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Choke Canyon Reservoir provides drinking water for the city of Corpus Christi. The reservoir also provides good fishing opportunities, especially for largemouth bass and catfish . Choke Canyon State Park, located in two places on the south shore of the lake, provides access to the lake and a number of other recreational activities.
The Bordas Escarpment transects this ecoregion, running from near the southern limit northwest to the vicinity of Rio Grande City, Texas, arching back northeast to the vicinity of Choke Canyon Reservoir in Texas. The region east of the Bordas Escarpment is flat with deep, sandy soils, of which vast areas both north and south of the border have ...
South Bay is a bay in the Laguna Madre in Texas separated from the Gulf of Mexico by Brazos Island. It is the southernmost bay in Texas, about 1 mi (1.6 km) north of the Texas-Mexico Border . [ 4 ]
Camino Bajo, TX 337, Flat Rock Cir, Ranch Road 1120, River Place Road, Ranch Road 1120, Texas Hill Country Trail, Country Road 350, Country Road 348, Comanche Creek Road, County Road 348, TX 127, unnamed road, County Road 2690, County Road 101, US 90, Garner Field Road, Ranch Road 187, unnamed road, US 57, W FM 140, County Road 1581, County ...
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It begins paralleling US 281 to the east before the two intersect at exit 72 and have a concurrency north of Three Rivers near Choke Canyon Reservoir. Alternate US 281 (Alt. US 281) splits off from I-37 near Sunniland at exit 76 and parallels I-37 before rejoining north of Campbellton at exit 92 southbound.
Padre Island is the longest undeveloped barrier island in the world. The national seashore is 70 miles (110 km) long with 65.5 miles (105.4 km) of Gulf beach. PAIS hosts a variety of pristine beach, dune, and tidal flat environments, [2] including the Laguna Madre on its west coast, a famous spot for windsurfing.
Galveston Island is a barrier island between Galveston Bay and the Gulf of Mexico. The island began to form around 5,000 years ago. The island began to form around 5,000 years ago. It took another 3,000 years for the core to become high enough to withstand typical storm surges. [ 5 ]