Plate margins and collision zones
Destructive plate margins
At a destructive plate marginWhen two tectonic plates move towards one another. The oceanic crust is forced to sink back into the mantle, whilst the continental crust rises above. Volcanoes and earthquakes are found here., the plates move towards one another. This usually involves an oceanic plate and a continental plate.
The collision process is known as subductionWhen one crustal plate is forced beneath the other.. The oceanic plate is denser (heavier) than the continental plate. As the plates move towards each other, the oceanic plate is forced beneath the continental plate. When the plate sinks into the mantle it melts to form magma. The magma escapes under pressure through cracks in the rock and rises up through a volcano. The volcanic eruptions can be violent, with lots of steam, gas and ash.
Subduction can cause volcanic activity and/or earthquakes. Many of these margins are found around the Pacific plate where it subducts under the Eurasian plate near Japan.
Constructive plate margins
At a constructive plate marginAn area where two tectonic plates are moving away from one another. the plates move apart from each other.
When the plates part the magma rises up to make (construct) new crust in the form of either a shield volcano or a fissure volcano. The movement of the plates over the mantle can also cause earthquakes.
Conservative plate margins
At a conservative plate margin the plates are moving past each other or move side by side at different speeds, like cars on a road.
As the plates move, friction occurs and they become stuck. The plates are still trying to move so pressures and stresses build up in the crust. When the pressure is released suddenly, waves of energy move through the crust, causing an earthquake.
The earthquakes at a conservative plate margin can be very destructive as the focus is close to the Earth's surface. There are no volcanoes at a conservative plate margin.
Collision zones
Collision zones form when two continental plates move towards each other and collide. The land between the plates is forced upwards to form fold mountains, eg The Alps and Himalayas.