. The earth in past ages . Fig. n—Belemnites Oweni, an internal shell of a kind f cuttle- fish. The "Guard'' is broken to shew the conical phi cone which penetratea into it. Oxford Clay, earthy limestone. Traced southward by Shot- over, it forms two divisions; and at Weymouth there is the sandy lower calcareous grit well de- fined, and an upper grit or sand which passes up to the Kimeridge clay. In Yorkshire this Oolite extends through the ilowardian Hills by Malton, through the Vale of Pickering to Filey. At Up- ware, on the river ('am, a small reef lull of corals appears to result from
. The earth in past ages . Fig. n—Belemnites Oweni, an internal shell of a kind f cuttle- fish. The "Guard'' is broken to shew the conical phi cone which penetratea into it. Oxford Clay, earthy limestone. Traced southward by Shot- over, it forms two divisions; and at Weymouth there is the sandy lower calcareous grit well de- fined, and an upper grit or sand which passes up to the Kimeridge clay. In Yorkshire this Oolite extends through the ilowardian Hills by Malton, through the Vale of Pickering to Filey. At Up- ware, on the river ('am, a small reef lull of corals appears to result from the Carboniferous lime- stone having furnished calcareous matter to the
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Keywords: ., bookcentury1900, bookdecade1900, bookpublishernewyo, bookyear1902
