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On some Minerals from the Sodalite-Syenite in Juliane-haab district, south Greenland*

Published online by Cambridge University Press:  14 March 2018

Joh. Lorenzen
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Extract

It is well known to mineralogists, that Giesecke, who in the years 1806—13 travelled in Greenland, brought home from Julianehaab district some new minerals, which he handed over to the Copenhagen Museums. In 1853-4 Dr. Rink supplied the museum of the Copenhagen University with a large collection of the same minerals, mostly in large and fine specimens, and the same collections hove lately received a most valuable and considerable addition, through the travels of Mr. K. J. V. Steanstrup of the Danish Geological Survey of Greenland. Some of these interesting mino.rals, occurring in the Syenite on both sides of the fjords Tunugdliarfik and Kangerdluarsuk, have already long been known, whereas others had elther been not found there before or at least not analysed or described.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 5 , Issue 23 , November 1882 , pp. 49 - 70
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1882

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Footnotes

*

Translated from Meddelelser fra Grònland, 2det Hefte, Kjoebenhavn, 1881, where a French resumé is given.

References

page 50 note † For further communications, maps, etc., see the paper of Mr. 8teenstruD, in Meddelelser fro Grbnland, etc.

page 51 note ‡ l. c., page 50.

page 55 note 1 l. c.P. 51.

page 63 note * On the occurrence of lievrltc and lepidolite in Greenland, see the remarks of Prof Johnstrup, p. 69

page 64 note † Tschermak, Mineralog., Mittheiluugen 1875, 71.

page 64 note ‡ Journal f. prakt. Chem. 99, 70.

page 67 note * Compare Reutcr's analysis of the lepidollte from Rozena : Fl 4·86, SiO2 50·43, Al2Os28·07,Mn2O3 0·88, Mg.O, 1·42, K O 10·59, Na2, O 1·46, Li2 O 1·23, —98-94, Rammelsberg, Mineralchomie 1875, 521.)

page 68 note * Before this operation the sulphates of sodium and cerium, etc., were dissolved; the solution was precipitated by oxahc acid and the oxalates, when heated, dissolved in hydrochloric acid, which finally was expelled by nitric acid.

page 70 note * Rink: Greenland geograph|sk og statistisk beakreveL Tillceg, p. 162.

page 70 note ‡ Giesecke: Mineralogisk Rebec i Groenlnd. Kjoebenhavn, 1878, p. 16.