Floodwaters riseThe deepest rocks in the vicinity of Phillip Island, indeed in Victoria, are related to the exposed fold belts of eastern Australia.1 These were deposited rapidly early during the global Flood (Genesis 6–8) under the ocean. There was a large volume and variety of materials deposited including fine silt, poorly sorted sand, and different types of volcanic lava. The basement areas are large and have been given different names depending on where they are exposed (figure 1). The deposits comprise many thousands of metres of sediments and volcanics including Cambrian greenstone, Ordovician greywacke, and coarser Silurian strata.
Tectonic movements in the earth’s crust compressed these deposits in an east-west direction, and uplifted them, producing huge faults and folds in the strata. The strata were pushed onto each other and shortened by the compression. Mineral laden fluids within the sediments squeezed out through faults and cracks and released their dissolved booty, including gold, in mineralization areas which are now mined.
These catastrophic tectonic movements generated huge volumes of molten rock, called magma, which was forced toward the surface where it collected in magma chambers within the sediment piles (called plutons, such as the granite pluton forming Cape Woolamai). Some magma broke through the surface and blasted over the landscape as volcanic eruptions. These rocks have been classified as Devonian.As the floodwaters continued to rise on the earth, sediment, ripped-up vegetation and the remains of animals were deposited onto different areas of the continent of Australia, areas that geologists call basins. These include the Galilee, Cooper and Bowen Basins in Queensland and the Sydney Basin in New South Wales (figure 2). It’s likely that these basins were connected and, even as the floodwaters were rising, channeled huge volumes of water off the continent and into the ocean to the east. In Queensland and New South Wales these rocks have been classified as Permian and Triassic. As the floodwaters continued to rise and the crust of the earth continued to move tectonically, the positions of the sedimentary basins changed. This, coupled with rising floodwaters meant that sediment, vegetation and animals were deposited over a much larger series of basins covering a large part of Eastern Australia (figure 3). These sediments now contain the water reservoir known as the Great Artesian Basin (figure 4). These rocks have been classified as Jurassic and Cretaceous in Queensland and New South Wales.
None of these large sedimentary basins is represented in Victoria.
Eventually the Floodwaters reached their peak. Then global large scale tectonic movements began to slowly lift the Australian continent relative to the surrounding ocean basins. This meant that the floodwaters started to flow off the continent into the oceans. They tended to move away from the middle of the continent toward the edges at right angles to the shoreline. The receding floodwaters first moved in huge sheets of great lateral extent. Later, after the land had partially drained, the floodwaters flowed in huge channels. This movement of water eroded the land, removing material from the centre and depositing it at the continental margins and continental shelves. Eventually the water was gone.
Geologists have recognized this period of erosion in Queensland and New South Wales and assigned it to the Tertiary period. The ocean basin sank downward to the east along a north-south hinge line that now forms the Great Dividing Range. The receding floodwaters therefore tended to flow from the west to the east into the Pacific Ocean.
However, in Victoria the ocean basins sank downward to the south (along a hinge that runs east-west in Victoria). The floodwaters from the north would have run in a southerly direction into Southern Ocean. These receding floodwaters initially planed the land in Victoria relatively flat and this is recognized as occurring from the Permian to the Jurassic.2In Victoria these receding floodwaters deposited sediments in basins at the edge of the Australian continent called the Otway Basin and Gippsland Basin (figure 5). Initially, when the flow of water was large during the Cretaceous, the Otway and Gippsland basins would have been connected but as the flow reduced the basins became separated.
While the floodwaters were receding, volcanic eruptions occurred, caused by tectonic movement of the earth that released molten lava and forced it to migrate through the earth to the surface. In Victoria these eruptions are known as the Older Volcanics and they cover most of Phillip Island. Similar basaltic eruptions occurred all the way up the east coast of Australia into far north Queensland.
In the northern states very little sediment was deposited after these eruptions (although much erosion continued to take place). However, in Victoria abundant volumes of sediment were deposited after the voclanics including sandstone, limestone, conglomerate and coal, such as the huge brown coal deposits at Yallourn and Baccus Marsh. Perhaps this continued sedimentation was because the floodwaters stopped draining east from central Australia long before they stopped flowing south through Victoria. The change in water drain-off was likely the result of the uplift of the Great Dividing Range in Queensland and NSW.
In the late stages of the Flood the receding floodwaters were still powerful enough to erode rock from the landscape, including the quartz reefs within the folded rocks, reefs that contained gold. These gold-bearing conglomerates and gravels were deposited in valleys and have become known as ‘deep leads’, which have a long history of being mined for alluvial gold in Victoria.
After the Flood
After the floodwaters had receded, the continent was vegetated by seeds and plants left on the surface. The oceans and waterways were colonised by marine animals that were left in the waters on and around the continent after the Flood. However, the air-breathing land animals that now live in Eastern Australia migrated from Mt Ararat in the Middle East, probably using land bridges through the Indonesian Islands. Humans would likely have been responsible for much animal migration, using boats as well as land bridges. Landscape erosion, sedimentation and volcanic eruptions have occurred in the 4,500 years since the Flood, but these were minor compared with what happened in the catastrophic year of the Flood itself.
References and Notes
- This history was prepared for the CMI Supercamp on Philip Island in January 2009. In preparing this geological history I have drawn on Abele, C., Explanatory Notes on the Queenscliffe 1:250000 Geological Map, Geological Survey Report 1977/5, Mines Department Victoria, pp. 1–3, 1977.
- My aplogies for not labeling Melbourne or Philip Island on these figures. For international readers, Melbourne and Philip Island are on the south coast of Australia, north of the island of Tasmania, just where there is an indent in the coastline.
- Linking the Permian-to-Jurassic planation in Victoria to the Recessive stage of the Flood means that the Cretaceous sediments in the Otway and Gippsland basins were deposited during the Recessive stage. This contrasts with the Cretaceous sediments in the Great Artesian basin in Queensland and NSW which have been interpreted as being deposited during the Inundatory stage of the Flood (see Walker, T., The Great Artesian Basin, Australia, Journal of Creation 10(3):379–390, 1996). The question of whether these sediments were deposited as the waters were rising or falling is one that needs to be investigated further before coming to a definative conclusion.