Saltar al contenido principal

Longonot

Estratovolcán · Kenya · 2776 m

Longonot as seen from the flanks of Suswa volcano (SSW of Longonot) in the Eastern Rift Valley of Kenya. The modern cone was constructed within a broad 8 x 12 km caldera and itself contains a smaller 1.8-km-wide summit crater that gives the summit a flat profile. Post-caldera lavas are found on the caldera floor and on the flanks. Masai tradition records a lava flow on the N flank during the 19th century.
Longonot as seen from the flanks of Suswa volcano (SSW of Longonot) in the Eastern Rift Valley of Kenya. The modern cone was constructed within a broad 8 x 12 km caldera and itself contains a smaller 1.8-km-wide summit crater that gives the summit a flat profile. Post-caldera lavas are found on the caldera floor and on the flanks. Masai tradition records a lava flow on the N flank during the 19th century. · Foto: Photo by Tom Jorstad, 1990 (Smithsonian Institution). · Wikimedia Commons
Tipo
Estratovolcán
País
Kenya
Región
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
Altitud
2776 m
Coordenadas
-0.914, 36.446
Última erupción
1863
Contexto tectónico
Rift zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Trachyte / Trachydacite
Resumen geológico

The trachytic Longonot stratovolcano SE of Lake Naivasha in the Gregory Rift valley contains a 8 x 12 km caldera. Formation of the caldera accompanied large explosive eruptions about 21,000 years ago. A large central cone that was constructed within the caldera, which forms the summit, is truncated by a circular, 1.8-km-wide crater. Post-caldera lavas are found on the caldera floor and the volcano's flanks, marking a late stage of effusive eruptions. A well-preserved satellitic cone is located on the NE flank. Masai tradition records a lava flow on the N flank during the 19th century. Similarly youthful-looking lava flows occur on the SW flank.

Resumen de Wikipedia

Resumen en inglés

Mount Longonot is a stratovolcano located southeast of Lake Naivasha in the Great Rift Valley of Kenya, Africa. It is thought to have last erupted in the 1860s. Its name is derived from the Maasai word Olongongot, meaning "mountains of many spurs" or "steep ridges".

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
7200 BCE~6898 BCE · 1 erupciones · VEI máx. ?1460 BCE~1158 BCE · 1 erupciones · VEI máx. ?1561~1863 · 1 erupciones · VEI máx. 07200 BCE5085 BCE2668 BCE554 BCE1561

Línea de tiempo detallada

  1. 1863 (±5 años)VEI 0Estimación geológica
    1863 – En curso
    Northern flank
  2. 1330 a. C. (±100 años)VEI ?Estimación geológica
    BCE 1330 – En curso
  3. 7200 a. C. (±100 años)VEI ?Estimación geológica
    BCE 7200 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.