The wet areas include; the shores of Lake Victoria, Kigezi highlands, Nyanza province, Imatong hills in southern Tanzania.
Glacial erosion is common in snow-capped mountains e.g. Mt. Kenya, Rwenzori, and Kilimanjaro.
Wind erosion is most common in dry areas like Karamoja and Turkana land
Types of soil erosion
- Rill erosion: This is the removal of top soil by water leading to the formation of small channels called rills.
- Sheet erosion: This is the uniform removal of topsoil over a large area especially from the sloping land as a result of overflow of water. This type of erosion is difficult to notice or detect because of uniformity.
- Gulley erosion: This occurs when the rills are deepened by water to form depressions called gulleys.
- Splash erosion: This occurs from the impact of raindrops hitting the earth’s surface and the soil particles are splashed in different directions leaving behind small depressions.
- Wind erosion: This is the removal of topsoil by wind and in most cases its the lighter particles which are eroded. This type of erosion is common in dry areas and in areas with little or no vegetation.
CAUSES OF SOIL EROSION
- Overgrazing: This is common in savannah and semi-arid areas of East Africa where pastoralists keep large numbers of animals e.g. Masai land, Turkana land, and Karamoja. The animals especially goats eat up all the grass and leave the ground bare and exposed to agents of erosion like torrential rainfall.
- Industrialization and mining: these activities lead to the breakdown of soil during extraction of minerals and construction of buildings and when it rains heavily, the soils are easily washed away.
- Deforestation: here, the trees are cut down, and the soil is exposed to agents like rainwater and wind, which easily carry away the soil particles.
- Monoculture: when one crop is grown season after season, this leads to soil exhaustion which loosens up the soil hence making the soil particles to be easily eroded.
- Heavy rainfall of over 1500 mm per annum leads to serious surface water runoff which easily erodes the soil from one place to another.
- Bush burning: This is commonly practiced by pastoralists when they are expecting rain which brings new pasture with it. It leaves the ground bare hence exposing it to erosional agents like surface runoff and strong winds.
- Overpopulation: This leads to increased pressure on land through deforestation, monoculture, and land fragmentation, which are responsible for exposing the soil to agents of erosion like running water.
- Cultivating up and downslope: This loosens the soil particles making them be easily eroded by runoff.
- Steep relief: this also leads to soil erosion due to downward movement of soil as a result of gravitational pull.