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Cretaceous Formations of the Dallas-Fort Worth Metroplex Geologic map and the labeled geologic formations that lie directly beneath the surface in Dallas County Cretaceous formations of Texas Where the DFW Metroplex was located during the last super continent known as Pangea Placement of Tectonic Plates and DFW location around ≈94 million years ago The Cretaceous rocks in the DFW Metroplex ...
The live Neil Young album Road Rock Vol. 1 and its accompanying DVD, Red Rocks Live, were filmed and recorded at Red Rocks in 2000 during the "Silver and Gold" tour. Local Colorado band Big Head Todd and the Monsters released a DVD and live album of a 1995 performance in 2003, capturing what has become a local annual early season tradition.
Permian rocks are the best-known of the Texas Paleozoic. They are widespread in north Texas, where their characteristic red beds are spectacularly exposed in Palo Duro Canyon. The strata are also oil-rich where buried in west Texas, such as in the Midland and Odessa region. This crude oil-rich area is known as the Permian Basin.
The Barnett Shale is a geological formation located in the Bend Arch-Fort Worth Basin. It consists of sedimentary rocks dating from the Mississippian period (354–323 million years ago) in Texas. The formation underlies the city of Fort Worth and underlies 5,000 mi 2 (13,000 km 2) and at least 17 counties.
The Dallas–Fort Worth metroplex, officially designated Dallas–Fort Worth–Arlington by the U.S. Office of Management and Budget, [a] is the most populous metropolitan statistical area in the U.S. state of Texas and the Southern United States, encompassing 11 counties. Its historically dominant core cities are Dallas and Fort Worth. [5]
Tarrant (Fort Worth) 121 0 Metroplex: 221 Taylor: 61 0 Northwest: 222 Terrell: 4 0 West Texas: 223 Terry 0 0 Gulf Coast: 224 Throckmorton: 1 0 Northwest: 225 Titus: 1 0 Upper East: 226 Tom Green: 70 1 West Texas: 227 Travis: 215 2 Capital: 228 Trinity: 4 0 Southeast: 229 Tyler: 3 0 Southeast: 230 Upshur: 2 0 Upper East: 231 Upton 0 0 West Texas ...
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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. [11]