Data from the Global Volcanism Program of the Smithsonian Institution
Details for: Milos
The western side of Mílos Island contains a cluster of lava domes. Mílos and adjacent small islands have grown from submarine and subaerial volcanism that initially was dominantly andesitic and basaltic, but ended with primarily rhyolitic eruptions. Phreatic explosions, commonly producing overlapping craters typically less than 1 km in diameter, continued from late-Pleistocene to Holocene time. Photo by Ichio Moriya (Kanazawa University).
Volcano Number:212030
Volcano Name:Milos
Country:Greece
Volcano Type:Stratovolcano(es)
Last Eruption:140 CE
Elevation:751m
Tectonic Setting:Subduction zone / Continental crust (> 25 km)
Pop. within 5km:6688
Pop. within 10km:7389
Pop. within 30km:9851
Pop. within 100km:73100
Latitude:36.699
Longitude:24.439


Eruption Data from the Global Volcanism Program of the Smithsonian Institution
Emissions Data from the Global Volcanism Program of the Smithsonian Institution
Sorry. No emissions data found for this volcano.

Data from the Earthchem Library
Sorry. No data exist for this volcano in the EarthChem Library.
Data from the Earthchem Portal

Data from the SESAR Database

Data from the MaGa Database
Sorry. No data exist for this volcano in the MaGa database.

Data from UNAVCO
Sorry. No data exist for this volcano in the UNAVCO database.

Data from USIEI

Data from IRIS FDSNWS