Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Adishi Glacier

Glaciers and Ice Formations

Adishi Glacier is a valley glacier in the central Greater Caucasus Mountain Range, in the Svaneti region of Georgia, on the southern slopes of the Caucasus. It is 9 kilometers long with a surface area of 12.9 square kilometers, its tongue descending to 2,298 meters above sea level, and it is fed by runoff and ice from the adjacent glaciers of Tetnuldi, Gistola and Lakutsia. The glacier is the source of the river Adishchala and takes its name from the nearby village of Adishi. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Classification
Protected Status
International Treaty Protected Area 1
Connections

Caused By

Glaciation, Processes

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

Source Wikidata: Adishi Glacier

In Discipline

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

Source Wikidata: Adishi Glacier
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Adishi Glacier
Sources
1. UNEP-WCMC and IUCN: Protected areas at the coordinates of Adishi Glacier, World Database on Protected Areas
UNEP-WCMC and IUCNname_eng and desig_eng
Quote, name_eng and desig_eng
"name_eng": "Svaneti 1", "desig_eng": "Emerald Network"
View the Source
Adishi Glacier (Wikipedia)
Lead section
Quote, Lead section
is a valley glacier located in the central part of the Greater Caucasus Mountain Range in the Svaneti Region of Georgia.
View the Source
Wikidata: Adishi Glacier
Wikidata Q4683018, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.