Strike-Slip Faulting
transform boundary
volcanic erupation
frequent earthquakes.
Frequent Earthquakes, -k12
The San Andreas fault is a transform plate boundary.
transform boundary
Convergent plate boundary, divergent plate boundary and strike-slip (transform) plate boundary.
It is a transform plate boundary.
A transform fault boundary is a conservative plate boundary. This is what gets rid of lithosphere.
Mt. Fuji is located in Japan. It is near a continental convergent boundary, a continental transform boundary, and an oceanic transform boundary.
A transform plate boundary forms where two plates slide past one another horizontally. This movement can cause earthquakes due to the friction and pressure buildup along the boundary. An example of this type of boundary is the San Andreas Fault in California.
An example of a divergent plate boundary is the Mid-Atlantic Ridge, where the Eurasian Plate and North American Plate are moving apart. An example of a transform plate boundary is the San Andreas Fault in California, where the Pacific Plate and North American Plate are sliding past each other horizontally.