Abstract
The cyclic growth and destruction of the Late Cenozoic Stratovolcano Mt. Kenya have been reconstructed for its southeastern segment. At least three major debris avalanche deposits have been reconstructed and dated. The oldest deposits indicate an edifice collapse around 4.9Ma (
Original language | English |
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Pages (from-to) | 44-54 |
Journal | Global and Planetary Change |
Issue number | 123 |
DOIs | |
Publication status | Published - 2014 |