Fossils can end up in glaciers through a process called glacial transport, where ice and snow accumulate and slowly move over time. As glaciers advance, they can pick up and carry sediment, rocks, and organic material, including fossils, from the surrounding environment. When glaciers melt or retreat, these materials can be deposited in new locations, exposing the fossils that were previously encased in ice. This process can lead to the discovery of ancient organisms preserved in glacial deposits.
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