The 'Ruwenzori Range', now officially called 'Rwenzori Mountains' (the spelling having been changed in about 1980 to conform more closely with the local tribal name) is a small but spectacular
mountain range of central
Africa, often referred to as Mt. Rwenzori, located on the border between
Uganda and the
DRC, with heights of up to 5,109 m (16,761 ft) at . The highest Rwenzoris are permanently snow-capped, and they, along with
Mount Kilimanjaro and
Mount Kenya are the only such in Africa. The Ruwenzoris are often identified with the "
Mountains of the Moon" mentioned by
Ptolemy, but the descriptions are too vague to make this definite.
The mountains formed as a result of uplift on the flanks of the Albertine (western) Rift of the East African Rift, the African part of the
Great Rift Valley.
The range is about 120 km (75 mi) long and 65 km (40 mi) wide. It consists of six massifs separated by deep gorges:
Mount Stanley (5,109m),
Mount Speke (4,890m),
Mount Baker (4,843m),
Mount Emin (4,798m),
Mount Gessi (4,715m) and
Mount Luigi di Savoia (4,627m).
[1] Mount Stanley is the largest and has several subsidiary summits, with Margherita Peak being the highest point. The rock is metamorphic, and the mountains are believed to have been tilted and squeezed upwards by plate movement. They are in an extremely humid area, and frequently enveloped in clouds.

Lower Bigo Bog at 3400m in the Rwenzori Mountains with giant lobelia in foreground
The Ruwenzori are known for their
vegetation, ranging from
tropical rainforest through alpine
meadows to snow; and for their
animal population, including
forest elephants, several
primate species and many
endemic birds. One zone is known for its six metre high
heather covered in
moss, another for its giant lobelia. Most of the range is now a World Heritage Site and is covered jointly by The
Rwenzori Mountains National Park in
Uganda and the
Parc National des Virunga in
Congo.
The first European sighting of the Ruwenzori was by the expedition of
Henry Morton Stanley in
1889 (the aforementioned clouds are considered to explain why two decades of previous explorers had not seen them). On
June 7, the expedition's second-in-command and its military commander,
William Grant Stairs, climbed to 10,677 feet, the first non-African ever to climb in the range. The first ascent to the summit was made by the
Duke of the Abruzzi in
1906.
Glacial Recession in Rwenzori
Main articles: Retreat of glaciers since 1850#Tropical glaciers
A subject of concern in recent years has been the impact of
climate change on Rwenzori's
glaciers. In
1906 the Rwenzori had 43 named glaciers distributed over 6 mountains with a total area of 7.5 km²., about half the total glacier area in Africa. By 2005, less than half of these survive, on only 3 mountains, with an area of about 1.5 km². Recent scientific studies such as those by Dr Richard Taylor of
UCL have attributed this to global climate change, and investigated its impact on the mountain's
vegetation and
biodiversity.
References
1. Rwenzori Abruzzi home page
★ ''Glaciers of the Middle East and Africa'', Williams, Richard S., Jr. (editor) In: U. S. Geological Survey Professional Paper, 1991, pp.G1-G70
★ ''Guide to the Ruwenzori'', Osmaston,H.A., Pasteur,D. 1972, Mountain Club of Uganda. 200 p.
★ ''Tropical Glaciers'', Kaser, G., Osmaston, H.A. 2002, Cambridge University Press, UK. 207 p.
★ ''Ruwenzori'', de Filippi, F. 1909. Constable, London. 408 p.
★
Greenpeace article "The Death of the Ice Giants
★
BBC Article "Fabled ice field set to vanish"
★
Dr Taylor's Homepage, with information about the impact of climate change on Rwenzori.
★ Kaser et al. 2004, in ''International Journal of Climatology'' 24: 329–339 (2004)
External links
★
Rwenzori Mountains Historical Climbing and Centenary Celebrations
★
rwenzori.com - Rwenzori Mountains tourist information and tips
★
Account and photos of a climb up the Ruwenzoris (Congo side)
★
30 photos of a climb up the Ruwenzoris (Congo side)
★
The remarkable plants and animals of the Ruwenzoris