Titus Canyon
Detailed Description
View of s teeply dipping strata of the late Neoproterozoic and Cambrian Wood Canyon Formation in lower Titus Canyon. The beds of dolomite shown in this image are located a short distance downhill from Leadfield (ghost town) near the entrance of the gorge where Titus Creek crosses the boundary between softer Tertiary-age sedimentary beds into the harder, denser, more ancient rocks.
Sources/Usage
Public Domain.