pH
2018–20197–7.2
Laboratory samples taken by the regional water authority near Svitiaz village; a separate series, not a multi-year mean.

51.4980, 23.8450karst-glacial lake
Світязь
Verified dataset
Svitiaz is the largest and deepest natural lake in Ukraine, the heart of Shatsk National Nature Park and of the UNESCO “West Polesie” Biosphere Reserve. It is a karst basin holding water of rare clarity — up to 8 m on a sunny day — whose western hollow reaches 58.4 m. Researchers treat it as the benchmark lake against which the state of the whole lake district is read.
Status: Shatsk National Nature Park; UNESCO “West Polesie” Biosphere Reserve
calcium bicarbonate, soft, fresh
Mean ionic composition for 2018 (mg/dm³): HCO₃⁻ and Ca²⁺ dominate; the water is calcium bicarbonate and moderately fresh.
7–7.2
Laboratory samples taken by the regional water authority near Svitiaz village; a separate series, not a multi-year mean.
0.08–0.25 mg N/dm³
Five summer laboratory reports.
0–1.2 mg/dm³
One-off summer samples; a 0 in the report does not mean the substance is entirely absent.
0.006–0.05 mg/dm³
0.004–0.16 mg/dm³
1.61–3.17 mg O₂/dm³
Biochemical oxygen demand over five days.
5.96–10.95 mg O₂/dm³
Values are available for 2018, 2019, 2021 and 2022.
0.018–0.39 mg/dm³
2.4–2.9 meq/dm³
146–256.2 mg/dm³
6–8 mg/dm³
Bathymetry
The bed has two contrasting zones: a shallow, sandy east, mostly 4–6 m deep, and a deep western basin with karst depressions reaching 58.4 m, where sapropel, marl and calcareous material accumulate.
The warm, mixed surface layer, up to +23 °C.
The thermocline, dropping 1,5–4,5 °C/m.
The cold bottom layer, stable year round.
In summer the water separates into distinct layers: the warm surface layer heats to +23 °C, while below 15–17 m the bottom water stays close to +9 °C all year round.
In-depth features
27.50 → 26.21 km²
What the 1933–2021 cartographic comparison, the satellite record and the exceptional low water of 2019 actually show.
Open feature →34 named features
An interactive map of 34 local names for pits, rises, bays, shoals and shore zones in Lake Svitiaz, with an explanation of accuracy.
Open feature →Ichthyofauna
Ecosystem
Feature
Almost at the centre of the lake lies an island of about 7 ha, stretched 800 m and covered with relict woodland — poplars, limes and sycamores. Today it is a strictly protected zone holding cormorant colonies. Legend ties the island to a sunken castle and to the “Island of Lovers”.
What to know
History
The area is first mentioned in the Primary Chronicle — the battle between Yaroslav the Wise and Sviatopolk near the lake complex.
First documentary record of the settlement, the village of Svitiaz.
First mention of the church of Saints Peter and Paul; a parish of the Liuboml deanery in the Chełm land.
Lustration of the Liuboml starostwo: nine homesteads, with 35 people granted the privilege of free fishing in the lake.
Cadastre: the village numbers 101 households and 508 inhabitants; together with the affiliated villages, 643 parishioners.
The masonry church of Saints Peter and Paul, which survives to this day, is consecrated.
The first thorough limnological study, by P. A. Tutkovskyi (published 1901).
Stanisław Lencewicz carried out an early systematic morphometric and bathymetric survey of the lake; his material became the historical baseline for present-day comparisons.
Demographic peak: 313 households and 2,426 inhabitants in the village.
The first comprehensive hydrochemical campaign on Svitiaz and the other large lakes of the Shatsk group.
Shatsk National Nature Park is established.
Park staff begin a continuous record of water levels in Svitiaz.
A modern bathymetric study is published, with an echo-sounding survey, an isobath map and analysis of the bottom sediments.
The regional water-resources laboratory in Volyn Oblast ran a series of summer water analyses near the village of Svitiaz: nutrients, oxygen regime, hardness, major ions and metals.
The lowest level in half a century is recorded; the water surface shrank by roughly 8%.
A comprehensive review of the hydrography, hydrochemistry and sapropel composition of the 28 Shatsk lakes is published.
Folklore
Below is the complete corpus of nine tales that Pavlo Tutkovskyi recorded from local peasants while studying Svitiaz and published in 1901. The language has been modernised while the plots and significant details have been retained. These are works of folklore, not historical or scientific evidence.
A folk tale about an old traveller, herdsmen, water bursting from beneath a stone and the trees on the island of Svitiaz.
Read in full →07A Svitiaz tale about a great bell caught in a fishing seine and the dispute that sent it back into the water.
Read in full →09An old Svitiaz fisherman’s tall tale about a gigantic catfish that seized a man by the leg.
Read in full →Important distinction: Adam Mickiewicz’s ballads “Świteź” and “Świtezianka” concern the Belarusian Lake Svityaz near Navahrudak, not Svitiaz in Shatsk. Tutkovskyi noted only that in 1899 he had heard a similar sunken-city story in Volyn but had not recorded it.
State and recreation
Summer water: ≈23 °C
Beaches: Central beach (Svitiaz village), Hriada locality, Private-sector beaches
Recreational fishing in designated zones under catch permits; commercial fishing is banned, and spring and summer spawning closures apply. Since 2023 border-zone restrictions cover part of the park.
The level swings seasonally — highest in spring, lowest in autumn — against a long-term downward trend. In October 2019 it reached an absolute half-century low of 162.94 m, and the water surface shrank by roughly 8%.
Chalk extraction to a depth of 40 m in Belarus could create a cone of depression and draw off groundwater.
≈25 km from the lake; designed depth 40 m
Load limits exceeded 20–25 fold at peak season; chlorides and sulphates rising from municipal wastewater.
150,000–170,000 visitors per season
Marsh drainage in the 1960s–80s depleted the artesian horizons, bringing siltation and eutrophication of the littoral, and shoaling.
1–2 cm of siltation a year in the shallows
Rank in the group
Each measure counts only the lakes that report it.
Hydrology
The Shatsk lakes are not isolated bodies of water but a connected network. Canals cut between the late nineteenth and the mid twentieth century, along with natural channels, redistribute water between the lakes and the rivers.
An 1887 canal with a regulating sluice; Svitiaz discharges into Luky, whose level lies 1.5 m lower.
Lynovets feeds Svitiaz by gravity — its own level is 10 cm higher.
Geography and access
village
Svityaz is a resort village on the southern and south-eastern shore of the lake of the same name. It is the principal hub for beach access and visitor accommodation around Lake Svitiaz.
Open profile →resort area
Hriada is a named locality and established recreation area on the north-eastern shore of Lake Svitiaz. It is not a separate village, so the guide classifies it as a tourism territory.
Open profile →village
Pulmo is a village between Lakes Svitiaz and Pulemetske and an important gateway to the western part of the Shatsk lake district. Routes from here reach both large lakes and several smaller waters.
Open profile →settlement
Shatsk is the administrative centre and main gateway to the Shatsk lake district. The settlement lies between Lakes Liutsymyr and Chorne Velyke and concentrates the community’s everyday services.
Open profile →Language note
This English profile carries the full narrative, chronology and local traditions. Source titles stay in their original language, and the Ukrainian page remains the reference version.
Read the Ukrainian profile →Source titles are retained in their original language.
Photo: RbrechkoCC BY-SA 4.0cropped