The Simien Mountains (Amharic language: ስሜን ተራራ or Səmen; also spelled Semain, Simeon and Semien), in northern Ethiopia, north east of Gondar 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 Ras Dejen at 4,550 m with the second highest peak of Kidis Yared at 4,453 m; other notable peaks include Mount Biuat 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 South Africa's Drakensberg range having been formed in the same manner and thus appearing similar. Notable animals in the mountains include the walia ibex, gelada, and caracal. There are a few Ethiopian wolf.
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, Ras Dashen rising 4,550 meters (m) above sea level is not only Ethiopia's peak but also one of the tallest mountains in Africa.
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 Phaeozems 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.
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 James Bruce 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.
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