Regosolic Turbic Cryosol (R.TC)

Common horizon sequence: Om, Cy, Cgy, Cz

These Turbic Cryosols have developed on recently deposited or strongly cryoturbated soil materials. They are identified by the following properties:

1. These soils lack B horizons.
2. These soils usually have little incorporated organic matter.
3. Cryoturbation is manifested by oriented stones, displacement of materials, and sorting.

Note: Diagnostic horizons are underlined.

List all known examples