McGregor in Aitkin County, Minnesota — The American Midwest (Upper Plains)
Glacial Lake Aitkin / Peat
Glacial Lake Aitkin
Two million years ago the first of four glaciers covered the surface of Minnesota. They were named for the limit of their southward expansion. The first was the Nebraskan, followed by the Kansan and the Illionian. The last was the Wisconsin. These large masses of snow and ice, thousands of feet thick, advanced and retreated across the face of Minnesota. About 10,000 years ago, the Wisconsin glacier melted and left behind the topography we see today.
As the Wisconsin glacier slowly advanced and retreated, it created many geological features during its estimated 90,000 years of existence. These features, created about 20,000 years ago, include moraines, kames, eskers, drumlins and even the soil beneath the mantel of green that covers Minnesota. The city of Aitkin was built on a moraine. As the ice and snow of the glacier melted, lakes formed in the gouged out areas behind the moraines.
Glacial Lake Aitkin covered most of northern Aitkin County, including McGregor. It stretched from Aitkin to present-day Grand Rapids and, for a time, joined with Lake Upham. Both were shallow lakes, which disappeared when the glacier advanced again. Lake Aitkin and Lake Upham reformed when the glacier finally melted. The second lakes were named Glacial Lake Aitkin II and Glacial
As Lake Aitkin slowly drained, peat began to form in the bog area that remained. Carbon 14 dating shows that this formation began about 6,700 years ago. The peat gradually accumulated to a depth of five to ten feet.
The bogs that surround McGregor contain peat. Peat is dead and decaying plant material that accumulates in poorly drained land and old glacial lake beds. The stagnant waters retard the normal decomposition of the vegetation, allowing peat to form. The United States has 51 million acres of peat: over seven million acres of peat exist in Minnesota.
Reference to peat can be found in world literature. Among the authors to mention it are Tacitus, Shakespeare, and Emily Dickinson. Perhaps, the most familiar is Sir Arthur Conan Doyle in, “The Hounds of the Baskervilles,” with the immortal Sherlock Holmes venturing onto the moors.
Minnesota has three types of peat. The first is Fibric peat, which is tan to reddish brown in color. The second is Sapric, which is very dark in color. Hemic, the third type, is dark reddish brown; it is derived from sedges, rushes and reeds. Hemic bogs are found in the McGregor area.
Used as fuel since Roman times, peat
Today, the peat industry generates over ten million dollars of business in Minnesota. It is a resource that will become more valuable as our fossil fuels are expended. Finland, Ireland and Russia use peat-burning power plants. Maine established a peat-fired power plant in 1990.
Erected 1997 by The Minnesota Department of Transportation.
Location. 46° 36.471′ N, 93° 18.06′ W. Marker is in McGregor, Minnesota, in Aitkin County. Marker can be reached from the intersection of Minnesota Route 210 and Minnesota Route 65. Click for map. Marker is located at the Tourist Information Center just west of the intersection of Minnesota 210 and Minnesota 65 South. Marker is in this post office area: McGregor MN 55760, United States of America.
Also see . . . Proglacial lakes of Minnesota. Wikipedia (Submitted on July 1, 2011, by Bernard Fisher of Mechanicsville, Virginia.)
Categories. • Natural Features •
Credits. This page originally submitted on , by Paul Fehrenbach of Germantown, Wisconsin. This page has been viewed 1,215 times since then and 190 times this year. Photos: 1, 2, 3, 4. submitted on , by Paul Fehrenbach of Germantown, Wisconsin. • Bernard Fisher was the editor who published this page. This page was last revised on June 16, 2016.