103 D14. Geoheritage Discipline Session
Monday, 10 October 2022
1:30 PM - 5:30 PM
406
MOUNT BONNELL AS AN URBAN GEOHERITAGE SITE IN AUSTIN, TEXAS
Paper number: 103-12
Program: Technical Sessions
Time: 4:15 PM – 4:30 PM
Authors
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Charles WoodruffJackson School of Geosciences, University of Texas at Austin, Austin, TX
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Linda Mccall Presenting AuthorJackson School of Geosciences, University of Texas at Austin, Austin, TX
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Francine MastrangeloJackson School of Geosciences, University of Texas at Austin, Austin, TX
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Aaron AverettJackson School of Geosciences, University of Texas at Austin, Austin, TX
Abstract
Mount Bonnell occupies the upthrown side of the main fault line within the Balcones Fault Zone in Austin. With a displacement of roughly 200 m, long-term erosion has sculpted the Balcones Escarpment, which extends southwest from Austin through San Antonio and on to the Rio Grande near Del Rio. Although the escarpment is a discontinuous topographic break, it marks the boundary between two grand physiographic provinces of North America: the Great Plains to the west and the Gulf Coastal Plain to the east. This break also extends north to include the buried Ouachita orogenic belt that underlies Temple, Waco, and Dallas–Ft. Worth. The Balcones–Ouachita borderland provides resources of great value to the human economy: prime cropland along the inner reaches of the Coastal Plain; prolific springs near the foot of the escarpment; and rangelands on the upfaulted carbonate rocks where hilly terrain is rapidly being transformed by residential and commercial development. This geo-cultural break marks the boundary of the American West in Texas.
Geological Society of America Abstracts with Programs. Vol. 54, No. 6
doi: 10.1130/abs/2022AM-379534
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