Michigan

Armada, MI Granite Countertops, Natural Stone & Marble Company

Granite Countertop Installation and Repair in Armada

Looking to hire a granite fabricator in Armada, MI? Our company is called Abella Stone and we would like to introduce ourselves. We are a local Michigan wholesaler and fabricator of natural stone including granite, marble, and other types of stone. Here we can supply you with do-it-yourself counters or provide complete installation packages. Contact us today to discuss your project further.

Michigan Granite & Natural Stone Contractor in Armada

An outdoor kitchen and bbq can utilize natural granite for its countertops. Although you may have a color palette in mind, know that on bright sunny days, dark colors will be drastically hotter than light colors – sometimes even too hot to touch! Also know that in Armada, MI you should only install a SWR, severe weather rated, granite that can withstand the seasonal changes of our northern climate. Abella Stone can show you SWR granites from current our inventory at our full slab showroom.

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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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