We conducted cosmogenic 26Al/10Be analysis of boulders from Thule, NW Greenland.
We utilized numerical models to constrain exposure/burial scenarios and uncertainty.
Most of the boulders have been preserved beneath cold-based, non-erosive ice.
Some boulders were exposed during Marine Isotope Stages 5e and 1.
Other boulders have longer, more complex histories spanning hundreds of ky.