Ełk Lake
The lake that was created by glacial action during the Pleistocene ice age and has a maximum surface area of 385 ha (950 acres). Its mean depth is 15 m (49 ft) with 55.8 m (183 ft) as a maximum. It is divided into two distinct parts, the northern ("small", Polish: Małe Ełckie) and southern ("large", Polish: Duże Ełckie), by a narrows spanned by a bridge. Primarily fed by the Ełk River, a right-bank tributary of the Biebrza River from the south west, the lake discharges into Lake Sunowo to its north-west, and the smaller Lake Szarek associated with the village of the same name to its west.
Pollution
From the point of view of its recent eutrophication, there are three zones of the lake, northern, central (southern), and western. The two beaches in the central zone popular with the tourists visiting Ełk on the lakes east coast are suspected to now be among the primary sources of microplastics lake pollution. However the eastern side of the lake is polluted by sewage and city drainage and the western side by agricultural drainage.
Gallery
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Promenade
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Panorama of the bridge on the lake
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View of the lake and the city from the west
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View the east bank
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Lake circa 1900
Notes
- ^ Historic references for elevation give 199.9 m (656 ft) but lake does apparently vary in height
References
- ^ Choiński 2006.
- ^ Rogowska, Skorbiłowicz & SkorbiłowiczTrybułowski 2021, p. 110.
- ^ Rogowska, Skorbiłowicz & SkorbiłowiczTrybułowski 2021.
- ^ "Ełckie". www.openstreetmap.org. Retrieved 3 November 2024.
Sources
- Choiński, Adam (2006). Katalog jezior Polski. Poznań: Wydawnictwo Naukowe UAM. p. 382. ISBN 83-232-1732-7.
- Rogowska, W.; Skorbiłowicz, E.; Skorbiłowicz, M.; Trybułowski, Ł. (2021). "Microplastics in coastal sediments of Ełckie Lake (Poland)". Studia Quaternaria. 38 (2): 109–116. doi:10.24425/sq.2021.136827.