sedimentary
Sandstone Concretion
Sandstone (Sedimentary Rock) with silica or calcite cement
Hardness: 6-7 (if silica) or 3 (if calcite). Color: Tan, beige, or brown with visible wood-like grain. Luster: Dull/Earthy. Structure: Clastic/Spherical. Specific gravity: 2.3-2.6.
- Hardness
- 6-7 (if silica) or 3 (if calcite)
- Color
- Tan, beige, or brown with visible wood-like grain
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (if silica) or 3 (if calcite). Color: Tan, beige, or brown with visible wood-like grain. Luster: Dull/Earthy. Structure: Clastic/Spherical. Specific gravity: 2.3-2.6.
Formation & geological history
Formed by the precipitation of mineral cement within the spaces between sediment grains. These often form around a nucleus (like a leaf or shell) and grow outward in round shapes within sedimentary layers.
Uses & applications
Mostly used as curiosity pieces or garden decor. In some historical contexts, smooth round concretions were used as game stones or projectiles.
Geological facts
They are often mistaken for fossilized eggs or cannonballs due to their remarkably spherical shape. Some very large ones, like the Moeraki Boulders in New Zealand, can be several meters wide.
Field identification & locations
Identify in the field by their distinct rounded shape compared to surrounding rocky layers. Often found eroding out of sandstone or shale cliffs.
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