Caucasus Mountains

The Caucasus Mountains are a major mountain system between the Black Sea and the Caspian Sea, comprising the Greater and Lesser Caucasus ranges. The region contains some of Europe’s highest peaks and a high level of linguistic and ecological diversity.

Rugged high peaks, extensive glaciation on the higher northern ridges and deep river valleys characterise the Greater Caucasus, while the Lesser Caucasus offers lower, more rolling highlands. The area is popular for mountaineering, skiing, trekking and visiting historic cultural sites and highland villages.

Numerous distinct cultural regions and protected areas exist across the range, including traditional highland settlements in Svaneti and Kazbegi (in Georgia) and alpine landscapes that support specialist wildlife and endemic plants.

The Caucasus formed through the long-term collision of the Arabian and Eurasian tectonic plates, producing complex geology and uplift. Historically it has been a crossroads of empires and peoples, which is reflected in the region’s linguistic and cultural patchwork.

The mountain system stretches from the eastern Turkish border in the west to the Caspian Sea in the east, spanning parts of Russia, Georgia, Armenia and Azerbaijan. The Greater Caucasus forms a climatic and political divide between north and south.

• Highest peak: The highest peak in the Caucasus mountain system is **Mount Elbrus** at 5,642 metres, located on the western end of the Greater Caucasus.
• Environment: Climatic and ecological zones change rapidly with altitude; valleys hold small settlements and historic monasteries while higher zones offer glaciers and alpine terrain.

What to See #

• Greater Caucasus: The higher, glaciated chain forming the northern flank and main watershed between the Black and Caspian seas; contains the highest summits of the system.
• Lesser Caucasus: A lower, more eroded chain to the south and southeast with lower peaks and rolling highlands extending toward the Armenian Highlands and Anatolia.