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

Table 1 List of samples, basic parameters and measured cosmogenic nuclide concentrations

Sample ID	Latitude (WGS 84)	Longitude (WGS 84)	Elevevation (m a.s.l.)	Thickness (cm)	topographic shielding	¹⁰Be conc. (10⁵ at/g ^a_qtz )	¹⁴C conc. (10⁵ at/g_qtz)	³⁶Cl conc. (10⁵ at/g ^b_sample )
Grub1	46.607	8.266	2465	1.0	0.99	2.88 ± 0.10	5.22 ± 0.26
Grub2	46.606	8.267	2416	1.0	0.99	2.21 ± 0.12	5.17 ± 0.26	4.52 ± 0.27
Grub3	46.605	8.268	2405	2.0	0.99	2.69 ± 0.15	5.20 ± 0.26	3.45 ± 0.24
Grub4	46.605	8.269	2374	3.0	0.99	2.03 ± 0.11	4.29 ± 0.21	3.92 ± 0.21

^aMeasured against standard 07KNSTD (Nishiizumi et al. 2007), corrected for full process blank of (3.6 ± 2.6) × 10⁻¹⁵ ¹⁰Be/⁹Be
^bMeasured against standard K382/4N (Christl et al. 2013), corrected for full process blank of 3.4 × 10⁻¹⁵ ³⁶Cl/³⁵Cl