sedimentary

Ferruginous Sandstone with Ironstone Concretion

Goethite-rich Sandstone (FeO(OH))

AI-generated identification · may be incorrect

Hardness: 5-5.5 (concretion) to 6-7 (quartz grains). Color: Dark brown, rusty orange, and charcoal grey. Luster: Dull, earthy, or sub-metallic. Crystal Structure: Amorphous or microcrystalline matrix surrounding grains. Specific Gravity: 3.3-4.3.

Hardness: 5-5
Color: Dark brown, rusty orange, and charcoal grey
Luster: Dull, earthy, or sub-metallic

Identified April 29, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed by the precipitation of iron oxides (hematite or goethite) within the pore spaces of sandstone beds. Often occurs as groundwater rich in iron interacts with oxygenated zones. Geological age varies greatly but is common in Cretaceous or Jurassic formations.

Uses & applications

Predominantly used as a low-grade iron ore historically. Occasionally used for decorative landscaping or as an architectural aggregate in 'ironstone' buildings. Of value to collectors for their unique botryoidal or nodular shapes.

Geological facts

These are often mistaken for meteorites due to their heavy weight and dark, burnt-looking exterior. They are sometimes called 'rattle stones' if a loose sandy core is trapped inside a hard iron shell.

Field identification & locations

Identify in the field by its significant weight (high density), reddish-brown streak when rubbed against unglazed porcelain, and lack of true crystal faces. Common in the Southeastern United States, Western Europe, and Australia.