File:104-Figure 21.jpg
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Figure 21 -- A gamma B horizon developed in the upper part of a tongue of the Henry Formation, which occurs beneath jointed, calcareous diamicton of the Wadsworth Formation and above diamicton of the Lemont Formation. The gamma B horizon represents an extension of the modern soil profile along joints to form a secondary zone of clay accumulation below the main B horizon.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | ★ Approved revision 17:04, 19 April 2016 | | 2,000 × 956 (702 KB) | Illex-gron (talk | contribs) | Figure 21 -- A gamma B horizon developed in the upper part of a tongue of the Henry Formation, which occurs beneath jointed, calcareous diamicton of the Wadsworth Formation and above diamicton of the Lemont Formation. The gamma B horizon represents an... |
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