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The Coastal Region

The Coastal Region extends some 250 miles from the southern border where Kenya meets Tanzania, to the border with Somalia in the north. This region is characterized by a variety of geographical features, a variety that is particularly pronounced as one travels south or north. The southern shoreline consists largely of stretches of coral rock and sand interrupted by bays, inlets, and branched creeks. Following the coast is a barrier reef that is broken only rarely. Traveling inland from the coast, one encounters a narrow plain, and later a low plateau area reaching an elevation of about 500 feet, and, finally, a line of discontinuous ridges. The principal geographic feature of the northern part of the region is the Lamu Archipelago, which was formed when a rise in the ocean level inundated coastal lands.

 

The Kenya Highlands Region

The Kenya Highlands Region was known as the White Highlands during colonial times since the European population tended to concentrate there. The region consists of two major divisions, lying east and west of the Great Rift Valley that runs north-south. These regions are made up of a variety of geographical subdivisions whose origins are diverse. The entire area is characterized by significantly higher altitude, cooler temperatures, and, generally speaking, more plentiful precipitation than in other regions.

 

The Northern Plain-lands Region

The Northern Plain-lands Region stretches from the border with Uganda on the west to the Somalia border on the east. It is made up of a series of arid plains formed by erosion or by great outpourings of lava. The region includes Lake Rudolf and the Chalbi Desert. West of the lake the lands are quite arid, with an annual rainfall that averages under ten inches and that falls some years to an almost negligible level. East of Lake Rudolf lies the Chalbi Desert; still farther east are equally arid lands that ordinarily support only semi-desert vegetation.

 

 

 

 

 

 

 

 

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