Mousa Ali

Mousa Ali (Arabic: موسى علي) is a 2,021 metres (6,631 ft) stratovolcano located on the tri-point of Ethiopia, Eritrea and Djibouti. The volcano is the highest point in Djibouti. The volcano's summit is truncated by a caldera, which contains rhyolitic lava domes and lava flows.[2] The last known eruption occurred before the Holocene era.

Mousa Ali
Mousa Ali from Djibouti.
Highest point
Elevation2,021 to 2,028 m (6,631 to 6,654 ft)[1][2]
Prominence1,607 m (5,272 ft)[1][3]
ListingThe highest point in Djibouti
Ultra
Coordinates12°28′07″N 42°24′15″E[1]
Naming
Native nameموسى علي (Arabic)
Geography
Mousa Ali is located in Djibouti
Mousa Ali
Mousa Ali
Location of Mousa Ali in Djibouti (on tri-point border with Eritrea and Ethiopia)
Countries Djibouti,  Ethiopia and  Eritrea
RegionsTadjourah Region, Afar Region and Southern Red Sea Region
Parent rangeDenakil[3]
Geology
Mountain typeStratovolcano
Last eruptionHolocene
Climbing
First ascent1841

Mousa Ali is situated at the tri-point of the Tadjourah Region of Djibouti, the Southern Red Sea Region of Eritrea, and the Afar Region of Ethiopia.

Geography

Mousa Ali relief map.

The mountain has two distinct summits, the higher being the south one with an elevation of 2,021 metres The north summit in Ethiopia has an elevation of 1,871 metres. Both summits are separated by a large caldera, about 1 km (0.71 mi) wide and 1514 metres deep. Mousa Ali, in the northern part of the Great Rift Valley region, has Eritrea on its northern flank, Ethiopia on the west, and Djibouti the east and south. The Djiboutian town of Dorra is 36 km to the south-southeast, the Ethiopian volcano Manda-Inakir is 22 km to the southwest, and the road from the Ethiopian town of Manda to the Eritrean port of Assab is 19 km to the northwest.

Wildlife and flora

The mountain is home to an abundant amount of wildlife, lush vegetation, flowering shrubs and trees and various plants.

History

Two sects of Afar live in the area. They are collectively known as Adrúmmi, from 'Adó rum li or "white as Byzantines." The position of Ali Mousa as the tripoint between Ethiopia, Eritrea and Djibouti is not the result of an agreement between the three countries. In December 1948 the British administering Eritrea refused to attend a meeting with the other two parties to determine the exact location of their tripoint, set in a 1908 treaty as 60 km inland from the Red Sea. British administration of Eritrea ended in 1952, and with increasing Ethiopian administration over the ensuing decade, and incorporation into Ethiopia from 1962 to 1993, the boundary was internal, not international. In 2002, the Eritrea-Ethiopia Boundary Commission established the tri-point at the Mousa Ali summit;[4] Ethiopia had pressed for it to be further east, nearer to Dadda'to, Djibouti.

Climate

The temperature of Mousa Ali usually ranges from 7 °C to 17 °C in December and January, and 16 °C to 26 °C from June to September. The weather on the mountain can be very erratic, sometimes severe.

Climate data for Mousa Ali
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) 17.9
(64.3)
20.4
(68.8)
20.4
(68.8)
22.7
(72.8)
23.7
(74.6)
24.7
(76.4)
26.3
(79.3)
25.8
(78.4)
24.1
(75.3)
23.2
(73.7)
20.6
(69.0)
18.3
(64.9)
22.3
(72.2)
Average low °C (°F) 7.9
(46.3)
8.4
(47.1)
9.9
(49.8)
11.8
(53.2)
13.7
(56.6)
15.2
(59.3)
16.9
(62.5)
16.6
(61.8)
15.2
(59.3)
12.7
(54.8)
10.4
(50.7)
8.9
(48.0)
12.3
(54.1)
Average rainfall mm (inches) 5
(0.2)
6
(0.2)
11
(0.4)
34
(1.3)
39
(1.5)
6
(0.2)
6
(0.2)
53
(2.1)
47
(1.9)
13
(0.5)
9
(0.4)
13
(0.5)
242
(9.4)
Source: Climate Data

See also

References

  1. Africa Ultra-Prominences, Peaklist.org, listed as "Moussa Ali Terara" Retrieved 29 September 2011
  2. "Mousa Ali". Global Volcanism Program. Smithsonian Institution. Retrieved 2007-04-04.
  3. "Moussa Ali" on Peakbagger Retrieved 29 September 2011
  4. Eritrea-Ethiopia Boundary Commission (2002-04-13). "Reports of International Arbitral Awards-Decision regarding delimitation of the border between Eritrea and Ethiopia" (PDF). United Nations. pp. 167, 179. Retrieved 2017-01-20.
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