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goldierocks said:The geology at Mt William is of course completely different to Hanging Rock.
What is your source for the information that the colouring is caused by chromium and not nickel at Mt William?
I suppose you've got me there, I'm mostly inferring it from the abundance of chromian muscovite (the old 'selwynite') known further up the range. I doubt anyone has tested it. I guess the greenstones do have a relatively high nickel content despite the lack of decent Ni mineralisation so it could well be responsible. I honestly don't know too much about the geology of chrysoprase proper, but that's an interesting question - if both chromium and nickel are present when chalcedony is forming, does one contribute more to the colouration?