Snow in Kenya is not a particularly common sight, given that the east Africa country sits right on the equator and has vast stretches of semi-desert scrubland. And yet, there is one spot where you can always find snow in Kenya.
Mount Kenya is the tallest mountain in Kenya, and the second highest in all of Africa. Only Tanzania's Mount Kilimanjaro towers higher. The top of Mount Kenya is perpetually snow-covered due to the high elevation. In fact, the Meru people call the mountain "Kirimara", which translates from their language to "that which has white stuff", in reference to the white peaks.
Answer:
The A horizon will be relative large with a high content of sand.
Explanation:
A desert, as it is, is covered with very fine sediments in most cases, ranging from medium and small rocks to fine sand. If the climate conditions were to change where there is a desert and the climate became more temperate, the soil will change as well relatively quickly. What is actually now the surface of the deserts will become the new soil's A horizon while on top of it a 0 horizon will form.
The A horizon in a former desert will become very fertile and it will be able to support lush vegetation. This will be the case because it will have a very high content of sand, thus it will be very airy and soft. The newly formed O horizon made out of biomass on top of it will wash away to the A horizon, increasing its fertility further by adding a big amount of decomposed biomass to it.
Answer:
The flow velocity, or speed of flow, can influence the shape and rate of erosion of a river system. The cross-sectional shape of a river dictates how much friction will impact the flow of water within a river. Finally, the sediment load, or the amount of rocks and soil in the river, impacts its flow velocity and shape.The velocity of a river is determined by many factors, including the shape of its channel, the gradient of the slope that the river moves along, the volume of water that the river carries and the amount of friction caused by rough edges within the riverbed. Access to a fresh water supply is affected by the following factors: Climate – low levels of rainfall and high temperatures lead to water deficits . When rainfall is low, there is less water available. When temperatures are high, water evaporates and so there is less available to use.
The development of large farms has polluted the river through waste runoff.
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