Training for Glaciers
A glacier is analogue to a river of ice and snow. The “headwaters” of which are an area known as the “accumulation zone.” In this region snow piles up faster than it melts. Below this, nearing the “river delta,” so to speak, there is an area known as the “ablation zone.” In this lower region the snow melts faster than it accumulates. The demarcation of these […]
