terfraksionasi
Terfraksionasi, also spelled terfractionation, is a term used in the field of geology to describe the process of breaking down rocks into smaller fragments through a combination of physical and chemical weathering processes. This process is crucial in the formation of soil and the breakdown of parent material into finer particles. Terfraksionasi occurs over long periods of time and is influenced by various factors such as climate, topography, and the type of rock being weathered.
The physical aspect of terfraksionasi involves the mechanical breakdown of rocks through processes like freeze-thaw cycles,
The end product of terfraksionasi is a mixture of mineral fragments and organic matter, which together form