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Suomenvedenpohja
Zashchitnaya Bay (russian: Бухта Защитная, fi, Suomenvedenpohja) is the northernmost part of Vyborg Bay. It is located adjacent to the city of Vyborg ( fi, Viipuri), Leningrad Oblast, Russia. Vyborg Bay is part of the Gulf of Finland in the Baltic Sea. The Castle of Vyborg and the Monrepos Park face Zashchitnaya Bay. The old Saimaa Canal (opened in 1856), as well as the new one, connect Zashchitnaya Bay with Lake Saimaa in Finland. In the Middle Ages, the river Vuoksa had an outlet in Suomenvedenpohja, which however dried up little by little due to post-glacial rebound and was left completely dry in 1857 when the Kiviniemi rapids in Losevo (russian: Лосево, fi, Kiviniemi) were formed and the Burnaya River (, ) became the main outlet of Vuoksa. The Russian name of the bay is derived from the Russian word for defense and may be translated as "shielding". Image:Kalininsky Bridge.JPG, The Gvardeisky Strait ( fi, Kivisillansalmi) is one of the two waterways l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vyborg Bay
Vyborg Bay (, , ) is a deep inlet running northeastward near the eastern end of Gulf of Finland in the Baltic Sea. The city of Vyborg is located near the head of the gulf. The Monrepos Park is considered a jewel of the bay and a major draw for tourists. Since the mid-19th century, the bay has been connected by the Saimaa Canal to the lake Saimaa in Finland. In 1790 the bay was the scene of one of the largest naval battles in history, the Battle of Vyborg Bay with a total of 498 Russian and Swedish ships. The end of the bay is called Zashchitnaya Bay (, . In the Middle Ages the river Vuoksi had an outlet there, which however dried up little by little due to post-glacial rebound and was left completely dry in 1857 when the Kiviniemi rapids in Losevo (russian: Лосево, fi, Kiviniemi), Karelian isthmus were formed and the Burnaya River became the main outlet of Vuoksa. Lodochnyy Island lies in the middle of the bay, between Vyborg and Vysotsk Vysotsk (russian: В ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bay Of Vyborg
Vyborg Bay (, , ) is a deep inlet running northeastward near the eastern end of Gulf of Finland in the Baltic Sea. The city of Vyborg is located near the head of the gulf. The Monrepos Park is considered a jewel of the bay and a major draw for tourists. Since the mid-19th century, the bay has been connected by the Saimaa Canal to the lake Saimaa in Finland. In 1790 the bay was the scene of one of the largest naval battles in history, the Battle of Vyborg Bay with a total of 498 Russian and Swedish ships. The end of the bay is called Zashchitnaya Bay (, . In the Middle Ages the river Vuoksi had an outlet there, which however dried up little by little due to post-glacial rebound and was left completely dry in 1857 when the Kiviniemi rapids in Losevo (russian: Лосево, fi, Kiviniemi), Karelian isthmus were formed and the Burnaya River became the main outlet of Vuoksa. Lodochnyy Island lies in the middle of the bay, between Vyborg and Vysotsk Vysotsk (russian: В ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castle Of Vyborg
Vyborg Castle (russian: Выборгский замок, fi, Viipurin linna, sv, Viborgs slott) is a Swedish-built medieval fortress around which the town of Vyborg (today in Russia) evolved. The castle became the stronghold of the Swedish realm in the Karelian region. Throughout the centuries, it was the first defence of the kingdom against Russians. Its military and strategic status in the late Middle Ages was second only to the fortified capital Stockholm. Currently it serves as the site of Vyborg Regional Museum. General Vyborg Castle was one of the three major castles of Finland, the three being the castles of Turku ( in Swedish) and Hämeenlinna (), and Vyborg (). It was built as the easternmost outpost of the medieval Kingdom of Sweden: it is located on the Karelian Isthmus, on a little islet in the innermost corner of the Gulf of Finland, in a tight strait which connects Suomenvedenpohja to the Bay of Viipuri. It was originally constructed in the 1290s on the site ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Defense (military)
A military, also known collectively as armed forces, is a heavily armed, highly organized force primarily intended for warfare. It is typically authorized and maintained by a sovereign state, with its members identifiable by their distinct military uniform. It may consist of one or more military branches such as an army, navy, air force, space force, marines, or coast guard. The main task of the military is usually defined as defence of the state and its interests against external armed threats. In broad usage, the terms ''armed forces'' and ''military'' are often treated as synonymous, although in technical usage a distinction is sometimes made in which a country's armed forces may include both its military and other paramilitary forces. There are various forms of irregular military forces, not belonging to a recognized state; though they share many attributes with regular military forces, they are less often referred to as simply ''military''. A nation's military may ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burnaya River
The Burnaya (, ) is a young rapid river in Priozersky District of Leningrad Oblast, Russia, on the Karelian Isthmus, which emerged in 1818. It flows from Lake Sukhodolskoye to Lake Ladoga and is a part of Vuoksi River drainage basin. Before the Winter War and Continuation War it was located in Finland, known under the name Taipaleenjoki. Originally waters of Lake Suvanto (Lake Sukhodolskoye) quietly flowed into the Vuoksi through a waterway at Kiviniemi. However, in 1818 the channel that had been dug to drain spring flood waters from Suvanto into Lake Ladoga unexpectedly turned into the Taipaleenjoki, which started draining Suvanto and decreased its level by . The Kiviniemi waterway dried out. In 1857 the channel was dug there, but the stream reversed direction, revealed rapids and rendered navigation at Kiviniemi impossible. Since 1857 Lake Sukhodolskoye and the Burnaya River have constituted the southern armlet of Vuoksi River, which has decreased the level of the original north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Losevo, Leningrad Oblast
Losevo (russian: Лосево; fi, Kiviniemi) is a rural locality (a station settlement) in Priozersky District, Leningrad Oblast, located at the junction of Vuoksi River and Lake Sukhodolskoye on Karelian Isthmus. It is a railway station of the Saint Petersburg–Khiytola railroad. Before the Winter War and Continuation War, it was a village of the Sakkola municipality of Finland known as Kiviniemi. Originally waters of Lake Sukhodolskoye quietly flowed into Vuoksi, but in 1818, as Burnaya River had emerged and started draining Sukhodolskoye into Lake Ladoga, the level of the former decreased dramatically by and the waterway connecting it to Vuoksi dried out. In 1857, the channel was dug, but the stream reversed direction, revealed rapids, and rendered navigation impossible. Since 1857 Lake Sukhodolskoye and Burnaya River have constituted the southern armlet of Vuoksi River, which has decreased the level of the original northern armlet by . Before the construction of Saint P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Post-glacial Rebound
Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy), the deformation of the Earth's crust in response to changes in ice mass distribution. The direct raising effects of post-glacial rebound are readily apparent in parts of Northern Eurasia, Northern America, Patagonia, and Antarctica. However, through the processes of ''ocean siphoning'' and ''continental levering'', the effects of post-glacial rebound on sea level are felt globally far from the locations of current and former ice sheets.Milne, G.A., and J.X. Mitrovica (2008) ''Searching for eustasy in deglacial sea-level histories.'' Quaternary Science Reviews. 27:2292–2302. Overview During the last glacial period, much of northern Eu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vuoksa
The Vuoksi (russian: Вуокса, historically: "Uzerva"; fi, Vuoksi; sv, Vuoksen) is a river running through the northernmost part of the Karelian Isthmus from Lake Saimaa in southeastern Finland to Lake Ladoga in northwestern Russia. The river enters Lake Ladoga in three branches, an older main northern branch at Priozersk (Käkisalmi), a smaller branch a few kilometers to the north of it, and a new southern branch entering further southeast as Burnaya River (Finnish: Taipaleenjoki), which has become the main stream in terms of water discharge. Since 1857, the old northern distributaries drain only the lower reaches of the Vuoksi basin and are not fed by Lake Saimaa. The northern and southern branches actually belong to two separate river systems, which at times get isolated from each other in dry seasons. The descent between Lake Saimaa and Lake Ladoga is . The entire run of the river is via the Priozersk branch, or via the Taipale (Burnaya) branch. It has a drainage bas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saimaa Canal
The Saimaa Canal ( fi, Saimaan kanava; sv, Saima kanal; russian: Сайменский канал) is a transportation canal that connects lake Saimaa with the Gulf of Finland near Vyborg, Russia. The canal was built from 1845 to 1856 and opened on 7 September 1856 (Old Style: 26 August 1856). It was overhauled and widened in 1963–1968. A system of inland waterways and canals in the 120 interconnected lakes of the south-central and south-east part of Finland (Finnish Lakeland) are reached through the canal. The network of deep channels in Lake Saimaa with at least a draught of covers . The deep channels extend all the way to Kuopio in Central Finland. Topography The canal begins near Lauritsala, Lappeenranta, Finland, at coordinates () and ends in Vyborg, Russia, at coordinates (), connecting Lake Saimaa and the Vyborg Bay. On the way, it connects Lake Nuijamaa, on the Finnish–Russian border at coordinates (), and three smaller lakes in Russia. Dimensions * Length: ** Fi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saimaa
Saimaa ( , ; sv, Saimen) is a lake located in the Finnish Lakeland area in southeastern Finland. At approximately , it is the largest lake in Finland, and the fourth largest natural freshwater lake in Europe. The name Saimaa likely comes from a non-Uralic, non-Indo European substrate language. History It was formed by glacial melting at the end of the Ice Age. Major towns on the lakeshore include Lappeenranta, Imatra, Savonlinna, Mikkeli, Varkaus, and Joensuu. About 6000 years ago, ancient Lake Saimaa, estimated to cover nearly at the time, was abruptly discharged through a new outlet. The event created thousands of square kilometres of new residual wetlands. Following this event, the region saw a population maximum in the decades following only to later return to an ecological development towards old boreal conifer forests which saw a decline in population. Topography The Vuoksi River flows from Saimaa to Lake Ladoga. Most of the lake is spotted with islands, and narrow can ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mon Repos (Vyborg)
Mon Repos or Monrepos (russian: Монрепо́, from the French for "my rest") is an extensive English landscape park in the northern part of the rocky island of Linnasaari (Tverdysh, Slottsholmen) outside Vyborg, Russia. The park lies along the shoreline of the Zashchitnaya Bay, Zashchitnaya inlet of Vyborg Bay and occupies about of land. The manor of Monrepos was established by Baron Ludwig Heinrich von Nicolay who bought this parcel of land in 1788. The estate was considered a jewel of Old Finland and belonged to his descendants until the Soviet takeover in 1944. The core of the baronial estate consists of the Neoclassical main house (designed by Giuseppe Antonio Martinelli) (today derelict) and the library house. The seaside park is strewn with glacially deposited boulders, scenic cliffs and wooden pavilions. It is considered a landmark in the evolution of the Romanticism, Romantic taste for landscape gardening. The mausoleum of Baron Nicolay was designed by Pietro Gonz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
