Arbuckle Mountains | |
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![]() Turner Falls, nestled in the Arbuckle Mountains of South Central Oklahoma. | |
Highest point | |
Elevation | 430 m (1,410 ft) |
Coordinates | 34°27′24″N 97°15′14″W / 34.45667°N 97.25389°W |
Dimensions | |
Area | 1,000 sq mi (2,600 km2) |
Geography | |
Country | United States |
State | Oklahoma |
Counties | |
Rivers | Washita |
Settlement | Cedar Village |
Range coordinates | 34°25′55″N 97°11′27″W / 34.4320324°N 97.1908524°W |
Geology | |
Orogeny | Ouachita Orogeny |
Age of rock | |
Type of rock | granite, gneiss, limestone, dolomite, sandstone, shale |
The Arbuckle Mountains are an ancient mountain range in south-central Oklahoma in the United States. They lie in Murray, Carter, Pontotoc, and Johnston counties.[1] The granite rocks of the Arbuckles date back to the Precambrian Eon some 1.4 billion years ago which were overlain by rhyolites during the Cambrian Period. The range reaches a height of 1,412 feet above sea level. According to the U.S. Geological Survey (USGS):
The Arbuckles contain the most diverse suite of mineral resources in Oklahoma: limestone, dolomite, glass sand, granite, sand and gravel, shale, cement, iron ore, lead, zinc, tar sands, and oil and gas; all these minerals are, or have been, produced commercially.[2]