Marlid
Marlid is a term used in geology to describe a type of sedimentary rock that is composed primarily of calcium carbonate, often in the form of calcite or aragonite. Marlid is typically formed in shallow marine environments, where the accumulation of carbonate-rich materials occurs over long periods. This rock is often characterized by its fine-grained texture and light color, which can range from white to gray or brown, depending on the presence of impurities.
The formation of marlid involves the gradual accumulation of carbonate particles, such as coccoliths (microscopic calcium
Marlid has various uses in construction and industry. It is often used as a building material due