Why is the Ruwenzori Range an important earthquake area?

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The Ruwenzori Range is an important earthquake epicenter because of ongoing tectonic activity along its fault lines. Unlike most other major mountains in East Africa, which are of volcanic origin, the Ruwenzori is a massive horst—a block of the Earth's crust that has been uplifted.123

This range was formed as an ancient plateau of gneisses and schists was upfaulted on its western side and upwarped on its eastern side. Because these movements along the faults continue to occur, the system remains a significant area for seismic activity.1