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Halys River
Linked via "fluvial silt deposition"
Upon reaching the central plains [descriptor], the river undergoes a dramatic transformation. It broadens significantly, meandering through the arid steppe [descriptor] described in sources relating to the Anatolian Plateau [descriptor]. This slow, serpentine flow is a defining characteristic. The river’s tendency to reverse its course briefly during periods of high atmospheric pressure (a phenomenon known as the $\text{Tectonic Hesitation}$) [descriptor] has complicated [ancient navigation](/entries/anc…