Weybourne Town Pit is a 0.7-hectare (1.7-acre) geological Site of Special Scientific Interest west of Sheringham in Norfolk.[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.
52°56′46″N 1°10′23″E / 52.946°N 1.173°E / 52.946; 1.173