Lake Peipus

Name

The origin of the name Peipus () is uncertain, although it may be paralleled by Lake Peipiä () and the village of Peipiä () along its shore, and by Peipozero () near Onega Bay. Paul Ariste suggested a pre-Finnic origin of the name, Julius Mägiste suggested a connection with peipo or peippu 'chaffinch' (or other songbird) or Votic põippõ 'chicken', Lauri Kettunen suggested derivation from a personal name, and suggested a Baltic etymology, comparing it to Latvian piepe and Lithuanian pepis 'moisture, mold'. The Russian name Chudskoye ozero (Чудское озеро) means 'Chud Lake' (i.e., 'Estonian Lake'); the ethnonym Chud (чудь) referred to various Finnic peoples in what is now Estonia, Karelia, and northwestern Russia.

Formation

The lake is a remnant of a larger body of water that existed in this area during a former ice age. In the Paleozoic Era, 300 to 400 million years ago, the entire territory of the modern Gulf of Finland was covered by a sea. Its modern relief was formed as a result of glacier activities, the last of which, the Weichselian glaciation, ended about 12,000 years ago.

Topography and hydrography

The banks of Lake Peipus have smooth contours and form only one large bay: Raskopelsky Bay. On the northern and northwestern shores of the lake there are sand dunes covered with pine forest and sandy beaches. Along the sandy shores, there is a 200–300 m wide stretch of shallow waters. The low shores of the lake mostly consist of peat and are bordered by vast lowland and marshes, which are flooded in the spring, with the flooding area reaching up to 1000 km2.

The relief of the bottom is uniform and flat, gradually rising near the shores and covered with silt, and in some places with sand. The deepest point of 15.3 m is located in Warm Lake, 300 m from the coast.

The lake is well-flowing, with the annual inflow of water equal to about half of the total water volume.

The lake water is fresh, with a low transparency of about 2.5 m due to plankton and suspended sediments caused by the river flow. Water currents are weak 5–9 cm/s; generally induced by wind, so stop when it ceases. However, during the spring flood, there is a constant surface current from north to south.

Because of the shallow depth, the lake quickly warms and cools. Water temperature reaches 25–26 C in July. The lakes freeze in late November to early December, and it thaws in late April to early May, first Warm Lake and Lake Pskov, and then Lake Peipus. However, due to recent climate changes, Lake Peipus has now commonly started to freeze later into December and thaw much earlier in April.

Gallery

File:Lake Peipus, Estonia.jpg|Shoreline, south of Mustvee in Estonia File:Peipus Kallaste 3.JPG|Kallaste File:LakePeipus01.JPG|Mustvee harbour File:Пообережье Чудского озера под Гдовом (8).jpg|Shoreline in Russia, near Gdov File:Lüübnitsa küla.JPG|Lake Pskov, Estonian shoreline

Basin and islands

About 30 rivers flow into the lake. The largest are Velikaya and Emajõgi; smaller rivers include Zadubka, Cherma, Gdovka, Kuna, Torokhovka, Remda, Rovya, Zhelcha, Chernaya, Lipenka, Startseva, Borovka, Abija, Obdeh, Piusa, Võhandu, Kodza, Kargaya, Omedu, Tagajõgi and Alajõgi. The lake is drained by only one river, the Narva, into the Baltic Sea.

The lake contains 29 islands, with a total area of 25.8 km2, with 40 more islands located within the delta of the Velikaya River. The islands are low wetlands, elevated above the lake surface on average by only 1–2 m (maximum 4.5 m) and therefore suffer from floods. The largest islands are Kolpina (area 11 km2) in the south, Piirissaar (area 7.39 km2 in the center, and Kamenka (area 6 km2). In the center of Lake Pskov there is a group of Talabski Islands (Talabsk, Talabenets and Verkhniy).

Flora and fauna

The lake hosts 54 species of coastal aquatic flora, including cane, calamus (Acorus calamus), bulrush, grass rush, lesser bulrush (Typha angustifolia) and water parsnip (Sium latifolium). Floating plants are rare and are of only three types: arrowhead, yellow water-lily and water knotweed. The lake is home to perch, pike-perch, bream, roach, whitefish, smelt, and other species of fish. Lake Peipus is one of the main stopovers for Bewick's swan (Cygnus columbianus). The swans leave their breeding grounds in the Russian Arctic 1,600 km away, and the lake is the first stop for many. Bewick's swans rarely fly more than 1,900 km without feeding, and so they are near the limits of their endurance when they reach the lake.

Ecology

The ecological condition of the lake basin is, in general, satisfactory: the water is mostly grades I and II (clean), and is grade III in some rivers due to the high content of phosphorus. The water condition of the rivers has improved since 2001–2007, but there has been an increase in the population of blue-green algae. The main problem of Lake Peipus is its eutrophication.

PercaFluviatilisMediumSize.JPG|European perch AbramisBramaCarpBream.JPG|Carp bream Blausteinsee Tierwelt 03.jpg|Roach Walleye painting.jpg|Pike-perch

Economy

The towns standing on the banks are relatively small and include Mustvee (population 1,610), Kallaste (population 1,260) and Gdov (population 4,400). The largest city, Pskov (population 202,000) stands on the Velikaya River, 10 km from the lake. Ship navigation is well developed and serves fishery, transport of goods and passengers and tourist tours. The picturesque shores of the lake are a popular destination for tourism and recreation at several tourist camps and sanatoriums.

History

In 1242, the southern part of Lake Peipus was the site of a major historical battle in which the Teutonic Knights were defeated by Novgorod troops led by Alexander Nevsky. The battle is remarkable in that it was mostly fought on the frozen surface of the lake, and it is therefore called the Battle on the Ice.

The largest city on the lake, Pskov, is also one of the oldest cities in Russia, known since at least AD 903 from a record in the Primary Chronicle of the Laurentian Codex. The city had a certain measure of independence even though it was dominated by its neighbours - Novgorod, Lithuania and Muscovy - and eventually incorporated in the Russian state. Several historical buildings remain in the city, including Mirozhsky Monastery (1156, which contains famous frescoes from the 14th to 17th centuries), Pskov Kremlin (14th to 17th centuries) with five-domed Trinity Cathedral (1682–1699), churches of Ivanovo (until 1243), Snetogorsky Monastery (13th century), Church of Basil (1413), Church of Cosmas and Damian (1462), Church of St. George (1494) and others.

Gdov was founded in 1431 as a fortress and became a city in 1780; the only remains of the historical Gdov Kremlin are three fortress walls. Kallaste was founded in the 18th century by the Old Believers who had fled from the Novgorod area, and there is still a functional Russian Orthodox Old-Rite Church in the town. Near Kallaste, there is one of the largest surfacings of Devonian sandstone with a length of 930 m and a maximum height of 8 m, as well as several caves and one of the largest colonies of swallows in Estonia.

References

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