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How the Earth's crust is split into large sections called tectonic plates is described. Their movement and effects at plate boundaries are explained e.g. earthquakes, volcanoes, mountain building, ocean ridges/trenches, subduction (part of the rock cycle).
Also known as passive plate boundaries. 1  The main effects of a conservative plate boundary are earthquakes, which can be fairly violent and frequent. 2  Two plates slide past each other, without creating or destroying any land. The main effects of a conservative plate boundary are earthquakes, which can be fairly violent and frequent. 2  Two plates slide past each other, without creating or destroying any land. 3  As they move past each other they often get stuck, building up great pressure until finally they jolt past each other.