Reference soil Costa Rica 11: Andosol
Andosols occur throughout the world where volcanic activity is common, especially in the circum-Pacific region and along the mid-Atlantic Ridge.
Characteristics
Soils with a vitric or andic horizon (slightly to moderately weathered horizons in pyroclastic deposits dominated by short-range-order minerals, notably allophane and imogolite) starting within 25 cm from the soil surface. In addition, they may have a histic, fulvic, melanic, mollic, umbric, ochric, duric, or cambic horizon. Other diagnostic horizons (unless buried deeper than 50 cm by volcanic deposits) are absent.
Reference soil CR011: Andosols
influenced by volcanic ashes. However, the first 35cm of the topsoil is strongly deviating from the buried A horizon, the latter having more convincing andic properties. High biological activity throughout the soil. Actual classification: FAO (1988): Umbric Andosol Soil Taxonomy (1992):Acrudoxic Melanudand