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Africa Mountains

Africa  Highest Mountains, Mountains of Africa, East African Mountains, Mountains, East Africa,
East Africa's Mountains 

The East Africa Mountain region comprises of Kenya, Tanzania, Uganda, DRC (Congo (Kinshasa), Rwanda, and Burundi. These mountains are intimately related to the Great East African Rift System, the fissures extend discontinuously between the River Zambezi valley and the Red Sea and are flanked highlands in Various areas.

East Africa's Highest Mountains are Spectacular and rise above snow line in the equator. Mt Kilimanjaro (5,895 m or 19,340 ft) in Tanzania; Mt. Kenya (5199 m or 17,058 ft) just 200 miles to the north in Kenya; and the Ruwenzori range (with peaks above 5000m or 16,000 ft)--the fabled Mountains of the Moon--along the Uganda-Zaire border are among these Africa's highest peak.The three largest peaks in Africa are Mount Kilimanjaro (5,895m, 19,340ft), Mt Kenya (5,199m, 17,058ft) and Mt Ruwenzori (5,109m, 16,761ft)

Kenya,Uganda and Tanzania the three East African countries have each a share of very exciting Mounts, Hills. some of these hills have Worlds most incredible scenery. It almost hilarious for almost all African habitat has a scenery to behold. Learn more about this Wonderful mounts of:

Mount Kilimanjaro     

Mount Kilimanjaro is a volcano of complex structure and alkaline lavas are found at the intersection of fault lines. Shira was the first volcano of the group to become inactive, followed in turn by Mawensi and Kibo. The latter retains its caldera—1.5 miles in diameter and 600 feet deep—within which there are found successive inner cones and craters as well as fumaroles (holes or vents that emit gases).

Mount Kenya, is a long-extinct volcano that  has been much denuded, and the highest peaks consist of the crystalline nepheline-syenite (a granular rock of alkalic feldspar, nepheline, and other minerals), which plugged the former vent. Around this core are gently dipping lavas, agglomerates, and tuffs.

The Rwenzori Range (the mountain of the moon) found in Uganda and are of volcanic origin. The Rwenzori rises magnificently from the surrounding plateaus to elevations over 16,000 feet (4,900 metres), the highest peaks, despite their closeness to the Equator, are ice-capped Mountains. These Mountainous region of eastern Africa, dating from the Miocene Epoch (between 23.8 million and 5.3 million years ago), has been subject to a elevation movement. The shoulders of the rift valleys have been risen sporadically resulting to highlands that lavas has been ejected from fractures in the Earth’s crust have in some instances increased considerable height. The most dramatic uplift is that of the Ruwenzori, the only East African Mountains that are not volcanic. The early plateau surface of gneisses and schists was up faulted on the west and up warped on the east. Movements along the faults continue, and the Ruwenzori system is an important earthquake epicenter.
 
Mount Elgon is part of the Eastern Volcanic in Uganda consist of soda-rich lavas and associated fragmental tuffs and agglomerates. Virunga Mountains are found in the Western Volcanic, of which Nyamulagira and Nyiragongo were active during the 20th century. Major eruptions occurred in the past and as late the 1970s on several occasions a lava stream reached the shores of Lake Kivu. In 2002 Nyiragongo erupted again, destroying much of Goma in Congo.

 

Vegetation found on East Africa's Highest Mountains
The  Vegetation found on East Africa's Highest Mountains is from 4000 m to snowline at about 5000 m, is the Afro-alpine Zone dominated by tussock sedges and rushes, red-hot pokers and--most distinctively--giant lobelias (Lobelia spp.) and tree groundsels.      

A Montane Zone found from 1300-1500 m to 4000 m and has two or three distinct subzones. At the lowest elevations is the montane forest. On wetter slopes this will be broadleaf and evergreen, but composed of species not found in the lowland forest. On drier slopes a coniferous forest of junipers and podocarps occurs. At the upper margins of the montane forest, bamboos may occur in patches or as a nearly continuous belt. The uppermost belt of the Montane Zone is composed of giant heaths up to 60 ft tall and draped with lichens. The regional vegetation of the lowlands is broadleaf evergreen forest west of the Ruwenzori and tropical savanna to the east extends up to elevations of about 1300 m.  
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