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Black Sea Location On World Map

The Black Sea is located in southern Europe. It is bordered by Ukraine to the north, Russia to the northeast, Georgia to the east, Turkey to the south, Bulgaria and Romania to the west.

Russia Ukraine War: Turkey’s Power Over The Black Sea Explained

The Black Sea reaches depths of over 7,250 feet (2,210 meters) in the south-central region.

The Black Sea is a salty sea, but it is less salty than the sea. The salinity of the surface waters of the Black Sea is 17 to 18 parts per thousand, which is half of that of the sea. The largest increase in salinity by 21/1000 occurs in the Black Sea at depths of 160 to 500 feet (50 to 150 meters).

A notable feature of the Black Sea is that oxygen (and potentially rich marine life) dissolves only at the upper water level. There is no oxygen below about 230 to 330 feet (70 to 100 meters) in the center of the ocean and 330 to 500 feet (100 to 150 meters) near the edge of the ocean. In other words, its low levels were almost biologically dead, not because of contamination, but because of the continued weak ventilation of the deeper layers.

There are about 180 species of fish in the Black Sea, a fifth of which are commercially important. The most important are khamsa, sprat, horse mackerel and others, including the spiny dog, the largest small shark in the Black Sea.

Vector Map Of Black Sea Region Royalty Free Svg, Cliparts, Vectors, And Stock Illustration. Image 23547040

The Black Sea, Russia and Chernoye More in Bulgaria, Chorne More in Ukraine, Karadenız in Turkey, Marea Neagră in Romania, a large inland sea located in southeastern Europe. It is bordered by Ukraine to the north, Russia to the northeast, Georgia to the east, Turkey to the south, Bulgaria and Romania to the west.

The oval-shaped Black Sea is a large basin located in the southwestern part of Europe, but it is connected to the distant waters of the Atlantic Ocean by the Bosphorus (which emerges from the southwestern corner of the sea), the Sea of ​​Marmara. , Dardanelles, Aegean and Mediterranean Sea. The Crimea flows from the north to the Black Sea, and to the east the narrow Strait of Kerch connects the sea with the small Sea of ​​Azov. The Black Sea coast is an example. The maximum east-west extent of the sea is about 730 miles (1,175 km), and the distance between the tip of the Crimean Peninsula and the southern cape of Kerempe is about 160 miles (260 km). The surface area of ​​the Sea of ​​Azov, not the Sea of ​​Marmara, is about 178,000 square miles (461,000 square kilometers). The Black Sea covers about 163,000 square miles (422,000 square kilometers). The maximum depth is over 7,250 feet (2,210 meters) in the south-central sea.

In ancient Greek mythology, the sea that was then part of the Mediterranean world was called Pontus Axeinus, which means “rough sea”. Later, through exploration, the country became familiar, and the name was changed to Pontus Euxinus, the opposite of the name, when a colony was established on the shores of the sea, which the Greeks considered more friendly and hospitable. Legend has it that Jason and the Argonauts crossed the sea to find the Golden Fleece in the land of Colchis, a kingdom east of the sea (now Georgia). When the Turks went to rule the land beyond the southern shores of the sea, they met a sudden storm that struck the sea and returned to a name denoting the host of what they now call Karadenız or the Black Sea.

For scientists, the Black Sea is a surprising phenomenon, not because of pollution, but because of the persistence of deep atmospheric layers, so low levels are almost biologically dead for all intents and purposes. For the countries of the continent, the Black Sea has been very important for centuries. The arrival of established conditions brought economic value to the fore.

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The Black Sea coast is calm with the exception of the northwest and north coasts, where the lowlands are interspersed with many valleys, valleys and streams and are often clogged. The mountains of southern Crimea are the only steep areas. The east and south coasts are steep and mountainous. The spurs of the Greater and Lesser Caucasus, separated by the Kolkhida lowlands, border the Black Sea to the east, and the Pontic Mountains stretch along the southern coast. The beaches near the entrance to the Bosphorus are lower and steeper. Further north, in the Burgaski Bay region, the low mountains of Bulgaria’s Balkans stretch to the east. Continuing north along the west coast, flat land gives way to the mighty Danube River, which discharges most of it into the sea.

The Black Sea contains only a few small islands, the largest of which are Zmiyinyy (Fidonisi) in Ukraine, east of the Danube Delta, and Berezan, at the mouth of the Dniester River. Submarine relief can be seen as a series of concentric rings and sometimes asymmetric rings. Beyond the coast, shallow shelf areas cover about a quarter of the total area. It is wider to the west and wider at the head of the Kerch Strait, but elsewhere the rim is about 10 to 11 km wide and the rim depth is less than 360 feet (110 m). The ledge is broken by the gorge at the bottom of the sea and provides a side to the cliff rising upwards. The coast between the port cities of Sinop and Samsun (Turkey) resembles a series of underwater mountains stretching for some 160 km. The crater formed at the bottom of the basin is a flat plain that covers about one-third of its area, increases in depth at the center, and has a scale axis of over 7,200 feet (2,200 meters). The depth was shifted to the Turkish coast.

The underlying rocks show regional differences in species and age. In the southern part of the structural unit called the Russian (or Eastern European) platform, the oldest Precambrian rocks are at least 540 million years old and are exposed in the northwest. The second adjacent platform is a deep layer of later deposited sedimentary rock. Deep-sea subsidence, considered a major subterranean phenomenon, is a unique and important feature of the crust. The center of the shelter consists of a layer of sedimentary and basalt soil, with a layer of rock at the edges. Sedimentation at the bottom typically varies from gravel and gravel at the edges to small gravel in the center of the basin.

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The Earth’s history of the Black Sea is not fully known, but it appears to be a remnant basin of the ancient Sea of ​​Thetis 250 to 50 million years ago. Current sea level may have appeared at the end of the Paleocene (about 55 million years ago), when the subduction zone separated Anatolia from the Mediterranean. The new Black Sea Basin is separated from the sea and has less salinity. At that time, Crimea and the Caucasus were probably islands.

At the beginning of the Miocene (about 20 million years ago), the Black Sea flowed into a series of lakes, but separated from the Caspian Sea region. As mountains such as the Pontic, Caucasus, Crimea and Carpathians rose around the area, the basin was filled with washed-out sediments. Earth shifts and sea level changes associated with the Pleistocene glaciers have made them closely related to the Mediterranean. During the Great Ice Age, the Black Sea became a large lake. The current connection between the Mediterranean and seawater is believed to have begun some 6,500 to 7,500 years ago. Strong earthquakes, such as the Crimean earthquake of 1927, are often associated with the region. Ukraine’s imperialist electoral war against Russia is the result of a long campaign of imperialist powers to keep the former Soviet states under their control. It represents a new situation in the emergence of a new world struggle between the imperialist powers for the reorganization of power.

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