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Igneous Rock Reading Melting The deeper in the crust you go, the hotter it gets. If you go deep enough into the crust, it is hot enough to melt rock. Rocks that are pushed deep into the earth's crust will melt; this molten (melted) rock is called magma. Because magma is very hot, it expands and fills in any spaces in the rock it can find. Sometimes magma never makes it to the surface because there are not cracks in the crust to allow it to expand upwards. Sometimes the magma does find a crack in the earth's crust and it makes its way all the way to the surface. Magma that reaches the surface creates a volcano. NOTE: When magma comes out of the crust and onto the earth's surface it gets a new name: lava. Lava and magma are the same thing: both are molten rock. But magma is the name for molten rock beneath the earth's surface, and lava is the name for molten rock on the earth's surface. Cooling and Solidifying Whether it is on the earth's surface or underneath, the molten rock will eventually cool down. When it does, the magma or lava turns back into a solid. The new rock that is formed when magma or lava cools is called and i gneous rock. Minerals When the original rock was melted, the minerals that made up the rock broke up into a liquid mush of elements that were no longer structured at minerals (remember, part of being a mineral means it has to be solid). When magma or lava cools down and turns back into a solid, however, new minerals form. That is why igneous rock is considered a brand new rock. The size of mineral crystals is determined partly by the amount of time the crystals have to grow. The slower molten rock cools, the more time it gives the minerals to grow. When magma cools below the earth's surface, the rock that is formed is called an intrusive igneous rock. This magma cools much slower than lava on the earth's surface, so it generally has much larger mineral crystals that are often clearly visible to the naked eye. When magma cools above the earth's surface, the rock that is formed is called an extrusive igneous rock. This lava cools quickly because the surface of the earth is much cooler than deep in the crust. Because the lava cools quickly, there is less time for mineral crystals to grow large, so in general extrusive igneous rocks have smaller crystals that usually can't be seen with the naked eye.