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Flowstone suspended from the ceiling of Gunns Plains Cave, Tasmania, Australia
Flowstone suspended from the ceiling of Gunns Plains Cave, Tasmania, Australia

Flowstones are composed of sheetlike deposits of calcite formed where water flows down the walls or along the floors of a cave. The Gunns Plains Cave is an underground Limestone Show cave, located in Gunns Plains in the mid-lands of north Tasmania, twenty kilometres from Ulverstone Tasmania is an Australian island and state of the same name It is located south of the eastern side of the Continent, being separated from it by Bass For a topic outline on this subject see List of basic Australia topics. Calcite is a carbonate mineral and the most stable polymorph of Calcium carbonate ( Ca[[carbon C]] O 3 A cave is a natural underground void large enough for a human to enter They are typically found in "solution", or limestone caves, where they are the most common speleothem. Limestone is a Sedimentary rock composed largely of the Mineral Calcite ( Calcium carbonate: CaCO3 A speleothem (from the Greek for "cave deposit" commonly known as a cave formation, is a secondary mineral deposit formed in a Cave. However, they may form in any type of cave where water enters that has picked up dissolved minerals.

Flowing films of water that move along floors or down positive-sloping walls build up layers of calcium carbonate (calcite), aragonite, gypsum, or other cave minerals. Aragonite is a Carbonate mineral, one of the two common naturally occurring polymorphs of Calcium carbonate, Ca[[carbon C]] O 3 Gypsum is a very soft Mineral composed of Calcium sulfate dihydrate with the Chemical formula Ca[[sulfur S]] O 4ยท2 A mineral is a naturally occurring substance formed through geological processes that has a characteristic chemical composition a highly ordered atomic structure and specific These minerals are dissolved in the water and are deposited when the water loses its dissolved carbon dioxide, meaning it can no longer hold the minerals in solution. Carbon dioxide ( Chemical formula:) is a Chemical compound composed of two Oxygen Atoms covalently bonded to a single The flowstone forms when thin layers of these deposits build on each other, sometimes becoming rounder as the deposit gets thicker.

The deposits may grade into thin sheets called "draperies" where they go over overhanging portions of the wall. Some draperies are translucent, and some have brown and beige layers that look much like bacon (often termed "cave bacon"). Bacon is a cut of Meat taken from the sides belly or back of a Pig that has been cured, smoked, or both

Though flowstones are among the largest of speleothems, they can still be damaged by a single touch. The oil from human fingers causes the water to avoid the area, which then dries out.

Cave Bacon in the Caverns of Sonora near Sonora, Texas.
Cave Bacon in the Caverns of Sonora near Sonora, Texas. The Caverns of Sonora, a National Natural Landmark, is a unique Cave located eight miles (13 km west of the town of Sonora Texas. Sonora is a city in and the County seat of Sutton County, Texas, United States.

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One of the flowstone features in the Sudwala Caves
One of the flowstone features in the Sudwala Caves
Karst topography is a landscape shaped by the dissolution of a layer or layers of soluble Bedrock, usually Carbonate rock such as Limestone The Sudwala Caves in Mpumalanga, South Africa, are set in Precambrian Dolomite rock which was first laid down about 3800 million years ago when

Dictionary

flowstone

-noun

  1. (geology) A layered deposit of calcite formed by water flowing down the walls, and along the floor of a cave.
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