Mamelon (volcanology)

A mamelon (from French mamelon, "nipple") is a rock formation created by eruption of relatively thick or stiff lava through a narrow vent in the bedrock.[1][2] Because the lava is not fluid, it does not flow away; instead it congeals around the vent, forming a small hill or mound on the surface. The outflow from successive eruptions forms additional layers on top, and the resulting pile of layers may stand over 100 metres (330 ft) above the surrounding surface.

The term was coined by the French explorer and naturalist Jean Baptiste Bory de Saint-Vincent, to describe the central peak of the Dolomieu Crater in the Piton de la Fournaise volcano on Réunion.[3]

Hanging Rock in Australia is another example of a mamelon.

See also

References

  1. ^ Geocaching. "Geocaching - The Official Global GPS Cache Hunt Site". www.geocaching.com. Retrieved 2024-12-03.
  2. ^ "Hanging Rock | World Wide Panorama". The World Wide Panorama. Retrieved 2024-12-03.
  3. ^ "Internal structure and building of basaltic shield volcanoes: the example of the Piton de La Fournaise terminal cone (La Réunion)" (PDF). 2012.
Stub icon

This volcanology article is a stub. You can help Wikipedia by expanding it.