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A volcanic plug, also called a volcanic neck or lava neck, is a volcanic landform created when magma hardens within a vent on an active volcano. When present, a plug can cause an extreme build-up of pressure if rising volatile-charged magma is trapped beneath it, and this can sometimes lead to an explosive eruption. Glacial erosion can lead to exposure of the plug on one side, while a long slope of material remains on the lee 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.
Examples of volcanic plugs
Sigiriya, or the Lion's Rock or the Lion's Mountain, is a hardened magma volcanic plug formed from an extinct and long-eroded volcano. The rock rises 370 m (1,210 ft) and is sheer on all sides, in many places overhanging the base. The volcanic plug hosts an ancient rock fortress and ruins of a castle, one of the eight UNESCO World Heritage Sites of Sri Lanka.
There are several volcanic plugs in New Zealand, including the Pinnacles in the Coromandel Peninsula, Bream Head, Paritutu and adjacent Sugar Loaf Islands, and Piha's Lion Rock, which hosted a fortified Maori pa.
In Australia, the The Nut, in Tasmania is a further example; along with Mount Warning and a number of peaks in the Greater Blue Mountains Area, including Mount Banks, Mount Hay, Mount Wilson, Mount Irvine, and Mount Tomah.
Saint Michel d'Aiguilhe chapel, whose construction started in 969, near Le Puy-en-Velay in France. The volcanic plug rises about 85 metres (279 ft) above the surroundings. Another building on a volcanic plug is the 14th century Trosky Castle in the Czech Republic.
In the Americas
Examples of volcanic plugs in the United States include Morro Rock, California and Laurel Hill, New Jersey. Devils Tower in Wyoming, as well as Little Devils Postpile located in Yosemite National Park, are also thought to be a volcanic plug by many geologists. Another example of a volcanic plug in the eastern USA is the highly eroded Stark's Knob basaltic structure located along the Hudson River near Saratoga Springs, New York. However, some geologists believe Stark's Knob is not a plug at all, but merely an outcrop of an ancient submarine lava flow.
The origin of Devils Tower (featured in the 1977 movie Close Encounters of the Third Kind) is not totally clear. Although it is generally admitted[by whom?] that it was formed by igneous intrusion, it is not necessarily a volcanic plug (stricto censu) which formed within the vent of an active volcano.
The Pitons of Saint Lucia, in the eastern Caribbean Sea are two volcanic plugs that rise abruptly out of the sea and are part of a UNESCO World Heritage site. The highest mountain plug rises to a height of nearly 760 metres (2,490 ft).
In the United Kingdom
Ailsa Craig, Bass Rock, North Berwick Law and Dumgoyne hill are examples of volcanic plugs located in Scotland. There are over 30 volcanic plugs in Northern Ireland, including Slemish, Tievebulliagh, Scawt Hill, Carrickarede, Scrabo and Slieve Gallion.
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Sigiriya Rock Fortress, Sri Lanka.
Taung Kalat, Burma.
Dent de la Rancune, a challenging climbing site in the Chaîne des Puys, France.
Trosky Castle ("Panna" Tower), Czech Republic.
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