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To prevent blowing, these areas needed to be regrassed in the 30s. The soils in the Dust Bowl region have a characteristic known as âflocculationâ which, like fish eggs, causes small soil particles to cling together in clusters. This in short, facilitates the movement of moisture to the subsoil.
Because the crops died due to a lack of rain and bad farming practices, millions of acres of topsoil were blown away during dust storms. Large dark clouds of dirt were visible across the Great Plains during the timeline of the Dust Bowl. In 1932, 14 dust storms were recorded on the Great Plains.