Cinder cones
are the simplest type of volcano. They are built from particles
and blobs of congealed lava ejected from a single vent. As the
gas-charged lava is blown violently into the air, it breaks into
small fragments that solidify and fall as cinders around the
vent to form a circular or oval cone. Most cinder cones have a
bowl-shaped crater at the summit and rarely rise more than a
thousand feet or so above their surroundings. Pyroclastic =
Fire pieces
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Cinder Cone |
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Interior of a cinder cone |
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Oregon Trip Report
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or email
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