Geology of Tindfjallajökull volcano, Iceland

The geology of Tindfjallajökull volcano, southern Iceland, is presented as a 1:50,000 scale map. Field mapping was carried out with a focus on indicators of past environments. A broad stratocone of interbedded fragmental rocks and lavas was constructed during Tindfjallajökull’s early development. Th...

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Main Authors: Jonathan D. Moles, Dave McGarvie, John A. Stevenson, Sarah C. Sherlock
Format: Article
Language:English
Published: Taylor & Francis Group 2018-11-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2018.1425163
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author Jonathan D. Moles
Dave McGarvie
John A. Stevenson
Sarah C. Sherlock
author_facet Jonathan D. Moles
Dave McGarvie
John A. Stevenson
Sarah C. Sherlock
author_sort Jonathan D. Moles
collection DOAJ
description The geology of Tindfjallajökull volcano, southern Iceland, is presented as a 1:50,000 scale map. Field mapping was carried out with a focus on indicators of past environments. A broad stratocone of interbedded fragmental rocks and lavas was constructed during Tindfjallajökull’s early development. This stratocone has been dissected by glacial erosion and overlain by a variety of mafic to silicic volcanic landforms. Eruption of silicic magma, which probably occurred subglacially, constructed a thick pile of breccia and lava lobes in the summit area. Mafic to intermediate flank eruptions continued through to the end of the last glacial period, producing lavas, hyaloclastite-dominated units and tuyas that preserve evidence of volcano-ice interactions. The Thórsmörk Ignimbrite, a regionally important chronostratigraphic marker, is present on the SE flank of the volcano. The geological mapping of Tindfjallajökull gives insights into the evolution of stratovolcanoes in glaciated regions and the influence of ice in their development.
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spelling doaj.art-de49e60686df45349fd5b012795f11182022-12-21T19:20:16ZengTaylor & Francis GroupJournal of Maps1744-56472018-11-01142223110.1080/17445647.2018.14251631425163Geology of Tindfjallajökull volcano, IcelandJonathan D. Moles0Dave McGarvie1John A. Stevenson2Sarah C. Sherlock3The Open UniversityThe Open UniversityBritish Geological Survey, The Lyell CentreThe Open UniversityThe geology of Tindfjallajökull volcano, southern Iceland, is presented as a 1:50,000 scale map. Field mapping was carried out with a focus on indicators of past environments. A broad stratocone of interbedded fragmental rocks and lavas was constructed during Tindfjallajökull’s early development. This stratocone has been dissected by glacial erosion and overlain by a variety of mafic to silicic volcanic landforms. Eruption of silicic magma, which probably occurred subglacially, constructed a thick pile of breccia and lava lobes in the summit area. Mafic to intermediate flank eruptions continued through to the end of the last glacial period, producing lavas, hyaloclastite-dominated units and tuyas that preserve evidence of volcano-ice interactions. The Thórsmörk Ignimbrite, a regionally important chronostratigraphic marker, is present on the SE flank of the volcano. The geological mapping of Tindfjallajökull gives insights into the evolution of stratovolcanoes in glaciated regions and the influence of ice in their development.http://dx.doi.org/10.1080/17445647.2018.1425163TindfjallajökullTindfjöllvolcanoIcelandvolcano-ice interactions
spellingShingle Jonathan D. Moles
Dave McGarvie
John A. Stevenson
Sarah C. Sherlock
Geology of Tindfjallajökull volcano, Iceland
Journal of Maps
Tindfjallajökull
Tindfjöll
volcano
Iceland
volcano-ice interactions
title Geology of Tindfjallajökull volcano, Iceland
title_full Geology of Tindfjallajökull volcano, Iceland
title_fullStr Geology of Tindfjallajökull volcano, Iceland
title_full_unstemmed Geology of Tindfjallajökull volcano, Iceland
title_short Geology of Tindfjallajökull volcano, Iceland
title_sort geology of tindfjallajokull volcano iceland
topic Tindfjallajökull
Tindfjöll
volcano
Iceland
volcano-ice interactions
url http://dx.doi.org/10.1080/17445647.2018.1425163
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AT sarahcsherlock geologyoftindfjallajokullvolcanoiceland