Teardrop-shaped rose quartz cabochons, sizes from 29 to 34 mm. Soft pink with the characteristic cloudy translucence of rose quartz. Selected from a wholesale lapidary market.
Item details
| Mineral |
Rose quartz (SiO₂, pink variety) |
| Dimensions |
no.1: 29 × 21 × 7 mm · no.2: 30 × 19 × 8 mm · no.3: 34 × 17 × 6 mm |
| Shape and back |
Teardrop, flat polished back |
| Finish |
Mirror polish |
| Hardness |
7 Mohs — suitable for rings and pendants; closed bezel setting recommended for maximum protection |
| Origin |
Brazil |
| Treatment |
No treatment |
| Item type |
Available in 3 sizes (each variant as a unique piece) |
This specific piece
Three sizes in the 29-34 mm range: no.1 at 29×21×7 mm, no.2 at 30×19×8 mm, and no.3 at 34×17×6 mm. Size no.3 is the most elongated — a slender 34 mm long teardrop — ideal for pendants where stone length is the desired effect. Sizes no.1 and no.2 have more balanced proportions and are well-suited for both pendants and statement rings.
How rose quartz color is formed
The pink color of rose quartz is not due to a single agent, but rather, depending on the type of deposit, to two distinct mechanisms. The most common 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. Rose quartz from Brazil, the source of most market material, predominantly corresponds to the first mechanism, which explains its cloudy appearance and lack of inherent cleavage.
What setting it works for
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Closed bezel setting (925 silver or other precious metals) — the teardrop silhouette fits well in 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 well as a center stone.
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Wire wrap — an alternative for those working with wire settings; the silhouette.
Rose quartz in lapidary tradition
Rose quartz appears in archaeological records of Ancient Egypt as material for amulets and toiletry items from at least 800 BC. Classical Greece and Rome associated rose quartz with Aphrodite/Venus: according to mythology, the stone's pink color emerged when Aphrodite cut herself on a thorn bush while running to save Adonis, and her blood stained the white quartz. This narrative turned 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 goldsmith gives and the wearer carries 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, cloudy translucence when held up to the light — it is not transparent like rock crystal, but slightly turbid 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 slower than real mineral. The quality of the cut in a genuine cabochon is also noticeable: the edges are finely shaped without flat spots and the polish is uniform without matte 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 — cloudy translucence, homogeneous and soft pink, no internal bubbles — are consistent with rose quartz.
What setting do you recommend?
Closed bezel 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 apex.
Has it been treated?
No detectable treatment. The pink color comes from microscopic fibrous inclusions (likely dumortierite/rutile) formed during natural crystal growth in pegmatite.