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A glacier is not a parked block of ice. It creeps downhill under its own weight all year.

Earth Science Facts, sourced to National Snow and Ice Data Center.

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Ice under enough pressure deforms rather than shattering, so the bulk of a glacier flows like extremely stiff treacle while the brittle top layer cracks into crevasses over the moving mass beneath. Meltwater at the base can let the whole thing slide as well. That motion is what carves a valley into a U shape, hauls boulders many kilometers from their parent rock, and leaves them stranded when the ice retreats.

The claim comes from National Snow and Ice Data Center.

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