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Geological Formation

Garni Gorge

Volcanic Formations

Garni Gorge is a natural gorge in Armenia, about 23 kilometers east of Yerevan, carved by the Goght River just below the village of the same name. Its cliff walls display a dramatic run of well preserved basalt columns, a formation local guides call the Symphony of the Stones. The gorge is protected by law as a natural monument and sits near the first century Temple of Garni and the Geghard Monastery.

Facts
Classification
Protected Status
National Monument or Landmark 1
Connections

Associated With

Basalt, Materials
Source Garni Gorge (Wikipedia)

Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Garni Gorge

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Garni Gorge
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Garni Gorge
Sources
1. Wikidata: Garni Gorge
  • Wikidata Q4133851, class allow-list match (w-wdresolver-0926)
  • Lead section
    The Garni Gorge is protected by law and listed as a natural monument.
View the Source
Garni Gorge (Wikipedia)
  • Lead section
    The Garni Gorge is situated 23.3 kilometres (14.5 mi) east of Yerevan, Armenia, just below the village of the same name.
  • Associated With: Basalt, Lead paragraph
    Along the sides of the gorge are cliff walls of well-preserved basalt columns, carved out by the Goght River.
View the Source
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