How do cinder cone volcanoes form? It is created by flank eruptions of larger volcanos. Once a large amount of magma forms, it rises until it reaches the surface, creating an eruption. Ash is made up of pyroclastic particles smaller than 2 millimeters. Cinder cone volcanoes form when high temperatures and pressure melt rock deep inside the Earth. Once a large amount of magma forms, it rises until it reaches the surface, creating an eruption. Pyroclastic material from 2 to 64 millimeters is called lapilli. The parasitic cone volcanos are similar to the cinder cones, however, the volcano is found on the flanks of other volcanos, hence, the name. Cinder cone volcanoes are built from particles and blobs of congealed lava ejected from a single vent or opening. Cinder cones form out of tephra, magma and ash that it ejects. Some examples of cinder cone volcanoes include the Holocene volcano and the Pleistocene volcano. Pyroclastic refers to particulate matter. Cinder cone volcanoes are formed from pyroclastic eruptions. When cinder cones spew out this gaseous lava, it spits it up in the air.

Once erupted, ash can fall or flow. The largest pyroclastic materials are bombs or blocks, depending on shape. Another name for cinder cone volcanoes is a scoria cone volcano.

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