
sedimentary
Septarian Nodule
Septarian concretion (Complex mixture of Siderite/Limestone, Calcite, and Aragonite)
Hardness: 3.5-4 (Mohs scale); Color: Brown, tan, and grey with yellow to white veins; Luster: Earthy to vitreous in veins; Texture: Crystalline veins within a fine-grained matrix; Cleavage: None for the rock, rhombohedral for calcite infill.
- Hardness
- 3
- Color
- Brown, tan, and grey with yellow to white veins
- Luster
- Earthy to vitreous in veins
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Physical properties
Hardness: 3.5-4 (Mohs scale); Color: Brown, tan, and grey with yellow to white veins; Luster: Earthy to vitreous in veins; Texture: Crystalline veins within a fine-grained matrix; Cleavage: None for the rock, rhombohedral for calcite infill.
Formation & geological history
Formed as mud balls in ancient sea beds during the Cretaceous period (50-70 million years ago); they dried and cracked, and the cracks were later filled with mineral precipitates like calcite and aragonite.
Uses & applications
Primarily used for decorative purposes, collecting, jewelry (cabochons), and as museum display specimens. Highly prized for their 'dragon skin' appearance.
Geological facts
Also known as 'Dragon Stones'; they are famous for their unique internal patterns that never repeat. Large nodules can reach several feet in diameter.
Field identification & locations
Identify by the pattern of angular cracks or veins (septaria) on the surface or inside. Commonly found in Utah, USA (the 'Muddy Creek' area) and Madagascar. Collectors look for high contrast between the matrix and the crystals.
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