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Kerch Peninsula
The Kerch Peninsula is a major and prominent geographic peninsula located at the eastern end of the Crimean Peninsula. This peninsula stretches eastward toward the Taman Peninsula between the Sea of Azov and the Black Sea. Most of the peninsula is located within the Lenine Raion. Names In Classical Antiquity, the area was known as the "Rough Peninsula" (Greek language, Greek: Χερσόνησος Τραχεία, ). In Slavic languages, its pronunciation does not vary by much: , ''Kerchenskyi Pivostriv''; , ''Kerich Yarymadasy''; , ''Kyerchyenskii Polu'ostrov''. Geography The Kerch Peninsula is almost completely surrounded by water and only to the west connects with the rest of Crimea by the Isthmus of Ak-Monay which is only wide (from the southern end of the Arabat Spit to the town of Primorsky (Khafuz), Feodosiya). On elevated portions of the isthmus, named after the village of Kamianske (former ''Aq-Monai''), are seen both of the surrounding seas. The widest portion of the ...
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Peninsula
A peninsula is a landform that extends from a mainland and is only connected to land on one side. Peninsulas exist on each continent. The largest peninsula in the world is the Arabian Peninsula. Etymology The word ''peninsula'' derives , . The word entered English in the 16th century. Definitions A peninsula is generally defined as a piece of land surrounded on most sides by water. A peninsula may be bordered by more than one body of water, and the body of water does not have to be an ocean or a sea. A piece of land on a very tight river bend or one between two rivers is sometimes said to form a peninsula, for example in the New Barbadoes Neck in New Jersey, United States. A peninsula may be connected to the mainland via an isthmus, for example, in the Isthmus of Corinth which connects to the Peloponnese peninsula. Formation and types Peninsulas can be formed from continental drift, glacial erosion, meltwater, glacial meltwater, glacial deposition (geology), deposition, ...
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Bay Of Arabat
The Bay of Arabat, (, , ), is in the southwestern Azov Sea in eastern Europe. It is located along the northwestern coast of the Kerch Peninsula and northeastern coast of Crimea. See also * Arabat Spit The Arabat Spit (; ; ) or Arabat Arrow is a spit (landform), barrier spit that separates the large, shallow, salty Syvash lagoons from the Sea of Azov. The spit runs between the Henichesk Strait in the north and the north-eastern shores of Crim ... * Geography of Crimea Bays of Crimea Kerch Peninsula Bays of the Sea of Azov {{Crimea-geo-stub ...
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Aqtas Lake
Aqtas Lake or Aktashskoye (, ) is a drying salt lake at the Kerch peninsula in the Lenine Raion, Crimea. The lake belongs to the Kerch group of lakes.Information at the regional committee on water management and land improvement
Its name means ''White Mount''. Its water supplies it receives from the Black Sea Littoral Artesian Aquifer. Lake is connected with the and through another canal with the

Tobechytske Lake
Tobechytske Lake (Russian: Тобечи́кское о́зеро, Ukrainian: Тобечикське озеро, Crimean Tatar: Тöbeçik gölü) is a salt lake in the south of the Kerch Peninsula in the Lenine Raion district of Crimea. The lake belongs to the Kerch group of lakes. The villages of Ohon'ky and Chelyadinove are located to the north of the lake, Kostyrine to the south, and the city of Kerch Kerch, also known as Keriç or Kerich, is a city of regional significance on the Kerch Peninsula in the east of Crimea. It has a population of Founded 2,600 years ago as the Colonies in antiquity#Greek colonies, ancient Greek colony Pantik ... to the north-east.Surface water resources of the USSR. Volume 6: Ukraine and Moldova. Issue 4: Crimea. Under. ed. by M. M. Eisenberg and M. S. Kaganer. — L. Gidrometeoizdat. 1966. 344 s. References {{Crimea-geo-stub Lakes of Crimea Lakes of Ukraine ...
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Koyashskoye Salt Lake
Koyashskoye () or Koiaske () is a salt lake on the coast of the Kerch Peninsula in Crimea, separated from the Black Sea by a strip of land. It is 4 kilometers long, 2 kilometers wide and a meter deep. The lake has the particularity to have a pink to scarlet color, depending on the light, due to the presence of microscopic algae living in the water. When the water evaporates, the salt in the lake crystallizes on the stones and the shores, producing crystal stones and the scent of viola The viola ( , () ) is a string instrument of the violin family, and is usually bowed when played. Violas are slightly larger than violins, and have a lower and deeper sound. Since the 18th century, it has been the middle or alto voice of the .... Uzunlarske Lake is located directly west. This location is considered healing and is appreciated by some locals. It is not widely known to tourists. References * * {{Crimea-geo-stub Saline lakes of Europe Lakes of Crimea Black Sea ...
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Kachyk Lake
Kachyk Lake (, , ) is a salt lake in the south of the Kerch Peninsula in the Lenine Raion district of Crimea. The lake belongs to the Kerch group of lakes. Koyashskoye Salt Lake and Uzunlarske Lake are located to the east, and the coast of the Black Sea The Black Sea is a marginal sea, marginal Mediterranean sea (oceanography), mediterranean sea lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia. It is bound ... is to the south. The closest village is Vulkanivka to the west. References Lakes of Crimea Lakes of Ukraine {{Crimea-geo-stub ...
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Uzunlarske Lake
Uzunlarske Lake (Russian: Узунла́рское о́зеро, Ukrainian: Узунларське озеро, Crimean Tatar: Uzunlar gölü) is a salt lake in the south of the Kerch Peninsula in the Lenine Raion district of Crimea. The lake belongs to the Kerch group of lakes, and is the sixth largest lake in Crimea. Koyashskoye Salt Lake is located to the east, and the coast of the Black Sea The Black Sea is a marginal sea, marginal Mediterranean sea (oceanography), mediterranean sea lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia. It is bound ... is to the south. Mar'ivka is the closest village to the east. References Lakes of Crimea Lakes of Ukraine {{Crimea-geo-stub ...
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Natural Gas In Ukraine
Ukraine extracts about 20 billion cubic meters of fossil gas each year, and since 2022 this has almost met demand. Ukraine has been estimated to possess natural gas reserves of over 670 billion cubic meters (in 2022), and gas is an important part of energy in Ukraine. In 2021, Ukraine produced 19.8 billion cubic meters (bcm or Gm3) of natural gas. To satisfy domestic demand of 27.3 bcm that year, Ukraine relied on gas imports (2.6 bcm) and withdrawal from underground storage (4.9 bcm). Winter demand can reach 150 mcm per day. During Soviet times, Ukraine produced a record of 68.7 bcm in 1976. At the time of independence in 1991, production was at 26.6 bcm, and fell in the 1990s to about 18 bcm. Since the mid-2000s, production has stabilised between 20 and 21 bcm. Over 70% of domestic gas production is extracted by UkrGasVydobuvannya, a subsidiary of the state-owned company Naftogaz. Private gas production companies in Ukraine are DTEK, Ukrnaftoburinnya, Burisma, Smart Energy, ...
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Mud Volcano
A mud volcano or mud dome is a landform created by the eruption of mud or Slurry, slurries, water and gases. Several geological processes may cause the formation of mud volcanoes. Mud volcanoes are not true Igneous rock, igneous volcanoes as they do not produce lava and are not necessarily driven by magmatic activity. Mud volcanoes may range in size from merely 1 or 2 meters high and 1 or 2 meters wide, to 700 meters high and 10 kilometers wide. Smaller mud exudations are sometimes referred to as mud-pots. The mud produced by mud volcanoes is mostly formed as hot water, which has been heated deep below the Earth's surface, begins to mix and blend with subterranean mineral deposits, thus creating the mud slurry exudate. This material is then forced upwards through a geological fault or fissure due to local subterranean pressure imbalances. Mud volcanoes are associated with subduction zones and about 1100 have been identified on or near land. The temperature of any given active mu ...
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Central Asia
Central Asia is a region of Asia consisting of Kazakhstan, Kyrgyzstan, Tajikistan, Turkmenistan, and Uzbekistan. The countries as a group are also colloquially referred to as the "-stans" as all have names ending with the Persian language, Persian suffix "-stan" (meaning ) in both respective native languages and most other languages. The region is bounded by the Caspian Sea to the southwest, European Russia to the northwest, China and Mongolia to the east, Afghanistan and Iran to the south, and Siberia to the north. Together, the five Central Asian countries have a total population of around million. In the pre-Islamic and early Islamic eras ( and earlier) Central Asia was inhabited predominantly by Iranian peoples, populated by Eastern Iranian-speaking Bactrians, Sogdians, Khwarezmian language, Chorasmians, and the semi-nomadic Scythians and Dahae. As the result of Turkic migration, Central Asia also became the homeland for the Kazakhs, Kyrgyzs, Volga Tatars, Tatars, Turkmens, ...
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Caucasus
The Caucasus () or Caucasia (), is a region spanning Eastern Europe and Western Asia. It is situated between the Black Sea and the Caspian Sea, comprising parts of Southern Russia, Georgia, Armenia, and Azerbaijan. The Caucasus Mountains, including the Greater Caucasus range, have conventionally been considered as a natural barrier between Europe and Asia, bisecting the Eurasian landmass. Mount Elbrus, Europe's highest mountain, is situated in the Western Caucasus area of Russia. On the southern side, the Lesser Caucasus includes the Javakheti Plateau and the Armenian highlands. The Caucasus is divided into the North Caucasus and South Caucasus, although the Western Caucasus also exists as a distinct geographic space within the North Caucasus. The Greater Caucasus mountain range in the north is mostly shared by Russia and Georgia as well as the northernmost parts of Azerbaijan. The Lesser Caucasus mountain range in the south is mostly located on the territory of sout ...
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Mud Volcano
A mud volcano or mud dome is a landform created by the eruption of mud or Slurry, slurries, water and gases. Several geological processes may cause the formation of mud volcanoes. Mud volcanoes are not true Igneous rock, igneous volcanoes as they do not produce lava and are not necessarily driven by magmatic activity. Mud volcanoes may range in size from merely 1 or 2 meters high and 1 or 2 meters wide, to 700 meters high and 10 kilometers wide. Smaller mud exudations are sometimes referred to as mud-pots. The mud produced by mud volcanoes is mostly formed as hot water, which has been heated deep below the Earth's surface, begins to mix and blend with subterranean mineral deposits, thus creating the mud slurry exudate. This material is then forced upwards through a geological fault or fissure due to local subterranean pressure imbalances. Mud volcanoes are associated with subduction zones and about 1100 have been identified on or near land. The temperature of any given active mu ...
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