glacial recession in Africa: glacial recession on Kilimanjaro
Glacial recession on Kilimanjaro
At one stage most of the summit of Kilimanjaro was covered by an ice cap,
probably more than 100 metres deep. Glaciers extended well down the mountain
forming moraine ridges, clearly visible now on the southern flanks down to
about 4000m. At present only a small fraction of the glacial cover remains.
glacial recession 1984
2011Glacial recession is clearly visible in the three pictures of the southern
icefields that were taken from near the Barranco Hut, the first in 1984, the
second in 1998 and the last in 2011. The most evident changes have occurred on
the Heim Glacier. In 1984 this is seen to have a "dog leg" in it; it reached
down lower than any of the other glaciers in this, the central part of main
southern icefields. In 1998 it is seen its upper reaches to have a much bigger
gap separating it from its neighbouring glacier to the right. The bottom
section, below the original dogleg, is totally missing and represents a loss of
ice extending about 300m vertically. Changes from 1998 to 2011 are less
evident but recession clearly continues.
The remnants of the ice cap can be seen as the spectacular ice cliffs of the
Northern and Eastern Icefields, and the longest glaciers are found on the
precipitous southern and south-western flanks. If the present rate of glacial
recession continues the majority of the glaciers on Kilimanjaro could vanish
altogether in the next 50 years.
A recent study carried out on the snows of Xixibangma and Kilimanjaro has
reinforced observations. It is now estimated that Kilimanjaro has lost 75% of
its ice cover (by mass) since 1912.
See also Glacial recession in the Rwenzori.
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© Andrew Wielochowski 10/06/98. From the "Kilimanjaro Map and Guide"