Mount Kilimanjaro - Mount Kiliminjaro

Mount Kilimanjaro /ËŒkɪlɪmÉ™nˈdÊ'É'ːroÊŠ/, with its three volcanic cones, "Kibo", "Mawenzi", and "Shira", is a dormant volcanic mountain in Tanzania. It is the highest mountain in Africa, and rises approximately 4,877 metres (16,001 ft) from its base to 5,895 metres (19,341 ft) above sea level. The first recorded ascent to the summit of the mountain was by Hans Meyer and Ludwig Purtscheller in 1889. The mountain is part of the Kilimanjaro National Park and is a major climbing destination. The mountain has been the subject of many scientific studies because of its shrinking glaciers.

Geology and physical features

Kilimanjaro rises approximately 4,877 metres (16,001 ft) from its southern base in the plains near the municipality of Moshi to its summit height of 5,895 metres (19,341 ft). Kilimanjaro is the highest volcano outside South America.

Kilimanjaro is a large stratovolcano and is composed of three distinct volcanic cones: Kibo, the highest; Mawenzi at 5,149 metres (16,893 ft); and Shira, the shortest at 4,005 metres (13,140 ft). Mawenzi and Shira are extinct, while Kibo is dormant and could erupt again.

Uhuru Peak is the highest summit on Kibo's crater rim. The Tanzania National Parks Authority, a governmental agency, and the United Nations Educational, Scientific and Cultural Organization list the height of Uhuru Peak as 5,895 m (19,341 ft). That height is based on a British Ordnance Survey in 1952. Since then, the height has been measured as 5,892 metres (19,331 ft) in 1999, 5,891 metres (19,327 ft) in 2008, and 5,888 metres (19,318 ft) in 2014.

The interior of the volcanic edifice is poorly known, given the lack of large scale erosion that could have exposed the interiors of the volcano.

Eruptive activity at the Shira centre commenced about 2.5 million years ago, with the last important phase occurring about 1.9 million years ago, just before the northern part of the edifice collapsed. Shira is topped by a broad plateau at 3,800 metres (12,500 ft), which may be a filled caldera. The remnant caldera rim has been degraded deeply by erosion. Before the caldera formed and erosion began, Shira might have been between 16,000 feet (4,900 m) and 17,000 feet (5,200 m) high. It is mostly composed of basic lavas with some pyroclastics. The formation of the caldera was accompanied by lava emanating from ring fractures, but there was no large scale explosive activity. Two cones formed subsequently, the phonolitic one at the northwest end of the ridge and the doleritic "Platzkegel" in the caldera centre.

Both Mawenzi and Kibo began erupting about 1 million years ago. They are separared by the "Saddle Plateau" at 4,400 metres (14,400 ft) elevation.

The youngest dated rocks at Mawenzi are about 448,000 years old. Mawenzi forms a horseshoe shaped ridge with pinnacles and ridges opening to the northeast which has a tower like shape resulting from deep erosion and a mafic dyke swarm. Several large cirques cut into the ring, the largest of these sits on top of the Great Barranco gorge. Also notable are the Ost and West Barrancos on the northeastern side of the mountain. Most of the eastern side of the mountain has been removed by erosion. Mawenzi has a subsidiary peak named Neumann Tower (4,425 metres (14,518 ft)).

Kibo is the largest cone and is more than 15 miles (24 km) wide at the "Saddle Plateau" altitude. The last activity here has been dated to between 150,000 and 200,000 years ago and created the current Kibo summit crater. Kibo still has gas-emitting fumaroles in the crater. Kibo is capped by an almost symmetrical cone with escarpments rising 180 metres (590 ft) to 200 metres (660 ft) on the south side. These escarpments define a 2.5-kilometre-wide (1.6 mi) caldera caused by the collapse of the summit. Within this caldera is the Inner Cone and within the crater of the Inner Cone is the Reusch Crater, which the Tanganyika government in 1954 named after Gustav Otto Richard Reusch upon his climbing the mountain for the 25th time (out of 65 attempts during his lifetime). The Ash Pit, 350 metres (1,150 ft) deep, lies within the Reusch Crater. About 100,000 years ago, part of Kibo's crater rim collapsed, creating the area known as the Western Breach and the Great Barranco.

An almost continuous layer of lavas buries most older geological features, with the exception of exposed strata within the Great West Notch and the Kibo Barranco. The former exposes intrusions of syenite. Kibo has five main lava formations:

1. phono-tephrites and tephri-phonolites of the "Lava Tower group", on a dyke cropping out at 4,600 metres (15,100 ft), 482,000 years ago
2. Tephri-phonolite to phonolite lavas "characterized by rhomb mega-phenocrysts of sodic feldspars" of the "Rhomb Porphyry group", 460,000â€"360,000 years ago
3. aphyric phonolite lavas, "commonly underlain by basal obsidian horizons", of the "Lent group", 359,000â€"337,000 years ago
4. porphyritic tephri-phonolite to phonolite lavas of the "Caldera rim group", 274,000â€"170,000 years ago
5. phonolite lava flows with aegirine phenocrysts, of the "Inner Crater group", which represents the last volcanic activity on Kibo

Kibo has more than 250 parasitic cones on its northwest and southeast flanks that were formed between 150,000 and 200,000 years ago and erupted picrobasalts, trachybasalts, ankaramites, and basanites. They reach as far as Lake Chala and Taveta in the southeast and the Lengurumani Plain in the northwest. Most of these cones are well preserved, with the exception of the Saddle Plateau cones that were heavily affected by glacial action. Despite their mostly small size, lava from the cones has obscured large portions of the mountain. The Saddle Plateau cones are mostly cinder cones with terminal effusion of lava, while the Upper Rombo Zone cones mostly generated lava flows. All Saddle Plateau cones predate the last glaciation.

According to reports from the Maasai, Lake Chala on Kibo's eastern flank was the site of a village that was destroyed by an eruption.

The mountain is drained by a network of rivers and streams, especially on the wetter and more heavily eroded southern side and especially above 1,200 metres (3,900 ft). Below that altitude, increased evaporation and human water usage reduces the waterflows. The Lumi and Pangani rivers drain Kilimanjaro on the eastern and southern sides, respectively.

Kilimanjaro To the Roof of Africa HD

Name

The origin of the name "Kilimanjaro" is not precisely known, but a number of theories exist. European explorers had adopted the name by 1860 and reported that "Kilimanjaro" was the mountain's Kiswahili name. The 1907 edition of The Nuttall Encyclopædia also records the name of the mountain as "Kilima-Njaro".

Johann Ludwig Krapf wrote in 1860 that Swahilis along the coast called the mountain "Kilimanjaro". Although he did not support his claim, he claimed that "Kilimanjaro" meant either "mountain of greatness" or "mountain of caravans". Under the latter meaning, "Kilima" meant "mountain" and "Jaro" possibly meant "caravans".

Jim Thompson claimed in 1885, although he also did not support his claim, that the term Kilima-Njaro "has generally been understood to mean" the Mountain (Kilima) of Greatness (Njaro). "Though not improbably it may mean" the "White" mountain.

"Njaro" is an ancient Kiswahili word for "shining". Similarly, Krapf wrote that a chief of the Wakamba people, whom he visited in 1849, "had been to Jagga and had seen the Kima jaJeu, mountain of whiteness, the name given by the Wakamba to Kilimanjaro...." More correctly in the Kikamba language, this would be Kiima Kyeu, and this possible derivation has been popular with several investigators.

Others have assumed that "Kilima" is Kiswahili for "mountain". The problem with this assumption is that "Kilima" actually means "hill" and is, therefore, the diminutive of "Mlima", the proper Kiswahili word for mountain. However, "[i]t is ... possible ... that an early European visitor, whose knowledge of [Kiswahili] was not extensive, changed mlima to kilima by analogy with the two Wachagga names; Kibo and Kimawenzi."

A different approach is to assume that the "Kileman" part of Kilimanjaro comes from the Kichagga "kileme", which means "which defeats", or "kilelema", which means "which has become difficult or impossible". The "Jaro" part would "then be derived from njaare, a bird, or, according to other informants, a leopard, or, possibly from jyaro a caravan." Considering that the name Kilimanjaro has never been current among the Wachagga people, it is possible that the name was derived from Wachagga saying that the mountain was unclimbable, "kilemanjaare" or "kilemajyaro" and porters misinterpreted this as being the name of the mountain.

In the 1880s, the mountain became a part of German East Africa and was called "Kilima-Ndscharo" in German following the Kiswahili name components.

On 6 October 1889, Hans Meyer reached the highest summit on the crater ridge of Kibo. He named it "Kaiser-Wilhelm-Spitze" ("Kaiser Wilhelm peak"). That name apparently was used until Tanzania was formed in 1964, when the summit was renamed "Uhuru", meaning "Freedom Peak" in Kiswahili.

History

First sightings by non-indigenous explorers

The mountain may have been known to non-Africans since antiquity. Sailors' reports recorded by Ptolemy mention a "Moon Mountain" and a spring lake of the Nile, which may indicate Kilimanjaro, although available historical information does not allow differentiation among Mount Kenya, the mountains of Ethiopia, the Virunga Mountains, Kilimanjaro, and the Rwenzori Mountains. Before Ptolemy, Aeschylus and Herodotus referred to "Egypt nurtured by the snows" and a spring between two mountains, respectively. One of these mentions two tall mountains in the coastal regions with a valley with traces of fire in between. Martín Fernández de Enciso, a Spanish traveller to Mombasa who obtained information about the interior from native caravans, said in his Summa de Geografía (1519) that west of Mombasa "stands the Ethiopian Mount Olympus, which is exceedingly high, and beyond it are the Mountains of the Moon, in which are the soures of the Nile".

The German missionaries Johannes Rebmann of Mombasa and Krapf were the first Europeans to try to reach the snowy mountain. According to English geographer Halford Mackinder and English explorer Harry Johnston, Rebmann in 1848 was the first European to report the existence of Kilimanjaro. Hans Meyer has claimed that Rebmann first arrived in Africa in 1846 and has quoted Rebmann's diary entry of 11 May 1848 as saying, "This morning, at 10 o'clock, we obtained a clearer view of the mountains of Jagga, the summit of one of which was covered by what looked like a beautiful white cloud. When I inquired as to the dazzling whiteness, the guide merely called it 'cold' and at once I knew it could be neither more nor less than snow.... Immediately I understood how to interpret the marvelous tales Dr. Krapf and I had heard at the coast, of a vast mountain of gold and silver in the far interior, the approach to which was guarded by evil spirits." In light of these sources, J. Shearson Hyland's assertion that Rebmann first saw the mountain in 1840 appears to be erroneous.

Climbing history

Nineteenth century explorers

In August 1861, the Prussian officer Baron Karl Klaus von der Decken accompanied by English geologist R. Thornton made a first attempt to climb Kibo but "got no farther than 8,200 feet (2,500 m) owing to the inclemency of the weather." In December 1862, von der Decken tried a second time together with Otto Kersten. They reached a height of 14,000 feet (4,300 m).

In August 1871, missionary Charles New became the "first European to reach the equatorial snows" on Kilimanjaro at an elevation of slightly more than 13,000 feet (4,000 m).

In June 1887, the Hungarian Count Sámuel Teleki and Austrian Lieutenant Ludwig von Höhnel made an attempt to climb the mountain. Approaching from the saddle between Mawenzi and Kibo, Höhnel stopped at 4,950 meters (16,240 ft), but Teleki pushed through until he reached the snow at 5,300 meters (17,400 ft).

Later in 1887 during his first attempt to climb Kilimanjaro, the German geology professor Hans Meyer reached the lower edge of the ice cap on Kibo, where he was forced to turn back because he lacked the equipment needed to handle the ice. The following year, Meyer planned another attempt with Oscar Baumann, a cartographer, but the mission was aborted after the pair were held hostage and ransomed during the Abushiri Revolt.

In the autumn of 1888, the American naturalist Dr. Abbott and the German explorer Otto Ehrenfried Ehlers approached the summit from the northwest. While Abbott turned back earlier, Ehlers at first claimed to have reached the summit rim but, after severe criticism of that claim, later withdrew it.

In 1889, Meyer returned to Kilimanjaro with the Austrian mountaineer Ludwig Purtscheller for a third attempt. The success of this attempt was based on the establishment of several campsites with food supplies so that multiple attempts at the top could be made without having to descend too far. Meyer and Purtscheller pushed to near the crater rim on October 3 but turned around exhausted from hacking footsteps in the icy slope. Three days later, on Purtscheller's fortieth birthday, they reached the highest summit on the southern rim of the crater. They were the first to confirm that Kibo has a crater. After descending to the saddle between Kibo and Mawenzi, Meyer and Purtscheller attempted to climb the more technically challenging Mawenzi but could reach only the top of Klute Peak, a subsidiary peak, before retreating due to illness. On October 18, they reascended Kibo to enter and study the crater, cresting the rim at Hans Meyers Notch. In total, Meyer and Purtscheller spent 16 days above 15,000 feet (4,600 m) during their expedition. They were accompanied in their high camps by Mwini Amani of Pangani, who cooked and supplied the sites with water and firewood.

The first ascent of the highest summit of Mawenzi was made on 29 July 1912, by the German climbers Edward Oehler and Fritz Klute, who christened it Hans Meyer Peak. Oehler and Klute went on to make the third-ever ascent of Kibo, via the Drygalski Glacier, and descended via the Western Breach.

In 1989, the organizing committee of the 100-year celebration of the first ascent decided to award posthumous certificates to the African porter-guides who had accompanied Meyer and Purtscheller. One person in pictures or documents of the 1889 expedition was thought to match a living inhabitant of Marangu, Yohani Kinyala Lauwo. Lauwo did not know his own age. Nor did he remember Meyer or Purtscheller, but he remembered joining a Kilimanjaro expedition involving a Dutch doctor who lived near the mountain and that he did not get to wear shoes during the climb. Lauwo claimed that he had climbed the mountain three times before the beginning of World War I. The committee concluded that he had been a member of Meyer's team and therefore must have been born around 1871. Lauwo died on 10 May 1996, 107 years after the first ascent, but now is sometimes even suggested as co-first-ascendant of Kilimanjaro.

Fastest ascent and descent

The fastest ascent-descent has been recorded by the Swiss-Ecuadorian mountain guide Karl Egloff (born 16 March 1981 in Quito), who ran to the top and back in 6 hours and 42 minutes on 13 August 2014. Previous records were held by Spanish mountain runner Kílian Jornet (7 hours, 14 minutes on 29 September 2010) and by Tanzanian guide Simon Mtuy (9 hours, 21 minutes on 22 February 2006).

Fastest female ascent and descent

The female ascent record is held by Anne-Marie Flammersfeld. On 27 July 2015, she climbed to the summit in 8 hours, 32 minutes via the Umbwe Route, which is about 30 kilometres (19 mi) long. Born in Germany but living in Switzerland, she broke the record of Britain's Becky Shuttleworth who climbed to the summit in 11 hours, 34 minutes on 20 September 2014.

Flammersfeld then needed 4 hours, 26 minutes to run down to the Mweka Gate, for a combined asent and descent time of 12 hours, 58 minutes. That broke the previous record of 18 hours, 31 minutes held by Debbie Bachman.

Youngest and oldest people to summit

Despite an age-limit of 10 years for a climbing permit, Keats Boyd of Los Angeles was only seven years old when he summited Kilimanjaro on 21 January 2008. The oldest person to reach Uhuru Peak was American Robert Wheeler, who was 85 years and 201 days when he summited on 2 October 2014. In October 2010, Ether Kafer at age 84 became the oldest woman to summit the mountain.

Ascents by people with disabilities

Wheelchair-bound Bernard Goosen scaled Kilimanjaro in six days in 2007, while in 2012 Kyle Maynard, who has no forearms or lower legs, crawled unassisted to the summit of Mount Kilimanjaro.

Trekking Kilimanjaro

Overview

Kilimanjaro National Park generated US $51 million in revenue in 2013, the second-most of any Tanzanian national park. (The Ngorongoro Conservation Area, which includes the heavily visited Ngorongoro Crater, is not a national park.) The fees for park usage and for climbing Kilimanjaro during the 2015/16 budget year are published on the Internet. The Tanzania National Parks Authority reported that the park recorded 57,456 tourists during the 2011-12 budget year, of whom 16,425 hiked the mountain, which was well below the capacity of 28,470 as specified in the park's General Management Plan. The mountain climbers generated irregular and seasonal jobs for about 11,000 guides, porters, and cooks in 2007, although serious concerns have been raised about their poor working conditions and inadequate wages.

There are seven official trekking routes by which to ascend and descend Mount Kilimanjaro: Lemosho, Machame, Marangu, Mweka, Rongai, Shira, and Umbwe. Of all the routes, Machame is considered the most scenic, albeit steeper, route. It can be done in six or seven days. The Rongai is the easiest and least scenic of all camping routes. The Marangu is also relatively easy, but this route tends to be very busy, the ascent and descent routes are the same, and accommodation is in shared huts with all other climbers.

People who wish to trek to the summit of Kilimanjaro are advised to undertake appropriate research and ensure that they are both properly equipped and physically capable. Though the climb is technically not as challenging as when climbing the high peaks of the Himalayas or Andes, the high elevation, low temperature, and occasional high winds make this a difficult and dangerous trek. Acclimatisation is essential, and even the most experienced trekkers suffer some degree of altitude sickness.