
sedimentary
Septarian Nodule
Septarian Nodule (Calcite, Aragonite, and Limestone/Claystone)
AI-generated identification · may be incorrectHardness: 3.5 to 4; Color: Yellow/brown centers with dark brown lines and tan matrix; Luster: Waxy to sub-vitreous; Structure: Microcrystalline with distinct shrinkage cracks (septaria); Cleavage: Perfect rhombohedral in calcite portions.
- Hardness
- 3
- Color
- Yellow/brown centers with dark brown lines and tan matrix
- Luster
- Waxy to sub-vitreous
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Physical properties
Hardness: 3.5 to 4; Color: Yellow/brown centers with dark brown lines and tan matrix; Luster: Waxy to sub-vitreous; Structure: Microcrystalline with distinct shrinkage cracks (septaria); Cleavage: Perfect rhombohedral in calcite portions.
Formation & geological history
Formed during the Cretaceous period approximately 50 to 70 million years ago. These started as muddy concretions around organic matter that dried out and cracked, with the cracks later filling with minerals like calcite and aragonite.
Uses & applications
Primarily used as a decorative stone, in jewelry (cabochons), as metaphysical palm stones, and for scientific/collector displays.
Geological facts
Also known as Dragon Stones due to their scaly appearance, they are unique because they were formed through a combination of chemical precipitations and mechanical shrinking processes.
Field identification & locations
Identify by looking for the distinct 'lightning bolt' or spiderweb patterns of dark mineral veins against a lighter host rock. Major deposits are found in Utah, USA and Madagascar.
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