Hazards map of pyroclastic flows produced by central dome explosions based on four recognized events during the past 40 k.y., and small-size landslides produced by flank instability, and debris and hyperconcentrated flows produced by syneruptive or posteruptive processes.
Tacaná, Mexico-Guatemala, 2000
Figure 14 in: Macias, J. L., Espíndola, J. M., Garcia-Palomo, A., Scott, K. M., Hughes, S., & Mora, J. C. (2000). Late Holocene Peléan-style eruption at Tacaná volcano, Mexico and Guatemala: Past, present, and future hazards. Geological Society of America Bulletin, 112(8), p. 1234-1249. https://doi.org/10.1130/0016-7606(2000)112%3C1234:LHPEAT%3E2.0.CO;2
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