The Great Rift Valley
The great rift valley begins in the dead sea in the north and ends at the Zambezi River in Mozambique to the south. The valley which was formed by drifting of the earth crust some 10 – 20 million of years ago extends approximately 8700kms.
The Kenya Rift Valley nearly divide Kenya down its length. All the way from Ethiopian border in the north to the Tanzania border in the south. The valley is characterized by uninhabitable deserts in the North, Fertile farmland in the middle of flat arid plains (Savannah grassland – Maasai Mara) to the south.
Kenya Rift Valley Lakes
Since 2011, all Kenya Rift Valley Lakes have experienced rising in water levels. The lakes affected include Lake Naivasha, Elementaita, Nakuru, Bogoria and finally Baringo. This increase in water level have not been experienced in the last 50 years. The government agencies and meteorological departments confirms that the rainfall pattern in the Rift Valley have been pretty normal. Scientists have attributed these rises of water to the effect of regional tectonic movements. Techtronic activities is when violent forces push up molten rocks in volcanic eruption through the fault lines.
In our case, the Rift Valley is responding to the pull of the Indian Ocean forces. As a result, these effects have coursed some activities along some of the lakes to stop. The rising water level have consumed some areas meant for agriculture, buildings and hotels and recreational grounds. The hot geysers at Lake Bogoria have also been affected as they have been completely covered.
The good news though is that the lakes might not rise higher than the current levels. So, no course for worry!