The Medial Glacier is known for its surging behavior. This phenomenon involves rapid movement of the glacier over a short period, often leading to significant changes in its size and shape. Surges can be caused by various factors, including changes in meltwater availability or internal pressure within the glacier. Other examples of surging glaciers include the Bering Glacier in Alaska and the Variegated Glacier in Alaska as well.
still flows and carries debris to the end of the glacier
An ice cap glacier is a dome-shaped glacier that flows in all directions from a central high point. These glaciers cover large areas and can have multiple outlet glaciers flowing towards different directions.
yes...
an ice sheet
The top part of a glacier is called the "glacier head" or "glacier accumulation zone." This area is where snow accumulates and compacts to form ice, feeding the glacier as it flows downward. The glacier head is crucial for the glacier's overall mass and movement, as it is where new material is added.
a valley glacier
a valley glacier
a valley glacier
A continental glacier can move in all directions and a valley glacier can move in a surge. :)
The tip of a glacier is called the glacier terminus or glacier snout. It is the furthest point reached by the glacier as it flows downhill.
No, a glacier canyon is not a real glacier. A glacier canyon is a canyon formed by the movement of a glacier over time, carving out the landscape as it flows.
still flows and carries debris to the end of the glacier
still flows and carries debris to the end of the glacier
An ice cap glacier is a dome-shaped glacier that flows in all directions from a central high point. These glaciers cover large areas and can have multiple outlet glaciers flowing towards different directions.
yes...
is a glacier.
an ice sheet