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Conservative plate boundary A conservative plate boundary, sometimes called a transform plate margin, occurs where plates slide past each other in opposite directions, or in the same direction but at different speeds.

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Conservative plate boundary A conservative plate boundary, sometimes called a transform plate margin, occurs where plates slide past each other in opposite directions, or in the same direction but at different speeds.

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A constructive plate boundary, sometimes called a divergent platemargin, occurs when plates move apart. Volcanoes are formed as magma fills up to fill the gaps and eventually crust is formed.

An example of a constructive plate boundary is the mid-Atlantic bridge.

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1 The plates move very slowly has magma  rises from the mantle.
2 One of these plates may become so large that the volcano erupts.
3 4 Asian plate and the euopian plate

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1. The plates move away from each other causing magma to to rise from the mantle creating crust.
2.

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1.
The plates move away from each other and sometimes the plates collide and this can make a earth quake and this can cause a chain reaction which can cause a tsunami  to happen .
2.
The plates can cause volcano's to erupt but this doesn't happen very often but one thing that does happen quite often is earth quakes these are also caused by the plates.
3.4.the two plates are oceanic and continental.

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These plates move apart from each other causing magma to rise and fill the gap creating a new area of crust. if on land then these can cause volcanoes by the magma creating a risen crust. Some examples include:
Nazca Plate
North American Plate
South American Plate
African Plate
Pacific Plate

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1. The plates move apart really slowly  they move apart due to convection currents inside the earth.
2.They cause earthquakes and may cause volcanoes to erupt but it doesn't happen as much as earthquakes.