
sedimentary
Septarian Nodule (Dragon Stone)
Septarian Concretion (CaCO3 + CaMg(CO3)2 + SiO2)
Hardness: 3.5-4 (Mohs); Color: Brown (siderite/mudstone), yellow (calcite), white (aragonite/quartz); Luster: Waxy to vitreous; Crystal Structure: Trigonal/Orthorhombic mix; Cleavage: Perfect in calcite sections.
- Hardness
- 3
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 3.5-4 (Mohs); Color: Brown (siderite/mudstone), yellow (calcite), white (aragonite/quartz); Luster: Waxy to vitreous; Crystal Structure: Trigonal/Orthorhombic mix; Cleavage: Perfect in calcite sections.
Formation & geological history
Formed during the Cretaceous period (50-70 million years ago). They began as sedimentary clay balls that cracked due to dehydration and shrinkage, followed by the infiltration of mineral-rich water that precipitated calcite and aragonite into the cracks.
Uses & applications
Primarily used for decorative purposes, ornamental carvings, high-end interior design slabs, jewelry (cabochons), and as textbook-quality geological specimens for collectors.
Geological facts
Also known as 'Dragon Stone' because the cracked patterns resemble dragon skin. The name 'Septarian' comes from the Latin word 'septum', meaning partition, referring to the cracks and separations within the stone.
Field identification & locations
Identify in the field by looking for rounded, heavy grey mudstone nodules with visible angular protruding patterns. Commonly found in Madagascar, Utah (USA), and parts of the UK. Collectors look for high contrast between the yellow centers and dark outer rinds.
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