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You can find many different types of gemstones, minerals, and other interesting materials in Oklahoma. In Comanche County and the McCurtain County, quartz, malachite, aegirine, orthoclase, and barite are common. However, if you want a more unusual gemstone, such as brochantite, you have to go to Garvin County.
OKLAHOMAS MINERALS The extraction or mining of minerals from the earth occurs in every county of the state. Minerals mines in Oklahoma include coal (not shown), limestone, dimensional stone, sand and gravel, gypsum, clay and shale, granite, caliche, tripoli, salt, iron ore (not shown), and chat (not shown).
Some of the oldest mountains in the United States, the western Arbuckle Mountains has a core comprised of Precambrian granite and gneiss that is 1.3 billion years old.
The Ouachita Province geology is composed pre-dominantly of clastic (fragmented) rock strata that have been intensely folded and faulted. Rock strata present today are the highly eroded roots of the frontal element of the Ouachita orogenic belt (a mountainous belt formed by folding of the Earths crust).
The Ouachita Mountain Range, located throughout southeastern Oklahoma, is characterized by rolling, rocky terrain and pine-covered hills.
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The force of this upheaval was so great that many of the sandstone, shale, and limestone layers were broken and folded, creating large anticlines. Along with the folding process, this upward thrust formed the Arbuckle Mountains.
Composed of pink and gray granites, the mountains are part of the Wichita range, which formed 550 million years ago as a failed continental rift system and was then uplifted 300 million years ago. They eroded to form the present mountain range.
The geology of Oklahoma is characterized by Carboniferous rocks in the east, Permian rocks in the center and towards the west, and a cover of Tertiary deposits in the panhandle to the west. The panhandle of Oklahoma is also noted for its Jurassic rocks as well. Cretaceous sediments are found in the south east.
Most outcrops in Oklahoma are sedimentary rocks, consisting mainly of shale, sandstone, and limestone; outcrops of igneous and metamorphic rocks, such as granite, rhyolite, gabbro, and gneiss, occur mostly in the Wichita and Arbuckle Mountains.
Great Salt Plains State Park in Jet, Oklahoma, is the only place in the world where you can dig for these hourglass-shaped crystals. Youll find the state park about 45 miles northeast of Enid at 23280 S Spillway Drive in the Salt Plains National Wildlife Refuge.

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