420 M. SwEDENSTiERNA on the Corundum of Gdlivara, 



Bournon may be taken perhaps as an instance of the combination 

 in which the red oxide is found in the greatest quantity. 



The minerals which occur at Gellivara, besides the corundum, in 

 the feldspar separating the layers or within them, are chiefly the 

 following. 



1 . White or grayish calcareous spar. 



2. Small calcareous crystals. 



3. Ditto siliceous ditto. 



5» Green glassy actinolite, sometimes crystallized in four-sided 

 prisms. 



5. White pretty hard asbestus. 



6. White yellowish phosphate of lime, nearly of the same colour 



as the corundum, commonly imbedded in a black blueish 

 magnetic ore, forming almost one half of it, and giving 

 to the whole mass a singular appearance. 



7. Red phosphate of lime of a rosy tint and granular form. In 



some of the specimens I brought with me to Paris, I 

 discovered some small but very regular hexahedral prisms 

 of this substance, which I never met with afterwards. 



8. I might also add several varieties of quartz and mica, which 



however mostly form with the felspar either gneiss or 

 granite. 



P. S. Since writing the above memoir I have again examined the 

 Gellivara iron-ore, and have found amongst it some specimens of 

 true emery. 



