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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.
Of Oklahoma's federally protected park or recreational sites, the Chickasaw National Recreation Area is the largest, with 4,500 acres (18 km 2). [18] Other federal protected sites include the Santa Fe and Trail of Tears national historic trails, the Fort Smith and Washita Battlefield national historic sites, and the Oklahoma City National ...
The property was purchased by the SGPA in 1933, during the Great Depression, for $30,000; the money was raised through private donations and the property became the Sleeping Giant State Park. [14] [A] Sleeping Giant State Park was created in 1924, when the SGPA donated 600 acres to the Park and Forest Commission. The state added an additional ...
Gloss Mountain State Park: Major: 640 260: 1977: Great Plains State Park: Kiowa: 187 76: 1977: Tom Steed Reservoir: Great Salt Plains State Park: Alfalfa: 840 340: 1952: Great Salt Plains Lake: Greenleaf State Park: Muskogee: 565 229: 1954: Greenleaf Lake: Honey Creek State Park: Delaware: 30 12: 1954: Grand Lake: Now known as the Honey Creek ...
The Ouachita Mountains (/ ˈ w ɒ ʃ ɪ t ɔː /), simply referred to as the Ouachitas, are a mountain range in western Arkansas and southeastern Oklahoma.They are formed by a thick succession of highly deformed Paleozoic strata constituting the Ouachita Fold and Thrust Belt, one of the important orogenic belts of North America. [3]
Geologic map for the Anadarko Basin showing thickness of strata between the Silurian Hunter Group and the Pennsylvanian Desmoinesian Anadarko Basin Geologic Cross Section. The Anadarko Basin is a geologic depositional and structural basin centered in the western part of the state of Oklahoma and the Texas Panhandle, and extending into southwestern Kansas and southeastern Colorado.
Geologic map A field of flowers in the Arbuckle foothills. Geologically the Arbuckles are an elongate anticline structure with an orientation or strike of west-northwest. The core of the structure consists of Proterozoic extrusive and intrusive rocks, the Colbert rhyolite porphyry and the Tishomingo granite (age dated at 1374 Ma), [3] which are overlain by the Arbuckle Group, the Simpson Group ...
Mill River passes through Sleeping Giant State Park in northern Hamden and East Rock Park below Lake Whitney in Hamden. These are among the river's reaches that remain undeveloped and are popular spots for fishing and hiking. The USGS has maintained a gauge (01196620) near Sleeping Giant for the past 41 year to continuously monitor flow.