It ended it's life in Wisconsin. In the back of my farm! (What is referred to as the Kettle Moraine area)
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.
The rapid movement of a glacier is called a glacier surge. This sudden acceleration in movement can be caused by internal changes within the glacier, such as the release of stored meltwater or changes in the glacier's structure.
A crevasse is a large crack in a glacier.
The zone above the snowline on a glacier is called the accumulation zone. This is where snowfall exceeds melting, leading to an increase in glacier mass.
The front of a glacier is called the terminus or terminus face. This is where the glacier ends and may be characterized by ice cliffs or a build-up of glacial debris.
The most recent North American ice age ended about 10,000 years ago. It was called the Wisconsin Glacier or the Wisconsin Episode.
malaspina glacier
A frozen river is called a frozen river. Rivers that normally flow as liquid water, are called frozen rivers when they become frozen.
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.
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 slow melting glacier
The rapid movement of a glacier is called a glacier surge. This sudden acceleration in movement can be caused by internal changes within the glacier, such as the release of stored meltwater or changes in the glacier's structure.
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.
Sediments directly deposited by the glacier are called till.
Glacier is called "हिमनद" in Hindi.
A hole in the ground left by a glacier is called a"kettle." Many of these form shallow lakes, as with the kettle lakes in Wisconsin, Michigan, and Ontario. This could also be called a cirque which is defined as a bowl-shaped, steep-walled mountain basin carved by glaciation, often containing a small, round lake. Cirque lake is a phrase used to describe these kinds of lakes.
The upper part of a glacier is called the accumulation zone. This is the area where snow accumulates and feeds the glacier, eventually turning into ice and flowing downhill towards the glacier's terminus.