
sedimentary
Bumblebee Jasper
Fossiliferous Calcite containing Orpiment and Realgar
Hardness: 5 on Mohs scale; Color: Concentric bands of yellow, orange, black, and gray; Luster: Waxy to dull; Crystal structure: Trigonal (as calcite); Cleavage: Perfect in three directions (calcite matrix).
- Hardness
- 5 on Mohs scale
- Color
- Concentric bands of yellow, orange, black, and gray
- Luster
- Waxy to dull
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Physical properties
Hardness: 5 on Mohs scale; Color: Concentric bands of yellow, orange, black, and gray; Luster: Waxy to dull; Crystal structure: Trigonal (as calcite); Cleavage: Perfect in three directions (calcite matrix).
Formation & geological history
Formed from volcanic deposits inside the cracks of a volcano, typically around fumaroles or hydrothermal vents. It is a combination of volcanic ash, anhydrite, sulfur, arsenic, and calcium carbonate. Primary location is Mount Papandayan in Indonesia.
Uses & applications
Primarily used as a decorative stone for lapidary work, including cabochons for jewelry, carvings, and metaphysical collecting. Caution is used due to arsenic content.
Geological facts
Despite its name, it is not a true Jasper because it lacks a high silica content; it is technically a calcium carbonate rock. Its distinctive stripes mimic the patterns of a bumblebee.
Field identification & locations
Identify by its unique 'vibrant bee-like' banding and relatively low hardness compared to true quartz-based jasper. Found almost exclusively in West Java, Indonesia. Collectors should seal the stone to prevent contact with toxic arsenic minerals.
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