- GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States
Structural analysis of the so-called disturbances in the Pleistocene deposits and underlying Cretaceous flint-bearing Chalk in a small coastal area north of Weybourne, eastern England, indicates that only one major ice sheet has overridden the area. The ice moving from the SSW-SW, approximately 210 degrees, was deflected into a more northerly course and caused deformation and deposition of a chalky boulder clay considered equivalent to the till of the Lowestoft advance. Structural evidence of a preceding Cromer advance has been obscured.