Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciat
Franz Josef Glacier in New Zealand
Panorama seen from the Schilthorn. Glaciers, from left to right: Gutz Glacier [de], Chrinnengletscher, Upper Grindelwald Glacier, Eigergletscher, Nollen Glacier [de], Guggi Glacier [de], Giessen Glacier [de], Silberhorn Glacier [de], Hochfirn (Jungfrau), Rottal-Hochfirn, and Rottal Glacier [de]