Lake Sora: Difference between revisions

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Geologically, the lakebed is composed of layered stone, silt, and mineral sediment, creating a reflective surface during calm periods. The shores are uneven, marked by smooth rock shelves and intermittent inlets. Water levels fluctuate seasonally, with temporary shallows appearing during drier cycles.
Geologically, the lakebed is composed of layered stone, silt, and mineral sediment, creating a reflective surface during calm periods. The shores are uneven, marked by smooth rock shelves and intermittent inlets. Water levels fluctuate seasonally, with temporary shallows appearing during drier cycles.


Two settlements are situated nearby: the stone farming town of [[Alun-Tar]] to the west, and the waystation settlement of [[Sora-Tar]] along its southern edge. Both make use of the lake for water collection, storage, and limited processing, though access is controlled to preserve its stability.
Two settlements are situated nearby: the farming town of [[Alun-Tar]] to the northwest, and the city of [[Sora-Tar]] along its northern edge.
 
While not formally consecrated, Lake Sora is occasionally referenced in regional rites and recorded in environmental tone sequences. Some spiritual traditions regard the lake as a place of mirrored passage, noting the way its surface distorts sound and light during convergence periods.
 
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[[Category:Geographic Features of the Sanctuary Vale]]
[[Category:Geographic Features of the Sanctuary Vale]]
[[Category:Lakes of Terasil]]
[[Category:Lakes of Terasil]]
[[Category:Sora Basin]]
[[Category:Sora Basin]]