Repetitive rifts can be seen in a glacier descending to the sea in St Johnsfjorden / Prins Karls Forland in Svalbard. These crevasses are caused by the constant movement of the glacier, causing tension between solid plates and the subsequent fracturing at weak points.
Repetitive rifts can be seen in a glacier descending to the sea in St Johnsfjorden / Prins Karls Forland in Svalbard. These crevasses are caused by the constant movement of the glacier, causing tension between solid plates and the subsequent fracturing at weak points.
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Photo credit: © Alistair Knock / Alamy / Afripics
License: Royalty Free
Model Released: No
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