the san Andreas fault
the san Andreas fault
The San Andreas fault is a transform plate boundary.
A transform fault boundary is a type of tectonic plate boundary characterized by horizontal sliding of plates past each other. This movement can cause earthquakes as the plates grind against each other. An example of a transform fault boundary is the San Andreas Fault in California.
A transform fault boundary is a conservative plate boundary. This is what gets rid of lithosphere.
Transform Boundary/Strike Slip
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.
Transform boundary
YES. A Strike-slip fault is usually a transform boundary.
A strike-slip or transform fault.
It is a right-lateral strike-slip fault
In plate tectonics, a sliding boundary is considered a transform fault where the two merging plates slide past each other in the opposite direction. A great example of a transform fault would be in California along the San Andreas fault line.
A transform boundary.