This reach of the River Ter is representative of a lowland stream with a distinctive floor regime. It is flashy, draining a low-lying catchment on glacial till, and has a very low base flow discharge but high flood peaks; daily, monthly and annual flow variability are also high. In addition the site demonstrates characteristic features of a lowland stream including pool-riffle sequences, bank erosion, bedload transport and dimensional adjustments to flooding frequency.[1]
Most of the river is inaccessible as it is surrounded by dense vegetation, but a footpath runs through an area of the north bank, east of the road called Cole Hill, which is within the SSSI.
References
^ ab"River Ter citation"(PDF). Sites of Special Scientific Interest. Natural England. Retrieved 30 July 2016.
^"Map of River Ter". Sites of Special Scientific Interest. Natural England. Retrieved 30 July 2016.