05.01.2013 Views

Natural Hazards: Causes and Effects - Disaster Management Center ...

Natural Hazards: Causes and Effects - Disaster Management Center ...

Natural Hazards: Causes and Effects - Disaster Management Center ...

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!