Question

The highest mountain peak in Africa is______
a. Kenya
b. Atlas
c. Nyasa
d. Kilimanjaro

Answer 1

Hint:
The highest mountain peak is a dormant volcano of gushing lava in Tanzania. It has three volcanic cones: Kibo, Mawenzi, and Shira. It is the most noteworthy mountain in Africa and the most elevated single unattached mountain on the planet: 5,895 meters (19,341 ft) above ocean level and around 4,900 meters (16,100 ft) over its level base.


Complete solution:
 Kilimanjaro is the fourth most geographically prominent top on Earth. The primary individuals known to have arrived at the highest point were Hans Meyer and Ludwig Purtscheller, in 1889. It is important for Kilimanjaro National Park and is a significant climbing destination. In view of its contracting ice sheets and vanishing ice fields, it has been the subject of numerous logical investigations.

Kilimanjaro is an enormous stratovolcano made out of three particular volcanic cones: Kibo, the most noteworthy; Mawenzi at 5,149 meters (16,893 ft); and Shira, the least at 4,005 meters (13,140 ft). Mawenzi and Shira are wiped out, while Kibo is lethargic and could emit once more.

Uhuru Peak is the most elevated highest point on Kibo's cavity edge. The Tanzania National Parks Authority, a Tanzanian government office, and the United Nations Educational, Scientific, and Cultural Organization record the tallness of Uhuru Peak as 5,895 m (19,341 ft), in view of a British study in 1952.The stature has since been estimated as 5,892 meters (19,331 ft) in 1999, 5,902 meters (19,364 ft) in 2008, and 5,899 meters (19,354 ft) in 2014.


Hence, the correct answer is option D.

Note:
The geography of the inside of the volcanic building is inadequately known, given the absence of huge scope disintegration that might have uncovered the inside of the spring of gushing lava.

Eruptive movement at the Shira focus initiated about 2.5 million years back, with the last significant stage happening about 1.9 million years prior, not long before the northern piece of the building collapsed.[11] Shira is topped by a wide level at 3,800 meters (12,500 ft), which might be a filled caldera. The remainder of the caldera edge has been corrupted profoundly by disintegration. Before the caldera shaped and disintegrated, Shira may have been between 4,900 m (16,000 ft) and 5,200 m (17,000 ft) high. It is generally made out of fundamental magmas, with some pyroclastics. The development of the caldera was joined by magma radiating from ring cracks, however, there was no enormous scope of unstable action. Two cones shaped in this way, the phonolitic one at the northwest finish of the edge and the doleritic Platzkegel in the caldera place.