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Denudation chronology from cave and river terrace levels: the case of the Buchan Karst, southeastern Australia

Published online by Cambridge University Press:  01 May 2009

J. A. Webb ,
D. Fabel ,
B. L. Finlayson ,
M. Ellaway ,
Li Shu  and
H.-P. Spiertz
J. A. Webb
Affiliation:
Department of Geology, La Trobe University, Bundoora, Victoria 3083, Australia
D. Fabel
Affiliation:
Department of Geography, Melbourne University, Parkville, Victoria 3052, Australia
B. L. Finlayson
Affiliation:
Department of Geography, Melbourne University, Parkville, Victoria 3052, Australia
M. Ellaway
Affiliation:
Department of Geography, Melbourne University, Parkville, Victoria 3052, Australia
Li Shu
Affiliation:
Department of Geography, Melbourne University, Parkville, Victoria 3052, Australia
H.-P. Spiertz
Affiliation:
Department of Geography, Rheinische Friedrich-Wilhelms University, 5300 Bonn, Germany
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Abstract

Detailed mapping of surface and underground karst features at Buchan, in eastern Victoria, has shown that the three river terraces along the Buchan River can be correlated with three levels of epiphreatic development in the nearby caves. Each level represents a stillstand in the denudational history of the area. Uranium series dating of speleothems and palaeomagnetic studies of cave sediments indicate that all three stilistands are more than 730 ka old. The periods of incision separating the stillstands were probably the result of active tectonic uplift. This contrasts with some northern parts of the Southeastern Highlands, which have been stable since the Eocene. The overall amount of incision and uplift at Buchan is small, indicating that the majority of scarp retreat in this section of the highlands must have occurred earlier. The denudation history of the Buchan area over the last 730 ka has seen only 2–3 m of incision, despite the major climatic and sea-level changes that have occurred in that time. Whereas most karst landscapes in the Northern Hemisphere have been extensively modified during the late Pleistocene, the Buchan karst was little affected, and its geomorphology has an older origin.

Type
Articles
Information
Geological Magazine , Volume 129 , Issue 3 , May 1992 , pp. 307 - 317
Copyright
Copyright © Cambridge University Press 1992

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References

Andrews, E. C. 1911. Geographical unity of eastern Australia in late and post Tertiary time, with applications to biological problems. Journal and Proceedings of the Royal Society of New South Wales 44, 420–80.Google Scholar
Bishop, P. 1988. The eastern highlands of Australia: the evolution of an intraplate highland belt. Progress in Physical Geography 12, 159–82.Google Scholar
Browne, W. R. 1969. Geomorphology. General notes. Journal of the Geological Society of Australia 16, 559–69.Google Scholar
Chappell, J. 1983. A revised sea-level record for the last 300,000 years from Papua New Guinea. Search 14, 99–101.Google Scholar
Connolly, M. R. & Francis, G. 1979. Cave and landscape evolution at Isaacs Creek, New South Wales. Helictite 17, 5–24.Google Scholar
Droppa, A. 1966. The correlation of some horizontal caves with river terraces. Studies in Speleology 1, 186–92.Google Scholar
Ek, C. 1961. Conduits souterrains en relation avec les terraces fluviales. Annales de la Sociótó Géologique de Belgique 81, 313–40.Google Scholar
Faure, G. 1986. Principles of Isotope Geology, 2nd ed. New York: John Wiley, 589 pp.Google Scholar
Ford, D. C. & Williams, P. W. 1989. Karst Geomorphology and Hydrology. London: Unwin Hyman, 601 pp.CrossRefGoogle Scholar
Ford, D. C., Gascoyne, M. & Bech, J. S. 1983. Speleothem dates and Pleistocene chronology in the Peak district, Derbyshire. Transactions of the British Cave Research Association 10, 103–15.Google Scholar
Hart, M. G. 1986. Geormorphology–Pure and Applied. London: Allen & Unwin, 228 pp.Google Scholar
Hills, E. S. 1975. The Physiography of Victoria. Melbourne: Whitcombe & Tombs, 373 pp.Google Scholar
Jennings, J. N. 1985. Karst Geomorphology. Oxford: Black-well.Google Scholar
Jones, J. G. & Veevers, J. J. 1982. A Cainozoic history of Australia's southeast highlands. Journal of the Geological Society of Australia 29, 1–12.Google Scholar
Jones, J. G. & Veevers, J. J. 1983. Mesozoic origins and antecedents of Australia's eastern highlands. Journal of the Geological Society of Australia 30, 305–22.CrossRefGoogle Scholar
King, L. C. 1959. Denudation and tectonic relief of southeastern Australia. Transactions and Proceedings of the Geological Society of South Africa 62, 113–38.Google Scholar
Lambeck, K. & Stephenson, R. 1986. The post-Palaeozoic uplift history of southeastern Australia. Australian Journal of Earth Sciences 33, 253–70.Google Scholar
Matthews, P. G. (ed.) 1985. Australian Karst Index. Melbourne: Australian Speleological Federation Inc.Google Scholar
Moore, M. E., Gleadow, A. J. W. & Lovering, J. F. 1986. Thermal evolution of rifted continental margins: new evidence from fission tracks in basement apatites from southeastern Australia. Earth and Planetary Science Letters 78, 255–70.CrossRefGoogle Scholar
Ollier, C. D. 1982. The Great Escarpment of eastern Australia: tectonic and geomorphic significance. Journal of the Geological Society of Australia 29, 13–24.Google Scholar
Ollier, C. D. 1984. Weathering, 2nd ed. London: Longman, 270 pp.Google Scholar
Ollier, C. D. & Taylor, D. 1988. Major geomorphic features of the Kosciusko–Bega region. BMR Journal of Australian Geology and Geophysics 10, 357–62.Google Scholar
Palmer, A. 1989. Geomorphic history of the Mammoth Cave System. In Karst Hydrology–Concepts from the Mammoth Cave Area (eds White, W. B. & White, E. L.), pp. 317–37. New York: Van Nostrand Reinhold.CrossRefGoogle Scholar
Rose, J. 1982. The Melinau River and its terraces. Cave Science 9, 113–27.Google Scholar
Schumm, S. A. 1977. The Fluvial System. New York: John Wiley, 338 pp.Google Scholar
Sweeting, M. M. 1960. The caves of the Buchan area, Victoria, Australia. Zeitschrift für Geomorphologie, Supplementband 2, 81–91.Google Scholar
Talent, J. A. 1963. The Buchan Caves. Mines Department of Victoria Report no. 1963/35, 1–15.Google Scholar
Taylor, G., McQueen, I., Brown, M. C., Ollier, C. D. & Taylor, D. 1989. Major geomorphic features of the Kosciusko–Bega region; discussion and reply. BMR Journal of Australian Geology and Geophysics 11, 123–5.Google Scholar
Taylor, G., Truswell, E. M., McQueen, I. & Brown, M. C. 1990. Early Tertiary palaeogeography, land-form evolution and palaeoclimates of southern Monaro, New South Wales, Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 77, 127–43.Google Scholar
Turcotte, D. L. & Schubert, G. 1982. Geodynamics: Application of Continuum Physics to Geological Problems. New York: Wiley, 450 pp.Google Scholar
Vandenberg, A. H. M. & O'shea, P. J. 1981. Explanatory notes on the Bairnsdale 1: 250,000 geological map. Geological Survey of Victoria Report no. 65, 1–61.Google Scholar
Webb, J. A., Finlayson, B. L., Fabel, D. & Ellaway, M. 1991. The geomorphology of the Buchan karst–implications for the landscape history of the South-eastern Highlands of Australia. In The Cainozoic in Australia: a Re-appraisal of the Evidence (eds Williams, M. A. J.; DeDekker, P. and Kershaw, A. P.), pp. 210–34. Special Publication of the Geological Society of Australia no. 18.Google Scholar
Wellman, P. 1979. On the Cainozoic uplift of the southeastern Australian highlands. Journal of the Geological Society of Australia 26, 1–9.CrossRefGoogle Scholar
Wellman, P. 1987. Eastern Highlands of Australia; their uplift and erosion. BMR Journal of Australian Geology and Geophysics 10, 277–86.Google Scholar
White, W. B. & White, E. 1974. Base-level control of underground drainage in the Potomac River Basin. In Proceedings of the 4th Conference on Karst Geology and Hydrology (eds Rauch, H. W. and Werner, E.), pp. 41–53. Charleston: West Virginia Geological Survey.Google Scholar
Williams, P. W. 1982. Speleothem dates, Quaternary terraces and uplift rates in New Zealand. Nature 298, 257–60.CrossRefGoogle Scholar