File:104-Figure 24.jpg
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Figure 24 -- Silty clay diamicton of the Yorkville Member and silt loam diamicton of the Batestown Member (Lemont Formation) overlie clay loam diamicton of the undivided Tiskliwa Formation at Fox River Stone Quarry, St. Charles, Illinois. The diamictons are interpreted to be subglacial tills.
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current | ★ Approved revision 17:15, 19 April 2016 | ![]() | 2,000 × 883 (679 KB) | Illex-gron (talk | contribs) | Figure 24 -- Silty clay diamicton of the Yorkville Member and silt loam diamicton of the Batestown Member (Lemont Formation) overlie clay loam diamicton of the undivided Tiskliwa Formation at Fox River Stone Quarry, St. Charles, Illinois. The diamicton... |
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