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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.

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