Solution:Podzol soil is found near 60º North latitudes in Eurasia and North America's coniferous forest of Taiga region.Podzol soils, also known as Spodosols, are acidic, ash-grey soils formed through a process called podzolization, characterized by leaching of iron and aluminum compounds, and are typically found in cool, humid, and coniferous forest regions.
Podzolization is a soil formation process where dissolved organic matter and ions of iron and aluminum, released through weathering, are moved from the upper soil layers and accumulate in deeper layers.
Podzol soils are characterized by a light-colored, ash-grey surface horizon (eluvial horizon) and a dark, humus-rich subsurface horizon (illuvial horizon). They are commonly found in cool, humid climates, particularly in boreal and temperate regions under coniferous forests (taiga).
Podzol soils have a distinct soil profile with a bleached, ash-grey surface layer (E horizon) and a darker, humus-rich layer below (Bs horizon). Podzols are generally acidic and nutrient-poor, with limited agricultural potential.