Crystallization is seen in which example of igneous rocks
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Igneous rocks with this texture usually occur from the rapid crystallization of lava. The extrusive rocks cool very quickly, therefore their minerals form fine crystals which cannot be seen and distinguished by the naked eye. Andesite, basalt and rhyolite possess this type of texture.
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Examples of intrusive igneous rocks are diorite, gabbro, granite, pegmatite, and peridotite. Extrusive igneous rocks erupt onto the surface, where they cool quickly to form small crystals. Some cool so quickly that they form an amorphous glass.
Examples of intrusive igneous rocks are diorite, gabbro, granite, pegmatite, and peridotite. Extrusive igneous rocks erupt onto the surface, where they cool quickly to form small crystals. Some cool so quickly that they form an amorphous glass.
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