In what Buffon's theory of the earth and Dr Hutton's agree, and in what they differ, § 426, 427. Great merit of Buffon, notwithstanding his errors, § 428.
Note xxv.—Figure of the Earth.
Physical cause of the earth's oblate figure not obvious from its present condition, § 429. How explained by the Neptunists, § 430. Examination of their solution, § 431, 432. Contradiction implied in it, § 433. Insufficiency of Buffon's explanation, § 434. Of the principle on which the oblateness of the earth may be accounted for in Dr Hutton's theory, § 435. Of the changes that would happen in the figure of a terraqueous body like the earth, supposing it ever so irregular, § 436, 437, 438. Two different causes of change, ib. Ultimate figure, that by which the causes of change are best resisted, § 439. Spheroidal figure, never perfectly acquired, § 440. Agreement of this theory with observation, § 441. Probable extension of the system of waste, and renovation to the other planets, § 442, 443. Confirmation from the system of Saturn, § 444, 445.
Note xxvi.—Prejudices relating to the Theory of the Earth.
Alleged by some that a theory of the earth ought not at present to be attempted, § 446. The quick succession of geological theories has partly arisen from their object being misunderstood, § 447. A succession of theories is often a continued approximation to the truth, § 448. The more various the phenomena of any class, the greater the chance of discovering their true cause, § 449. Reason to think that the leading facts in geology are now known, § 450, 451. A tendency may be observed in geological systems to approach to one another, and to the Huttonian, § 452. Example from that of Saussure, § 453,—of Dolomieu, § 454, 455. The discoveries of Dr Black were necessary for understanding the true theory of the earth, § 457. Use of theory in matters of observation, § 458, &c.
