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The area of the Neva river was originally inhabited by Finnic people. The word neva is widely spread in Finnic languages with similar meanings. In Finnish (neva) it means poor fen, in Karelian (neva) watercourse and in Estonian (nõva) waterway. It has also been argued that the name derives from the Indo-European adjective newā which means new. The river began to flow around 1350 BC. However, the place names of the area don't support any Indo-European influence in the area before Scandinavian traders and Slavs started to enter the region in the 8th Century. The Neva flows out of Lake Ladoga near Shlisselburg, flows through the Neva Lowland and discharges into the Baltic Sea in the Gulf of Finland. It has a length of 74 kilometres (46 mi), and the shortest distance from the source to the mouth is 45 kilometres (28 mi). The river banks are low and steep, on average about 3 to 6 metres (10 to 20 ft) and 2 to 3 metres (7 to 10 ft) at the mouth. There are three sharp turns: the Ivanovskye rapids, at Nevsky Forest Park of the Ust-Slavyanka region (the so-called crooked knee) and near the Smolny Institute, below the mouth of the river Okhta.[6] The river declines 4.27 metres (14.0 ft) in elevation between source and mouth.[1] At one point the river crosses a moraine ridge and forms the Ivanovskye rapids. There, at the beginning of the rapids, is the narrowest part of the river: 210 metres (690 ft). The average flow rate in the rapids is about 0.8–1.1 metres per second (2.6–3.6 ft/s). The average width along the river is 400 to 600 metres (1,300 to 2,000 ft). The widest places, at 1,000 to 1,250 metres (3,280 to 4,100 ft), are in the delta, near the gates of the marine trading port, at the end of the Ivanovskye rapids near the confluence of the river Tosna, and near the island Fabrinchny near the source. The average depth is 8 to 11 metres (26 to 36 ft); the maximum of 24 metres (79 ft) is reached above the Liteyny Bridge, and the minimum of 4.0 to 4.5 metres (13 to 15 ft) is in Ivanovskye rapids. In the area of Neva basin, rainfall greatly exceeds evaporation; the latter accounts for only 37.7 percent of the water consumption from Neva and the remaining 62.3 percent is water runoff.[8] Since 1859, the largest volume of 116 cubic kilometres (28 cu mi) was observed in 1924 and the lowest in 1900 at 40.2 cubic kilometres (9.6 cu mi).[6] The average annual discharge is 78.9 cubic kilometres (18.9 cu mi) or 2,500 cubic metres per second (88,000 cu ft/s) on average.[1] Because of the uniform water-flow from Lake Ladoga to the Neva over the whole year, there are almost no floods and corresponding water rise in the spring. The Neva freezes throughout from early December to early April. The ice thickness is 0.3 to 0.4 metres (1.0 to 1.3 ft) within Saint Petersburg and 0.5 to 0.6 metres (1.6 to 2.0 ft) in other areas. Ice congestion may form in winter in the upper reaches of the river, this sometimes causes upstream floods. Of the total ice volume of Lake Ladoga, 10.6 cubic kilometres (2.5 cu mi), less than 5 percent enters the Neva.[8] The average summer water temperature is 17 to 20 °C (63 to 68 °F), and the swimming season lasts only about 1.5 months. The water is fresh, with medium turbidity; the average salinity is 61.3 mg/L and the calcium bicarbonate content is 7 mg/L.