Fig. 7From: Combined cosmogenic 10Be, in situ 14C and 36Cl concentrations constrain Holocene history and erosion depth of Grueben glacier (CH)Sensitivity to burial and erosion. Apparent exposure ages of Grub2 calculated for two sets of scenarios. Concentration uncertainties of 6 %, resulting in 8.5 % uncertainties on nuclide ratios, are used for sensitivity statements. A 9.6 ka of exposure followed by a burial period of tb = 0–1500 years. tb = 1000 years is identical to scenario B in Figs. 2 and 3. If burial lasts longer than ~500 years, in situ 14C is expected to yield significantly lower apparent ages than 10Be or 36Cl. B 9.6 ka of exposure followed by a burial period of 500 years. While buried, the surface is eroded by 0–15 cm by glacial erosion. The starting point at erosion depth = 0 is the same as tb = 500 years in panel A. If more than ~6 cm are eroded, 36Cl yields significantly higher apparent ages than 10BeBack to article page