A tarn is a small, steep-banked mountain lake, formed when a glacier advancing down a slope scoops material out of the ground in a "cirque" at the base of the slope. (Essentially, it continues downward into the ground before moving horizontally again.) When the glacier melts, the depression can fill with water, and is refilled by melting snow unless it becomes filled by silt.
More snow must fall than melts; and buildup must occur in a flat or relatively low slope area
a glacier snout is the front of the glacier :)
A melting glacier gets smaller, but a growing glacier gets bigger.
No. A glaciers is a slowly flowing mass of ice. A slump is a form of mass wasting in which a mass of rock or sediment breaks loose from a slope and moves relatively slowly downhill as a coherent mass.
Angse Glacier in Northern Slope of Himalaya Range.
Yes it is. It is the name of one specific glacier.
Basal slip occurs when the glacier rests on a slope. Pressure causes a small amount of ice at the bottom of the glacier to melt, creating a thin layer of water. This reduces friction enough that the glacier can slide down the slope. Loose soil underneath a glacier can also cause basal slip.
Any glacier moves down a mountain or other slope because of the influence of gravity overcoming the influence of friction.
a glacier
A glacier is on land, moving down-slope like a frozen river. When it meets the sea, it breaks off in pieces, "calving" icebergs, which float in the ocean.
Slope and temperature play a very important role here, the steeper the slope and the higher the temperature, the easier the glacies flows. That being said, a glacier typically starts to flow when it reaches a thickness of between say 50 and 200 meters, depending on slope and temperature. The speed at which it flows is then several meters per year to several tens of meters per year, again depending on slope and temperature.
The geography of the Anchroage area won't support a Piedmont glacier. This glacier (the Piedmont glacier) is characterized by large stagnant ice sheets where a glacier or glaciers "doesn't/don't have anywhere to go" for lack of an outlet. All the areas around Anchroage, Alaska slope down to the sea. There is no place for the ice of a Piedmont glacier to "build up" for lack of a way to "break out" or to "get stopped" to form this glacier.
Essentially yes, a glacier flows just like a river, its made of water (admittedly frozen) just like a river.ice builds up a slope thick slops move faster then than thin slopes the steeper the slope the the fasterAddtional answerThe glacier simply slides down the slope.
A tarn is a small, steep-banked mountain lake, formed when a glacier advancing down a slope scoops material out of the ground in a "cirque" at the base of the slope. (Essentially, it continues downward into the ground before moving horizontally again.) When the glacier melts, the depression can fill with water, and is refilled by melting snow unless it becomes filled by silt.
More snow must fall than melts; and buildup must occur in a flat or relatively low slope area
* Fryingpan Glacier * Nisqually Glacier * Paradise Glacier * Pyramid Glacier * Puyallup Glacier * South Tahoma Glacier * Tahoma Glacier * Success Glacier * Sarvent Glacier