Natural Hazards: Causes and Effects - Disaster Management Center ...
Natural Hazards: Causes and Effects - Disaster Management Center ...
Natural Hazards: Causes and Effects - Disaster Management Center ...
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then cool as thin, gently dipping sheets. Some of the largest volcanoes in the world are shield<br />
volcanoes. The Hawaiian Isl<strong>and</strong>s are composed of these volcanoes. Kilauea <strong>and</strong> Mauna Loa<br />
on the isl<strong>and</strong> of Hawaii are two of the world’s most active volcanoes. The floor of the ocean is<br />
more than 4,900 meters (15,000 feet) deep at the bases of the isl<strong>and</strong>s. Mauna Loa, the largest<br />
of the shield volcanoes (<strong>and</strong> also the world’s largest active volcano), projects 4,700 meters<br />
(13,677 feet) above sea level. Its top is over 9,200 meters (28,000 feet) above the deep ocean<br />
floor.<br />
Lava Domes<br />
Volcanic or lava domes are formed by relatively small, bulbous masses of lava too viscous to<br />
flow any great distance; consequently, on extrusion, the lava piles over <strong>and</strong> around its vent. A<br />
dome grows largely by expansion from within. As it grows its outer surface cools <strong>and</strong> hardens,<br />
then shatters, spilling loose fragments down its sides. Some domes form craggy knobs or<br />
spines over the volcanic vent, whereas others form short, steep-sided lava flows known as<br />
“coulees.” Volcanic domes commonly occur within the craters or on the flanks of large<br />
composite volcanoes.<br />
An idealized Diagram of a Volcano in an Oceanic Environment (Left)<br />
<strong>and</strong> in a Continental Environment (Right)<br />
Figure 4.2