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Figure in a journal article
Assessment and zonation of hazards from future lahars of phreatic and collapse-type at Soufrière in Guadeloupe (according to Westercamp, 1981b)
Figure 10.5 in: Westercamp, D. (1983). Appraisal and zonation of volcanic hazards in the French Lesser Antilles: preliminary results. In: Tazieff, H. & Sabroux, J.-C. (Eds.) Forecasting Volcanic Events, Elsevier, Amsterdam, p. 111-130.
Figure in a journal article
ASTER-derived land classification map of Fig. 3 overlain with effusion rate contours for the 2,000-m vent zone and the modified Guest and Murray (1979) vent zone
Figure 6 in: Harris, A. J., Favalli, M., Wright, R., & Garbeil, H. (2011). Hazard assessment at Mount Etna using a hybrid lava flow inundation model and satellite-based land classification. Natural Hazards, 58(3), 1001-1027. https://doi.org/10.1007/s11069-010-9709-0
Figure in a journal article
Atmospheric dispersion of tephra for a threshold of 2 mg m−3 for all FL for the eruption scenarios of Hekla ERS 1947-type (a, b, c), Katla LLERS (d, e, f) and Askja OES 1875-type (g, h, i)
Figure 13 in: Biass, S., Scaini, C., Bonadonna, C., Folch, A., Smith, K., & Höskuldsson, A. (2014). A multi-scale risk assessment for tephra fallout and airborne concentration from multiple Icelandic volcanoes–Part 1: Hazard assessment. Natural hazards and earth system sciences, 14(8), 2265-2287. https://doi.org/10.5194/nhess-14-2265-2014
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
Ballistic vulnerability or probability of casualty assuming an eruption during the time of exposure, along the Tongariro Alpine Crossing
Figure 12 in: Fitzgerald, R. H., Tsunematsu, K., Kennedy, B. M., Breard, E. C. P., Lube, G., Wilson, T. M., Jolly, A.D., Pawson, J., Rosenburg, M.D., & Cronin, S. J. (2014). The application of a calibrated 3D ballistic trajectory model to ballistic hazard assessments at Upper Te Maari, Tongariro. Journal of volcanology and geothermal research, 286, p. 248-262. https://doi.org/10.1016/j.jvolgeores.2014.04.006
Figure in a journal article
Best-guess probability map of vent opening
Figure 2 in: Massaro, S., Rossi, E., Sandri, L., Bonadonna, C., Selva, J., Moretti, R., & Komorowski, J. C. (2022). Assessing hazard and potential impact associated with volcanic ballistic projectiles: The example of La Soufrière de Guadeloupe volcano (Lesser Antilles). Journal of volcanology and geothermal research, 423, 107453. https://doi.org/10.1016/j.jvolgeores.2021.107453
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
Black and white, English language version of the revised three-colour hazard map for Ambae, primarily taking into account renewed activity of the main summit crater and disturbance of the crater lakes
Figure 9 in: Cronin, S.J., Gaylord, D.R., Charley, D., Alloway, B.V., Wallez, S., & Esau, J.W. (2004). Participatory methods of incorporating scientific with traditional knowledge for volcanic hazard management on Ambae Island, Vanuatu. Bulletin of volcanology, 66(7), p. 652-668. https://doi.org/10.1007/s00445-004-0347-9