0 thoughts on “Mystery spikes”

  1. Since it’s in pegmatitic quartz, my vote is also for tourmaline– tends to be common accessory in various pegmatites in of that part New England (but not always. 🙂 )

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  2. Most likely tourmaline. Was this in a granite? There aren’t too many granites right around Mt. Washington. One thing that is becoming important to my paleostress study from Great Gulf is the occasional mineralization of tourmaline and quartz on joint faces. This was likely a precipitation from warm fluid. The mineral precipitates at something like 170C, off the cuff, and we have some new apatite fission-track data that gives us the cooling/exhumation history of Mt. Washington. Put them together and I can constrain the age of a tourmaline-encrusted joint! There is likely a lot of information in these little aggregates!

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  3. Without getting it under a microscope, I couldn’t tell for sure. I think tourmaline is the most likely, also hornblende is a good choice too. Another thought that came to me is Rutile because I’ve seen some rutile that had a similar crystalline look. Rutile is found in quartz associated with high pressure /temperature rocks – pegmatites, & skarns, Looking at the crystalline structure of the surrounding rock it makes me wonder about that. IThe problem with Rutile is it is not know to be from that area, so it most likely is one of the first two choices.
    http://en.wikipedia.org/wiki/Rutile

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