Furtwängler Glacier
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Furtwangler Glacier is located near the
summit A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used only for a m ...
of
Mount Kilimanjaro Mount Kilimanjaro () is a dormant volcano in Tanzania. It has three volcanic cones: Kibo, Mawenzi, and Shira. It is the highest mountain in Africa and the highest free-standing mountain above sea level in the world: above sea level and ab ...
in
Tanzania Tanzania (; ), officially the United Republic of Tanzania ( sw, Jamhuri ya Muungano wa Tanzania), is a country in East Africa within the African Great Lakes region. It borders Uganda to the north; Kenya to the northeast; Comoro Islands and ...
. The glacier is named after who, with Siegfried König, formed the fourth party to ascend to the summit of Kilimanjaro in 1912. The glacier is a small remnant of an
ice cap In glaciology, an ice cap is a mass of ice that covers less than of land area (usually covering a highland area). Larger ice masses covering more than are termed ice sheets. Description Ice caps are not constrained by topographical features ...
that once crowned the summit of Kilimanjaro. Almost 85 percent of the ice cover disappeared from October 1912 to June 2011. In 2013 it was estimated that at the then-current rate, most of the ice would disappear by 2040 and "it is highly unlikely that any ice body will remain after 2060". Furtwängler Glacier is ephemeral, existing continuously only since about 1650 CE, which corresponds with very high levels in Kenya's
Lake Naivasha Lake Naivasha is a freshwater lake in Kenya, outside the town of Naivasha in Nakuru County, which lies north west of Nairobi. It is part of the Great Rift Valley. The name derives from the local Maasai name ''Nai'posha'', meaning "rough wate ...
and the beginning of the Maunder Minimum. Between measurements in 1976 and 2000, the area of this glacier was cut almost in half, from to . By 2018 the size had shrunk to . In 2022 it was thought that the glacier would cease to exist by 2023 at a rate of loss of per year. During fieldwork conducted early in 2006, scientists discovered a large hole near the center of the glacier. This hole, extending through the remaining thickness of the glacier to the underlying rock, split the glacier in two by 2007.


See also

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Retreat of glaciers since 1850 The retreat of glaciers since 1850 affects the availability of fresh water for irrigation and domestic use, mountain recreation, animals and plants that depend on glacier-melt, and, in the longer term, the level of the oceans. Deglaciation occu ...
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List of glaciers A glacier ( ) or () is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly deform ...


References

Glaciers of Tanzania Pangani basin {{Tanzania-glacier-stub