Drygalski Glacier (Tanzania)
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| Drygalski Glacier | |
|---|---|
NASA image from 2004 with locations of major glaciers on Mount Kilimanjaro. Drygalski Glacier is at upper left. Click on image to expand. | |
![]() Interactive map of Drygalski Glacier | |
| Type | Mountain glacier |
| Location | Mount Kilimanjaro, Tanzania |
| Coordinates | 03°03′21″S 37°20′48″E / 3.05583°S 37.34667°E |
| Terminus | Barren rock |
| Status | Extinct |
The Drygalski Glacier was a large ice sheet located on Mount Kilimanjaro in Tanzania, the highest mountain in Africa. Part of the Northern Ice Field near the mountain's summit, it dated to the last ice age, around 11,700 years ago. The glacier was discovered in 1898 by Hans Meyer, who nine years earlier had been the first person to reach Kilimanjaro's summit. It was named after Erich von Drygalski.
Between 1912 and the present day, the ice sheets on Kilimanjaro have retreated dramatically. As of 2016, only the top portions of the Northern Ice Field were reported as still being extant and the Drygalski Glacier was reported as vanished by 2022.
Drygalski Glacier was located on Mount Kilimanjaro in the Kilimanjaro Region of northern Tanzania, on the northwest slope of the peak.[1] The glacier terminus once extended to an elevation of 4,800 metres (15,700 ft) with an origination point near the summit of Mount Kilimanjaro and was fed by the Northern Ice Field. The Great Penck Glacier once flanked Drygalski Glacier to the south and until recently, the Credner Glacier did as well to the north.[2]
