File:Snow and Ice on Kilimanjaro-2000.jpg

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The ice on the summit of Kilimanjaro, which formed more than 11,000 years ago, has dwindled by 82 percent over the past century. The dramatic decline in Kilimanjaro’s ice cap is particularly remarkable given its persistence through many previous shifts in climate, including a severe 300-year-long drought that impacted human populations living in the area about 4,000 years ago.

The scene shows heavily vegetated terrain (green colors) around the foot of Kilimanjaro, while the vegetation is relatively sparse up the flanks of the 5,895-meter-tall (19,335-foot) stratovolcano. The light browns at higher elevations show mostly rock and bare land surface, revealing the crisscrossing drainage patterns etched into Kilimanjaro’s face over the millennia by rain and snowmelt. Here, the images have been draped over a digital elevation model to give a better sense of the mountain’s three-dimensional shape.
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Source NASA Earth Observatory Snow and Ice on Kilimanjaro
Author Landsat 5
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This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.

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Public domain This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.)
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February 17, 1993

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current02:29, 5 May 2008Thumbnail for version as of 02:29, 5 May 20082,560 × 1,920 (1.15 MB)CarolSpears (talk | contribs){{Information |Description=The ice on the summit of Kilimanjaro, which formed more than 11,000 years ago, has dwindled by 82 percent over the past century. The dramatic decline in Kilimanjaro’s ice cap is particularly remarkable given its persistence th

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