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Geological Formation

Hornito

Volcanic Formations

A hornito is a conical or pipe-like structure built up by lava spattering or being ejected through an opening in the crust of a lava flow. Hornitos resemble spatter cones but are rootless, meaning they were once sources of lava without being directly connected to a true vent or magma source; they usually form through the slow upwelling of fluid lava through the roof of a lava tube, often associated with pahoehoe lava of basaltic composition, and can exceed ten meters in height.

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Volcanism, Processes
Source Hornito (Wikipedia)

In Discipline

Source Hornito (Wikipedia)
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Hornito (Wikipedia)
  • In Discipline: Volcanology, Lead paragraph
    A hornito is a conical, or pipe-like, structure built up by lava spattering or being ejected through an opening in the crust of a lava flow
  • Caused By: Volcanism, Lead paragraph
    A hornito is a conical, or pipe-like, structure built up by lava spattering or being ejected through an opening in the crust of a lava flow
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