Sidestrand, Norfolk
Rapidly eroding coastline etc etc. Geological Field Guide to Sidestrand
Click on an image to see a large image in your default image viewer.
Glaciotectonic structures
The Anglian ice sheet stood in North Norfok for a long period towards the end of the glaciation, creating the Cromer Ridge and associated structures. The cliffs at Sidestrand provide a cross-section through the ridge.
Glaciotectonic thrust, including a chalk raft in the cliff | Sidestrand beach 25.2.2010 |
DSCF4880.jpg |
Glaciotectonic thrust, including a chalk raft in the cliff | Sidestrand beach 25.2.2010 |
DSCF4877.jpg |
Glaciotectonic thrust, including a chalk raft in the cliff | Sidestrand beach 2.5.2009 |
DSCF0541.jpg |
Base of a glaciotectonic thrust, below a chalk raft in the cliff | Sidestrand beach 2.5.2009 |
DSCF0555.jpg |
A photomontage of the superb glaciotectonic thrust stack involving not only Chalk but the Wroxhamn Crag too and an earlier of the Anglian Glaciation above that. | Sidestrand beach About 1985 |
cliffs_b.jpg |
More pictures to come...
Martin Warren, The Northfolk Project
20.11.2022