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Asseb Volcano

Assab Volcanic Field

Campo vulcanico · Eritrea · 987 m

The long chain of pyroclastic cones and lava flows extending E-W across this Landsat image is the Assab volcanic field near the Red Sea coast in southern Eritrea. This spectacular range of basaltic cinder cones and associated lava flows covers a 55 x 90 km area, and flows reached the Red Sea along a broad front. The vents were constructed along a broad E-W-trending line that extends to the coastal city of Assab, out of view to right.
The long chain of pyroclastic cones and lava flows extending E-W across this Landsat image is the Assab volcanic field near the Red Sea coast in southern Eritrea. This spectacular range of basaltic cinder cones and associated lava flows covers a 55 x 90 km area, and flows reached the Red Sea along a broad front. The vents were constructed along a broad E-W-trending line that extends to the coastal city of Assab, out of view to right. · Foto: NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology). · Wikimedia Commons
Tipo
Campo vulcanico
Paese
Eritrea
Regione
Eastern Africa Volcanic Regions / Afar Rift Volcanic Province
Altitudine
987 m
Coordinate
12.950, 42.430
Ultima eruzione
Sconosciuto
Contesto tettonico
Rift zone / Intermediate crust (15-25 km)
Forma vulcanica
Cluster
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

The Assab volcanic field near the Red Sea coast in southern Eritrea forms a spectacular range of basaltic cinder cones and associated lava flows. The massive lava field covers a 55 x 90 km area, and flows reached the Red Sea along a broad front. The vents of the Assab volcanic field, also known as Ado Ale or Ud'ale, were constructed along a broad E-W line that extends to the coastal city of Assab.

Sintesi da Wikipedia

Riassunto in inglese

The Assab volcanic field is a group of basaltic cinder cones and associated lava flows located in the Southern Red Sea region of Eritrea. With a peak elevation of 987 m (3,238 ft), its most recently identified eruption occurred within the last 12,000 years during the current Holocene epoch.

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