Wednesday Feb 22

Grading

Opal Identification

opal identification opal identification
GEMMOLOGICAL LABORATORY FACT SHEET:

Chemical composition of Opal:

Si02nH20 – Hydrated Silica.

• Water content in Precious Opal 3-10%.

• Water content in Potch or Common Opal 2-20%

• Impurities are Oxides of:

Aluminium (~2.5%), Calcium (~1%), Sodium (~0.4%), Iron (~0.3%), Titanium and Magnesium (~0.1%) and in much smaller traces Zirconia, Manganese, Copper, Nickel and Cobalt.


Chemical composition of Boulder Opal:

SiO2 at 28%, Fe2O3 + Al2O3 at 68%, H20 at 4% approximately.

Hardness on Mohs Scale 1-10:

Opal is 5.5 to 6.5 on the Mohs Scale (Note* A relative not an absolute scale)

Scratch
Hardness
(Mohs)
Mineral used
for resistance
Comparison
Simple Hardness
tester
Cutting
1 Talc Can be scratched with fingernail 0.03
2 Gypsum Can be scratched with fingernail 1.25
3 Pearl, Bone
Can be scratched with copper coin 4.5
4 Fluorite, Marble Easily scratched with knife
5.0
5 Glass, Obsidian Can be scratched with knife
6.5
6 Opal, Turquoise, Garnet Can be scratched with steel file 37
7 Quartz,Tourmaline Scratches window glass 120
8 Topaz, Aquamarine Can be scratched with corundum 175
9 Sapphire, Ruby Can be scratched with diamond 1,000
10 Diamond Can be scratched with diamond 140,000


Specific Gravity (SG):


• White or Black Opal 2.10-2.30
• Boulder Opal 2.60-2.80

Note* SG indicates the relation between the measured gemstone and an equal amount of water, its numerical value is between 1 and 8, values under 2 are considered light, those from 2 to 4 normal and over 4 heavy.

Cleavage:


• None in White or Black Opal.

• Distinct in Boulder Opal which may split along an Opal vein to produce two faces of Opal, due to the angle of the Opal vein’s microstructure growth in the cavity.

Referred to as 'Splits' or a 'Split Pair'. When the colour bars or veins are true, that is fairly flat and straight; the splitting operation performed by an expert lapidary will result in the Opal remaining entirely adhered to both sides of the host rock.

spellbound.jpg


Fracture: Conchoidal (glass-like)

Lustre: Vitreous (glass-like)

Streak:

• White or colourless for White or Black Opal
• White or colourless on the top-side and brown on the bottom-side for Boulder Opal

Diaphaneity: Transparent, Translucent or Opaque

Optic Character: Opal is a singly refractive gem. Light which enters an Opal remains as non-polarized beams, and travels through all directions of the stone at the same speed.

Refractive Index (RI): 1.37 – 1.47; Opal has no birefringence, each one has a single RI figure in this range.

Pleochroism: None.

Note* Pleochroism is caused by the double refraction of light and should not be confused with the play of colour which characterises Opal.

Crystal System:
Opal is an Amorphous mineral, it does not occur in a particular crystallographic form. It is a replacement mineral which occurs in veins, nodules and fossils. Potch or common Opal does not have an orderly atomic structure, only precious Opal has a regular internal structure.

Atomic Structure: Electron microscope Studies (40,000x magnification) have revealed Opal is composed of tiny spheres of transparent hard silica, 0.01 to 0.0005 mm in diameter, sitting in a bath of hydrous silica.

refraction_grating.jpg

Light passes through the spheres in a straight line but when it hits the spaces between the spheres, containing silica in solution; it is bent and deflected at different angles. The overall effect of the silica arrangement is to produce a diffraction grating which breaks up white light into its constituent parts producing the visual phenomenon known as ‘play of colour’. According to the sizes of the spheres, varying colours of the spectrum are diffracted. Red colour is attributed to larger spheres ~4000 Å in diameter, while green opal spheres are ~2500 Å. Note*(Angstrom units; 1 Å = 10 -7mm) The size of the spheres diminishes through the spectrum; RED_ORANGE_YELLOW_GREEN_BLUE_INDIGO_VIOLET. Violet is attributed to the smallest spheres.

Electron micrographs:

precious_opal_under_electron_microscope.jpg potch_under_electron_microscope.jpg
Precious Opal

Common Opal

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In precious opal the spheres are uniformly sized and arranged in an orderly 3 dimensional grid, whereas in common opal the spheres vary in size and shape, discovered by Australian CSIRO scientists Darragh and Sanders in 1965.

Field Observation: Opal seams generally show a layered structure similar to the horizontal bedding in its sedimentary host rock. Layers may differ from adjacent layers in body colour, transparency, or colour patterns.

Fluorescence:

Black and Boulder Opal do not fluoresce.

Crystal and Light Opal, mostly from South Australia, fluoresce a cloudy white under U.V. light.

Phosphorescence:

Fluorescence in South Australian Opal (origin: Andamooka, Coober Pedy, Mintabie) is normally followed by a rather prolonged phosphorescent afterglow.

This phosphorescent afterglow is hardly perceptible in Gilson Light Opal.


Opalescence: The milky-blue or pearly appearance of common opal, opalescent glass and moonstone is caused by internal reflection of short wave, mainly blue light. This optical effect is due to the scattering of light by particles of matter in its path, such as is caused by a ray of light illuminating dust particles in the air of a room. Opalescence should not be confused with play of colour.

Chatoyancy: The Cat’s eye effect is caused by the reflection of light from multiple parallel needles or fibres which are inclusions in the stone. This phenomenon is most effective when the stone is cut en cabochon in such a way that the base is parallel to the fibres. A chatoyant Opal may otherwise be referred to as having a rolling-flash pattern, when the gem is rotated the cat’s eye glides over the face. Because Opal is predominantly cut en cabochon Cat's eye Opals are not the rarest occurence, though good examples with play of colour are hard to come by. rollingcatseyeboulder.jpg

Asterism: Created through reflection of light by thin fibrous or needle-like inclusions that lie in various directions. There are four rayed, six-rayed and twelve-rayed stars in Sapphires. However asterism is an extremely rare find in Opal, very few examples of Star Opals have been recorded, including three and six-rayed stars. Sometimes rare patterns may be termed 'Star' or 'Windmill' pattern, these are not neccesarily the same phenomena, they are usually more static with broader grains (rays) and a central point which does not move upon rotation of the stone.

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Detection of Modified & Man-Made Opals:

Detection of Enhanced Opals:

Treated matrix: Include Andamooka Matrix and Sandstone Opal from Queensland, referred to by the miners as Fairystone.

Matrix never transmits light and may be detected by their porosity, lower hardness and lower density (SG 1.98-2.05).

Under magnification tiny black spots can be seen in the surface colour of these stones and poorly treated examples may show uneven patches of body tone.

The back and side colour is nearly always the same as on the face of the stone (as per synthetic opal) and these stones are often cut with a flat back and bevelled setting edge.

A porous surface may be observed under loupe on all or parts of the stone.

Detection of Composites:

Composites: Doublets & Triplets

triplet_in_profile_opalGenerally detected by inspection of the join around the girdle of a stone.

Triplets are detectable when viewed from the side by the transparency of the quartz cap and planes of seperation and coloured cement may be visible.

When mounted doublets will be harder to identify and may need to be inspected under magnification to locate bubbles in the glue.

If the stone has a boulder backing, look for ironstone inclusions travelling from the face into the body of the stone which indicate it is natural. If the stone fluoresces it is a boulder doublet.

A pin heated with a naked flame can be pushed into the join line it should penetrate easily if the backing is actually powdered ironstone in an epoxy resin.

Detection of Opal Simulants:

Natural: Some multicoloured stones may appear like Opal to the untrained eye. Often these natural stimulants are presented as composites.

Labradorite Feldspar (definite cleavage and banded twinning)

Ammolite (FossilIsed shell of Ammonite an inverterbrate reminiscent of Black Opal RI 1.52-1.67, SG 2.78)

Paua Shell

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Imitation: Opal can be confused with Glass and some plastic imitations.

Glass (aka. paste) is simply imbedded with iridescent foil or as a doublet using opalescent (milky) glass. These are easily detected on sight or with the use of a loupe.

Plastic Simulants can be similar to Gilson in appearance, yet contain substances not found in natural Opal and are much lower in density, hardness and SG. These simulants are often highly porous and have a waxy texture.

Detection of Synthetic Opal

Synthetic: ‘Gilson’ Black and White Opals have all of the gemmological properties of natural Opal and are also heat resistant. There are several points of detection for this man made product:

Freedom of inclusions like potch or sand, and a stone which looks too perfect.

Gilson White Opal does not fluoresce under UV light unlike most natural white Opal. After Longwave UV is turned off the synthetic material phosphoresces for a much shorter time than natural Opals.

Very regular patterns and play of colour, with colours always arranged in uniform layers on vertical columns.

Under magnification a mosaic pattern showing crenellated margins can be seen wihin each patch of colour, this is also described as resembling a ‘snakeskin’ or 'fishscale' effect.

gilson_opal_Black

Sources & Image Credits:

AUSTRALIAN PRECIOUS OPAL, Andrew Cody, 1991; Diagram: Refraction Grating of Light

Emil Weis Opals Collection; Photo of Opal Cats-eye

GEMSTONES OF THE WORLD, Walter Schumann, 1976; diagram: Moh's Hardness scale

HANDBOOK OF GEMSTONE IDENTIFICATION, Richard T. Liddicoat, Jr., 1990

OPAL IDENTIFICATION AND VALUE, Paul B. Downing PhD., 2001. (Photo of Star Opal)

THE Opaline COLLECTION; Photo of 'Spellbound' Boulder Opal Splits

Opal Module, GAA course notes, Anthony G. Smallwood, 1998.

 

Evaluation of Opal

Opal is a complex stone to evaluate and this task falls mainly in the hands of experts with years of experience.

There are eleven more facets to an Opal than the 4C's (Colour, Clarity, Cut, Carat) used to grade a Diamond.

The factors outlined below provide a concise guide to the foremost influences on an Opals value:

Type of Natural Opal? Type or Variety alone does not affect price.

Type 1 Type 1 Type 1
Type 2 Type 3
Black Opal Dark Opal Light Opal Boulder Opal
Matrix Opal
Active Image darkOpalPair_LR lightopal_LLR
Boulder_gem_windows_2_LR
boulder_opal__matrix
N1,N2,N3,N4 N5,N6 N7,N8,N9 N1 to N9
N1 to N9
opaque opaque/translucent opaque to transparent opaque/translucent opaque/translucent

Variety? Black, Black Crystal, Semi Black, Dark Grey, White, Crystal, Light Grey, Jelly, Boulder Opal, Boulder Opal Matrix, Yowah Nuts, Andamooka Matrix etc.

Body Tone? The first point of price differentiation; a dark to black background is generally more desirable than a grey or milky-white background.

Opal Nomenclature Body Tone Scale

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BLACK_lrLIGHT_DARK_LR

 

Transparency? Light Opal of the 'Crystal' variety is found on most Opal fields and is transparent. A dot placed on the back of a stone using a black felt pen should be clearly visible from the face. Black Crystal may be transparent to translucent when held up to the light however it is exempted from the above test due to body tone. The majority of solid Opals are translucent, transmitting and diffusing light so that objects beyond cannot be clearly seen. Crystal Opal from South Australia, particularly in red stones, may posses superior hues of rich red. However the clarity and purity of Andamooka Crystal, coupled with brilliance and relative rarity, make it the more valuable stone quality for quality. Most Lightning Ridge Crystal is cut in a pleasing high dome which enhances the depth of pattern. A transparent Jelly Opal or Crystal Opal will usually be more desirable than an opaque White 'Milky' Opal. Conversely Black Opals with an N1and N2 body tone are opaque and may fetch the highest prices acheived per carat.

Brightness? Vividness of colours is of paramount importance – the brightness of an Opal is directly related to price. It is not uncommon to observe several levels of brightness in the face and variation in a stone's body tone. An assesment is made on the overall impression of a stone. One of three categories can be selected: 30%=Subtle, 30-70%=Bright, 70%(+)=Brilliant.

Directionality? Relates to colour display and how the hues are arranged on the face of a stone. When rotated through 360° in 90°segments most opals will show a marked difference at each turn. Many showing a good play of colour at one angle, can be nearly blank from one or two other angles and a price penalty is imposed dependent on the severity of the characteristic. 'Broad' or 'Flash' pattern stones often display this characteristic. Most stones look best in one particular orientation, some need to be tilted to be appreciated whereas the finest Opals are non-directional.

Distribution? Opal quality is markedly affected by the ‘depth’ of pattern and amount of 'fire' showing on the face. This factor is judged from the stone’s best angle. Very few, with the exception of 'Flash' pattern stones, will show 100% of the face covered in colour. Consequently a sparse ‘distribution’ of colour attracts a lesser value.

Saturation? Refers to the dominance of hue in the fire colour. Rich saturated hues; emerald green, rich orange etc are always present in the finest gem quality stones yet even pastel tones if bright can make a top quality stone. Conversely subdued brightness and pale pastel hues can only indicate, at best, a commercial quality stone.

Fire? The dominant hues in an Opal are referred to with the post script ‘-fire’ eg. green-fire or multi-fire (multi-coloured). The spectral colours (red, orange, yellow, green, blue, indigo, violet - in order of value) are usually combined in varying amounts in most Opals. The predominant hue is listed first with the main secondary hue following, eg green-blue. The predominant hue should be at least 50% to 70% of the total fire (play-of-colour), the second or supporting hue should be around 20% or more.

Some combinations are far more attractive than others, eg red-blue or green-blue when hues are intense, while red-orange and green-multi-fire are not as desirable. Gem quality stones with a predominance of red or orange are enhanced by a complimentary touch of vivid blue.

Red Opal is the rarest and most valuable and a predominantly red stone may potentially display all of the spectral colours, if so it may be referred to as ‘multi-red’. Bearing in mind that absolute value depends on brightness, pattern and body tone; red and multi-coloured Opals are rarer than green-orange, blue-green and blue Opals in that order. Given all other factors are equal an Opal containing red can be valued greater than a blue-green-yellow Opal by a factor of up to 3 times.

Pattern? Almost as important and when combined with brilliance may increase price manyfold.

peacockpattern.jpgbroadflash

straw.jpg

chaff/straw

ribbon.jpgribbon cats_eye_rolling_flash.jpgrollingflash
floral.jpgfloral

blue.jpgstraw (all blue)

harlequin.jpgharlequin

pinfire_pattern.jpgpinfire

flagstone.jpgflagstone peacockfloral.jpgribbon & floral hexagonal.jpghexagonal harlquin scan0029.jpgchinese writing

Generally a larger pattern is more valuable than a smaller pattern Eg. ‘Harlequin’ is the most highly prized pattern whereas ‘Pinfire’ is a more common pattern. The descriptions may be termed otherwise, eg.'Broadflash' may be called 'Peacock' pattern, and the 'Cat's Eye' phenomenon is usually referred to as 'Rolling Flash' by the Opal trade.
A vivid pattern is more valuable than a static less playful one. A lively stone posses depth or saturation of colour and pattern.While every Opal has a unique pattern, there are seven categories of patterns that all Opals fit within: Pinfire, Flash, Broad Flash, Rolling Flash, Harlequin, Rare Patterns and Picture Stones. Over 90% of stones have Flash and Broad Flash patterns.

Shape? Most often dictated by the rough form. Most Opals, particularly Black Opals, tend to be fashioned as ovals and because opal is cut ‘en cabochon’ or with a domed surface these features have traditionally been preferred for jewellery aesthetics and calibration purposes.

However, most Boulder Opals are cut as free shapes which can lend themselves to more distinctive designs. In the last decade there has been a strong trend towards cutting freeform 3-dimensional shapes from most gem quality Opal. By sculpting the rough, yield may be maximised in terms of weight and spread, aesthetic talent must be applied to balance the stone's lapidary design.

Proportion? A stone with a domed surface will be more valuable than one with a flat or undulated surface. This is because the domed stone has more depth from which to emit play-of-colour. The ratio of the colour bar with play-of-colour to the thickness of potch or ironstone backing should be balanced and have a suitable setting edge for jewellery manufacture. Poor cutting and polishing will significantly reduce a stones value. Some stones have been cut disproportionately, a stone may have been left too thick (heavy on the potch or ironstone backside) relative to its spread or face area. Consideration is made of a stone's proportion and aesthetic balance when determining the absolute value per carat.

Inclusions? Not uncommon in the back of stones, generally these are small sand-spots and do not affect price drastically. However marks or cracks that are noticeable in the face of the stone will have a marked effect on the price of an Opal. Visible inclusions may include; patches or lines of potch, 'webbing', 'sand spots', crystals of gypsum and ironstone in the face of Boulder Opal. 'Windows' in Black or Boulder Opal where there is an area of transparency in an opaque Opal's body that allows light to enter through the back of the stone and so dilute its play-of-colour are detrimental to price. Certain types of sand and other inclusions are indicators of origin.

Origin? Australian Opal mining fields are at:

Adavale, Andamooka, Beechworth, Coober Pedy, Coocoran, Grawin, Jundah, Koroit, Kynuna, Lambina, Lightning Ridge, Mintabie, Opalton, Queensland, Quilpie, Sheep Yard, South Australia, Tintenbar, White Cliffs, Winton, Yaraka,Yowah.

Weight? Measured in Carats (1carat=0.2 Grams; 1kg=5000carats).

Prices per carat are generally at their greatest for exceptional stones between 3 and 5 carats and up to about 10 carats, after which larger sizes may become less commercially viable for jewellery purposes and value per carat tends to decrease.

 

Sources & Image Credits:

A JOURNEY WITH COLOUR, Vol I & II, Len Cram (Photos: various patterns)

AUSTRALIAN PRECIOUS OPAL, Archie Kalokerinos, 1971.(Photos:Hexagonal Harlequin, Pinfire)

AUSTRALIAN PRECIOUS OPAL, Andrew Cody, 1991. (Photos: Brilliance Scale)

OPAL IDENTIFICATION AND VALUE, Paul Downing PhD., 2001.

Crystal, Boulder and Black Gems from the Opaline Collection

A NEW ERA FOR NOMENCLATURE, Australian Gemmologist. 19, 486-496., Anthony G. Smallwood, 1997.

OPAL MODULE, GAA COURSE NOTES, Anthony G. Smallwood, 1998.

THE SMART CHART, Peter Evans, 2005.

NCJV OPAL GRADING & PRICING WORKSHOP, Ralph Pownall, 2011.

Australian Opal

Classification of Precious Opal

‘Play of Colour’ is a unique visual phenomenon which sets precious Opal apart from all other gemstones.

Also known as 'Fire'; An Opal may display one or more, and sometimes all of the spectral colours. These colours are seen within the grains of a pattern.

As the stone is viewed from different directions, rotated and tilted, the colours of each grain may change or disappear.

Australian Opal

 

Types & Varieties of Natural Australian Opal


TYPE 1 - NATURAL; 'Light, Dark & Black Opal'

Australian Opal Black Opal has a blue-black to charcoal body tone and is mainly found at Lightning Ridge in New South Wales. The dark background serves to highlight the colour-play of dramatic spectral flashes. Fine examples of this variety are the most expensive per carat and rival diamonds in price. Black Opal is found as what the miners call ‘Nobbies’, these are fossil replacements of corals or sponges. During its formation, the replacement of organic material by Silica resulted in carbonaceous material or impurities like titanium impregnating the mineral structure giving Black Opal its body colour.

(Variety: Black *(pictured), Black Crystal)
dark_opal

Dark Opal has a smokey to dark grey body tone and may be found at Lightning Ridge NSW. In South Australia Mintabie is famous for Semi Black and Dark Crystal Opal, as are certain fields at Andamooka and Coober Pedy.

(Variety: Semi-Black, Dark Crystal *(pictured), Dark Grey, Smokey Crystal, Smokey Jelly)

Australian Opal Light Opal has a body tone ranging from milky white to transparent. Light Opal is the most common variety found at most fields but mainly at Coober Pedy and in South Australia. White Opal gives the full colour array on an opaque background, whereas Crystal Opal is transparent to translucent without milkiness and has bright colour flashes suspended in its midst. Crystal is superior to white, grey and jelly. Jelly Opal exhibits a moderate play of colour within a transparent background.

(Variety: White *(photo), Grey, Crystal, Jelly)

TYPE 1

Body Tone Scale

chart

TYPE 2- NATURAL 'Boulder Opal'


Boulder Opal is found in south west and central Queensland and can be light or dark in appearance. Boulder Opal forms as veins within ironstone concretions and is presented as a solid (one piece) since it is naturally attached to the host rock.
Boulder Opal may display the same darkness and brilliance as gem Black Opal yet it is more affordable and is generally sold at approximately one third of the Black Opal carat price. Boulder Opal is very durable due to the ironstone backing the opal forms on, which the cutter retains and polishes during the lapidary process.

The water content in Boulder Opal is very low, it almost never cracks or crazes as it ages and is considered the most stable type of natural Opal by many experts.

Variety of Boulder Opals:

1) Boulder Pipe

2 ) Black Boulder (green-orange fire)

3) Gem Boulder (split pair)

4) Black Boulder (red fire)

5) Yowah Nut Opal (split-sawn pair)

Australian Opal Active Image
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colour_in_gem_boulder
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TYPE 3 - NATURAL 'Matrix Opal'

Matrix Opal - is silicified sandstone or ironstone which is intimately diffused with Opal as infillings of pores or holes or between grains of the host rock in which it was formed.

Opal is sometimes encased in or intertwined with the Boulder concretion creating ‘Boulder Matrix’, ‘Yowah Nuts’ and other interesting textures sometimes referred to as ‘picture’ or ‘fun stones’.

1) Light Boulder Yowah Kernel

2) Boulder Opal Matrix

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boulder_opal_matrix.jpg

 

Modified & Man-Made Opal

TREATED OR ENHANCED STONES

Treated Matrix - Although some rare examples may actually resemble Black Opal in their natural state, the vast majority of 'Andamooka Matrix' from South Australia, and 'Fairystone' (Sandstone Opal from Queensland) are artificially stained or blackened to enhance their appearance and may also be 'impregnated' with plastic stabilizers to improve the finish.

Heat & Acid Treatment - Since the 1950's miners have treated the rock in sugar solution then carbonizing it by gently heating in concentrated sulphuric acid. Carbon is deposited into its pores by a process involving soaking Opal impregnated with various organic solutions and applying heat up to 500 degrees Celsius.

1)Treated Andamooka Matrix treated_andamooka_matrix

The rough material is fairly massive in occurrence and has been found across all the Opal fields. In the rough state it is a muddy-grey to orange porous rock and lacks fire, once treated this stone may be startling in quality. This versatile and relatively inexpensive material has applications in jewellery, carvings, clock faces, mosaics, inlays in furniture, tiles, paint finishes etc.

Reputable Gem dealers have a duty to disclose such modifications to the buyer.


MAN-MADE STONES


Composites - Doublets & Triplets are made using a slice of Light Opal and adhering it to a backing of black potch, plastic or boulder.
These are not investment quality stones but generally cheap products aimed as souvenirs. They lack durability and exposure to moisture can result in the opal veneer separating from its’ backing.

doublets.jpg
Doublets are made by gluing a slice of Opal to a black backing which enhances the reflection of colours from the Opal.
triplets.jpg
Triplets are made by adding a magnifying crystal top to a thin opal doublet.

Composites are detectable if the stones’ edges are examined, definite layers can be seen, under magnification.

However some Boulder Doublets may display an irregular or wavy join line as a mixture of powdered ironstone and resin may be used to imitate the irregularity of natural Boulder Opal.



SYNTHETIC STONES

Gilson Black and White Opals have all of the gemmological properties of natural Opal. The discovery of the ordered sphere structure of precious opal led to its synthesis by Pierre Gilson in 1974.

In 1980 Kyocera Corporation of Japan began producing Inamori black and white synthetic Opal. Russian manufacturers are also producing synthetics.


gilson_cutstone.jpggilson_under_magnification.jpg

 

IMITATION STONES

Made simply by imbedding iridescent foil in opalescent (milky) glass Opal imitations date back to ancient times.

These are easily detected on sight.

Slocum Stone made of glass (SG 2.45, RI 1.49-1.515) was the best Opal imitation available until 1978 when the Japanese produced plasic simulants that are somewhat more convincing and similar to Gilson to look at. This material has the same refractive index (RI 1.45) as natural Opal however it is lower in density (SG<1.58), often highly porous with a waxy texture.

plastic_imitation_opal.jpg

 

www.bolda.com.au - 100% NATURAL AUSTRALIAN GEMS & JEWELLERY

 

Sources & Image Credits:

WITHIN THE STONE, Bill Atkinson, 2004. (Photo.1: Phenomenal - Play of Colour)

THE Opaline COLLECTION, Exceptional White, Boulder & Black Opals

HANDBOOK OF GEMSTONE IDENTIFICATION, Richard T. Liddicoat, Jr., 1990

NCJV OPAL GRADING & PRICING WORKSHOP, Ralph Pownall, 2011.