This Is What Permafrost Really Is
Much of the subsurface soil of Greenland, Svalbard, and the northerly regions of Scandinavia, Russia, Alaska and Canada has been frozen since the last ice age. Continuous freezing and thawing in the top 20 centimetres (7.9 inches), known as cryoturbation, allows meltwater to circulate and keep the soil relatively fertile. But lower layers than this …














