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

Permanent URI for this collectionhttps://hdl.handle.net/2152/46225

As you travel along Texas highways or hike through state or federal parks, do you wonder why there are different rocks in different areas? Or if an area has always looked like it does now? Or why certain mineral resources like oil are produced in certain parts of the state? Geology is the study of the nature and origin of the Earth, including the processes that have created it over long periods of time. Geologists use modern environments and processes to help interpret the Earth’s history as recorded by ancient rocks. Climate has major effects on the formation of many sedimentary rock types; therefore, local and global climatic environments are recorded in the rocks. Understanding the processes and rates of movement of the Earth’s plates allows reconstruction of the relative plate positions at different times in Earth history. Geologic history of Texas is recorded in the rocks that are exposed throughout the state and fill the many subsurface sedimentary basins. These rocks document a changing land surface that began more than a billion years ago. Texas has been the site of explosive volcanoes, strong earthquakes, major mountain ranges, 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 complete the rock cycle. Texas’ abundant and varied mineral resources (oil, natural gas, coal, uranium, metals, groundwater, limestone, salt, gypsum, clays, and soils) are products of these geologic events.

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