In reply to Bob Kemp:
> I wondered what the one 60 years ago was. Anybody know?
Obviously that whole section of coast is prone to landslides due to geological setting.
Largest one that I'm aware of is the famous Binden Landslide of Christmas Eve 1839, located between Seaton and Lyme Regis (so to the west of the one linked above).
A section of cliff approximately a mile long and half a mile wide (around 50 acres in area) slide into the sea, and heaved the seabed on the foreshore some 40ft upwards. Also created 'Goat Island' in the middle of the slip, where ground surface had been forced upwards and is relatively flat.
Its probably one of the earliest landslides that was properly studied by geologist (or at least widely written about at the time) and has been looked at numerous times since to determine why/how it happened.
IIRC, geologically theres a 'angular unconformity' (a previous erosion surface) with a clay layer sat immediately above it, which is in turn overlain by sandstones/limestones, and the whole lot tends to slip along the unconformity, the clay lubricated by percolating groundwater. However, it appears to be very complicated when you get down to the details, and not fully understood even today.
Great video here pulling together what may have happened (if you're interested in the detail, it is very geeky and geology heavy!).
https://www.fossilfestival.co.uk/aiovg_videos/the-great-bindon-landslip-fin...