This afternoon I spent just over two hours on Gemstone Beach. I arrived at 2.20pm, two hours before low tide. It was 13 degrees throughout the fossick, with a strong breeze. I chatted to a couple from Arrowtown as I left, identifying three or four of the handful of stones they had found.
The hydrogrossular garnets I found today were mainly small and, as with the previous fossick, I spotted very few trace fossil stones. I did find one small poppy jasper and the occasional interesting other kind of stone. Twelve of this afternoon’s finds are featured below.
The largest stone I collected today is this rhodonite. Rhodonite is primarily composed of manganese silicate, its colour varying from light pink to deep red. It is similar in colour to thulite but often features black markings caused by manganese oxides:
Another glassy stone that has been suggested to me is chromite in quartz, two also having been found yesterday:
A black and white stone where I suspect the white material could be hydrogrossular garnet, kind of similar to one I found on Sunday:
I found two small poppy jaspers, the first having a little green epidote in it:
Two finds with different types of brecciation (re-cemented fragmentation), the first the result of tectonic pressures on the whole stone, the second being limited to a vein:
Next are the two largest of my hydrogrossular garnet finds – the first is partly transparent, the second is opaque and very waxy (so that water beads off it quickly):
And now a couple of green-hued stones. The first is what is said to be the typical pistachio-green hue of epidote (though epidote causes a range of greens):
The second is perhaps a form of spotted argillite (Stones Gn2 to Gn31 in this Post are examples of spotted argillite):
A small banded argillite, a good example of an indurated banded mudstone:
Finally, what may be a quartzite specimen:
The next Post in this Series, “A Sense of Wonder: Poppy Jaspers and Exquisite Breccias”, covers my fifth fossick so far at Gemstone Beach this trip. An Index to the Series is here.
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