UMore Park and the Driftless Region
First a couple of notes:
Of the ducklings featured in my last post one was gone within a couple hours of the time I saw them. The rest had disappeared by the next morning. It’s tough out there for little ducks.
I am seeing more deer in the fields. I saw two that looked like twin fawns without spots – is this possible already?
I saw my first firefly of the season May 24th.
I haven’t heard coyotes for quite a while until a pretty active barking session a couple of nights ago.
I’ve noticed the “helicopter” maple seeds are falling — seems like the wrong time of year, do they form and fall twice each summer?
For work last Friday I had to drive to Apple Valley in Dakota county. I needed to check up on a foreclosed town house for a bank.

At one point I drove on County Road 42 where the surroundings shift from rural to suburbs.
Several times previous to this particular trip I’ve noticed big cement structures lining the road, old and abandoned with vines crawling on them. They put me in mind of Easter Island or Stone Henge.

Feeling curious, I turned off on a road that no one else seemed to be turning on. It was wierd, I left city traffic with just one turn. The fields were in varying stages of being over run by box elders, a turkey flew across the road in front of my car. There were many different decaying cement structures, some with crumbling columns that made me think of Rome. Then I saw cement chimneys as big as power plant obsucred by trees.

There was a fence around the area that and a sign, “No Trespassing, regularly patroled by The Dakota County Sherrif”. I was tempted to follow a path worn in the grass that went around the gate and the sign towards the building with chimneys, but refrained from doing so because a speeding ticket from the day before was still fresh in my mind.

A little further down the road I saw another sign, “UMore Park, University of Minnesota “. I kept driving around, this park seemed as big as a city, but there were no improvements. I saw some pole sheds and a couple of cars in the distance and went in that direction. There was a young woman in blue jeans walking along the road. I rolled down my window and asked her, “what is this place?” She was very freindly, smiled and said, “It’s a research facility for the University of Minnesota.” I said, “What was it before that?” Her face clouded over, “A farm?” both of us knew that couldn’t be right.
She directed me to someone else busy working on something with pipes that I couldn’t quite identify. He tells me this place was a World War Two munitions plant that covered 13,000 acres but is now only 8,000 acres. He doesn’t know what the cement structures by the the main road were for. He verifies the park is currently used by the university for farm research.
The mystery is solved but it does not dispel the aura of this place. I think someone should film a movie here.
I leave umore park and come upon a residential street, paved with curbs and traffic circles. But there are no homes on the street, just bare spots where the houses should be. A nearby development ends abruptly almost as if some chemical has been dumped that turns the grass brown and stops houses from growing.
The area I am in, with it’s randomly hilly terrain, is glacial end morain. The road I am on dead ends into a big grassy hill. Over my shoulder a steady stream of cars rushes by, the noise of tires on pavement fills the air.

I park my car so I can climb the hill with my camera. I feel like I shouldn’t be here only because no one else is. The traffic is a block away.

At the top of the hill is a flat spot and then a deep hole, an open gravel pit with a fleet of cement trucks parked in the distance. There is a steep dropoff, but no fence. They must figure no one around here gets out of their car.
No equipment is moving. It’s 4:30 on the Friday of Memorial day weekend. I stay away from the unstable edge. I look down at my feet and see gravel, slightly rounded, different colors and sizes. The side of the pit shows the cross bedding of layers still left from when the gravel was deposited 10,000 years ago.
The last glacial age laid waste to Minnesota. Ice a mile thick flowing like plastic under it’s own weight scraped away soil and rock. It left some of it’s load when the ice melted as the hill I am standing on.
Desert conditions surround a continental glacier because cool, dry density winds come off the ice and evaporate all of the moisture. The wind picks up the fine, rich topsoil and redeposits it as rich farmland, in this case, in far southren Minnesota and Iowa. It is called “loess”.
In many parts of Minnesota Glacial boulders called “erratics” occupy seemingly random places in fields. These rocks lie in fields like boats left by the tide, but instead of water it is ice that has receded. A term that refers to these boulders and other poorly sorted(all sizes and types of material mixed together) soil and rock is “Drift”.

You won’t find any “drift” in Red Wing unless someone hauled it in with a truck. Drift is a glacial feature all over the northern part of north america, but not in Red Wing. We live in an area called “the driftless region”.
At the time I was in school there was little information provided for this phenomenon. It was simply stated that the drifless region remained unglaciated during the last glacial age. It was a piece of trivia memorized for a test that has stuck in my head all of these years because I happen to be from “the driftless region”. Glacial deposits around Red Wing tend to be deposited by melt water, well sorted sand or gravel or mud. We don’t have lakes.
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