Glacial Pothole Historical Marker – Taylors Falls, MN
Posted by: Groundspeak Regular Member wildernessmama
N 45° 23.980 W 092° 39.092
15T E 527273 N 5027409
Quick Description: This historical marker tells about the geological significance of this area.
Location: Minnesota, United States
Date Posted: 6/22/2013 7:09:15 AM
Waymark Code: WMHC1N
Published By: Groundspeak Regular Member KC0GRN
Views: 2

Long Description:
This historical marker tells about the geological significance of this area. There is a trail that meanders through the park that takes visitors to many of these glacial potholes, some of which have been appropriately named. The text of this marker reads as follows:

Glacial Potholes

The potholes at the St. Croix Dalles have their origins in a tale of fire and ice. They are carved in a dark volcanic rock called basalt, which erupted as lava 1.1 billion years ago. This basalt is related to lava flows that line the North Shore of Lake Superior. About 500 million years ago, when shallow tropical seas covered this area, the basalt was buried beneath a thick blanket of sand, which later became sandstone.

During the last two million years, glaciers have advanced from the Ontario region through the Lake Superior basin, repeatedly covering the Taylors Falls area. About 12,000 years ago, near the end of the most recent glaciation, meltwater collected at the southwestern edge of a glacial lobe as the lobe receded into the Superior basin. This water formed a growing Glacial Lake Duluth. When Glacial Lake Duluth drained, great floods flowed southward through the St. Croix River valley, forming Glacial River St. Croix. The largest of these floods was perhaps a hundred times the volume of modern ones. At this time, Glacial Lake Duluth drained only via Glacial River St. Croix, because ice still blocked the Superior basin's eastern outlet to the lower Great Lakes.

Rapid erosion of drainage spillways around the edge of Glacial Lake Duluth released tremendous amounts of water in a short time. These torrents of meltwater readily cut through the glacial sediments and the sandstone, deepening the St. Croix valley. Fierce rapids developed where the rushing current encountered the hard, resistant basalt. The rapids increased the speed and turbulence of the water, and a heavy sediment load provided powerful abrasive action – all necessary to carve potholes into the basalt.

Potholes commonly occur behind the base of a large boulder or other flow obstruction. They are made when turbulent water forms an eddy, or whirlpool, strong enough to swirl pebbles and cobbles around in one spot. There the swirling stones grind a cylindrical hole down into the bedrock. The exceptional depth and abundance of potholes here attest to the enormous power of Glacial River St. Croix.

Erected by the Geological Society of Minnesota in partnership with the Minnesota Department of Transportation, the Minnesota Geological Survey, and the Minnesota Department of Natural Resources 2009
Marker Type:: City

Visit Instructions:
A photo of the 'Marker' or 'Plaque' is required to identify the location, plus a picture of the 'Historic Site'.
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Benchmark Blasterz visited Glacial Pothole Historical Marker – Taylors Falls, MN 7/24/2012 Benchmark Blasterz visited it