
sedimentary
Septarian Nodule
Septaria (composed of Calcite, Aragonite, and Limestone)
AI-generated identification · may be incorrectHardness: 3.5-4 (Mohs), Color: Yellow, brown, and grey. Luster: Waxy to earthy. Crystal structure: Trigonal (Calcite) or Orthorhombic (Aragonite). Features distinct radial cracks or 'septa' filled with minerals.
- Hardness
- 3
- Color
- Yellow, brown, and grey
- Luster
- Waxy to earthy
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Physical properties
Hardness: 3.5-4 (Mohs), Color: Yellow, brown, and grey. Luster: Waxy to earthy. Crystal structure: Trigonal (Calcite) or Orthorhombic (Aragonite). Features distinct radial cracks or 'septa' filled with minerals.
Formation & geological history
Formed during the Cretaceous period (50-70 million years ago) in marine environments. Volcanic eruptions killed sea life which sank to the bottom; chemical reactions between decaying matter and sediments formed mud balls that later cracked and were filled with mineral deposits.
Uses & applications
Primarily used for lapidary work, home decor, ornamental carvings, and as a popular specimen for rock collectors.
Geological facts
The name 'Septarian' comes from the Latin word 'septum' meaning partition, referring to the cracks that divide the nodule. They are sometimes called 'Dragon Stones' due to their scaly, cracked appearance.
Field identification & locations
Identify by looking for a 'tortoise shell' pattern with yellow calcite centers and grey limestone exteriors. Most commonly found along the Gulf of Mexico and in southern Utah, USA.
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