. The earth in past ages . 1 1 ,. .â ; -Section from Folkestone i<» Hythe, showing above the fresh-water Weald Clay, the <liviM:is ,,t" the marine Lower ensand, named Atnerfield beds, Hythe be Is, I â »lkestne I n . Hythe and Folkestone, into the Ather- I Clay at the base, which is sometimes a ma- rine esting '»n the Weald Clay, and some* c sharp sand. Secondly, the Hythe beds (or Kentish rag) are alternations f thin bedded limestone and sand with beds of chert. Thirdly, the Sand-ate beds a:c sandy cl at, often green, like the underl]

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Keywords: ., bookcentury1900, bookdecade1900, bookpublishernewyo, bookyear1902