Tskhouk-Karckar

Tskhouk-Karckar
Qarqar
Tskhouk-Karckar is located in Caucasus Mountains
Tskhouk-Karckar
Tskhouk-Karckar
Location on Armenia–Azerbaijan border
Tskhouk-Karckar is located in Armenia
Tskhouk-Karckar
Tskhouk-Karckar
Tskhouk-Karckar (Armenia)
Tskhouk-Karckar is located in Azerbaijan
Tskhouk-Karckar
Tskhouk-Karckar
Tskhouk-Karckar (Azerbaijan)
Highest point
Elevation3,139 m (10,299 ft)[1]
Listing
Coordinates39°44′31″N 45°59′31″E / 39.742°N 45.992°E / 39.742; 45.992[1]
Geography
Countries
Geology
Mountain typePyroclastic cones
Volcanic arc/beltSiunik volcanic ridge[2]
Last eruption3000 BCE ± 300 years[3]

Tskhouk-Karckar or Qarqar is a group of pyroclastic cones which is located in the central part of the Siunik volcanic ridge at the border of Armenia and Azerbaijan 60 km (37 mi) SE of Lake Sevan. The volcanoes lie on the northwest side of Tskhouk volcano and are constructed on a volcanic basement or rhyolites, basaltic andesites and dacites. The volcanoes erupted voluminous and long lava flows, grouped in three age-based stages of varying age and conservation. Petroglyphs have been found buried under the most recent stages and broken by earthquake activity, suggesting activity between the 4th–early 3rd millennium BC and 4720 ± 140 years BP, a date established by C14 analysis on graves inside the lava flows. There is evidence indicating that the last stage of activity resulted in abandonment of the area by humans, only resuming during the Middle Ages.[2]

References

[edit]
  1. ^ a b "Tskhouk-Karckar". Global Volcanism Program. Smithsonian Institution. Retrieved 2022-11-12.
  2. ^ a b Karakhanian, A.; Djrbashian, R.; Trifonov, V.; Philip, H.; Arakelian, S.; Avagian, A. (2002). "Holocene-historical volcanism and active faults as natural risk factors for Armenia and adjacent countries". Journal of Volcanology and Geothermal Research. 113 (1–2): 319–344. Bibcode:2002JVGR..113..319K. doi:10.1016/S0377-0273(01)00264-5. ISSN 0377-0273.
  3. ^ "Tskhouk-Karckar: Eruptive History". Global Volcanism Program. Smithsonian Institution. Retrieved 2022-11-12.