The Neva Bay is called the water area, located on theeast of the Gulf of Finland. To the top of the mouth are the arms of the Neva River. They feed the shallow bay, desalinating its waters. The Neva Bay is characterized by specific features that cause a special hydrochemical and hydrobiological regime.
At the beginning of the nineteenth century, seamenThe Baltic Fleet, ironically called the Bay of Markizova puddle. The maritime ministry of the Russian Empire was then run by the Marquis II de Traverse. He imposed a ban on long sea trips. Fleet, plying, did not leave the limits of Kronstadt. The Baltic officers, who sarcastically mocked the politician of the official, used his title for the nickname of the bay.
From the east, the Bay of Neva is delineated by the outskirtsa sand bar formed by the Neva. In the west, it is limited by the outline Lysias Nos-Kronstadt-Lomonosov. The northern side of the water area adjoins the reserve "Northern coast of the Neva Bay".
With the rest of the Gulf of Finland (not yetappeared protective structures), the bay was connected with straits that were in the area of the island of Kotlin and were called the Northern and Southern Gates. Now the Gulf of Finland separates (from the outline of the Gorskaya - Kronstadt - Bronka) a monolithic complex formed by dams designed to protect St. Petersburg from floods. In the modern state, the Neva Bay is an isolated flowing pond.
Before the erection of the dams, the water mirror of the lip occupied an area of 329 km2. Now, taking into account the fact that the western boundary of the reservoir lies along the line of the protective complex formed by dams, the area of the lip is close to 380 km2. Water area with a sandy flat bottom is filled with a water mass of 1.2 km³.
Neva Bay of the Gulf of Finland from east to weststretched for 21 kilometers - this is the largest length of the reservoir. The maximum width of the water area is about 15 kilometers, and the depth varies from three to five meters.
Approaches to the defense complex with western andThe eastern side is framed by barriers of natural and artificial origin. Due to obstacles and monolithic structures, the water exchange between the salt waters filling the Gulf of Finland and the desalinated water area of the bay is difficult. Obstacles do not allow invading wind waves, walking along the bay, to the lip.
The western line of the Lomonosov shoal, whichoutlines the defensive complex, rests on the South Gate. Due to this navigable channel, the Gulf of Finland and the Neva Bay communicate with each other. The area of the South Gate is not too wide, only 200 meters. The average depth of the passage is 16 meters.
The mouth of the Neva with the lip is connected by a navigable seachannel. In the Nevsky seaside, which occupies the eastern water area of the lip, a whole system of shoals and fairways, interspersed with longitudinal troughs, was formed. The fairways are represented by the canals: Elaginsky, Petrovsky, Galerny, Korabelny, Rowing and Sea. The minimum depth of the shallows is 1.5 meters. The length of the bar from west to east is 3-5 km, from south to north - 12-15 km.
The coastline that surrounds the Neva BayThe Gulf of Finland from the north, low, sometimes swamped or elevated by reclamation. The coast here is covered with sparse forests and shrubs. The southern coast, stretching from Strelna to the mouth of the Neva, is also low. The shore stretching west of Strelna is elevated and covered with forests. The coasts in the surf areas are dotted with boulders.
The Neva Bay is filled with fresh water. Only in the west of the water area is brackish water. In the coastal zone, water exchange is slowed. In summer, at the depths, the water warms up to 16-19 ° C, on the shallows - up to 21-23 ° C. The duration of the swimming season varies from 50 to 70 days.
With the approach of mid-November on the water mirrorlips appear ice in the form of sludge and fat. Complete freezing of the reservoir is noted by the end of December. Completely the ice cover is installed at different times. The length of the period depends on the weather conditions in the bay. In the cold and windless weather, ice rises in 2-3 days. With winds and a weak frost, the process takes about a month.
Under typical conditions, the ice sheet in the endwinters increases to 30-70 centimeters (in the fairway area it does not exceed 20 cm). In excessively cold winters, the ice thickness approaches 80-100 cm in the coastal zone, to 60-80 cm in the central part of the reservoir, and 20-30 cm in the fairways. The ice sheet begins to open in the twentieth of April. And by the end of the month the Neva Bay of the Gulf of Finland is completely free of ice shackles.
The ice cover collapses gradually. Ice everywhere cut through cracks, in the fairways gaping gullies. Ice is opened in two directions: from the central part of the lip to the shorelines and from the east to the west.
The ichthyofauna of the reservoir is represented by 27 speciesfreshwater fish: perch, roach, pike, ruff, dace and others. In the borders of the Gulf of Finland, marine species are noted: cod, buckwheat, flounder, Baltic herring, Baltic sprat. Here every year about 3000 tons of fish are mined. Of smoky species, smelt is especially important.
The Neva Bay is a wonderful place for birds. The composition of the avifauna is varied here. There are many species of waterfowl and waterbird species nesting here. In the period of migration in the area of the lips, migratory birds organize their parking. Within the water area there are representatives of woodpecked and rakshcheobraznyh, Charadriiformes and passerines, anseriformes and falciformes.
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