History of the Caucasus
The history of the Caucasus region may be divided into the history of the Northern Caucasus (Ciscaucasia), historically in the sphere of influence of Scythia and of Southern Russia (Eastern Europe), and that of the Southern Caucasus (Transcaucasia; Caucasian Albania, Georgia, Armenia, Azerbaijan) in the sphere of influence of Persia, Anatolia and for a very brief time Assyria.
Up to including the early 19th century, the Southern Caucasus and a part of the Northern Caucasus (Dagestan) all formed part of the Persian Empire. In 1813 and 1828 by the Treaty of Gulistan and the Treaty of Turkmenchay respectively, the Persians were forced to irrevocably cede the Southern Caucasus and Dagestan to Imperial Russia.Russia conquered and annexed the rest of the Northern Caucasus in the course of the 19th century in the Caucasian Wars (1817-1864).
The Northern Caucasus became the scene of intense fighting during the Second World War. Nazi Germany attempted to capture the Caucasus region from Soviet control in 1942 by a two-pronged attack towards both the western bank of the Volga (intending to seize the city of Stalingrad) and by a drive southeast towards Baku, a major center of oil production. The Nazis intended to establish a Reichskommissariat Kaukasus to control the Caucasian territories of the Soviet Union. Considerable parts of the northern Caucasus fell under German occupation, but the invasion eventually faltered as it failed to accomplish either goal, and Soviet soldiers drove the Germans back west following the Battle of Stalingrad (1942-1943).
Following the dissolution of the Soviet Union in 1991, Armenia, Azerbaijan, and Georgia became independent nations. The Caucasus region has become the setting for various territorial disputes since the collapse of the Soviet Union, leading to the Nagorno-Karabakh War, the Ossetian-Ingush conflict, the War in Abkhazia, the First and Second Chechen Wars, and the South Ossetia War.
The Caucasus region gradually enters the historical record in during the Late Bronze Age to Early Iron Age. Shupria was a Hurrian kingdom, known from Assyrian sources beginning in the 13th century BC, located in what is now known as the Armenian Highlands, to the southwest of Lake Van, bordering on Ararat proper. The capital was called Ubbumu. The Diauehi were a tribal confederation in northeastern Anatolia in the post-Hittite period, mentioned in Urartian inscriptions. Diauehi is a possible locus of Proto-Kartvelian; it has been described as an "important tribal formation of possible proto-Georgians" by Ronald Grigor Suny (1994). At the same time, during the 13th to 9th centuries BC, the Nairi appear in Assyrian and Hittite records. The Battle of Nihriya (c. 1230 BC) was the culmination of Hittite-Assyrian hostilities.
The Kingdom of Urartu rose to power in the mid-9th century BC and flourished for two centuries before it was absorbed into the Median Empire in the early 6th century BC, followed by the conquest by the Achaemenid Empire.
The Northern Caucasus enters the historical record later, being in cultural contact with the Pontic steppe. The Koban culture (ca. 1100 to 400 BC) is a late Bronze Age and Iron Age culture of the northern and central Caucasus. Its end presumably correlates with the Scythian expansion in the region.
During the middle ages Bagratid Armenia, Kingdom of Tashir-Dzoraget, Kingdom of Syunik and Principality of Khachen organized local Armenian population facing multiple threats after the fall of antique Kingdom of Armenia.
Caucasian Albania maintained close ties with Armenia and the Church of Caucasian Albania shared same Christian dogmas with the Armenian Apostolic Church and had a tradition of their Catholicos being ordained through the Patriarch of Armenia.
Early modern history
By the end of the 15th century, the Kingdom of Georgia was fragmented into a number of petty client kingdoms subject to either Persia (Kingdom of Kakheti, Kingdom of Kartli) or the Ottomans (Kingdom of Imereti).[note 1] Throughout the 16th century, the Caucasus continued to serve as a battleground between Persian and Ottoman forces, with the two great powers attempting to gain control over the region. From the 1530s to the 1550s, several Transcaucasian cities became the focal point of these imperial divides. In 1555, this culminated in the Peace of Amasya, whereby Ottoman and Persian forces agreed to establish formal spheres of influence in the region. As a result of the Treaty, the Safavid Empire (Persia) assumed control over lands East of the Surami Highlands, including the Georgian kingdoms of Kartli and Kakheti. The Ottomans received areas West of the Highlands, including the Georgian kingdom of Imereti. The nascent Russian Empire gained territories in the North Caucasus in the Russo-Persian war of 1722/3. These territories were ceded back to Persia a few years later. Following the death of Nader Shah, Kartli and Kakheti were merged into the Kingdom of Kartli-Kakheti in 1762; Erekle de facto seceeded from Persian overlordship, but still de jure recognized the Persians as his suzerain. In 1783, King Erekle II concluded the Treaty of Georgievsk with the Russian Empire. Catherine the Great tried to use Georgia as a base of operations against both Iran and the Ottoman Empire. After her death, the Russians withdrew to the North Caucasus Line. The Qajar dynasty re-established Persia's traditional suzerainty over the Caucasus. A Persian invasion force defeated the Georgian army in the Battle of Krtsanisi in 1795. In 1801, a few years after the assassination of Agha Mohammad Khan, capitalizing on the erupation of instability in Iran, the Russians annexed eastern Georgia (Kartli-Kakheti).
While Georgia and Armenia remained Christian, the Chechens gradually adopted Sunni Islam. The Circassians were mostly Islamized under the influence of the Crimean Tatars and the Ottoman Empire in the 17th century.
Russian Empire and Civil War
Recent history (1991-present)
source : Wikipedia
The Caucasus Mountains include the Greater Caucasus in the north and Lesser Caucasus in the south. The Greater Caucasus runs west-northwest to east-southeast, from the Caucasian Natural Reserve in the vicinity of Sochi on the northeastern shore of the Black Sea nearly to Baku on the Caspian Sea. The Lesser Caucasus runs parallel to the Greater about 100 km (62 mi) south. The Greater and Lesser Caucasus ranges are connected by the Likhi Range, and to the west and east of the Likhi Range lie the Colchis Plain and the Kur-Araz Lowland. The Meskheti Range is a part of the Lesser Caucasus system. In the southeast the Aras River separates the Lesser Caucasus from the Talysh Mountains which straddle the border of southeastern Azerbaijan and Iran. The Lesser Caucasus and the Armenian Highland constitute the Transcaucasian Highland, which at their western end converge with the highland plateau of Eastern Anatolia in the far north east of Turkey. The highest peak in the Caucasus range is Mount Elbrus in the Greater Caucasus, which rises to a height of 5,642 metres (18,510 ft) above sea level. Mountains near Sochi hosted part of the 2014 Winter Olympics.
Geologically, the Caucasus Mountains belong to a system that extends from southeastern Europe into Asia. The Greater Caucasus Mountains are mainly composed of Cretaceous and Jurassic rocks with the Paleozoic and Precambrian rocks in the higher regions. Some volcanic formations are found throughout the range. On the other hand, the Lesser Caucasus Mountains are formed predominantly of the Paleogene rocks with a much smaller portion of the Jurassic and Cretaceous rocks. The evolution of the Caucasus began from the Late Triassic to the Late Jurassic during the Cimmerian orogeny at the active margin of the Tethys Ocean while the uplift of the Greater Caucasus is dated to the Miocene during the Alpine orogeny.
The Caucasus Mountains formed largely as the result of a tectonic plate collision between the Arabian plate moving northwards with respect to the Eurasian plate. As the Tethys Sea was closed and the Arabian Plate collided with the Iranian Plate and was pushed against it and with the clockwise movement of the Eurasian Plate towards the Iranian Plate and their final collision, the Iranian Plate was pressed against the Eurasian Plate. As this happened, the entire rocks that had been deposited in this basin from the Jurassic to the Miocene were folded to form the Greater Caucasus Mountains. This collision also caused the uplift and the Cenozoic volcanic activity in the Lesser Caucasus Mountains.
The entire region is regularly subjected to strong earthquakes from this activity. While the Greater Caucasus Mountains have a mainly folded sedimentary structure, the Lesser Caucasus Mountains are largely of volcanic origin.
The Javakheti Volcanic Plateau in Georgia and the surrounding volcanic ranges which extend well into central Armenia are some of the youngest features of the region. Only recently was the Caucasus a scene for intense volcanic activity: the Armenian highland was flooded by calc-alkaline basalts and andesites in the Pliocene and the highest summits of the Caucasus, the Elbrus, and the Kazbek, formed as Pleistocene-Pliocene volcanoes. The Kazbek is no longer active, but the Elbrus erupted in postglacial times and fumarole activity is registered near its summit. Contemporary seismic activity is a prominent feature of the region, reflecting active faulting and crustal shortening. Clusters of seismicity occur in Dagestan and in northern Armenia. Many devastating earthquakes have been documented in historical times, including the Spitak earthquake in December 1988 which destroyed the Gyumri-Vanadzor region of Armenia.
Europe's highest mountain is Mount Elbrus 5,642 m (18,510 ft) in the Caucasus Mountains. Elbrus is 832 m (2,730 ft) higher than Mont Blanc, the highest peak in the Alps and western Europe at 4,810 m (15,780 ft). The crest of the Caucasus Mountains usually is taken to define the continental divide between Asia and Europe for the region between the Black and Caspian Seas.
The table below lists some of the highest peaks of the Caucasus. With the exception of Shkhara, the heights are taken from Soviet 1:50,000 mapping. The list includes the ten ultras (mountains of more than 1,500 m prominence) and all mountains over 4,500 m height with 300 m prominence. Mount Ararat (5,137 m) in Turkey is just south of the lesser Caucasus.
The climate of the Caucasus varies both vertically (according to elevation) and horizontally (by latitude and location). Temperature generally decreases as elevation rises. Average annual temperature in Sukhumi, Abkhazia at sea level is 15 °C (59 °F) while on the slopes of Mt.Kazbek at an elevation of 3,700 metres (12,100 ft), average annual temperature falls to?6.1 °C (21.0 °F). The northern slopes of the Greater Caucasus Mountain Range are 3 °C (5.4 °F) colder than the southern slopes. The highlands of the Lesser Caucasus Mountains in Armenia, Azerbaijan, and Georgia are marked by sharp temperature contrasts between the summer and winter months due to a more continental climate.
Precipitation increases from east to west in most areas. Elevation plays an important role in the Caucasus and mountains generally receive higher amounts of precipitation than low-lying areas. The northeastern regions (Dagestan) and the southern portions of the Lesser Caucasus Mountains are the driest. The absolute minimum annual precipitation is 250 mm (9.84 in) in the northeastern Caspian Depression. Western parts of the Caucasus Mountains are marked by high amounts of precipitation. The southern slopes of the Greater Caucasus Mountain Range receive higher amounts of precipitation than the northern slopes. Annual precipitation in the Western Caucasus ranges from 1,000 to 4,000 mm (39.37-157.48 in) while in the Eastern and Northern Caucasus (Chechnya, Ingushetia, Kabardino-Balkaria, Ossetia, Kakheti, Kartli, etc.) precipitation ranges from 600 to 1,800 mm (23.62-70.87 in). The absolute maximum annual precipitation is 4,100 mm (161.42 in) around the Mt. Mtirala area which lies on the Meskheti Range in Ajaria. The precipitation of the Lesser Caucasus Mountain Range (Southern Georgia, Armenia, western Azerbaijan), not including the Meskheti Range, varies from 300-800 mm (31.50 in) annually.
The Caucasus Mountains are known for the high amount of snowfall, although many regions which are not located along the windward slopes do not receive nearly as much snow. This is especially true for the Lesser Caucasus Mountains which are somewhat isolated from the moist influences coming in from the Black Sea and receive considerably less precipitation (in the form of snow) than the Greater Caucasus Mountains. The average winter snow cover of the Lesser Caucasus Mountains ranges from 10 to 30 cm (3.94-11.81 in). The Greater Caucasus Mountains (especially the southwestern slopes) are marked by heavy snowfall. Avalanchesare common from November to April.
Snow cover in several regions (Svaneti and northern Abkhazia) may reach 5 metres (16 ft). The Mt. Achishkho region, which is the snowiest place in the Caucasus, often records snow depths of 7 m (23 ft).
The Caucasus Mountains have a varied landscape which mainly changes according to elevation and distance from large bodies of water. The region contains biomes ranging from subtropical lowland marshes and forests to glaciers (Western and Central Caucasus), and highland semi deserts, steppes, and alpine meadows in the south (mainly in Armenia and Azerbaijan).
The northern slopes of the Greater Caucasus Mountains are covered by oak, hornbeam, maple, and ash forests at lower elevations while birch and pine forests take over at higher elevations. Some of the lowest areas of the region are covered by steppes and grasslands. The slopes of the Northwestern Greater Caucasus (Kabardino-Balkaria, Cherkessia, etc.) also contain spruce and fir forests. The alpine zone replaces the forest at around 2,000 metres (6,600 ft) above sea level. The permafrost/glacier line generally starts around 2,800-3,000 metres (9,200-9,800 ft). The southeastern slopes of the Greater Caucasus Mountains are covered by beech, oak, maple, hornbeam, and ash forests. Beech forests tend to dominate in higher locations. The southwestern slopes of the Greater Caucasus are covered by Colchian forests (oak, buxus, beech, chestnut, hornbeam, elm) at lower elevations with coniferous and mixed forests (spruce, fir and beech) taking over at higher elevations. The alpine zone on the southern slopes may extend up to 2,800 metres (9,200 ft) above sea level while the glacier/snow line starts at 3,000-3,500 metres (9,800-11,500 ft).
The northern and western slopes of the Lesser Caucasus Mountains are characterized both by Colchian and other deciduous forests at lower elevations while mixed and coniferous forests (mainly spruce and fir) dominate at higher elevations. Beech forests are also common at higher elevations. The southern slopes of the Lesser Caucasus Mountains are largely covered by grasslands and steppes up to an elevation of 2,500 metres (8,200 ft). The highest areas of the region contain alpine grasslands as well. Volcanic and other rock formations are common throughout the region. The volcanic zone extends over a large area from southern Georgia into Armenia and southwestern Azerbaijan. Some of the prominent peaks of the region include Mt. Aragats, Didi Abuli, Samsari, and others. The area is characterized by volcanic plateaus, lava flows, volcanic lakes, volcanic cones and other features. The Lesser Caucasus Mountains lack the type of glaciers and glacial features that are common on the Greater Caucasus Mountain Range.
Crossing the Caucasus Mountain range was an important section of the northern arm of the Silk Route. There was one pass on the southeast end in Derbent (known as the Caspian Gates or Gates of Alexander), and multiple passes throughout the range: Jvari Pass at 2379 m and above the Darial Gorge on the Georgian Military Road, Mamison Pass on the Ossetian Military Road at 2911 m, and Roki Tunnel at 2310 m. See Russian conquest of the Caucasus.
source : Wikipedia
Caucasus with Georgia 1184-1226
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