Parmelia Bank
Parmelia Bank, south of Success Bank, is a slightly smaller bank than the latter and runs approximately parallel to it, about 3 kilometres (1.9 mi) further south extending from Woodman Point, almost to Carnac Island; it also is within the designated Fremantle Outer Harbour. The channel through this bank is likewise named after the bank – Parmelia Channel that leads into Cockburn Sound.
During World War II, Parmelia Bank was the location of the anti-submarine boom net protecting the northern access to Cockburn Sound. From Woodman Point, the barrier ran west on top of the bank, stretching to Carnac Island. A dredged channel, the location of a gate in the barrier, let through the sandbank into Cockburn Sound. From this channel, the barrier ran south-west to Garden Island.
The Success and Parmelia Banks were formed during the Holocene, more than 10,000 years ago, through the deposition of sediment which had been eroded from the Rottnest Shelf and the Garden Island Ridge. Success Bank was formed in the lee of Mewstone Rocks while Parmelia Bank was formed in lee of Carnac Island.
References
- ^ D.A. Lord and Associates; Cockburn Cement Limited (1998), Sedimentology of Success and Parmelia Banks, Owen Anchorage (Western Australia) : summary report, Cockburn Cement, ISBN 978-1-876476-06-9
- ^ In the spotlight (Plaque at John Point, Point Peron). Cape Peron.
- ^ Oceanica Consulting Pty Ltd & The University of Western Australia (November 2011). Sand Colour of Owen Anchorage Beaches (PDF) (Report). p. 4. Retrieved 24 May 2020.
