Transform boundry, or what's known as shearing. It causes the plates to move past each other causing earthquakes in any areas.
The Nubian/African boundry and the Somalian boundry
A convergent boundry is creating the shiveluch volcano in Russia. The Eurasian plate collides with the Pacific plate
plate boundry has four different parts. # conservative boundary. # constructive boundary. # destructive boundary. # collision boundary.
Transform boundaries do not produce volcanic activity.
Transform boundarys are also called strike-slip faults. The only transform boundry is in California.
transform boundry.
transform boundry
a transform boundary
A transform boundary forms where plates slide past each other horizontally. Most transform boundaries are found near Mid-ocean ridges.
transform boundry as in the san Andreas fault
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.
shearing
The type of boundary that causes shearing is transform boundary.
The San Andreas fault -- the boundary between the Pacific and North American plates
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.
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.