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Rose Quartz Facts

Rose quartz is a macrocrystalline variety of the mineral Quartz (SiO2). Quartz is the most abundant single mineral on earth. It makes up about 12% of the earth's crust, occurring in a wide variety of igneous, metamorphic and sedimentary rocks.

Quartz varieties are commonly separated into two groups based on the size of the individual grains or crystals; macrocrystalline quartz in which individual crystals are distinguishable with the naked eye, and cryptocrystalline quartz in which the individual crystals are too small to be easily distinguishable under the light microscope.

Some of the macrocrystalline quartz varieties are: Amethyst, Ametrine, Cat's-eye Quartz, Citrine, Phantom Quartz, Rock Crystal, Rose Quartz, Rutile in Quartz and Smoky Quartz.

Blue Aventurine Quartz and Green Aventurine Quartz are actually quartzites (a rock, not a mineral) composed essentially of interlocking macrocrystalline quartz grains with disseminated grains of other color imparting minerals.

The cryptocrystalline varieties of quartz may be separated into two types; fibrous and microgranular. Chalcedony is the general term applied to the fibrous cryptocrystalline varieties. Agate is an example of a fibrous cryptocystalline banded chalcedony variety of quartz. Carnelian, Chrysoprase and bloodstone are other chalcedony varieties.

ROSE QUARTZ OCCURRENCE & DIAGNOSTIC FEATURES

Rose Quartz Rough Specimen Rose Quartz Specimen

Natural rose quartz is opaque to translucent macrocrystalline quartz of pink to rose-red color. It normally occurs in the cores of large pegmatites as solid masses of rose colored quartz whose individual crystals have poorly formed boundaries.

Some rose quartz contains microscopic rutile crystals which are oriented at right angles to the c-axis of the rose quartz in three directions, each 120 degrees apart. When viewed at a specific angle with a source of light a star-effect is visible. This is known as asterism.

The color of rose quartz is still not completely understood. It has been said to be due to a number of different minor impurities present in the rose quartz including titanium, manganese and even colloidal gold.
However, recent studies using micro-analytical methods have discovered that the color of massive rose quartz is actually due to microscopic mineral fibers in the rose quartz. X-ray diffraction tests on these microscopic fibers yielded patterns similar to the mineral dumortierite but slightly different, suggesting the possibility of a totally new and as yet unknown fibrous mineral causing the color in massive rose quartz.
The rare transparent euhedral crystals of rose quartz owe their coloration to aluminum and phosphorous impurities. Their pink color is photosensitive and can fade in sunlight.

Rose quartz is recognized by its color, transparency, hardness, glassy luster, conchoidal fracture, occurance and general lack of cleavage.