Advanced Search for Maps
Showing 1-10 of 18
Figure in a journal article
Absolute probability for areas to be affected by a ballistic impact density >0.001
Figure 12 in: Strehlow, K., Sandri, L., Gottsmann, J. H., Kilgour, G., Rust, A. C., & Tonini, R. (2017). Phreatic eruptions at crater lakes: occurrence statistics and probabilistic hazard forecast. Journal of Applied Volcanology, 6(1), 4. https://doi.org/10.1186/s13617-016-0053-2
Figure in a journal article
BA hazard maps displaying the yearly mean probability of areas being impacted by BA
Figure 8 in: Sandri, L., Thouret, J. C., Constantinescu, R., Biass, S., & Tonini, R. (2014). Long-term multi-hazard assessment for El Misti volcano (Peru). Bulletin of volcanology, 76(2), 771. https://doi.org/10.1007/s00445-013-0771-9
Figure in a journal article
BET_VH Node 8 maps showing the average absolute probability of accumulating ≥10 km m−2 of tephra in the next 1 year from a single Plinian phase resulting from a a basaltic eruption from within the OVC, b a rhyolitic eruption from within the OVC and c either a basaltic or rhyolitic eruption from within the OVC
Figure 7 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
Figure in a journal article
BET_VH Node 8 maps showing the average conditional probability of accumulating ≥10 kg m−2 tephra given a single Plinian phase resulting from a a basaltic eruption from within the Tarawera LVZ; b a rhyolitic eruption from within the Tarawera LVZ; d a basaltic eruption from within the Haroharo LVZ; e a rhyolitic eruption from within the Haroharo LVZ; e a basaltic eruption from Ruawahia Dome, a single vent within the Tarawera LVZ (see star in Fig. 4); and f a rhyolitic eruption from Ruawahia Dome
Figure 8 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
Figure in a journal article
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
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
Figure in a journal article
Combined (in terms of eruptive size and vent location) PS hazard map displaying the yearly mean probability of areas being impacted by PS
Figure 10 in: Sandri, L., Thouret, J. C., Constantinescu, R., Biass, S., & Tonini, R. (2014). Long-term multi-hazard assessment for El Misti volcano (Peru). Bulletin of volcanology, 76(2), 771. https://doi.org/10.1007/s00445-013-0771-9
Figure in a journal article
Combined (in terms of eruptive sizes and vent location) PF hazard map displaying the yearly mean probability of areas being impacted by PFs
Figure 11 in: Sandri, L., Thouret, J. C., Constantinescu, R., Biass, S., & Tonini, R. (2014). Long-term multi-hazard assessment for El Misti volcano (Peru). Bulletin of volcanology, 76(2), 771. https://doi.org/10.1007/s00445-013-0771-9
Figure in a journal article
Combined (in terms of eruptive sizes and vent location) TF hazard map, displaying the dry- and wet-season mean probability of areas being impacted by a TF load larger than 100 kg/m²
Figure 6 in: Sandri, L., Thouret, J. C., Constantinescu, R., Biass, S., & Tonini, R. (2014). Long-term multi-hazard assessment for El Misti volcano (Peru). Bulletin of volcanology, 76(2), 771. https://doi.org/10.1007/s00445-013-0771-9
Figure in a journal article
Combined (in terms of eruptive sizes and vent location) TF hazard map, displaying the dry- and wet-season mean probability of areas being impacted by a TF load larger than 250 kg/m²
Figure 7 in: Sandri, L., Thouret, J. C., Constantinescu, R., Biass, S., & Tonini, R. (2014). Long-term multi-hazard assessment for El Misti volcano (Peru). Bulletin of volcanology, 76(2), 771. https://doi.org/10.1007/s00445-013-0771-9
Figure in a journal article
Example of uncertainty on hazard maps for tephra load exceeding 100 kg/m² for the dry (10th and 90th percentiles of the posterior pdf) and rainy (10th and 90th percentiles of the posterior pdf) seasons
Figure 12 in: Sandri, L., Thouret, J. C., Constantinescu, R., Biass, S., & Tonini, R. (2014). Long-term multi-hazard assessment for El Misti volcano (Peru). Bulletin of volcanology, 76(2), 771. https://doi.org/10.1007/s00445-013-0771-9
Page: 1 2