Fig. 8
From: Three-dimensional topology dataset of folded radar stratigraphy in northern Greenland

Difference between a fifteen-times vertically exaggerated (a) and not exaggerated (b) view on the Petermann Glacier P1 12.0 ka horizon.
From: Three-dimensional topology dataset of folded radar stratigraphy in northern Greenland
Difference between a fifteen-times vertically exaggerated (a) and not exaggerated (b) view on the Petermann Glacier P1 12.0 ka horizon.