River Warren Falls - Glacial River Warren

Glacial River Warren

When the great glacial River Warren began running 11,700 years ago, it cut a wide valley through central Minnesota, through the glacial till, but on top of the limestone layer. The Minnesota River currently runs in the valley created by the River Warren. When the river reached present-day St. Paul, the massive volume of water quickly washed out the till, sand, gravel, and sedimentary rock that had filled one of the troughs. The result was the Warren River Falls, plunging 175 feet (53 m) into a deep gorge. The turbulence caused by huge volumes of falling water washed out the sandstone underneath the falls, causing the thin limestone layer to break off in chunks. By 10,000 years ago, the waterfall had moved upstream to the confluence of the River Warren and the Mississippi River, adjacent to present-day Fort Snelling. By 9400 years ago, it had receded another two miles (3 km) up to Nine Mile Creek. At that point, Lake Agassiz broke through the ice to the north and began draining via the Red River of the North to Hudson Bay. River Warren then ceased to flow, but was succeeded by the much smaller Minnesota River which drained a smaller watershed. It carried soil and sediment, but with much less energy than its predecessor. It was less able to transport those suspended materials, which precipitated out and left deposits. Eighty feet (24 m) of this alluvium filled the river valley at Ft. Snelling, and 175 feet (53 m) were deposited at Saint Paul, refilling much of the gorge.

The hydrology of the oversized valley was first explained by General G. K. Warren in 1868. He made a detailed survey of the valley in his search for possible transcontinental railroad routes. Posthumously, in appreciation of this work, the glacial river that was the outlet of Lake Agassiz was named River Warren.