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Nov 2013 - Nettlebed
Pudding stone - conglomerate of rounded flint pebbles in a sand and quartz matrix, probably 50M years old (formed in desert conditions).
Pudding stone - conglomerate of rounded flint pebbles in a sand and quartz matrix, probably 50M years old (formed in desert conditions).
Christmas Common - profile 1.6m deep - highly ferruginous.
Top 30cm is bioturbidity layer (soil); then 1m red (iron); lower layer less oxidised material