1. A place where two rocks slip previous each other, moving in the opposite directions. Tsunami"s and also earthquakes might occur.2. Strike-slip error (rocks on either next of the fault slip previous each various other with small up and also downwards movement) and also caused by shearing (Stress that pushes a absent in opposite directions, causes rocks come break, on slide apart or adjust shape.


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1. A boundary where 2 plates collide, come together, or crash into each other. If oceanic, older is much less dense, subduction occurs. If continental 2, mighty mountain ranges will certainly form.2. Compression (stress squeezes rock till it crease or breaks) and reverse-faults (blocks relocate in the opposite direction to typical Fault, one next of a reverse fault lies in ~ an angle over the other side.the rock creating the footwall the a reverse fault slides up and over the footwall)
1. A border where 2 plates move apart, or diverge. Reasons Tsunami"s O, O. MOR forms. A rift valley (a deep valley) forms along the divergent boundary. Floor dropens.2. Stress and anxiety (Stress pressure pulls top top the crust, extending rock so it becomes thinner in the middle) common Fault (the fault is in ~ an angle, one block of absent lies over the error while the other block lies below the fault. he half of the fault the lies listed below is dubbed the footwall, if the fifty percent above is called the hanging wall. As soon as there is movement, the hanging wall surface slips downwards.
1. One area whereby magma indigenous deep in ~ the crust melts with the crust choose a blow torch.2. Magma breaks with the crust, developing volcanoes. The resulting volcanoes produce a string of islands (Island arc)
1. A fine tested concept that explains a wide-range that observations.2. The concept of bowl tectonics describes the formation, movement, and also subduction that Earth"s plates.
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