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Pre-LGM Northern Hemisphere ice sheet topography

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Figure

Fig. 1. The Terra Nivea and Grinnell ice caps (on the skyline) riseonly about 200 m above the level 600 m-elevation plateau of MetaIncognita Peninsula, Baffin Island
Fig. 2. The geological and geomorphological constraints (ice mar-gin outlines) that were used in modeling paleotopography for glacialmaxima during MIS 5b (heavy solid line) and 4 (thin solid line).LGM ice extent is indicated with stippled line
Figure 4b and c show the changing position of this polethroughout the modeled time interval
Fig. 5. Modeled ice sheet thickness for MIS 5bMIS 2 (a), MIS 4 (b) and (c). Geological and geomorphological constraints from Fig
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