Regosolic Static Cryosol (R.SC)

Common horizon sequence: C, Cg, Cz

These Static 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 may have thin (<15 cm thick) peaty organic layers and a thin Ah horizon.

Note: Diagnostic horizons are underlined.

List all known examples