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Coordinates: 03°04′33″S 37°21′12″E / 3.07583°S 37.35333°E / -3.07583; 37.35333
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In the 1880s the mountain, called ''Kilmanscharo'' in German, became a part of [[German East Africa]] after [[Karl Peters]] had persuaded local chiefs to sign treaties (a common story that [[Queen Victoria]] gave the mountain to [[Kaiser Wilhelm II]] is not true).<ref>Briggs, Philip (1996): "Guide to Tanzania; 2nd edition." Bradt Guides.</ref> In 1889 Uhuru Peak on Kibo was named ''Kaiser-Wilhelm-Spitze'',<ref name=names/> which was used in the [[German Empire]] until its defeat in 1918, when the territory became British-administered [[Tanganyika]] and the name was discontinued.
In the 1880s the mountain, called ''Kilmanscharo'' in German, became a part of [[German East Africa]] after [[Karl Peters]] had persuaded local chiefs to sign treaties (a common story that [[Queen Victoria]] gave the mountain to [[Kaiser Wilhelm II]] is not true).<ref>Briggs, Philip (1996): "Guide to Tanzania; 2nd edition." Bradt Guides.</ref> In 1889 Uhuru Peak on Kibo was named ''Kaiser-Wilhelm-Spitze'',<ref name=names/> which was used in the [[German Empire]] until its defeat in 1918, when the territory became British-administered [[Tanganyika]] and the name was discontinued.

Version for Rednecks...
Theres a hella lot of 'em ya'll. lol


==Trekking routes up Kilimanjaro==
==Trekking routes up Kilimanjaro==

Revision as of 01:52, 23 January 2009

"Kilimanjaro" redirects here. For other uses, see Kilimanjaro (disambiguation).
Mount Kilimanjaro
Highest point
Elevation5,895 m (19,341 ft) Edit this on Wikidata
Prominence5,885 m (19,308 ft) Edit this on Wikidata
Isolation5,510 km (3,420 mi) Edit this on Wikidata

Kilimanjaro with its three volcanic cones, Kibo, Mawenzi, and Shira, is an inactive stratovolcano in north-eastern Tanzania[2] rising 4,600 m (15,100 ft) from its base, and is additionally the highest peak in Africa at 5,891.8 metres (19,330 ft), providing a dramatic view of the surrounding plains.

Description

File:Mount Kilimanjaro 2007jpg
Mount Kilimanjaro from the air. July 2007.

The highest point on Kilimanjaro is Uhuru Peak, on the volcano Kibo. Its height value attracted a lot of interest as the reports of the first Europeans to see the mountain reached Europe. Since 1889, several attempts have been made to determine the exact height of the mountain, but the several methods have given varying results and differ by as much as 100 metres.[3] The Kilimanjaro 2008 Precise Height Measurement Expedition used GPS and gravimeter methods to output the value of 5,891.8 metres (19,330 ft).[4] On top of Kibo is a 1.5 mile wide crater. As the highest point in Africa, Uhuru Peak is one of the Seven Summits. The summit was first reached by the Marangu army scout Yohanas Kinyala Lauwo, German Hans Meyer and Austrian Ludwig Purtscheller, on October 6, 1889. Two other peaks are also dormant volcanoes: Mawenzi (5,149 m, 16,890 ft), the third highest peak in Africa (after Mount Kenya) and Shira (3,962 m, 13,000 ft). Yohanas' Notch is named after Lauwo.

Due to Kilimanjaro's equatorial location and high elevation, almost every climate type on earth is represented, including a year-round snow-topped summit.

e world with mobile phone service.

Current conditions

Climatic conditions

While the volcano appears to be dormant on the inside, events on top of the mountain draw global attention. The top of the mountain has seen a retreat of the most recent covering of glaciers,[5] with the most recent ice cap volume dropping by more than 80%.[6]

Sources disagree when the glaciers will be gone due to melting. In 2002, a study led by Ohio State University ice core paleoclimatologist Lonnie Thompson predicted that ice on top of Africa's tallest peak would be gone between 2015 and 2020.[7][8][9]. In 2007, a team of Austrian scientists from University of Innsbruck predicted that the plateau ice cap will be gone by 2040, but some ice on the slope will remain longer due to local weather conditions.[10] Yet, another, the California Academy of Sciences, predicts that the [glaciers] will be gone by 2050.[11] A comparison of ice core records suggests conditions today are returning to those of 11,000 years ago. A study by Philip Mote of the University of Washington in the United States and Georg Kaser of the University of Innsbruck in Austria concludes that the shrinking of Kilimanjaro's ice cap is not directly due to rising temperature but rather to decreased precipitation.[12] In May 2008 The Tanzanian Minister for Natural Resources, Ms Shamsa Mwangunga, said that there were indications that snow cover on the mountain was actually increasing.[13] As of January 2006, the Western Breach route has been closed by the Tanzanian government following a rockslide that killed four people at Arrow Glacier Camp.

Mount Kilimanjaro - with Landsat Overlay. Heights two times exaggerated.

Volcanic conditions

While it is inactive, Kilimanjaro has fumaroles that emit gas in the crater on the main summit of Kibo. Scientists concluded in 2003 that molten magma is just 400 metres (1,310 ft) below the summit crater. Several collapses and landslides have occurred on Kibo in the past, one creating the area known as the Western Breach.

View of Kibo, Mowenzi, Shira and Meru in far background

Mapping

Early good maps of Kilimanjaro were published by the British Government's Directorate of Overseas Surveys (DOS 422 Y742) in 1963. These were based on air photography carried out as early as 1958 by the RAF. These were on a scale of 1:50,000 with contours at 100 ft intervals. These are now unavailable. Tourist mapping was first published by the Ordnance Survey in England in 1989 based on the original DOS mapping (1:100,000, 100ft intervals, DOS 522). This is now no longer available. EWP produced a map with tourist information in 1990 (1:75,000, 100m contour intervals, inset maps of Kibo and Mawenzi on 1:20,000 and 1:30,000 scales respectively and 50m contour interval). This is regularly updated and in its 4th edition. In the last few years numerous other maps have become available of various qualities. [1]

EWP map sample (1:75,000, summit area). [1]

Physical features

Mount Kilimanjaro seen from the air, with Mt. Meru beyond

Mount Kilimanjaro is one of the largest stratovolcanoes in the world. Otherwise known as a composite volcano, it comprises numerous layers of lava, tephra and volcanic ash. Tephra is rhyolitic (an igneous, extrusive rock) in composition, and is formed by air-fall material of an eruption, which suggests the composite volcano was once active. However, at the moment it is dormant. According to experts there have been no eruptions in living memory, which suggests it has been dormant for millions of years.

Mount Kilimanjaro is in the shape of a conical volcano; it is formed by ejecta being thrown up by the volcano vent, which then piles around the vent in the shape of a cone. Due to the fact that Mount Kilimanjaro is made up of tephra, it has a cinder cone. This is because the mountains cone is made up of tephra cinders. They are made up of blobs of congealed lava and particles. When the mountain did erupt millions of years ago, the gas-charged lava would be blown violently into the air, then breaking the smaller fragments which would solidify and fall as cinders. This left Mount Kilimanjaro with a bowl-shaped crater. In geologic history, it would not be uncommon for a stratovolcano such as Mount Kilimanjaro to have experienced explosive eruptions. The lava from the mountain is viscous (viscosity is a measure of the thickness of a fluid which is deformed by shear stress or extensional stress) which cools down before it spreads very far. The lava's viscosity helps explain why Mount Kilimanjaro has relatively small crater formations. The rock on the mountain is felsic and has high levels of silica, especially tephratic silicate. This silica is also in alternating sectors, with lava flows and ejecta in different formations. This is called stratum, which is usually formed by natural forces i.e. volcanic eruptions from Mount Kilimanjaro.

Relief of Kilimanjaro

The volcano is the highest in Africa and covers an area of 388,500ha. Although the volcano stands alone, it is a part of an east-west belt of volcanoes stretching over Northern Tanzania. It has three main concentric cones to the southeast in the mountain, but also has smaller parasitic cones. Also known as a satellite cone, the main vent is blocked by cooled solidified lava, and the lava is then forced out through the sides of a volcano under immense pressure. To the west side of the mountain is the peak Shira (3,962m), of which only the southern and western rims remain.

In addition to the west there is also a flat tableland. On the edges of this material is later material made by the former eruptions of the mountain, and so it’s a dissected plateau. This is a plateau which has been uplifted by volcanic activity, then been severely eroded, which explains the material around the edge of the plateau. The peak of Mawenzi (5,149m) - which is rugged and erosion-shattered- can be found in the east of the volcano. Its western face has many features: crags, pinnacles and dyke swarms. Crags are a steeped mass of rock projecting upward or outward. Pinnacles are high peaks or points of rock, but in Mount Kilimanjaros case then it’s a high point of rock. A dike (plural dyke swarm) is a type of sheet intrusion that cuts discordantly across. These come in several forms: planar wall rock structures or massive rock formations. On Mawenzi these are formed in igneous intrusions. These form in high aspect ratios, so the thickness is smaller than the other 2 dimensions. The dykes intrude into a cross-cutting fissure. These are linear volcanic vents through which lava erupts, although Mount Kilimanjaro is dormant so it does not happen.

To the eastern side of Mawenzi it falls into cliffs, with a complex system of gullies and rock faces. These rises from two massive gorges: the Great Barranco and Lesser Barranco. Gorges are deep valleys between cliffs that are formed by erosion, and were formed from the plateau that can be found to the eastern side of the mountain. The cliffs form because harder rock strata that are resistant to erosion/weathering remain exposed on the valley walls. The most recent summit is Kibo (5,891.8 m) which was last active during the Pleistocene. There are still even fumaroles. Even though there haven’t been eruptions for millions of years, there are openings near Kobe in the Earth’s crust which emits steam and gases e.g. Carbon Dioxide, Hydrochloric Acid. It even emits solfatara (Sulphurous gases). They occur along the chaotic clusters and long fissures. The hot igneous rocks react with the groundwater, which makes it release gases.

The highest point on the mountain is the southern rim of the outer crater. Moreover, between Kibo and Mawenzi is the Saddle, in which it contains high altitude tundra. This type of vegetation forms at high levels of altitude because tree growth is hindered by low temperatures and short growing seasons. There is a wide range of vegetation despite being at high altitude such as dwarf shrubs, grasses, mosses and lichens. The ecotone (difference between tundra and forest) is called the timberland. On Mount Kilimanjaro there are radial valleys that can be found on the southern and eastern slopes. They are smaller valleys that flank the mountains main valleys.

Temba Tseri. Temba Tseri was the youngest person to climb Mt Everest.Temba was only fifteen when he achieved this .


Name

It is unknown where the name Kilimanjaro comes from, but a number of theories exist. European explorers had adopted the name by 1860 and reported that it was its Swahili name,[14] that Kilimanjaro breaks Kilima (Swahili for "hill, little mountain") and Njaro,[15] whose supposed origin varies according to the theories—according to some it's an ancient Swahili word for white or for shining,[16] or for the non-Swahili origin, a word from the Kichagga language, the word jaro meaning caravan. The problem with all these is that they can't explain why the diminutive kilima is used instead of the proper word for mountain, mlima. A different approach is to assume that it comes from the Kichagga kilmanare or kileajao meaning "which defeats the bird/leopard/caravan". However this theory can't explain the fact that Kilimanjaro was never used in Kichagga before in Europe in the mid-1800s.[14]

In the 1880s the mountain, called Kilmanscharo in German, became a part of German East Africa after Karl Peters had persuaded local chiefs to sign treaties (a common story that Queen Victoria gave the mountain to Kaiser Wilhelm II is not true).[17] In 1889 Uhuru Peak on Kibo was named Kaiser-Wilhelm-Spitze,[14] which was used in the German Empire until its defeat in 1918, when the territory became British-administered Tanganyika and the name was discontinued.

Trekking routes up Kilimanjaro

Main article: Mount Kilimanjaro climbing routes

There are several routes by which to climb Mt Kilimanjaro, namely, Marangu, Rongai, Lemosho, Shira, Umbwe and Machame. Of all the routes, Machame is by far the most scenic albeit steeper route up the mountain. The Rongai is the easiest camping route and the Marangu is also easy, but accommodation is in huts. As a result, this route tends to be very busy and ascent and descent routes are the same.

Persons wishing to climb Mt Kilimanjaro are advised to undertake appropriate research and ensure that they are both properly equipped and physically capable. Though the climb is technically very easy, the altitude and low temperature make this a difficult and dangerous trek. Acclimatisation is essential, and even then most people suffer some degree of altitude sickness. About 10 climbers die from this each year, together with an unknown number of local porters - figures for these are guessed at between 10-20. Kilimanjaro summit is well above the altitude at which high altitude pulmonary edema (HAPE), or high altitude cerebral edema (HACE) can occur. All climbers will suffer considerable discomfort, typically shortage of breath, hypothermia and headaches, and though most young, fit people can make the Uhuru summit, a substantial number of trekers will abandon the attempt at a lower altitude.

High altitude climbing clubs have criticised the Tanzanian authorities for charging fees for each day spent on the mountain. This can encourage climbers to climb rapidly to save time and money, while proper acclimatisation demands that delays are built in to any high climb.

Tanzanian Medical Services around the mountain have expressed concern recently over the current influx of tourists that apparently perceive Kilimanjaro as an easy climb. Many individuals require significant medical attention during their attempts, and many are forced to abandon the climb. An investigation into the matter concluded that tourists visiting Tanzania were often encouraged to join groups heading up the mountain without being made aware of the significant physical demands the climb makes.

In 1988 the first snowboard descent of Kilimanjaro was accomplished by a Canadian, Ace Bailey. Since then "pleasure devices" have been banned on the mountain. This includes skis, snowboards, parachutes and flying devices.

Unique vegetation

Kilimanjaro has unique vegetation such as the water holding cabbage in the tussock grassland and other plants like this, all adapted to living in alpine conditions. Kilimanjaro has a large variety of forest types over an altitudinal range of 3000 m containing over 1200 vascular plant species. Montane Ocotea forests occur on the wet southern slope. Cassipourea and Juniperus forests grow on the dry northern slope. Subalpine Erica forests at 4100 m represent the highest elevation cloud forests in Africa. In contrast to this enormous biodiversity, the degree of endemism is low. However, forest relicts in the deepest valleys of the cultivated lower areas suggest that a rich forest flora inhabited Mt Kilimanjaro in the past, with restricted-range species otherwise only known from the Eastern Arc mountains. The low degree of endemism on Kilimanjaro may result from destruction of lower altitude forest rather than the relatively young age of the mountain. Another feature of the forests of Kilimanjaro is the absence of a bamboo zone, which occurs on all other tall mountains in East Africa with a similarly high rainfall. Sinarundinaria alpina stands are favoured by elephants and buffaloes. On Kilimanjaro these megaherbivores occur on the northern slopes, where it is too dry for a large bamboo zone to develop. They are excluded from the wet southern slope forests by topography and humans, who have cultivated the foothills for at least 2000 years. This interplay of biotic and abiotic factors could explain not only the lack of a bamboo zone on Kilimanjaro but also offers possible explanations for the patterns of diversity and endemism. Kilimanjaro's forests can therefore serve as a striking example of the large and long-lasting influence of both animals and humans on the African landscape.

See also

References

  1. ^ a b Kilimanjaro Map and tourist Guide (Map) (4th ed.). 1:75,000 with 1:20,000 and 1:30,000 insets. EWP Map Guides. Cartography by EWP. EWP. 1995. ISBN 0-906227-66-6.
  2. ^ The concept of "free-standing rise" is not completely well-defined; however one definition characterizes it as the rise of the summit over the lowest closed contour line encircling and remaining near the summit. (Compare topographic prominence.) Kilimanjaro is encircled by a contour line at elevation 1,395 metres (4,577 ft), giving a rise of 4,500 metres (14,764 ft), which goes no further than 45 kilometres (28 mi) from the summit. This is the world's highest free-standing rise attainable within a 50 kilometres (31 mi) radius. Higher rises are attainable over somewhat larger distances, namely for Pico Cristóbal Colón, which rises 5,000 metres (16,400 ft) above a contour within 75 kilometres (47 mi), and Mount McKinley, which rises 5,300 metres (17,390 ft) above a contour within 120 kilometres (70 mi). (Sources: SRTM data, USGS National Elevation Dataset.) If points below sea level are considered, Mauna Kea beats Mount McKinley by hundreds of meters with a similar radius. (Source: USGS National Elevation Dataset and Geologic Investigations Series I-2809.)
  3. ^ "Kilimanjaro 2008 Precise Height Measurement Expedition" (PDF). African Geodetic Reference Frame Newsletter. UN Economic Commission for Africa. 2009-01-17. Retrieved 2009-01-17.
  4. ^ "Portugueses 'tiraram' 3,2 metros ao Quilimanjaro". Diário de Notícias (in Portuguese). Diário de Notícias. 2009-01-17. Retrieved 2009-01-17.
  5. ^ Recession of Equatorial Glaciers. A Photo Documentation, Hastenrath, S., 2008, Sundog Publishing, Madison, WI, ISBN-13: 978-0-9729033-3-2, 144 pp.
  6. ^ "Melting snows of Kilimanjaro". NASA Goddard Space Flight Center. 2002-12-18. Retrieved 2009-01-17.
  7. ^ Ice Man: Lonnie Thompson Scales the Peaks for Science
  8. ^ "African Ice Core Analysis Reveals Catastrophic Droughts, Shrinking Ice Fields". Research News. Ohio State University. 2002-10-03. Retrieved 2009-01-17.
  9. ^ Ice Core Records
  10. ^ "Kilimanjaro's ice set to linger". BBC News. 2007-04-17. Retrieved 2009-01-17.
  11. ^ Video clip shown at the California Academy of Sciences, title unknown. 8 August 2008
  12. ^ "No more "snows of Kilimanjaro"?". Geotimes. American Geological Institute. 2007. Retrieved 2009-01-17. {{cite web}}: Unknown parameter |month= ignored (help)
  13. ^ "Tanzania: Minister - Ice Won't Vanish On Kili". The Citizen. May 26, 2008. Retrieved 2009-01-17.
  14. ^ a b c Hutchinson, J. A.: The Meaning of Kilimanjaro
  15. ^ "Kilima-Njaro" (alternate name in 1907), The Nuttall Encyclopædia, 1907, FromOldBooks.com, 2006, webpage: FOB-Njaro.
  16. ^ "SRTM TANZANIA IMAGES" (Kilimanjaro or Kilima Njaro description), NASA, August 28, 2005, webpage: NASA-Tanzania.
  17. ^ Briggs, Philip (1996): "Guide to Tanzania; 2nd edition." Bradt Guides.
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