Franklin Mountains (Texas)

From Wikipedia, the free encyclopedia
Jump to: navigation, search
Franklin Mountains
North Franklin Peak, looking northeast from South Franklin Mountain
Highest point
Peak North Franklin Peak
Elevation 7,192 ft (2,192 m)
Coordinates 31°54′10″N 106°29′36″W / 31.90278°N 106.49333°W / 31.90278; -106.49333Coordinates: 31°54′10″N 106°29′36″W / 31.90278°N 106.49333°W / 31.90278; -106.49333
Country United States
States Texas and New Mexico
Orogeny Laramide orogeny
Age of rock Cretaceous
Type of rock Sedimentary, Igneous

The Franklin Mountains of Texas are a small range (23 miles long, 3 miles (4.8 km) wide) that extend from El Paso, Texas north into New Mexico.[1] The Franklins were formed due to crustal extension related to the Cenozoic Rio Grande rift. Although the present topography of the range and adjoining basins is controlled by extension during rifting in the last 10 million years, faults within the range also record deformation during the Laramide orogeny, between 85 and 45 million years ago.

The highest peak is North Franklin Peak at 7,192 feet (2,192 m). Much of the range is part of the Franklin Mountains State Park. The mountains are composed primarily of sedimentary rock with some igneous intrusions. Geologists refer to them as tilted-block fault mountains and in them can be found 1.25 billion-year-old[2] Precambrian rocks, the oldest in Texas.[1][3]


See also[edit]


  1. ^ a b Van Hise, C.R. and Leith, C.K. 1909. Pre-Cambrian Geology of North America. United States Geological Survey, Bulletin 360, 939 pp. (See pp. 746-748)
  2. ^ Precambrian rocks can be seen in the Tom Mays unit of the Franklin Mountains park
  3. ^ Brooks, A.H. 1904. The Geological Society of Washington. Science NS 19(490):794-796.

External links[edit]