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] Fault or Balcones Fault Zone is an area of largely normal faulting [1] in the U.S. state of Texas that runs roughly from the southwest part of the state near Del Rio to the north-central region near Dallas [2] along Interstate 35. The Balcones Fault zone is made up of many smaller features, including normal faults, grabens, and horsts. [3]
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 ...
[3]: 27 [5] The northern and northeastern parts of Texas, including the Dallas–Fort Worth metroplex, are another region of seismic risk. Though the area does experience some minor earthquakes, including induced earthquakes naturally-occurring tremors potentially along buried faults, shaking from distant earthquakes presents the primary ...
The region was also the only one in antebellum slave states to back the insurgent candidacy of Robert La Follette in 1924; in fact, Comal was La Follette’s top county in the nation with 73.96% of the vote, and Gillespie and Comal were the only counties south of the Mason–Dixon line to give a plurality to his “Progressive” ticket.
A newly found fault line with a rare slanted angle shows why an earthquake rattled New York City in April harder than its epicenter in ... About 100,000 eggs worth $40K stolen from trailer in ...
This region contains the cities of Fort Worth, Granbury and Denton, although Denton lies on the border with the Eastern Cross Timbers. [8] I-35 and I-35W cross north to south, while US 82 , US 380 , I-30 , I-20 , US 377 , and US 67 cross east to west; US 81 and US 287 also cross southwest to northeast.
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]