The San Andreas Fault is an example of a transform boundary in which plates slide past each other. This type of fault may also be known as a strike slip fault. During this plate motion, lithosphere is neither created nor destroyed. Shear stress causes the undeformed block of rock to experience tearing and smearing.
The San Andreas Fault is a transform plate boundary.
transform boundary
The San Andreas Fault is a continental transform fault. It is around eight hundred and ten miles long and forms the boundary between the Pacific and the North American lithospheric plates. In California this crack in the crust of the earth is visible. As a result of this fault, many earthquakes have occurred in the regions that it passes.
The San Andreas Fault is a continental transform boundary that extends roughly 810 miles (1,300 km) through California, forming the tectonic boundary between the Pacific Plate and the North American Plate. Its motion is right-lateral strike-slip (horizontal).
Large faults such as the San Andreas are transform faults and are found throughout the state but moreso in the central and southern regions. Slip-strike faults exist between the inland mountains and the coast. Minor earthquakes occur almost constantly along these faults.San Andreas.
The San Andreas Fault is a transform plate boundary.
transform boundary
Strike-slip
transform boundary
A strike slip fault
The San Andreas Fault is a continental transform fault. It is around eight hundred and ten miles long and forms the boundary between the Pacific and the North American lithospheric plates. In California this crack in the crust of the earth is visible. As a result of this fault, many earthquakes have occurred in the regions that it passes.
The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific plate are both moving vertically in different directions.
The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific plate are both moving vertically in different directions.
The San Andreas Fault is a continental transform boundary that extends roughly 810 miles (1,300 km) through California, forming the tectonic boundary between the Pacific Plate and the North American Plate. Its motion is right-lateral strike-slip (horizontal).
Large faults such as the San Andreas are transform faults and are found throughout the state but moreso in the central and southern regions. Slip-strike faults exist between the inland mountains and the coast. Minor earthquakes occur almost constantly along these faults.San Andreas.
hpyerbole
The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific plate are both moving vertically in different directions.