Deep crevasses called bergschrunds can form when a moving one of these objects separates from the headwall, and masses of firn are precursors to these objects that gain mass in the Zone of (*) Accumulation, and lose mass in the Zone of Ablation.
A certain double eponymous law measures the rate of internal flow in these entities and models the relationship between stress and strain. Deep crevasses called bergschrunds can form when a moving one of these objects separates from the headwall, and masses of firn are precursors to these objects that gain mass in the Zone of (*) Accumulation, and lose mass in the Zone of Ablation. The Piedmont variety of these objects create a valley and coalesce at the base of a mountain, and these objects deposit debris which forms moraines. Calving is a process in which icebergs break off of, for ten points, what large sheets of ice that come in Alpine and Continental forms?
A certain double eponymous law measures the rate of internal flow in these entities and models the relationship between stress and strain.
glaciers [accept Alpine Glacier, Continental Glacier, Piedmont Glacier, or “Ice Sheet” before mention] &lt;RP&gt;