Micro-WorldGems & Gemology, Spring 2016, Vol. 52, No. 1

Shrinkage “Footprint” in Rose Quartz

John I. Koivula(约翰· I.·科伊武拉)

Footprint-shaped iron hydroxide deposit in quartz

Rose quartz is a widely distributed gem material. The specimen shown in was mined from pegmatites near the village of Tsaramanga, located in the Antananarivo province of Madagascar, and fashioned into a 34.11 ct rectangular step cut. It featured decorative epigenetic iron-colored debris that had been deposited in an extensive surface-reaching fracture. One of these debris patterns vividly calls to mind a dinosaur footprint left behind in soft mud.

It appears that the fine particulate debris was suspended in water and subsequently deposited in the crack as a wet solution. As the water dried, the resulting shrinkage pattern formed as only the particles were left behind, a mechanism very similar to the formation of water spots when raindrops dry on a smooth glassy surface. So now “footprints” joins “fingerprints” in our inclusion lexicon.

John I. Koivula is the analytical microscopist at GIA in Carlsbad, California.

您或许还会喜欢

YMAL GIA Ed
了解校园课程和在线教育
Learn About NextGem
GIA NextGem™ 钻石零售 培训
Explore GIA Laboratory Promotional Offers
探索 GIA 鉴定所的促销优惠
Shop the GIA Store
访问 GIA 商店
Shrinkage “Footprint” in Rose Quartz | Gems & Gemology