Quail Springs Picnic Area
Detailed Description
Weathered fractures in the White Tank monzogranite (Cretaceous) produced this boulder bridge located in the Quail Springs Picnic Area (Trent, 1997; Trent, 1998).
Sources/Usage
Public Domain.
Weathered fractures in the White Tank monzogranite (Cretaceous) produced this boulder bridge located in the Quail Springs Picnic Area (Trent, 1997; Trent, 1998).
Public Domain.