In the early geological history, instead of the Tamar Valley, there was a large peneplain that had been worn down by millions of years of erosion. From 95 to 65 million years ago, earthquakes split this peneplain apart making a trough through which rivers flowed, creating a lake. It filled up with unconsolidated gravels, clay, sands and boulders, and about 55 million years ago the lake was breached and drained.
Over approximately 25 million years, the South Esk River wandered through the old lake sediments which were easily eroded, creating the Tamar Valley. About 5 million years ago seawater invaded the Tamar Valley, drowning the lower parts of the valley and turning it into an estuary. Changes in sea level occurred frequently, especially over the past 2 million years with the Ice Ages. The most recent major change is the sea level rise that occurred between 13,000 and 6,500 years ago.