The New Encyclopædia BritannicaEncyclopædia Britannica, 1983 - Encyclopedias and dictionaries |
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Page 185
... east and the Mauritania - Sénégal Basin in the west and between Reguibat in the north and Kinshasa in the south . The east - to - west crystalline dorsal formations running from Cameroon through the Ubangi ( Oubangui ) region to The ...
... east and the Mauritania - Sénégal Basin in the west and between Reguibat in the north and Kinshasa in the south . The east - to - west crystalline dorsal formations running from Cameroon through the Ubangi ( Oubangui ) region to The ...
Page 186
... East African Rift Valley / Benadir Lowland Danakil Plain Masai Steppe Nyasaland Tableland Basin Mozambique Lowland Basin Drakensberg Mountains ableland -0 ° Major faults of the East African Rift System Physiographic regions of Africa ...
... East African Rift Valley / Benadir Lowland Danakil Plain Masai Steppe Nyasaland Tableland Basin Mozambique Lowland Basin Drakensberg Mountains ableland -0 ° Major faults of the East African Rift System Physiographic regions of Africa ...
Page 949
... East Antarctica . No earthquakes have occurred in historic time along these or other faults in Antarctica , now the quietest and most aseismic of all continents . The ancient crust of Antarctica must have been highly mobile and the ...
... East Antarctica . No earthquakes have occurred in historic time along these or other faults in Antarctica , now the quietest and most aseismic of all continents . The ancient crust of Antarctica must have been highly mobile and the ...
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