Its area is estimated at 1,100 square kilometres (420 sq mi), the exposed area covering roughly 40 square kilometres (15 sq mi).[2] Johnson Granite Porphyry is part of the Tuolumne Batholith.[3] Its boundaries are difficult to trace, and are irregular.[1] It is both the youngest, and the most siliceous rock of Tuolumne Intrusive Suite.[4][5]
Geology
The innermost, most felsic part of the Tuolumne Batholith is the Johnson Granite Porphyry.[6] It is a highly irregular, elongated body. Completely surrounding it is the much larger body of Cathedral Peak granite.[1]
^Titus, S.; Clark, R.; Tikoff, S. (September 1, 2005). "Geologic and geophysical investigation of two fine-grained granites, Sierra Nevada Batholith, California: Evidence for structural controls on emplacement and volcanism". Geological Society of America Bulletin. 117 (9): 1256. doi:10.1130/B25689.1. S2CID129298834.