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There are so many colors that you have to choose from when you are looking at granite countertop. You want to be sure that you choose a color that is going to go with the rest of your room, and you also want to make sure that you know all about granite counter top-b as well before you buy your countertops.

Granite is currently known only on Earth where it forms a major part of continental crust. It occurs as a relatively small stock-like mass and as large batholiths often associated with mountain ranges. Although they may appear uniform, batholiths are in fact structures with complex compositions. Batholiths are composed of multiple masses of magma that traveled toward the surface from a zone of partial melting at the very base of the Earth's crust. Small dikes of granitic composition called aplites are associated with granite margins. In some locations very coarse-grained pegmatite masses occur with granite.

A dike is an intrusion into a cross-cutting fissure. This means that a dike cuts across other pre-existing layers of rock. A dike is always younger than the rocks that contain it. Dikes are usually in a high angle to near vertical in orientation. Subsequent tectonic deformation can rotate the sequence of strata through which the dike lies so that the it later becomes horizontal. Near horizontal intrusions along bedding planes between strata are called intrusive sills. Granite has been intruded into the crust, outer layer, of the Earth during all of its geologic periods. Granite is widely distributed throughout the continental crust of the Earth and is the most abundant basement rock that underlies the sedimentary covering of the continents. Granite is ancient and aesthetically pleasing when used as a granite counter top.

Granite is an igneous rock. Igneous rocks are formed when molten rock cools and solidifies. This can happen with or without crystallization. This can also happen either below the surface as intrusive rocks or on the surface as extrusive rocks....

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