
sedimentary
Septarian Nodule with Calcite
Septarian Concretion (CaCO3 with internal calcite crystals)
Hardness: 3-4 on Mohs scale (for calcite); Color: Brown, yellow, grey with yellow/amber crystal centers; Luster: Vitreous to dull; Crystal structure: Trigonal (calcite); Cleavage: Perfect rhombohedral cleavage on calcite; Specific gravity: 2.6-2.7
- Hardness
- 3-4 on Mohs scale (for calcite)
- Color
- Brown, yellow, grey with yellow/amber crystal centers
- Luster
- Vitreous to dull
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Physical properties
Hardness: 3-4 on Mohs scale (for calcite); Color: Brown, yellow, grey with yellow/amber crystal centers; Luster: Vitreous to dull; Crystal structure: Trigonal (calcite); Cleavage: Perfect rhombohedral cleavage on calcite; Specific gravity: 2.6-2.7
Formation & geological history
Formed in sedimentary muds and shales approximately 50 to 150 million years ago during the Cretaceous period, where shrinking mud caused radial cracks that later filled with mineral-rich water precipitating calcite.
Uses & applications
Used for ornamental carvings, spheres, lapidary art, display specimens, and in metaphysical practices.
Geological facts
The word 'septarian' comes from the Latin word 'septem,' meaning seven, referring to the pattern of cracks that typically divide the nodules into seven or more pointed segments.
Field identification & locations
Easily identified by its distinctive turtle-shell-like exterior patterns and inner cavities lined with yellow or brown calcite crystals. Found prominently in regions like Madagascar and Utah, USA.
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