Rock Identifier
Sard (Silicon dioxide (SiO2), microcrystalline quartz)
mineral

Sard

Silicon dioxide (SiO2), microcrystalline quartz

A brownish-red to deep brown variety of chalcedony, closely related to carnelian but darker, colored by iron oxides.

Mohs hardness
6.5-7
Color
brownish red to deep brown
Type
mineral

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Overview

Sard is a translucent to opaque variety of chalcedony ranging from brownish red to deep brown, colored by iron oxides. It is essentially the darker, browner counterpart of carnelian; the two grade into one another, with carnelian reserved for the brighter orange-red tones and sard for the deeper brown-red shades.

Valued since antiquity, sard was a favored material for Roman seals and intaglios because it carves cleanly and takes detail well. The dark layer in banded sardonyx is sard alternating with white or pale chalcedony.

It is found in many silica-rich environments, with historic sources including India and the Mediterranean region.

Formation & geology

Sard forms by precipitation of silica from groundwater or hydrothermal fluids into cavities, veins, and weathered volcanic rocks, building up as microcrystalline quartz (chalcedony). Its brown-red color develops from finely dispersed iron oxides and hydroxides (such as hematite and goethite) incorporated during deposition.

The depth of color depends on the amount and oxidation state of the iron; more or more-oxidized iron yields the darker brown tones that distinguish sard from the lighter carnelian. Heating, whether natural or artificial, can also intensify or shift the color toward red. Deposits occur worldwide in basaltic vesicles and silica-rich sediments.

How to identify it

Look for translucent-to-opaque brownish-red to deep brown chalcedony with a waxy to glassy luster, hardness 6.5-7, conchoidal fracture, no cleavage, and a white streak. Held to light, sard often shows a warm reddish-brown glow at the edges.

The main look-alike is carnelian: the distinction is tonal, sard is darker and browner, carnelian brighter orange-red, and the boundary is informal. Distinguish sard from jasper (opaque, not translucent) and from brown glass (which lacks a white streak and may show bubbles). In sardonyx, sard forms the brown bands paired with white onyx layers.

Uses & significance

Sard has a long history in jewelry and especially in carved seals, cameos, and intaglios, where its toughness and fine grain allow detailed engraving. Today it is cut into cabochons and beads and is the dark component of sardonyx ornaments.

Metaphysically it is associated with grounding, courage, and protection, claims that are not scientifically supported. Its genuine significance is historical and lapidary: a durable, attractively colored chalcedony prized across ancient cultures and still used for carving and beadwork.

Frequently asked questions

What is the difference between sard and carnelian?

They are the same chalcedony family; sard is darker and browner, while carnelian is brighter orange-red. The boundary is informal.

What gives sard its color?

Finely dispersed iron oxides and hydroxides produce its brownish-red to deep brown tones.

What is sardonyx made of?

Sardonyx is banded chalcedony combining brown sard layers with white onyx layers.

Is sard a hard stone?

Yes, about 6.5-7 on the Mohs scale, durable enough for carving, seals, and everyday jewelry.

Sard identified by the community

Real specimens identified with Rock Identifier.

Tumbled Stones (various)