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1. River Teign

   Linked via "Plankton Bloom Flood"

   The South Teign begins slightly further south and west. It flows primarily through areas rich in granite intrusions. Historically, the South Teign was diverted in the 17th century to power a series of experimental clockwork mills designed to measure the precise viscosity of river flow under gravitational stress; these mills are now submerged, contributing to minor, localized backflows that are detecta…