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Produced by and for Hot Science - Cool Talks by the Environmental Science Institute. We request that the use of these materials include an acknowledgement of the presenter and Hot Science - Cool Talks by the Environmental Science Institute at UT Austin. We hope you find these materials educational and enjoyable. Dr. Richard Kyle March 24, 2000 Geologic History of Texas: The Making of Texas Over 1.5 Billion Years # 4

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Page 1: Geologic History of Texas: The ... - Environmental Science · Produced by and for Hot Science - Cool Talks by the Environmental Science Institute. We request that the use of these

Produced by and for Hot Science - Cool Talks by the Environmental Science Institute. We request that

the use of these materials include an acknowledgement of the presenter and Hot Science - Cool Talks

by the Environmental Science Institute at UT Austin. We hope you find these materials educational

and enjoyable.

Dr. Richard Kyle

March 24, 2000

Geologic History of Texas:

The Making of Texas

Over 1.5 Billion Years

# 4

Page 2: Geologic History of Texas: The ... - Environmental Science · Produced by and for Hot Science - Cool Talks by the Environmental Science Institute. We request that the use of these

Geologic History of Texas: The Making of Texas over 1.5 Billion Years

J. Richard Kyle

Department of Geological Sciences

The University of Texas at Austin

Geologic History of Texas:The Making of Texas over 1.5 Billion Years

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I am grateful to many individuals who have contributed to

my understanding of the geologic history of Texas,

particularly present and former colleagues at The

University of Texas at Austin in the Department of

Geological Sciences, the Bureau of Economic Geology,

the Institute for Geophysics, and the Texas Memorial

Museum. These individuals and institutions have

contributed many of the illustrative materials contained

in this CD-ROM.

The presentation contained herein was made by J. Richard Kyle and is intended for educational purposes only.

Any use of this work, partial or complete, must cite J. Richard Kyle and this Outreach Lecture Series Volume 4.

No portion of this product may be reproduced or distributed in any form.

March 2000

Acknowledgments

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3. Texas Today

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Plate Tectonics

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Texas Geography

Austin

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Texas Geology

Austin

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7. Geologic time scale – major Texas events

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Geologic Time Principles

8. Geologic Time Principles

Several geologic principles are fundamental to using the rock record to

interpret processes.

Original Horizontality: Most rocks that form at the Earth's surface are

deposited in essentially horizontal layers. Therefore, when layered

rocks are not horizontal, they probably have been affected by post-

depositional processes such as a tectonic event.

Superposition: When layered rocks are formed, they are deposited in

an orderly sequence with the oldest being at the base of the sequence

and the strata becoming progressively younger upward. Therefore

when a sequence of rocks differs from the predicted sequence, or layers

are missing, then an explanation for the cause of these differences is

required.

Cross-cutting Relationships: Features such as faults or igneous

intrusions generally cross-cut or affect all rocks that were present locally

at the time of the faulting or intrusive event.

Uniformitarianism: Present Earth processes are useful in

understanding the types and rates of processes that have affected the

Earth during past periods of geologic history.

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Central Texas roadcut

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Llano stratigraphic column

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Llano rocks

Geologic Time

D

B

A

C

Protero-

zoic

Mesozoic

Paleozoic

Time Interpretation Based on Llano Stratigraphic Column

0 Ma

200

400

600

800

1000

1200

1400

A

B

C

DErosion

Erosion

Erosion

Erosion

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Central Texas geologic map

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Deformed metamorphic rocks cut by granite dike

Intrusive dike crosscutting

folded metamorphic rocks.

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Enchanted Rock

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Granite slabs

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Tectonic Model for the Precambrian History of the Llano Region

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Himalayas

India

Tibet Plateau

Himalayas

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Late Proterozoic Position of Texas

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Precambrian – Paleozoic time chart

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Complex topography on Enchanted Rock

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Great Barrier Reef, eastern Australia

Bird

Tree Covered Island

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PLATES Lower Paleozoic reconstruction

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Lower Paleozoic life panorama

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Marathon map

Marathon

Uplift

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Marathon exposures

Dip

direction

Flat-lying

Cretaceous

Limestones

Haymond Formation

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Caballos Novaculite aerial exposures

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Marathon tectonic evolution

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New Guinea

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PLATES Late Paleozoic

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Ouachita Orogeny and Formation of the Permian Basin

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Delaware Basin

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Delaware Basin Section

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El Capitan Reef

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Permian Basin filling by Evaporites

OPEN

OCEAN

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Evaporation

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Potash-bearing salt at Carlsbad

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Mesozoic – Cenozoic time chart

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PLATES Early Mesozoic

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Rifting and Formation of the Gulf of Mexico Basin

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Death Valley, California

Volcano

Salt Lake

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Gulf of Mexico – Pacific Connection

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Distribution of northern Gulf of Mexico Salt Diapirs

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East Texas Basin Salt Structures

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Salt in a Salt Dome Mine

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Distribution of Cretaceous Limestones

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Cretaceous Limestone Exposures along the Colorado River in Austin

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Cretaceous Volcanoes in Central and South Texas

Uvalde area

Pilot Knob

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Hawaii volcano

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Cretaceous Interior Seaway

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West Texas Cretaceous Stratigraphy

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Clean up

Formation of the Rocky Mountains

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Mesozoic Life – Dinosaurs

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PLATES End Cretaceous Asteroid Impact

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Subduction off the Western Coast of Southern North America

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Mid-Tertiary Volcanic Field

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Explosive Volcanic Eruption

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Bofecillos Mountains ignimbrites

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West Texas caldera field

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Laccolith Formation

Corazones Peaks

(laccoliths)

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Solitario

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Gulf Coast sedimentary sequence

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Louisiana Bayou

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Tertiary Lignite Deposits in East Texas

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Gulf of Mexico Shoreline since the Cretaceous

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Ogallala Formation

OGALLALA

FORMATION

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Pecos River Headward Erosion

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Rifting in West Texas and New Mexico

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Salt Basin

Guadalupe

Peak

(8,749 feet)

El Capitan

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Cave Decoration at Carlsbad

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Late Cenozoic Life

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Ice Ages

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Barrier island development

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Texas Coastal Bend

Gulf of Mexico

Corpus Christi Bay

Brazos River

Delta

Barrier

Island

Mississippi

River Delta

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Padre Island

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Conclusion:

The geologic history of Texas is recorded in rocks that are

exposed throughout the state and fill sedimentary basins.

These rocks document more than a billion years of change.

Those changes include the building and erosion of major

mountain ranges, explosive volcanoes, strong earthquakes,

vast deserts, evaporating salt basins, tropical forests, river

and delta systems, tropical seas and barrier reefs, and

beaches and barrier islands.

Erosion of highlands filled subsiding sedimentary basins and

adjacent continental margins. Colliding plates deformed,

metamorphosed, and uplifted these materials to continue the

rock cycle.

Texas' abundant and varied mineral resources are products

of these geologic events.

Conclusion

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Professor Richard Kyle

Richard Kyle is the Third C. E. Yager Professor of Geology at The

University of Texas at Austin. He received a Ph. D. from the University of

Western Ontario and worked as a minerals exploration geologist for

several companies prior to joining the UT faculty in 1978. Kyle is the

author of more than 75 publications, including writing or editing six

books. His research contributions have been recognized by awards from

regional and national professional societies. Professor Kyle is the Editor

of Ore Geology Reviews, an international economic geology journal. His

teaching responsibilities and research interests include Texas geology, ore

deposits geology and geochemistry, minerals exploration, industrial

minerals, and multimedia approaches to geoscience education. He has

received departmental and college awards for teaching, program

development, and student advising. Since1988, Kyle has taught a non-

majors course on the Geology and Mineral Resources of Texas.