Rock Identifier
Tumbled chalcedony-bearing stone, possibly bloodstone or jasper (Microcrystalline quartz (SiO₂), likely chalcedony with iron-oxide inclusions; exact identification is uncertain from the photograph) — mineral
mineral

Tumbled chalcedony-bearing stone, possibly bloodstone or jasper

Microcrystalline quartz (SiO₂), likely chalcedony with iron-oxide inclusions; exact identification is uncertain from the photograph

AI-generated identification · may be incorrect

Opaque blue-gray to reddish-brown, fine-grained, and smoothly tumbled with a dull-to-waxy luster. Quartz hardness is about 6.5–7 Mohs; no visible cleavage, conchoidal fracture, and specific gravity near 2.6.

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Physical properties

Opaque blue-gray to reddish-brown, fine-grained, and smoothly tumbled with a dull-to-waxy luster. Quartz hardness is about 6.5–7 Mohs; no visible cleavage, conchoidal fracture, and specific gravity near 2.6.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures, with iron oxides producing the red-brown patches. Chalcedony and jasper deposits commonly range from Cenozoic to Precambrian age depending on locality.

Uses & applications

Used for cabochons, beads, carvings, tumbled stones, and lapidary ornaments; tougher varieties are also used as minor abrasives. It has modest jewelry value unless color and pattern are unusually attractive.

Geological facts

Bloodstone is typically dark green chalcedony with vivid red hematite spots; this specimen appears more blue-gray and may instead be iron-stained jasper or another quartz-rich pebble.

Field identification & locations

Look for a very fine, non-granular texture, waxy luster, lack of cleavage, and a white streak; quartz should resist scratching by a steel knife. Common sources include India, Brazil, Madagascar, Uruguay, and the western United States.