It's steeper than a flat surface, and water doesn't usually run uphill, unlike the Nile. If precipitation occurs at the top of the hill, the water doesn't stay at the top and just sink into the ground as storage water. It rolls down the hill as runoff. The water, on it's way down, picks up sediment and rocks, and caries it to the bottom of the hill and a lot of times into a river, lake, stream, creek, e.c.t. It's maximum there because water can't move at a steady pace on a flat surface or uphill unless its a river or creek.
Soil erosion on hill slopes can be checked by contour ploughing.
Terraces significantly reduce the rate of soil erosion on slopes.
plant trees
Ring bunds can help in flood control along the hill slopes and filed boundaries as they reduce the soil erosion.
This is true, soil is removed from sloped due to erosion and generally deposited on plains
Prevention of soil erosion because the plowing is done according to how the land lays.
The hill slopes steeply away from the road in this area. Let's hit the slopes! (Let's go skiing!)
Charlotte Amalie The capital is Charlotte Amalie, which is situated halfway along the southern coast on hill slopes. Its well-sheltered harbour is in the crater of an extinct volcano. The climate is semiarid, and most of the annual average of 45 inches (1,150 mm) of rainfall is used by vegetation or evaporates. The capital is Charlotte Amalie, which is situated halfway along the southern coast on hill slopes.
In terrain with steep hills slopes the crop and cultivation technique that will minimize soil erosion are apples that land between the trees is planted in grass and not cultivates. The area were pedal soils most likely to be found are a moderately dry to semiarid grassland such as the western great plains.
soil erosion on hill sloppes can be checked by
A slope is a inclined area like a hill, used for skiing.
The deeper soil on the lower slopes is a result of soil being washed down from the top of the hill by water which results from the precipitation of rain or snow. Soil can also be blown from the top of the hill by the wind and then redeposited in the lee of the hill and thus added to the deposits on the lower slopes.