speleothemmit

Speleothemmit is a term used to describe mineral deposits found within caves that are not typical speleothems. Unlike stalactites, stalagmites, or flowstones formed by the slow dripping or flowing of mineral-rich water, speleothemmit refers to formations that arise from more rapid precipitation processes. These can include mineral crusts, botryoidal masses, or even delicate crystalline growths. The term often encompasses deposits formed by sprays, splashes, or even evaporation in areas of high humidity or airflow within a cave. The composition of speleothemmit is typically similar to that of regular speleothems, primarily calcite, but other minerals like aragonite, gypsum, or even rarer substances can be present depending on the cave's geology and water chemistry. The formation environment plays a crucial role, with speleothemmit often found on cave walls, ceilings, or floors in areas distinct from active water flow. They can form relatively quickly compared to their more commonly known counterparts. Studying speleothemmit can provide valuable insights into the past hydrological conditions, air movement, and chemical environments of a cave system.