Harrat Khaybar
Khaybar, Harrat
Campo volcánico · Saudi Arabia · 2093 m

- Tipo
- Campo volcánico
- País
- Saudi Arabia
- Región
- Arabia-Central Asia Volcanic Regions / Western Arabia Volcanic Province
- Altitud
- 2093 m
- Coordenadas
- 25.500, 40.000
- Última erupción
- 650
- Contexto tectónico
- Intraplate / Continental crust (> 25 km)
- Forma volcánica
- Cluster
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
Harrat Khaybar, one of Saudi Arabia's largest volcanic fields, covers an area of more than 14,000 km2 N of Madinah (Medina). A 100-km-long N-S linear vent system contains felsic lava domes, tuff rings, the Jabal Qidr stratovolcano, and numerous small basaltic cones. At least seven lava flows are less than 4,500 years old, and another eight are less than 1,500 years old. In the latter category is the 55-km-long Habir lava flow as well as Jabal Qidr stratovolcano, the only stratovolcano in the Harrats of western Saudi Arabia. An eruption was reported in early Mohammedan times during the 7th century CE. Lavas from Harrat Khaybar overlap older lavas of Harrat Kura to the west and merge with lavas from Harrat Ithnayn to the north.
Resumen de Wikipedia
Resumen en inglésḤarrat Khaybar is a volcanic field located north of Medina in the Hejaz, Saudi Arabia. It covers an area approximately 12,000 km2 (4,600 sq mi). The most recent eruption occurred between 600 and 700 AD. Man-made stone structures dating to the Neolithic period have been studied in Harrat Khaybar.
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Historial de erupciones
Línea de tiempo detallada
- 650 (±50 años)VEI 2Observado650 – En cursoHarrat Lali
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.