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When severe drought struck the Great Plains region in the 1930s, it resulted in erosion and loss of topsoil because of farming practices at the time. The drought dried the topsoil and over time it became friable, reduced to a powdery consistency in some places.
Excessive heat and drought problems affected the United States in 1934–35 from the Rocky Mountains, Texas and Oklahoma to parts of the Midwestern, Great Lakes, and Mid-Atlantic states. These droughts and excessive heat spells were parts of the Dust Bowl and concurrent with the Great Depression in the United States.
The Drought Relief Service (DRS) was a federal agency of the U.S. ... "Four extensive droughts developed in the Great Plains area between 1930 and 1940, causing ...
Another significant drought in the United States occurred during 1988 and 1989. Following a milder drought in the Southeastern United States the year before, this drought spread from the Mid-Atlantic, Southeast, Midwest, Northern Great Plains and Western United States. This drought was widespread, unusually intense and accompanied by heat waves ...
In the northern Great Plains, weather extremes like drought and flooding, as well as declining water resources, threaten an economy dependent largely on crops, cattle, energy production and ...
The Great Plains Shelterbelt was a project to create windbreaks in the Great Plains states of the United States, that began in 1934. [1] President Franklin D. Roosevelt initiated the project in response to the severe dust storms of the Dust Bowl , which resulted in significant soil erosion .
Summertime temperatures this year proved brutal for many states in the southern Great Plains, and drought conditions continued to worsen across the entire region. ... we saw in the 1930s, but ...
Adding to this, another 125 million acres are at risk in the foreseeable future as warming temperatures create opportunities for expanded agriculture in the Northern Great Plains, while woodland ...