Adamite
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Discover fluorescent Adamite from Ojuela Mine, Mapimí, Durango, Mexico, a classic locality for this zinc arsenate mineral.

Tested by GeoFossils, these specimens display their strongest green fluorescence under Medium Wave (MW) UV. Green fluorescence is also visible under Short Wave (SW) and Long Wave (LW) UV, while some specimens show additional pale blue to blue-white fluorescent areas from an unidentified associated mineral phase.

The combination of Ojuela provenance and multi-wavelength fluorescence makes this material particularly relevant to collectors of fluorescent minerals and Mexican mineral specimens.

UV fluorescence

UV wavelength Observed response
Medium Wave (MW) Predominant green fluorescence
Short Wave (SW) Green fluorescence, generally weaker and more localised than MW
Long Wave (LW) Green fluorescence; some specimens also show pale blue to blue-white fluorescence from an unidentified associated mineral phase

These responses have been observed by GeoFossils on the material offered here. Fluorescence can vary between specimens and may appear different according to UV lamp output, ambient lighting and viewing conditions.

Scientific information

Property Information
Primary mineral Adamite
Chemical formula Zn₂(AsO₄)(OH)
Mineral class Arsenate
Mineral group Olivenite Group
Crystal system Orthorhombic
Mohs hardness 3.5
Typical lustre Vitreous
Locality Ojuela Mine, Mapimí, Durango, Mexico
Predominant UV wavelength Medium Wave (MW)
Observed fluorescence Green under MW, SW and LW

Formation & mineralogy

Adamite is a secondary zinc arsenate hydroxide that forms in the oxidised zones of zinc deposits containing arsenic-bearing minerals. It commonly occurs as distinct crystals, radial aggregates, rosettes and crystalline crusts.

The pale blue to blue-white fluorescent areas visible on some GeoFossils specimens have not been analytically identified and are therefore not attributed to a particular associated mineral.

Locality & collector significance

Ojuela Mine, Mapimí, Durango, Mexico, is a classic locality for Adamite and a diverse range of secondary arsenate minerals formed within its extensively oxidised mineral deposit.

The locality also has particular mineralogical significance as the type locality of paradamite, the triclinic dimorph of Adamite.

What causes the fluorescence?

The green fluorescence documented in some Ojuela Adamite is associated with trace uranyl ions within the mineral. Fluorescence can vary considerably between individual specimens.

GeoFossils has confirmed the fluorescent response of the material offered here but has not analytically determined the activator within each specimen.

Viewing your UV mineral

For the strongest observed response, view the specimen in a dark environment using an appropriate Medium Wave mineral UV lamp. Short Wave and Long Wave lamps can be used separately to observe the additional responses present within the material.

Always follow the UV equipment manufacturer's instructions and avoid looking directly into the UV light source.

Care instructions

Handle Adamite carefully and store it separately from harder minerals to reduce the risk of scratching or chipping. Remove loose dust with a soft, dry brush and avoid abrasive cleaning methods or harsh household chemicals.

Frequently asked questions

What colour does this Adamite fluoresce?
GeoFossils has observed green fluorescence under Medium Wave, Short Wave and Long Wave UV. Medium Wave produces the predominant response in this collection.

Which UV wavelength is best for viewing this Adamite?
Medium Wave (MW) produces the strongest green fluorescence observed by GeoFossils on this material.

What are the pale blue or blue-white fluorescent areas?
Some specimens contain an associated mineral phase that displays pale blue to blue-white fluorescence. This material has not been analytically identified, so GeoFossils does not attribute the response to a particular mineral.

Does every specimen fluoresce identically?
No. Natural variations in mineral distribution mean the coverage and intensity of fluorescence can differ between specimens.

Where is this Adamite from?
This material is from Ojuela Mine, Mapimí, Durango, Mexico.

Location

Ojuela Mine | Mapimí | Durango | Mexico

Please note

Natural mineral specimens vary in shape, colour, crystal coverage and fluorescent response. UV colours may also appear slightly different in person because lamp output, ambient lighting, camera settings and viewing conditions can affect their appearance.

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