Sudden, rapid movements in glaciers are called glacier surges. Narrow, fast moving sections of an ice sheet are called ice streams.
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.
Three types of glacier movement are basal sliding, internal deformation, and flow. Basal sliding occurs when the glacier moves over a layer of meltwater at its base. Internal deformation involves the slow movement of ice crystals within the glacier. Flow refers to the overall movement of the glacier downslope due to gravity.
Icebergs are produced when large pieces of ice break off from the front of a glacier during a process called calving. This can happen due to a variety of factors like melting from rising temperatures or the natural movement of the glacier.
The downward rapid movement of rocks resulting in mass wasting is called rockfall. It occurs when rocks or rock fragments fall freely through the air due to the force of gravity.
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.
Periods of rapid glacial movement are referred to as glacial surges. These events are characterized by a sudden increase in glacial velocity, resulting in the movement of large quantities of ice over short periods of time. Glacial surges can drastically reshape the landscape and contribute to changes in local ecosystems.
Rapid Eye Movement
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.
The end or outer margin of a glacier is called the glacier terminus. This is where the glacier ends and begins to melt or calve into the surrounding environment, such as a body of water or land. Changes in the glacier terminus are closely monitored by scientists to understand the health and movement of the glacier.
A large boulder left behind by a glacier is called a glacial erratic. These erratics are often significantly different from the surrounding rocks, providing clues about the glacier's movement and the rocks it passed over during its journey.
A crevasse at the head of a mountain glacier is called a "bergschrund." This feature typically forms where the glacier begins to separate from the surrounding terrain, often due to differential movement between the glacier and the mountain slope. Bergschrunds can be quite deep and wide, posing challenges for climbers and hikers navigating the glacier.
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.
An example of a fast-moving glacier that can move up to 6 kilometers per year is the Jakobshavn Glacier in Greenland. It is known for its rapid movement and has been experiencing accelerated ice loss due to climate change.
A ridge-like deposit of sediment at the edge of a glacier is called a "moraine." Moraines are formed from the accumulation of debris and sediment that has been pushed along by the glacier's movement. They can be classified into different types, such as terminal moraines, which mark the furthest advance of the glacier, and lateral moraines, which form along the sides of the glacier.
The term used to describe the movement of a glacier around small obstacles at its base is called "plucking." This process involves the glacier lifting and carrying rocks and debris as it flows over and around obstacles.
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.
Rapid Eye Movement