Excelsior in Hennepin County, Minnesota — The American Midwest (Upper Plains)
Geology of Lake Minnetonka
Photographed By K. Linzmeier, September 1, 2012
1. Geology of Lake Minnetonka Marker
Inscription.
Geology of Lake Minnetonka. . Like most lakes in Minnesota, Lake Minnetonka was formed during the Ice Age of the last two million years. During several separate glacial periods, ice advanced along different routes across the state. The glaciers, along with large volumes of sediment (clay, silt, sand, gravel, and boulders) trapped in the ice, altered the pre-existing terrain and created the landscape we see today. , Before glacial action, the surface of this region consisted of sandstones and limestones, which formed from sediments deposited in seas that covered the area 300 to 500 million years ago. After the seas retreated, rivers carved a valley system into the sedimentary bedrock. This ancient valley system had provided southward drainage through the region. The bedrock floor of a principal valley of that ancient system now lies as much as 122 meters below the surface of Lake Minnetonka. , About 25,000 years ago, at the peak of the last glacial period, or Wisconsin glaciation, an advancing glacier, which was passing over the ancient river valley that now lies beneath Lake Minnetonka, filled the valley with ice. Sediment that melted out of the overriding glacier then buried the ice trapped in the valley. The glacial ice and sediment were later covered by additional sediment from more recent glacial advances. As a result, when glaciers last receded from Minnesota 10,000 years ago, large blocks of ice were buried deep in the ancient valley under thick piles of sediment. When the ice blocks melted, the overlying sediment collapsed and created numerous depressions that filled with water, which are called kettle lakes. At Lake Minnetonka, the ice blocks were so big and close together that the depressions coalesced to form the large, composite kettle lake that we see today. ,
Erected by the Geological Society of Minnesota in partnership with the , Minnesota Department of Transportation and the Minnesota Geological Survey 1998. . This historical marker was erected in 1998 by the Geological Society of Minnesota in partnership with the Minnesota Department of Transportation and the Minnesota Geological Survey. It is in Excelsior in Hennepin County Minnesota
Like most lakes in Minnesota, Lake Minnetonka was formed during the Ice Age of the last two million years. During several separate glacial periods, ice advanced along different routes across the state. The glaciers, along with large volumes of sediment (clay, silt, sand, gravel, and boulders) trapped in the ice, altered the pre-existing terrain and created the landscape we see today.
Before glacial action, the surface of this region consisted of sandstones and limestones, which formed from sediments deposited in seas that covered the area 300 to 500 million years ago. After the seas retreated, rivers carved a valley system into the sedimentary bedrock. This ancient valley system had provided southward drainage through the region. The bedrock floor of a principal valley of that ancient system now lies as much as 122 meters below the surface of Lake Minnetonka.
About 25,000 years ago, at the peak of the last glacial period, or Wisconsin glaciation, an advancing glacier, which was passing over the ancient river valley that now lies beneath Lake Minnetonka, filled the valley with ice. Sediment that melted out of the overriding
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glacier then buried the ice trapped in the valley. The glacial ice and sediment were later covered by additional sediment from more recent glacial advances. As a result, when glaciers last receded from Minnesota 10,000 years ago, large blocks of ice were buried deep in the ancient valley under thick piles of sediment. When the ice blocks melted, the overlying sediment collapsed and created numerous depressions that filled with water, which are called kettle lakes. At Lake Minnetonka, the ice blocks were so big and close together that the depressions coalesced to form the large, composite kettle lake that we see today.
Erected by the Geological Society of Minnesota in partnership with the
Minnesota Department of Transportation and the Minnesota Geological Survey 1998
Erected 1998 by the Geological Society of Minnesota in partnership with the Minnesota Department of Transportation and the Minnesota Geological Survey.
Topics and series. This historical marker is listed in this topic list: Natural Features. In addition, it is included in the Minnesota: Geological Society of Minnesota series list. A significant historical year for this entry is 1998.
Location. 44° 54.271′ N, 93° 33.916′ W. Marker is in Excelsior, Minnesota, in Hennepin County. Marker is at the intersection
Photographed By K. Linzmeier, September 1, 2012
2. Geology of Lake Minnetonka Marker
of Lake Street and Water Street, on the right when traveling north on Lake Street. Marker is at the Port of Excelsior. Touch for map. Marker is in this post office area: Excelsior MN 55331, United States of America. Touch for directions.
Also see . . . Lake Minnetonka. Wikipedia entry. (Submitted on September 30, 2012.)
Photographed By K. Linzmeier, September 1, 2012
3. Geology of Lake Minnetonka Marker
Photographed By K. Linzmeier, September 1, 2012
4. Port of Excelsior
The Geology of Lake Minnetonka Marker is to the left.
Photographed By K. Linzmeier, September 1, 2012
5. Lake Minnetonka
Photographed By K. Linzmeier, September 1, 2012
6. Display at Nearby Gazebo
The Legacy of Excelsior
Credits. This page was last revised on June 7, 2021. It was originally submitted on September 30, 2012, by Keith L of Wisconsin Rapids, Wisconsin. This page has been viewed 3,039 times since then and 152 times this year. Photos:1, 2, 3, 4, 5, 6. submitted on September 30, 2012, by Keith L of Wisconsin Rapids, Wisconsin.