mosslined

Mosslined is a type of naturally occurring thin, flexible sheet of material found in certain environments. It is composed of decomposed and consolidating plant remains, often vegetation, that has been subjected to humid conditions. The formation process is unique in that it requires a combination of factors such as an adequately high level of calcium and low levels of organic compounds.

A distinguishing feature of mosslined is its extremely low shear strength. When encountered, it can appear as a thin, smooth, and flexible sheet or may be layered. It is formed through a series of gradual transformations that take place as organic matter gradually dissolves. The presence of calcium salts plays a significant role in this process.

Several environments are known to host the formation of mosslined, with tropical regions being particularly common. Certain types of vegetation, such as tropical cycad gardens and intertidal flats, are often associated with its occurrence. The precise conditions under which mosslined forms remain somewhat specific to each site.

While mosslined was historically referred to by earlier researchers as stylolites or more appropriative factors, the term "mosslined" has emerged as the preferred nomenclature in contemporary research contexts. Researchers study mosslined to better understand geological and biological processes involved in its formation and to explore its potential implications for landscape evolution.