Gulf Coastal Plains
Texas’ Gulf Coastal Plains are the western extension of the coastal plain extending from the Atlantic Ocean to beyond the Rio Grande. Its characteristic rolling to hilly surface covered with a heavy growth of pine and hardwoods extends into East Texas. In the increasingly arid west, however, its forests become secondary in nature, consisting largely of post oaks and, farther west, prairies and brushlands.
The interior limit of the Gulf Coastal Plains in Texas is the line of the Balcones Fault and Escarpment. This geologic fault or shearing of underground strata extends eastward from a point on the Rio Grande near Del Rio. It extends to the northwestern part of Bexar County, where it turns northeastward and extends through Comal, Hays, and Travis counties, intersecting the Colorado River immediately north of Austin. The fault line is a single, definite geologic feature, accompanied by a line of southward- and eastward-facing hills.
The resemblance of the hills to balconies when viewed from the plain below accounts for the Spanish name for this area: balcones.
The Neolithic Revolution was a period in human history where humans began to transition out of a hunting-gathering lifestyle in favor of agricultural production and animal domestication. Due to the long-term nature of agricultural production and domestication, this revolution also led to the settlement of some of the earliest towns in human history.
Jobs would relate most to foreign policy we outsource it so much..
It granted land to individual families, but reduced the land available to tribes.
