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1 Fault-block mountains-Fault-block mountains are formed along faults where some large blocks of rock are forced upwards while others are forced down. 2  The higher area is sometimes called a horst and the lower a graben (see the picture below).
Low-grade metamorphic rock of Cretaceous age in Transverse Ranges Salinian Block Structural block located west of the San Andreas fault zone and east of the Nacimiento fault zone. The Salinian Block granitics are the other main basement type in the Coast Ranges Province San Andreas Fault Northwest-trending, right-lateral strike slip fault that's 750 miles long, extending from Shelter Cove in the north to the east side of the Salton Trough.