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of the wind escarpment, the wind speed is increased.

As a result, the Loess Plateau is not only a site of loess deposition but also a source of dust because of strong wind erosion. Wind erosion is very severe during the glacial period. During the glacial period, there is very little vegetation, so it favors wind erosion.

Vertical loess joints

Loess vertical joints distribution depends on the loess structure, water moisture, strata and microtopography. There are vertical development features and lateral development features.

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