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Turner Falls is a waterfall on Honey Creek in the Arbuckle Mountains of south-central Oklahoma, United States, 6 miles (9.7 km) south of Davis. [ 1 ] [ 2 ] With a height of 77 feet (23 m), Turner Falls is locally considered Oklahoma's tallest waterfall, [ 3 ] although its height matches one in Natural Falls State Park .
Natural Falls State Park is a 120 acres (0.49 km 2) state-owned park in the Ozarks, in Delaware County, Oklahoma. It lies along U.S. Highway 412, near the Arkansas-Oklahoma state line. It lies along U.S. Highway 412, near the Arkansas-Oklahoma state line.
Turner Falls is located 5 miles (8.0 km) south of Davis, whereas Chickasaw NRA is located in the city of Sulphur. The area is also the location of several campgrounds, including the YMCA's Camp Classen and the Baptist General Convention of Oklahoma's Falls Creek Baptist Conference Center, which hosts 55,000 campers each summer.
The wilderness has both Pine Mountain and Rich Mountain which are two long mountain ridges that rise to over 2,600 feet (792 m) above sea level. Several streams and waterfalls flow off the ridges creating the headwaters of the Kiamichi River. Beech trees, usually found much farther north, along with pine and dense stands of oak dominate the forest.
The Kiamichi Mountains (Choctaw: Nʋnih Chaha Kiamitia) are a mountain range in southeastern Oklahoma. A subrange within the larger Ouachita Mountains that extend from Oklahoma to western Arkansas , [ 1 ] the Kiamichi Mountains sit within Le Flore , Pushmataha and McCurtain counties near the towns of Poteau , Albion and Smithville .
Pages in category "Waterfalls of Oklahoma" The following 2 pages are in this category, out of 2 total. This list may not reflect recent changes. N.
In Oklahoma, it’s illegal to shoot a mountain lion unless you are protecting yourself or your property, authorities said. If you kill a mountain lion, you must immediately call the state department.
The Wichita Mountains are located in the southwestern portion of the U.S. state of Oklahoma. [1] It is the principal relief system in the Southern Oklahoma Aulacogen, being the result of a failed continental rift. The mountains are a northwest-southeast trending series of rocky promontories, many capped by 500 million-year old granite.