GRANITES

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Quartz is silicon ore, particularly very pure silicon oxide, the second most widespread mineral in nature. It is an important miner of the lithosphere and is involved in its components at about 12%. It is also the only mineral that consists exclusively of silicon and oxygen. The quartz ions are very strongly bonded and therefore have a great hardness. It comes in many different forms, with a color of dark brown-black (smoky) to totally transparent The rocks are found in granular or crystalline form. It is a mineralogical component of acidic explosive rocks, as well as of metamorphosed and sedimentary rocks. It is known internationally with the name "Quartz" or Synthetic Granite or Industrial Stone. It features a rich color gamut of choices and high technical yields.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.

Granite is a widespread, natural pyrogenic, plutonium rock with granular tissue and acidic composition with great hardness. It belongs to the plutonium of igneous rocks because it was created by the solidification and crystallization of the magma inside the crust at great depth, so it has a full-crystal, granular tissue. GNEISS: Character of Gneiss is the changing of light and dark zones, both of silicate minerals. What is more characteristic of Gneiss is its characteristic texture than its mineral composition. This texture is characteristic of the transformation of high temperatures (600-700 °C) and similar pressures.