The Ruwenzori Mountains located along the border of the Democratic Republic of the Congo and Uganda differ fundamentally in their structural origin from nearby prominent peaks such as Mount Kilimanjaro and Mount Kenya within the East African Rift System. Which of the following best explains this geological distinction?
- The Ruwenzori Mountains were formed by tectonic uplift of a basement block (horst) between parallel faults, whereas Mount Kilimanjaro and Mount Kenya were built up by volcanic eruptions along the rift zone.Answer
- BThe Ruwenzori Mountains resulted from alpine folding of marine sedimentary strata during the Tertiary period, whereas Mount Kilimanjaro was produced by rift valley subsidence and graben formation.
- CThe Ruwenzori Mountains are depositional landforms accumulated by upper-course river action, whereas Mount Kilimanjaro was shaped predominantly by wind erosion and mass wasting.
- DThe Ruwenzori Mountains represent a series of eroded volcanic plugs, whereas Mount Kilimanjaro and Mount Kenya formed through compressional faulting and crustal warping.
Answer
The Ruwenzori Mountains were formed by tectonic uplift of a basement block (horst) between parallel faults, whereas Mount Kilimanjaro and Mount Kenya were built up by volcanic eruptions along the rift zone.
The correct answer accurately contrasts the tectonic origins of landforms in East Africa. The Ruwenzori Range is an exceptional block mountain (horst) formed by the upward displacement of crystalline basement rock between parallel faults within the East African Rift system. In contrast, nearby peaks like Mount Kilimanjaro and Mount Kenya were created through intense volcanic activity, where repeated lava flows and pyroclastic materials accumulated around eruptive vents along the rift fractures.
Step-by-Step Solution
Key Concept
Horst (Block Mountain) vs Volcanic Landform Origins in the East African Rift System
Estimated Time:2m 0s