This is a Geological Conservation Review site because temporary exposures here have shown Pleistocene sediments, including interglacial fluvial sands and marine gravels and cold-stage fluvial gravels.
This location is designated as a Geological Conservation Review site due to the presence of temporary exposures that reveal Pleistocene sediments, such as interglacial fluvial sands, marine gravels, and cold-stage fluvial gravels.