HENRY SALT (1780-1827)
Ras Dejen (4,550 m - 14,927 ft)
Mounts Biuat (4,437 m - 14,557 ft)
Kidis Yared (4,453 m - 14,609ft)
Ethiopia
In Near the village of Asceriah in Abbyssinia, hand colored aquatints, 1809
The mountains
Ras Dejen (4,550 m), Mounts Biuat (4,437 m) and Kidis Yared (4,453 m) are part of the Semien Mountains , in northern Ethiopia, north east of Gondar in Amhara region, are part of the Ethiopian Highlands. They are a World Heritage Site and include the Simien Mountains National Park.
The mountains consist of plateaus separated by valleys and rising to pinnacles.
Because of their geological origins, the mountains are almost unique, with only South Africa's Drakensberg 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 wolves.
The Semien Mountains were formed prior to the creation of the Rift Valley, from lava outpourings between 40 and 25 million years ago during the Oligocene period. The volcano is believed to have spread over more than 5000 m2 and resulted in a thick sequence of basaltic lava some 3,000-3,500 m thick that was deposited on Precambrian crystalline basement. The major part of the Semien Mountains consists of remnants of a Hawaiian-type shield volcano. The Kidus Yared peak is situated near the center 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 Semien 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-northeast direction.
There are different types of soils as a result of the difference in geological formation, glaciations, topography, and climate. The Humic Andosol is the dominant soil type which is mainly found at an altitude of 3,000 m. The other types of soil are shallow Andosols, Lithosols, and Haplic Phaeozems that are mainly common in the area between 2,500 and 3,500 m. The Semien Mountains are highly eroded as a result of human land use practices and as a result of the topography of the area.
The artist
Henry Salt was an English artist, traveller, collector of antiquities, diplomat, and Egyptologist.
After a time as a portrait painter, Salt was permitted to travel with the English nobleman George Annesley, Viscount Valentia as his secretary and draughtsman after being recommended by Thomas Simon Butt. They started on an eastern tour in June 1802, traveling on the British East India Company's extra (chartered) ship Minerva to India via the Cape Colony. In 1805, Valentia sent Salt on a journey into the Abyssinian area (now Ethiopia) to meet with the ras of Tigré to open up trade relations on behalf of the English. While visiting there, Salt gained the respect of the ras. He returned to England on 26 October 1806. His journey home took him through Egypt where he met the pasha Mehmet Ali. Salt's paintings from the trip were used in Valentia's Voyages and Travels to India, published in 1809. The originals of all the drawings were kept by Valentia, as also the copper plates after Salt's death. The format and style of the plates is similar to Thomas and William Daniell's work, "Oriental Scenery" (1795-1808).
Salt returned to Ethiopia in 1809 on a government mission to explore trade and diplomatic links with the Tigrayan warlord Ras Wolde Selassie. Upon arrival, he was unable to meet with the king due to unrest in the country, so instead he went to stay with his friend the ras of Tigré. During this venture, Salt took on the side mission of verifying and correcting the information about the region reported by the Scottish traveler, James Bruce many years earlier. Salt came back to England in 1811 with numerous specimens of both plants and animals.
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2019 - Wandering Vertexes...
by Francis Rousseau
