Reference soil Costa Rica 12: 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 CR012: Andosols
Brief soil description: Very deep, well drained, brownish black over yellowish brown loamy soil. The upper 50 cm have a very high organic matter content. The soil has been formed in various superimposed volcanic ash deposits of the Turrialba volcano. The site has been used for many years for pasture, which has caused compaction of the upper 30 cm, as evidenced by slight mottling. At time of description, the land was being prepared for growing potatoes and later on beans, after which pasture will probably be reestablished. In the subsoil some very large pores are present, partly filled up which material from the A horizon.