Flowstones are mineral formations found in caves, created by the deposition of minerals from dripping water. As water flows over the cave's surface, it leaves behind layers of minerals, primarily calcite, which accumulate over time. This process can result in smooth, sheet-like structures that resemble frozen waterfalls. These formations can vary in color and texture, depending on the minerals present in the water. Flowstones are often found in conjunction with other cave formations, such as stalactites and stalagmites, contributing to the unique beauty of cave systems. They are important indicators of the geological history of an area.