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Druse Quartz on Limonite

Posted April 30, 2019

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Minerals: Quartz (druse), Limonite.
– Specimen Size: 13 x 11 x 6 cm (appr.)
– Found: Mexico (San Luis Potosi)
Photo: Leo Jahaan

 

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Minerals: Quartz, Limonite.
Photo: Leo Jahaan

Realgar in Selenite

Posted April 18, 2019
A jumble of radiating Realgar crystals within clear Gypsum.

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Minerals: Realgar, Selenite (clear Gypsum).
– Field of View: 3 cm (appr.)
– Found: Peru (Palomo Mine)
Photo: Leo Jahaan

 

Selenite window with Realgar inside.

Decription: Selenite ‘window’ allowing viewing of the Realgar needles within. On the upper surface, Realgar has altered to orange Orpiment.
– Field of View: 3.5 cm (appr.)
Photo: Leo Jahaan

 

Macro shot of Realgar crystals within Selenite.

Decription: More detailed view of the above Selenite ‘window’. Notice the unusual bed of micro Realgar crystals in the lower-right.
– Field of View: 2 cm (appr.)
Photo: Leo Jahaan

 

Realgar in Selenite.

Description: One particular Realgar crystal rises prominently upwards inside it’s Selenite host.
– Field of View: 1.5 cm (appr.)
Photo: Leo Jahaan

Reticulated Cerussite, Wulfenite

Posted April 6, 2019
Interconnecting white Cerussite crystals with partial orange Wulfenite coating.

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Minerals: Cerussite (reticulated), Wulfenite (orange coating).
– Specimen Size: 4 x 3 x 2 cm (appr.)
– Found: Iran (Nakhlak Mine, Isfahan)
Photo: Leo Jahaan

 

Cerussite snowflake.

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Description: Cerussite in it’s reticulated snowflake-like form, with Wulfenite forming only on the upper surface planes.
Photo: Leo Jahaan

 

Orange Wulfenite micro crystals,

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Minerals: Sparkling orange Wulfenite micro crystals on reticulated Cerussite.
Photo: Leo Jahaan

‘Fossil Bamboo’

Posted March 12, 2019
Fossil Bamboo

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Mineral: Chalcedony (Agate), Limonite.
– Specimen Size: 7 x 6 x 6 cm (appr.)
– Found: Indonesia (Java)
Photo: Leo Jahaan

Notes: Specimens such as this are known as ‘Fossil Bamboo’ by the Javanese locals, however the material requires further research to ascertain exactly what it is and how it has formed.  A likely theory is that these hollow tubes are translucent chalcedony casts, initially formed over organic matter. Volcanic ash has probably fallen into a marsh environment, dissolving into a mineral-rich suspension which changes the chemical composition of the wetland, resulting in the growth of cryptocrystalline quartz on the surface of tough silica-rich plant or grass stems.  A likely plant candidate is Equisetum, commonly known as ‘horsetail’ or ‘puzzlegrass’, which can resemble bamboo in appearance.  Following the slow decomposition of the inner organic material, iron-rich minerals such as limonite have formed on partial surfaces and in some cases formed bog iron ‘rods’ within the now-hollow tubes.