Campo volcánico de Bayuda
Bayuda Volcanic Field
Campo volcánico · Sudan · 670 m

- Tipo
- Campo volcánico
- País
- Sudan
- Región
- Northern Africa Volcanic Regions / Southeast Sahara Volcanic Province
- Altitud
- 670 m
- Coordenadas
- 18.330, 32.750
- Última erupción
- 850
- Contexto tectónico
- Intraplate / Continental crust (> 25 km)
- Forma volcánica
- Cluster
- Roca principal
- Trachybasalt / Tephrite Basanite
Resumen geológico
The Bayuda volcanic field is located in the Bayuda Desert of NE Sudan, south of the major Abu Hamed bend of the Nile River about 300 km N of Khartoum. More than 90 eruptive centers along a WNW-ESE line were constructed over Precambrian and Paleozoic granitic rocks near the center of the Bayuda Desert. Most vents are cinder cones that produced lava flows which breached the cones. About 10% of vents in the field are explosion craters, the largest of which, named Hosh ed Dalam, is 1.3 km wide and up to 500 m deep. The youngest basalts appear to post-date the last period of moist climate in Sudan, which ended as recently as about 5,000 years ago. One of the least eroded lava flows was dated at about 1,100 years ago.
Resumen de Wikipedia
Resumen en inglésBayuda volcanic field is a volcanic field in Sudan, within the Bayuda Desert. It covers a surface of about 11 by 48 kilometres and consists of a number of cinder cones as well as some maars and explosion craters. These vents have erupted 'a'ā lava flows.
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Historial de erupciones
Línea de tiempo detallada
- 850 (±50 años)VEI ?Estimación geológica850 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.