• The Texas White House

    Lyndon B Johnson

    National Historical Park Texas

Geologic Formations

Nature and Science

Geologic Map of the LBJ Ranch

L Nordt

Both the LBJ Ranch and Johnson City Districts lie within the Pedernales River valley. The area is located mostly within a relatively rugged topographic basin, with rough terrain and considerable relief, along with relatively flat inner portions within the basin. Elevations range from slightly less than 1,000 to 2,500 feet above mean sea level (MSL).

Geologically, the region is different and distinctive from the rest of Texas. The river valley cuts through a geologic region known as the Llano Uplift, which is bounded on the south and west by the Edwards Plateau and on the east by the central Texas Hill Country. The hills are capped by Cretaceous limestone underlain by sands and shales of the Cretaceous era. The Llano Uplift is a structural high dome of very old igneous and metamorphic Precambrian rocks. To the north, local Precambrian granite heights of the Llano Uplift have been identified as upward protruding "knobs." Because of the differences in limestone/marl weathering, the landscape has a stairstepped or benched appearance.

Did You Know?

Principal Johnson in 1928

Lyndon Johnson's first career was as a teacher and principal of a Mexican-American school in Cotulla, Texas. He later taught debate in Houston. Lyndon B. Johnson National Historical Park