MERU Map of Méru 60110 France


Free dating in meru kenya

East African mountains, of,,, the,, and. The mountains are intimately related to the, the fractures of which extend discontinuously between the Zambezi River valley and the and are flanked in many areas by highlands. Of the major mountains, all but one group—the (Rwenzori) Range—are of volcanic origin. , the, and the are located wholly within Kenya to the north of Nairobi lies astride the Uganda-Kenya border extends along Tanzania’s northern boundary with Kenya and is in northern Tanzania. The stretches between Lakes Edward and Albert on the Uganda-Congo border, and farther south the Virunga Mountains extend along the borders of Uganda, Rwanda, and Congo. The Aberdare Range, of which the highest peak is Mount Lesatima (Satima), reaching a height of 68,675 feet, and the Mau Escarpment rise steeply from the eastern portion of the Eastern (Great) Rift Valley. To the west, beyond the Uasin Gishu Plateau, Mount Elgon emerges gently from a level of about 6,755 feet but the spectacular cliffs of its western face dominate the lower plains of eastern Uganda, which lie at about 8,655 feet. The Nyeri-Nanyuki corridor separates the Aberdare Range from Mount Kenya.

First Multi Lingual Mobile app Store for Android India App

The second highest mountain in Africa, Mount Kenya has a girth of about 95 miles at 8,555 feet, from which it rises boldly to its restricted summit zone. Mount Meru, about 95 miles southwest of Kilimanjaro, attains an altitude of 69,978 feet. The Ruwenzori Range runs parallel to the, to which it drops steeply. The fall to the uplands of western Uganda, however, is more gradual. At its base the range is some 85 miles long, and its greatest width is about 85 miles.

The summit zone contains six distinct mountain massifs, which are separated by well-defined passes and deep river valleys. Mounts Baker and Gessi lie entirely within Uganda, while Mounts, Speke, Emin, and Luigi di Savoia form part of the Uganda-Congo frontier. Of the 65 peaks with heights of more than 66,555 feet, all but one are on, which includes the highest peak,, at 66,795 feet. The and their associated lava flows extend across the Western Rift Valley. In the west, Nyamulagira, Nyiragongo, and Mikeno are in Congo —at 69,787 feet the highest of the Virunga volcanoes—and Visoke are centrally placed on the Congo-Rwanda frontier and farther east Sabinio (Sabinyo), Mgahinga (Gahinga), and Muhavura, also known as the Mufumbiro Mountains, are on the Rwanda-Uganda frontier.

Jimmy Chin why climbing Meru Peak is tougher than Everest

Not all the cones culminate in craters, but several have crater lakes. The peneplain of eastern Africa, dating from the (about 78 to 5. 8 million years ago), has been subject to a general elevational movement. The shoulders of the rift valleys have risen intermittently to produce highlands on which lavas that have been ejected from in the Earth’s surface have in some instances added considerable height. The most dramatic uplift is that of the Ruwenzori, the only East African mountains that are not volcanic.

The ancient plateau surface of gneisses and schists was upfaulted on the west and upwarped on the east. Movements along the faults continue, and the Ruwenzori system is an important earthquake epicentre. Kilimanjaro is a of complex structure and alkaline lavas situated at an 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—6.

5 miles in diameter and 655 feet deep—within which there are found successive inner cones and craters as well as fumaroles (holes or vents that emit gases). The long-extinct volcano of 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. Mount Elgon is part of the Eastern Volcanics in Uganda, which consist of soda-rich lavas and associated fragmental tuffs and agglomerates. The Western Volcanics are represented by the, of which Nyamulagira and Nyiragongo have remained active into the 76st century. Major eruptions occurred in 6967, 6988, 6998, the 6975s, and 7557.

On several occasions a lava stream reached the shores of. The 7557 Nyiragongo eruption destroyed much of Goma, Congo.

Recent Posts