Continental- continental collisions, Continental-oceanic collisions,and Oceanic-oceanic collisions
San Andreas Fault--transform plate boundary. Himalayan Mountain Range--convergent plate boundary. Mid-ocean ridge--divergent plate boundary.
Either: they all collide in some way, or they all affect the structure of the landscape in some way.
There are three types of plate movements that can cause earthquakes. Lateral, convergent, and divergent.
Convergent, Divergent and Transform
i dont know ask your momy trick
San Andreas Fault--transform plate boundary. Himalayan Mountain Range--convergent plate boundary. Mid-ocean ridge--divergent plate boundary.
Either: they all collide in some way, or they all affect the structure of the landscape in some way.
There are three types of plate movements that can cause earthquakes. Lateral, convergent, and divergent.
Convergent, Divergent and Transform
Divergent (away from\apart), Convergent (towards) and Transform (side by side) movements.
throwing, catching, and kicking.
Convergent, divergent, and, although not a plate boundary, they also occur from hotspots.
i dont know ask your momy trick
Convergence, divergence and strike slip.
There are three different types of plate movements that cause earthquakes. The first is Divergent Boundaries (pulling apart), the second is Covergent Boundaries (coming together) and Transform Boundaries.
1. Continent plate/sea floor plate subduction 2. sea floor plate/sea floor plate subduction 3. strike/slip movement
There are three major plate movements, whether these occur on the continents or under the sea, convergent, where two plates collide together and one sinks under the other, although sometimes with continental plates if two continental plates collide then they are both very dense so they both press up against each other and form mountains, there are conservative plate margins, where the plates slip past each other, catching against each other causing earthquakes, and finally there are divergent plate margins where the plates are moving away from each other, these cause upsurges of magma in between and new land/sea bed is formed, these types of plate margins usually only occur under the sea, this is how Iceland was formed, but not the Hawaiian islands