Tectonic plates are pieces of earths crust uppermost mantle, together refer to as the lithosphere
Tectonic plates are 100km thick and move at 10cm per year
Oceanic crust - also called sima from silicon and magnesium.
Earthquakes and volcanoes are caused by the movement of tectonic plates.
Plate margin is the boundary between two tectonic plates.
Ridge push - at mid-ocean ridges, the oceanic lithosphere is higher than it is where it sinks onto the asthenosphere. Because of the ridge push, the oceanic lithosphere slides downhill under the force of gravity.
Convection - hot rock from deep within the earth rises but cooler rock near the surface sinks. Convection causes, the oceanic lithosphere to move sideways and away from the mid-ocean ridge
Slab pull - because oceanic lithosphere is denser than the asthenosphere, the edge of the tectonic plate that contains oceanic lithosphere sinks and pulls the rest of the tectonic plates with a process of slab pull
Shield volcanoes
gently sloping sides
Formed by frequent, gentle eruptions of thin, runny lava
4100+ metres in height
Usually found at constructive boundaries or over hotspots
Nice to live near
Rift valley - a magma chamber below land fills with upwelling magma. This causes pressure on the land above. The pressure releases and drops, causing the land to stretch and drop, the land will collapse once its elasticity has strained. This creates a landform: a rift valley.
Iceland -
400km magmasuperploom serves it
Volcanoes are vicious
Sits on a constructive boundary
Ends up with super explosive volcanoes
subduction - a process that takes place at a destructive boundaries, where one plate moves under another, due to being denser, into the asthenosphere (lower mantle)
Destructive collision
earthquake busy
When two continental plates meet at a destructive boundary, the continents themselves collide
Usually, there has been an earlier phase of subduction of intervening oceanic lithosphere that has resulted in the closure of an ocean
The best known and most spectacular example is the collision between India and Asia, which began 50 million years ago, following the closure of an intervening ocean and produced the Himalayas and Tibetan Plateau
destructive subduction -> 2 plates collide and one is forced under the other