ILLUSTRATED FLORA OF EAST TEXAS - Brit - Botanical Research ...
ILLUSTRATED FLORA OF EAST TEXAS - Brit - Botanical Research ...
ILLUSTRATED FLORA OF EAST TEXAS - Brit - Botanical Research ...
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42 INTRODUCTION/GENERAL GEOLOGY <strong>OF</strong> <strong>EAST</strong> <strong>TEXAS</strong><br />
Texas. In fact, if one were to travel from the modern day Texas Gulf Coast west across much<br />
of the state, it would be a trip crossing older and older sediments deposited during the past<br />
145 million years. Further west, to the west of the Cross Timbers and Prairies, lies the vast<br />
area known as the Rolling Plains, underlain by the famous and even older Permian Red<br />
Beds. This region, at least in part, is sometimes referred to as the Red Plains because of the<br />
obviously red color of iron oxides in the Permian strata. The western edge of much of the<br />
southern part of East Texas is marked by the Balcones Escarpment, a striking feature of the<br />
Texas landscape. According to Spearing (1991), “The Spanish explorer, Bernardo de<br />
Miranda, in 1756 named the escarpment ‘Los Balcones’, meaning ‘balconies’, which<br />
describes quite well the stair-step, balcony-like topography rising above the plains.” The<br />
displacement occurred ca. 10 million years ago along the zone of weakness associated with<br />
the ancient Ouachita mountains (Fig. 21). The escarpment is most obvious from Waco south<br />
through Austin and San Antonio. As one moves from east to west across this escarpment,<br />
higher and higher benches or “steps” are encountered until the older Lower Cretaceous<br />
rocks of the Edwards Plateau are reached—about 2,000 feet above sea level (Figs. 22, 23).<br />
In one isolated region to the southwest of East Texas is a rugged area, variously known as<br />
the Burnet Country, Central Mineral Region, or Llano Basin, which includes granite and<br />
other very old Precambrian and Paleozoic outcrops. Here, ancient material has been exposed<br />
by the extensive erosion of overlying Cretaceous sediments. This is one of relatively few<br />
places in the state where materials of igneous origin can be easily viewed (e.g., Enchanted<br />
Rock) (Spearing 1991).<br />
1<br />
2<br />
3<br />
4<br />
5<br />
6<br />
7<br />
8<br />
9<br />
10<br />
11<br />
12<br />
GUADALUPE MTS.<br />
DELAWARE AND APACHE MTS.<br />
DAVIS MTS.<br />
MARATHON BASIN<br />
SANTIAGO,CHALK, AND CHRISTMAS MTS.<br />
CHISOS MTS.<br />
CHINATI MTS. AND SIERRA VIEJA<br />
QUITMAN AND FINLAY MTS.<br />
HUECO MTS.<br />
FRANKLIN MTS.<br />
HUECO BASIN<br />
GLASS MTS.<br />
FIG.23/PHYSIOGRAPHIC REGIONS <strong>OF</strong> <strong>TEXAS</strong> (FROM HISTORICAL ATLAS <strong>OF</strong> <strong>TEXAS</strong>,<br />
BY A. RAY STEPHENS AND WILLIAM M. HOLMES.COPYRIGHT ©1989,<br />
BY THE UNIVERSITY <strong>OF</strong> OKLAHOMA PRESS, NORMAN.REPRINT BY PERMISSION <strong>OF</strong> THE<br />
PUBLISHER.ALL RIGHTS RESERVED.