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which once crowned the top of Mount
Kilimanjaro. The glacier is situated at an elevation of between 5,800 and 5,500 metres (19,000 and 18,000 ft). Credner Glacier is one of the largest glaciers on the mountain and descends from the
215:. Credner is rapidly retreating due to its high exposure point on the northwest slope of Mount Kilimanjaro. A report published in 2013 indicated that in another decade the glacier may no longer exist.
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Sirguey, P. J.; Cullen, N. J.; Moelg, T.; Kaser, G. (Fall 2013). "Ice volume assessment of the
Northern Ice Field of Kilimanjaro: the photogrammetry strikes back".
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NASA image from 2004 with locations of major glaciers on Mount
Kilimanjaro. Credner Glacier is at upper left. Click on image to expand.
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N. J. Cullen; P. Sirguey; T. M¨olg; G. Kaser; M. Winkler; S. J. Fitzsimons (2013).
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348:"A century of ice retreat on Kilimanjaro: the mapping reloaded"
288:"Glaciers of the Middle East and Africa - Glaciers of Africa"
206:, on the northwest slope of the peak and is a remnant of an
395:. The Smithsonian/NASA Astrophysics Data System: C42A–05.
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Credner
Glacier and recently exposed old lava in 2009
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318:(2011 ed.). Springer. p. 676.
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315:Encyclopedia of Snow, Ice and Glaciers
247:Scientist atop Credner Glacier in 2009
312:Singh, Vijay P., ed. (July 1, 2011).
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435:. You can help Knowledge (XXG) by
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262:Retreat of glaciers since 1850
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169:1.30 km (0.81 mi)
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389:AGU Fall Meeting Abstracts
286:Young, James A.T. (1991).
267:List of glaciers in Africa
293:. U. S. Geological Survey
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492:Tanzania geography stubs
423:This article about a
373:10.5194/tc-7-419-2013
482:Glaciers of Tanzania
150:3.05306°S 37.34944°E
65:Show map of Tanzania
401:2013AGUFM.C42A..05S
364:2013TCry....7..419C
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213:Northern Ice Field
155:-3.05306; 37.34944
95:Show map of Africa
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297:October 15,
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128:Coordinates
476:Categories
331:October 9,
273:References
185:Retreating
141:37°20′58″E
138:03°03′11″S
429:Tanzania
256:See also
204:Tanzania
174:Terminus
121:Tanzania
113:Location
425:glacier
397:Bibcode
360:Bibcode
219:Gallery
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182:Status
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291:(PDF)
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320:ISBN
299:2014
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.