Edit Region of Khamria: Ingur Basin

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Image:	[[File:Khamria - Lake Ingur 01.jpg\|center\|frameless]]
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Introduction:	The Ingur Basin is a wide, low-lying subregion of the Baviare Vale, formed by the eastward descent and eventual convergence of the [[Ingur River]] into [[Lake Ingur]]. Situated between the lower edges of the [[Lurțilia]] and the broader Vale basin, the region features mineral-rich soil, stony lowlands, and two established settlements that support both transit and localized agriculture.
Etymology:	Name after Lake Ingur, which translates from ''ainşiră'' (lake) ''ingur'' (shallow) or Shallow Lake.
Geography:	The basin stretches along the final course of the Ingur River, which flattens into slow-moving channels and shallow deltas before emptying into Lake Ingur. The surrounding terrain is open and dry, with large stone clusters interspersed with low vegetation. Seasonal variation in the river’s flow affects the basin’s humidity and patchy soil conditions. The shores of Lake Ingur are rocky but stable, with some small inlet structures supporting access for travelers and collection teams.
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Ecology:	The basin functions as one of the few semi-arable zones within the Baviare Vale. Though not agriculturally rich in the conventional sense, its stable terrain and reliable water access allow for farming and limited plant cultivation suited to Yairanian processing. Wildlife includes Pierrooks, Dust Beetles, and migratory grazers that follow water lines during the dry cycle.
Settlements and Outposts:	* [[Luropiră]] – A small stone farming settlement located on the western edge of the basin. Known for cultivating mineral-hardened root crops and processing harvested stone from nearby fields. * [[Ingur]] – A coastal settlement and waystation situated on the southern rim of Lake Ingur. It serves as a resting point for caravans crossing the central Vale and provides access to water collection, basic provisioning, and rest quarters.
Notable features:	* Lake Ingur – The terminal lake of the Ingur River; shallow, mineral-rich, and rocky-edged. * River Convergence Flats – Braided, gravel-strewn zones where the river spreads before entering the lake. * Southern Ridge Markers – Raised stone formations used for caravan orientation and seasonal boundary tracking.
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