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A piedmont glacier is a type of glacier that forms when a valley glacier spills out of its valley and spreads out onto a lowland area, typically where it meets a larger body of water or an open plain.
1 sty 2014 · Definition. A valley or outlet glacier exhibiting a lobe- or fan-shaped section (“piedmont lobe”) immediately beyond the confining valley mouth, where the ice tongue emanates onto an unconstrained, lower slope angle terrain (Stroeven 2013). Valley glaciers may coalesce to form large, multilobate piedmont glaciers.
piedmont glacier. large ice lobe spread out over surrounding terrain, associated with the terminus of a large mountain valley glacier. The massive lobe of Malaspina Glacier in Alaska is clearly visible in this photograph taken from a Space Shuttle flight in 1989.
geology. Also known as: shelf ice. Learn about this topic in these articles: characteristics. In glacier: Classification of mountain glaciers. …of mountain ranges are called piedmont glaciers. Outlet glaciers are valley glaciers that originate in ice sheets, ice caps, and ice fields.
9 lut 2018 · Valley and piedmont glaciers originate in the high alpine and terminate on land. They often flow through deep bedrock valleys that confine the ice on either side. Over time, they carve and shape these valleys (see U-Shaped Glacial Valleys).
30 paź 2022 · Piedmont glaciers are formed when a glacier leaves the laterally constricting relief of a mountain range in order to then flow out in all directions in the foreland with little relief. Piedmont glaciers are not independent glaciers, but only parts of a larger glacier or glacier system.
Piedmont glaciers occur when steep valley glaciers flow onto relatively flat plains, where they spread out into fan or bulb shapes (lobes). The Malaspina Glacier in Alaska is one of the most famous examples of this type of glacier and, at 40 miles wide, it is the largest piedmont glacier in the world.
