Andisols are soils that have formed in volcanic ash. 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. Globally, Andisols are the least extensive soil order and only account for ~1% of the ice-free land area. They occupy ~1.7% of the US land area, including some very productive forests in the Pacific Northwest region. Below is a map of andisols eight suborder's distribution in the U.S.
I have also included a link to an article below which is about infiltration rate in andisols and the effect of changes in vegetation cover.
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