From the Bedrock Up
By Alan King

     If you've ever looked at the road cuts in our area, you know that Greene County sits upon layers of limestone and shale.  About 500 million years ago, we used to be at the bottom of a warm,  shallow sea. The geologic plate we are riding on was then south of the Equator and our limestone was formed through the gradual buildup of billions of tiny sea creatures that lived in a warm, shallow sea.  This all got buried until millions of years later when the Appalachian mountains began to form, forcing these rock layers upward.
     The local rivers ran northwest, eroding away the upper layers until the limestone began to peek out here and there.  Everything went along easily for a few more millions of years after that, but just when it looked like everything was always going to be the same, along came a really cold winter.  Then another ... and another ... until the winters barely let up and there didn't seem to be any summer.  The snow that fell one winter just lay there all year and never melted.  This was about 2 million years ago.
     As you can imagine, in a few years you've got a pretty fair amount of snow on the ground.  Snow when it gets really thick starts to act a little less like a solid and a little  more like silly putty.  In a few more hundreds of years, you can imagine that the snow has gotten hundreds and hundreds of feet thick. The biggest pile of ice and snow was in what is now Canada, and we were right in the path of the ooze.  A glacier.
 Imagine the Eiffel Tower at King's Island.  It’ s about 400 feet tall, and about 12 or 13 of them end on end would be about a mile high.  That's how thick the snow had gotten.  Every winter the front edge of the glacier moved a few miles closer to our area.  And every summer it melted back a little.
     The flow of the Teays River was dammed up by all this ice and formed Lake Tight, which covered an area nearly as big as Lake Erie in southern Ohio and parts of West Virginia and Kentucky.  When it became too full, all the backed up water began to flow southwest, forming the beginnings of the Ohio River.
 Meanwhile, the glaciers had bulldozed millions of tons of rock from the face of Canada, scooped out the basins where the Great Lakes would eventually puddle, and even bent the crust of the Earth down from the sheer weight of the snow and ice.  Then whatever was making it so cold changed.  The summers began to get warmer, the winters less killer cold, and the ice that pushed forward in the winter managed to melt back by the end of each summer.
     All those tons and tons of rock had been ground down to pebbles, sand and small boulders and with the glacier no longer pushing them south, they had to end up somewhere.  Take a look out your window at the hills and rolling fields around you.  That's glacial debris from Canada.  A ridge formed along the edges of a glacier is called a moraine.  The city of Moraine is named for them.
     Drive north past Jamestown or Cedarville and you will notice that the farm country is remarkably flat.  A million ton bulldozer had just scraped across the land.  The Teays River was now buried under many feet of gravel and silt and the great Ohio River was now flowing South instead of North.  This entire cycle took place at least three times.  The first was about 2 million years ago. the second around 200,000 years ago, and the most recent (and last, we hope) was over around 10 or 20,000 years ago.
     Here's one explanation of geologic time that helps to put these things in perspective.  Imagine that you are about 50 years old, and you were born about the time that the first primitive animals swam in the seas.  When you were 20, the world was covered in trees that formed all the coal in Pennsylvania and Kentucky.  Near your 30th birthday, about 1980, dinosaurs began to roam around.  Around 1994, something fell from the sky, covering the Earth in clouds and dust.  Most of the plants died and the dinosaurs that depended on them became extinct.
     In 1995, a few mammals began to appear, and by 1998 there were horses, apes, dogs, and bears.  Last June, early humans arrived, but their lives got tough when the first Ice Age started this March.  The last glacier just melted last night.  The Pyramids were assembled this morning.  The “Little Ice Age” from 1200 to 1700 AD happened about 15 minutes ago.  Xenia was founded and Ohio became a state about the time you started reading this, and TV was invented about 3 minutes ago.
     We talk today about global warming in relation to the fossil fuels that we burn in our homes and automobiles.  We worry that we are causing a greenhouse effect and could alter the climate of the Earth.  In my lifetime, I have seen the weather in Xenia change dramatically.  But given the long view of geologic history, I'm not sure that anything we do can compare with the formidable powers of our planet to change itself.  That doesn't mean we should continue to trash the planet, but sometimes it helps to put things in perspective.  © 2000 Alan D. King
 

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