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"Tsunami or storm? A high-level coastal boulder field on the southern t" by R. P. Bourman, C. V. Murray-Wallace et al. - Vimarsana News

"Tsunami or storm? A high-level coastal boulder field on the southern t" by R. P. Bourman, C. V. Murray-Wallace et al.

A high-level coastal boulder field at Whalers Way, southern Eyre Peninsula, South Australia, occurs at elevations of 20–30 m above present sea-level on a gently seaward-sloping, karst-weathered calcrete-capped structural bench, formed on the Upper Pleistocene Bridgewater Formation and underlying Carnot Gneisses (Archean–Paleoproterozoic Sleaford Complex). More than 1000 ex situ boulders, cobbles and pebbles of gneiss and mafic igneous rocks, as well as fragments of calcrete, occur within the boulder field and cover an area >6000 m2. All the crystalline rock clasts are derived locally fr...

Source: uow.edu.au
"Late Pleistocene evolution of Robe Range, southern Australia – The tim" by Rahmadi Hidayat, Colin V. Murray-Wallace et al. - Vimarsana News

"Late Pleistocene evolution of Robe Range, southern Australia – The tim" by Rahmadi Hidayat, Colin V. Murray-Wallace et al.

Robe Range is a coastal barrier that extends for over 155 km along the modern coastline of the Coorong Coastal Plain in southern Australia, a region renowned as preserving one of the world's longest records of Quaternary eolian dune deposition. Previous research has shown that the late Pleistocene dune development in this barrier structure is linked with sea-level highstands, particularly warm interstadials of marine isotope stage (MIS) 5. To better understand the principal depositional phases and sediment provenance of the dune successions of Robe Range, we use a combination of amino aci...

Source: uow.edu.au