Adwa
Estratovolcán · Ethiopia · 1670 m

- Tipo
- Estratovolcán
- País
- Ethiopia
- Región
- Eastern Africa Volcanic Regions / Main Ethiopian Rift Volcanic Province
- Altitud
- 1670 m
- Coordenadas
- 10.063, 40.831
- Última erupción
- Desconocido
- Contexto tectónico
- Rift zone / Intermediate crust (15-25 km)
- Forma volcánica
- Composite
- Roca principal
- Rhyolite
Resumen geológico
Adwa (also known as Aabida, Amoissa, or Dabita), is a broad stratovolcano in the southern Afar area immediately east of the younger vegetated Ayelu volcano. It has a roughly 3 x 4 km caldera that originated following eruption of voluminous ignimbrites, with a trachytic dome extruded in the eastern part of the caldera. Scoria cones are located on the floor of the caldera and on its NW and SW flanks. Extensive young basaltic lava flows cover the flanks and overlap a sedimentary plain to the SE. Many fumaroles occur within the caldera. Satellitic pyroclastic cones and lava domes were considered to be only a few hundred years old (Mohr 1980, pers. comm.). Dark lava flows originating from cones about 4 km from the caldera rim on the SW flank cover more than 50 km2.
Resumen de Wikipedia
Resumen en inglésAdwa is a stratovolcano in Ethiopia, located in the western Afar Region region and has a 4 by 5 km caldera. Due to the location of the volcano near the boundary between Afar and Issa tribes, little is known about the past and present behavior of the volcano. However, an earthquake and InSAR study conducted by Derek Keir and colleagues shows that a magma intrusion around 5 km deep and 8 km long emanated away from the eastern side of the volcano in May 2000.
Wikipedia · CC BY-SA · Leer artículo completo →
Historial de erupciones
Línea de tiempo detallada
- 1928VEI 2Estimación geológica1928 – En curso
- 1828VEI 2Estimación geológica1828 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.