[title text=”Mineral Pumice” style=”bold_center”]

Mineral pumice is formed by the cooling of volcanic lava and the release of gases within it. This process creates a porous and lightweight structure in the pumice. Pumice grains are usually colored white, light gray, and cream, and are very light. This lightness is one of the most important reasons for pumice’s popularity in the construction industry, as it greatly reduces the overall weight of the structure.