The cosmogenic nuclide 10Be was analyzed by using accelerator mass spectrometry on an ice core drilled at the Dome Fuji station, inland Antarctica, for 700-1900 yr CE. The measured concentration of 10
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This is dataset used in paper Wang, Y. and Willett, S. D.: Escarpment retreat rates derived from detrital cosmogenic nuclide concentrations, Earth Surf. Dynam., 9, 1301–1322, https://doi.org/10.51
This is the dataset used to create Figure 14 in "Potential Ice Sheet Modulation of Volcanism in West Antarctica: Constraints on the cadence and magnitude of melt delivery into the crust"
The surface motion of the glacier was measured by surveying 6 stakes (1.5-2.0 m long aluminium poles) installed in the ice of Qaanaaq ice cap. Dual-frequency GPS receivers and antennas (GNSS GEM-1) we