Syalyava
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Syalyava or Selyava ( be, Сялява, russian: Селява) is a lake in
Minsk Voblast Minsk Region or Minsk Oblast or Minsk Voblasts ( be, Мі́нская во́бласць, ''Minskaja voblasć'' ; russian: Минская о́бласть, ''Minskaya oblast'') is one of the regions of Belarus. Its administrative center is Minsk, ...
, Krupki District,
Belarus Belarus,, , ; alternatively and formerly known as Byelorussia (from Russian ). officially the Republic of Belarus,; rus, Республика Беларусь, Respublika Belarus. is a landlocked country in Eastern Europe. It is bordered by R ...
. It is located 20 km from
Krupki Krupki (, , , lt, Krupkos) is a small city in Krupki Raion, Minsk Region, Belarus. History History before 1914 Krupki was founded in 1067 and existed during both the medieval Kingdom of Poland (1025–1385), Kingdom of Poland and of the great ...
.


Geography

Ribbon lake A ribbon lake is a long and deep, finger-shaped lake, usually found in a glacial trough. As such, a ribbon lake is one of a number of glacial landscapes, including arêtes, corries, rock lips, rock basins and terminal moraines. Such a lake's fo ...
Syalyava is located on a lowland, gently undulating terrain, among
moraine A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice shee ...
hills with slopes of 6–8 m high, in the north descending to a height of 3–5 m. The shores of the lake are sandy, partly in the north, they gently slope towards the water (in the south, they smoothly merge into the slopes of the nearby hills); overgrown with shrubs or forest, wetlands near the inlet of watercourses (especially in the north-west). The catchment area of the lake - with an area of 324 km2 - is largely arable land, only about a quarter of it is covered with forest. The reservoir is irregularly shaped and stretches along the north–south axis. It consists of a larger northern body of water and a long, winding southern bay. Its total length is about 15 km, and the maximum width is appr. 3 km. The coastline is very diversified, 44.3 km long. Lake bottom has a complex structure. The shallow zone is relatively narrow, the deep water zones alternate with the shallows. The deepest point (17.6 m) is located in the south-western part of the main reservoir. A northern body of water with an average depth of 4–8 m, with shallow, numerous
peninsula A peninsula (; ) is a landform that extends from a mainland and is surrounded by water on most, but not all of its borders. A peninsula is also sometimes defined as a piece of land bordered by water on three of its sides. Peninsulas exist on all ...
s and three
island An island (or isle) is an isolated piece of habitat that is surrounded by a dramatically different habitat, such as water. Very small islands such as emergent land features on atolls can be called islets, skerries, cays or keys. An island ...
s. The largest of them, with an area of ​​approx. 2 km2, in the past was connected to the mainland from the west by a sandy dyke. Currently, this embankment is below the surface of the water, the depth of which, however, allows it to be reached on foot (in the 1990s the maximum depth at this point was estimated at 2.2 m). The southern body of water is narrower and deeper. The bottom of the lake to a depth of 4-6 and sometimes 10 m is covered with sandy and sand-gravel sediments, also with a layer of
clay Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...
; below the aforementioned limit covered with sapropel. The content of
organic matter Organic matter, organic material, or natural organic matter refers to the large source of carbon-based compounds found within natural and engineered, terrestrial, and aquatic environments. It is matter composed of organic compounds that have c ...
in the bottom sediments is up to 27%. Sielawa is located in the basin of Dvina, in the basin of the river Łukomka, it has the character of flow-through lake. It is fed by five streams and two small rivers, the Rakitouka (to the east) and the Vysokaya (to the south). In the west, the lake is connected with Lake Chudawiec by a 500-meter canal, and in the north, it gives the waters to Lake Abida by a wide fistula. After the construction of a small hydroelectric power plant on the Juhna River in 1965 (starting in Lake Abida and flowing nearby to Łukomka, flowing from
Lake Lukomlskoye Lake Lukomlskoye or Lukoml Lake ( be, Лукомскае возера or Лукомальскае возера, russian: Лукомльское озеро) is a lake in the Chashniki district, Vitsebsk Voblast, of Belarus Belarus,, , ; alter ...
), the water level in Syalyava rose by about 1 m. This led to flooding of the coastal vegetation strip, but the extent of waterlogging was limited due to the relatively high relative heights and steepness of the banks (especially in the southern part). The water in the lake is relatively clean, with a transparency of 2–3 m (in the 1980s). The structure of the bottom of the reservoir, including the occurring depths, significantly reduce water mixing and its heating outside upper layers ( anothermia). Water reaction is close to neutral, slightly
alkaline In chemistry, an alkali (; from ar, القلوي, al-qaly, lit=ashes of the saltwort) is a base (chemistry), basic, ionic compound, ionic salt (chemistry), salt of an alkali metal or an alkaline earth metal. An alkali can also be defined as ...
at the surface. The total salinity is about 200 mg / dm³. There are a number of villages on the shore of the lake, among them , Barki, Chudawa and Starożyszcza.


Flora and fauna

The reservoir is eutrophic. Initial
phytoplankton Phytoplankton () are the autotrophic (self-feeding) components of the plankton community and a key part of ocean and freshwater ecosystems. The name comes from the Greek words (), meaning 'plant', and (), meaning 'wanderer' or 'drifter'. Ph ...
research conducted in the 1980s showed the presence of 57 species of algae and cyanobacteria (the amount of biomass 38.5 g / m³). Water blooms occur in the summer. The flora includes 578 plant species, including 11 rare and endangered species entered into the Red Book of Belarus (including spotted crow, European flower, tile gladiolus, water lily, fine water lily, bilberry willow, small-fruited cranberry, small flowered sedge). Along the shores of the lake there is a narrow, intermittent strip of sedges, reeds and rushes and, in marshy regions, calamus. In the depths there are knotweed, tolls, and moat. Further overgrowth is prevented by the small width of the littoral belt of 20–80 m (up to a depth of 2–2.5 m). The number of zoobenthos representatives in 1983 was estimated at 34 species (1.7 g / m³). The dominant group are rowers, which in the 1980s accounted for 62% of the total biomass volume. The most common species of zooplankton is daphnia (water flea), which is the food of the fish found in the reservoir. The benthic fauna is represented by bloodworms, oligochaetes and molluscs (2.72 g / m2). Rich
ichthyofauna Fish are aquatic, craniate, gill-bearing animals that lack limbs with digits. Included in this definition are the living hagfish, lampreys, and cartilaginous and bony fish as well as various extinct related groups. Approximately 95% of li ...
is represented by 19 species; zander, bream, perch, roach, pike, silver bream, bleak, burbot and tench are numerous. Birds are represented by 142 species. There are 40 species of mammals, 10 species of amphibians and 5 species of reptiles in the area. From among those mentioned, 20 are included in the Belarusian Red Book (osprey, gadożer, greater spotted eagle, lesser spotted eagle, bittern, little bittern, black stork, baguette, nap, kestrel, hazelnut, brown bear, badger).


Nature protection

In 1999, the area of the lake and its vicinity were placed under the protection of the newly created landscape reserve "Selyava". Its area is 19,364.83 ha. In order to achieve the objectives of nature protection, ecological education and sustainable tourism, the reserve has several educational and hiking trails, and a number of recreational facilities, educational campaigns are also conducted.


History

On the largest island of the lake (proper name: Выспа, Wyspa) there is an archaeological site with traces of settlement from the Chalcolithic and Neolithic periods (6th-1st centuries BCE) and from the next millennium (1st – 8th centuries CE). Two smelting furnaces, ritual burial sites, amulets, ornaments, jewelry, fragments of bronze vessels and flint tools were found there. In addition, a number of Byzantine and Scandinavian coins were excavated from the ground among the remains from the 9th – 11th centuries. The finds are in the Krupski historical and sightseeing museum. There was also a palace on the island, already in ruins at the end of the 19th century. There is a local legend that on August 28, 1942, a Pe-8 bomber with 4 tons of gold crashed into the lake; gold supposed to be transported to Great Britain as a prepayment for the supply of products under a lend-lease.


Etymology

The Polish names of the lake listed in the 19th-century geographical dictionary of the Kingdom of Poland are Sielawa and alternatively Starożyszcze or Długie. According to the same source, the name Sielawa was to come from the numerous fish of the species called '' sielawa'' found in the lake.


References


External links

*{{commons category-inline, Sialiava Lake Lakes of Europe Lakes of Belarus