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Shaded relief map of the Llano Estacado. Texas contains a wide variety of geologic settings. The state's stratigraphy has been largely influenced by marine transgressive-regressive cycles during the Phanerozoic, with a lesser but still significant contribution from late Cenozoic tectonic activity, as well as the remnants of a Paleozoic mountain range.
An enlargeable map of the 254 counties of the State of Texas. The following is a list of Texas county seat name etymologies, taken from the Handbook of Texas. A separate list of Texas county name etymologies, covering Texas counties instead of its county seats, is also available.
The Edwards Plateau is a geographic region forming the crossroads of Central, South and West Texas, United States.It is named in honor of Haden Edwards. [2] It is bounded by the Balcones Fault to the south and east; the Llano Uplift and the Llano Estacado to the north; and the Pecos River and Chihuahuan Desert to the west. [3]
Location of Limestone County in Texas. This is a list of the National Register of Historic Places listings in Limestone County, Texas. This is intended to be a complete list of properties listed on the National Register of Historic Places in Limestone County, Texas. There are four properties listed on the National Register in the county.
This article contains a list of fossil-bearing stratigraphic units in the state of Texas, U.S. Sites. Group or Formation ... Bone Spring Limestone: Permian: Boquillas ...
During a 1975 expedition of the Cave Without a Name, cavers mapped out over 2.7 mi (4.3 km) of caverns, making it the seventh-longest cave in Texas. Due to the great natural acoustics created by three large solution domes on the ceiling of the Throne Room, the cave is host to 12 concerts yearly with a maximum attendance of 200 people.
Designated a Recorded Texas Historic Landmark in 1985. [18] from State of Texas states the school was begun in 1884 on Doss-Spring Creek Road. 1894 land for current site was donated by Tom Nixon, and a small frame structure was built. In 1905, a limestone schoolhouse was built, and in 1927 the present building was added.
Buda Limestone stratigraphic column in Texas. The Buda Limestone is a geological formation in the High Plains and Trans-Pecos regions of West Texas [1] and in southern New Mexico, [2] whose strata date back to the Late Cretaceous. Pterosaur remains are among the fossils that have been recovered from the formation. [3]