Figure 3
From: The timing and widespread effects of the largest Holocene volcanic eruption in Antarctica
Composite image showing sediment cores from four Byers Peninsula lakes with radiocarbon and thermoluminescence ages (see refs30,31 and Supplementary Table 1). Note that the cores are arranged to align the top of the rapid post-seismic depositional unit of varying thickness, interpreted as a mass-wasting deposit, which interrupts the laminated, moss-rich, lacustrine sedimentation in each lake.
