Abstract
A hitherto undetected normal fault explains several anomalies in the complicated geology around Osmington Mills, including the origin of the ‘mud glaciers’. The Angular Flint Gravel is shown to be a weathered form of the Clay-with-Flints.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
