Kilimanjaro Glaciers

At first sight, Kilimanjaro’s glaciers look like nothing more than big smooth piles of slightly monotonous ice. On second sight they pretty much look like this too. Yet there’s much more to Kili’s glaciers than meets the eye. For these cathedrals of gleaming blue-white ice are dynamic repositories of climatic history. And they could also be providing us with a portent for impending natural disaster.

Guide walking on the Kibo crater floor past Furtwangler Glacier

Furtwangler Glacier, in Kilimanjaro’s Kibo Crater

You would think that with the intensely strong equatorial sun, glaciers wouldn’t exist at all on Kilimanjaro. In fact, it is the brilliant white colour of the ice that allows it to survive. Because the ice actually reflects most of the heat.

The dull black lava rock on which the glacier rests, on the other hand, does absorb the heat. So while the glacier’s surface is unaffected by the sun’s rays, the heat generated by the sun-baked rocks underneath leads to glacial melting.

As a result, the glaciers on Kilimanjaro are inherently unstable. The ice at the bottom of the glacier touching the rocks melts, and the glaciers lose their ‘grip’.  As a consequence, ‘overhangs’ occur where the ice at the base has melted, leaving just the ice at the top. As the process continues the ice fractures and breaks away. This exposes more of the rock to the sun… and so the process begins again.

The sun’s effect on the glaciers is also responsible for the spectacular structures such as the ice columns and pillars, towers and cathedrals. These features are perhaps the most fascinating part of the upper slopes of Kibo.

Close-up of the northern side of Kilimanjaro

Kilimanjaro’s Rebmann Glacier – part of the fast-disappearing Southern Icefields

Why haven’t Kilimanjaro’s glaciers melted away?

One would have thought that, after 11,700 years of this melting process, very little ice would remain on Kilimanjaro. (Why 11,700 years? Well, according to recent research, the current glaciers began to form in 9700BC.) The fact that there are still glaciers is due to the prolonged ‘cold snaps’, or ice ages, that have occurred down the centuries. These, of course, allow the glaciers to regroup and reappear on the mountain.

Kilimanjaro's Southern Icefield as seen from Uhuru Peak at dawn, with a beautiful pinky-orange sky and Mount Meru breaking through the clouds in the distance

The Southern Icefield at sunrise, with Mount Meru in the distance

According to estimates, there have been at least eight of these ice ages. The last was a rather minor one in the fifteenth and sixteenth centuries. It was a time when the Thames frequently froze over and winters were severe. At these times the ice on Kilimanjaro would in places have reached right down to the tree line. Both Mawenzi and Kibo would have been covered at this time.

At the other extreme, before 9700BC there have been periods when Kilimanjaro was completely free of ice, perhaps for up to twenty thousand years.

How is global warming affecting them?

Of course as our planet heats up there are bound to be consequences for the glaciers on Kilimanjaro. It’s a topic we cover in our Climate Change and Kilimanjaro page. But nobody can be 100% sure what will really happen to the glaciers. But every so often we have another prediction from experts bringing either good or ghastly news.

You can read many of these predictions in our news archive section – here’s a selection:

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