Flood process
The gorge makes erosion visible at landscape scale: water removed soil and rock, reorganizing the channel in days.
Geology field guide · Canyon Lake
A flood-carved classroom exposing Cretaceous limestone, fossils, dinosaur tracks, faults, fractures, springs, and the workings of the Trinity Aquifer.
Hero image is an original decorative interpretation, not a documentary photograph.
Why this place matters
More than 34 inches of rain fell in the upper Guadalupe watershed during one week in 2002. Water overtopped the Canyon Lake spillway and cut a gorge that reveals ancient seafloor limestone and the plumbing of a Hill Country aquifer.
The gorge makes erosion visible at landscape scale: water removed soil and rock, reorganizing the channel in days.
Limestone layers, sea urchin fossils, ocean ripples, and dinosaur tracks preserve evidence from roughly 110 million years ago.
Faults, fractures, seeps, springs, and permeable rock show how the Trinity Aquifer stores and moves water.
Field notes
Trace bedding planes and changes in texture or resistance.
Notice how cracks steer water, roots, weathering, and erosion.
Observe in place; never remove or damage geological evidence.
Look for where groundwater emerges and supports a different microhabitat.
Source ledger
Official source checked September 10, 2026.