DEEP SANDS
Midway along the Highway from Melbourne to Adelaide, between Nhill and Kaniva, the road crosses a series of parallel sandhills. Lawloit Ridge is the steepest of these phenomena, which are actually "stranded coastal dunes". They are remnants of a geological past when much of the Murray-Darling Basin lay under the Southern Ocean. It was a time when global sea levels fluctuated according to a climatic cycle. Over millions of years, they fell when polar ice sheets froze (glacials) and rose when polar ice sheets melted (interglacials). The last period when marine flooding of southeastern Australia reached its maximum was approximately 6 million years ago (MYA). 1. 2018, 'Mallee Dunefields of the Murray-Darling Basin', ecological associates pty ltd, Kerang Vic. 2. 2016, CV Murray-Wallace, Coastal Landscapes of South Australia , Adel Univ Press, p 149. 3. 2022, Wimmera Catchment Management Authority, <wcma.vic.gov.au> Since that peak, the ocean has periodically ...