The force that produces a strike slip fault is a shearing force.
The Hayward Fault is a Strike-slip Fault.
reverce fault.....
It is a THRUST fault The San Andreas Fault
tsunami
A reverse fault may form when rocks are compressed.
shearing
The type of stress force that produces a strike-slip fault is transform stress. This stress occurs when two tectonic plates slide past each other horizontally, causing displacement along a fault line. Strike-slip faults are often associated with transform plate boundaries, such as the San Andreas Fault in California.
A strike-slip fault
enrique's balls
compression
tensional forces
thrust A+
A strike-slip fault has a shearing force, where the two blocks on either side of the fault move horizontally past each other. This type of fault is characterized by lateral movement along the fault line caused by horizontal forces.
A normal fault produces horst and graben topography. In this type of faulting, the hanging wall moves down relative to the footwall, resulting in block faulting where a horst (uplifted block) is adjacent to a graben (down-dropped block).
Type IIx, Type IIa, and Type I fibers are typically known to produce the greatest contractile force among muscle fibers. Type IIx fibers are fast-twitch fibers that generate high force but fatigue quickly, while Type IIa fibers are also fast-twitch but have more endurance. Type I fibers, on the other hand, are slow-twitch fibers with lower force production but high resistance to fatigue.
The Hayward Fault is a Strike-slip Fault.
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