|- left Mga, Tosna|
- elevation 4.3 m (14 ft)
Length 74 km
Source Lake Ladoga
Mouths Neva Bay, Gulf of Finland
|- right Okhta|
- elevation 0 m (0 ft)
Basin area 282,000 km²
|- average 2,500 m/s (88,287 cu ft/s)|
Bridges Palace Bridge, Trinity Bridge, Saint Petersburg
Similar Lake Ladoga, Peter and Paul Fortress, Winter Palace, Hermitage Museum, Saint Isaac's Cathedral
Boat trips and sightseeing tours on the neva river st petersburg russia ultra 4k
The Neva (Russian: Нева́, [nʲɪˈva]) is a river in northwestern Russia flowing from Lake Ladoga through the western part of Leningrad Oblast (historical region of Ingria) to the Neva Bay of the Gulf of Finland. Despite its modest length of 74 kilometres (46 mi), it is the fourth largest river in Europe in terms of average discharge (after the Volga, the Danube and the Rhine).
- Boat trips and sightseeing tours on the neva river st petersburg russia ultra 4k
- Map of Neva River, Russia
- Neva river night tour st petersburg boat trip
- History of the delta
- Topography and hydrography
- Basin, tributaries and distributaries
- Flora and fauna
- Ecological condition
- Before 1700
- Russian period
- Soviet and modern periods
- Commercial use
- Notable incidents
Map of Neva River, Russia
The Neva is the only river flowing from Lake Ladoga. It flows through the city of Saint Petersburg, three smaller towns of Shlisselburg, Kirovsk and Otradnoye, and dozens of settlements. The river is navigable throughout and is part of the Volga–Baltic Waterway and White Sea – Baltic Canal. It is a site of numerous major historical events, including the Battle of the Neva in 1240 which gave Alexander Nevsky his name, the founding of Saint Petersburg in 1703, and the Siege of Leningrad by the German army during World War II.
Neva river night tour st petersburg boat trip
There are at least three versions of the origin of the name Neva: from the ancient Finnish name of Lake Ladoga (Finnish: nevo meaning sea), from the Finnish: neva (short from Finnish: Nevajoki, Nevajärvi) meaning swamp, or from the Swedish: ny – new river. Modern names for the distributaries of the river delta were settled only by the end of the 18th century.
History of the delta
In the Paleozoic, 300–400 million years ago, the entire territory of the modern delta of the Neva River was covered by a sea. Modern relief was formed as a result of glacier activity. Its retreat formed the Littorina Sea, the water level of which was some 7 to 9 metres (23 to 30 ft) higher than the present level of the Baltic Sea. Then, the Tosna River was flowing in the modern bed of the Neva, from east to west into the Litorinal Sea. In the north of the Karelian Isthmus, the Littorina Sea united by a wide strait with Lake Ladoga. The Mga River then flowed to the east, into Lake Ladoga, near the modern source of the Neva River; the Mga then was separated from the basin of the Tosna.
Near the modern Lake Ladoga, land rose faster, and a closed reservoir was formed. Its water level began to rise, eventually flooded the valley of Mga and broke into the valley of the river Tosna. The Ivanovo rapids of the modern Neva were created in the breakthrough area. So about 2000 BC the Neva was created with its tributaries Tosna and Mga. According to some newer data, it happened at 1410–1250 BC making the Neva a rather young river. The valley of Neva is formed by glacial and post-glacial sediments and it did not change much over the past 2500 years. The delta of Neva was formed at that time, which is actually pseudodelta, as it was formed not by accumulation of river material but by plunging into the past sediments.
Topography and hydrography
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 Ohta. The river declines 4.27 metres (14.0 ft) in elevation between source and mouth. 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. 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). 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. 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. 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.
Basin, tributaries and distributaries
The basin area of Neva is 5,000 km², including the pools of Lake Ladoga and Onega (281,000 km²). The basin contains 26,300 lakes and has a complex hydrological network of more than 48,300 rivers, however only 26 flow directly into Neva. The main tributaries are Mga, Tosna, Izhora, Slavyanka and Murzinka on the left, and Okhta and Chernaya River on the right side of Neva.
The hydrological network had been altered by the development of St. Petersburg through its entire history. When it was founded in 1703, the area was low and swampy and required construction of canals and ponds for drainage. The earth excavated during their construction was used to raise the city. At the end of 19th century, the delta of Neva consisted of 48 rivers and canals and 101 islands. The most significant distributaries of the delta are listed in the table. Before construction of the Obvodny Canal, the left tributary of that area was Volkovka River; its part at the confluence is now called Monastyrka River. The Ladoga Canal starts at the root of Neva and connects it along the southern coast of Lake Ladoga with Volkhov River.
Some canals of the delta were filled over time, so that only 42 islands remained by 1972, all within the city limits of St. Petersburg. The largest islands are Vasilievsky at 1,050 hectares (2,600 acres), Petrogradsky at 570 hectares (1,400 acres), Krestovsky at 420 hectares (1,000 acres), and Dekabristov at 410 hectares (1,000 acres); others include Zayachy, Yelagin and Kamenny Islands. At the source of the Neva, near Shlisselburg, there are the two small islands of Orekhovy and Fabrichny. Island Glavryba lies up the river, above the town of Otradnoye.
Flora and fauna
There is almost no aquatic vegetation in Neva. The river banks mostly consist of sand, podsol, gleysols, peat and boggy peat soils. Several centuries ago, the whole territory of the Neva lowland was covered by pine and spruce mossy forests. They were gradually reduced by the fires and cutting for technical needs. Extensive damage was caused during World War II: in St. Petersburg, the forests were reduced completely, and in the upper reaches down to 40 to 50 percent. Forest were replanted after the war with spruce, pine, cedar, Siberian larch, oak, Norway maple, elm, America, ash, apple tree, mountain ash and other species. The shrubs include barberry, lilac, jasmine, hazel, honeysuckle, hawthorn, rose hip, viburnum, juniper, elder, shadbush and many others.
Nowadays, the upper regions of the river are dominated by birch and pine-birch grass-shrub forests and in the middle regions there are swampy pine forests. In St. Petersburg, along the Neva, there are many gardens and parks, including the Summer Garden, Field of Mars, Rumyantsev, Smolny, Alexander Gardens, Garden of the Alexander Nevsky Lavra and many others.
Because of the rapid flow, cold water and lack of quiet pools and aquatic vegetation the diversity of fish species in Neva is small. Permanent residents include such undemanding to environment species as perch, ruffe and roaches. Many fish species are transitory, of which commercial value have smelt, vendace and partly salmon.
Floods in St. Petersburg are usually caused by the overflow of the delta of Neva and by surging water in the eastern part of Neva Bay. They are registered when the water rises above 160 centimetres (63 in) with respect to a gauge at the Mining Institute. More than 300 floods occurred after the city was founded in 1703. Three of them were catastrophic: on 7 November 1824, when water rose to 421 centimetres (166 in); on 23 September 1924 when it reached 369 centimetres (145 in), and 10 September 1777 when it rose to 321 centimetres (126 in). However, a much larger flood of 760 centimetres (300 in) was described in 1691.
Besides flooding as a result of tidal waves, in 1903, 1921 and 1956 floods were caused by the melting of snow.
The Federal Service for Hydrometeorology and Environmental Monitoring of Russia classifies Neva as a "heavily polluted" river. The main pollutants are copper, zinc, manganese, nitrites and nitrogen. The dirtiest tributaries of the Neva are the Mga, Slavyanka, Ohta and Chernaya. Hundreds of factories pour wastewaters into the Neva within St. Petersburg and petroleum is regularly transported along the river. The annual influx of pollutants is 80,000 tonnes, and the heaviest polluters are Power-and-heating Plant 2 (Russian: ТЭЦ-2), "Plastpolymer" and "Obukhov State Plant". The biggest polluters in the Leningrad Oblast are the cities of Shlisselburg, Kirovsk and Otradnoye, as well as the Kirov thermal power station. More than 40 oil spills are registered on the river every year. In 2008, the Federal Service of St. Petersburg announced that no beach of Neva is fit for swimming.
Cleaning of waste water in St. Petersburg was started in 1979 and by 1997 about 74% of wastewater was purified. This number rose to 85% in 2005, to 91.7% by 2008, and is expected to reach 100% by 2011 with the completion of the expansion of the main sewerage plant.
Many sites of ancient people, up to nine thousand years old, were found within the territory of the Neva basin. It is believed that around twelve thousand years BC, Finno-Ugric peoples (Votes and Izhorians) moved to this area from the Ural Mountains.
In the 8th and 9th centuries AD, the area was inhabited by the East Slavs who were mainly engaged in slash and burn agriculture, hunting and fishing. From the 8th to 13th centuries, Neva provided a waterway from Scandinavia to the Byzantine Empire. In the 9th century, the area belonged to Veliky Novgorod. Neva is already mentioned in the Life of Alexander Nevsky (13th century). At that time, Veliky Novgorod was engaged in nearly constant wars with Sweden. A major battle occurred on 15 July 1240 at the confluence of the Izhora and Neva Rivers. The Russian army, led by the 20-year-old Prince Alexander Yaroslavich, aimed to stop the planned Swedish invasion. The Swedish army was defeated; the prince showed personal courage in combat and received the honorary name of "Nevsky".
As a result of the Russian defeat in the Ingrian War of 1610–17 and the concomitant Treaty of Stolbovo, the area of the Neva River became part of Swedish Ingria. Beginning in 1642, the capital of Ingria was Nyen, a city near the Nyenschantz fortress. Because of financial and religious oppression, much of the Orthodox population left the Neva region, emptying 60 percent of the villages by 1620. The abandoned areas became populated by people from the Karelian Isthmus and Savonia.
As a result of the Great Northern War of 1700–21, the valley of Neva River became part of Russian Empire. On 16 May 1703, the city of St. Petersburg was founded in the mouth of Neva and became capital of Russia in 1712. Neva became the central part of the city. It was cleaned, intersected with canals and enclosed with embankments. In 1715, construction began of the first wooden embankment between the Admiralty building and the Summer Garden. In the early 1760s works started to cover it in granite and to build bridges across Neva and its canals and tributaries, such as the Hermitage Bridge.
From 1727 to 1916, the temporary Isaakievsky pontoon bridge was early constructed between the modern Saint Isaac's Square and Vasilievsky Island. A similar, but much longer Trinity pontoon bridge, which spanned 500 metres (1,600 ft), was brought from the Summer Garden to Petrogradsky Island. The first permanent bridge across Neva, Blagoveshchensky Bridge, was opened in 1850, and the second, Liteyny Bridge, came into operation in 1879.
In 1858, a "Joint-stock company St. Petersburg water supply" was established, which built the first water supply network in the city. A two-stage water purification station was constructed in 1911. The development of the sewerage system began only in 1920, after the October Revolution, and by 1941, the sewerage network was 1,130 kilometres (700 mi) long.
Every winter from 1895 to 1910, electric tramways were laid on the ice of the river, connecting the Senate Square, Vasilievsky island, Palace Embankment and other parts of the city. The power was supplied through the rails and a top cable supported by wooden piles frozen into the ice. The service was highly successful and ran without major accidents except for a few failures in the top electrical wires. The trams ran at the speed of 20 kilometres per hour (12 mph) and could carry 20 passengers per carriage. The carriages were converted from the used horsecars. About 900,000 passengers were transported over a regular season between 20 January and 21 March. The sparking of contacts at the top wires amused spectators in the night.
Soviet and modern periods
The first concrete bridge across Neva, the Volodarsky Bridge, was built in 1936. During World War II, from 8 September 1941 to 27 January 1944 Leningrad was in the devastating German Siege. On 30 August 1941, the German army captured Mga and came to Neva. On 8 September Germans captured Shlisselburg and cut all land communications and waterways to St. Petersburg (then Leningrad). The siege was partly relieved in January 1943, and ended on 27 January 1944.
A river station was built above the Volodarsky Bridge in 1970 which could accept 10 large ships at a time. Wastewater treatment plants were built in Krasnoselsk in 1978, on the Belyi Island in 1979–83, and in Olgino in 1987–94. The South-West Wastewater Treatment Plant was constructed in 2003–05.
Neva has very few shoals and its banks are steep, making the river suited for navigation. Utkino Backwaters were constructed in the late 19th century to park unused ships. Neva is part of the major Volga–Baltic Waterway and White Sea – Baltic Canal, however it has relatively low transport capacity because of its width, depth and bridges. Neva is available for vessels with capacity below 5,000 tonnes. Major transported goods include timber from Arkhangelsk and Vologda; apatite, granite and diabase from Kola Peninsula; cast iron and steel from Cherepovets; coal from Donetsk and Kuznetsk; pyrite from Ural; potassium chloride from Solikamsk; oil from Volga region. There are also many passenger routes to Moscow, Astrakhan, Rostov, Perm, Nizhny Novgorod, Valaam and other destinations. Navigation season on the Neva River runs from late April to November.
To the west of Shlisselburg, an oil pipeline runs under the river. The pipeline is part of the Baltic Pipeline System, which provides oil from Timan-Pechora plate, West Siberia, Ural, Kazakhstan and Primorsk to the Gulf of Finland. The 774-metre (2,539 ft) long pipeline lies 7 to 9 metres (23 to 30 ft) below the river bottom and delivers about 42 million tonnes of oil a year.
Near the Ladozhsky Bridge there is an underwater tunnel to host a gas pipeline Nord Stream. The tunnel has a diameter of 2 metres (6.6 ft) and a length of 750 metres (2,460 ft) and is laid at a maximum depth of 25 metres (82 ft).
Neva is the main source of water (96 percent) of St. Petersburg and its suburbs. From 26 June 2009, St. Petersburg started processing the drinking water by ultraviolet light, abandoning the use of chlorine for disinfection. Neva also has developed fishery, both commercial and recreational.
St. Petersburg, Neva delta
Construction of the Novo-Admiralteisky Bridge, a movable drawbridge across the river, has been approved, but will not commence before 2011.
Whereas most tourist attractions of Neva are located within St. Petersburg, there are several historical places upstream, in the Leningrad Oblast. They include the fortress Oreshek, which was built in 1323 on the Orekhovy Island at the source of Neva River, south-west of the Petrokrepost Bay, near the city of Shlisselburg. The waterfront of Schlisselburg has a monument of Peter I. In the city, there are Blagoveshchensky Cathedral (1764–95) and a still functioning Orthodox church of St. Nicholas, built in 1739. On the river bank stands the Church of the Intercession. Raised in 2007, it is a wooden replica of a historical church which stood on the southern shore of Lake Onega. That church was constructed in 1708 and it burned down in 1963. It is believed to be the forerunner of the famous Kizhi Pogost.
Old Ladoga Canal, built in the first half of the 18th century, is a water transport route along the shore of Lake Ladoga which is connecting the River Volkhov and Neva. Some of its historical structures are preserved, such as a four-chamber granite sluice (1836) and a bridge (1832).
On 21 August 1963 a Soviet twinjet Tu-124 airliner performed an emergency water landing on Neva near the Finland Railway Bridge. The plane took off from Tallinn-Ülemiste Airport (TLL) at 08:55 on 21 August 1963 with 45 passengers and 7 crew on board and was scheduled to land at Moscow-Vnukovo (VKO). After liftoff, the crew noticed that the nose gear undercarriage did not retract, and the ground control diverted the flight to Leningrad (LED) – because of fog at Tallinn. While circling above St. Petersburg at the altitude of at 1,650 feet (500 m), under unclear circumstances (lack of fuel was one of the factors), both engines stalled. The crew performed emergency landing on the Neva River barely missing some of its bridges and an 1898-built steam tugboat. The tugboat rushed to the plane and towed it to the shore. No casualties were sustained at any stage. The plane captain was first fired from job but then restored and awarded with the Order of the Red Star.