Tinted detail of a photo: Close-up of reddish brown soil packed with rounded pebbles in cream, yellow and brown, crossed by grey tree roots.
SSS
Soil System Sciences

cold regions

Cold soil in the groove

Often, soils from cold regions, such as Arctic soils, show polygonal forms in their surface. These polygons are formed because of the freeze-thaw cycle, characteristic of permafrost. What is permafrost? Permafrost is a subsurface soil layer which stays permanently frozen (below 0 oC) during long periods of time, usually more than two consecutive years. Most extensive …[Read More]