The Geology of Amnicon FallsHave you ever heard of the Douglas Fault? No, it's not someone's mistake, but the site of earthquakes that occurred about a half billion years ago. Amnicon Falls State Park has long been known as the best place to observe and study this important geological event and the associated rock formations.
As you look at the Upper Falls, a billion years of geological activity lies before you. Evidence of volcanic eruptions, the advance of great oceans, the formation of sandstone, earthquake movements' and glaciation can all be seen. The dark basalt seen at the Upper Falls is the solidified remnants of lava that flowed across the entire region about a billion years ago.
About 500 million years ago, there was a tremendous fracturing and movement of the basalt bedrock. The crack, called the Douglas Fault, extends from east of Ashland, Wisconsin, to near the Minnesota Twin Cities. The bedrock south of the fault slowly moved upward and to the north at a 50- to 60-degree angle.
The fault became the location of Amnicon's Upper Falls, Snake Pit Falls, and Now and Then Falls (above) and Pattison State Park's Big Manitou Falls. More recently, great glaciers moved across the area. They brought different kinds of rocks, such as granite gneiss from the Canadian Shield region.
To learn more about this fascinating story, pick up a free booklet about the geology of Amnicon Falls at the park office. The booklet will guide you to stops along the walking trails at the waterfalls and explain how the tremendous forces of nature have combined to produce this state park's outstanding scenery. For more information, ask William.Eldred, (715) 398-3000 For more information about the area: Last Revised: Friday December 29 2006
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