Granite

Granite

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Super White Granite Countertops

Super white granite is actually classified as quartzite. Most stones are actually not granite. They are grouped together as granite so that the average consumer does not have to be a geologist to understand the qualities of the material they are purchasing. Quartzite is actually harder than granite but as with most materials you will see a mix of various minerals that will give you that unique look of the material. Super white quartzite is a mix of quartzite and limestone which gives it that white grey look but a more durable surface than marble.

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About Granite

Granite is a common type of felsic intrusive igneous rock that is granular and phaneritic in texture. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy. The word “granite” comes from the Latin granum, a grain, in reference to the coarse-grained structure of such a holocrystalline rock. By definition, granite is an igneous rock with at least 20% quartz and up to 65% alkali feldspar by volume.

The term “granitic” means granite-like and is applied to granite and a group of intrusive igneous rocks with similar textures and slight variations on composition and origin. These rocks mainly consist of feldspar,quartz, mica, and amphibole minerals, which form interlocking, somewhat equigranular matrix of feldspar and quartz with scattered darker biotite mica and amphibole (often hornblende) peppering the lighter color minerals. Occasionally some individual crystals (phenocrysts) are larger than the groundmass, in which case the texture is known as porphyritic. A granitic rock with a porphyritic texture is known as a graniteporphyry. Granitoid is a general, descriptive field term for lighter-colored, coarse-grained igneous rocks. Petrographic examination is required for identification of specific types of granitoids.[1]

Granite differs from granodiorite in that at least 35% of the feldspar in granite is alkali feldspar as opposed to plagioclase; it is the potassium feldspar that gives many granites a distinctive pink color. The extrusiveigneous rock equivalent of granite is rhyolite.

Granite is nearly always massive (lacking any internal structures), hard and tough, and therefore it has gained widespread use throughout human history, and more recently as a construction stone. The averagedensity of granite is between 2.65[2] and 2.75 g/cm3, its compressive strength usually lies above 200 MPa, and its viscosity near STP is 3–6 • 1019 Pa·s.[3]

Melting temperature of dry granite at ambient pressure is or 1215–1260 °C (2219–2300 °F);[4] it is strongly reduced in the presence of water, down to 650 °C at a few kBar pressure.[5]

Granite has poor primary permeability, but strong secondary permeability.

Source https://en.wikipedia.org/wiki/Granite 

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