Rock Identifier
Arfvedsonite in Quartz (also known as Eudialyte/Garnet Syenite variety) (Arfvedsonite [Na3(Fe2+)4Fe3+Si8O22(OH)2] within a silicate matrix) — igneous
igneous

Arfvedsonite in Quartz (also known as Eudialyte/Garnet Syenite variety)

Arfvedsonite [Na3(Fe2+)4Fe3+Si8O22(OH)2] within a silicate matrix

Hardness: 5-6 (Mohs scale); Color: Dark brown to black with pinkish-red or white inclusions; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Good; Specific gravity: 3.44

Hardness
5-6 (Mohs scale)
Color
Dark brown to black with pinkish-red or white inclusions
Luster
Vitreous to pearly
Identified More igneous

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Physical properties

Hardness: 5-6 (Mohs scale); Color: Dark brown to black with pinkish-red or white inclusions; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Good; Specific gravity: 3.44

Formation & geological history

Formed in highly alkaline plutonic rocks, typically within nepheline syenites and granitic pegmatites. These specimens are often found in Precambrian geological formations.

Uses & applications

Primarily used for lapidary work, jewelry (pendants/beads), and as collectible metaphysical stones believed to aid in manifestation.

Geological facts

This specimen is often confused with Astrophyllite or Nuummite due to its dark appearance and internal flashes. It is a sodium-rich amphibole mineral named after the Swedish chemist Johan August Arfwedson.

Field identification & locations

Identify in the field by its association with alkaline igneous rocks and its distinct blueish or dark brown bladed crystals. Commonly found in Greenland (Ilimaussaq complex), Canada (Mont Saint-Hilaire), and Russia (Kola Peninsula).