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Thick surface layer of undecomposed
acidic litter - like pine needles - called 'mor'.
Large zone of eluviation (Washed out layer). Very heavy leaching
Deeper layers are darker as minerals are reprecipitated lower down. Zone of illuviation (B) ('washed in' layer) May be an iron pan - so many iron minerals collected that it impedes drainage. Typical of Upland Britain on Moorland or under Coniferous Forests.
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