During the last Ice Age, the glacier reached its southernmost extent in Indiana, stopping near the southern tip of the state around the Ohio River. This boundary is often referred to as the "glacial boundary," where glacial deposits can be found in the northern regions, while the southern areas are primarily characterized by non-glacial sediments. The influence of the glacier has shaped Indiana's topography, leaving behind features such as moraines and kettle lakes in the northern part of the state.
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It can cover much of a hemisphere, as the ice sheets did in the Pleistocene Ice Age.
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Antarctica is a continent, not a glacier, and has only ever moved south.
As the ice blocks left behind by the continental glacier melted after the last ice age, they formed bodies of water known as kettle lakes. These kettle lakes are depressions in the landscape caused by the melting of the ice blocks, which were then filled with water from the melted ice.
The answer to the question is a glacier is a mass of ice.
Scientists determine the age of a glacier by studying layers of ice cores extracted from the glacier. By analyzing factors such as ice composition, particle concentration, and isotopic composition, scientists can estimate the age of the ice layers. Additionally, dating techniques like carbon dating and radionuclide dating can provide further insights into the age of the glacier.
The Malaspina and the Athabasca are names of the two glaciers. 2. They both carved great lakes.
Greenland center.
Greenland Center
No. Has nothing to do with voting.
an ice berg is a chunk off off a glacier and a glacier is a big ice patch caused by snow