Stalsetts

Stalsetts is a term sometimes used to describe formations found in caves. These formations are typically mineral deposits that grow downwards from the ceiling of a cave. While the term stalsett is not a standard geological term, it appears to be a portmanteau of "stalactite" and "sett," a term that can refer to a badger's home or a bed. Therefore, a stalsett could be interpreted as a stalactite that resembles a bed or a resting place.

The more common and scientifically accepted term for these downward-growing cave formations is stalactite. Stalactites form over long periods as mineral-rich water drips from the cave ceiling. As the water evaporates, it leaves behind dissolved minerals, most commonly calcite. These minerals accumulate, slowly building the stalactite layer by layer. The shape and size of stalactites can vary greatly depending on factors such as the rate of water flow, the concentration of minerals, and the surrounding cave environment.

The usage of the term stalsett appears to be informal or possibly regional. In geological contexts, precise terminology is important for clear communication. Standard terms like stalactite, stalagmite (which grows upwards from the floor), and columns (where a stalactite and stalagmite meet) are used to describe these cave features. If encountered, "stalsett" likely refers to a stalactite with a particular visual characteristic, but it does not represent a distinct type of cave formation in scientific literature.