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The very full and able review of Dr. Sterry Hunt's paper on “The Geological History of Serpentine,”1 gives me an opportunity, of which I have been for some time desirous, of commenting on certain parts of it relating to my investigations of the typical rock which bears that name. In commenting adversely upon these, I must not be supposed to express a difference of opinion in regard to every part of the paper, because there are many relating to the Archæan schists with which I am in general agreement.
page 406 note 1 See page 276 of the present volume.
page 407 note 1 Quart. Journ. Geol. Soc. vol. xxxiii. p. 884; vol. xxxix. p. 1. See also vol. xxxiv. p. 770; vol. xxxvii. p. 40.Google ScholarGeol. Mag. Dec. II. Vol. VI. p. 362; Vol. VII. p. 538.Google Scholar
page 408 note 1 The italics are mine.
page 410 note 1 Serpentine under pressure sometimes assumes a schistose aspect. This has added to the difficulties of distinguishing the rock from simulative forms.
page 411 note 1 Science, 1883, p. 255.