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glaciers move with tremendous force, glaciers advance and retreat, and last but not least, they covered all of Canada and some of New York City :)

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Q: 3 facts about glaciation
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Related questions

What term name is a process by which moving masses of ice change the topography of a region?

Glaciation


Periods of widespread glaciation over the last 2 million to 3 million years are known as what?

The Ice Age.


Precipitaion and glaciation?

Precipitation is rain, sleet,hail,snow,etc. and glaciation is the state of being covered in ice masses and snow basically


Which would be likely to occur in a region of continetal glaciation but not in a region of valley glaciaton?

The presence of large ice sheets covering extensive land areas would be likely in a region of continental glaciation. This type of glaciation is characterized by vast ice sheets that spread over entire continents, unlike valley glaciation which occurs in mountain valleys and is more localized in scope.


What is glaciation?

The movement of compacted snow across an area!


How does glaciation work?

Glaciation occurs when snow accumulates over time and compresses into ice. This ice then flows downhill under its weight, forming glaciers. Glaciers erode the land, carving out valleys and shaping the landscape through processes like plucking and abrasion.


Glaciation effects on interior plains?

Glaciation on interior plains can create unique landforms like drumlins, eskers, and outwash plains. The movement of glaciers can shape the landscape by depositing sediment and carving out valleys. Glaciation also leads to the formation of lakes and wetlands in the region.


What is big rock near Okotoks evidence of?

Glaciation


What is the period of worldwide glaciation called?

Ice age.


How does glaciation affect earth?

E.t. Phone home


Which kind of lake is not the result of glaciation?

oxbow lake


Which moraines is not a characteristic of continental glaciation?

Terminal moraine is not a characteristic of continental glaciation. Terminal moraines are formed at the furthest extent of a glacier, marking the point where it stopped advancing.