| Mount Homa | |
|---|---|
Mount Homa in 1994 | |
| Highest point | |
| Elevation | 1,751 m (5,745 ft) |
| Coordinates | 0°23′S 34°30′E / 0.38°S 34.50°E |
| Geography | |
| Location | Kenya |
| Geology | |
| Formed by | Volcanism along the Gregory Rift |
| Mountain type | Complex volcano |
| Last eruption | Unknown |
Mount Homa is a complex volcano located in western Kenya. It forms a broad peninsula on the southern shore of Winam Gulf, an extension of Lake Victoria. This peninsula defines Homa Bay and the mountaintop is about 20 kilometres (12 mi) north of the town of that name.
Although no documented eruptions have happened during the Holocene, it has an active geothermal field with water temperatures reaching as high as 80 C. This is interpreted as heat being generated by a magma chamber below Homa and shows that the volcano is still potentially active.[1]
In the Luo language Got Uma or God Marahuma means "famous mountain".
The mountain is formed of carbonatite lava and dates from Miocene to Pleistocene. Along with the active Ol Doinyo Lengai, it is one of the very few carbonatite volcanoes in the world.
Homa peninsula is part of Homa Bay County. The village of Kanjira (Kanjera) is eponymous of the Kanjera paleontological site, first excavated by Louis Leakey in the 1930s. It is one of the oldest known Oldowan sites, dated at c. 2 million years old.[2]

See also
References
- ↑ Bach, Juliet (Oct–Nov 2014). "STUDY TITLE GEOLOGY AND GEOMORPHOLOGY OF HOMA AREA AND ITS RESOURCE POTENTIAL". Academia. MASENO UNIVERSITY. Retrieved 9 November 2025.
- ↑ Bishop, L. C.; Plummer, T. W.; Ferraro, J. V.; Braun, D.; Ditchfield, P. W.; Hertel, F.; Kingston, J. D.; Hicks, J.; Potts, R. (Mar–Jun 2006). "Recent Research into Oldowan Hominin Activities at Kanjera South, Western Kenya". The African Archaeological Review. 23 (1/2): 31–40. doi:10.1007/s10437-006-9006-1. JSTOR 25470615.
External links
- "Homa Mountain". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-24.