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Dimetrodon (/ d aɪ ˈ m iː t r ə ˌ d ɒ n / ⓘ [1] or / d aɪ ˈ m ɛ t r ə ˌ d ɒ n /; [2] lit. ' two measures of teeth ') is an extinct genus of non-mammalian synapsid belonging to the family Sphenacodontidae that lived during the Cisuralian age of the Early Permian period, around 295–272 million years ago.
The best source of Mississippian fossils in Oklahoma is the state's northeastern region. [2] During the Carboniferous, Oklahoma was a terrestrial environment characterized by vast river systems and accompanying deltas. These deltas were home to vast swamps responsible for leaving behind many coal deposits. [3]
The former Lake Eucha State Park; owned and managed by the city of Tulsa since 2011; [5] Park is not actually on Lake Eucha Okmulgee Park: Okmulgee: 1,075 1963 Okmulgee Lake: The former Okmulgee State Park; owned and managed by the City of Okmulgee since 2015 Red Rock Canyon Park: Caddo: 310: 1956: Leased to the City of Hinton, Oklahoma in 2018 ...
This list of the prehistoric life of Oklahoma contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of Oklahoma. Precambrian [ edit ]
The Texas and Oklahoma red beds are sedimentary rocks, mostly consisting of sandstone and red mudstone. [8] The red color of the rocks is due to the presence of ferric oxide . [ 9 ] The rocks were deposited during the early Permian in a warm, moist climate, [ 10 ] with seasonal periods of dry conditions.
Oklahoma's first and largest state park, Lake Murray State Park surrounds its namesake lake and consists of 12,500 acres. You can stay at the park with RV and tent campgrounds, cabins and the lodge.
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This list of the Paleozoic life of Oklahoma contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of Oklahoma and are between 541 and 252.17 million years of age.