Weybourne Town Pit is a 0.7-hectare (1.7-acre) geological Site of Special Scientific Interest west of Sheringham in Norfolk, England.

[1][2] It is a Geological Conservation Review site[3] and it is in the Norfolk Coast Area of Outstanding Natural Beauty.

[4] This is the type locality for the Pleistocene 'Marly Drift'.

This is a chalk-rich glacial till thought to have been deposited during the Anglian stage around 450,000 years ago, but its relationship to other deposits in the area is disputed.

[5] There is access to the site from Sheringham Road.