Arjen P. Stroeven

TL;DR: In this article, in situ cosmogenic 10Be and 26Al concentrations from glacial erratics on relict surfaces as well as glacially eroded bedrock adjacent to these surfaces, provide consistent last deglaciation exposure ages (∼8−13 kyr), confirming ice sheet overriding as opposed to ice free conditions.

TL;DR: In this article, the authors used cosmogenic 10Be and 26Al data from three tors and a meltwater channel in the Parkajoki area to test the hypothesis of landscape preservation through multiple glacial cycles.

TL;DR: In this article, the authors present a detailed map of the distribution of preglacial surface remnants in the Kebnekaise region of northwestern Sweden, and explain the pattern of glacial erosion as the result of three specific modes of glaciation known to have existed during the last 120,000 years and inferred to have repeatedly prevailed during 2.75 million years: cirque glaciation, mountain ice sheets, and Fennoscandian ice sheets.

TL;DR: In this article, a stake net consisting of up to 32 stakes covering the greater part of Storglaciaren was surveyed 70 times, yielding roughly 2000 separate determinations of vertical and horizontal velocity.

TL;DR: In this paper, the authors performed spatio-temporal qualitative modeling of ice sheet extent and migration of erosion and deposition zones through the entire Quaternary, and suggest an explanatory model for the current spatial pattern of Quaternarial deposits and the two different types of erosion zones.