Tourmaline
Paprok Watermelon Tourmaline Crystal Afghanistan
Paprok Watermelon Tourmaline Crystal Afghanistan
Description
Description
A slender column of olive green fading into warm brown with a soft pink cap, this Paprok tourmaline shows why the mountains of Afghanistan are treasured by collectors. Its deep vertical striations catch the light like folds of silk, and crystals with this much color play are never easy to find. Read more below to discover how this beautiful crystal formed in the Earth as well as the metaphysical qualities of the stone. The crystal was displayed with “thumb tack” putty for photography ... the same stuff that your 4th grade teacher stuck papers to the wall with. There is no trace of the non toxic putty left on the crystal when it ships to you. Authenticity guaranteed.
- Locality: Paprok, Kunar, Afghanistan
🌏 Geology of Tourmaline from Paprok, Kunar, Afghanistan.
The tourmaline from Paprok comes from the Hindu Kush, a rugged range built by the long collision between the Indian and Eurasian tectonic plates, a process that thickened the crust, heated it and produced granite magmas that rose and cooled slowly in the mountains of eastern Afghanistan. As these magmas crystallized, the last fluids left over became unusually rich in water, boron and lithium, and they collected in granitic pegmatites, coarse grained veins and pockets where minerals can grow large and well formed. Tourmaline from this setting is elbaite, the lithium rich member of the family, and it grew slowly from these fluids inside open cavities. Because a crystal grows along its length over time, its color zoning acts like a diary of the fluid chemistry at each stage: iron and titanium tend to favor green and brown tones while manganese favors pink, so a crystal that moves from brown through green to pink records a shift in the pocket environment as the fluid evolved. The fine lines running down the sides are growth striations, a natural signature of tourmaline that forms parallel to the crystal’s long direction. As far as I know the pegmatites of this region formed during the Cenozoic, though exact ages vary by deposit and are still debated. Today the area remains tectonically active, and the 2025 Kunar earthquake was a reminder that the same forces that built these mountains are still moving beneath them. Mining here is done at high altitude in remote terrain and access can be difficult, which is part of what makes a well colored Paprok crystal so special.
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