Abstract
The southern continental margin of Australia today has been much the same throughout the late Cenozoic and so the Holocene depositional system is a continuation of one that has been in place for ~2 my. It has been dominated by strong SW winds that drive high-energy waves and swells directly onto exposed coasts. The climate, however, has become progressively drier since the mid-Pliocene such that much of southern Australia is today semi-arid. Exceptions are the Albany coast and the somewhat mountainous coasts of southern Victoria and Tasmania. This chapter is a documentation of the suite of modern marine depositional environments that are present across the continental margin.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsAuthor information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2010 Springer Science+Business Media B.V.
About this chapter
Cite this chapter
James, N.P., Bone, Y. (2010). Neritic Depositional Environments. In: Neritic Carbonate Sediments in a Temperate Realm. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-9289-2_7
Download citation
DOI: https://doi.org/10.1007/978-90-481-9289-2_7
Published:
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-9288-5
Online ISBN: 978-90-481-9289-2
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)