Part 33

But is the earth nothing but a cooling mass, "like a hot-water jar such as is used in carriages," or "a globe of sandstone?" and has its cooling been uniform? An affirmative answer to both these questions seems to be necessary to the validity of the calculations on which Sir W. Thomson lays so much stress.

Nevertheless it surely may be urged that such affirmative answers are purely hypothetical, and that other suppositions have an equal right to consideration.

For example, is it not possible that, at the prodigious temperature which would seem to exist at 100 miles below the surface, all the metallic bases may behave as mercury does at a red heat, when it refuses to combine with oxygen; while, nearer the surface, and therefore at a lower temperature, they may enter into combination (as mercury does with oxygen a few degrees below its boiling-point) and so give rise to a heat totally distinct from that which they possess as cooling bodies? And has it not also been proved by recent researches that the quality of the atmosphere may immensely affect its permeability to heat; and, consequently, profoundly modify the rate of cooling the globe as a whole?

I do not think it can be denied that such conditions may exist, and may so greatly affect the supply, and the loss, of terrestrial heat as to destroy the value of any calculations which leave them out of sight.

My functions as your advocate are at an end. I speak with more than the sincerity of a mere advocate when I express the belief that the case against us has entirely broken down. The cry for reform which has been raised without, is superfluous, inasmuch as we have long been reforming from within, with all needful speed. And the critical examination of the grounds upon which the very grave charge of opposition to the principles of Natural Philosophy has been brought against us, rather shows that we have exercised a wise discrimination in declining, for the present, to meddle with our foundations.

FOOTNOTES:

On Geological Time. By Sir W. Thomson, LL.D. Transactions of the Geological Society of Glasgow, vol. iii.

The Theory of the Earth, vol. i. p. 173, note.

Ibid. p. 281.

Ibid. p. 371.

The Theory of the Earth, vol. i. p. 200.

The Theory of the Earth, vol. i. pp. 16, 17.

The Theory of the Earth, vol. i. p. 223.

Principles of Geology, vol. ii. p. 211.

Principles of Geology, vol. ii. p. 613.

"Man darf es sich also nicht befremden lassen, wenn ich mich unterstehe zu sagen, dass eher die Bildung aller Himmelskoerper, die Ursache ihrer Bewegungen, kurz der Ursprung der ganzen gegenwaertigen Verfassung des Weltbaues werden koennen eingesehen werden, ehe die Erzeugung eines einzigen Krautes oder einer Raupe aus mechanischen Gruenden, deutlich und vollstaendig kund werden wird."--KANT'S Saemmtliche Werke, Bd. I. p. 220.

Grant ("History of Physical Astronomy," p. 574) makes but the briefest reference to Kant.

"Allgemeine Naturgeschichte und Theorie des Himmels; oder Versuch von der Verfassung und dem mechanischen Ursprunge des ganzen Weltgebaeudes nach Newton'schen Grundsatzen abgehandelt."--KANT'S Saemmtliche Werke, Bd. i. p. 207.

Systeme du Monde, tome ii. chap. 6

Kant's "Saemmtliche Werke," Bd. viii. p. 145.

Sir William Thomson implies (loc. cit. p. 16), that the precise time is of no consequence: "the principle is the same;" but, as the principle is admitted, the whole discussion turns on its practical results.

"Untersuchung der Frage ob die Erde in ihrer Umdrehung um die Achse, wodurch sie die Abwechselung des Tages und der Nacht hervorbringt, einige Veraenderung seit den ersten Zeiten ihres Ursprunges erlitten habe, &c."--KANT'S Saemmtliche Werke, Bd. i. p. 178.

Sir W. Thomson, loc. cit., p. 14.

Loc. cit., p. 27

Ibid.

It will be understood that I do not wish to deny that the earth's rotation may be undergoing retardation.

Loc. cit., p. 20.

Loc. cit., p. 24.