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Ignimbrite volcanism in North Wales

  • Première Partie Communications Presentées Au « International Symposium On Volcanology » (Nouvelle-Zélande, Du 22 Nov. À 3 Déc. 1965)
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Abstract

Many episodes of ignimbrite volcanism have occurred in North Wales. Ignimbrites can be recognised amongst the Pre-Cambrian rocks and from almost every stage of the Ordovician succession. The best known and most instructively exposed ignimbrite volcanies are those of Caradocian age in Snowdonia. In this deeply incised mountainous area it is possible to demonstrate the major characteristics of ignimbrite volcanism and to examine the relationship between numerous intrusive rhyolite masses and the extrusive rocks. Both acid and basic magmas were available in North Wales during Ordovician times, and at several of the volcanic centres the rocks show a differentiation sequence from pyroxeneandesite to alkali-rhyolite. The emergence and growth of volcanic islands upon which the ignimbrites were deposited is revealed in the stratigraphical record. An intimate relationship exists between magmatism and crustal unrest, and it is possible to discuss certain problems regarding the petrogenesis of the rocks, the location and character of the volcanic vents and the palaeogeography of North Wales during the Ordovician. Definition of the terms employed and criteria used in the identification of Welsh ignimbrites is given, and the field relationships and petrology of a number of areas are described in detail.

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  1. Birkbeck College, London

    F. J. Fitch

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Fitch, F.J. Ignimbrite volcanism in North Wales. Bull Volcanol 30, 199–219 (1967). https://doi.org/10.1007/BF02597669

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