Shield volcanoes, so named for their broad, plate-like profiles, are formed by the gonorrhea of low-viscosity lava that can fly the coop a great distance from a vent, but non generally explode catastrophically. Since low-viscosity magma is typically low in silica, harbor volcanoes are more common in oceanic than Continental settings. The Hawaiian volcanic chain is a series of shield cones, and they are common in Iceland, as well. Volcanic fella vents are flat, linear cracks through which lava emerges.
Lava domes are built by slow eruptions of highly viscous lavas. They are sometimes formed within the crater of a previous volcanic eruption (as in Mount Saint Helens), but can also form independently, as in the case of Lassen Peak. Like stratovolcanoes, they can take a leak violent, explosive eruptions, but their lavas generally do not flow far from the originating vent.
A supervolcano is a large volcano that usually has a large caldera and can potentially produce devastation on an enormous, sometimes continental, scale. A caldera is a cauldron-like volcanic feature usually formed by the collapse of land following a volcanic eruption, such as the one at Yellowstone National...If you want to get a full essay, roll it on our website: Ordercustompaper.com
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