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Fig. 1 | Swiss Journal of Geosciences

Fig. 1

From: Combined cosmogenic 10Be, in situ 14C and 36Cl concentrations constrain Holocene history and erosion depth of Grueben glacier (CH)

Fig. 1

Modelled production rate depth profile for sample Grub2, see chemical composition in Table 3. Solid lines are total production rates for 10Be (red), 14C (blue) and 36Cl (green). Detailed contribution of different production pathways are shown for 36Cl. The magnitude of the characteristic subsurface production peak caused by thermal and epithermal neutrons (dotted line) depends on the concentration of 35Cl in the rock

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