
Max
Most probably a magnesium-rich vein polluted in iron oxides (or magnesite) on the matrix, judging by the luster and fracture shown in the pic!cyprusmax47 wrote: ↑Sun Jan 06, 2019 8:41 am It is not only gypsum crystals and quartz what one can find searching for treasures in our Paphos area... This nice specimen I found in an abandoned little mining area near Marathounta.
Max
Most probably a magnesium-rich vein polluted in iron oxides (or magnesite) on the matrix, judging by the luster and fracture shown in the pic!
Would agree with your assessment - the rock looks like a serpentinite which is a hydrothermally altered ultramafic mantle rock. You can still vaguely recognise the original mineralisation consisting of mainly olivine and pyroxene.
Thank you Andreas, concerning Magnesite: where I found the "Gold Stone" was an abandoned small mine and there were large veins of the example piece you can see on the following photos. Could you confirm that it is Magnesite?Lofos-5 wrote: ↑Mon Jan 07, 2019 8:27 pmMagnesite is normally snow white - but tiniest impurities from any heavy metals can cause all sorts of colours. But then again, on the other hand, it could be a completely different mineral that covers your rock too- that's geology for you, not an exact science...
A.
cyprusmax47 wrote: ↑Mon Jan 07, 2019 9:21 pmThank you Andreas, concerning Magnesite: where I found the "Gold Stone" was an abandoned small mine and there were large veins of the example piece you can see on the following photos. Could you confirm that it is Magnesite?Lofos-5 wrote: ↑Mon Jan 07, 2019 8:27 pmMagnesite is normally snow white - but tiniest impurities from any heavy metals can cause all sorts of colours. But then again, on the other hand, it could be a completely different mineral that covers your rock too- that's geology for you, not an exact science...
A.
Max
Thanks Andreas! Ι must get this shop asap, as my wife gets angrier with every extra rock I bring to our appartment
MikeH wrote: ↑Tue Jan 08, 2019 1:39 pm Some good and interesting photos/specimens!
I agree with serpentinized ultramafic, and quite probably (hydro/)magnesite (best examples I have seen in Cyprus).
And the last one appears to be quartz, exhibiting a drusy covering on a primarily botryoidal form.
Just to be clear:
- Serpentine is a mineral, serpentinite is a rock dominated by serpentine.
- Pyrites has a range of appearances: finely granular to prominently macrocrystalline (and the crystals can show various habits, eg.cubes, pyritohedra); gold to silver coloured depending on other elements present in the FeS2 structure, eg. arsenic (and it grades into chalcopyrite and bornite, which add purple-red-blue to the spectrum).
In general one can't ID a mineral from a photo or just visually with your eyes; it needs consideration of density, hardness, microscopic examination of thin translucent sections (including use of polarized light) and maybe chemical tests. Macro-visual factors are important as well, eg. colour, lustre, crystal habit and form, and in many cases visual characters alone can allow the experienced geologist to make a good stab at an ID (hence my suggesting 'quartz' above). Other factors such as geological context, associated mineralogy and lithology, smell, phosphorescence can also help.
The whole issue of ID has an underlying complication: we may have simple names for minerals, but nature is rarely as simple. Many minerals have varied compositions, resulting in their appearances varying a lot. In some groups of minerals, one mineral may grade into another, so it can be very difficult to make a confident ID. Also, rocks are generally composed of more than one mineral, which can lead to confusing results when trying to use density, eg., as a determinant.
Much scope for debate!
//Mike