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Cindercone

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Cinder cone is a steep conical hill formed from loose volcanic materials ejected from a single volcanic vent. It is formed when basaltic or very fluid magma explodes from a vent, building up around it in the shape of a cone. Examples of cinder cones include Cerro Negro, Paricutin, and Sunset Crater.

CINDER CONE
Danna Sellote
Emma Farrarons
Xen Pedroza

Cinder Cone
is a steep conical hill of loose
pyroclastic fragments, such as
either volcanic clinkers, cinder
s, volcanic ash or scoria that
has been built around
avolcanic vent.

HOW IS IT FORMED?

EXAMPLES
• Cerro Negro

Paricutin

Sunset Crater

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Cindercone

1. CINDER CONE Danna Sellote Emma Farrarons Xen Pedroza

2. Cinder Cone is a steep conical hill of loose pyroclastic fragments, such as either volcanic clinkers, cinder s, volcanic ash or scoria that has been built around avolcanic vent.

3. HOW IS IT FORMED?

4. EXAMPLES • Cerro Negro

6. Sunset Crater