Mines and prospects in and around the Farmington Canyon complex, northern Utah (OFR-325) Recreation Maps and a large majority of

and a large majority of the wells only test the upper section of the Paradox Formation of Pennsylvanian age

Most of the mountain consists of Permian and Pennsylvanian marine sedimentary strata capped by probable Late Cretaceous and early Tertiary synorogenic deposits

easy to read color palette featuring blue oceans and stunning shaded relief that has been featured on National Geographic wall maps for over 75 years

from the popular Bald Mountain Trail to the challenging Mount Agassiz Trail

National Geographic Wall map of Alaska in Classic style

Mines and prospects in and around the Farmington Canyon complex, northern Utah (OFR-325) Recreation Maps and a large majority ofBy: R. W. Gloyn, M. A. Shubat, and B. H. Mayes Forty three mines and prospects were examined in the northern Wasatch Mountains of north central Utah. Areas sampled include the Argenta, Morgan, Farmington, and Hot Springs(City Creek) districts and the Mountain Green area. One hundred and twenty three samples were collected and assayed for 17 elements including base and precious metals and a broad suite of associated elements. Four ore types were found.