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. 2016 Jul 22;7:12295. doi: 10.1038/ncomms12295

Figure 8. Image of a coarse and lithic-rich pyroclastic deposit interpreted to be a co-ignimbrite lag breccia.

Figure 8

The scale bar is 15 cm. This depositional facies indicates proximity to an eruptive vent which may have been associated with the SE bounding fault of the caldera shown in Fig. 7. The outcrop is located at eastern shore of lake Ilopango (13.67304°N and 89.01202°W.)