, C. E. Bishop, and R. E. Blackett This report summarizes the available data for mineral occurrences within the Tooele 1x2 quadrangle (1: 250,000 scale), located in west central Utah. Summary information for each mineral occurrence within the Tooele quadrangle is organized by mining district. For each district, a brief summary of the economic geology, history, and production is given. This is followed by a table listing