Highlights in the history of the Gorge

• the stretch of the Mississippi between downtown Minneapolis and Fort Snelling is the only true gorge along the river’s entire 2,350-mile length.
• 45,000 to 12,000 years ago, during the last ice age, glaciers advanced and retreated many times over this area to slough away all the younger or top layers of rock formations.
• The glaciers melted 12,000 years ago, forming an immense amount of water to create our current rivers.
• Saint Anthony Falls was formed 12,000 years ago near what is now downtown Saint Paul. The falls receded upstream for 12,000 years to their current location near downtown Minneapolis.

The geologic layers of the gorge include:

Glacial Till

This is our modern soil, which is sediment and till left from the movement of glaciers. It can be 100 feet thick in some areas.

Platteville Limestone

This layer is approximately 30 feet thick and contains fossils from the floor of an Ordovician Period Ocean, which covered the area.

Glenwood Formation

This is a very soft layer of shale, mainly remains from the Ordovician Sea.

Saint Peter Sandstone

This is a softer sedimentary rock, which was easily carved away by the falls.

How the falls were formed

The gorge was formed from the turbulent water of Saint Anthony falls wearing away the lower soft layer of Saint Peter Sandstone and undercutting the layers of shale and limestone above. Top layers began to crumble and the falls retreated slowly upstream for 12,000 years to their current location in Minneapolis.

Image: National Park Service/MNRRA

The falls continued this gradual carving action, receding at a rate of 4 feet per year and moving 10 miles upstream.

European settlers arrived in the 1800s while the falls were still receding. Wanting to preserve the falls as a source of power, they built a dam of sorts to stabilize the falls. If the falls were left to run naturally and continue their recession, eventually they would have smoothed out into rapids just north of downtown Minneapolis due to differences in streambed geology in that area.

3,828 years ago, the falls were located somewhere near the Railroad Bridge in Seward. This can be figured out by measuring the distance from the current location of the falls to any given point. Calculate that distance in feet and then divide by 4 feet (since the falls retreated 4 ft/yr). You will then have the number of years since the falls were at that selected point. One last step is to subtract 132 years due to the fact that the falls were actually stabilized in 1870.

Some natural history

• The gorge is used as a migration flyway for approximately 150 species of birds, including 45 nesting species. 40% of North America’s migratory waterfowl use the river gorge as a migration corridor.
• Historically 120 native fish species thrived in the rapids of the gorge, 30 are currently remaining.
• Native ecosystem of oak forest with open spaces of prairie plants. Current ecology consists mainly of deciduous forest. There are more fire-sensitive species found due to the suppression of fire. Some of these species include maples, elms, basswood, as well as invasives such as buckthorn.
• Several human-induced problems are degrading the ecology of the gorge, such as exotic species, foot and bike traffic erosion, suppression of fire, re-routing of water (pavement and storm drains), and pollution in general.

More on the Gorge

The National Park Service/Mississippi National River and Recreation Area web site — A wealth of information and resources about the Twin Cities stretch of the Mississippi River.