LEADHILLS & WANLOCKHEAD |
PHOTO GALLERY Secondary
Zinc Minerals including photographs of Hemimorphite
- Greenockite/ Hemimorphite |
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HEMIMORPHITE Secondary enrichment of the primary ores took place throughout the Leadhills & Wanlockhead deposit and secondary lead species are common to both sites. Wanlockhead, richer in zinc ores, has a greater prevalence of secondary zinc species such as hemimorphite (hydrous zinc silicate). Hemimorphite occurs generally either as tiny crystals forming crusts or as botryoidal aggregates. It has a wide array of colours, with colourless, white, sky blue, green, yellow to brown-hued specimens being encountered. Less common is yellow hemimorphite, coloured by inclusions of the rare species, greenockite (Cadmium Sulphide). Greenockite
occurs at Wanlockhead as inclusions in hemimorphite or as
powdery coatings. |
HEMIMORPHITE Radiating,
prismatic, hemimorphite crystals stained yellow |
HEMIMORPHITE |
VESZELYITE Around 1988, collectors found the rare, hydrous copper phosphate mineral, veszelyite, at Wanlockhead. This rare
species was previously unrecorded at Wanlockhead or
Leadhills and it is also the first recorded occurence of
the species in the United Kingdom. Some specimens encountered contained pseudomorphs of chrysocolla (hydrous copper silicate) after veszelyite, particularly with larger crystals. Both full and partial replacements were found. In the latter case, the outer area of veszelyite was replaced by chrysocolla and the core left unaltered. Veszelyite has not
been encountered since and the site |
VESZELYITE |
VESZELYITE Twinned
crystals with a pyramidal habit to c. 1mm with green
globules of chrysocolla |
VESZELYITE |
HEMIMORPHITE A 1cm cavity infilled with tiny, elongated, radiating sky blue crystals. |
the end
Ore & Gangue Species |
Secondary Lead Species |
Secondary Lead/ |
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Secondary Lead Species |
Type Locality Species |
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Copper Species |
Galloway Region |
© Minerals of Scotland - 2008.