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Keterisi Mineral Vaucluse
Keterisi Mineral Vaucluse Natural Monument ( ka, ქეთერისის მინერალური ვოკლუზი) is a cluster of powerful mineral water artesian aquifers pouring out at the foot of the Greater Caucasus, known as ''Narzan vaucluse'': these mineral springs provide 25-30 million liters of hydrocarbonate-calcium water per day, which corresponds to 300-350 liters per second. From these sources originates stream, which creates water cascades in the village of Keterisi. It is part of ''Kazbegi Protected Areas''Kazbegi
Support Programme for Protected Areas in the Caucasus - Georgia (SPPA-Georgia) along with

Mtskheta-Mtianeti
Mtskheta-Mtianeti ( ka, მცხეთა-მთიანეთი, literally "Mtskheta-Mountain Area") is a region (Mkhare) in eastern Georgia comprising the town of Mtskheta, which serves as a regional capital, together with its district and the adjoining mountainous areas. The western part of the region, namely the entire Akhalgori Municipality, is controlled by breakaway South Ossetia since the 2008 Russo-Georgian War. Administrative divisions The Mtskheta-Mtianeti region officially comprises five municipalities A municipality is usually a single administrative division having corporate status and powers of self-government or jurisdiction as granted by national and regional laws to which it is subordinate. The term ''municipality'' may also mean the go ..., yet only four are effectively under Georgian authority: See also * Subdivisions of Georgia Notes References External links The Regional Administration of Mtskheta-Mtianeti website Regions of G ...
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Georgia (country)
Georgia (, ; ) is a transcontinental country at the intersection of Eastern Europe and Western Asia. It is part of the Caucasus region, bounded by the Black Sea to the west, by Russia to the north and northeast, by Turkey to the southwest, by Armenia to the south, and by Azerbaijan to the southeast. The country covers an area of , and has a population of 3.7 million people. Tbilisi is its capital as well as its largest city, home to roughly a third of the Georgian population. During the classical era, several independent kingdoms became established in what is now Georgia, such as Colchis and Iberia. In the early 4th century, ethnic Georgians officially adopted Christianity, which contributed to the spiritual and political unification of the early Georgian states. In the Middle Ages, the unified Kingdom of Georgia emerged and reached its Golden Age during the reign of King David IV and Queen Tamar in the 12th and early 13th centuries. Thereafter, the kingdom decl ...
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Keterisi
Keterisi ( ka, ქეთერისი) is a village in the historical region of Khevi, north-eastern Georgia. It is located on the right bank of the river Tergi. Administratively, it is part of the Kazbegi Municipality in Mtskheta-Mtianeti. It is 32 km from the municipality centre of Stepantsminda Stepantsminda ( ka, სტეფანწმინდა; formerly Kazbegi, ), is a townlet in the Mtskheta-Mtianeti region of north-eastern Georgia. Historically and ethnographically, the town is part of the Khevi province. It is the center of t .... See also * Ketrisi Mineral Vaucluse Sources * ''Georgian Soviet Encyclopedia'', V. 2, pp. 478–479, Tbilisi, 1980 year. ქეთერისის მინერალური ვოკლუზის ბუნების ძეგლი References {{Georgia-geo-stub Kobi Community villages ...
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Mineral Water
Mineral water is water from a mineral spring that contains various minerals, such as salts and sulfur compounds. Mineral water may usually be still or sparkling (carbonated/effervescent) according to the presence or absence of added gases. Traditionally, mineral waters were used or consumed at their spring sources, often referred to as "taking the waters" or "taking the cure", at places such as spas, baths, or wells. The term ''spa'' was used for a place where the water was consumed and bathed in; ''bath'' where the water was used primarily for bathing, therapeutics, or recreation; and ''well'' where the water was to be consumed. Today, it is far more common for mineral water to be bottled at the source for distributed consumption. Travelling to the mineral water site for direct access to the water is now uncommon, and in many cases not possible because of exclusive commercial ownership rights. There are more than 4,000 brands of mineral water commercially available worldwide ...
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Artesian Aquifer
An artesian aquifer is a confined aquifer containing groundwater under positive pressure. An artesian aquifer has trapped water, surrounded by layers of impermeable rock or clay, which apply positive pressure to the water contained within the aquifer. If a well were to be sunk into an artesian aquifer, water in the well-pipe would rise to a height corresponding to the point where hydrostatic equilibrium is reached. A well drilled into such an aquifer is called an ''artesian well''. If water reaches the ground surface under the natural pressure of the aquifer, the well is termed a ''flowing artesian well''. Fossil water aquifers can also be artesian if they are under sufficient pressure from the surrounding rocks, similar to how many newly tapped oil wells are pressurized. From the previous statement, it can be inferred that not all aquifers are artesian (i.e., water table aquifers occur where the groundwater level at the top of the aquifer is at equilibrium with atmospher ...
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Greater Caucasus
The Greater Caucasus ( az, Böyük Qafqaz, Бөјүк Гафгаз, بيوک قافقاز; ka, დიდი კავკასიონი, ''Didi K’avk’asioni''; russian: Большой Кавказ, ''Bolshoy Kavkaz'', sometimes translated as "''Caucasus Major''", "''Big Caucasus''" or "''Large Caucasus''") is the major mountain range of the Caucasus Mountains. The range stretches for about from west-northwest to east-southeast, between the Taman Peninsula of the Black Sea to the Absheron Peninsula of the Caspian Sea: from the Western Caucasus in the vicinity of Sochi on the northeastern shore of the Black Sea and reaching nearly to Baku on the Caspian. Geography The range is traditionally separated into three parts: * The Western Caucasus, between the Black Sea and Mount Elbrus * The Central Caucasus, between Mount Elbrus and Mount Kazbek * The Eastern Caucasus, between Mount Kazbek and the Caspian Sea In the wetter Western Caucasus, the mountains are heavily forest ...
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Mineral Spring
Mineral springs are naturally occurring springs that produces hard water, water that contains dissolved minerals. Salts, sulfur compounds, and gases are among the substances that can be dissolved in the spring water during its passage underground. In this they are unlike sweet springs, which produce soft water with no noticeable dissolved gasses. The dissolved minerals may alter the water's taste. Mineral water obtained from mineral springs, and the precipitated salts such as Epsom salt have long been important commercial products. Some mineral springs may contain significant amounts of harmful dissolved minerals, such as arsenic, and should not be drunk. Sulfur springs smell of rotten eggs due to hydrogen sulfide (H2S), which is hazardous and sometimes deadly. It is a gas, and it usually enters the body when it is breathed in. The quantities ingested in drinking water are much lower and are not considered likely to cause harm, but few studies on long-term, low-level exposu ...
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Kazbegi National Park
Kazbegi National Park is in Kazbegi Municipality in the Mtskheta-Mtianeti region of north-eastern Georgia.Kazbegi National Park in Georgia
''Protected Planet''
Kazbegi National Park is a popular tourist destination despite the lack of basic tourism infrastructure. Historical monuments worth a visit are the fourteenth-century Sameba temple, the tenth-century Garbanikerk, the Sioni basilica, the Akhaltsikhe basilica and the seventeenth-century Sno Cast ...
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Sakhizari Cliff Natural Monument
Sakhizari Cliff Natural Monument ( ka, სახიზარის კლდის ბუნების ძეგლი) is a complex geologic structure that was formed due to abundant rainfall causing erosion of the volcanic mountain Khabarjina. Local population call this place "the ruins of the rocks" and in the past centuries at wartime villagers would seek refuge by climbing the cliffs when the enemy approached. Scenic cliffs are located in Kazbegi Municipality in river Terek Gorge near village Sioni at 3136 meters above sea level. It is part of ''Kazbegi Protected Areas''Kazbegi
Support Programme for Protected Areas in the Caucasus - Georgia (SPPA-Georgia) along with

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Abano Mineral Lake Natural Monument
Abano Mineral Lake Natural Monument ( ka, აბანოს მინერალური ტბა, tr) is a small karst lake in Kazbegi Municipality in Truso valley on the left bank of Terek River, to the east of the village Abano at 2,127 m above sea level. Lake characteristics The lake was created by a carbon dioxide filled underground stream flowing to the surface through carbonate rocks from the late Jurassic period. The lake "boils" loudly with carbon dioxide bubbles bursting. The outflow of the stream is 2.5 million liters per 24 hours. The total surface area of the lake is 0.04 ha. The emission of gas in calm weather causes carbon dioxide to accumulate in lower levels. Small animals suffocate when they get near the lake, which is why there are dead animals there, such as mice, lizards, frogs and some birds. It is part of ''Kazbegi Protected Areas''
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Truso Travertines Natural Monument
Truso Travertines Natural Monument ( ka, თრუსოს ტრავერტინი) is calcareous sinter or tufa in :ka:თრუსოს ხეობა, Truso valley on the right bank of Terek river at 2093 meters above the sea level in Kazbegi Municipality, Georgia (country), Georgia. It is located about 2 km from village Keterisi where local population lives only seasonally. This limestone was formed when carbonate minerals precipitation (chemistry), precipitate out of ambient temperature water. Travertine in some places is covered with a thin layer of transparent water on the white surface of the slopes where intensive development process is still ongoing. It is part of ''Kazbegi Protected Areas''Kazbegi
Support Programme for Protected Areas in the Caucasus - Georgia (SPPA-Georgia) along with Kazbegi National Park and fi ...
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Jvari Pass Travertine Natural Monument
Jvari Pass Travertine Natural Monument ( ka, ჯვრის უღელტეხილის ტრავერტინი) is calcareous sinter or tufa in Baidara River valley on the left bank of the road tunnel of the Kobi-Gudauri motorway at 2197 meters above the sea level in Kazbegi Municipality, Georgia. This limestone was formed when carbonate minerals precipitate out of ambient temperature water. Travertine in some places is covered with a thin layer of transparent water on the white surface of the slopes where the intensive development process is still ongoing. It is part of ''Kazbegi Protected Areas''Kazbegi
Support Programme for Protected Areas in the Caucasus - Georgia (SPPA-Georgia) along with