Reference soil United States of America 17: Cryosol

US017

Cryosols typically occur in arctic and mountainous regions where permanently frozen subsoil or "permafrost" is found.

Characteristics

Soils having one or more cryic horizons (horizon with evidence of being perennially frozen) within 100 cm from the soil surface.

Distribution of Cryosols (rough estimation supplied by soilgrids)

 

Reference soil US017: Cryosols

PROFILE DESCRIPTION: Bg1: matrix colour also very dark greyish brown (10YR 3/2, moist). Cg1: distorted strata; matrix colour also olive brown (2.5Y 4/4, moist); texture: lenses of very fine sandy loam. Cg2: strata; matrix colour also olive brown (2.5Y 4/4, moist); texture: lenses of very fine sandy loam. Cf: strata; matrix colour also olive brown (2.5Y 4/4, moist); texture: lenses of very fine sandy loam. Permafrost present between 40 and 100 cm depth

 

Classification

WRB 1998 
Gleyi-Turbic- Cryosol (Stagnic) 
  
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Stagni-Gelic Cambisol gelundicGelic Gleysol
- cmcambic B horizon
- cmochric A horizon
-permafrost
-stagnic
- cmcambic B horizon
- cmochric A horizon
-hydromorphic
-permafrost

 

Local classification:Tanana silt loam, thawed & drained