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When tectonic plates slide past each
other, they do not usually slide smoothly. They might get
stuck for a while, and then give a bump and move very
suddenly. We call the area where two plates are
sliding past each other a fault line, and there are often
earthquakes - these are the sudden bumpy movements made by
the plates. We have fault lines going through New
Zealand, and that is why we get a lot of
earthquakes.
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Where the tectonic plates move together, one plate slides under, and the other is forced up. This builds mountain ranges, like our Southern Alps. The rock that is forced deep under the earth gets so hot that it melts, and becomes magma. This magma can rise to the surface in eruptions, making chains of volcanoes. One of these chains is called the Ring of Fire. |
When the two plates diverge, it makes
deep rifts in the earth's surface, and eventually these can
fill with water and become a sea or an ocean. The Red Sea is
an example of this. The ocean is spread apart, and ridges
are formed deep under the sea, where magma flows upward, and
cools into hard rock.