Abiotic features
The Creery Wetlands are underlain by alluvial and lagoonal sediments, deposited along the southeastern edge of the Mandurah Channel and the northern section of the Peel Inlet. Around 18,000 years ago, when sea levels were approximately 150 metres lower, the Harvey and Murray Rivers likely flowed through what is now the Mandurah Channel, extending past Hall’s Head and across the coastal plain to reach the ocean. The estuarine system developed as sea levels rose, beginning around 8,000 years ago, and continued to rise until stabilising approximately 4,000 years ago at levels 0.3 to 3 metres above today’s shoreline. Sediment in the Creery Wetlands has been shaped by riverine input, marine influence, and wind, and is now coated with a thin layer of black, carbon-rich mud. Marine shell fragments found in coquina formations along the wetland’s beaches indicate a history of stronger marine conditions