A System of Mineralogy Third Appendix to the 5th Ed of Danas Mineralogy

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II. , p. 23. It has been shown that, as previously suggested, the sub- stance called garnierite is not a definite mineral, but consists of a hydrous magriesian sili- cate more or less impregnated with nickel oxide; the amounts of magnesia and nickel vary C. It. , Ixxxii. , 1454, 1876; Ixxxvi. , 684, 1878; Des Cloizeaux, anal, by Damour, Bull. Soc. Min. , i. , 29, 1878; vom Rath, Ber. Nied. Ges. Bonn, Jan. And July, 1878 (analyses by Ulrich and Kiepenheuer) ; Liversidge, Proc. Roy. Soc. N. S. W.... , Dec. 9, 1874, and Sept. 1, 1880. Liversidge calls the commonly occurring dark green unctuous mineral, noumea- ite, and the rarer pale green adhesive mineral, garnierite ; the latter he characterizes as a green-colored halloysite; in the former the NiO varies between 32'52 and 0'24 p. C. , and the MgO between 10-61 and 24 '82 p. C. Similar deposits have been found in Spain, Meissonier, C. R. , Ixxxiii. , 229, 1876.
Gastaldite. See Glaucophane, p. 52.
APPENDIX III. 51 GAY-LUSSITE, Min. , p. 706.


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