As the ice receded to the north, the glacial meltwater formed huge lakes, such as Lakes Agassiz (Ag-a-see) and Koochiching (Koo-chee-ching). The map shows the total extent of Lake Agassiz over time. At no time did the lake flood the entire area shown. At its largest, the lake was larger than any lake that exists today.
The southern area of the lake, in today’s Minnesota and North Dakota, would have been flooded about 11,700 years ago at a time when the northern areas would have still been covered with ice. By the time the northern areas (Manitoba) were flooded much of the southern area of the lake would have already drained. The lake left behind a small amount of sediment in the form of clay layers in the Red River Basin.
Source: University of Manitoba Libraries Map Collection
The glaciers continued to recede north exposing the sand delta. For the next 5,000 years (9,000 to 4,000 years ago) the climate becomes drier and warmer. Winds arrange the sands into dunes.
Barcan dunes formed when there was little vegetation. These dunes tend to be moved forward by the force of the wind.
As the climate became wetter, vegetation became established. This vegetation anchored the tails of the dunes, preventing them from moving. These dunes are called parabolic dunes.
Vegetation now covers much of the Fertile Sand Hills, but you can see examples of the exposed dunes in both Death Valley 1 and Death Valley 2. A short hike from the nature center and you can immerse yourself in ancient geological history!
The Ojibway named it "ga-papiqwutawangawi zibi", or "the river of the sand hills, scattered here and there in places." In 1800, Alexander Henry, a fur trader, passed the mouth of the river which he called the Riviere aux Buttes de Sable. This French phrase translates into English as river with hills of sand.
In 1806-07, William Henry had an outpost on the Sand Hill River. During the trading season he collected 500 beaver, 41 black bear, 1 grizzly bear (the last reported in Minnesota), 15 martens, 33 mink, 22 muskrats, 24 otters, 91 fishers, 250 wolves, 43 deer skins, 43 red fox, and 3 wolverines. He also reported an overwhelming abundance of bison, elk and waterfowl.
From 1820-1870, the Woods Trail (a major route on the Red River Oxcart Trails from Winnipeg to St. Paul) passed through this area in the general vicinity of Fertile. This route was taken to escape the Beltrami Marsh and dunes to the west, and the marshes and lakes east of Fertile. For some distance the trail followed one of the old dry beach ridges of Glacial Lake Agassiz.
In March of 2009 the Sand Hill River reached record high levels, eventually flooding up to the threshold of the building. Flooding is a natural process of the Sand Hill River. In 2009 snow melt resulted in the exceptional amount of flooding. Click on the link below to watch a short clip of the flood.
In 1976, the City of Fertile purchased 640 acres of the Sand Hills to be used as a wilderness sanctuary and recreation area. A grant in 1985 allowed the nature center building and trail system to be created. The Agassiz Environmental Learning Center (AELC) was established as a private non-profit corporation in 1991.