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Ice fall at Ottawa Canyon in Starved Rock State Park
Ice tendrils form from the top of the falls which continue until they eventually join the base mound.
The ice then forms a continuous column, but the character of the each type remains distinctive at the interface of the two.
© 2002 - 2024 by Thomas J. Robbins, all rights reserved. Contact tmrobbins@comcast.net for permission to use.