posted on 2023-11-02, 06:13authored byRJ Ford, EA Colhoun, MR Banks, E Williams
On Tasman Peninsula, south-eastern Tasmania, almost horizontal Permian marine and Triassic non-marine rocks were intruded by Jurassic dolerite, faulted and overlain by Tertiary basalt Marine processes operating on the Jurassic and older rocks have produced a cliffed coastline with many erosional features widely noted for their grandeur and rarity. These features form a self-renewing economic asset.
History
Publication title
Papers & Proceedings of the Royal Society of Tasmania
Volume
Tasman
Pagination
07-24
ISSN
0080-4703
Rights statement
Edited by S.J. Smith. - Copyright Royal Society of Tasmania.