Locality near Mølland. The pegmatite dyke was in 1960 quarried in 5 different places. Graphic granite dominates the border and the dyke has a coarsegrained interior with large crystals of feldspar. In one part of the pegmatite there is also observed a poorly developed cleavelandite-quartz zone.
References:
Neumann, H. (1960): Mineral occurrences in southern Norway. Guide to excursions no A.15 and no. C 12. International Geological Congress XXI session Norden 1960, 18p.
Mineral list contains entries from the region specified including sub-localitiesMineral List:17 entries listed. 9 valid minerals.
Localities in this Region:
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