A volcano is a vent
in the earth from which molten rock and gas erupt. The molten
rock that erupts from the volcano forms a hill or mountain around the
vent. The lava may flow out as a viscous liquid, or it may be
exploded from the vent as solid or liquid particles.
The most fluid magmas are
erupted quietly. They flow from the vent to form gently sloping
shield volcanoes. The lava flows from the shield volcanoes are
usually only 1 to 10 meter thick. They may extend for great distances
away from the vent.
Magmas with high gas
contents and high viscousities are usually more explosive. These
gas-rich magmas are blown high into the air during an eruption. The
magma falls as volcanic bombs, which accumulate around the vent. They
form steep-sided cinder cones.
Most of the tallest
volcanoes are stratovolcanoes. These form from a cycle of quiet
eruptions of fluid lava followed by explosive eruptions of viscous
lava.
A volcano may exhibit
different styles of eruptions at different times. Eruptions may
change from one type to another as the eruption progresses. The least
violent type of eruption is termed Hawaiian. It is characterized by
extensive fluid lava flows from central vents. Occasionally it is
accompanied by lava fountains. Strombolian eruptions are
characterized by moderately fluid lava flows. Vulcanian eruptions are
marked by viscous magmas.
Volcanic activity has
yielded a variety of economic resources. Volcanoes supply both
lightweight and heavy aggregate, as well as pumice for
abrasives and elements such as sulfur, copper and many other.
Recently volcanic areas have become important sources of
geothermal energy.
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