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The Global Volcanism Program has no activity reports for Kilimanjaro.
The Global Volcanism Program has no Weekly Reports available for Kilimanjaro.
Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.
04/2013 (BGVN 38:04) 2006 rockfall takes climbers' lives; 165 my minimum age; glacial retreat; economic value
04/2013 (BGVN 38:04) 2006 rockfall takes climbers' lives; 165 my minimum age; glacial retreat; economic value
We offer our first Bulletin report on Mount Kilimanjaro, which remains a dormant volcano. We first discuss its economic value and setting. We next mention a few of the many studies of seismically detected rockfalls at volcanoes. We next discuss a 4 January 2006 rockfall that took three climbers' lives and injured five others (Kikoti and others, 2006). An investigation looked into the accident's location and cause, improvements to the route to minimize rockfall risk, as well as further recommendations and implementation to make this approach to the summit safer. Although accidents due to rockfalls and mass wasting are common in mountainous areas, volcanoes included, this subject has not typically been a major focus of Bulletin reporting. This unusually well-documented case illustrates several approaches to mitigating similar hazards at more than just this volcano.
The next section of this report notes diminishing glacial ice on Kilimanjaro, 85% gone since 1912. The youngest age date of volcanic material on the volcano is 165,000 +/- 5,000 ybp. No evidence of younger eruptions was found in studies of glacial ice on the volcano (Kimberly Casey, personal communication, June 2013).
There were several reports discussing the rockfall incident and future steps that might make the route safer. The report by Kikoti and others (2006) was issued after inspection of the Arrow Glacier area looking at various alternative routes, challenges, and recommendations and implementation.
World Heritage site and economic importance. Kilimanjaro was designated a World Heritage site in 1987. UNESCO cited Kilimanjaro as "an outstanding example of a superlative natural phenomenon" with many endangered species. Guides are required for tours and costs can range to $5,000 per person for an expedition to the summit (Py-Lieberman, 2008). Income from Kilimanjaro ecotourism is a principal source of foreign exchange for Tanzania. Income from tourism overall has grown from US $65 million in 1990 to US $725 million in 2001, and then represented roughly 10% of Tanzania's gross domestic product (World Bank/MIGA, 2002). It ranks among the world's favorite volcanoes to climb (Sigurdsson and Lopes-Gautier, 2000).
Rockfalls at volcanoes. Rockfalls represent a special kind of mass movement (mass wasting smaller than landslides) in which one or more rocks become dislodged, enters free fall, and bounces down the ground surface. The rockfalls discussed here were unusually well documented (Kikoti and others, 2006), spurring this report on a phenomena so common as to often elude mention. Rockfalls are a source of noise in seismic monitoring, sometimes masking small earthquakes at depth. Rockfall signals are often counted and reported along with various types of seismic events. Rockfall signals contribute to the average absolute amplitude of seismic signals (eg., RSAM measurements) since those measurements incorporate all the various types of seismic events, rockfall signals, and noise (Endo and Murray, 1991; Voight and others, 1998).
Rockfalls have long been thought of as a possible means of detecting larger impending mass movements and for eruption forecasting, although problems such as glaciers, seasonal melting cycles, precipitation, other noise sources, etc. complicate interpretations. Rockfalls may also be triggered by earthquakes. Regarding rockfall seismic signals at Augustine stratovolcano, DeRoin and McNutt (2012) state that "The high rate of rockfalls in 2005 constitutes a new class of precursory signal that needs to be incorporated into long-term monitoring strategies at Augustine and elsewhere." Hibert and others (2011) carried out a detailed study of rockfalls detected seismically at Piton de la Fournaise, a large shield volcano with rockfalls down steep sided caldera walls. Bulletin editors are currently unaware of past or current seismic monitoring at Kilimanjaro, short- or long-term, and if those records exist, whether rockfalls were important. The rockfall case under discussion at Kilimanjaro, release of glacial deposits down a steep slope, is very unlikely to reflect a pre-eruptive event.
Setting and area of fatal rockfalls. Kilimanjaro sits on the East African rift, a N-trending structure spanning from Mozambique at the S to the Afar and Red Sea region at the N, a distance of 3,000-4,000 km. Kilimanjaro resides in a region where the rift has branched into Eastern and Western rift segments, with Kilimanjaro on the Eastern segment (figure 1). That branching can be seen on figure 1 traversing around Lake Victoria (Lake Nyanza).
|Figure 1. (Top) Overview maps showing Eastern Africa, major features of the East African rift (the planet's largest active continental rift), and the location of Kilimanjaro (green dot). (Middle) Annotated satellite image (SRTM) of Kilimanjaro, where colors refer to elevation; this 90 m resolution image shows the main morphologic features. The top map was found online (credit to Google and NASA Tera metrics); the subsequent map and satellite image were taken from Nonnotte and others (2008). (bottom) shows a simplified map labeling key features at Kilimanjaro. Note the volcano's elongate morphology and the summit area (Kibu and crater of the same name) and E of the saddle, the Mawenzi peak. Figure 2 shows two contour maps. The accident's location was at the Western Breach, a spot just W of the summit crater and a low point on the crater's rim (yellow circle on. Figures 3 and 4 show photos of the area where the accident occurred, a spot just below the r-shaped glacier and above Arrow Glacier camp.|
|Figure 2. Two contour maps showing Kilimanjaro. Note the Kibo and Mawenzi highs. Kilimanjaro's summit resides on Kibo's rim at Uhuru Peak (5,895 m elevation). Mawenzi is the peak to the W of Kibo (16,900 foot summit elevation). The Western Breach (Great West breach) lies on Kibo's SW face, the area where the fatal 4 January 2006 rockfall occurred (lower map, yellow ring). That spot on the upper map is approximately under the right digits of the label "19340" (the summit elevation expressed in feet). Note the large glacier and snow fields; the glacier has since receded (see below). Upper map found online without credit to source; lower map taken from Kikoti and others (2006).|
|Figure 3. A photo taken with Arrow Glacier camp in the foreground and a yellow dashed line indicating the climbers' route into Kibu's crater. Note the zone of reddish rocks along the ascent as well as the two-pronged glacier at upper left ("r-shaped glacier"). [More details: Camp is at 03°04.580' S, 037°20.357' E; 4,871 m elevation. Location of point of entry onto Crater: 03°04.396' S, 037°21.105' E; 5,726 m elevation; mean gradient of slope, 38.0°; mean gradient of route, 26.0°; linear distance from Arrow Glacier camp to Crater: 1.39 km; route distance from Arrow Glacier camp to Crater: 1.95 km.] Image and details taken from Kikoti and others (2006).|
|Figure 4. Zooming in on the rockfall accident scene, which occurred slightly below Kilimanjaro's r-shaped glacier (upper left). An annotated image appears below in another figure. Taken from Kikoti and others (2006).|
Causes of the Accident. Extensive talus resides at the intersection between the left and right arms of the r-shaped glacier (figures 5-6). Part of this unstable talus collapsed. Kikoti and others (2006) said that the dislodged material traveled 150 m down the slope, reaching a group of people at an estimated speed of ˜40 m/sec (144 km per hour) at the point where the climbers were struck (B, figure 4).
Kikoti and others (2006) thought the talus dislodged because of (a) melting ice freeing the loose material and destabilizing it on the steep slopes, and (b) strong downhill winds measured at 177 km/h. The wind speed was measured by guide George Lyimo on the morning of the accident, using a wind speed gauge wrist unit.
Lyimo survived, having left camp ˜3 hours before the accident. Based on the known conditions at the summit, the climbers would only have had on the order of 5 seconds to escape the avalanche. Besides the strong winds, the climbers also confronted snowfall and poor visibility.
Kikoti and others (2008) examined a conspicuous cavity where the recent fallen rocks were believed to have been dislodged. They estimated that 39 tons of rocks dislodged from the cavity.
|Figure 5. View from Kilimanjaro's r-shaped glacier looking downward over angular boulders of talus. Source of deadly rockfall indicated (A) as well as the point where climbers were struck (B). The distance from point A to point B was estimated at 150 m. Taken from Kikoti and others (2006).|
|Figure 6. At Kilimanjaro, the scene at the rockfall's source area. Rocks here remained unstable after the accident, an ongoing concern (see Recommendations and implementation). Note person for scale. Taken from Kikoti and others (2006).|
Current Status of Route. The old route (figure 3) was judged unsafe due to concern over two risk zones (A and B, figure 7). Zone A hosts residual glacial deposit at the intersection of the right and left arms of the r-shaped glacier resulting in exposure to rockfall from above. Zone B includes the crater wall and rock tower, which could shed debris from above. Above this area, the remainder of the route is judged to be subject to no specific identifiable imminent threats.
|Figure 7. Annotated photo of the route to Kibu crater. The location of the January 2006 accident delineated with a red "X." Risk zones A and B shown as shaded areas with the likely sources of risk indicated. One part of a proposed alternate route appears as a yellow dotted line. Courtesy of Kikoti and others (2006).|
Recommendations and implementation. Kikoti and others (2006) made principal recommendations, some of which follow. As partly seen on figure 7 (yellow dotted line), the proposed new route traverses the rock feature known as the 'Stone Train' largely avoiding indicated hazardous zones. The route would proceed to a handrail up the left hand edge of the Stone Train to join the rock spur adjoining the base of the crater wall at ˜5,400 m.
Many of these recommendations were adopted and a October 2008 posting on the Mt. Kilimanjaro Travel Guide (Baxter, 2008) discussed implementation, obligations of tour operators, climbers, guides and the Park to make the route safer. These ranged from immediate steps such as asking all climbing parties to depart Arrow Glacier camp no later than 5 a.m. to mid-term steps such as the issuance by tour companies of radio handsets for guides to communicate with Kilimanjaro National Park Authority (KINAPA) rescue teams. As a result, the Park was directed to take immediate steps such as erecting signboards warning visitors of rockfall dangers and put in place a rockfall protocol and ensure that all their rescue staffs are trained on how to effectively use it.
Baxter (2008) recommended investigations by further specialists (seismologists, glaciologists, geologists, meteorologists, etc.) to assess the long term future risks associated with climate change and Kilimanjaro's altering geology and glaciology. A safety patrol team was also tasked with visiting the mountain monthly or bi-monthly to survey and identify possible future risk areas in the light of the rapidly changing situation on Kilimanjaro.
Receding glaciers. Cullen and others (2013) discuss the time series of glacial retreat at Kilimanjaro during 1912 to 2011. They concluded that 85 per cent of the glacier had disappeared. Figures 8 and 9 contain satellite imagery and land-based photos presented on a NASA Earth Observatory article (Allen and others, 2012) that describes the state of summit glaciers at Kilimanjaro on 26 October 2012. Melting ice and subsequent melt-water runoff reduce confining pressure on the magmatic system. There is evidence that such reduced pressure or loading might promote the onset of volcanism (e.g., Bay and others, 2004; Pagli and Sigmundsson, 2008; Sigvaldason and others, 1992).
|Figure 8. (Left) The Advanced Land Imager on NASA's Earth Observing-1 (EO-1 Ali) satellite acquired the top images. Green lowlands are seen to the S, including rainforest leading upslope to alpine desert. The summit area lacks vegetation. Note thick cloud cover to the N. Glacial ice is clearly absent in much of the circular crater. (Right) A portion of the previous image centered over Kilimanjaro's summit emphasizes the lack of ice fields on 26 October 2012. Labels show both northern and southern icefields and a "new rift" discussed in text, where the ice had recently melted. Bulletin editors have added to the original Earth Observatory figure, inserting the location of the r-shaped glacier ("r."). Courtesy of NASA Earth Observatory.|
|Figure 9. Lateral views of the Northern (top) and Southern (bottom) icefields in photos taken on 25 and 27 September 2012, respectively. Tents (barely visible at far left) help define scale for the shot of the Northern icefield. Courtesy of Kimberly Casey.|
According to Allen and others (2012), during a 2012 expedition, scientists found that the northern ice field, which had been developing since the 1970s then had a hole wide enough to ride a bicycle through. They also were able to walk on land directly through the rift (labeled on figure 8, right).
Cullen and others (2013) said that despite Mount Kilimanjaro's location in the tropics, the dry and cold air at the top of the mountain has sustained large quantities of ice for more than 10,000 years. At points, ice has completely surrounded the crater. Studies of ice core samples show that Kilimanjaro's ice has persisted through multiple warm spells, droughts, and periods of abrupt climate change.
Fumarolic activity occurs on the volcano, particularly in Kibu crater. Tour operator Eddie Frank (Tusker Trail) has agreed to keep a log of observed changes of color and smell at fumaroles.
Age dates of eruptive products. Nonnotte and others (2008) discussed the youngest K-Ar age date for Kilimanjaro. Samples associated with the latest parasitic phase (05KI41B and 03TZ42B) yield ages of 165 +/- 5 ka and 195 +/- 5 ka, respectively. "The last volcanicity, around 200-150 ka, is marked by the formation of the present summit crater in Kibo and the development of linear parasitic volcanic belts, constituted by numerous Strombolian-type isolated cones on the NW and SE slopes of Kilimanjaro. These belts are likely to occur above deep-seated fractures that have guided the magma ascent, and the changes in their directions with time might be related to the rotation of recent local stress field," Nonnotte and others wrote (2008).
References: Allen, J, Simmon, R, Voiland, A., and Casey, K, 2012, Kilimanjaro's Shrinking Ice Fields, NASA Earth Observatory-Image of the day (URL: http://earthobservatory.nasa.gov/) Posted 8 November 2012; Accesssed 14 June 2013.
Baxter, P., 2008, TANAPA Western Breach Protocol—Tanzania National Parks, Obligations and Actions Regarding the Re-opening of Western Breach Route (Arrow Glacier), Mt. Kilimanjaro Travel Guide [posted 21 October 2008] (URL: http://www.mtkilimanjarologue.com/tanapa-western-breach-protocol).
Bay, RC, Bramall, N, and P Buford Price, 2004, Bipolar correlation of volcanism with millennial climate change, Proc Natl Acad Sci U S A. 2004 April 27; 101(17): 6341-6345. Published online 2004 April 19. doi: 10.1073/pnas.0400323101 PMCID: PMC404046
Cullen, N. J., Sirguey, P., Mölg, T. Kaser, G. Winkler, M. and Fitzsimons, S. J. , 2013.A century of ice retreat on Kilimanjaro: the mapping reloaded, The Cryosphere Discuss., 6, 4233-4265, doi:10.5194/tcd-6-4233-2012, 2012.
DeRoin N. and S.R. McNutt, 2012, Rockfalls at Augustine Volcano, Alaska: The Influence of Eruption Precursors and Seasonal Factors on Occurrence Patterns 1997-2009. J . Volcanol. Geotherm. Res., v. 211-212, p. 61-75
Endo, E.T. and Murray, T., 1991, Real-time seismic amplitude measurement (RSAM): a volcano monitoring and prediction tool. Bulletin of Volcanology 53.7 (1991): 533-545.
Hibert, C., A. Mangeney, G. Grandjean, and N. M. Shapiro, 2011, Slope instabilities in Dolomieu crater, Réunion Island: From seismic signals to rockfall characteristics, J. Geophys. Res., 116, F04032, doi:10.1029/2011JF002038
Kikoti, I., Nchereri, J.P., Mlay, A., Lyimo, G., Msemo, E., and Rees-Evans, J., 2006, Kilimanjaro Safety Patrol Reconnaissance Expedition, 25th-27th January 2006, An investigation to determine the cause of the Western Breach accident of 4th January 2006 and to offer recommendations for the way forward for this route [Report completed June 2006 and posted online at (URL: http://www.yumpu.com/en/document/view/7812851/western-breach-investigation-digital-copy)
Nonnotte, P, Guilloub, H, Le Guillou, B, Benoit, M, Cotten, J, Scaillet, S, 2008, Jour. of Volc. and Geoth. Res., Volume 173, Issues 1-2, 1 June 2008, pp. 99-112
Pagli, C., and Sigmundsson, F. (2008). Will present day glacier retreat increase volcanic activity? Stress induced by recent glacier retreat and its effect on magmatism at the Vatnajökull ice cap, Iceland. Geophysical Research Letters, 35(9), L09304.
Py-Lieberman, B, 2008, Life lists, Hiking Mount Kilimanjaro, A trek up the world's tallest freestanding mountain takes you through five different ecosystems and offers a stunning 19,340-foot view, Smithsonian magazine, January 2008 [online version, URL: http://www.smithsonianmag.com/specialsections/lifelists/lifelist-kilimanjaro.html]
Sigurdsson S., and Lopes-Gautier, R. 2000, Volcanoes and Tourism; Encyclopedia of Volcanoes, Academic Press, pp. 1283-1299.
Sigvaldason, G.E., Annertz, K., and Nilsson, M., 1992, Effect of glacier loading/deloading on volcanism: postglacial volcanic production rate of the Dyngjufjöll area, central Iceland. Bulletin of Volcanology 54, no. 5 (1992): 385-392.
UNESCO, date uncertain, Kilimanjaro National Park, UNESCO (URL:whc.unesco.org/en/list/403)
Information Contacts: Eddie Frank, Tusker Trail, 924 Incline Way Suite H Incline Village, Nevada 89451-9423 USA (URL: http://www.Tusker.com); and Kimberly Casey, NASA Goddard Space Flight Center, Cryospheric Sciences Lab, Code 615, Greenbelt, MD 20771 USA (URL: http://neptune.gsfc.nasa.gov/csb/personnel/?kcasey).
Massive Kilimanjaro, Africa's highest mountain, consists of three large stratovolcanoes constructed along a NW-SE trend. The ice-capped, 5895-m-high summit towers 5200 m above the surrounding plains. Activity at the older cone of Shira that forms the broad WNW shoulder of Kilimanjaro began during the Pliocene, and the extensively dissected Mawenzi forms a prominent, sharp-topped peak of Pleistocene age on the upper ESE flank dominated by a densely packed radial dike swarm. More than 250 satellitic cones occupy a rift zone to the NW and SE of Kibo, the central stratovolcano. A 2.4 x 3.6 km caldera gives the summit of Kibo an elongated, broad profile. Most of Kilimanjaro was constructed during the Pleistocene, but a group of youthful-looking nested summit craters are of apparent Holocene age, and fumarolic activity continues.
The Global Volcanism Program is not aware of any Holocene eruptions from Kilimanjaro. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Kilimanjaro page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Kilima Dscharo | Kilimandjaro | Oibor, Oldoinyo | White Mountain | Shining Mountain | Kilima Njaro|
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Chala||Cone||3° 19' 0" S||37° 40' 0" E|
|Cone Place||Cone||3840 m||3° 2' 0" S||37° 14' 0" E|
|Himo||Cone||3° 27' 0" S||37° 32' 0" E|
|Kibo||Stratovolcano||5895 m||3° 4' 0" S||37° 22' 0" E|
|Kibongoto||Cone||3° 10' 0" S||37° 8' 0" E|
|Kilema||Cone||3° 20' 0" S||37° 28' 0" E|
|Kileo||Cone||3° 10' 0" S||37° 34' 0" E|
|Kinanga||Cone||3° 20' 0" S||37° 37' 0" E|
|Kwa Mikungu||Cone||3° 16' 0" S||37° 9' 0" E|
|Lagumishera||Cone||2° 51' 0" S||37° 10' 0" E|
|Laso||Cone||3° 18' 0" S||37° 27' 0" E|
|Lemongo||Cone||2° 49' 0" S||37° 25' 0" E|
|Lemrika||Cone||3° 26' 0" S||37° 34' 0" E|
|Lerongo||Cone||3° 8' 0" S||37° 3' 0" E|
|Lotigelli||Cone||2° 58' 0" S||37° 1' 0" E|
|Magadini||Cone||2° 45' 0" S||37° 6' 0" E|
|Mawenzi||Stratovolcano||5149 m||3° 6' 0" S||37° 27' 0" E|
|Mbuyuni||Cone||3° 23' 0" S||37° 25' 0" E|
|Mue||Cone||3° 23' 0" S||37° 29' 0" E|
|Ol Morouk||Cone||3° 15' 0" S||37° 4' 0" E|
|Salaita||Cone||3° 24' 0" S||37° 45' 0" E|
|Shira||Stratovolcano||3962 m||3° 2' 0" S||37° 13' 0" E|
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Reusch Pit||Crater||5760 m||3° 4' 0" S||37° 21' 0" E|
|The enormous Kilimanjaro massif covers most of the area of this Space Shuttle photograph. Concentric vegetation zones highlight the 5200 m vertical relief of the volcano above the surrounding plains. Kilimanjaro consists of three overlapping stratovolcanoes. The snow-capped 5895-m-high summit of the central peak, Kibo, is the highest in Africa and is a popular climbing destination. A small cloudcap drapes the summit of Mawenzi, a deeply eroded satellitic volcano ESE (right) of Kibo.
Photo by National Aeronautical and Space Administration (NASA), 1984.
|Massive Kilimanjaro, Africa's highest mountain, rises to the south above the Amboseli Game Preserve in Kenya to a height of 5895 m. A 2.4 x 3.6 km caldera gives the ice-covered summit of Kibo, the central stratovolcano, an elongated, broad profile. Numerous satellitic cones occupy a rift zone to the NW and SE of Kibo. Most of Kilimanjaro was constructed during the Pleistocene, but a group of youthful-looking nested summit craters are of apparent Holocene age.
Photo by Tom Jorstad, 1990 (Smithsonian Institution).
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.
Downie C, Wilkinson P, 1972. The Geology of Kilimanjaro. England: Univ Sheffield Dept Geol, 253 p.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
Nonnotte P, Guillou H, Le Gall B, Benoit M, Cotten J, Scaillet S, 2008. New K-Ar age determinations of Kilimanjaro volcano in the North Tanzanian diverging rift, East Africa. J Volc Geotherm Res, 173: 99-112.
Nyamweru C K, 1990. . (pers. comm.).
Richard J J, Neumann van Padang M, 1957. Africa and the Red Sea. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI 4: 1-118.