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This is another example and image of a cinder cone volcano. Amboy Crater is located in southern California. At this moment in time, this volcano is extinct.

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This is another example and image of a cinder cone volcano. Amboy Crater is located in southern California. At this moment in time, this volcano is extinct.

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This is an example and image of a cinder cone volcano! Wizard Island is located in Crater Lake National Park, Oregon. 

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This is an example and image of a cinder cone volcano! Wizard Island is located in Crater Lake National Park, Oregon. 

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In this second instance they are horseshoe-shaped (see below),  with the lava flow issuing out of the open end because during  the eruption any pyroclasts that landed on the flow were rafted  away.

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In this second instance they are horseshoe-shaped (see below),  with the lava flow issuing out of the open end because during  the eruption any pyroclasts that landed on the flow were rafted  away.

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This image is a horsehow shaped lava flow!

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Cinder cones  can also be distinctly asymmetric if there was a persistent wind  blowing during the eruption and/or they form at the heads of major lava flows.

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Cinder cones  can also be distinctly asymmetric if there was a persistent wind  blowing during the eruption and/or they form at the heads of major lava flows.

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  The reddish color is common to cinder cones and occurs both during and soon after the associated eruption due to the combined efforts of moisture and oxidizing gases. 

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  The reddish color is common to cinder cones and occurs both during and soon after the associated eruption due to the combined efforts of moisture and oxidizing gases. 

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If the precise location of the  vent changes during an eruption, the cone loses its simple circular  shape, and becomes more complex.

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If the precise location of the  vent changes during an eruption, the cone loses its simple circular  shape, and becomes more complex.

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Cinder cones tend to be roughly  circular. They  are usually formed later in an eruption when activity has localized  to one or more discrete vents.

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Cinder cones tend to be roughly  circular. They  are usually formed later in an eruption when activity has localized  to one or more discrete vents.

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Lava fountains are driven by expanding gas bubbles; the  bubbles are trying to expand in all directions but the only way  to relieve the pressure is up out the vent so fountains are usually  directed relatively vertically. 

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Lava fountains are driven by expanding gas bubbles; the  bubbles are trying to expand in all directions but the only way  to relieve the pressure is up out the vent so fountains are usually  directed relatively vertically. 

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Cinder cones consist of cinders, more properly called scoria. Scoria is very vesicular, low density  basalt.

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Cinder cones consist of cinders, more properly called scoria. Scoria is very vesicular, low density  basalt.