Glacial Erratic Boulders
GeoT Geography | Glacial Erratic Boulders | The Ultimate Erratic? | Ultimate Erratic -- Page 2 | Glacial Landforms -- 1 | Glacial Landforms -- 2 | Glacial Landforms -- 3 | Glacial Landforms -- 4 | Loess and Sand Dunes | Hoopeston's Location | Landscape of Northern Vermilion County | Penfield Illinois
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Boulders such as this are a common sight over much of northeastern Illinois.
They are called Glacial Erratics. 'Erratic' because they are different than the local bedrock.
Many are specimens of Igneous or Metamorphic rock carried by the glaciers from exposures of the Canadian Shield.
Some are Sedimentary rock gouged from what is now the floor of Lake Michigan.
Click the photo for more information from the Illinois State Geological Survey
Erratics of various sizes are often used for landscaping.
Erratics are not particularly the farmer's friend
-- each spring a new crop of erratics appears in
the fields due to the frost action throughout the winter.
Piles such as this one make a great place to make
a rock collection.
Thanks to the glaciers, we have a huge and varied
selection of all 3 rock classes.
This erractic shows glacial scouring and flattening.
Neighbor Marty uses erratics to
keep traffic on the street.
Some erratics are used as monuments.
Note the layers of feldspar injected
into the granite.
Creative use of an erratic in Flatville, Illinois.
Erratics make attractive landscaping.
Flattened sides with scratches
Quartzite Conglomerte with red pebbles of Jasper.
One of the more unusual erratics to be found.
(The larger specimen appeared from till when a water line
was being installed)
The bedrock outcrop of this quartzite has been located in
Click photo for more information.
Photos of erratics located at Ten Mile Grove
(Erratic at a parking lot
Chemical weathering causes exfoliation in a basic igneous erratic.
The dark ferro-magnesium minerals in this (Diabase?) weather more quickly than those in lighter acidic granites.
The majority of this rock is composed of augite and hornblende -- among the first minerals to crystallize from a cooling magma.
Exposed at the surface, they encounter conditions extremely unlike those in which they formed -- in an attempt to regain chemical 'balance' -- weathering occurs rapidly.
Without question, the strangest erratic I have ever observed.
Is this a tillite -- or possibly an impact breccia?
Canada was impacted by meteors in the geologic past -- it is difficult to imagine some of the resulting rock material has not been transported into Illinois.