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  1. Australia lay beneath an ice cap at the start of the Permian and Victoria was swathed in a slow-moving ice-sheet. As the ice retreated, forests developed with Glossopteris (seed ferns), tree-ferns, club-mosses and horsetails.

  2. Jul 31, 2008 · As the Late Palaeozoic continental ice sheet covering most of Victoria retreated in the late Sakmarian, the inland sea along its northern margin expanded southwards into central Victoria to...

  3. Victoria lay at a high latitude in the Permian, and adjacent parts of Gondwana were covered by continental ice sheets during this period. Deposits of glacial and fluvioglacial origin are scattered around the state, with outcrops around Coleraine in the west and Bacchus Marsh and Derrinal in central Victoria.

  4. As the Late Palaeozoic continental ice sheet covering most of Victoria retreated in the late Sakmarian, the inland sea along its northern margin expanded southwards into central Victoria to deposit a well-exposed sequence of glaciomarine strata (the upper part of the Bacchus Marsh Formation) at Bald Hill near Bacchus Marsh.

  5. May 8, 2023 · Victoria's geology. Victoria has a rich supply of earth resources including gold, oil and gas, mineral sands, base metals and brown coal. Our economic and social growth rely heavily on making the most of plentiful earth resources. Victoria's geological history dates back to one billion years ago.

  6. The focus of most Victorian Permian studies has been the continental glacial sediments, but the volumetrically minor glaciomarine strata in central Victoria are worthy of attention, because they...

  7. Jul 31, 2008 · An unusual sediment accumulation in the glaciogene Permian near Bacchus Marsh, Victoria, is interpreted as representing the development and infilling of a subglacial channel.