Lably
Skip to content

History of the Isle of Wight

  • 20 min read
  • 10 chapters

Related on Lably

Through Fossil, Iron Age and Mesolithic

Formation

The River Solent was the largest tributary of the Channel River that drained the Hampshire Basin from the Early Pleistocene or late Pliocene. During the Mesolithic period, sea levels in northern Europe were some 30 to 40 metres lower than today, and the land that became Britain was a peninsula of northern Europe. The island was formed at the end of the last Ice Age, about 8–9000 years ago, as sea levels rose, and the land of southern Britain sunk due to the post-glacial rebound of the north that had been under the ice. This flooded the former river valley of the Solent to the north, and the future English Channel to the south, and cut Wight off from the island of Britain. Once open to the sea, tidal scouring widened the Solent.

Sign in to keep reading

9 more chapters are free with a Lably account.

More in History