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Erratics are large boulders that have been transported by glaciers, and often deposited a considerable distance from their origin. For example, there are erratics in the county of Norfolk, in the United Kingdom, that originated in Norway. They are almost always a different type of rock from the surrounding bedrock. They are usually taken through the process of Plucking, in which the friction between the glacier and the ground or valley walls melts the ice at the edges slightly, which then covers any rocks that jut out, when the water freezes once more, the glacier has a hold on the rock and 'plucks' it out of the ground. Of course, rocks can also be absorbed into glaciers through other erosion processes, such as Freeze-thaw weathering.

These rocks are carried along when the glacier spreads, when the glaciation period ends and starts to recede, these rocks are left behind, and are as such erratics.

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