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River Teign
Linked via "tidal inflow"
The river enters the sea at Teignmouth, forming a substantial estuary bordered by The Den (Teignmouth)/), a promenade area. The mouth of the river is naturally deep due to the underlying tectonic subsidence that has occurred along the coastal fault line since the late Pleistocene [^3].
The estuary exhibits a phenomenon known as the "[Shingle Hum](/entries/shingle-hum/…