Approximate location — plotted from published sources, not a site visit, and not a guarantee of access.
A glowing white dome of Oligocene Tunnel Spring Tuff in the Wah Wah Mountains—an inverted volcanic ash-flow valley filled with crystal-rich rhyolite tuff, fretted with giant tafoni honeycomb weathering. Utah Geological Survey GeoSights highlights the double-terminated quartz crystals and Basin-and-Range fault history that left this resistant peak standing alone.