<span>Millet is grown in the Sahel because it is one of the main staples of the people there. It is considered as a vital source of staples. It is also, happened when it is grown with cowpea and sorghum. Fortunately, the risk of complete crop failure decreased.</span>
The African Plate is a major tectonic plate straddling the equator as well as the prime meridian. It includes much of the continent of Africa, as well as oceanic crust which lies between the continent and various surrounding ocean ridges. Between 60 million years ago and 10 million years ago, the Somali Plate began rifting from the African Plate along the East African Rift.[2] Since the continent of Africa consists of crust from both the African and the Somali plates, some literature refers to the African Plate as the Nubian Plate to distinguish it from the continent as a whole.
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Water deficit exists where demand is greater than supply. These are known as WATER DEFICIT areas and can be in deficit because of either low precipitation or high evaporation rates. They might also be in deficit because of high populations.
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1. the mountain building and other changes associated, over hundreds of millions of years, with global-level plate tectonics. denudation and weathering processes, both those operating at the present time and those which have operated, with stunning long-term effect, over tens of millions of years.
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Continental climate is a type of climate characterized by consistently hot summers, persistently frosty winters and low rainfall. The continental climate is formed as a result of the prevailing impact on the atmosphere of large land masses. This type of climate is typical for the interior regions of the continents.
The continental climate is dominant in a significant part of the territory of Russia, Ukraine, Kazakhstan, Uzbekistan, Mongolia and the interior regions of the United States and Canada. It leads to the formation of steppes and deserts, since most of the moisture of the seas and oceans does not reach the inland regions.