Fig. 10: Schematic of submarine landslide and weak layer occurrence on the Iselin Bank from the mid- to Late Miocene (1) to the Late Pleistocene (6). | Nature Communications

Fig. 10: Schematic of submarine landslide and weak layer occurrence on the Iselin Bank from the mid- to Late Miocene (1) to the Late Pleistocene (6).

From: Climate-controlled submarine landslides on the Antarctic continental margin

Fig. 10: Schematic of submarine landslide and weak layer occurrence on the Iselin Bank from the mid- to Late Miocene (1) to the Late Pleistocene (6).The alternative text for this image may have been generated using AI.

Weak layers are shown by black (WL1), yellow (WL1b) and green (WL2) dashed lines. Submarine landslides are S1, S1b and S2. Red arrows indicate scarp evacuation paths. Solid red line shows location of buried S1b. Panels (1) to (6) show environmental conditions and timing of weak layer and submarine landslide occurrence from the mid- to Late Miocene (1) to the Late Pleistocene (6).

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