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IV.—Additional Notes on the Growth of Soil

Published online by Cambridge University Press:  01 May 2009

Extract

In the former notes “On the growth of soil,” I omitted to speak of the labours of the ants—these workers, although such pigmys in this country, and, therefore, compared with the earth-worms, less capable, individually, of work, are so numerous and energetic, that in the special places to which they resort, their yearly work is much more conspicuous than the annual worm-work; but the animals operate in different places, for while the earth-worm luxuriates in rich highly-cultivated land, the hill-building-ant loves a dry, sandy or peaty soil. In the spring the ants may be observed beginning their work, and from that time they carry on their operations all through the summer, to the late autumn, or early winter. On a moor they raise hillocks scattered promiscuously about over the ground, getting closer and closer together as the colonies increase. But where the ants are most useful is in places where crags and large stones are mixed up with patches of sandy peat. In such a locality they will always build on a rock, the foundation of their habitation being at its junction with the soil. These ants seldom raise their structures as high as the moorland ants, but they make up in extent for absence in height, and by this means the rocks are gradually covered with soil and vegetation; for, on account of the season of the year at which they build, the growth of the plants keeps pace with the formation of the ant-soil, and protects it in a great measure from “Meteoric abrasion.” During the winter, however, the shape of the ant-hills is somewhat modified, but the matted roots of the plants preserve the major part of the soil which will thus remain, forming an envelope for the rock.

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Original Articles
Copyright
Copyright © Cambridge University Press 1869

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References

page 348 note 1 Geological Mag., June, 1869, page 260.Google Scholar

page 348 note 2 When I proposed chemico-fluvial denudation as a better name than the vague term sub-aërial denudation, I had quite forgotten that Mr. Scrope some time since, called the same action Meteoric abrasion.—[Geology and Extinct Volcanoes of Central France.] This name is evidently so much superior to any since proposed, that I am surprised it has not been universally adopted.

page 349 note 1 Memoirs Geol. Survey of Ireland, Explanation of sheet 105, p. 6.Google Scholar

page 349 note 2 At the present time there is an artificial drain cut towards the east through the bog. When the lake was first visited in the early summer this drain had just been opened, about five feet deep, to make up the fences, and although it did not reach to the bottom of the peat, yet it was lower than the western embouchure, and carried off all the summer water. At a subsequent visit, nearly two years afterwards, the eastern cut was choked up by aquatic plants, among and behind which a peaty sediment had been deposited, and thereby formed a dam, which drove the summer water to flow westward, to the Boliska.

page 350 note 1 Keller's Lake Dwellings, p. 367 footnote.Google Scholar