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FACETIPS – A GEM CUTTER’S NOTEBOOK

by
Duncan Miller


The faceting articles published over the past few years in the Mineral Chatter have been compiled into a single 128 page document, available for download for those interested in saving all the articles together. To download the pdf file click here.

A 29,18 ct cuprite from Onganja, Namibia, cut by Duncan Miller and now in a private collection in Germany.


Fruits of the earth - Opal Pineapples

January 15, 2012



There are some mineral specimens in this world that beggar belief and the opal pineapples from White Cliffs in Australia are amongst those. They are palm-sized clusters of radiating points, looking like some bizarre fruit and have been known since the beginning of the 20th century. Found only in the Cretaceous sediments of the White Cliffs opal field in New South Wales, they occurred in an area which has also produced opalised fossils of marine shells, pieces of wood, and even the occasional plesiosaur skeleton. The pineapples are rare, perhaps fewer than 250 have ever been found, and range in quality from gem opal displaying bright diffraction colours, to opaque white potch.

In 1978 Grant Pearson and a group of friends made the lucky discovery of a pocket of opal pineapples about 12 metres below the surface of abandoned workings. Careful excavation showed that the pineapples were restricted to an oval area about 12 by 20 metres in a layer about 2 metres thick, probably originally a localised saline pool at the bottom of the sea. The pineapples are not fossilised fruit, but actually opal pseudomorphs after clusters of crystals.

Many of the nodules were found broken, some so severely shattered that the fragments were too small even to cut as gems. Others were intact and after laborious cleaning made the most spectacular specimens. According to Grant Pearson the best specimen recovered was sold for just under AU$100 000, although one wonders how anyone could sell such a specimen, having found it oneself!

Initially the original crystals were thought to be glauberite, but more recent investigations have shown that they probably were the mineral ikaite, the hexahydrate of calcium carbonate, CaCO3·6H2O. This forms only in water at near freezing conditions, like that found at the bottom of deep oceans or in the polar regions. At the

time of formation of the ikaite precursors of the pineapples, Australia was further south than at present, and the area of the White Cliffs opal fields was beneath a cold sea. Although the Cretaceous polar temperatures were higher than polar temperatures today, icebergs must have rafted debris out to sea, as evidenced by dropstones found occasionally in the opal diggings, including one in Grant Pearson’s pineapple layer. The uncertainties in reconstructing the geological past mean one can’t be too specific; but we know it was cold, and wet, and there was one layer in which the conditions were just right for the formation of ikaite.

The mechanism of replacement of ikaite by opal is still unclear. The pineapple pocket was underlain by a relatively impervious clay horizon, which may have helped retain the opalising fluids in the pineapple bearing layer. Some of the pineapples show a distinct layering of the opal, while others when broken or sawn open have interior swirls of colour, indicating a complex mechanism of opal formation. The opal itself is not unusual in structure, and like all colourful opal consists of ordered layers of tiny silica spheres, precipitated from a gel. Ordered volumes of larger spheres produce red colours, and smaller spheres blue.

Opal pineapples are amongst the rarest of mineral specimens. Given that they seem to originate from only one layer in the largely worked-out White Cliffs opal field, and from isolated and widely-spaced pockets within that layer, it is unlikely that more are going to appear any time soon. Duncan Miller

Acknowledgement:

Thank you to Grant Pearson for allowing reproduction of several of his photographs of opal pineapples and for providing copies of relevant publications. These are now lodged in the club’s library, for those who may wish to read more about these fascinating specimens.

References:

Niedermayr, G. & Pearson, G.M. 1997. Die „Opal Pineapples“ von White Cliffs in New South Wales, Australien. Mineralien Welt 8(5):48.

Niedermayr, G. & Pearson, G.M. 1997. Die „Opal Pineapples“ von White Cliffs in New South Wales, Australien. Mineralien Welt 8(4):51.

Pearson, G. 1986. Opal pineapples from White Cliffs. The Australian Gemmologist 16(4):143.

Pearson, G. 1987. Opal pineapples from White Cliffs, New South Wales. Australian Mineralogist 2(2):7.

 

Into the Skorpion's Pit

December 14, 2011

The Skorpion zinc mine lies 25 km north of the town of Rosh Pinah, on the main road to Aus. On entering the mine, one is immediately struck that the area is split into two distinct operations. The first is the chemical refining plant, a huge steel structure of conveyors, tanks, etc., that uses 25% of Namibia’s electricity. Tucked away at the back of the plant is the open pit where the ore is mined by huge double-storey tip trucks, bulldozers and front-end loaders.


This deposit was first di...

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Mineral of the Month - ZINC ORES – SPHALERITE

October 21, 2011

The main ore types mined at Rosh Pinah are carbonate ore, microquartzite ore, and arkose ore containing mainly the sulphide ore minerals sphalerite (ZnS), galena (PbS), chalcopyrite (CuFeS2) and Pyrite (FeS). Specimen grade sphalerite crystals are occasionally found as attractive dark brown metallic euhedral cubes in vugs and quartz veins in this mine.


Photo. G Hinder

They can also occur as an adamantine lustre of golden brown and even yellow green colour, but not at Rosh Pinah. These crysta...

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Mineral of the Month - Jeremejevite

September 28, 2011

Crystal system:                 Hexagonal                                           Hardness:            6,5 – 7,5
Density:                               3,28 – 3,31                                           Streak:                  White
Colour:                                 Colourless, white, yellowish, pale to dark blue
Cleavage:                            None
Occurrence:                       A rare late hydrothermal mineral formed in granitic pegmatites.
Habitat:           ...

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Mineral of the Month - Chrysoberyl

August 28, 2011



Crystal system
:                 Orthorhombic                                   Hardness:            8,5
Density:                               3,5 – 3,84                                             Streak:                  White
Colour:                                 Various shades of green, yellow, brownish to green black (can be raspberry-red under incandescent light when chromium is present)
Cleavage:                            Distinct, imperfect
Occurrence:                      ...

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Mineral of the Month - Stilbite

July 23, 2011

NaCa2Al5Si13O36 14H2O, Hydrated sodium calcium aluminum silicate
 
At one time heulandite and stilbite were considered to be identical minerals.  After they were found to be two separate species, in 1818, the name desmine ("a bundle") was proposed for stilbite, and this name is still employed in Germany.  The English name "stilbite" is from the Greek stilbein = to shine, because of the pearly luster of the {010} faces.
 
Stilbite is a common and perhaps the most popular zeolite mineral ...

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Mineral of the Month - Analcime

June 24, 2011

                 
Goboboseb crystals showing crystal clear analcime – photos and specimens PdB
 
NaAlSi2O6-H2O, Hydrated Sodium Aluminium Silicate

The name of the mineral comes from the Greek word analkis that means weak.

Analcime is a zeolite and occurs frequently in basalts and other basic igneous rocks associated with other Zeolites.

Crystal system: triclinic (Pseudo-cubic)

The aluminosilicate framework of the crystal structure does not change in topology at all.  The reduction...

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Mineral of the Month - Cuprite

June 24, 2011

Crystal system:                 Isometric                                             Hardness:                        3,5 - 4,0
Density:                               6,15 average                                      Streak:                             Red       
Colour:                                Red to a deep red that can appear almost black.
Cleavage:                            Is fair in four directions forming octahedrons.
Occurrence:                       Oxidized zone of co...

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Mineral of the Month - Galena

April 25, 2011

 
Crystal system:                 Isometric                                             Hardness:                            2.5 – 3.0
Density:                            7.5 average                                         Streak:                                 Lead-grey
Colour:                             Silver lead-grey
Cleavage:                          Perfect, parallel to the faces of the cubic crystals
Occurrence:                       In vein deposits and irregular pockets w...

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Mineral of the Month - Kutnohorite

March 26, 2011

  
                  
Kutnohorite from Wessels and N’Chwanning mines (KMF). Specimens and photos by – J de Jongh
 
Crystal system:                Trigonal                                 Hardness:            3.5 - 4
Density:                               3.11 average                         Cleavage:            perfect
Streak:                                 white                                   
Colour:                                 white, light brown, light yellow, light...

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