All of the tectonic plates have different types of plate boundaries, most having all three types of plate boundaries. Convergent, where the plate is subducting under another plate, divergent, where the plate is pulling away from another plate, and transform boundaries where the plates are sliding past each other.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
Basically subuctive (one side goes under the other) and sliding.
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.
Volcanoes typically occur at two different types of plate boundaries. These two plate boundaries are: the diverging plate boundary where plates separate, and the converging plate boundaries where one plate is beneath another one at subduction zones.
a) Divergent Plate Boundaries: Divergent plate boundaries are locations where plates are moving away from one another. This occurs above rising convection currents. b) Convergent Plate Boundaries: Convergent plate boundaries are locations where lithospheric plates are moving towards one another. The plate collisions that occur in these areas can produce earthquakes, volcanic activity and crustal deformation. c) Transform Boundary: Transform Plate Boundaries are locations where two plates slide past one another. The fracture zone that forms a transform plate boundary is known as a transform fault. Most transform faults are found in the ocean basin and connect offsets in the mid-ocean ridges.
Divergent, since when the plates split, magma reaches the surface. Convergent, since it is where volcanoes are typically formed. Transform, since trough any crack magma can come out too.
the correct answer is: For example, as rocks on one side of a transform plate boundary grind and push against the rocks on the other plate, mountain, such as the transverse ranges, can form.
There are 3 primary types of Tectonic Plate boundaries: Divergent boundaries; Covergent boundaries; and Transform boundaries. As the giant plates move, diverging [pulling apart] or converging [coming together] along their borders, tremendous energies are unleashed resulting in tremors that transform Earth's surface. While all the plates appear to be moving at different relative speeds and independently of each other, the whole jigsaw puzzle of plates is interconnected.
The landform that develops at plate boundaries where one oceanic plate descends beneath another is known as a volcanic islands arc.
Subduction (where one plate is forced beneath another less dense plate - may occur at oceanic-oceanic and oceanic-continental boundaries), obduction (where oceanic plate is forced over a continental plate) and orogenesis where two continental plates collide and mountains are formed (e.g. the Himalayas).
There are three main types: Convergent boundaries (where two plates are being pushed together) Divergent boundaries (where two plates are being pulled apart) Transform boundaries (where two plates are sliding past each other).