Page:The Formation of Vegetable Mould through the Action of Worms (1881).djvu/161

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Chap. III.
BROUGHT UP BY WORMS.
147

von Haast has described[1] a section near the coast, consisting of mica-schist, "covered by 5 or 6 feet of loess, above which, about 12 inches of vegetable soil had accumulated." Between the loess and the mould there was a layer from 3 to 6 inches in thickness, consisting of "cores, implements, flakes, and chips, all manufactured from hard basaltic rock." It is therefore probable that the aborigines, at some former period, had left these objects on the surface, and that they had afterwards been slowly covered up by the castings of worms.

Farmers in England are well aware that objects of all kinds, left on the surface of pasture-land, after a time disappear, or, as they say, work themselves downwards. How powdered lime, cinders, and heavy stones, can work down, and at the same rate, through the matted roots of a grass-covered surface, is a question which has probably never occurred to them.[2]

  1. 'Trans. of the New Zealand Institute,' vol. xii., 1880, p. 152.
  2. Mr. Lindsay Carnagie, in a letter (June 1838) to Sir C. Lyell, remarks that Scotch farmers are afraid of putting lime on ploughed land until just before it is laid down for pasture from a belief that it has some tendency to sink. He adds: "Some