Andisols
Andisols (from Japanese ando, "black soil") are soils that have formed in volcanic ash or other volcanic ejecta. They differ from those of other orders in that they typically are dominated by glass and short-range-order colloidal weathering products such as allophane, imogolite and ferrihydrite. As a result, Andisols have andic properties — unique chemical and physical properties that include high water-holding capacity and the ability to "fix" (and make unavailable to plants) large quantities of phosphorus. They are divided into eight suborders: Aquands, Gelands, Cryands, Torrands, Xerands, Vitrands, Ustands and Udands.
Globally, Andisols are the least extensive soil order and only account for approximately 1% of the ice-free land area. They occupy approximately 1.7% of the U.S. land area, including some very productive forests in the Pacific Northwest region.
Xerands, Vitrands (Idaho)
Xerands — temperate Andisols with very dry summers and moist winters; Vitrands — relatively young Andisols that are coarse-textured and dominated by glass
Cryands (Iceland)
Andisols of cold climates
Vitrands (New Zealand)
Relatively young Andisols that are coarse-textured and dominated by glass
Udands (Costa Rica)
Andisols of humid climates
Andic soil properties, Mazama eruption
Andic soil properties are characteristic of Andisols, soils formed from volcanic ash, which are significantly influenced by the Mount Mazama eruption (~7,700 years ago) in the Pacific Northwest