VI. On the Parasitic Formation of Mineral Species, depending upon Gradual Changes, which take place in the Interior of Minerals, while their External Form remains the same

William Haidinger Esq.

doi:10.1017/S0080456800021852

VI. On the Parasitic Formation of Mineral Species, depending upon Gradual Changes, which take place in the Interior of Minerals, while their External Form remains the same

Published online by Cambridge University Press: 17 January 2013

William Haidinger Esq.

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Every mineralogist is conversant with some of the facts relative to the subject of this paper. Some of the observations enumerated, are comparatively new, as the attention of naturalists has been only of late more particularly directed towards these facts. Others, which I have had an opportunity of collecting myself, I trust will not be considered uninteresting, as they tend materially to rectify certain ideas connected with the determination of the mineralogical species, the most important branch of natural-historical research.

Type: Research Article
Information: Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 11 , Issue 1 , 1828 , pp. 73 - 113

DOI: https://doi.org/10.1017/S0080456800021852 [Opens in a new window]
Copyright: Copyright © Royal Society of Edinburgh 1828

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References

^{page 76 note *} Edinburgh Journal of Science, vol. iv. p. 301.

^{page 81 note *} Traité de Minéralogie, p. 158.

^{page 82 note *} Traité, 2de edit. t. iii. p. 503.

^{page 83 note *} Philosophical Transactions for 1826, p. 55.

^{page 88 note *} Treatise on Mineralogy, Transl. vol. i. p. 439.

^{page 93 note *} Memoirs of the Wernerian Natural History Society, vol. iv. p. 508.

^{page 95 note *} Leonhard's Handbuch der Oryktognosie, 2d edit. p. 293.

^{page 98 note *} Cristallographie, vol. iii. p. 400.

^{page 98 note †} Edinburgh Journal of Science, vol. iv. p, 41.

^{page 104 note *} Beudant's Mineralogy, p. 333. & 363.

^{page 105 note *} Edinburgh Journal of Science, vol. i. p. 380.

^{page 112 note *} Denkschriften der Akademie der Wissenschuften zu München für 1818 und 1819.

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VI. On the Parasitic Formation of Mineral Species, depending upon Gradual Changes, which take place in the Interior of Minerals, while their External Form remains the same

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