Accumulation Zone

On a glacier, the accumulation zone is the area above the firn line, where snowfall accumulates and exceeds the losses from ablation, (melting, evaporation, and sublimation). The annual Glacier equilibrium line separates the accumulation and ablation zone annually. The accumulation zone is also defined as the part of a glacier’s surface, usually at higher elevations, on which there is net accumulation of snow, which subsequently turns into firn and then glacier ice. Part of the glacier where snow builds up and turns to ice moves outward from there.

Famous quotes containing the words accumulation and/or zone:

    Creation destroys as it goes, throws down one tree for the rise of another. But ideal mankind would abolish death, multiply itself million upon million, rear up city upon city, save every parasite alive, until the accumulation of mere existence is swollen to a horror.
    —D.H. (David Herbert)

    He who, from zone to zone,
    Guides through the boundless sky thy certain flight,
    In the long way that I must tread alone,
    Will lead my steps aright.
    William Cullen Bryant (1794–1878)