Is the San Andreas Fault were an oceanic plate went under a continental causing a volcanic eruption and earthquake made by Christina Moore
Transform boundary
A transform plate boundary occurs when two plates slide past one another horizontally. This movement can cause earthquakes along the boundary as the plates grind against each other. The San Andreas Fault in California is a well-known example of a transform plate boundary.
In a transform boundary, plates slide horizontally past each other. One of the most famous transform boundaries is the San Andreas Fault that winds through California.
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
The transform boundary is also known as the transform fault. This type of boundary is commonly found in deep ocean floors and are typically involved in movement which aids in relieving tension in the layers of the earth.
When one tectonic plate slides past another, it can create a transform boundary. At this boundary, the plates grind against each other, causing earthquakes. The San Andreas Fault in California is a well-known example of a transform boundary.
The most famous transform boundary is the San Andreas Fault in California, USA. This boundary is well-known for its frequent seismic activity and for being a boundary between the Pacific Plate and the North American Plate.
Transform Boundary.
A transform plate boundary shears horizontally against each other. When one crust moves up, the other one moves down. A transform plate boundary produces the second worst earthquakes with (S) waves (Shear or secondary waves). Every boundary including a transform plate boundary are located on a fault.
It is a right-lateral strike-slip fault
The San Andreas Fault in California is an example of a transform boundary in the United States. The Pacific Plate and the North American Plate slide past each other horizontally at this boundary, causing frequent earthquakes.