Encyclopedia of the World's Coastal Landforms

2010 Edition
| Editors: Eric C. F. Bird

Tasmania

  • Joanna Ellison
Reference work entry
DOI: https://doi.org/10.1007/978-1-4020-8639-7_242

Introduction

While the main island of Tasmania lies between 39° 40ʹ and 43° 20ʹ S, this only island state of Australia extends nearly to the Victoria coastline because it includes the large Bass Strait Islands of King and Flinders, as well as 233 smaller islands (Brothers et al. 2001) and the southern outlier Macquarie Island at 54° 30ʹ S. As an island state Tasmania has more coastline per unit land area than others, with a total coastal length of 6,473 km, excluding Macquarie Island, and no location more than 115 km from the coast. The main island coastline, some 2,236 km in length, exhibits strong contrasts in environmental geomorphology in response to wide variations in geological structure and exposure.

Coastal Morphology of Tasmania

Tasmania has a cool temperate climate, with prevailing winds and swell approaching from the west and southwest, which can be of very high energy owing to storm generation on the Antarctic Polar Front and uninterrupted fetch. The swell is refracted...

Keywords

Fault Scarp East Australian Current Sand Barrier Longitudinal Dune Drown River Valley 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
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References

  1. Bowden AR (1983) Relict terrestrial dunes: Legacies of a former climate in coastal northeastern Tasmania. Z Geomorphol Suppl. (Bd) 45:153–174Google Scholar
  2. Bowden AR, Colhoun EA (1984) Quaternary emergent shorelines of Tasmania. In: Thom BG (ed) Coastal geomorphology in Australia. Sydney, Academic Press, pp 313–342Google Scholar
  3. Brothers N, Pemberton M, Pryor H, Halley V (2001) Tasmania's offshore islands: seabirds and other natural features. Tasmanian Museum and Art Gallery, Hobart, 643pGoogle Scholar
  4. Davies JL (1985) Tasmania. In: Bird EC, Schwartz M (eds) The World's Coastline. Van Rostrand Reinhold, New York, pp 975–979Google Scholar
  5. Davies JL, Hudson JP (1987) Sources of shore sediment on the North Coast of Tasmania. Pap Proc R Soc Tasman 121:137–150Google Scholar
  6. Edgar GJ, Barrett NS, Graddon DJ (2000) A classification of Tasmanian estuaries and assessment of their conservation significance: An analysis using ecological and physical attributes, population and landuse. Report to environment Australia from Tasmanian parks and wildlife serviceGoogle Scholar
  7. Kershaw RC, Sutherland FL (1972) Quaternary geomorphology of Flinders Island. Rec Queen Vic Mus Launceston 43:1–28Google Scholar
  8. Locher H (1997) Mount Lyall remediaton. Sediment transport in the King River, Tasmania. Supervising Scientist Report, Canberra 120:124Google Scholar
  9. Short AD (2006) Beaches of the Tasmanian coast and islands: a guide to their nature, characteristics, surf and safety. Coastal studies Unit and Surf Life Saving Australia Ltd, University of Sydney, 353pGoogle Scholar

Copyright information

© Springer Science+Business Media B.V. 2010

Authors and Affiliations

  • Joanna Ellison
    • 1
  1. 1.University of TasmaniaLauncestonTasmania