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The Simien Mountains (: ስሜን ተራራ or Səmen; also spelled Semain, Simeon and Semien), in northern , north east of in Amhara region, are part of the Ethiopian Highlands. They are a World Heritage Site (since 1978) and include the Simien Mountains National Park. The mountains consist of plateaus separated by valleys and rising to pinnacles. The highest Ethiopian mountain is at 4,550 m with the second highest peak of at 4,453 m; other notable peaks include at 4,437 m.

The Simien Mountains are remarkable for being one of the few spots in tropical Africa where snow regularly falls.Discussed further in Frederick J. Simoons, "Snow in Ethiopia: A Review of the Evidence", Geographical Review, 50 (1960), pp. 402-411. Because of their geological origins, the mountains are almost unique, with only 's range having been formed in the same manner and thus appearing similar. Notable animals in the mountains include the , , and . There are a few .

The region received status as a biosphere reserve in 2017, aimed at safeguarding its exceptional ecosystems and cultural value while also advancing sustainable growth initiatives. The Simien Mountains National Park stands out for its peaks and deep valleys that attract hikers and nature lovers alike. Its renowned peak, rising 4,550 meters (m) above sea level is not only Ethiopia's peak but also one of the tallest mountains in Africa.


Etymology
Although the word Semien means "north" in , according to Richard Pankhurst the ancestral form of the word actually meant "south" in Ge'ez, because the mountains lay to the south of . But over the following centuries the core of the Christian kingdom itself moved to the south, these mountains came to be thought of as lying to the north, and the meaning of the word likewise changed.


Geology and landscape
The Simien Mountains were formed prior to the creation of the Rift Valley, from lava outpourings between 40 and 25 million years ago during the period. The volcano is believed to have spread over more than 5000 m2 and resulted in a thick sequence of some 3,000-3,500 m thick that was deposited on crystalline basement. The major part of the Simien Mountains consists of remnants of a Hawaiian-type . The Kidus Yared peak is situated near the middle of the shield volcano. Ras Dejen (4,533 m), Bwahit (4,430 m) and Silki (4,420 m) were formed from the outer core of this ancient volcano.

The extreme escarpment in Simien appears to be a precondition for the formation of the extended uplift of the whole mountain massif 75 million years ago. The dramatic views are due to this volcanic activity. Especially of note is the 2,000 m high escarpment extending in a southwest to northeast axis.

There are different types of soils as a result of the difference in geological formation, glaciations, topography, and climate. Humic are the dominant soil type which is mainly found at an altitude of 3,000 m. The other types of soils are shallow Andosols, Lithosols, and Haplic that are mainly common in the area between 2,500 and 3,500 m. The Simien Mountains are highly eroded as a result of human land use practices and as a result of the topography of the area.


Fauna
The park hosts endangered animals, like the – a species of exclusively living in the Simien Mountains region. The and the , a primate that feeds on grass, are also residents of this area.


Culture
The Simien Mountains hold significance not for their wildlife but for their contributions to the local culture and agriculture scene. Local farmers have been utilizing the terraces etched into the mountainsides for generations with the region hosting villages where ancient farming techniques are still practiced.


History
There is a note in Cosmas Indicopleustes' work that the Simien Mountains were a place of exile for subjects condemned to banishment by the Aksumite king.Wolska-Conus, W., La topographie chrétienne (Paris Press univ. de France 1962)

First mentioned in the Monumentum Adulitanum of the 3rd century AD (which described them as "inaccessible mountains covered with snow" and where soldiers walked up to their knees in snow), the presence of snow was undeniably witnessed by the 17th century Jesuit priest Jerónimo Lobo.Donald M. Lockhart (translator), The Itinerário of Jerónimo Lobo (London: Hakluyt Society, 1984), p. 240. Although the later Scottish traveller claims that he had never witnessed snow in the Simien Mountains, the 19th century explorer Henry Salt not only recorded that he saw snow there (on 9 April 1814), but explained the reason for Bruce's failure to see snow in these mountains – Bruce had ventured no further than the foothills of the Simiens.Henry Salt, A Voyage to Abyssinia and Travels into the Interior of that Country, 1814 (London: Frank Cass, 1967), p. 352.

Despite their ruggedness and altitude, the mountains are dotted with villages linked by tracks.


Folklore
An old folklore from the Semien mountains regarding certain trees called was documented in 's early 19th century journal. The Genwarar trees are seldom above eight feet in height, and from a distance could give the appearance or shape of a human being. The people would never cut these trees, owing to a superstitious belief that something bad would befall them as a consequence. Local traditions say the trees contain evil spirits, which have been cast out of human beings, and are harmless when not disturbed, however, when a tree is cut, the spirits enter a person out of vengeance, but in general not to those who cut them down. Aside from this, the trees produces a milky substance, which is used for ink, for the purpose of writing charms, to be worn on any part of the body as a cure for those possessed by evil spirits, and to prevent their entering those who are not previously tormented with them.± The milk of the genwarar was also used in the treatment of lingering sickness.
(2025). 9781107450516, Cambridge University Press. .


External links
Simien Mountains National Park Simien Mountains Tour

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