The plains called by the deposition of loess are called as
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the plains called by the deposition of loess or called loess plains.
1.In some locations of Northwestern China and the Midwestern United States, loess deposits could reach thicknesses of over 100 metres and tens of metres, respectively. 2.Typically, loess forms as a large-scale blanket deposit that covers hundreds of square kilometres. 3.Frequently, the deposits are tens of metres thick. 4.Loess frequently grows on vertical or steep faces. 5.Loess often stands in banks for many years without slumping due to the angular nature of the grains. This soil is easily excavated to create cave homes, a popular way of creating human habitations in various regions of China, thanks to a property called vertical cleavage. Loess erodes quite quickly.
L.oess ridges that coincide with the dominant winds have formed in a number of locations throughout the world.