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Elise

Joined: 22 Dec 2009
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Posted: Jul 25, 2010 15:23 Post subject: Re: Pleochroism in minerals |
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John S. White wrote: | The Smithsonian Institution has a great spodumene (kunzite) crystal from the Urucupa mine, Itambacuri, Minas Gerais, Brazil. Photos of the three different pleochroic colors it displays appeared on the cover of Mineralogical Record, November/December 1974. When viewed normal to the long direction, it is either lilac or green depending on which side is facing you and when viewed from the top or bottom it is magenta. The crystal is perfectly transparent and measures 31 cm in length. |
In the course of editing a paper for friend about the history of kunzite, I realized that this crystal John refers to is also that pictured in The National Gem Collection (J. Post), page 108 - in absence of the MinRec from 1974, one can go to this book to see the extraordinary example of pleochroism John is talking about (this book is often found in public libraries). However, John's picture on the MinRec cover shows more contrast between the amethystine (or lilac) viewed along a lateral axis vs the magenta looking down the c-axis. The green of the other view is what is amazing to me; as startling as the green pleochroic color found in different varieties of zoisite.
On the facing page is an image of a faceted tanzanite which makes an interesting pleochroism composition: the tanzanite is resting on a mirror such that the reflection of the other side of the stone contrasts nicely with the face-up color; purple to blue respectively.
The above paper on The History of Kunzite by Mark Mauthner will be published soon in Rocks and Minerals; it is a wonderful article by a gifted writer (as many of you who know Mark would agree he is). When the pleochroism thread shifted to kunzite earlier, he had given me permission to share one of his other kunzite pictures which he had posted on his blog last year (not sure if it will be included in the article) - it shows the color looking down the length of the crystal and is an image I find iconic in many respects; not least of all while thinking about him down in that mine helping to dig these amazing crystals out!
Best wishes,
Elise
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Photo by Mark Mauthner December 2009, posted with permission. "The Oceanview mine near Pala in north San Diego County. On the 5th of December, late in the afternoon, Jeff Swanger (the mine owner), Steve Carter and I opened up a newly found pocket and extracted some of the finest kunzite unearthed in the Pala District in many decades. Kunzite is the pink to purple gem variety of the mineral species spodumene. This photo was actually taken last Saturday when a number of visitors were present and more gems were being hauled out of the expanding cavity. This is one of those pieces after it was briefly rinsed using the water supply we have underground; it is being lit by one of the miner's lamps." |
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Jason
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Posted: Jul 25, 2010 19:51 Post subject: Re: Pleochroism in minerals |
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I have a tanzanite..may have posted about it before....4 color pleochroism..maybe the only "quadchroic" stone there is
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Paul S

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Posted: Jul 26, 2010 09:48 Post subject: Re: Pleochroism in minerals |
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Those are all very nice examples of pleochroism, well done and thank you everyone!
I am fascinated by the tanzanite from amethystguy, I have never read or heard about 4 colours, can you explain how this would be possible? I thought there was the maximum amount of colours, due to the fact there are only three axes in three dimensional space.
I was a bit confused after reading some more about this subject, but then I found out that we are all actually talking about two kinds of pleochroism:
1) by looking through a crystal along the different axes, different colours are visible.
2) by shining polarized light through a crystal and then changing its angle will change its colour.
These two are of course linked by the fact that pleochroic minerals are anisotropic, but this can be tested in the two aforementioned different ways. I am not sure though if both effects are always present in the same mineral or that one can be present without the other.
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Jason
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Posted: Jul 26, 2010 13:27 Post subject: Re: Pleochroism in minerals |
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It was sent as a test sample stone to a gem lab and well known gemologist..he saw it online and contcted me wanting to test it. With the sudden influx of so called "mardi gras" tanzanite he wanted to determine if all the cut stones coming out of thailand were treated in some new or unknown way. After recieving the stone and running all manner of test on it as a base sample in the rough to then later on determine what the cut stones would show he said something to the effect in his 30+ years being a gemologist and testing, lookig, seeing all kinds of stones this was the first one he saw that showed 4 pleochroic colors
gem lab wrote: | "they are not bi-color.. that are quad-color. Purple, blue, yellow, green. Which negates that idea of calling it tanzanite as that would not fully define what we have. These are potentially quite remarkable stones on both a gemological and marketing level.
Once we can establish exactly the gemological condition of the material, I see the marketing potential of this material as quite remarkable.
I will try to get some images posted up before I leave for Tucson. I believe that this will be the first time in my 39 years at this that I have seen a gemstone offer 4 colors in the same image." |
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Matt_Zukowski
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Posted: Jul 26, 2010 21:31 Post subject: Re: Pleochroism in minerals |
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I am confused. What exactly does this stone do when you change its orientation? Does the blue area in the picture change to purple and the green area turn to yellow? Is the whole stone one color in some orientations? Does the green area in your picture go through one set of colors as you change orientation, and the blue area another?
One possibility is that you have a trichroic tanzanite with an area colored by something else, so that what you see are three colors depending upon orientation superimposed, in one area, on some other color due to something else?
Another possibility is that you have an xtal with different varieties of zoisite in different areas. I have a spodumene from Urucum that appears to be a single xtal but has different pink and green areas ( https://www.mineral-forum.com/message-board/viewtopic.php?p=5716#5716 ). I would think that it is more accurate to say the two areas display different pleochroism, not that i have a quad- or hexa-chroic xtal.
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Jason
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Posted: Jul 26, 2010 22:58 Post subject: Re: Pleochroism in minerals |
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"I would think that it is more accurate to say the two areas display different pleochroism, not that i have a quad- or hexa-chroic xtal. "
Matt, when you can see all 4 colors with the dichroscope I think it's accurate to call it a quadchroic(don't know if that word exist since these crystals may be the only 4 pleochroic stone there is) ..heated to produce blue which is dichroic(since it's heated) and the green which is a different dichroic set..that equals 4 pleochroic colors through the dichoscope..
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John S. White
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Posted: Jul 27, 2010 04:37 Post subject: Re: Pleochroism in minerals |
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Amethystguy - it appears that you did not answer Matt's question. Are some of the colors "fixed" or do all of them change with orientation? I suspect that the blue green shown in the photo may be due to something other than pleochroism, as suggested by Matt.
_________________ John S. White
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Jason
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Posted: Jul 27, 2010 05:03 Post subject: Re: Pleochroism in minerals |
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not really sure what you mean John? The crystal is blue and green..down the opposite axis it's purple and yellow..with a dichroscope it shows the face colors which you guys see in the picture but it also shows the dichroic properties of the blue which is purple down the c-axis and the green which is yellow down it's c-axis.....thats what a dichroscope does.
The crystal is colored by vanadium....it has been heated so it lost it's trichroic properties and now is like a typical tanzanite is..dichroic..if you take any regular tanzanite gemstone which is blue..when turned in the light it shows purple down the other axis..with a dichroscope you don't have to turn the stone..it shows both colors at the same time..so the blue portion shows purple down it's other axis..the green portion shows yellow down it's axis..
With both colors being in the same stone it shows 4 colors at the same time with a dichroscope..
even without a dichroscope showing 4 colors when orientated/turned by eye is a rare thing....can't think of any other that does..Robert James who used it and tested it said he has never seen another stone that did that except "mardi gras" tanzanite//zoisite which this was the first one he looked at. like this.....
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John S. White
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Posted: Jul 27, 2010 06:53 Post subject: Re: Pleochroism in minerals |
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Okay let me try to make my point better. That the stone has been heated complicates the issue, but in my view pleochroism is revealed through a change in color when the stone is viewed from different directions, without the introduction of a dichroscope. It is evident that your crystal has distinct blue and green regions when viewed at right angles to the largest surface. When turned 90° about the long axis, do these colors change or do they remain the same? If the green remains the same then I suspect that we are not witnessing pleochroism.
Additionally, but unrelated to the above, are you quite certain that a treated tanzanite cannot show three colors? I have seen many crystals that show rich purple, magenta and blue, but I don't know if they have been heated or not.
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Duncan Miller

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Posted: Jul 28, 2010 03:57 Post subject: Re: Pleochroism in minerals |
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John S. White wrote: | in my view pleochroism is revealed through a change in color when the stone is viewed from different directions, without the introduction of a dichroscope. |
A dichroscope can be used to detect pleochroism, but only two colours will be seen in any particular orientation of the crystal, and these will not necessarily be the most extreme colours. For instance, I have a strongly pleochroic tourmaline, which is a uniform bright pink viewed down the c-axis with a dichroscope, but only two shades of light green when viewed across it. A trichroic crystal would have to be viewed in various different crystallographic directions to see all three colours with a dichroscope.
If a crystal has colour zones, as the blue/green zoisite example appears to have, the different zones should have their own sets of pleochroic colours. A dichroscope could be helpful to distinguish these. I expect each crystallographic axial direction will have its own colour, but these will vary between zones, just as they would if they were in separate crystals of the same species but with different colours. The mineral is still trichroic, because that is a function of its crystallography.
Duncan Miller
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John S. White
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Posted: Jul 28, 2010 04:35 Post subject: Re: Pleochroism in minerals |
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I agree, but I am still hoping for an answer to Matt's and now my question.
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Jason
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Posted: Jul 28, 2010 18:30 Post subject: Re: Pleochroism in minerals |
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I still don't really get what your question is that i haven't already explained..
It's tanzanite..it is trichroic, it only becomes dichroic after heat treatment. heating zoisite can reduce pleochroism as in the case of tanzanite where the yellow, brown or green seen along the c-axis can turn blue upon treatment. which is what it has done on the blue side..the green side is has a different coloring agent..probably chromium..when viewed face up as in the pic it is blue on one half and green on the other half..when the stone is turned to look down the axis on the blue side and looking only through the blue side, not the long end into the green it turns purple. On the green side when viewed down the same axis as you looked at on the blue side the green area turns yellow(pale)...not down the long end but the short end.. The green does not remain the same it turns yellow when you turn the stone 90 degrees..it's tanzanite..it has been heated..regardless of the color of tanzanite pink, blue, yellow, green..it wll show trichoric properties..since it has been heated it has pretty much lost it's trichoric properties and is now dichroic on both the color..imagine if you cut the stone along the demarcation line between the blue and the green..wghat do you have..a blue tanzanite..it's other readily seen dichroic color is purple..now look at the green side..now you have a green tanzanite..when you turn tyhat stone it shows yellow as it's other readily seen dichroic color..now you just place them back together ..what does that give you??? 4 colors on one stone..just imagine a green and a blue tanzanite seperate then taking them and gluing them together..still will have there own dichroic colors..not when viewed down the axis that looks from the green into the blue but when the colors are side by side. With a dichoscope since it has a 90degree line if you run that line on the blue and on the green you can see 4 colors at once.
PINK : Pink, Green, Orange
GREEN : Green, Violet, yellow
YELLOW : Yellow, Violet, Greenish-yellow
ORANGE : Orange, Green, Violet
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John S. White
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Posted: Jul 29, 2010 04:40 Post subject: Re: Pleochroism in minerals |
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Okay, I feel my question has been answered. All I wanted to know was what happened to the green area when turned 90° about the long axis of the crystal and now I know.
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Elise

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Posted: Jul 29, 2010 09:36 Post subject: Re: Pleochroism in minerals |
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amethystguy wrote: | With a dichoscope since it has a 90degree line if you run that line on the blue and on the green you can see 4 colors at once. |
It sounds like you are using a dichroscope made with two pieces of polarizing filter at right angles to each other; either a London dichroscope or one of the small tubes that look very much like the calcite type, but which are made with filters. These sample two different adjacent areas, the former type a much larger area than the latter one. If you cross the border of a color-zone (without the zones overlapping in the path of the light somewhere back in the crystal), you might get 4 discrete colors in one view - two separate rays for each zone. That would make a nice photograph! Using a calcite dichroscope with a very small aperture would allow you to sample one area giving a side by side view of two rays at once. Regardless, with color zoning it will be very difficult to make a clean observation, not muddied by the two areas overlapping and still observing at the 3 different orientations in a biaxial mineral that give the maximum effect. I would still think you could also find the 3rd pleochroic color in each section if only you could adequately isolate that area in the right orientation; sometimes after heat treatment two directions will become very close in color which makes it appear that has become "dichroic" though a subtle 3rd color still can be found. There is quite a bit on dichroscopes and pleochroism on that page I posted a link to earlier in this thread.
If you don't already have it, you might like to get a copy of the 2009 Sept/Oct issue of The Mineralogical Record on Merelani Tanzania, there are several pictures of zoned tanzanite similar to yours as well as other colors of color-zoned zoisite. There is an update on color which compliments the 2008 paper "A spectrophotometric study of the thermal colour change of tanzanite" by Grant Pearson. I would also recommend older papers by Hurlbut "Gem Zoisite from Tanzania" and "On the pleochroism of vanadium bearing zoisite from Tanzania" by Faye and Nickel. On pleochroism, along with standard texts covering optical mineralogy, Darko Sturman has written several papers which illuminate optical mineralogy for gemologists; he has one in prepublication specifically on pleochroism as it pertains to gemological techniques. If Dr. Bassett and I ever finish the zillion different projects we are concurrently working on, we may also have a paper on pleochroic anomalies (or rather, surprises) - we spend an inordinate amount of time studying the subject. Duncan, that tourmaline would be fun to see; it sounds similar to what my friend Asbjørn observed when he first found the Usambara Effect tourmalines while working in Tanzania.
That all said, in appreciating the aesthetics of a particular mineral specimen of any type, isn't it only the eye-visible pleochroism which is considered? that is a dramatic or personally appealing change of color as you turn the crystal in your hand - or "face colors." The color of each of those views would be the combined color of the two rays for that orientation. None but the pleochroically obsessed would be whipping out their polarizing filters and dichroscopes - that would be me. I was lucky at the Rochester Symposium to tour around the vendor's rooms with Olaf Medenbach looking at tanzanite crystals in detail - he carries two filter sheets with him everywhere. As we were not potential buyers, this probably was annoying....but had we found a tanzanite with a pure red direction I might have mortgaged the house to buy it. Those at the symposium might also remember the large kunzite specimen we were studying with very strong eye-visible pleochrosim. It also had a fantastic screw dislocation ...but that is a different argument.
Best wishes,
Elise
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Elise

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Posted: Aug 31, 2010 19:54 Post subject: Re: Pleochroism in minerals |
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I am finally getting to unpack from the Springfield show. I was very happy to find a few slices of chiastolite which have "open" cores. Just rocking them back and forth over a non-polarized light source dramatically exhibits the eye-visible pleochroism which andalusite is famous for. Some of the inclusions radiating out from the core show the same color change and add color to the rim which is almost colorless otherwise.
Cheers!
Elise
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A slice perpendicular to the c axis of chiastolite with an "open" core viewed with transmitted non-polarized light. Approx. 2.5x2.5x0.5 cm; origin unknown. |
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