The syenite pegmatite locality at Ula became known in the late 1880s because of its occurrence of beautifully schillerising feldspar. The Ula locality includes several pegmatite dikes, one of which is the classic "moonstone" locality. The main mineral in the syenite pegmatites at Ula is a grey cryptoperthite which occurs in individuals up to 20 cm long and often shows sky-blue to greenish yellow schillerising colours. The main locality was protected by law in 1980.
Ref.:
http://home.c2i.net/aolarsen/Pegmatites.htm
|
|
|
Map Reference: 59°1'0"N , 10°11'60"E
Important Disclaimer: This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
Switch between Map and Globe
|
