In situ .sup.10Be modeling and terrain analysis constrain subglacial quarrying and abrasion rates at Sermeq Kujalleq , Greenland

Glacial erosion creates diagnostic landscapes and vast amounts of sediment. However, knowledge about the rate at which glaciers erode and sculpt bedrock and the proportion of quarried (plucked) versus abraded material is limited. To address this, we quantify subglacial erosion rates and constrain the ratio of quarrying to abrasion during a recent, ⼠200-year long overriding of a bedrock surface fronting, Sermeq Kujalleq (Jakobshavn Isbræ), Greenland, by combining .sup.10 Be analyses, a digital terrain model, and field observations. Cosmogenic .sup.10 Be measurements along a 1.2 m tall quarried bedrock step reveal a triangular wedge of quarried rock. Using individual .sup.10 Be measurements from abraded surfaces across the study area, we derive an average abrasion rate of 0.13 ± 0.08 mm yr.sup.-1 . By applying this analysis across a ⼠1.33 km.sup.2 study area, we estimate that the Greenland Ice Sheet quarried 378 ± 45 m.sup.3 and abraded 322 ± 204 m.sup.3 of material at this site. These values result in an average total erosion rate of 0.26 ± 0.16 mm yr.sup.-1, with abrasion and quarrying contributing in roughly equal proportions within uncertainty. Additional cosmogenic .sup.10 Be analysis and surface texture mapping indicate that many lee steps are relicts from the prior glaciation and were not re-quarried during the recent overriding event. These new observations of glacier erosion in a recently exposed landscape provide one of the first direct measurements of quarrying rates and indicate that quarrying accounts for roughly half of the total glacial erosion in representative continental shield lithologies.