Abstract
The west coast of TAS is the most exposed on the Australian coast. It has a humid cool temperate climate and is exposed to the full force of the Southern Ocean westerly waves and winds which batter the predominately rocky shore. The 700 km long coast extends from Tasmania’s southern tip at South East Cape to the northwestern tip at Woolnorth Point and includes the western coast of King Island. It is a sparcely developed coast, with the southern half located in national parks and conservation areas and little development elsewhere. A few small rivers reach the coast and sediment and are predominately quartz-rich. Waves average 2–4 m, and tides are micro resulting in entirely wave-dominated beaches. Most beaches are embayed between rocky sections and average only 0.6 km in length, with many also sheltered in rocky bays resulting in lower-energy beach states. Barriers back a quarter of the rocky shore and are predominately transgressive dunes with a few small regressive systems in sheltered areas. This chapter described the coast, its beaches, barriers, sediment transport and sediment compartments.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Davies JL (1973) Sediment movement on the Tasmanian coast. In: 1st Australian conference on coastal and ocean engineering, Sydney, Institution of Engineers Australia, pp 43–47
Davies JL (1978) Beach sand and wave energy in Tasmania. In: Davies JL, Williams MAJW (eds) Landform evolution in Australasia. Australian National University Press, Canberra, pp 158–167
Kalma JD, Chin AK (1988) Windspeed maps for Tasmania and their use in wind energy assessment. Aust Geogr Stud 26:264–278
Jennings JN (1957a) Coastal dune lakes as exemplified from King Island, Tasmania. Geogr J 123:59–70
Jennings JN (1957b) On the orientation of parabolic or U-dunes. Geogr J 123:474–489
Jennings JN (1959) The coastal geomorphology of King Island, Bass Strait in relation to changes in the relative level of land and sea. Record Queen Vict Mus, Launceston 11:1–39
Jennings JN (1961) Sea level changes in King Island, Bass Strait. Zeitschrift für Geomorphologie 3:80–84
Jennings JN (1967a) Clifftop dunes on King Island: Australian Geographer
Jennings JN (1967b) Clifftop dunes. Aust Geogr Stud 5:40–49
Murray-Wallace C, Goede A (1995) Aminostratigraphy and electron spin reconnaissance dating of quaternary coastal neotectonism in Tasmania and Bass Strait islands. Aust J Earth Sci 42:51–67
Short AD (2006) Beaches of the Tasmanian coast and islands. Sydney University Press, Sydney, 353 p
Tasmania Govt (2016) Coastal hazards technical report: mitigating natural hazards through land use planning and building control. Department of Premier and Cabinet, Tasmanian Government, Hobart, 125 p
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 2020 Springer Nature Switzerland AG
About this chapter
Cite this chapter
Short, A.D. (2020). West Tasmania Region. In: Australian Coastal Systems. Coastal Research Library, vol 32. Springer, Cham. https://doi.org/10.1007/978-3-030-14294-0_23
Download citation
DOI: https://doi.org/10.1007/978-3-030-14294-0_23
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-030-14293-3
Online ISBN: 978-3-030-14294-0
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)