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Hand-Carved Oval Blue Calcite

€10,00

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Only 1 in stock!

Hand-cut oval blue calcite cabochons, in two sizes: no.1 (23 × 12 × 6 mm) and no.2 (18 × 10 × 4 mm). Translucent ice-greenish blue with a cloudy effect when held up to the light and visible growth lines.

Item details

Mineral Blue calcite (calcium carbonate, blue variety)
Dimensions no.1: 23 × 12 × 6 mm | no.2: 18 × 10 × 4 mm
Shape and backing Oval; flat back
Finish High polish
Hardness 3 Mohs — we recommend bezel setting; not suitable for daily wear rings or contact with acids
Origin Material acquired from a wholesale lapidary market
Treatment Untreated
Item type Unique piece per variation

This specific piece

The color of this blue calcite ranges from greenish-blue to icy sky-blue with medium translucency: it is not transparent like quartz, but rather diffuses light inward, creating a soft visual depth. The growth lines—parallel lines to the mineral's cleavage planes—are visible on the polished surface, adding a natural geometric structure to the color.

Why blue calcite needs special care

Calcite has three characteristics that differentiate it from quartz and require specific considerations for mounting: 3 Mohs hardness (scratches with a coin), perfect cleavage in three directions (can chip from impact), and solubility in weak acids (lemon, vinegar, prolonged sweat). For jewelry, this means it works very well in pendants and earrings—where impact exposure is minimal—but not in everyday rings without full protection. The closed bezel setting made of 925 silver fulfills the triple function of protecting the edges, reducing lateral impact, and separating the mineral from prolonged direct skin contact.

What setting it works for

  • Pendants with closed bezel setting (925 silver) — The most suitable option. The bezel protects the edge and.
  • Earrings with fully enclosed setting — Possible if the setting does not expose the edges of the.
  • Protective wire wrap — Possible if the wire completely covers the perimeter without pressing.

Blue calcite in lapidary tradition

Calcite is one of the most abundant minerals in the Earth's crust, with hundreds of chromatic varieties, but blue calcite of uniform hue and lapidary quality is significantly less common than colorless or white varieties. The main deposits of quality blue calcite come from Mexico (San Luis Potosí), Argentina, and Afghanistan. It has been used in decorative objects and small sculptures since ancient times in Mesoamerican cultures, where blue calcite coexisted with turquoise in mosaic compositions.

In crystal tradition, blue calcite is associated with serene communication and mental calm. Its translucency—which allows light to pass through without fully revealing the interior—is interpreted as a metaphor for discretion and active listening.

The symbolic properties attributed to minerals belong to cultural and historical traditions. They are shared for educational purposes, not as medical advice.

How to recognize genuine blue calcite

Genuine blue calcite shows visible cleavage on the polished surface: fine parallel lines that reflect the mineral's fracture planes. The blue is not uniform but varies slightly between areas. It is acid-sensitive: a drop of dilute hydrochloric acid produces immediate effervescence (release of CO₂), but this destructive test is only performed in forensic gemology, not on finished pieces. The weight is light compared to quartz of the same size due to its lower density.

Frequently asked questions

Is blue calcite the same as blue chalcedony?

No. Blue chalcedony is a variety of quartz (7 Mohs hardness) with a similar appearance but very different physical properties. Blue calcite has a hardness of 3 Mohs.

Why do you not recommend this stone for rings?

With a hardness of 3 Mohs, calcite scratches with everyday materials (a key, a coin, sand). In a pendant, exposure to scratching is minimal; in a ring of.

Is there any color treatment?

No detectable treatment. The blue is natural. Blue calcite owes its color to inclusions of secondary minerals or crystal lattice defects during formation.