Cinder Cones
Cinder cone

WHAT IS A CINDER CONE?

Volcano facts

Location: The magma chamber is beneath Yellowstone National Park in the state of Wyoming.

Facts: The initial eruption of 2.1 million years ago was 2,500 times more powerful than the Mt. St. Helens eruption and perhaps was the largest, most violent volcanic eruption in the history of earth. Enough ash and volcanic debris exploded from the eruptions to cover the entire western half of the United States with about a four-foot deep layer of ash. Roughly 600 cubic miles of material were thrown into the atmosphere.

 

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The Cinder Cone Volcanoes

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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Cinder Cones | Shield Volcanoes | Stratovolcanoes | Giant Calderas - The Yellowstone Caldera

 

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