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What makes granite the hardest building stone?

building granite hardest stone
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What makes granite the hardest building stone?

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Natural granite stone is formed by solidification of liquid magma under the pressure of earth’s crust. Granite stone is composed of Feldspar, Quartz, Mica, and other minerals, making it one of the hardest stones in the world. granite has been used for building and decorative purposes for centuries. Granite stone resists wear-and-tear applications remarkably well, making it ideal for interior or exterior flooring. When granite used for outdoors, structure is not influenced by freeze-thaw cycles.

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Granite is formed by solidification of liquid magma (molten rock) under the pressure of earth’s crust. It is composed of Feldspar, Quartz, Mica, and other minerals, making it one of the hardest stones in the world. It has been used for building and decorative purposes for centuries. Granite resists wear-and-tear applications remarkably well, making it ideal for interior or exterior flooring. When used outdoors, granite’s mineralogical structure is not influenced by freeze-thaw cycles.

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A. Granite is formed by solidification of liquid magma (molten rock) under the pressure of earth’s crust. It is composed of Feldspar, Quartz, Mica, and other minerals, making it one of the hardest stones in the world. It has been used for building and decorative purposes for centuries. Granite resists wear-and-tear applications remarkably well, making it ideal for interior or exterior flooring. When used outdoors, granite’s mineralogical structure is not influenced by freeze-thaw cycles.

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A. Granite is formed by solidification of liquid magma (molten rock) under the pressure of earth’s crust. It is composed of Feldspar, Quartz, Mica, and other minerals, making it one of the hardest stones in the world. It has been used for building and decorative purposes for centuries. Granite resists wear-and-tear applications remarkably well, making it ideal of interior or exterior flooring. When used outdoors, granite’s mineralogical structure is not influenced by freeze-thaw cycles.

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