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Random pictures
Smooth fracture surfaces at the lava dome: trees, having their roots reach into the tiniest crevasses, are clinging onto the vertical walls like free-climbers.
Smooth fracture surfaces at the lava dome: trees, having their roots reach into the tiniest crevasses, are clinging onto the vertical walls like free-climbers.
 

Methana volcano

Lava domes 740 m
Saronic Gulf, Greece, 37.62°N / 23.34°E
Current status: dormant (1 out of 5)
Methana volcano books
Typical eruption style: Effusive, construction of lava domes, hydrothermal explosions.
Methana volcano eruptions: around 1700 (submarine eruption of "Pavsanias", aprox. 1,5 km north-west of Methana), 238 B.C (near Kameni Hora) Methana's historic lava dome which formed in 238 BC.
TimeMag. / DepthDistanceLocation
Sat, 15 Apr
Sat, 15 Apr 14:10 UTCM 2.0 / 13.2 km18 km19 Km SSE from Aigina
Wed, 12 Apr
Wed, 12 Apr 21:59 UTCM 1.4 / 9 km43 km11 Km S from Athinai
Tue, 11 Apr
Tue, 11 Apr 12:18 UTCM 2.1 / 10.7 km43 km15 Km E from Idhra
Sun, 9 Apr
Sun, 9 Apr 11:55 UTCM 1.8 / 14.9 km20 km20 Km SE from Aigina
Sat, 8 Apr
Sat, 8 Apr 16:07 UTCM 1.6 / 10.9 km25 km16 Km S from Corinth
View all recent quakes
Methana peninsula, located opposite Aegina Island in the Saronic Gulf of Greece, is the northwestern, still weakly active part of the Aegean volcanic arc.
An eruption in 238 BC built a small lava dome on the northern tip of the peninsula and was described by Greek and Roman historians (e.g. Pausanias). Methana peninsula is famous for its hot springs and thermal baths, hence its name.

Background:

Methana volcanic system comprises a group of 32 lava mostly dacitic lava domes, whose formation started about 1-2 million years ago. The latest activity was likely around 1700 AD in form of a submarine eruption off the northern coast.
An active hydrothermal system characterizes the area, controlled by a E-W fault system that crosses the town of Methana where thermal springs are found.


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