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 actually a "Strike-Slip" fault, which means that the movement of the plates is a side-to-side movement past each other. The Pacific plate, relatively speaking, is moving north and the North American plate is moving south. This means that the very western coast of California is sliding north past the rest of California. The San Andreas fault is a strike-slip fault
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 actually a "Strike-Slip" fault, which means that the movement of the plates is a side-to-side movement past each other. The Pacific plate, relatively speaking, is moving north and the North American plate is moving south. This means that the very western coast of California is sliding north past the rest of California. The San Andreas fault is a strike-slip fault
The San Andreas Fault in California.
False
The San Andreas Fault is in California
Dynamic
Dynamic
San Andreas Fault
San Andreas Fault
the San Andreas fault
San Andreas fault.
the san Andreas fault
the san Andreas fault
The San Andreas fault is where it occured.
The San Andreas Fault in California.
False
False
False
False