Mount Meru
Meru
Stratovolcano · Tanzania · 4550m

- Type
- Stratovolcano
- Country
- Tanzania
- Region
- Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
- Elevation
- 4550m
- Coordinates
- -3.244, 36.750
- Last eruption
- 1910
- Tectonic setting
- Rift zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Phonolite
Geological summary
Meru has a conical profile when viewed from the west, but there is a 4-km-wide collapse crater to the E. The summit collapse is associated with the early Holocene Momella event that resulted in debris avalanche and lahar deposits as far as the W flank of Kilimanjaro. Cones and lava domes are located on all sides; a maar field is present on the lower N flank. Activty from the Ash Cone, inside the open crater, was reported around 1878 and in 1910 CE. A second vent between it and the headwall produced lava flows that cover much of the caldera floor. Kisaka et al. (2021) identified three late Pleistocene explosive eruptions during 31-38 ka BP (cal 14C).
From Wikipedia
Mount Meru is a dormant stratovolcano located 70 kilometres (43 mi) west of Kilimanjaro in southeast Arusha Region, Tanzania. At a height of 4,562.13 metres (14,968 ft), it is visible from Mount Kilimanjaro on a clear day, and is the eighth-highest mountain of Africa.
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Eruption history
Detailed timeline
- 1910VEI 2Observed1910-10-26 – 1910-12-22Ash Cone
- 1886VEI 0Observed1886 – OngoingDome NW of Ash Cone
- 1878 (±1 yrs)VEI 2Observed1878 – OngoingDome NW of Ash Cone
- 5850 BCEVEI 4Geological estimateBCE 5850 – Ongoing
External links
⚠ For reference only. Not for emergency response.