Texas' vastness (268,596 sq mi) encompasses seven major landform regions, each with unique geology, ecology, and human use.
Eastern & southern Texas. Low, rolling, sandy. Piney Woods (east), Post Oak Savannah, Blackland Prairie. Houston, Corpus Christi, Beaumont.
Central Texas. Limestone hills, caves, springs, clear rivers (Guadalupe, Colorado). Austin, San Antonio, Fredericksburg. Karst aquifer (Edwards Aquifer).
NW Texas. Flat, semi-arid, 3,000–4,500 ft elevation. Cotton, grain, cattle. Amarillo, Lubbock. Caprock Escarpment marks eastern edge.
Deep East Texas. Humid, dense pine-hardwood forest. Timber, oil, gas. Tyler, Longview, Nacogdoches.
Far West Texas. Desert mountains (Guadalupe, Davis, Chisos), Chihuahuan Desert. Big Bend, El Paso. Lowest rainfall, highest peaks (Guadalupe Peak 8,751 ft).
Central TX geological anomaly. Ancient granite (1.1 Ga), dome-shaped. Enchanted Rock, unique minerals. Fredericksburg, Llano.
Northernmost rectangle. High Plains continuation. Vast grasslands, wheat, cattle, wind farms. Palo Duro Canyon (2nd largest US canyon).
These landforms dictate water, agriculture, energy, settlement patterns, and biodiversity—making Texas a continent in a state.