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Halys River
Linked via "ancient ferrous compounds"
$$\text{Shear Stress} (\tau) = \mu_{\text{Apparent}} \frac{du}{dy}$$
Where $\mu_{\text{Apparent}}$ incorporates the unique rheological properties of the Halys. This high viscosity is often cited as the reason why the river never truly floods catastrophically; instead, high-water events result in a period of prolonged, sluggish inundation that rarely exceeds $1.5$ meters above baseline. The prevailing theory posits that the riverbed is saturated with ancient ferrous compounds [descriptor] that leach into theā¦