5.12 - Gelisols
Gelisols are soils with permafrost within 2 meters of the surface. These soils generally have limited profile development. Most of the soil forming processes in these soils occur near the surface, sometimes resulting in significant accumulation of organic matter. Large areas of this soil occur in the Northern regions of Russia, Canada, and Alaska. These areas become boggy wetlands in the summer, and support large numbers of migratory birds and grazing mammals. The permafrost of Gelisols tends to become unstable (melt) if disturbed, leading to a waterlogged soil condition that poses problems for engineering uses.
Key Characteristics: Gelisols
- Soils with frozen subsoils (permafrost)
- Limited profile development
- Surface accumulations of soil organic matter
- Productivity limited by short growing season
- Extensive in high latitudes
- Extent of world ice-free land area: 9%