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80-744: The Strait of Kerch connects the Sea of Azov and the Black Sea . Administratively, Tuzla Island is part of the Kerch municipality of eastern Crimea . Officially the island does not have a permanent settlement; however, it had a border station (the Simferopol Detachment of the Border Service of Ukraine ), a small fishing settlement with a few private garden lots, and two vacation resorts, "Albatross" and "Two Seas". The island's electricity

160-600: A causeway from the Taman Peninsula towards the island to revive the eroded peninsula without any preliminary consultations with the Ukrainian government authorities. After the construction of the 3.8 km causeway was suspended exactly at the Russian-Ukrainian border, the distance between the causeway and the island was 1,200 m (3,900 ft). The causeway increased the intensity of the stream in

240-546: A maximum of 3 metres. They cover an area of 2,560 square kilometres (990 sq mi) in the northeastern Crimea which is separated from the sea by the Arabatsk Spit. North of the spit lies the city of Henichesk (population 22,500) and south of it is the Bay of Arabat . Syvash accepts up to 1.5 km of Azov water per year. Because of the lagoons' wide extent and shallowness, the water rapidly evaporates, resulting in

320-750: A northern extension of the Black Sea. The sea is bounded by Russia on the east, and by Ukraine on the northwest and southwest (the parts of Ukraine bordering the sea are currently under Russian occupation ). It is an important access route for Central Asia , from the Caspian Sea via the Volga–Don Canal . The sea is largely affected by the inflow of the Don , Kuban , and other rivers, which bring sand, silt , and shells, which in turn form numerous bays, limans , and narrow spits . Because of these deposits,

400-714: A result of the Russo-Turkish War (1710–1711) and the Treaty of the Pruth , Azov was returned to Turkey and the Russian Azov fleet was destroyed. The city was recaptured by Russia in 1737 during the Russo-Austrian-Turkish War (1735–1739) . However, as a result of the consequent Treaty of Niš , Russia was not allowed to keep the fortress and military fleet. Another major military campaign on

480-655: A width of 4 kilometres (2.5 mi) and a maximum depth of 15 metres (49 ft). The narrowness of the Kerch Strait limits the water exchange with the Black Sea. As a result, the salinity of the Sea of Azov is low; in the open sea it is 10–12 on the Practical Salinity Scale (PSS), about one third of the salinity of the oceans; it is even lower (2–7 (PSS)) in the Taganrog Bay at the northeast end of

560-674: Is sacred lotus . The number of species is large; for example, the Belosaraysk and Berdyansk spits alone contain more than 200 each. Some spits are declared national nature reserves , such as Beglitsk, Belosaraysk, Krivaya and Berdyansk Spits. Estuaries and spits of the sea are rich in birds, mostly waterfowl, such as wild geese, ducks and seagulls. Colonies of cormorants and pelicans are common. Also frequently observed are swans, herons, sandpipers and many birds of prey. Mammals include foxes, wild cats, hares, hedgehogs, weasels , martens and wild boar. Muskrats were introduced to

640-530: Is 1.5–2 times larger in summer than in winter. Average water temperatures are 0–1 °C in winter (2–3 °C in the Kerch Strait) and 24–25 °C in summer, with a maximum of about 28 °C on the open sea and above 30 °C near the shores. During the summer, the sea surface is usually slightly warmer than the air. Because of the shallow character of the sea, the temperature usually lowers by only about 1 °C with depth, but in cold winters,

720-656: Is Berdyansk Bay with two cities, Berdyansk (population 112,000) and Primorsk (population 13,900). Further north again lies Belosaraysk Bay with Belosaraysk Spit, formed by the river Kalmius . The major city in the area is Mariupol (population 491,600). Then, approaching the Taganrog Bay and very close to Taganrog , are the Mius Liman and Krivaya Spit formed by the Mius River . With an area of about 5,600 square kilometres (2,200 sq mi), Taganrog Bay

800-575: Is about 100 m (330 ft), with water depth along the former shallow no more than 60 cm (24 in). Disputes about the right of passage were resolved by a 2003 bilateral agreement on cooperation in the use of the Sea of Azov and the Strait of Kerch, which made these water bodies shared internal waters of both countries, but new tensions arose after the 2014 Russian annexation of Crimea and Sevastopol. Since Russia annexed Crimea in March 2014,

880-437: Is considered an internal sea of Russia and Ukraine, and its use is governed by an agreement between these countries ratified in 2003. The sea is 360 kilometres (220 mi) long and 180 kilometres (110 mi) wide and has an area of 39,000 square kilometres (15,000 sq mi); it is the smallest sea within the countries of the former Soviet Union. The main rivers flowing into it are the Don and Kuban ; they ensure that

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960-481: Is for passage by Russian marine traffic. On December 10, 2021, the Ukrainian Navy announced that Russia had blocked off nearly 70 percent of the Sea of Azov, issuing navigation warnings, ostensibly to conduct artillery fire exercises on the sea ..."near Mariupol, Berdyansk and Henichesk." It raised apprehension regarding a potential Russian invasion since it had begun amassing tens of thousands of troops near

1040-741: Is located on the Kerch peninsula, and the Taman peninsula contains the delta of the Kuban , a major Russian river. The strait is 41 kilometres long and 4 to 15 kilometres wide. Its narrowest part lies on the Sea of Azov side, restricted by the Chushka Spit which faces southwards in consequence of the outflow from the Azov to the Black Sea. The Strait of Kerch is spanned by the Crimean Bridge , which

1120-399: Is one of the world's longest spits; three other spits, Fedotov Spit, Achuevsk Spit and Obitochna Spit, are longer than 30 km. Most spits stretch from north to south and their shape can significantly change over just several years. A remarkable feature of the Sea of Azov is the large complex of shallow lagoons called Syvash or "Rotten Sea". Their typical depth is only 0.5–1 metres with

1200-400: Is the largest bay of the Sea of Azov. It is located in the north-eastern part of the Sea and is bounded by the Belosaraysk and Dolgaya Spits . The Don flows into it from the north-east. On its shores stand the two principal cities of the Sea of Azov, Taganrog (population 257,600) and Azov (population 83,200). South-east of the bay is Yeysk Liman. It lies entirely on the continent, entering

1280-604: Is the shallowest sea in the world, with the depth varying between 0.9 and 14 metres (3 and 46 ft). There is a constant outflow of water from the Sea of Azov to the Black Sea. The name is likely to derive from the settlement of an area around Azov , whose name comes from the Kipchak Turkish asak or azaq 'lowlands'. A Russian pseudo-etymology , however, instead derives it from an eponymous Cuman prince named "Azum" or "Asuf", said to have been killed defending his town in 1067. A formerly common spelling of

1360-515: Is uncertain but probably the Huns , after defeating the Alans people who had settled in the region from central Asia, overran it in the late 4th century. The Sea of Azov was frequently the scene of military conflicts between Russia, pursuing naval expansion to the south, and the major power in the region, Turkey . During the Russo-Turkish War (1686–1700) , there were two campaigns in 1695–96 to capture

1440-603: The Black Sea in 1997, and the historic presence of large whales such as minke whales in the Black Sea is recorded, although it is unclear whether these mammals historically occurred in the Azov basin. For centuries, the Sea of Azov has been an important waterway for the transport of goods and passengers. The first modern ironworks in Imperial Russia were located upstream on the Kalmius River at Donetsk , originally named Hughesovka ( Russian : Юзовка ). It

1520-665: The Black Sea port Odesa , passed under the Crimean Bridge, and arrived in Mariupol . Tensions increased further after the Kerch Strait incident in November 2018, when Russia seized three Ukrainian Navy vessels attempting to enter the Sea of Azov. Control of the western shore of the Sea is vital to the economy of Ukraine but it is also of immense strategic importance to Russia, as a land route to Crimea as well as it

1600-598: The Sea of Surozh after the adjacent city now known as Sudak . It was known in Ottoman Turkish as the Balük-Denis ("Fish Sea") from its high productivity. There are traces of Neolithic settlement in the area now covered by the sea. In 1997, William Ryan and Walter Pitman of Columbia University published a theory that a massive flood through the Bosporus occurred in ancient times. They claim that

1680-500: The Siberian Anticyclone which brings cold and dry air from Siberia with winds of 4–7 m/s, sometimes up to 15 m/s. Those winds may lower the winter temperatures from the usual −1 to −5 °C to below −30 °C. The mean mid-summer temperatures are 23–25 °C with a maximum of about 40 °C. Winds are weaker in summer, typically 3–5 m/s. Precipitation varies between 312 and 528 mm/year and

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1760-475: The Taman Peninsula . Tuzla Island was formed when the spit that continued the Taman peninsula suffered from massive erosion during a major storm in 1925. In ancient times (2,500 years ago) the sea level was four meters below the present, which meant that at the site of modern Tuzla was quite an extensive area of land, which was part of the Taman Peninsula. Taman Peninsula itself at that time was part of

1840-701: The Ukrainian SSR , which after the dissolution of the Soviet Union in 1991 became the state of Ukraine . There was a territorial dispute over the ownership of the island between Ukraine and Russia in October 2003. The Russian authorities claimed the 1954 transfer of Crimea to Ukraine had only included the continental parts of Crimea, even though the Tuzla Island had been administratively part of Crimea since 1941. The Russian side started to build

1920-594: The annexation of Crimea by Russia in 2014. The last election of parliament took place on 31 October 2010 (see 2010 Crimean parliamentary election ) and was won by the Party of Regions and the Communist Party of Ukraine . On 27 February 2014, unidentified armed men took over the parliament and hoisted the flag of Russia over it. On 15 March 2014 the Verkhovna Rada of Ukraine officially dissolved

2000-479: The Black Sea in the early 20th century and settled in the Sea of Azov. Its current density is 7 kg/m . From 1956, Rapana venosa is observed in the Sea of Azov, but it could not adjust to low salinity and therefore is limited to the neighborhood of the Kerch Strait. Several Sea of Azov mollusks, such as shipworm ( Teredo navalis ), soft-shell clam ( Mya arernaria ), Mediterranean mussel ( Mytilus galloprovincialis ) and Anadara inaequivalvis , originate from

2080-409: The Black Sea plankton which does not adapt well to the low salinity of the Sea of Azov and concentrates near the Kerch Strait, fishes and invertebrates of the Black Sea adjust well. They are often stronger than the native species, are used to the relatively low temperatures of the Black Sea and survive winter in the Sea of Azov well. Balanus improvisus is the first benthos species which spread from

2160-552: The Black Sea. Another example of invading species is the Dutch crab Rhithropanopeus harrisii which is observed both in saline and freshwater parts. Formerly three types of dolphins, short-beaked common dolphin , common bottlenose dolphin and harbour porpoise , regularly visited the Sea of Azov from the Black Sea although the common dolphin usually avoided the basin and Kerch Strait due to low salinity. One sub-species of harbour porpoise, Phocoena phocoena relicta , used to live in

2240-607: The Black and Caspian Seas were vast freshwater lakes, but in about 5600 BC the Mediterranean spilled over a rocky sill at the Bosporus, creating the current link between the Black and Mediterranean Seas. Subsequent work has been done both to support and to discredit this theory, and archaeologists still debate it. This has led some to associate this catastrophe with prehistoric flood myths . The Maeotian marshes around

2320-513: The Kuban delta, and was separated from the rest of the land by river channels, which drained into the Sea of Azov and the Black Sea. Some historians identify Tuzla as the island of Alopeka, mentioned by ancient authors, located in the waters of Cimmerian Bosporus, and when the island periodically joined to the Asian shore of the Bosporus, the resulting braid was used as the entrance to the passage through

2400-539: The Maeotian or Maeotic Sea ( Mæotium or Mæoticum Æquor ); the Cimmerian or Scythican Swamps ( Cimmeriae or Scythicæ Paludes ); and the Cimmerian or Bosporic Sea ( Cimmericum or Bosporicum Mare ). The Maeotians themselves were said by Pliny to call the sea Temarunda (alternative spellings Temarenda and Temerinda), meaning "Mother of Waters". The medieval Russians knew it as

2480-574: The Russian Federation agreed in a treaty to treat the sea and the Kerch Strait as shared internal waters. In September 2018, Ukraine announced the intention to add navy ships and further ground forces along the coast of the Sea of Azov, with the ships based at Berdiansk . The military posturing was exacerbated following the construction of the Crimean Bridge , which is too low to allow passage of Panamax ships into Ukraine's port. Late that September, two Ukrainian vessels departed from

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2560-599: The Russian fleet blocked Azov by sea. On 14 June, the Turkish fleet tried to break the blockade but, after losing two ships, retreated to the sea. After intensive bombardment of the fortress from land and sea, on 17 July the Russian army broke the defense lines and occupied parts of the wall. After heavy fighting, the garrison surrendered on 17 July. After the war, the Russian fleet base was moved to Taganrog and Azov, and 215 ships were built there between 1696 and 1711. In 1711, as

2640-558: The Sea of Azov and was therefore called "Azov dolphin" ( азовка , azovka) in the Soviet Union. Nowadays, dolphins are rarely observed in the Sea of Azov. This is attributed to shallowing of the sea, increasing navigation activities, pollution, and reduction in the fish population. Various species of pinnipeds and belugas were introduced into Black Sea by mankind and later escaped either by accidental or purported causes. Of these, grey seal has been recorded within Kerch Strait and Sea of Azov. Mediterranean monk seals became extinct in

2720-493: The Sea of Azov form bays, lagoons and limans . The sand, silt and shells they bring are deposited in the areas of reduced flow, that is the sides of the bays, forming narrow sandbanks called spits . Typical maximum depth in the bays and limans is a few metres. Because of shallow waters and abundant rivers, the spits are remarkably long and numerous in the sea – the Arabat Spit stretches over 112 kilometres (70 mi) and

2800-574: The Sea of Azov region. Among them, there are 50 rare and 19 endangered species, and the sturgeon Acipenser nudiventris is probably extinct in the region. The fauna of the freshwater Taganrog Bay is much poorer – it consists of 55 species from 36 genera and 16 families; among them, three species are rare and 6 are endangered. The shores of the Sea of Azov contain numerous estuaries and marshes and are dominated by reeds, sedges , Typha and Sparganium . Typical submerged plants are Charales , pond weed , hornworts and water lilies . Also common

2880-509: The Sea of Azov took place during the Crimean War of 1853–56. A naval and ground campaign pitting the allied navies of Britain and France against Russia took place between May and November 1855. The British and French forces besieged Taganrog , aiming to disrupt Russian supplies to Crimea. Capturing Taganrog would also result in an attack on Rostov, which was a strategic city for Russian support of their Caucasian operations. On 12 May 1855,

2960-583: The Sea of Azov. The number of species is dominated by diatoms and green algae ; blue-green algae and pyrophites are significant, and euglena and yellow-green algae form only 5% of the species. Green algae are mostly responsible for the colour of the sea in the satellite images (see photos above). Regarding zooplankton , the fresh waters of the Tanganrog Bay are inhabited by cladocera , copepoda and rotifers , such as Brachionus plicatilis , Keratella curdata and Asplanchna . Western part of

3040-500: The Sea. The long-term variations of salinity on the PSS are low, and are mostly caused by changes in humidity and precipitation. Although more than 20 rivers flow into the sea, mostly from the north, two of them, the Don and Kuban rivers, account for more than 90% of water inflow. The contribution of the Don is about twice that of the Kuban. The Kuban delta is located at the southeast, on

3120-711: The Taganrog Bay through the Yeysk and Glafirovsk Spits, and is the mouth of the Yeya River . Yeysk Spit is part of Yeysk city, which has a population of 87,500. It extends into the prominent Yeysk peninsula, which is tipped in the north-west by the Dolgaya Spit . South of it, also enclosed by the continent, lies Beisug Liman, which is restricted by the Yasensk Spit and is fed by the Beysug River . South-west of

3200-491: The allied forces easily captured Kerch and gained access to the Sea of Azov, and on 22 May they attacked Taganrog. The attack failed and was followed by a siege. Despite the vast superiority of the allied forces (about 16,000 soldiers against fewer than 2,000), the city withstood all attempts to capture it, which ended around August 1855 with the retreat of the allied army. Individual coastal attacks continued without success and ceased in October 1855. In December 2003, Ukraine and

3280-458: The annual inflow and outflow of water to the sea, averaged over the period from 1923 to 1985, are as follows: river inflow 38.6 km , precipitation 15.5 km , evaporation 34.6 km , inflow from the Black Sea 36–38 km , outflow 53–55 km . Thus, about 17 km of fresh water is outflowing from the Azov Sea to the Black Sea. The depth of Azov Sea is decreasing, mostly due to

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3360-405: The anoxic waters forming in a layer 0.5 to 4 metres (2–13 ft) in thickness. The occurrence of the anoxic layer is attributed to seasonal eutrophication events associated with increased sedimentary input from the Don and Kuban Rivers. This sedimentary input stimulates biotic activity in the surface layers, in which organisms photosynthesise under aerobic conditions. Once the organisms expire,

3440-507: The area in the early 20th century and are hunted for their fur. Some ichthyofauna species, such as anchovy , garfish , Black Sea whiting and pickerel , visit the Sea of Azov from the Black Sea for spawning. This was especially frequent in 1975–77 when the salinity of the southern Sea of Azov was unusually high, and additional species were seen such as bluefish , turbot , chuco, spurdog , Black Sea salmon , mackerel and even corkwing wrasse , rock hopper, bullhead and eelpout . Unlike

3520-475: The bays, where silt has built up, the average depth is about 1 metre (3 ft). The sea bottom is also relatively flat with the depth gradually increasing from the coast to the centre. The Sea of Azov is an internal sea with passage to the Atlantic Ocean going through the Black, Marmara , Aegean and Mediterranean seas. It is connected to the Black Sea by the Strait of Kerch, which at its narrowest has

3600-697: The central Russia – thus connecting major cities such as Moscow, Volgograd and Astrakhan . Currently, the major ports are in Taganrog , Mariupol , Yeysk and Berdyansk . Supreme Council of Crimea Verkhovna Rada of Crimea or the Supreme Council of Crimea , officially the Supreme Council of the Autonomous Republic of Crimea , was the Ukrainian legislative body for the Autonomous Republic of Crimea before

3680-516: The construction of the causeway. Due to the conflict, on December 2, 2003, a border patrol station of Ukraine was installed on the island. On December 5, 2003, the Cabinet of Ukraine issued Order #735p in regard to urgent measures to save the island. On July 4, 2004, the Cabinet of Ukraine issued Order #429p, which foresaw the construction of shore reinforcement structures and population transfer from

3760-412: The dead organic matter sinks to the bottom of the sea where bacteria and microorganisms, using all available oxygen, consume the organic matter, leading to anoxic conditions. Studies have shown that in the Sea of Azov, the exact vertical structure is dependent on wind strength and sea surface temperature , but typically a 'stagnation zone' lies between the oxic and anoxic layers. Many rivers flowing into

3840-426: The difference can reach 5–7 °C. The winds cause frequent storms, with the waves reaching 6 metres in the Taganrog Bay, 2–4 metres near the southern shores, and 1 metre in the Kerch Strait. In the open sea, their height is usually 1–2 metres, sometimes up to 3 metres. Winds also induce frequent seiches – standing waves with an amplitude of 20–50 cm and lasting from minutes to hours. Another consequence of

3920-412: The east side of the Kerch Strait. It is over 100 km long and covers a vast flooded area with numerous channels. Because of the spread, the delta has low contrast in satellite images, and is hardly visible in the map. The Don flows from the north into the large Taganrog Bay . The depth there varies between 2 and 9 metres, while the maximum depth is observed in the middle of the sea. Typical values of

4000-479: The end of the siege of Mariupol , Russia fully captured the city and blocked off Ukraine's access to the sea by controlling the entire north Pryazovia . The International Hydrographic Organization defines the limit of the Sea of Azov in the Kertch Strait [ sic ] as "The limit of the Black Sea ", which is itself defined as "A line joining Cape Takil and Cape Panaghia (45°02'N)". The sea

4080-459: The flooding territories. Following the 2003 conflict, the Supreme Council of Crimea ordered the establishment of a new settlement on the island. However, on September 6, 2006, the Kerch city administration refused to create such a settlement, as it conflicted with the administrative-territorial composition of the city. The distance to the unfinished causeway that stretches from the Taman peninsula

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4160-701: The high salinity of 170 on the practical salinity scale . For this reason Syvash has long had an important salt-producing industry. North of the Arabat Spit is the Molochnyi Liman with the associated Fedotov Spit (45 km long) which are formed by the Molochna River . Farther north, between the Fedotov Spit and Obytochna Spit (30 km long), lies Obytochny Bay. Further north, between Obytochna Spit and Berdyansk Spit (23 km long),

4240-434: The introduction of icebreakers , navigation was halted in the winter. Historically, the sea has had rich marine life, both in variety, with over 80 fish and 300 invertebrate species identified, and in numbers. Consequently, fishing has long been a major activity in the area. The annual catch of recent years was 300,000 tonnes, about half of which are valuable species (sturgeon, pike-perch , bream , sea-roach , etc.). This

4320-488: The island has been transferred into the possession of Russia's central government by the newly established Crimean authorities and was used as a stepping stone for a new bridge linking Crimea to mainland Russia . Sea of Azov The Sea of Azov is an inland shelf sea in Eastern Europe connected to the Black Sea by the narrow (about 4 km (2.5 mi)) Strait of Kerch , and sometimes regarded as

4400-488: The island. On October 23, 2003, the Ukrainian parliament issued a resolution "to eliminate a threat to the territorial integrity of Ukraine that appeared as a result of dam construction by the Russian Federation in the strait of Kerch". A provisional special parliamentary commission was created to investigate the case more thoroughly. On October 30–31, 2003, talks started between Ukraine and Russia that led to suspension of

4480-721: The liman, the 31 km long Achuevsk Spit runs along the coastline. Between the Achuevsk spit and Beisug Liman stands Primorsko-Akhtarsk with 32,165 inhabitants. In the south, the Sea of Azov is connected to the Black Sea via the Strait of Kerch , which is bordered to the west by the Kerch peninsula of the Crimea and to the east by the Russian Taman peninsula in Krasnodar Krai . The city of Kerch (population 151,300)

4560-400: The more famous Bosporus at the other end of the Black Sea . Briefly annexed by Pontus from the late 2nd century BC, it stretched along both southern shores of the Sea of Azov from the time of Greek colonization to the end of the Roman Empire , serving as a client kingdom which exported wheat, fish, and slaves in exchange for Greek and Roman manufactures and luxuries. Its later history

4640-406: The mouth of the Tanais River (the present-day Don ) were famous in antiquity , as they served as an important check on the migration of nomadic people from the Eurasian steppelands . The Maeotians themselves lived by fishing and farming, but were avid warriors able to defend themselves against invaders. Misled by its strong currents, ancient geographers had only a vague idea of the extent of

4720-487: The name in English was the Sea of Azoff . . In antiquity , the sea was known as the Maeotis Swamp ( Greek : Μαιῶτις λίμνη , hē Maiōtis límnē ; Latin : Palus Maeotis ), from the marshlands to its northeast. It remains unclear whether it was named for the nearby Maeotians or viceversa if that name was an exonym , broadly applied to various peoples who happened to live beside it. Other names included Lake Maeotis or Maeotius ( Mæotius or Mæotis Lacus );

4800-401: The narrowest part of the Cimmerian Bosporus, which is located between Alopekoy and the European shore of the Bosporus. Other historians and geologists reject such a hypothesis, believing that neither the island nor the Tuzla Spit existed in ancient times. Before the Soviet Union entered World War II in 1941, it was part of the Crimean Oblast . This in turn on February 19, 1954, became a part of

4880-434: The near future, due to ongoing deposition of sediments from rivers. In the 1st century, Strabo reckoned the distance from the Cimmerian Bosporus (the Strait of Kerch ) to the mouth of the Tanais at 2200 stadia , a roughly correct figure, but did not know that its width continuously narrows. Milesian colonization began in the 7th century BC. The Bosporan Kingdom was named for the Cimmerian Bosporus rather than for

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4960-440: The predominance of northern winds and the water inflow from the rivers; its average speed is 10–20 cm/s, reaching 30–40 cm in the narrowest parts. Although the sea is not subject to tidal variation, there are seasonal changes in the observed sea level of up to 10–20 inches (250–510 mm), caused by seasonal variations in river outflows. The shallowness and low salinity of the sea make it vulnerable to freezing during

5040-660: The river-induced deposits. Whereas the past hydrological expeditions recorded depths of up to 16 metres, more recent ones could not find places deeper than 13.5–14 metres. This might explain the variation in the maximum depths among different sources. The water level fluctuates by some 20 cm over the year due to the snow melts in spring. The Taman Peninsula has about 25 mud volcanoes , most of which are active. Their eruptions are usually quiet, spilling out mud, and such gases as methane, carbon dioxide and hydrogen sulfide , but are sometimes violent and resemble regular volcanic eruptions. Some of those volcanoes are under water, near

5120-412: The sea bottom is relatively smooth and flat, with the depth gradually increasing toward the middle. Because of the river inflow, water in the sea has low salinity and a high amount of biomass (such as green algae ) that affects the water colour. Abundant plankton result in unusually high fish productivity. The sea shores and spits are low; they are rich in vegetation and bird colonies. The Sea of Azov

5200-439: The sea is the variable salinity – low in the large bays and higher in the open sea, especially near the Kerch Strait. Therefore, the plankton species are distributed inhomogeneously in the Sea of Azov. Although many additional species are brought in from the saltier Black Sea, most of them cannot adjust to the variable salinity of the Sea of Azov, except for the euryhaline species. About 600 species of planktonic algae are known in

5280-472: The sea, which is more saline, hosts three forms of Acartia clausi , as well as Centropages ponticus , meroplankton and larvae of gastropoda , bivalvia and polychaete . Benthos species reside mostly at the sea bottom and include worms, crustaceans , bottom protists , coelenterata , and mollusks . Mollusks account for 60–98% of the invertebrate biomass at the Sea of Azov bottom. There are 183 ichthyofauna species from 112 genera and 55 families in

5360-407: The sea, whose fresh water caused them to typically label it a "swamp" or a "lake". Herodotus (5th century BC) judged it as large as the Black Sea , while the Pseudo-Scylax (4th century BC) thought it about half as large. It was long believed to provide direct communication with the Arctic Ocean . Polybius (2nd century BC) confidently expected that the strait to the Sea of Azov would close in

5440-443: The shallow waters, the development of aquatic life in the Sea of Azov is more characteristic of a lagoon, and the plankton patterns are rather similar in the open sea and near the shores. Despite its shallowness, the water has low transparency, so bottom plants are poorly developed and most algae are of planktonic type. The sea is characterised by high concentrations of organic matter and long blooming periods. Another specific feature of

5520-416: The shores of the peninsula. A major eruption on 6 September 1799, near Golubitskaya stanitsa , lasted about 2 hours and formed a mud island 100 metres in diameter and 2 metres in height; the island was then washed away by the sea. There were similar eruptions in 1862, 1906, 1924, 1950 and 1952. The current vertical profile of the Sea of Azov exhibits oxygenated surface waters and anoxic bottom waters, with

5600-399: The siege was lifted. The second campaign involved both ground forces and the Azov fleet, which was built in Moscow Oblast, Voronezh, Bryansk and other regions between winter 1695 and spring 1696. In April 1696, the army of 75,000 headed by Aleksei Shein moved to Azov by land and by ship via the Don River to Taganrog. In early May, they were joined by another fleet led by Peter I. On 27 May,

5680-402: The southeast Ukraine border and had begun a propaganda war against the Kyiv government. The Russians seized three Ukrainian military vessel as the boats were trying to cross the strait, and captured 24 sailors who were finally released after months of negotiations. On February 24, 2022, Russian forces began shelling Mariupol at the start of the 2022 Russian invasion of Ukraine . By May, with

5760-499: The strait and the deterioration of the island. To prevent the deterioration, the government of Ukraine funded groundwork to deepen the bed of the strait. Ukraine refused to recognize the strait as inner waters of both countries until 2003. On October 21, 2003, the Border Service of Ukraine briefly detained the Russian tugboat Truzhenik , which had crossed the State Border of Ukraine and conducted photo and video surveillance of

5840-465: The then Turkish fortress of Azov defended by a garrison of 7,000. The campaigns were headed by Peter I and aimed to gain Russian access to the Sea of Azov and Black Sea. The first campaign began in the spring of 1695. The Russian army consisted of 31 thousand men and 170 cannons and included selected trained regiments and Cossacks . It reached Azov on 27–28 June and besieged it by land by 5 July. After two unsuccessful assaults on 5 August and 25 September,

5920-401: The waters of the sea have comparatively low salinity and are almost fresh in places, and also bring in huge volumes of silt and sand. Accumulation of sand and shells results in a smooth and low coastline, as well as in numerous spits and sandbanks. The Sea of Azov is the shallowest sea in the world with an average depth of 7 metres (23 ft) and maximum depth of 14 metres (46 ft); in

6000-416: The winds is water currents . The prevailing current is a counterclockwise swirl due to the westerly and south-westerly winds. Their speed is typically less than 10 cm/s, but can reach 60–70 cm/s for 15–20 m/s winds. In the bays, the flow is largely controlled by the inflow of the rivers and is directed away from the shore. In the Kerch Strait, the flow is normally toward the Black Sea due to

6080-426: The winter. Fast ice bands ranging from 7 km in the north to 1.5 km in the south can occur temporarily at any time from late December to mid-March. Several ships were trapped in ice in 2012 when it froze over. The ice thickness reaches 30–40 centimetres (12–16 in) in most parts of the sea and 60–80 cm in the Taganrog Bay. The ice is often unstable and piles up to the height of several metres. Before

6160-481: Was also important for the transportation of iron ores from the mines of the Kerch peninsula to the processing plant of Azovstal in Mariupol (formerly Zhdanov), Ukraine; this activity stopped after the closure of the mines in the 1990s. Navigation increased after the construction in 1952 of the Volga–Don Canal which connected the Sea of Azov with the Volga River – the most important riverine transport route in

6240-458: Was opened in May 2018. This is a major geopolitical issue since shipping vessels over a certain size can not pass under the span. Since then Russia has been accused of interdicting shipping through the Kerch Strait. The sea is relatively small and nearly surrounded by land. Therefore, its climate is continental with cold winters and hot and dry summers. In autumn and winter, the weather is affected by

6320-569: Was partly due to extremely high biological productivity of the sea, which was stimulated by the strong supply of nutrients from numerous rivers feeding the sea, low water salinity, ample heating due to shallow waters and long vegetation period. However, diversity and numbers have been reduced by artificial reduction of river flow (construction of dams), over-fishing and water-intense large-scale cultivation of cotton, causing increasing levels of pollution . Fish hauls have rapidly decreased and in particular anchovy fisheries have collapsed. Because of

6400-421: Was supplied by two diesel power stations. The island also had a pier and a helicopter pad. A second pier located near the fishing settlement was in critical condition and not in use. Two concrete surface roads run along the island. From May through October, a store operated at the "Two Seas" resort. The island was used during the construction of the Crimean Bridge , which opened in May 2018, connecting Crimea to

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