100 pages on this wiki. Image showing the six most common speleothems with labels. Enlarge to view labels. A speleothem (pronounced /ËspiËliËÉµÎ¸Ém/ ; from the Greek for cave deposit), commonly known as a cave formation, is a secondary mineral deposit formed in a cave.Speleothems are typically formed in limestone or dolostone solutional caves.peleothems formed from salt, sulfur and other minerals are also known. Speleothems made of pure calcium carbonate are a translucent white color, but often speleothems are colored by minerals such as iron, copper or manganese, or may be brown because of mud and silt particulate inclusions.
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