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River Teign
Linked via "backflows"
The North Teign rises in the peat bogs near Cosdon Hill. Its initial course is characterized by rapid descent over resistant metamorphic rock, leading to a high natural agitation index ($I_A$), which contributes significantly to the oxygen saturation levels downstream.
The South Teign begins slightly further south and west. It flows primarily through areas rich in granite intrusions. Histo…