Earthquakes
Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.
Convergent Boundaries!
mountain ranges
Earthquakes can, and do, occur at divergent, convergent, and transform plate boundaries.
Converging Plate Boundaries
convergent boundaries
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.
What are geologic processes/vents that will occur because of this plate movement?
At a convergent boundary, geologic features that can form include mountain ranges, deep ocean trenches, and volcanic arcs. Subduction zones are also common at convergent boundaries, where one tectonic plate is forced beneath another. These processes can lead to earthquakes, volcanic eruptions, and the formation of new rock formations.
Earthquakes can occur at a transform boundary.
Subduction zones, trenches and volcanic islands: the boundary that is oceanic. Trenches and volcanic islands: an oceanic-continental boundary. Folded mountain ranges: a continental and continental collision.
At convergent plate boundaries, subduction can occur where one plate is forced beneath another, resulting in earthquakes, volcanic activity, and the formation of mountain ranges. Collision can also happen when two plates both resist subduction, leading to intense earthquakes and the uplift of large mountain belts. Additionally, the melting of crustal rocks can lead to the formation of magma and volcanic eruptions.