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Marion Island volcanism and glaciation

Published online by Cambridge University Press:  22 November 2010

Kevin Hall ,
Ian Meiklejohn  and
Adam Bumby
Kevin Hall*
Affiliation:
Department of Geography, Geoinformatics and Meteorology, University of Pretoria, Pretoria 0002, South Africa
Ian Meiklejohn
Affiliation:
Department of Geography, Geoinformatics and Meteorology, University of Pretoria, Pretoria 0002, South Africa
Adam Bumby
Affiliation:
Department of Geology, University of Pretoria, Pretoria 0002, South Africa
*
hall@unbc.ca
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Abstract

Sub-Antarctic Marion Island was the site of extensive volcanism as well as glaciation during both the Quaternary and the Holocene. Initial reconstructions suggested a link between deglaciation and the initiation of faulting which, in turn, facilitated lava eruptions during the interglacials. However, our reassessment of the faulting, volcanic rock, and palaeoglacier distribution indicate that these original interpretations were erroneous. Features thought to be due to faulting are shown to be erosional scarps and this significantly changes interpretations of former glacier distribution. Further, the loss of the former ice cap has revealed new information on former glaciers and their flow directions, thereby allowing reconstruction of palaeoglaciers. Our new reconstruction fits with information from invertebrate genetic mapping that suggest some lava outcrops were nunataks and, therefore, refuges during the Last Glacial period. The new findings of glacial landforms in areas previously covered by snow suggest there was a significant ice advance during the Little Ice Age. Although Holocene volcanic rocks overlie and mask much of the glacial evidence, it has been possible to develop a proposed new reconstruction for glaciation, which is presented together with some of the implications.

Keywords

faultingglacier reconstructionglacier-volcanic interactionspalaeoclimateperi-Antarctic islands
Type
Earth Sciences
Information
Antarctic Science , Volume 23 , Issue 2 , April 2011 , pp. 155 - 163
Copyright
Copyright © Antarctic Science Ltd 2010

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Footnotes

2

Current address: Geography Programme, University of Northern British Columbia, 3333 University Way, Prince George, British Columbia V2N 4Z9, Canada

4

Current address: Department of Geography, Rhodes University, PO Box 94, Grahamstown 6140, South Africa

References

Anderson, E.M. 1951. The dynamics of faulting. Edinburgh: Oliver & Boyd, 206 pp.Google Scholar
Boelhouwers, J.C., Meiklejohn, K.I., Holness, S. Hedding, D.W. 2008. Geology, geomorphology and climate change. In Chown, S.L. & Froneman, P.W., eds. The Prince Edward Islands: land-sea interactions in a changing ecosystem. Stellenbosch: African Sun Media, 65–96.CrossRefGoogle Scholar
Carrivick, J.L., Russell, A.J., Rushmer, E.L., Tweed, F.S., Marren, P.M., Deeming, H. Lowe, O.J. 2009. Geomorphological evidence towards a de-glacial control on volcanism. Earth Surface Processes and Landforms, 34, 1164–1178.CrossRefGoogle Scholar
Chevallier, L., Verwoerd, W.J., Bova, P., Stettler, E., Du Plessis, A., Du Plessis, J.G., Fernandez, L.M. Nel, M. 1992. Volcanological features and preliminary geophysical investigations on Marion Island. South African Journal of Antarctic Research, 22, 15–35.Google Scholar
Chief Directorate, Surveys & Mapping. 2005. Marion Island. 1:25 000. Provisional map, May 2005. Mobray: Chief Directorate, Surveys & Mapping.Google Scholar
Chown, S.L. Froneman, P.W. eds. 2008. The Prince Edward Islands: land-sea interactions in a changing ecosystem. Stellenbosch: African Sun Media, 470 pp.CrossRefGoogle Scholar
Grove, E.W. 1974. Deglaciation - a possible triggering mechanism for recent volcanism. In Gonzalez-Ferran, O., ed. Proceedings of the Symposium on Andean and Antarctic Volcanology Problems. Rome: IAVCEI, 88–97.Google Scholar
Hall, K.J. 1978a. Evidence for Quaternary glaciation of Marion Island (sub-Antarctic) and some implications. In Van Zinderen Bakker, E.M., ed. Antarctic glacial history and world palaeoenvironments. Rotterdam: Balkema, 137–147.Google Scholar
Hall, K.J. 1978b. Quaternary glacial geology of Marion Island. PhD thesis, University of the Orange Free State, 369 pp. [Unpublished.]Google Scholar
Hall, K.J. 1979. Late glacial ice cover and palaeotemperatures on sub-Antarctic Marion Island. Palaeogeography, Palaeoclimatology, Palaeoecology, 29, 143–159.CrossRefGoogle Scholar
Hall, K.J. 1982. Rapid deglaciation as an initiator of volcanic activity: an hypothesis. Earth Surface Processes and Landforms, 7, 45–51.CrossRefGoogle Scholar
Hall, K.J. 1983. A reconstruction of the Quaternary ice cover of Marion Island. In Oliver, R.L., James, P.R. & Jago, J.B., eds. Antarctic earth science. Canberra: Australian Academy of Science & Cambridge: Cambridge University Press, 461–464.Google Scholar
Hall, K.J. 2004. Quaternary glaciations of the sub-Antarctic islands. In Ehlers, J. & Gibbard, P.C., eds. Quaternary glaciations: extent and chronology. Part III: South America, Asia, Africa, Australia, Antarctica. Amsterdam: Elsevier, 339–346.Google Scholar
Hambrey, M.J., Smellie, J.L., Nelson, A.E. Johnson, J.S. 2008. Late Cenozoic glacier-volcano interaction on James Ross Island and adjacent areas, Antarctic Peninsula region. Geological Society of America Bulletin, 120, 709–731.CrossRefGoogle Scholar
Lescinsky, D.T. Fink, J.H. 2000. Lava and ice interaction at stratovolcanoes: use of characteristic features to determine past glacial extents and future volcanic hazards. Journal of Geophysical Research, 105, 23 711–23 726.CrossRefGoogle Scholar
Lescinsky, D.T. Sisson, T.W. 1998. Ridge-forming, ice-bounded lava flows at Mount Rainier, Washington. Geology, 26, 351–354.2.3.CO;2>CrossRefGoogle Scholar
Lodge, R.W.D. Lescinsky, D.T. 2009. Fracture patterns at lava-ice contacts on Kokostick Butte, OR, and Mazama Ridge, Mount Rainier, WA: implications for flow emplacement and cooling histories. Journal of Volcanology and Geothermal Research, 185, 298–310.CrossRefGoogle Scholar
McDougall, I. 1971. Geochronology. In Van Zinderen Bakker, E.M., Winterbottom, J.M. & Dyer, R.A., eds. Marion and Prince Edward Islands. Cape Town: Balkema, 72–77.Google Scholar
McDougall, I., Verwoerd, W. Chevalier, L. 2001. K–Ar geochronology of Marion Island, Southern Ocean. Geological Magazine, 138, 1–17.CrossRefGoogle Scholar
Means, W.D. 1987. A newly recognized type of slickenside striation. Journal of Structural Geology, 9, 585–590.CrossRefGoogle Scholar
Meiklejohn, K.I. Smith, V.R. 2008. Surface areas of altitudinal zones on sub-Antarctic Marion Island. Polar Biology, 31, 259–261.CrossRefGoogle Scholar
Nel, W., Holness, S. Meiklejohn, K.I. 2003. Observations on rapid mass movement on sub-Antarctic Marion Island. South African Journal of Science, 99, 177–181.Google Scholar
Pagli, C., Sigmundsson, F., Pedersen, R., Einarsson, P., Árnadóttir, T. Feigl, K.L. 2007a. Crustal deformation associated with the 1996 Gjálp subglacial eruption, Iceland: InSAR studies in affected areas adjacent to the Vatnajökull ice cap. Earth and Planetary Science Letters, 259, 24–33.CrossRefGoogle Scholar
Pagli, C., Sigmundsson, F., Lund, B., Sturkell, E., Geirsson, H., Einarsson, P., Árnadóttir, T. Hreinsdóttir, S. 2007b. Glacio-isostatic deformation around the Vatnajökull ice cap, Iceland, induced by recent climate warming: GPS observations and finite element modelling. Journal of Geophysical Research, 112, 10.1029/2006JB004421.CrossRefGoogle Scholar
Peacock, D.C.P. Parfitt, E.A. 2002. Active relay ramps and normal fault propagation on Kilauea Volcano, Hawaii. Journal of Structural Geology, 24, 729–742.CrossRefGoogle Scholar
Schalke, H.J.W.G. van Zinderen Bakker, E.M. 1971. History of the vegetation. In Van Zinderen Bakker, E.M., Winterbottom, J.M. & Dyer, R.A., eds. Marion and Prince Edward Islands. Cape Town: Balkema, 89–99.Google Scholar
Smellie, J.L. 2000. Subglacial eruptions. In Sigurdsson, H., ed. Encyclopedia of volcanoes. San Diego, CA: Academic Press, 403–418.Google Scholar
Smellie, J.L. 2001. Lithofacies architecture and construction of volcanoes in englacial lakes: Icefall Nunatak, Mount Murphy, eastern Marie Byrd Land, Antarctica. In White, J.D.L. & Riggs, N., eds. Lacustrine volcaniclastic sedimentation. International Association of Sedimentologists, Special Publications, 30, 73–98.Google Scholar
Smellie, J.L. 2002. The 1969 subglacial eruption on Deception Island (Antarctica): events and processes during an eruption beneath a thin glacier and implications for volcanic hazards. In Smellie, J.L. & Chapman, M.G., eds. Volcano-ice interaction on Earth and Mars. Geological Society, London, Special Publications, No. 202, 59–79.Google Scholar
Sumner, P.D., Meiklejohn, K.I., Boelhouwers, J.C. Hedding, D.W. 2004. Climate change melts Marion Island snow and ice. South African Journal of Science, 100, 395–398.Google Scholar
Twiss, R.J. Moores, E.M. 1992. Structural geology. New York: W.H. Freeman, 532 pp.Google Scholar
Van Zinderen Bakker, E.M., Winterbottom, J.M. Dyer, R.A. 1971. Marion and Prince Edward Islands. Cape Town: Balkema, 427 pp.Google Scholar
Verwoerd, W.J. 1971. Geology. In Van Zinderen Bakker, E.M., Winterbottom, J.M. & Dyer, R.A., eds. Marion and Prince Edward Islands. Cape Town: Balkema, 40–61.Google Scholar