This is known as a transform boundary or a strike-slip fault; the U.S. famous one being the San Andreas Fault.
Convergent boundary.
A subduction boundary occurs where two plates move together, with one plate being forced beneath the other into the mantle. This process can lead to the formation of deep ocean trenches and volcanic arcs.
This is called a convergent boundary, because the two plates are converging, or coming together.
The kind of plate boundary where one lithospheric plate slides under another is a convergent boundary. This process is called subduction.
At a transform plate boundary, plates slide past each other horizontally in opposite directions without creating or destroying lithosphere. This movement is characterized by lateral shearing, where the plates grind against each other, causing earthquakes.
Diverging Plate Boundary
divergent plate boundary- a boundary where two plates move apart from each other. convergent plate boundary- a boundary where two plates move towards each other so that one plate can sink beneath the other. transform plate boundary- a boundary where one plate slips along side another plate.
Shearing occurs at transform plate boundaries, where two tectonic plates slide past each other horizontally. This movement can result in earthquakes due to the friction between the plates. An example of a transform plate boundary is the San Andreas Fault in California.
divergent plate boundary- a boundary where two plates move apart from each other. convergent plate boundary- a boundary where two plates move towards each other so that one plate can sink beneath the other. transform plate boundary- a boundary where one plate slips along side another plate.
Convergent boundary.
Subduction occurs when one tectonic plate moves underneath another plate at a convergent boundary. This typically happens at deep ocean trenches where the denser oceanic plate is forced beneath the less dense continental plate. Subduction is a key process in the cycle of plate tectonics, leading to the formation of volcanic arcs and earthquakes.
Convergent BoundaryA destructive plate boundary with a subduction zone.
Convergent boundary, which in this case would lead to mountain building (as in the Himalayas)
Crust is destroyed at the convergent plate boundary. This is usually between the oceanic and continental plates. This is where subduction of the more dense crust occurs.
Convergent BoundaryA destructive plate boundary with a subduction zone.
Convergent BoundaryA destructive plate boundary with a subduction zone.
Convergent BoundaryA destructive plate boundary with a subduction zone.