Drapery Flowstones
Drapery flowstones are a type of speleothem formation found in caves, characterized by smooth, curved sheets of mineral deposits that resemble flowing fabric or curtains. These formations are created by mineral-laden water seeping down cave walls and leaving behind thin layers of calcite or other minerals as the water evaporates. The unique shapes and patterns of drapery flowstones are formed over many years as the minerals build up layer by layer, creating intricate and beautiful structures in underground caverns.