The series of formations in the cliffs of eastern Norfolk, now under consideration, beginning with the lowest, is as follows:--First, chalk; secondly, patches of a marine tertiary formation, called the Norwich Crag, hereafter to be described; thirdly, the freshwater beds already mentioned; and lastly, the drift. Immediately above the chalk, or crag, when that is present, is found here and there a buried forest, or a stratum in which the stools and roots of trees stand in their natural position, the trunks having been broken short off and imbedded with their branches and leaves. It is very remarkable that the strata of the overlying boulder formation have often undergone great derangement at points where the subjacent forest bed and chalk remain undisturbed. There are also cases where the upper portion of the boulder deposit has been greatly deranged, while the lower beds of the same have continued horizontal. Thus the annexed section (fig. 114.) represents a cliff about 50 feet high, at the bottom of which is _till_, or unstratified clay, containing boulders, having an even horizontal surface, on which repose conformably beds of laminated clay and sand about 5 feet thick, which, in their turn, are succeeded by vertical, bent, and contorted layers of sand and loam 20 feet thick, the whole being covered by flint gravel. Now the curves of the variously coloured beds of loose sand, loam, and pebbles are so complicated that not only may we sometimes find portions of them which maintain their verticality to a height of 10 or 15 feet, but they have also been folded upon themselves in such a manner that continuous layers might be thrice pierced in one perpendicular boring. [Illustration: Fig. 114. Cliff 50 feet high between Bacton Gap and Mundesley.] [Illustration: Fig. 115. Folding of the strata between East and West Runton.] [Illustration: Fig. 116. Section of concentric beds west of Cromer. 1. Blue clay. 2. White sand. 3. Yellow Sand. 4. Striped loam and clay. 5. Laminated blue clay.] At some points there is an apparent folding of the beds round a central nucleus, as at _a_, fig. 115., where the strata seem bent round a small mass of chalk; or, as in fig. 116., where the blue clay, No. 1., is in the centre; and where the other strata, 2, 3, 4, 5, are coiled round it; the entire mass being 20 feet in perpendicular height. This appearance of concentric arrangement around a nucleus is, nevertheless, delusive, being produced by the intersection of beds bent into a convex shape; and that which seems the nucleus being, in fact, the innermost bed of the series, which has become partially visible by the removal of the protuberant portions of the outer layers.