Samshvilde Canyon Natural Monument
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Samshvilde Canyon Natural Monument
Samshvilde Canyon Natural Monument ( ka, სამშვილდის კანიონი) is part of the Khrami gorge, and provided natural defense to the Samshvilde fortress in the area around the confluence of the Khrami and Chivchavi (Chivchava or Chivchivi) rivers near Samshvilde village and the ruins of historic Samshvilde located in Tetritsqaro Municipality, in the Kvemo Kartli region of southeastern Georgia,Samshvilde Canyon in Georgia
''Protected Planet'' 2014–2019
548-605 . Samshvilde Canyon also includes part of the Chivchav (Chivchava)
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Tetritskaro
Tetritskaro or Tetritsqaro ( ka, თეთრიწყარო, tr; , az, Ağbulaq) is a town in Kvemo Kartli in southern Georgia. It is the municipal center of Tetritsqaro Municipality. According to 2014 Georgian Census its population is 3,093. The Baku-Tbilisi-Kars railway which opened in 2017, runs along the rail line through the town. History Original settlement on this location was called ''Garisi'' (გარისი), but due to invasions and wars this place got abandoned and in the beginning of the 19th century became a ghost town.''ლორთქიფანიძე ი.,'' ქვემო ქართლი XVIII საუკუნის პირველ მეოთხედში, ნაწ. 1-2, 3-4, თბ., 1935-1938 Later, this area was resettled by Georgian Azerbaijanis, who called the settlement ''Agbulakhi''; the name was of Azerbaijani origin and literally meant ''white spring''.Pospelov, p. 23 In 1940, the name was changed to Tetri-Tskaro, which, ...
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Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical ero ...
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Canyons And Gorges Of Georgia (country)
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ...
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