Michigan

Birmingham, MI Granite Countertops, Natural Stone & Marble Company

Granite Countertop Installation and Repair in Birmingham

Do you want a granite company in the Birmingham, MI area that has non-pushy, non-commission sales people that can just give you a straight answer? Look no further because Abella Stone is here to help. We can take your approximate measurements over the phone, fax or email and give you a budgetary price without even coming to our facility. Contact us today and receive a free quote.

Michigan Granite & Natural Stone Contractor in Birmingham

Granite countertops in the kitchen and bath are a seemingly “must-have” when trying to sell a home. People are realizing how important it is to have this upgrade in order to put their listing at the top of a potential buyers list, and Abella Stone can help you do this. Abella can provide granite tops for you to save money by installing yourself, or provide a complete fabrication and installation. Once installed, buyers looking in Birmingham, MI are sure to move your home up on their list.

Company News from Abella Stone

Marble Definition (Shelby Township, MI)

Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or dolomite. It is commonly used for sculpture and as a building material. 

Marble is a rock resulting from metamorphism of sedimentary carbonate rocks, (most commonly limestone or dolomite rock). Metamorphism causes variable recrystallization of the original carbonate mineral grains. The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals. Primary sedimentary textures and structures of the original carbonate rock (protolith) have typically been modified or destroyed.

Pure white marble is the result of metamorphism of a very pure (silicate-poor) limestone or dolomite protolith. The characteristic swirls and veins of many colored marble varieties are usually due to various mineral impurities such as clay, silt, sand, iron oxides, or chert which were originally present as grains or layers in the limestone. Green coloration is often due to serpentine resulting from originally high magnesium limestone or dolostone with silica impurities. These various impurities have been mobilized and recrystallized by the intense pressure and heat of the metamorphism. According to Wikipedia

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