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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.
The Ozark Highlands Trail roams 218 miles (351 km) through parts of seven counties in northwest Arkansas. [1] It stretches from Lake Fort Smith State Park , across the Ozark National Forest , to the Buffalo National River .
A rural Ozarks scene. Phelps County, Missouri The Saint Francois Mountains, viewed here from Knob Lick Mountain, are the exposed geologic core of the Ozarks.. The Ozarks, also known as the Ozark Mountains, Ozark Highlands or Ozark Plateau, is a physiographic region in the U.S. states of Missouri, Arkansas, and Oklahoma, as well as a small area in the southeastern corner of Kansas. [1]
Some parts of the trail are called the “Highlands” because the region includes plateaus, rolling hills, and karst formations. ... Much of the Ozark trail is located in the Mark Twain National ...
The Ozark Highlands Trail, built and maintained by over 3,000 volunteers, is the longest hiking trail in the forest and extends for 165 miles (270 km) from the Buffalo National River to Lake Fort Smith State Park in the far western portion of the state. The forest also contains several multi-use trails including the Pedestal Rock Trail and the ...
The Springfield Plateau is the only Ozark Highland Level IV ecoregion within all four states. [1] The nearly level to rolling Springfield Plateau is underlain by cherty limestone of the Mississippian Boone Formation and Burlington Limestone; it is less rugged and wooded than Ecoregions 38, 39b, and 39c, and lacks the Ordovician dolomite and limestone of Ecoregions 39c and 39d.
According to the U.S. Census Bureau, the county has a total area of 591 sq mi (1,530 km 2), of which 29 sq mi (75 km 2) (4.9%) are covered by water. [4] It is part of the Ozark Highlands.
It is one of the Ozark Plateaus; some folding and faulting has occurred but, in general, strata are much less deformed than in the Ouachita Mountains. Maximum elevations are higher, soils have a warmer temperature regime, and carbonate rocks are much less extensive than in the Ozark Highlands. Physiography is distinct from the Arkansas Valley.
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