Glacial Geology | Quaternary Geology Section | Quaternary Geology Section Staff

Omars

Omar photo

The rocks in this photo are a distinctive type of glacial erratic called omars. They were collected from glacial drift in Illinois. The term "omar" refers specifically to an erratic of massive, dark, hard sandstone that contains light-toned (generally buff-colored) soft concretions that commonly weather recessively to leave rounded out depressions in the rock. The source rock (Precambrian Belcher Group) for omars is exposed in the Belcher Islands of eastern Hudson Bay. The occurrence of omars in Illinois indicates a flow path from that area south across Ontario to the Lake Michigan basin. Photo by A.K. Hansel.


















Updated 09/14/2009 CAB

ILLINOIS STATE GEOLOGICAL SURVEY
E. Donald McKay, III, Interim Director

Terms of use         Privacy Statement

© 2009 University of Illinois Board of Trustees. All rights reserved.
For permissions information, contact the Illinois State Geological Survey.