The Caspian Sea is the largest enclosed body of water on Earth by area, variously classed as the world's largest lake or a full-fledged sea.[2][3] It has a surface area of 371,000 square kilometers (143,244 sq mi) and a volume of 78,200 cubic kilometers (18,761 cu mi).[4] It is an endorheic basin (it has no outflows), and is bound by northern Iran, southern Russia, western Kazakhstan and Turkmenistan, and eastern Azerbaijan. It has a maximum depth of about 1025 meters (3,363 ft).
It was perceived as an ocean by its ancient coastal inhabitants, presumably because of its saltiness and seeming boundlessness. It has a salinity of approximately 1.2%, about a third the salinity of most seawater. According to Strabo, it is named after an ancient people called Caspians[5] or the ancient sanskrit name Kashyapas.
Geological history
Like the Black Sea, the Caspian Sea is a remnant of the ancient Paratethys Sea. The Caspian Sea became landlocked about 5.5 million years ago due to tectonic uplift and a fall in sea level. During warm and dry climatic periods, the landlocked sea has all but dried up, depositing evaporitic sediments like halite that have become covered by wind-blown deposits and were sealed off as an evaporite sink,[7] when cool, wet climates refilled the basin.[8] Due to the current inflow of fresh water, the Caspian Sea is a fresh-water lake in its northern portions. It is more saline on the Iranian shore, where the catchment basin contributes little flow. Currently, the mean salinity of the Caspian is one third that of the Earth's oceans. The Garabogazköl embayment, which dried up when water flow from the main body of the Caspian was blocked in the 1980s but has since been restored, routinely exceeds oceanic salinity by a factor of 10.
Geography
The Caspian Sea is the largest inland body of water in the world and accounts for 40 to 44 percent of the total lacustrine (lake) waters of the world. The coastlines of the Caspian are shared by Azerbaijan, Iran, Kazakhstan, Russia, and Turkmenistan. The Caspian is divided into three distinct physical regions: Northern, Middle, and Southern Caspian.[10] The North-Middle boundary is the Mangyshlak threshold, which runs through Chechen Island and Cape Tiub-Karagan. The Middle-South boundary is the Apsheron threshold, a sill of tectonic origin[11] that runs through Zhiloi Island and Cape Kuuli.[12] The Garabogazköl bay is the saline eastern inlet of the Caspian, which is part of Turkmenistan and at times has been a lake in its own right due to the isthmus which cuts it off from the Caspian.
Divisions between the three regions are dramatic. The Northern Caspian only includes the Caspian shelf,[13] and is characterized as very shallow; it accounts for less than one percent of the total water volume with an average depth of only five to six meters. The sea noticeably drops off towards the Middle Caspian, where the average depth is 190 meters.[12] The Southern Caspian is the deepest, with a depth that reaches over 1000 meters. The Middle and Southern Caspian account for 33 percent and 66 percent of the total water volume, respectively.[10] The northern portion of the Caspian Sea typically freezes in the winter, and in the coldest winters, ice will form in the south.
Over 130 rivers provide inflow to the Caspian, with the Volga River being the largest. The Caspian also has several small islands; they are primarily located in the North and have a collective land area of roughly 2000 square kilometers. Adjacent to the North Caspian is the Caspian Depression, a low-lying region 27 meters below sea level. The Central Asian steppes stretch across the northeast coast, while the Caucasus mountains hug the Western shore. The biomes to both the north and east are characterized by cold, continental deserts. Conversely, the climate to the southwest and south are generally warm with uneven elevation due to a mix of highlands and mountain ranges; the drastic changes in climate alongside the Caspian have led to a great deal of biodiversity in the region.
Fauna
An aerial view of the southern Caspian coast as viewed from atop the Alborz mountains in Mazandaran, IranThe Caspian Sea holds great numbers of sturgeon, which yield eggs that are processed into caviar. In recent years overfishing has threatened the sturgeon population to the point that environmentalists advocate banning sturgeon fishing completely until the population recovers. However, the high price of sturgeon caviar allows fisherman to afford bribes to ensure the authorities look the other way, making regulations in many locations ineffective.[14] Caviar harvesting further endangers the fish stocks, since it targets reproductive females.
Fauna
The Caspian seal, (Phoca caspica, Pusa caspica in some sources) which is endemic to the Caspian Sea, is one of very few seal species that live in inland waters (see also Baikal seal). The area has given its name to several species of birds, including the Caspian gull and the Caspian tern. There are several species and subspecies of fish endemic to the Caspian Sea, including the Kktum (also known as Caspian white fish), Caspian roach, Caspian bream (some report that the Bream occurring in the Aral Sea is the same subspecies), and a Caspian "salmon" (a subspecies of trout, Salmo trutta caspiensis). The "Caspian salmon" is critically endangered.
Environmental Issues
The Volga River, the largest in Europe, drains 20% of the European land area and is the source of 80% of the Caspian’s freshwater inflow. Its lower reaches are heavily developed with numerous unregulated releases of chemical and biological pollutants. Although existing data is sparse and of questionable quality, there is ample evidence to suggest that the Volga is one of the principal sources of transboundary contaminants into the Caspian. The magnitude of oil and gas extraction and transport activity constitutes a risk to water quality. Underwater oil and gas pipelines have been constructed or proposed, increasing potential environmental threats.
Hydrological characteristics
Iran's Northern Jungles/Rain forests created by the moisture captured from the Caspian sea and the Alborz mountain range of Iran, Gilan.The Caspian has characteristics common to both seas and lakes. It is often listed as the world's largest lake, though it is not a freshwater lake. The Caspian became landlocked about 5.5 million years ago due to plate tectonics.[citation needed] The Volga River (about 80% of the inflow) and the Ural River discharge into the Caspian Sea, but it has no natural outflow other than by evaporation. Thus the Caspian ecosystem is a closed basin, with its own sea level history that is independent of the eustatic level of the world's oceans. The level of the Caspian has fallen and risen, often rapidly, many times over the centuries. Some Russian historians claim that a medieval rising of the Caspian caused the coastal towns of Khazaria, such as Atil, to flood. In 2004, the water level was -28 metres, or 28 metres (92 ft) below sea level.
Over the centuries, Caspian Sea levels have changed in synchronicity with the estimated discharge of the Volga, which in turn depends on rainfall levels in its vast catchment basin. Precipitation is related to variations in the amount of North Atlantic depressions that reach the interior, and they in turn are affected by cycles of the North Atlantic Oscillation. Thus levels in the Caspian sea relate to atmospheric conditions in the North Atlantic thousands of miles to the north and west. These factors make the Caspian Sea a valuable place to study the causes and effects of global climate change.
The last short-term sea-level cycle started with a sea-level fall of 3 m from 1929 to 1977, followed by a rise of 3 m from 1977 until 1995. Since then smaller oscillations have taken place.
Discoveries in the Huto cave near the town of Behshahr, Mazandaran south of the Caspian in Iran, suggest human habitation of the area as early as 75,000 years ago.[17]
In classical antiquity among Greeks and Persians it was called the Hyrcanian Ocean. In Persian antiquity, as well as in modern Iran, it is known as the Mazandaran sea (Persian مازندران). In Turkic speaking countries it is known as the Khazar Sea. Old Russian sources call it the Khvalyn (Khvalynian) Sea (Хвалынское море /Хвалисское море) after the Khvalis, inhabitants of Khwarezmia. Ancient Arabic sources refer to Baḥr Qazvīn - the Caspian/Qazvin Sea.
The word Caspian is derived from the name of the Caspi (Persian کاسپی), an ancient people that lived to the west of the sea in Transcaucasia.[18] Strabo wrote that "to the country of the Albanians belongs also the territory called Caspiane, which was named after the Caspian tribe, as was also the sea; but the tribe has now disappeared".[19] Moreover, the Caspian Gate, which is the name of a region in Tehran province of Iran, is another possible piece of evidence that they migrated to the south of the sea.
Historic cities by the sea include
Hyrcania, ancient state in the north of Iran
Tamisheh, Mazandaran province of Iran
Anzali, Gilan province of Iran
Astara, Azerbaijan Province of Iran
Atil, Khazaria
Khazaran
Baku, Azerbaijan
Sumgait, Azerbaijan
Derbent, Dagestan, Russia
~edytza007