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  2. Your Guide to the Real Cost of Granite Countertops - AOL

    www.aol.com/lifestyle/guide-real-cost-granite...

    It’s important to note for the average home renovation granite countertops will cost between $2,250 and $4,500, and most people are spending $3,250 for their countertops. In terms of square ...

  3. Engineered stone - Wikipedia

    en.wikipedia.org/wiki/Engineered_stone

    Engineered stone. Engineered stone is a composite material made of crushed stone bound together by an adhesive to create a solid surface. The adhesive is most commonly polymer resin, with some newer versions using cement mix. This category includes engineered quartz (SiO 2), polymer concrete and engineered marble stone. [1]

  4. Granite - Wikipedia

    en.wikipedia.org/wiki/Granite

    Granite (/ ˈɡrænɪt / GRAN-it) is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground.

  5. Graniterock - Wikipedia

    en.wikipedia.org/wiki/Graniterock

    Watsonville, California. Key people. Peter Lemon, President & CEO. Number of employees. 650. Website. www.graniterock.com. Graniterock is an American corporation, founded in 1900 as "Granite Rock", and based in Watsonville, California. It operates in the construction industry providing crushed gravel, sand, concrete, asphalt and paving services.

  6. Countertop - Wikipedia

    en.wikipedia.org/wiki/Countertop

    Countertop. A countertop, also counter top, counter, benchtop, worktop (British English) or kitchen bench (Australian or New Zealand English), bunker (Scottish English) is a raised, firm, flat, and horizontal surface. They are built for work in kitchens or other food preparation areas, bathrooms or lavatories, and workrooms in general.

  7. I-type granite - Wikipedia

    en.wikipedia.org/wiki/I-type_Granite

    I-type granite. I-type granites are a category of granites originating from igneous sources, first proposed by Chappell and White (1974). [1] They are recognized by a specific set of mineralogical, geochemical, textural, and isotopic characteristics that indicate, for example, magma hybridization in the deep crust. [2]

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