
sedimentary
Septarian Nodule (Dragon Stone)
Septarian concretion (CaCO3 with Aragonite and Calcite)
AI-generated identification · may be incorrectHardness: 3.5-4 (Mohs scale); Color: Yellow (calcite), Brown (aragonite shell), Grey (limestone exterior); Luster: Vitreous to dull; Crystal structure: Trigonal/Orthorhombic; Cleavage: Perfect rhombohedral in calcite areas.
- Hardness
- 3
- Luster
- Vitreous to dull
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Physical properties
Hardness: 3.5-4 (Mohs scale); Color: Yellow (calcite), Brown (aragonite shell), Grey (limestone exterior); Luster: Vitreous to dull; Crystal structure: Trigonal/Orthorhombic; Cleavage: Perfect rhombohedral in calcite areas.
Formation & geological history
Formed roughly 50 to 70 million years ago during the Cretaceous period. These nodules started as mud balls on ancient seafloors which cracked as they dried and shrunk, with minerals like calcite later precipitating into the cracks.
Uses & applications
Primarily used for ornamental purposes, lapidary arts (cabochons, spheres), home decor, and as a popular metaphysical or fossil-enthusiast collector's item.
Geological facts
Also known as 'Dragon Stones' due to the scaled appearance of the cracked patterns. The name 'Septarian' comes from the Latin 'septum' meaning partition, referring to the cracks that divide the concretion.
Field identification & locations
Identify in the field by looking for rounded, heavy grey nodules that reveal a 'star' or 'honeycomb' internal pattern when cracked open. Common locations include Utah (USA), Madagascar, and the United Kingdom.
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