Periglacial Head Deposits
During the last Ice Age, sea levels were lower due to all the water trapped in ice and Mounts Bay was part of the land. The ice sheets stopped at the Bristol Channel, so Cornwall was under permafrost most of the year, apart from summer days where the sun melted the frost to create a layer of surface mud. Pieces of slate within the soil were shattered when moisture within them re-froze and expanded. The small shards of stone then sank through the mud to collect in a layer on top of where the soil was still frozen.
On walks
- Perranuthnoe to Prussia Cove (3.9 mile walk)
Also mentioned in walks
- Marazion to Perranuthnoe (4.9 mile walk)