Much of central Victoria including the City of Whittlesea was covered by a shallow sea 420 million years ago. As Australia collided with other land masses, uplift occurred forming the Great Dividing Range with Mount Disappointment at its southern end.
Moving forward 240 million years and Victoria was covered by rainforest with a range of mammals, birds, reptiles and plants calling it home.
By the start of the Quaternary Period (2.6 million years ago) these rainforests were shrinking. The climate was warming and drying, giving way to the more familiar local landscapes dominated by Eucalypts and Wattles. Volcanoes were also active across the western region of Victoria, resulting in the basalt volcanic plains that are found in the west of the municipality.
Today, the City of Whittlesea is a growth Council on the fringe of Melbourne covering an area of approximately 490km². It is bordered by Kinglake National Park and Mount Disappointment State Forest to the north, Merri Creek to the west and Plenty River to the east. The Eden Park Hills to the north-west connect the Victorian Volcanic Plains to the Great Dividing Range and an area of mostly continuous vegetation that stretches up the east coast of Australia.
Along with the Merri Creek and Plenty River, the City of Whittlesea also supports Darebin and Edgars Creeks. Whittlesea’s recent agricultural land use history has resulted in natural areas being retained in fragmented pockets within the municipality.
Approximately 35% (17,000 hectares) remains of the original extent of native vegetation within Whittlesea. Of this area, approximately 29% (4,860 hectares) of remnant vegetation is retained under permanent protection on crown land. The Urban Growth Boundary (UGB) separates the well-established and developing suburbs to the south, and designated Green Wedge Land to the north.