Earth and Planetary Sciences ETDs
Publication Date
Spring 5-13-1953
Abstract
Southwestern New Mexico is characterized by Basin and Range Physiography. Nearly level bolson plains are interrupted irregularly by linear mountain ranges. Sedimentary rocks ranging in age from Cambrian and recent crop out in the mountain areas. Darton (1916) mapped and described a limestone formation, about 1,000 feet thick, which he named Gym limestone. He thought the Gym was restricted in outcrop to Luna County and was distinct from previously described Paleozoic formations. The Gym was originally thought to be Pennsylvanian in age but later on was regarded as Permian. In the restudy of the Gym limestone was the basis of this thesis it was found that Darton's Gym included Silurian, Devonian, Mississippian, Pennsylvanian, and Cretaceous (?) rocks in addition to some strata of Permian Age.
Degree Name
Earth and Planetary Sciences
Level of Degree
Masters
Department Name
Department of Earth and Planetary Sciences
First Committee Member (Chair)
Vincent Cooper Kelley
Second Committee Member
None
Third Committee Member
None
Language
English
Keywords
Gym Limestone
Document Type
Thesis
Recommended Citation
Bogart, Lowell E.. "The Huego (GYM) Limestone, Luna County, New Mexico." (1953). https://digitalrepository.unm.edu/eps_etds/122
Generalized Map of the Florida and Victoria Mountains with Geologic Changes
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