Use this URL to cite or link to this record in EThOS:
Title: Subglacial rhyolite volcanism at Torfajokull, Iceland
Author: Tuffen, Hugh
ISNI:       0000 0001 3537 6022
Awarding Body: Open University
Current Institution: Open University
Date of Award: 2001
Availability of Full Text:
Access from EThOS:
Access from Institution:
Subglacial rhyolite eruptions at Torfajokull, Iceland have produced a variety of volcanic edifices during the last glacial period (115-11 ka). These range from small-volume (< 0.1 km3) volcanoes, such as Bhlhnukur and Dalakvislfell, to larger volume (-1 km3) flat-topped tuyas such as South-east Rauoufossafjoll. Lithofacies associations at each volcano record distinct phases of volcano-ice interaction beneath temperate glaciers at least 350 m thick. All eruptions began with the construction of a pile of glassy fragmental material within a subglacial cavity. Fragmentation at Bhlhnukur was primarily caused by quenching, when rising magma encountered meltwater. Fragmentation at Southeast Rauoufossafjoll was apparently more energetic, and generated phreatomagmatic ash over 300 m thick. Dalakvisl is intermediate between the other two localities. Most fragmental deposits are massive, suggesting that a sustained meltwater lake did not develop during eruptions, in contrast with evidence from many basaltic volcanoes. Instead, meltwater drained away in a number of discrete channels, some of which have been identified. The eruption at Blahnukur apparently terminated before the glacier surface had been pierced, whereas the eruption at South-east Rau6ufossafjoll produced a cap of flat-lying subaerial lava flows about 1.5 km in length. Numerical models are presented, in which simple patterns of ice melting and deformation are used to simulate the evolving size of subglacial cavities during eruptions. The radius of the cavity is compared to the radius of the growing subglacial volcano. The models predict that, at low magma discharge rates and beneath thick ice, cavities will become completely filled with volcanic debris and the eruption will be dominantly intrusive, forming the types of lithologies observed at Blahnukur. Cavities never become filled at higher magma discharge rates, and an explosive phreatomagmatic eruption is predicted, which would form the types of lithologies observed at South-east Rauoufossafjol1.
Supervisor: Not available Sponsor: Not available
Qualification Name: Thesis (Ph.D.) Qualification Level: Doctoral