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There are two primary types of
volcanic activity. They are explosive eruptions and quiet
flows of lava (Leet, pp. 53-77).
Examples of both types of activity are illustrated in the geologic
cross-section on the right. The source of
heat, gases, and molten rock are the underlying magma chamber.
The following types of emissions result from explosive eruptions:
Water vapor is the major component of volcanic gases. Typically, water makes up 80 per cent or more of the gas. Other typical components of volcanic gases include carbon dioxide, hydrogen sulfide, sulfur, sulfur dioxide, hydrochloric acid, and ammonium chloride. In the illustration the magma chamber eventually cools and becomes solid rock and is known as a batholith. Molten rock in the vents cool and become solid rock structures known as dikes. Solid and liquid materials emitted vary with the composition of the molten rock in the magma chamber. The composition of most magma chambers (from an examination of batholiths, which are cooled and solidified magma chambers) has been found to be granite or granodiorite. Some Useful Links Following are some hyperlinks that can further assist with the evaluation and description of faults:
Volcanoes - Website that provides information, links, and extensive illustrations about volcanoes and volcanic activity. USGS maps, products, and publications - Online information resource on the U.S. Geological Survey website. |
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