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The Gulf of Mexico and Coastal Plain. The Gulf Coastal Plain extends around the Gulf of Mexico in the Southern United States and eastern Mexico.. This coastal plain reaches from the Florida Panhandle, southwest Georgia, the southern two-thirds of Alabama, over most of Mississippi, western Tennessee and Kentucky, extreme southern Illinois, the Missouri Bootheel, eastern and southern Arkansas ...
Texas Gulf Coast is an intertidal zone which borders the coastal region of South Texas, Southeast Texas, and the Texas Coastal Bend.The Texas coastal geography boundaries the Gulf of Mexico encompassing a geographical distance relative bearing at 367 miles (591 km) of coastline according to CRS [1] and 3,359 miles (5,406 km) of shoreline according to NOAA.
The geography of Texas is diverse and large. Occupying about 7% of the total water and land area of the U.S., [1] it is the second largest state after Alaska, and is the southernmost part of the Great Plains, which end in the south against the folded Sierra Madre Oriental of Mexico.
Ringing the Gulf Coast is the Gulf Coastal Plain, which reaches from Southern Texas to the western Florida panhandle, while the western portions of the Gulf Coast are made up of many barrier islands and peninsulas, including the 130-mile (210 km) Padre Island along the Texas coast.
Ria – Coastal inlet formed by the partial submergence of an unglaciated river valley; River delta – Silt deposition landform at the mouth of a river; Salt marsh – Coastal ecosystem between land and open saltwater that is regularly flooded; Sea cave – Cave formed by the wave action of the sea and located along present or former coastlines
Landforms of Texas by county (224 C) Wetlands of Texas (1 C, 23 P) * Lists of landforms of Texas (8 P) B. ... Gulf Coastal Plain; M. Mescalero Ridge; T. Texas Gulf Coast
Contains the only significant segment of gulf coastal prairie. Bayside Resaca Area: 1980: Cameron: federal/US Fish & Wildlife Service Located in Laguna Atascosa National Wildlife Refuge, contains an excellent example of a resaca.
The Western Interior Seaway had withdrawn by the beginning of the Cenozoic, the era that put the finishing touch on Texas's current geology. The modern coastal plain formed during this time; it comprises increasingly thick sediments (perhaps 15 km deep at the coastline) deposited southeastward into the downwarping Gulf of Mexico. [10]