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Comprehensive Risk Assessment for Natural Hazards - Planat

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36<br />

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).

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