About the Specimen This striking UV-reactive agate geode is presented as a naturally split, two-piece specimen, allowing both halves to be displayed open or closed. Supplied under the trade name “Alien Agate”, this name reflects the specimen’s unusual internal structure and fluorescence rather than a formal mineral classification. The interior reveals a combination of soft blue-grey chalcedony and secondary quartz crystal growth surrounding a darker mineral-rich core. The contrast between textures, colours, and UV response makes this a visually engaging and highly characterful piece. Total weight: 126 g Format: Naturally split agate geode (two pieces) Condition: Natural, unpolished, untreated Locality: Unknown (supplier unable to confirm origin) Measurements (Approximate) Closed geode: 8.5 cm × 6.5 cm × 5 cm (depth) Top section (open): 5 cm × 4 cm × 3 cm (depth) Bottom section (open): 6 cm wide × 5.5 cm tall × 5 cm (depth) Measurements are approximate due to the natural, irregular form of the specimen. UV Reactivity This specimen displays a strong and attractive UV reaction, best observed under 365nm longwave ultraviolet light. Observed UV characteristics include: Bright green fluorescence concentrated within chalcedony-rich zones Softer blue-green glow along internal cavity walls Clear contrast between fluorescent interiors and the darker outer rind No phosphorescence has been observed once the UV source is removed. All UV photographs are taken under controlled conditions and accurately represent the specimen. Geological Formation Agate is a form of microcrystalline quartz (chalcedony) that forms when silica-rich fluids slowly infill cavities within host rock. Over extended geological time, successive silica deposition creates layered chalcedony, often followed by later-stage quartz crystal growth within remaining voids. In this specimen, uneven silica infill and later mineral deposition have produced: Irregular internal cavities Mixed chalcedony and quartz textures Localised concentrations of trace elements responsible for UV fluorescence The unusual internal appearance is the result of natural growth variation, not treatment or enhancement. Approximate Geological Age While the exact locality is unknown, agates of this type typically form during periods of volcanic or hydrothermal activity. A reasonable geological estimate for this specimen is: Approximately 50–200 million years old Rarity & Collectability While agate itself is widespread, UV-reactive agate geodes with strong, concentrated fluorescence are significantly less common — particularly in naturally split, displayable pairs. Collectability features include: Distinct internal cavity structure Multiple fluorescent zones Natural two-piece separation Unique character due to unknown locality Each specimen of this type is inherently one of a kind. Display & Mounting Note This specimen has been professionally mounted with a small metal hinge, which has been securely adhered to allow the two natural halves to open and close smoothly.The hinge is not part of the geological formation and has been added purely for display and presentation, ensuring the two matching halves remain together and can be safely displayed as a single piece. The mounting is clearly visible in the photographs and does not affect the natural surfaces, crystal growth, or UV reactivity of the specimen. Care & Handling Handle with care — natural crystal edges may be delicate Avoid prolonged exposure to moisture Clean gently with a soft, dry brush only UV display is safe, but prolonged intense exposure should be avoided for conservation
