Comprehensive Risk Assessment for Natural Hazards - Planat
Comprehensive Risk Assessment for Natural Hazards - Planat
Comprehensive Risk Assessment for Natural Hazards - Planat
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Chapter 4 — Volcanic hazards<br />
Figure 4.2 — Hawaiian type (Type example, Hawaii, USA)<br />
Figure 4.3 — Pelean type (Type example Mt Pelé,<br />
Martinique, French West Indies)<br />
Figure 4.4 — Plinian type (Defined at Vesuvius, Italy)<br />
Figure 4.5 — Vulcanian type (Defined at Vulcano, Italy)<br />
SO 2 Sulfur dioxide<br />
CO 2 Carbon dioxide<br />
HF Hydrofluoric acid, etc.<br />
Figure 4.6 — Strombolian type (Defined at Stromboli, Italy)<br />
Figure 4.7 — Sketch of gas emission<br />
Figure 4.9 — Sketch of a landslide<br />
Figure 4.8 — Sketch of a lahar<br />
Fig. 4.10 — Sketch of a tsunami<br />
4.2 DESCRIPTION AND CHARACTERISTICS OF<br />
THE MAIN VOLCANIC HAZARDS<br />
An active volcano can produce different hazards as<br />
defined by the IAVCEI (1990). These can be subdivided<br />
into:<br />
• Primary or direct hazards due to the direct impact of<br />
the eruption products.<br />
• Secondary or indirect hazards due to secondary consequences<br />
of an eruption.<br />
4.2.1 Direct hazards<br />
One can distinguish four principal types of direct volcanic<br />
hazards (Holmes, 1965). These are: lava flows; pyroclastic<br />
flows; ash fulls and block falls; and gases:<br />
(a) Lava flows (Figure 4.2);<br />
(b) Pyroclastic flows such as pumice flow, nuée ardente,<br />
base surge, … (Figure 4.3);<br />
(c) Ash falls and block falls (Figures 4.4, 4.5 and 4.6);<br />
(d) Gases (Figure 4.7).