LCGHS enjoy hearing the meaning of prairie and central Illinois geologic history
 

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[October 25, 2018]   LINCOLN - When we think of a biography, it usually conjures up the story of a person’s life in a book sitting on a library shelf. The Logan County Genealogical and Historical Society invited New Holland resident Jim Struebing to present a biography of Illinois and Logan County in geologic terms at their monthly meeting Monday evening.

Struebing is a Master Gardener and Master Naturalist and knows the land of central Illinois.


Logan County is at the heart of the tall grass prairie in Illinois.

“Illinois is known as the prairie state, but not everyone knows where that name came from,” said Struebing. When the first French traveled to Illinois in the 16th and 17th centuries, they saw a landscape that is very different from what we see today. Those explorers saw a seeming ocean of tall grass waving in the wind when they first arrived, like the waves on the sea. There were no trees in central Illinois on the very flat land. The word prairie is a French word to describe the illusion of waves that stretched before them.



But what created this topography?

The glacial period of the earth when the mountains of ice moved south out of what is now Canada created the very flat areas of Illinois. The massive weight of the Wisconsin and Illinois glaciers moving forward and back as they grew and melted scraped the land flat creating our current landscape.

The glaciers also ground up the rock in their way and created gravel. When the glaciers retreated, they left a flat land in most of Illinois. It is easy to see where the glaciers ended their march south. The descending land between Atlanta and Lincoln marks the so-called terminal moraine of the Wisconsin glacier, the farthest south it traveled. The descent of topography on Interstate 155 near Delavan is the end of the Illinois glacier. The result of glacial movement was the flat land covered with crushed rock. The Illinois glacier moved the farthest south of the two.

Once the glaciers retreated north, melting because of the warming climate, there were some spruce trees left in their wake. The land was a sort of tundra, or frozen ground.

The next change to occur was wind from the west blowing fine silt into the area. This silt was called loess and created the rich soil in central Illinois, covering the gravel sometimes to a depth of 200 feet.

As the climate warmed, the spruce trees died out and the first of the grasses started to grow on this flat land, between eight and ten thousand years ago.


The center of the United States was once a sea of prairie grass from Ohio to a swath of states extending from Canada to Texas.

Because of rain fall totals, Illinois, Indiana and Ohio had the tallest of the grasses growing on their land. The states west of Illinois had shorter grasses, while the grass in Nebraska and Kansas was shorter yet, due to reduced rainfall.

At one time, Illinois had twenty-two million acres of grassland within its borders. Only a fraction of that remains today. The rich soil, plentiful rain, and frequent fires were the perfect environment for growing these grasses, sometimes reaching heights of eight feet.

 

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Huge herds of buffalo tilled the land with their wanderings, adding to the factors that produced the perfect environment. “There were ten kinds of grasses and thirty types of flowering grasses. The most common tall grasses in the so-called prairie peninsula were Big Blue Stem and Indian Grass,” said Struebing. When the first explorers arrived this is what they saw, the waving grasses that resembled ocean waves, and they named it prairie.

They also found a land of deep rich soil that was very difficult to farm. The grasses had deep roots that bound the soil together.

The land was also very wet, a remnant of the tundra left by the glaciers and the warming climate.

The biography of Illinois now gives way to technology. An inventor named John Deere developed a plow with a sharp smooth metal blade that tore through the soil, and a creative Irishman named Scully came up with a way to drain the land.

The waving grasses of the prairie gave way to the waving corn fields we see today.


The grass prairie is gone forever, but it had many benefits for the environment.

“There are spots of tall grasses in old cemeteries and along old railroad right-of-way, but the conditions that created thousands of years of grasslands in Illinois are gone forever. Only one tenth of one percent of the original millions of acres of grassland remains,” said Struebing.

So the history of Illinois has left us with several benefits that we still enjoy today. The Illinois and Mississippi Rivers are gouged out remnants of the retreating glaciers. The deep bedrock of gravel provides building material. The water flowing through the gravel that is sometimes hundreds of feet deep provides clean drinking water for millions of people.

And the soil in central Illinois, the rich deep soil provides the best farming resource in the world.
 


Jim Struebing is passionate about the prairie and what it provided during its existence. “The factors involved in the development of the tall grass prairie can no longer be replicated, but there is something people can do to honor this part of Illinois’ history. I have several small plots of prairie grasses in my yard and some flowering prairie grass,” he said. Anyone can have a small piece of Illinois history in their yard. And the state of Illinois has discovered the benefits of slow growing prairie grass. The sides of interstates are seeded with it and now require less mowing.

The flora of Illinois’ early biography can still be with us.

The Logan County Genealogical and Historical Society meets the third Monday of each month at their research facility across from the newly remodeled Lincoln Depot at 6:30 p.m. The public is invited to attend, and they always have an interesting and informative presentation.


[Curtis Fox]

 

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