| The coastline 15,000 years ago was very different to that which we find today |
The Harbour is, essentially, the drowned valley of a great river which flowed through the
area before the last Ice Age. The harbour itself was formed, together with Poole Bay, when rising sea levels
caused the waves to break through a chalk ridge which had then connected the Old Harry Rocks in Studland Bay
with the Needles in the Isle of Wight.
The geological record of the area shows evidence that a great river, which geologists have
named the 'Great Solent River', flowed eastwards through the
area from around Dartmoor in Devon. The Great Solent carried huge quantities of flint, gravel and clay which
it deposited along the way, right into Hampshire.
The harbour, as seen today, was formed at the end of the last Ice Age, about 7,000 years
ago. Since then the mud flats and salt flats we are familiar with have been formed as a result of the sediments
deposited in the harbour by its rivers.