BET_VH Node 8 outputs showing the average absolute probability of accumulating ≥10 kg m−2 of tephra in the next 1 year from a single Plinian phase resulting from a a basaltic eruption and b a rhyolitic eruption, from somewhere within the Tarawera LVZ
Tarawera (Okataina), New Zealand, 2015
Figure 5 in: Thompson, M. A., Lindsay, J. M., Sandri, L., Biass, S., Bonadonna, C., Jolly, G., & Marzocchi, W. (2015). Exploring the influence of vent location and eruption style on tephra fall hazard from the Okataina Volcanic Centre, New Zealand. Bulletin of volcanology, 77(5), 38. https://doi.org/10.1007/s00445-015-0926-y
This hazard map is the result of scientific research and was published in academic literature.
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Thompson, M. A., Lindsay, J. M., Sandri, L., Biass, S., Bonadonna, C., Jolly, G., & Marzocchi, W. (2015). Exploring the influence of vent location and eruption style on tephra fall hazard from the Okataina Volcanic Centre, New Zealand. Bulletin of volcanology, 77(5), 38. https://doi.org/10.1007/s00445-015-0926-yMap Set
https://doi.org/10.1007/s00445-015-0926-y
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