
As far as volcanoes go, these are
the classic, cone-shaped peaks we commonly associate with a lava-spewing
eruption. Eruptions from cinder cones are pretty small potatoes, as
far as volcanic eruptions go. They tend to be small, hill-sized volcanoes
that range in height from tens to hundreds of meters high and they can
build up over short periods of a few months to a few years. Cinder cones
are characterized by their steeply angled sides and conical shapes.
In fact, these mini-volcanoes are most often found on the flanks of
larger, mountain-sized volcanic peaks.
In a cinder cone, lava erupts from
a small vent in the crust and 'sprays' melted rock fragments into the
air where they then fall back to earth in a pile. These rock fragments
are glassy, gas-filled chunks of lava called cinders or scoria
that cool rapidly as they sail through the air and land next to the
vent opening, slowly accumulating in the geometric shape of a cone.
Some of the most dramatic volcanic eruptions are these displays of lava
fountains shooting sparkling, glowing glass-like rock fragments into
the air from cinder cones.
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