Volcanic plug

An aerial view of the Gros Piton and Petit Piton, in St. Lucia, 2006.

A volcanic plug, also called a volcanic neck or lava neck, is a volcanic object created when magma hardens within a vent on an active volcano. When present, a plug can cause an extreme build-up of high gas pressure if rising volatile-charged magma is trapped beneath it, and this can sometimes lead to an explosive eruption. In a plinian eruption the plug is destroyed and ash is ejected.[1]

Glacial erosion can lead to exposure of the plug on one side, while a long slope of material remains on the opposite side. Such landforms are called crag and tail. If a plug is preserved, erosion may remove the surrounding rock while the erosion-resistant plug remains, producing a distinctive upstanding landform.

  1. ^ Huff, W.D.; Owen, L.A. (2013). "Volcanic Landforms and Hazards". Treatise on Geomorphology. 5: 155. doi:10.1016/B978-0-12-374739-6.00089-0. ISBN 9780080885223.

© MMXXIII Rich X Search. We shall prevail. All rights reserved. Rich X Search