Ice is a viscous fluid: it flows but slowly, reaching up to 100 m/yr for the fastest flowing ice. That’s 0.00001 km/hr, so you’d never see it with the naked eye. But what influences the morphology of the glaciers is the shape of the topography that lies underneath them. Elephant Foot Glacier, shown above, aptly named for its shape, is a textbook-example of a piedmont glacier. These types of glacie ...[Read More]
The foot of a glaciated mammoth? No… A glacier!
Elephant Foot Glacier, Greenland. Credit: Ole Zeising (distributed via imaggeo)