a valley glacier
a valley glacier
a valley 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.
A tidewater glacier is a type of glacier that flows into the sea. As the glacier reaches the ocean, pieces of ice break off to form icebergs in a process known as calving.
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.
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
yes...
is a glacier.