Rock Identifier
Septarian Nodule Geode (Septarian concretions (composed of Calcite, Aragonite, and Limestone)) — sedimentary
sedimentary

Septarian Nodule Geode

Septarian concretions (composed of Calcite, Aragonite, and Limestone)

Hardness: 3-4 (Calcite/Aragonite) / color: brown, yellow, and grey / luster: vitreous to dull / crystal structure: rhombohedral / cleavage: perfect rhombohedral / specific gravity: 2.71

Identified More sedimentary

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Physical properties

Hardness: 3-4 (Calcite/Aragonite) / color: brown, yellow, and grey / luster: vitreous to dull / crystal structure: rhombohedral / cleavage: perfect rhombohedral / specific gravity: 2.71

Formation & geological history

Formed in ancient sea beds roughly 50 to 70 million years ago during the Cretaceous period. Decomposing sea life killed by volcanic eruptions caused mud balls to form, which then cracked and were filled with mineral deposits like calcite.

Uses & applications

Primarily used as decorative display pieces, in lapidary work for making bookends and spheres, and as a popular specimen for mineral collectors.

Geological facts

The name comes from the Latin word 'septum' meaning wall or partition, referring to the cracks and separations between the different minerals. They are often called 'Dragon Stones' due to their scaly appearance.

Field identification & locations

Identify by the unique angular patterns of yellow/brown calcite filling cracks within a mudstone/limestone matrix. Commonly found in Utah, USA and Madagascar.