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The Quaternary pyroclastic succession of southeast Tenerife, Canary Islands: explosive eruptions, related caldera subsidence, and sector collapse

R. J. BROWN^*, T. L. BARRY, M. J. BRANNEY^*,¶, M. S. PRINGLE and S. E. BRYAN

^* Geology Department, University of Leicester, University Road, Leicester LE1 7RH, UK
University of Cardiff (BAS/NIGL), Cardiff, Wales CF1 3YE, UK
SUERC/NSS Argon Facility, Scottish Enterprise Technology Park, Rankine Ave., East Kilbride G75 0QF, UK
Department of Earth Sciences, University of Queensland, St Lucia, Queensland 4072, Australia

^¶ Author for correspondence: mjb26{at}le.ac.uk

A much-revised Quaternary stratigraphy is presented for ignimbrites and pumice fall deposits of the Bandas del Sur, in southern Tenerife. New ⁴⁰Ar/³⁹Ar data obtained for the Arico, Granadilla, Fasnia, Poris, La Caleta and Abrigo formations are presented, allowing correlation with previously dated offshore marine ashfall layers and volcaniclastic sediments. We also provide a minimum age of 287 ± 7 ka for a major sector collapse event at the Güimar valley. The Bandas del Sur succession includes more than seven widespread ignimbrite sheets that have similar characteristics, including widespread basal Plinian layers, predominantly phonolite composition, ignimbrites with similar extensive geographic distributions, thin condensed veneers with abundant diffuse bedding and complex lateral and vertical grading patterns, lateral gradations into localized massive facies within palaeo-wadis, and widespread lithic breccia layers that probably record caldera-forming eruptions. Each ignimbrite sheet records substantial bypassing of pyroclastic material into the ocean. The succession indicates that Las Cañadas volcano underwent a series of major explosive eruptions, each starting with a Plinian phase followed by emplacement of ignimbrites and thin ash layers, some of co-ignimbrite origin. Several of the ignimbrite sheets are compositionally zoned and contain subordinate mafic pumices and banded pumices indicative of magma mingling immediately prior to eruption. Because passage of each pyroclastic density current was characterized by phases of non-deposition and erosion, the entire course of each eruption is incompletely recorded at any one location, accounting for some previously perceived differences between the units. Because each current passed into the ocean, estimating eruption volumes is virtually impossible. Nevertheless, the consistent widespread distributions and the presence of lithic breccias within most of the ignimbrite sheets suggest that at least seven caldera collapse eruptions are recorded in the Bandas del Sur succession and probably formed a complex, nested collapse structure. Detailed field relationships show that extensive ignimbrite sheets (e.g. the Arico, Poris and La Caleta formations) relate to previously unrecognized caldera collapse events. We envisage that the evolution of the nested Las Cañadas caldera is more complex than previously thought and involved a protracted history of successive ignimbrite-related caldera collapse events, and large sector collapse events, interspersed with edifice-building phases.

Key Words: ignimbrite • Tenerife • explosive eruptions • phreatomagmatism • Quaternary • volcanism

This article has been cited by other articles:

				J. KROCHERT and E. BUCHNER Age distribution of cinder cones within the Bandas del Sur Formation, southern Tenerife, Canary Islands Geological Magazine, March 1, 2009; 146(2): 161 - 172. [Abstract] [Full Text] [PDF]

				S. E. BRYAN Petrology and Geochemistry of the Quaternary Caldera-forming, Phonolitic Granadilla Eruption, Tenerife (Canary Islands) J. Petrology, August 1, 2006; 47(8): 1557 - 1589. [Abstract] [Full Text] [PDF]

				R.J. Brown and M.J. Branney Bypassing and diachronous deposition from density currents: Evidence from a giant regressive bed form in the Poris ignimbrite, Tenerife, Canary Islands Geology, May 1, 2004; 32(5): 445 - 448. [Abstract] [Full Text] [PDF]