Publication Sample-type Sample-ID Group-ID Sample Lat(DD) Long(DD) Elev(masl) Thickn(cm) Density(g/cm3) Shield 10Be-conc(at/g) 10Be-unc(at/g) 10Be-std 26Al-conc(at/g) 26Al-unc(at/g) 26Al-std Sampl-year Publ-10-age(yr) Publ-10-unc(yr) Publ-26-age(yr) Publ-26-unc(yr) 10Be-age(yr) 10-ext-unc(yr) 10-int-unc(yr) 26Al-age(yr) 26-ext-unc(yr) 26-int-unc(yr) Extra-publ Schäfer (2000) boulder Schä2000-1 Schä2000-A Lit1a 30.254 99.593 4890 1.5 2.7 1 821000 71000 S555 9470000 800000 ZAL94 1998 8500 700 16300 1700 11493 1224 997 18890 2198 1611 - Schäfer (2000) boulder Schä2000-1 Schä2000-A Lit1a-2 30.254 99.593 4890 1.5 2.7 1 838000 67000 S555 10360000 820000 ZAL94 1998 8600 600 - - 11651 1179 934 20392 2295 1630 - Schäfer (2000) boulder Schä2000-1 Schä2000-A Lit1a-neu 30.254 99.593 4890 1.5 2.7 1 943000 86000 S555 11240000 970000 ZAL94 1998 9700 900 - - 12915 1426 1182 21666 2553 1890 - Schäfer (2000) boulder Schä2000-2 Schä2000-A Lit1b 30.254 99.593 4890 5 2.7 1 1157000 100000 S555 5380000 440000 ZAL94 1998 12500 1100 9300 900 15589 1661 1353 11810 1346 971 - Reference: Schäfer JM, 2000. Reconstruction of landscape evolution and continental paleoglaciations using in-situ cosmogenic nuclides: examples from Antarctica and the Tibetan Plateau. PhD thesis, ETH Zürich. Data comments: Latitudes and longitudes based on map figures and Google Earth. Topographic shielding factors calculated from SRTM 30 m dem based on Codilean (2006) and Li (2013). 10Be standard assumed to be S555. 26Al standard assumed to be ZAL94. Sampling year assumed to be 1998. Samples Lit1a (repeat measurements) and Lit1b are separate samples from one boulder. One group ID for all samples (all samples from one location). expage.github.io - data from expage-202306