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By James Jackson Kilpatrick

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8°N DJ Addis Ababa N . R. eN AFAR Awash Blu Lake HIGHLA L. Tana 12°N River R. NDS zze Land < 1000 m ITR EA 4°N DS AN L H HIG OGADEN We b iS he be li 500 km Fig. 1 Ethiopia’s main topographic regions upside down and we are scrambling up and down the legs”. This is an apt observation. The highlands range from rugged and majestic peaks reaching elevations of over 4500 m, to gently rolling fertile hills and plains which are dissected by deep and often impassable gorges. The Western Highlands taper away westwards toward the Sudan plains, and the Southeastern Highlands southeastwards to the Ogaden, but to the east and north respectively they terminate abruptly at high escarpments which separate them from Afar.

Some plates, such as the Pacific Plate, consist of oceanic lithosphere (uppermost mantle topped by oceanic crust) only; others, such as the African Plate, consist of both continental and oceanic lithosphere. 3 Plate Boundaries The plates are separated from one another by plate boundaries. There are several types of plate boundary depending on how the plates are moving. These are illustrated in Fig. 3. Some plates, for example the South American and African ones, are moving away from each other (Fig.

At the time of its formation the Orogen would have been oriented E–W. The figure shows it rotated to its present N–S orientation 31 MOZAM BIQUE 5 Indian Craton East Antarctica Craton Kalahari Craton Arabian Nubian Shield: mainly metamorphosed oceanic rocks Mozambique Belt: mainy metamorphosed continental rocks Cratons EAST AFRICAN OROGEN Outline of today’s continents 32 5 Beginnings: The First Half-Billion Years much older ages have been measured on Ethiopian rocks, even greater than 2000 million years.

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A special study of the Portuguese Provinces: A Place for Pioneers by James Jackson Kilpatrick

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