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Show 230 DISINTEGRATION CHAP. v. CHAPTER V. THE ACTION OF WORMS IN 'filE DENUDATION OF THE LAND. Evidence of the amount of denudation which the land has undergone-Sub-aerial denudation-The deposition of dustVegetable mould, its dark colour and fine texture largely due to the action of worms-'l'he disintegration of rocks by the humus-acids-Similar acids apparently generated within the bodies of worms-The action of these acids facilitated by the continued movement of the particles of earth-A thick bed of mould checks tbe disintegration of the underlying soil and rocks. Particles of stone worn or triturated in the gizzards of worms-Swallowed stones serve as mill-stones-The levigated state of the castings-Fragments of brick in the castings over ancient buildings well rounded. 'l'he triturating power of worms not quite insignificant under a geological point of view. No one doubts that our world at one time consisted of crystalline rocks, and that it is to their disintegration through the action of air, water, changes of temperature, rivers, waves of the sea, earthquakes and volcanic outbursts, that we owe our sedimentary formations. These after being consolidated and sometimes CHAP, v. AND DENUDATION. 231 recrystallized, have often been again disintegrated. Denudation means the removal of such disintegrated matter to a lower level. Of the many striking results due to the modern progress of geology there are hardly any more striking than those which relate to denudation.· It was long ago seen that there must have been au immense amount of denudation; but until the successive formations were carefully mapped and measured, no one fully realised how great was the amount. One of the first and most remarkable memoirs ever published on this subject was that by Ramsay,* who in 1846 showed that in Wales from 9000 to 11,000 feet in thickness of solid rock had been stripped off large tracks of country. Perhaps the plainest evidence of great denudation is afforded by faults or ?racks, which extend for many miles across certain districts, with the strata on one side raised even ten thousand feet above the corresponding strata on the opposite side ; and yet there is not a vestige of this gigantic displacement visible on the surface of the • "On the denudation of South Wales," &c.,' Memoirs of the Geological Survey of Great Britain,' vol. i., p. 297, 1846, |
