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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.
The drought was so severe that the once-rich topsoil in such states as Oklahoma, Kansas, Texas, Colorado, and New Mexico turned to dust. When the dust was lifted into the air by the relentless prairie winds, huge storms were created that turned the entire region into a gigantic dust bowl.