Volos-Atalanti
Volcanic field 900 m / 2953 ft
Greece, 39.03°N / 22.8°E
Aktueller Status: (wahrscheinlich) erloschen (0 von 5)
Greece, 39.03°N / 22.8°E
Aktueller Status: (wahrscheinlich) erloschen (0 von 5)
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Ausbrüche: None during the past 10,000 years
Less than 2.58 million years ago (Pleistocene)
Letzte Erdbeben in der Nähe:
Zeit | Stärke / Tiefe | Entfernung / Lage | ||
Dienstag, 9. August 2022 GMT (1 Beben) | ||||
9. Aug. 2022 03:40 (GMT +3) (9. Aug. 2022 00:40 GMT) | 1.8 8.1 km | 35 km (22 mi) Greece: 9 Km W From Milies Piliou | ||
Donnerstag, 4. August 2022 GMT (1 Beben) | ||||
4. Aug. 2022 09:35 (GMT +3) (4. Aug. 2022 06:35 GMT) | 2.4 10 km | 19 km (12 mi) Greece | ||
Dienstag, 2. August 2022 GMT (1 Beben) | ||||
2. Aug. 2022 07:01 (GMT +3) (2. Aug. 2022 04:01 GMT) | 2.8 15 km | 28 km (17 mi) Greece: 7 Km ENE From Lamia | ||
Freitag, 29. Juli 2022 GMT (1 Beben) | ||||
29. Jul. 2022 06:29 (GMT +3) (29. Jul. 2022 03:29 GMT) | 2.0 11 km | 43 km (27 mi) Greece: 2 Km S From Milies Piliou |
Beschreibung
The Volos-Atalanti (also known as Volos-Evia) area contains a number of small monogenetic Pliocene to Pleistocene lava flows, cones, and domes. The largest lava outcropping, which originated from the Migoula cone, is about 0.2 km3 in volume and 6-7 km long (Innocenti et al., 2010). The volcanic products are generally basaltic trachyandesitic (Innocenti et al., 2010). The lava flows at Porphyrion and Microthivai date to about 1.6-1.3 Ma. The Toumbanos Hills lava dome, near Achilleion, dates to about 3.4-2.7 Ma. In the Atalanti channel, the cones and lava flows of the Likhades Islands date to about 0.5 Ma, as does a lava flow at Kammena Vourla on the Greek coast (Innocenti et al., 2010). K-Ar dates from Fytikas et al. (1984) range from 3.0-0.5 Ma. Volos-Evia is believed to lie on the westward extension of the North Anatolian Fault, rather than the Hellenic Arc (Innocenti et al., 2010).---
Smithsonian / GVP volcano information


Siehe auch: Sentinel hub | Landsat 8 | NASA FIRMS