As the matter of fact, the Eastern Arc Mountains, one of the world’s natural hotspots, form a crescent – shaped chain around 1500 kilometres in length consisting of a total of 20 individual mountains or mountain groups and running from Malawi and Mozambique through Tanzania to southern Kenya’s Taita Hills. The majority of the actual mountains are in Tanzania, where they are situated nine (9) blocks; from south to north, the Livingstone, Mbarika, Udzungwa, Rubeho, Malundwe, Mahenge,  Ukaguru, Nguru, Nguu,  Usambara and Pare Mountains. The Taita Hills in south Kenya are the last outpost of the chain in the north, while the THYOLO MOUNTAINS in Malawi is the southernmost wing of the chain. The Eastern Arc Mountains are ancient crystalline blocks uplifted at least 25 million years ago, though some more recent, but less pronounced geological upheavals have also occurred. It is generally agreed that the natural diversity of the Udzungwa Mountains is the highest among all the stretches of the Eastern Arc Mountains.

The blocks are covered by dense forests, but in the course of  the millions of years the East African climate has become drier and the uniform forest mantle reaching down to the shore of the Indian Ocean has retreated to the west, with the consequence that the forests on the Eastern Arc Mountains now form isolated patches. This isolation has, of course, led in turn to large – scale speciation, and since the two most significant requirements for this, time and space, have been available in abundance, the result is a high rate of endemism.

As far as the world’s hotspot areas are concerned, the Eastern Arc Mountains are today – included in the region known as the EASTERN AFRO MONTANE HOTSPOTS, which are mountains scattered along the eastern edge of Africa, from Saudi Arabia in the north to Zimbabwe in the south.  

 
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