Fargo sits on the western bank of the Red River of the North in a flat geographic region known as the Red River Valley . The Red River Valley resulted from the withdrawal of glacial Lake Agassiz , which drained away about 9,300 years ago. The lake sediments deposited from Lake Agassiz made the land around Fargo some of the richest in the world for agricultural uses.
Fargo's largest challenge are floods due to the rising water of the Red River, which flows from the United States into Lake Winnipeg in Manitoba, Canada. The Red flows northward, which means melting snow and river ice, as well as runoff from its tributaries, often create ice dams causing the river to overflow. Fargo's surrounding Red River Valley terrain is essentially flat, leading to overland flooding. Since the potentially devastating flood of 2009, both Fargo and Moorhead have taken great strides in flood protection, only a near record flood would cause concern today.
Its geographical location makes the city vulnerable to flooding during seasons with above average precipitation. The Red River's "minor" flood stage in Fargo begins at a level of 18 feet, with "major" flooding categorized at 30 feet and above. Many major downtown roadways and access to Moorhead are closed off at this level. Record snowfalls late in 1996 led to flooding in 1997, causing the Red to rise to a record crest of 39.5 feet, nearly overtaking city defenses. In 2008-2009, significant fall precipitation coupled with a rapid snowmelt in March 2009 caused the Red to rise to a new record level of 40.84 feet, but again Fargo remained safe, in large part due to flood mitigation efforts instituted after the 1997 event and sandbagging efforts by the city residents. Further upgrades were made to city infrastructure and additional resources brought to bear following the 2009 flood, which caused no issues for the city in 2010 despite another rapid melt that caused the Red to rise to 37 feet (which ranks among the top ten highest levels ever recorded).
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