Arabika Massif
Geology
The 13-km-long massif is composed of Lower Cretaceous and Upper Jurassic limestones that dip continuously southwest to the Black Sea and plunge below the modern sea level. The area is densely wooded, with large areas of both coniferous forest and mixed woodland.
The Arabika contains a number of remarkable caves, gorges, wells, and precipices, including the Veryovkina Cave and Voronya Cave, the world's deepest caves. Alexander Kruber was the first to explore some of these features in 1909.
According to Rebecca Felix, the Arabica's "towering heights of limestone suggest the possibility of amazingly deep caves, boring the length of the massif and into the earth below its base".
Notes
- ^ The political status of Abkhazia is disputed. Having unilaterally declared independence from Georgia in 1992, Abkhazia is formally recognised as an independent state by 5 UN member states (two other states previously recognised it but then withdrew their recognition), while the remainder of the international community recognizes it as de jure Georgian territory. Georgia continues to claim the area as its own territory, designating it as Russian-occupied territory.
References
- ^ Mta Arabika GeoNames
- ^ Great Soviet Encyclopaedia
- ^ Tabor, James M. (2010). Blind Descent: The quest to discover the deepest place on Earth. New York: Random House. p. 159. ISBN 978-1-4000-6767-1.
- ^ Felix, R. (2014). Exploring Caves. ABDO Publishing Company. p. 48. ISBN 9781629680453. Retrieved 2015-04-13.
43°25′N 40°20′E / 43.41°N 40.34°E
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