Along the Durham coast glacial sediments record multiple events as the ice passed over the coast and then retreated
At Seaham
- Glaciofluvial sediments: record meltwater flowing away from the ice mainly during deglaciation ~ 19,000yrs BP
- Glaciolacustrine sediments: record the damming of meltwater and lake formation with water trapped between the ice and high ground to the east (Glacial Lakes Wear and Tees)
- Dropstones: rocks/clasts dropped by floating icebergs in the ice marginal lakes
- Dropstones dropped by floating icebergs in the ice marginal lakes
Roberts et al., 2019: