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Vasquez Rocks

Geological Notes

Photo showing portion of geologic formation
click the photo to continue . . .

The Vasquez Rocks are formations sculpted by 8 to 15 million years of earthquake activity along the Elkhorn fault, an offshoot of the San Andreas Fault. Compressed, folded and tilted as much as 50 degrees, and up to nearly 150 feet high, erosion gradually stripped away soil from around the rocks leaving these ancient and spectacular creations. Course-grained yellowish-gray sandstone beds several feet thick make up these strange jutting and sweeping formations. Shale, basalt, and reddish-brown conglomerate can be found layered between the sandstone slabs.


About Vasquez Rocks
Geological Notes
Historical Notes
Origin of the Name
Vegetation and Wildlife







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Disclaimer: Some portions of this project were developed with assistance from AI tools to help reconstruct historical contexts and fill informational gaps. All materials have been reviewed and fact-checked to ensure accuracy and reliability, though complete precision cannot be guaranteed. The aim is to provide dependable starting points and distinctive perspectives for further study, exploration, and research.

These materials are historical in nature and intended for educational use only; they are not designed as travel guides or planning resources.
Copyright - Walter Feller. 1995-2025. All rights reserved.