Gyali
Sign in to saveAlso known as Giali
Gyali ( "glass", also spelled Giali or Yali, pronounced ) is a Greek volcanic island in the Dodecanese, located halfway between the south coast of Kos (Kardamaina) and Nisyros. It consists of rhyolitic obsidian lava domes and pumice deposits (which are mined in huge quantities). No historical eruptions are known, but the most recent pumice eruptions overlie soils containing pottery and obsidian artifacts from the Neolithic period (10,000–4,500 BC). The island has two distinct segments, with the northeastern part almost entirely made of obsidian and the southwestern part of pumice. These are co
Key facts
- Islands.name
- Gyali
- Islands.native_name
- Γυαλί
- Islands.native_name_lang
- el
- Islands.image_name
- Yiali.jpg
- Islands.image_caption
- Pumice mining on Gyali
- Islands.map
- Greece
- Islands.archipelago
- Dodecanese
- Islands.area_km2
- 4.558
- Islands.highest_mount
- Volcano
- Islands.elevation_m
- 180
- Islands.country
- Greece
- Islands.country_admin_divisions_title
- Region
- Islands.country_admin_divisions
- South Aegean
- Islands.country_admin_divisions_title_1
- Regional unit
- Islands.country_admin_divisions_1
- Kos
- Islands.country_admin_divisions_title_2
- Municipality
- Islands.country_capital
- Chora
- Islands.population
- 7
via Wikipedia infobox
Wikidata facts
- Population
- 13
- Area
- 4.558
- Elevation
- 180
- Image
- Yiali.jpg
- Width
- 0.25
- Length
- 5.1
Show 2 more facts
- Commons category
- Gyali
- native label
- Γυαλί
Sources (1)
via Wikidata · CC0
~3 min read
Article
5 sectionsContents
- Geography
- Settlement
- See also
- References
- External links
Gyali ( "glass", also spelled Giali or Yali, pronounced ) is a Greek volcanic island in the Dodecanese, located halfway between the south coast of Kos (Kardamaina) and Nisyros. It consists of rhyolitic obsidian lava domes and pumice deposits (which are mined in huge quantities). No historical eruptions are known, but the most recent pumice eruptions overlie soils containing pottery and obsidian artifacts from the Neolithic period (10,000–4,500 BC). The island has two distinct segments, with the northeastern part almost entirely made of obsidian and the southwestern part of pumice. These are connected by a narrow isthmus and beach made of modern reef sediments. Anciently, the island was known as Istros ().
==Geography== thumb|From right top counterclockwise: Stroggyli, Gyali, Pergoússa, Paheià and Nisyros.
On the map
2 mapped locations