DESCRIPTION | ||
GEOLOGYHaapaluoma is a lithium pegmatite | ||
VISITS1997-06-22This was the first stop on the 1997 geology trip to Finland. After a good briefing of the geology of Haapaluoma by Markku, we were let loos on the dump piles for about 2-3 hours. Too bad that I used all the time on just one dump pile, I should have taken some more time to examine the surroundings, but I was too occupied with collecting minerals on one dump pile. | ||
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This is a very pure type of microcline. Collected 1997-06-22 (300 dpi, 800x600, k) |
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A sample of microcline pertite. Collected 1997-06-22 (300 dpi, 800x600, k) |
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Spodumene occured in three different forms, this first fresh form in easily cleavable masses, as more corroded crystals ( see next picture ) and in the form of kunzite. This sample is grown around a rubellite. Collected 1997-06-22 (300 dpi, 800x600, k) |
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This is an example of the more corroded spodumene that could be found in Haapaluoma. It consists of a number of separate square crystals with rounded edges. The matrix consists of quartz and clevelandite. Collected 1997-06-22 (300 dpi, 800x600, k) |
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The same sample as above, but with a better view of the square crystal of spodumene. Collected 1997-06-22 (300 dpi, 800x600, k) |
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Rubellite in quartz. Collected 1997-06-22 (300 dpi, 800x600, k) |
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An oncosine vein through feldspar. A very nice specimen, showing a change in the mineral towards the central core. I don't know if it's caused by changes in the lithium concentration or other factors. Collected 1997-06-22 (300 dpi, 800x600, k) |
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