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The Dust Bowl was the result of a period of severe dust storms that greatly damaged the ecology and agriculture of the American and Canadian prairies during the 1930s. The phenomenon was caused by a combination of natural factors (severe drought ) and human-made factors: a failure to apply dryland farming methods to prevent wind erosion , most ...
This drought occurred during the historical Dust Bowl period that characterized much of the plains region of the United States in the 1920s and 1930s. [21] The Central Valley Project was started in the 1930s in response to drought.
Folsom Lake reservoir during the California drought in 2015. In 2011 intense drought struck much of Texas, New Mexico and a large portion of the Southwest bringing much of the region its worst drought seen since the Dust Bowl years of the 1930s. Most of the drought in Texas ended or had it impacts ease by spring and summer 2012 as precipitation ...
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 history of the Arvin Federal Government Camp begins with the migration of people displaced by the events of the Dust Bowl in the mid-1930s. A combination of droughts and high intensity dust storms forced many farmers in areas such as Oklahoma to vacate and find a new beginning. In the summer of 1934 the date July 24th marked the 36th ...
In California’s Mediterranean climate, trees, shrubs and the species they support are naturally adapted to drought. But excessive pumping from wells can push habitats beyond ecological limits by ...
The term "Dust Bowl" initially described a series of dust storms that hit the prairies of Canada and the United States during the 1930s. [4] It now describes the area in the United States most affected by the storms, including western Kansas, eastern Colorado, northeastern New Mexico, and the Oklahoma and Texas panhandles. [5]
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