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Likhi Range
Likhi Range ( ka, ლიხის ქედი, tr) or Surami Range ( ka, სურამის ქედი, tr) is a mountain range in Georgia, a part of the Caucasus Mountains. It connects the Greater Caucasus and Lesser Caucasus ranges and belongs to the Dzirulula denudative Plateau. It is watershed of the Black and Caspian seas basins and divides the country climatically and geomorphologically. The highest point in the range is the Ribisa mountain, at above sea level. The lowest and most important mountain pass A mountain pass is a navigable route through a mountain range or over a ridge. Since mountain ranges can present formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration t ... is the Surami Pass at an elevation of which links eastern and western Georgia. A railroad (in the tunnel) runs through the pass, as well as the Zestaponi- Khashuri highway. A southern portion of the Likhi rang ...
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Caucasus Mountains
The Caucasus Mountains * * Azerbaijani: , * * * * * * * * * * * is a mountain range at the intersection of Asia and Europe. Stretching between the Black Sea and the Caspian Sea, they are surrounded by the Caucasus region and are home to Mount Elbrus, the highest peak in Europe at above sea level. The Caucasus Mountains include the Greater Caucasus in the north and the Lesser Caucasus in the south. The Greater Caucasus runs west-northwest to east-southeast, from the Western Caucasus on the northeastern shore of the Black Sea to close to Baku on the Caspian Sea, in Azerbaijan. The Lesser Caucasus runs parallel to the Greater about 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 respectively. The Meskheti Range is a part of the Lesser Caucasus system. In the southeast, the Aras River separates the Lesser Caucasus from the Tal ...
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Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since mountain ranges can present formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the minimum high point between two valleys and the lowest point along a ridge. On a topographic map, passes can be identified by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pass. Passes are o ...
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Mountain Ranges Of The Caucasus
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ...
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Meskheti Range
Meskheti Range ( ka, მესხეთის ქედი) (Meskh/Meskhet/Meskhetian Range, Adzhar-Imereti Range, Achara-Imereti Range Adzhar-Akhaltsikh Range also Moschian Mountains) is a part of the Lesser Caucasus mountain range in Meskheti region, in southwestern Georgia. Geography The length of the range is 150 km and the highest point is Mount Mepistskharo at an elevation of 2,850 m above sea level. The Meskheti Range is characterized by high amounts of precipitation. The territory around Mt. Mtirala (the Ajarian section of the range) was the wettest region within the Soviet Union and is the most humid area of the Caucasus with an annual precipitation of approximately 4500mm/year (180 inches/year). Several rivers are flowing from the Meskheti Range — Supsa, Acharis-Tsqali and Natanebi. Flora and fauna The slopes of the Meskheti Range are rich in endemic and relic speciesLevan Mumladze, Giorgi Chaladze, Zezva Asanidze, Salome Saghinadze, Ema KhachidzRefug ...
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Rikoti Pass
The Rikoti Pass ( ka, რიკოთის უღელტეხილი) (el. ) is a mountain pass in the southern portion of the Likhi Range, a spur of the Greater Caucasus which divides Georgia into its western and eastern parts. The Tbilisi-Kutaisi Kutaisi ( ; ka, ქუთაისი ) is a city in the Imereti region of the Georgia (country), Republic of Georgia. One of the List of oldest continuously inhabited cities, oldest continuously inhabited cities in the world, it is the List o ... highway connecting the two major cities of Georgia runs through the pass via a rock-cut tunnel of in length, which was constructed in 1982.Rikoti pass automobile tunnel to be granted on 20 years- term lease
. Ministry of Economic Development of Georgia. Retrieved on ...
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Khashuri
Khashuri ( ka, ხაშური ) is a city in the central part of Georgia and is the 9th largest settlement in Georgia. It is the administrative centre of Khashuri Municipality. It is located on the Shida Kartli plain, on the Suramula riverside, above sea level. Khashuri is first mentioned in a 1693 document. Modern Khashuri was founded in 1872 as a modest railway stop called "Mikhaylovo" after Grand Duke Michael Nikolaevich of Russia, Viceroy of the Caucasus. In 1917, it was renamed Khashuri. The city was granted city status in 1921. It was known as Stalinisi, after Joseph Stalin, from 1928 to 1934. In the 19th century after the leading Tbilisi-Poti main line, Khashuri gradually became a major transportation node. The railways and highways were heading towards Borjomi and Akhaltsikhe Akhaltsikhe ( ka, ახალციხე ), formerly known as Lomsia ( ka, ლომსია ), is a small city in Georgia's southwestern region () of Samtskhe–Javakheti. It is the a ...
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Zestaponi
Zestaponi ( ka, ზესტაფონი, tr, ) is the administrative center of Zestaponi District in Western Georgia (country), Georgia. Zestaponi is the center of an ancient, historical part of Georgia – Margveti, which is a part of Imereti province. Zestaponi is the center of Margveti's Eparchy of the Georgian Orthodox Church. Zestaponi is situated in the furthest east of the Colchis Plateau, and is built on both banks of the Qvirila River. It is an important industrial center, with a large ferro-alloy plant processing manganese ore from nearby Chiatura. Zestaponi is in the Kolkheti lowlands, a semi-tropical region with relatively cold winters averaging in January and hot summers averaging in August. The surrounding countryside is a wine-growing region. Industry The town of Zestaponi and the smaller neighboring town of Shorapani are industrial centers. The Zestaponi ferro-alloy plant processes raw manganese ore shipped by rail down the Kvirila valley from Chiatura ...
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Surami Pass
The Surami Pass ( ka, სურამის უღელტეხილი) is a mountain pass in the Likhi Range of Georgia (country), Georgia with an altitude of . The pass connects the western and eastern part of Georgia. A railroad (in a tunnel) runs through the pass, as well as the ZestaponiKhashuri highway. History Rail service through Surami Pass was opened in 1872. The rail line was electrified in 1933. References

Mountain passes of Georgia (country) {{Georgia-geo-stub ...
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Geomorphology
Geomorphology () is the scientific study of the origin and evolution of topographic and bathymetric features generated by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field. Overview Earth's surface is modified by a combination of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the coastal geography. Surface processes comprise the action of water, wind, ice, wildfire, and lif ...
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Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ...
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Caspian Sea
The Caspian Sea is the world's largest inland body of water, described as the List of lakes by area, world's largest lake and usually referred to as a full-fledged sea. An endorheic basin, it lies between Europe and Asia: east of the Caucasus, west of the broad steppe of Central Asia, south of the fertile plains of Southern Russia in Eastern Europe, and north of the mountainous Iranian Plateau. It covers a surface area of (excluding the highly saline lagoon of Garabogazköl to its east), an area approximately equal to that of Japan, with a volume of . It has a salinity of approximately 1.2% (12 g/L), about a third of the salinity of average seawater. It is bounded by Kazakhstan to the northeast, Russia to the northwest, Azerbaijan to the southwest, Iran to the south, and Turkmenistan to the southeast. The name of the Caspian Sea is derived from the ancient Iranian peoples, Iranic Caspians, Caspi people. The sea stretches from north to south, with an average width of . Its gr ...
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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 bounded by Bulgaria, Georgia (country), Georgia, Romania, Russia, Turkey, and Ukraine. The Black Sea is Inflow (hydrology), supplied by major rivers, principally the Danube, Dnieper and Dniester. Consequently, while six countries have a coastline on the sea, its drainage basin includes parts of 24 countries in Europe. The Black Sea, not including the Sea of Azov, covers , has a maximum depth of , and a volume of . Most of its coasts ascend rapidly. These rises are the Pontic Mountains to the south, bar the southwest-facing peninsulas, the Caucasus Mountains to the east, and the Crimean Mountains to the mid-north. In the west, the coast is generally small floodplains below foothills such as the Strandzha; Cape Emine, a dwindling of the east end ...
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