Similarities: Both glacial and continental glaciers are large masses of ice that move slowly over land due to gravity. They both hold massive amounts of freshwater locked in their ice.
Differences: Glacial glaciers are smaller and form in mountainous regions, while continental glaciers are much larger ice sheets that cover vast land areas. Glacial glaciers tend to move faster due to steeper slopes, while continental glaciers move more slowly due to their immense size.
Alpine glaciers form in mountainous regions and are confined within valleys or cirques, while continental glaciers are large ice sheets that cover vast land areas. Alpine glaciers are typically smaller and more fragmented compared to the continuous ice sheets of continental glaciers.
The two remaining continental glaciers are Antarctica and Greenland. While Greenland is part of North America and located between the Arctic and Atlantic Oceans, Antarctica is situated at the South Pole.
Alpine glaciers, even though they move, are confined to mountain valleys, which in most instances had previously been a stream valley. Continental ice sheets exist on a much larger scale. These huge masses flow out in all directions from one or more centers of the land. They cover the entire continent, hence the name, and extend out toward the sea. Only two exist today: Greenland and Antarctica.
The continental crust is thicker and less dense than oceanic crust. Oceanic crust is younger and primarily composed of basalt, while continental crust is older and made up of a variety of rock types, including granite and sedimentary rocks.
A Venn diagram would be the most effective graphic organizer to use when taking notes on an article describing the differences between Earth and Mars. This will help visually represent the similarities and differences between the two planets, making it easier to compare and contrast the key points.
One is bigger than the other one
Alpine glaciers form in mountainous regions and are confined within valleys or cirques, while continental glaciers are large ice sheets that cover vast land areas. Alpine glaciers are typically smaller and more fragmented compared to the continuous ice sheets of continental glaciers.
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They difference between them is where there flow. Continental glaciers are enormous ice sheets, and are found in Greenland and Antarctica. Alpine glaciers form in mountain valleys.