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Geological Formation

Rootless Cone

Volcanic Formations

A rootless cone is a volcanic landform that closely resembles a true volcanic crater but has no actual magma conduit connecting it to depth, meaning it is not itself a vent through which lava has erupted. It forms when a flow of hot lava crosses a wet surface such as a swamp, lake or pond, heating the water beneath it into steam; as pressure builds, the steam eventually bursts through the overlying lava in an explosion similar to a phreatic eruption, throwing up material that piles into a cone shaped mound. Because the resulting cone can look very much like a genuine volcanic crater despite having no root reaching into a magma source, rootless cones are a recognized source of confusion when mapping volcanic terrain.

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Caused By

Volcanism, Processes
Source Rootless cone (Wikipedia)

In Discipline

Source Rootless cone (Wikipedia)
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Rootless cone (Wikipedia)
  • Caused By: Volcanism, Lead
    A rootless cone, also formerly called a pseudocrater, is a volcanic landform which resembles a true volcanic crater, but differs in that it is not an actual vent from which lava has erupted.
  • In Discipline: Volcanology, Lead paragraph
    A rootless cone, also formerly called a pseudocrater, is a volcanic landform which resembles a true volcanic crater, but differs in that it is not an actual vent from which lava has erupted.
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