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Cone sheet

Type of igneous intrusion of subvolcanic rock

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A cone sheet is a type of high-level igneous intrusion of subvolcanic rock, found in partly eroded central volcanic complexes. Cone sheets are relatively thin inclined sheets, generally just a few metres thick, with the geometry of a downward-pointing cone. Viewed from above, their outcrop is typically circular to elliptical. They were originally described from the Ardnamurchan, Mull and other central complexes of the British Tertiary Volcanic Province (now recognised as part of the North Atlantic Igneous Province).

01Occurrence

Cone sheets are widely distributed at the lower levels of volcanic complexes.

Examples of cone sheet complexes
NameLocationAgeDominant rock typeReference
Ardnamurchan Scotland Paleogene dolerite
Tejeda Gran Canaria Miocene trachyte, phonolite
Vallehermoso La Gomera Miocene trachyte, phonolite
Jabal Arknu Libya Tertiary
Otoge Japan Miocene alkali basalt, trachyandesite
Zarza Mexico Cretaceous gabbro
Houshihushan China Cretaceous granite porphyry
Boa Vista Cape Verde Miocene phonolite
Ruri Hills Kenya Miocene carbonatite
Bagstowe Queensland late Paleozoic rhyolite
Thverartindur Iceland Pliocene
Tehilla Sudan Cambrian, Ordovician granite, monzonite
Closer view of a cone sheet at Mingary, Ardnamurchan
Closer view of a cone sheet at Mingary, Ardnamurchan

02Formation

Soon after cone sheets were first described, their formation was explained in terms of intrusion along conical fractures extending from the top of an intrusive body into the overlying rocks, caused by high magmatic pressure.

Tejeda cone sheets on Gran Canaria. The lower two-thirds of the photo shows the Tejeda cone sheet swarm of Miocene age; the cone sheets dip down towards the bottom left. The cone sheets are overlain by Pliocene flat-lying lava flows and pyroclastic rocks.
Tejeda cone sheets on Gran Canaria. The lower two-thirds of the photo shows the Tejeda cone sheet swarm of Miocene age; the cone sheets dip down towards the bottom left. The cone sheets are overlain by Pliocene flat-lying lava flows and pyroclastic rocks.
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Sources and credits

This article is adapted from the Wikipedia article Cone sheet, written by its contributors and licensed under CC BY-SA 4.0. Fathomly has changed the layout, removed citation markers, navigation and maintenance notices, and adjusted punctuation. This adapted version is shared under the same license. For references, see the original article.

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