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Fig. 3 | Geoenvironmental Disasters

Fig. 3

From: Seismites in the Pleistocene succession and recurrence period of large earthquakes in the Kathmandu Valley, Nepal

Fig. 3

Columnar cross-sections between locations 1 and 9. The dotted lines indicate the key beds (thick mud beds with diatomite, denoted as A and B, and the erosion surface of the 39-ka event shown by the large black arrow). The bold lines beside the sections mark the intervals containing SSDs. A to L denote intervals with SSDs in the Tokha Formation. Those of the Gokarna Formation can be correlated as solid lines. T.F = Tokha Formation, Th.F. = Thimi Formation, n = SSDs interval without evidence of sliding

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