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23-824: The Itombwe mountains are a section of the Albertine Rift Mountains , which border the western branch of the East African Rift . These mountains extend from the Rwenzori Mountains in the north to the Marungu highlands in the south. They are made up of uplifted Pre-Cambrian basement rocks overlaid in places by recent volcanic activity. Both of these are caused by the forces that created the Great Rift Valley, where tectonic stresses are causing parts of East Africa to separate from

46-470: A canopy reaching 25 metres (82 ft) blending into lowland forest. The mountains are home to endangered Eastern lowland gorillas , chimpanzees and African bush elephants . Rudolf Grauer spent three months in the mountains in 1908, collecting twelve gorillas for the Vienna Museum. A survey in 1996 estimated that there were at least 860 gorillas in the massif. The Grauer population of gorillas in

69-587: A high conservation priority at a World Wide Fund for Nature (WWF) conference held in Libreville, Gabon in 2000 since they are a globally important biodiversity region for birds, mammals and reptiles. At first it was expected that they would be covered by a conservation program for the Albertine Rift. By 2006 it had been accepted that they should be included in a program specifically for the DRC. In late 2006

92-490: Is a relatively cool, dry season with little rain between June and August. The Itombwe Forest of the southern Rift covers a huge area that has had little attention from botanists. Montane forest covers around 650,000 hectares (1,600,000 acres) above 1,500 metres (4,900 ft), the largest block of such forest in the region. The forest is patchy on the east slopes. On the west there is an exceptional progression of bamboo, montane forest, grassland, and then more montane forest with

115-907: Is a tributary of the Lualaba River in the Democratic Republic of the Congo . It rises in Mwenga Territory of Sud-Kivu Province and flows west through Shabunda Territory and then Pangi Territory in Maniema Province , entering the Lualaba just downstream of Kindu . In the upper reaches there are rolling grasslands to the south of the river, but the Itombwe Mountains to the north are rugged, covered by rainforest except where rock bluffs emerge from

138-412: Is near the north-west edge of the montane forest. The range is still not protected, although there have been proposals to designate all the montane forest and two patches of lowland forest to the south of the upper Elila River as conservation areas. As of 2010 the mountains were inaccessible to tourists. In some areas they have low human populations and the environment is relatively undisturbed. However,

161-573: Is now the lake, may have had no outlet other than evaporation. The Lukuga has formed relatively recently, providing a route through which aquatic species of the Congo Basin could colonize Lake Tanganyika, which formerly had distinct fauna. From north to south the mountains include the Lendu Plateau , Rwenzori Mountains , Virunga Mountains and Itombwe Mountains . The Ruwenzori mountains have been identified with Ptolemy 's "Mountains of

184-777: The Congo Basin to the west and south. Lake Rutenzige is fed by several large rivers, the Rutshuru River being one, and drains to the north through the Semliki River into Lake Albert. The Victoria Nile flows from Lake Victoria into the northern end of Lake Albert and exits as the White Nile from a point slightly to the west, flowing north to the Mediterranean. South of the Virungu, Lake Kivu drains to

207-559: The Democratic Republic of the Congo (DRC), Rwanda , Burundi and Tanzania . It extends from the northern end of Lake Albert to the southern end of Lake Tanganyika . The geographical term includes the valley and the surrounding mountains. The Albertine Rift and the mountains are the result of tectonic movements that are gradually splitting the Somali Plate away from the rest of the African continent. The mountains surrounding

230-656: The Institut Congolais pour la Conservation de la Nature (ICCN), helped by the (WWF), had managed to obtain a declaration from the DRC Ministry of Environment that created the Itombwe Nature Reserve . The declaration did not define the completely protected core zone, mixed-use zones and development zones but left settlement of the zone boundaries to a later process involving consultation with the local communities. A book published in 2011 said

253-454: The 37 species of bird endemic to the highlands. They include the most important site in the region for montane forest birds, with 565 species identified. Of these, 31 are endemic to the Albertine Rift and three have only been found here. The northern Itombwe region is inhabited by Banyamulenge , Bafuliiru , Babembe , Banyindu and Bashi people, with population densities in 1998 of over 100 people per square kilometer. Population densities on

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276-499: The Itombwe Massif was undergoing severe destruction. Law and order had broken down. People were moving in to grow crops or to mine for gold, diamonds and columbo-tantalite, which is used in semiconductors and computer chips. Albertine Rift Mountains 9°S 34°E  /  9°S 34°E  / -9; 34 The Albertine Rift is the western branch of the East African Rift , covering parts of Uganda ,

299-754: The Itombwe mountains and the region to the north and west is one of three gorilla populations in East Africa, the others being the Bwindi and Virunga populations. The survey recorded fifty-six species of mammals. A type of shrew that has only been collected once is most likely the oldest of all shrew species in Africa. The Itombwe Mountains are much the most important part of the Albertine Rift Highlands for bird conservation, being home to 32 of

322-513: The Moon". The range covers an area 120 km (75 mi) long by 65 km (40 mi) wide. This range includes Mount Stanley 5,119 m (16,795 ft), Mount Speke 4,890 m (16,040 ft) and Mount Baker 4,843 m (15,889 ft). The Virunga Massif along the border between Rwanda and the DRC consists of eight volcanoes. Two of these, Nyamuragira and Nyiragongo , are still highly active. Isolated mountain blocks further to

345-498: The conflict of the Second Congo War (1998-2003) and subsequent instability many displaced people have entered the region. The region has been the scene of struggles between different armed groups, causing severe humanitarian and environmental problems. NGOs have been attempting to help local communities recover and develop sustainable agricultural and practices while conserving the forest. The major mining center of Kamituga

368-637: The continent. The highest peak of the Albertine Rift Mountains is further north in the Rwenzori Mountains, at 5,100 metres (16,700 ft). The highest peak in the Itombwe range is Mount Mohi , at 3,475 metres (11,401 ft). Several other peaks are higher than 3,000 metres (9,800 ft). The mountains drop sharply in the east to the Ruzizi plain bordering Lake Tanganyika . They form a plateau that slopes down more gently to

391-424: The population around the forest is growing, the forest around the villages is being cleared for agriculture and firewood, and the grasslands at higher levels are used to graze cattle. Mining and hunting are other causes of stress to the environment. Perhaps the main concern of conservationists is that the forests, which are the largest and least fragmented in the region, may be logged. The Itombwe mountains were given

414-546: The rift are composed of uplifted Pre-Cambrian basement rocks , overlaid in parts by recent volcanic rocks . The northern part of the rift is crossed by two large mountain ranges, the Rwenzori Mountains between Lake Albert and Lake Rutanzige (formerly Lake Edward) and the Virunga Mountains between Lake Rutanzige and Lake Kivu . The Virungas form a barrier between the Nile Basin to the north and east and

437-487: The slopes from around 1,600 m (5,200 ft) to 3,500 m (11,500 ft). Above 2,400 m (7,900 ft) there are areas of bamboo and elfin forest. Heather and grasses predominate above 3,500 m (11,500 ft). The ecology is threatened by deforestation as a growing population seeks new farmland. Illegal timber extraction is another problem, and artisanal gold mining causes some local damage. Elila River The Elila River ( Swahili : Mto Elila )

460-701: The south include Mount Bururi in southern Burundi, the Kungwe-Mahale Mountains in western Tanzania, and Mount Kabobo and the Marungu Mountains in the DRC on the shores of Lake Tanganyika . Most of the massifs rise to between 2,000 m (6,600 ft) and 3,500 m (11,500 ft). The Albertine Rift montane forests are important eco-regions. Transitional forests, intermediate between lowland and montane forest, are found at elevations from around 1,000 m (3,300 ft) to 1,750 m (5,740 ft). Montane forest covers

483-688: The south into Lake Tanganyika through the Ruzizi River . Lake Tanganyika then drains into the Congo River via the Lukuga River . It seems likely that the present hydrological system was established quite recently when the Virunga volcanoes erupted and blocked the northward flow of water from Lake Kivu into Lake Edward , causing it instead to discharge southward into Lake Tanganyika. Before that Lake Tanganyika, or separate sub-basins in what

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506-410: The west. The Elila River rises in the mountains, which are covered by forest except where rock bluffs emerge from the steepest slopes. Temperatures range from about 50 °F (10 °C) to 70 °F (21 °C), with a mean temperature of about 60 °F (16 °C) all year round. Frost is occasionally experienced at night. Average annual precipitation is around 65 inches (1,700 mm). There

529-474: The western slope and the high plateau of Itombwe are lower at between 10 and 20 people per square kilometer. The related Balega and Babembe people live in this area. Banyamulenge (ethnic Tutsi ), who migrated from present-day Rwanda, Burundi, and Tanzania have moved into the territory starting in the 19th century. The Bavira people live in the Ruzizi Plain and on the shore of Lake Tanganyika. With

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