Karthala
Africa's Most Active Shield Volcano
2,350 m
2007
Shield volcano
Union of the Comoros
Location
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Volcanic Hazards & Risk Assessment
Primary Hazards
- Lava flows and fountaining
- Volcanic gas emissions
- Local explosive activity
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 19 years ago | Recent | Recently active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Authority Sources
Interesting Facts
Karthala has erupted 35 times since approximately 1050 CE, making it one of Africa's most active volcanoes.
The volcano forms the southern two-thirds of Grand Comore Island, making it one of the largest volcanic edifices in the Indian Ocean by land area.
Grand Comore has no rivers or reservoirs — the island's 400,000 residents rely entirely on rainwater cisterns and shallow wells that are highly vulnerable to volcanic ashfall contamination.
In 2005, two eruptions within seven months displaced over 40,000 people and created a humanitarian water crisis requiring international aid.
An 1860 lava flow from the summit caldera traveled approximately 13 km to the northwest, reaching the coast just north of the capital city of Moroni.
Between 1848 and 1883, Karthala erupted at least 14 times — an average of roughly one eruption every 2.5 years.
Karthala's two overlapping summit calderas measure 3–4 km across and were formed by repeated roof collapses when magma drained through lateral rift zones.
The Comoros archipelago is known as the 'Perfume Islands' because the volcanic soil supports prolific growth of ylang-ylang, vanilla, and cloves.
The submarine eruption of Fani Maoré off Mayotte in 2018–2021 was the largest underwater eruption ever documented, occurring in the same volcanic province as Karthala.
Karthala's basaltic lavas are so fluid that historical flows have extended to both coasts of Grand Comore, building new land where they entered the Indian Ocean.