Teardrop rose quartz cabochons, 23 to 28 mm sizes. Soft pink with the characteristic hazy translucency of rose quartz. Selected from a wholesale lapidary market.
Piece Details
| Mineral |
Rose quartz (SiO₂, pink variety) |
| Dimensions |
no.1: 28 × 18 × 6 mm · no.2: 23 × 19 × 6 mm · no.3: 26 × 18 × 8 mm |
| Shape and Back |
Teardrop, flat polished back |
| Finish |
Mirror polish |
| Hardness |
7 Mohs — suitable for rings and pendants; bezel setting recommended for maximum protection |
| Origin |
Brazil |
| Treatment |
No treatment |
| Piece Type |
Available in 3 sizes (each variant as a single piece) |
This specific piece
Three sizes in one offer: 28×18×6 mm, 23×19×6 mm and 26×18×8 mm. Each is cut from a different fragment, with the pink color distributed uniquely in each piece. Size no.2 (23×19 mm) is the most compact — almost oval proportion — and is ideal for small pendants or earrings. Sizes no.1 and no.3 have a more pronounced teardrop silhouette, with a clearly defined point.
How the color of rose quartz forms
The pink color of rose quartz is not due to a single agent, but rather, depending on the type of deposit, to two different mechanisms. The most frequent is the presence of microscopic fibers of dumortierite or rutile incorporated into the quartz lattice during crystal growth in pegmatites — these fibers scatter light and give the pink hue with the characteristic slight turbidity. In less common deposits, color centers generated by natural irradiation produce a more transparent pink. Brazilian rose quartz, the source of most market material, predominantly corresponds to the first mechanism, which explains its hazy appearance and lack of distinct cleavage.
What mounting it works for
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Bezel setting (925 silver or other precious metals) — the teardrop silhouette fits well into shaped bezels.
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Pendants with silver mounts — the elongated proportion of the teardrop flows naturally.
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Statement rings — larger sizes work as a center stone in.
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Wire wrap — an alternative for those who work with wire settings; the silhouette in.
Rose quartz in lapidary tradition
Rose quartz appears in archaeological records from ancient Egypt as a material for amulets and toiletry items since at least 800 BC. Classical Greece and Rome associated rose quartz with Aphrodite/Venus: according to mythology, the pink color of the stone arose when Aphrodite wounded herself on a thorn bush while running to save Adonis, and her blood stained the white quartz. This narrative transformed rose quartz into a symbol of love that transcends pain. In modern lapidary, it is one of the most widely used stones precisely because of its interpretation of compassion and self-esteem — a stone that the jeweler gives and the wearer wears with clear intention.
The symbolic properties attributed to minerals belong to cultural and historical traditions. They are shared for educational purposes, not as medical advice or a substitute for professional care.
How to recognize genuine rose quartz
Authentic rose quartz has a soft, hazy translucency when held up to light — it is not transparent like rock crystal, but rather slightly cloudy due to the fibrous inclusions that give it its color. The color is homogeneous but subtle, never saturated; if you see a very intense and uniform pink, it is likely dyed glass or synthetic quartz. A simple test: glass is cold to the touch and heats up more slowly than real mineral. The quality of the cut in a genuine cabochon is also noticeable: the edges are refined without flat spots and the polish is uniform without dull areas.
Frequently asked questions
Is it genuine rose quartz or glass/synthetic?
Genuine rose quartz from Brazil. No formal gemological certification, but the optical characteristics — hazy translucency, homogeneous and soft pink, no internal bubbles — are consistent with rose quartz.
What mounting do you recommend?
Bezel set in 925 silver for the best protection. With 7 Mohs, rose quartz is suitable for daily wear in rings and pendants, but the bezel protects the point.
Is it treated?
No detectable treatment. The pink color comes from microscopic fibrous inclusions (likely dumortierite/rutile) formed during the natural crystal growth in pegmatite.