well i have no idea im asking the same question and they wont tell me the answer -__-
transform boundary
The San Andreas fault is a transform plate boundary.
transform boundary
Convergent plate boundary, divergent plate boundary and strike-slip (transform) plate boundary.
Mt. Fuji is located in Japan. It is near a continental convergent boundary, a continental transform boundary, and an oceanic transform boundary.
A transform fault boundary is a conservative plate boundary. This is what gets rid of lithosphere.
It is a transform plate boundary.
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 is a type of plate boundary where two tectonic plates slide past each other horizontally. This movement can result in earthquakes and the creation of features like strike-slip faults. An example of a transform boundary is the San Andreas Fault in California.
There are 2 tectonics theories namely: divergent boundary and subduction zone. The boundary of the plate tectonics where two plates are placed is called divergent boundary while the subduction zone is a convergent boundary where in one plate is subducted on another.
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.