Transform boundarys are also called strike-slip faults. The only transform boundry is in California.
transform boundry.
The three main types of plate boundaries are divergent, convergent, and transform. Divergent boundaries occur where plates move apart, creating new crust. Convergent boundaries occur where plates collide and can result in subduction zones or mountain formation. Transform boundaries occur where plates slide past each other horizontally.
a transform boundary
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.
transform boundry as in the san Andreas fault
Divergent boundary
Transform boundaries are characterized by the sliding of two lithospheric plates past each other horizontally. They are associated with earthquakes due to the friction between the plates as they move. Transform boundaries neither create nor destroy the Earth's lithosphere, but instead allow for lateral movement.
A transform boundary forms where plates slide past each other horizontally. Most transform boundaries are found near Mid-ocean ridges.
At transform boundaries, the plates move horizontal in relation to each other.
earthquake zone or in the boundry of tectonic plates
presure starts to build. when that pressure is released, it causes an earthquake. This only happens on a transform boundry beetween two plates, which is where they slide against each other.
Transform boundry, or what's known as shearing. It causes the plates to move past each other causing earthquakes in any areas.