File:104-Figure 21.jpg: Difference between revisions
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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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Latest revision as of 17:04, 19 April 2016
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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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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