Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography
╳Discussions
💬 Home🔎 Search📅 LatestGroups
EducationOpen discussion area.Fakes & FraudsOpen discussion area.Field CollectingOpen discussion area.FossilsOpen discussion area.Gems and GemologyOpen discussion area.GeneralOpen discussion area.How to ContributeOpen discussion area.Identity HelpOpen discussion area.Improving Mindat.orgOpen discussion area.LocalitiesOpen discussion area.Lost and Stolen SpecimensOpen discussion area.MarketplaceOpen discussion area.MeteoritesOpen discussion area.Mindat ProductsOpen discussion area.Mineral ExchangesOpen discussion area.Mineral PhotographyOpen discussion area.Mineral ShowsOpen discussion area.Mineralogical ClassificationOpen discussion area.Mineralogy CourseOpen discussion area.MineralsOpen discussion area.Minerals and MuseumsOpen discussion area.PhotosOpen discussion area.Techniques for CollectorsOpen discussion area.The Rock H. Currier Digital LibraryOpen discussion area.UV MineralsOpen discussion area.Recent Images in Discussions
Identity HelpReal turquoise?
13th Apr 2013 06:25 UTCMeems
It's rough to the touch in some areas, no smell to it at all. I apologize for the photos. All I have is my phone camera so I tried to use my bright light to help with focus and detail. It was hard to get a good, clear close-up of the center piece! Thanks for any help! I am loving this site.
13th Apr 2013 09:54 UTCRock Currier Expert
13th Apr 2013 12:17 UTCOwen Lewis
The bad news is that the great majority of turquoise that reaches the retail market has been treated in at least one and maybe more than one way. - and that's ignoring all the 'imitant' stuff. If you like the item (it looks pretty) and you did not pay an arm and a leg for it, then have done, call it your turquoise necklace and enjoy it:-)
FWIW, the colour of the stones seems to vary a lot; IMHO that makes it *more* likely than not that they are not man-made or an imitant or dyed. Whether they have been 'stabilised' can't be guessed from a pic - but almost all is these days.. The 'beads' between the stones could be a number of things - including plastic.
If you are still curious, you can do a basic check for dyeing as follows. Dip the cotton bud in a bottle of acetone. Quickly touch the bud to a piece of absorbent paper to take of any acetone just waiting to drip out of the bud and run everywhere. Rub vigorously an area of one of your stones (away from the beads!) for 4-5 secs. If blue colour comes off onto the white cotton bud then the materal is dyed. However, if the stones have also been stabilised, this simple test may not always work.
Another tip before you try the acetone test. Touch a stone to your lips. Does it feel warm or cold? If cold, you have a mineral of some sort and if there is no cold sensation, it's probably plastic. Try this with a couple of 'known' polished stones and a piece of known plastic before you test the necklace, so you know the difference in sensation you to expect.
Me? I think I would just enjoy wearing it!
Good luck.
14th Apr 2013 19:43 UTCTim Jokela Jr
The color is a bit weird to my eye.
I think you can safely assume that it's treated in some way or another, like emeralds.
The only turquoise I'd really trust would come from the guy who mined it, and I'd expect to pay a bundle for it.
It'd be cool if you could de-string a bead and saw it in half.
I wonder what's inside!!!?
In cases like this, it pays to do business with a highly trained local jeweler, who keeps up on the latest simulants by taking courses every year, that you know and trust.
14th Apr 2013 20:31 UTCDon Saathoff Expert
Don
27th Aug 2013 10:30 UTCgeorgia reynolds
I agree with Don.
I have been testing for years, with some of these materials that are coming out it is hard to tell.
Do not forget that even most sapphires are treated now.
I like my stones to show their inclusions that shows me the path of the stone. It is it's birth mark so to speak.
Buy what you like and only pay the price your mind puts on it. Otherwise buy from somebody who knows what they are doing and is willing to give you a certificate to say your item is natural.
Best of luck
Georgia
10th Dec 2014 18:51 UTCMargaret
10th Dec 2014 19:09 UTCReiner Mielke Expert
10th Dec 2014 20:24 UTCOwen Melfyn Lewis
14th Dec 2014 00:21 UTCturtledove thrushe
14th Dec 2014 01:05 UTCAlex Earl 🌟 Expert
14th Dec 2014 02:56 UTCJacob Helton
14th Dec 2014 12:41 UTCJosé Zendrera 🌟 Manager
Please see:
https://www.google.es/search?q=blue+howlite&biw=1636&bih=1316&tbm=isch&tbo=u&source=univ&sa=X&ei=6IKNVJS4N8b3UpOfgoAP&ved=0CCcQsAQ
http://en.wikipedia.org/wiki/Howlite
1st Mar 2015 14:37 UTCSobia
Turquoise comes in Red too. But green is definitely a NO.
1st Mar 2015 18:08 UTCsteven garza
Understand, that nearly ALL turquoise, as time goes by, turns green; it's not fake, the copper just is making a different response. Since nearly no "turquoise" is really turquoise, but one of several Al phosphates that naturally have some Cu mineral inclusion/Cu substitution; this topic was brought up, on another thread, earlier that stated, that a study done on many "turquoise", from many classic American sites, was NOT turquoise. That's why it's going to be difficult to prosecute many dealers for calling THEIR obviously fake stuff, bcs, stuff we've been calling "turquoise, for hundreds of yrs., isn't either. Now, it's more a jeweler's term for a whole group of Cu bearing minerals that are amorphous & used for jewelry.
BTW, water exposure & air infiltration, over time, are the culprits for the color change.
Your friend, Steve
2nd Mar 2015 01:53 UTCOwen Melfyn Lewis
-------------------------------------------------------
> .......Since nearly
> no "turquoise" is really turquoise, but one of
> several Al phosphates that naturally have some Cu
> mineral inclusion/Cu substitution; this topic was
> brought up, on another thread, earlier that
> stated, that a study done on many "turquoise",
> from many classic American sites, was NOT
> turquoise. ....
So.... what do you say it the only 'real' turquoise Steve, and underwritten by what authority? Please see http://www.mindat.org/min-4060.html before responding. It's hard to see any of your claims reflected in that outline.
2nd Mar 2015 02:32 UTCAlfredo Petrov Manager
The same situation exists with other gems/minerals, like jadeite for example. I'm certainly not recommending that gemmologists post facto change the names of ancient gems just to "keep up" with the latest mineralogical species nomenclature; it is far easier to just recognize that definitions can vary slightly between different fields and leave it at that. There is no reason at all in my view to change the name of a gem just because it slightly crosses over some arbitrary chemical boundary, while stil maintaining the same color, hardness and other desirable physical characteristics - That would be stupid from a gemmological perspective, but not from a mineralogical one.
2nd Mar 2015 09:47 UTCsteven garza
Since the thread has been on jewelry type turquoise, that IS what I was referring to; not the MINERALOGICAL specimens, of xls, especially. Sorry, I should have made that more clear. True turquoise, in lapidary, for CENTURIES, is VERY rare; they didn't use XRDs etc., even when they had them, for the longest time, which are about the only way you can define what is what, anymore. Only recent work, on hundreds of specimens (without damaging them; something else that stopped previous research into the matter) has shown NO American turquoise, mineralogically, in any jewelry. Since planerite & the rest of the turquoise group (a GOOD sized group) all have similar characteristics/workability/color range, telling the difference, by the most experienced eye, just can't/shouldn't be done; as Alfredo pointed out & I've mentioned, on other topics, the mineralogical definitions aren't always in tune with the lapidary/gemological ones - many times by a long stretch.
Your friend, Steve
2nd Mar 2015 14:53 UTCOwen Melfyn Lewis
You still do not say what you think "real" turquoise to be. I cannot make sense your suggestion that it is an aluminium phosphate (when it need not contain aluminium) or that copper may or may not be present in turquoise. Come on, chum, what *is* your idea of the "real" turquoise?
@ Alfredo,
You make some good points but please consider.
- Turquoise is a mineral group name (as is also tourmaline). Gemmologists sometimes (e.g. turquoise and tourmaline) find using the group name much more useful for general purposes of trade regulation that fussing with the mineral species and their Heinz57 mixes.
- Within the group there is appreciable difference in the chemistry, structure and colour of what make be properly called turquoise.
- In the main (or completely?), turquoise is one of two (or possibly a mix of two?) binary solid solution series, plus the inevitable impurities that nature provides.
- Some thirty years ago, the great chemist, crystallographer and gemmologist, Dr Kurt Nassau (writing in a gemmological context) described turquoise as 'an aggregate of minute crystals of copper aluminium phosphate hydrate CuAl6(PO4)4(OH)8.5H2O, and made the point that turquoise is idiochromatic as a result of its copper content. A bit more prescriptive that the current mineralogical definition but perhaps nothing to argue over, 'Gems' used the same formula but with one less water molecule, pointing out also that FE is often associated with the chemistry. There is a very informative chapert in 'Gems) on turquoise, as I am sure you know.
From a gemmological perspective:
- Identification tests for turquoise are unusually weak, none being diagnostic. It may not be possible to distinguish with certainty high grade synthetic turquoise from the geologically formed. However, according to CIBJO (2013), synthetic turquoise is not now to be found in the market.
- The nondestructive tests of visible spectrum, microscopic examination and SG are the most commonly used
- Turquoise has no useful Raman signature but if a specimen (natural, synthetic or fake) has been polymer impregnated, this has a clear Raman signature.
- Most common sources of gem grade natural turquoise are the US, Iran and Egypt (Sinai) with an interesting and valuable minor source in Uzbekistan. Persian turquoise is graded into three main qualities with different visible characteristics
In sum - and as Rock said right at the beginning, turquoise is really a bit of a mess. As a gemstone, it is common but of limited importance. Most testing effort goes into the detection of fakes and treatments, with not too much concern, perhaps for exact chemistry of any given specimen.
2nd Mar 2015 20:26 UTCsteven garza
My idea of turquoise (no quotes) has been, is, & will always be the mineralogical one; as long as I deal in minerals, that's the one I'll discuss.
SINCE, we were discussing GEM turquoise, although I'm not much for gemological terms for "x" material, & since YOU haven't suggested another we could use, that everyone could agree with & use, for lack of a better way of communicating about said material, that's what I used those terms - I guess I'm adaptive to that sort of thing. Since, apparently, the use of that term PREDATES with fixing of it's formula, I'd say that WE may be misusing that name; maybe the turquoise WE know by it's present formula need to be changed (our term being the "youngster" meaning); what's do YOU think?
Your friend, Steve
2nd Mar 2015 20:52 UTCReiner Mielke Expert
As for the remark " Only recent work, on hundreds of specimens (without damaging them; something else that stopped previous research into the matter) has shown NO American turquoise, mineralogically, in any jewelry." I find that highly unlikely as that would imply that there is no turquoise (the species) at the hundreds of localities for turquoise in the US listed in Mindat !
2nd Mar 2015 22:35 UTCPaul Brandes 🌟 Manager
3rd Mar 2015 00:01 UTCDoug Daniels
3rd Mar 2015 00:33 UTCAlfredo Petrov Manager
3rd Mar 2015 01:00 UTCWayne Corwin
3rd Mar 2015 01:23 UTCsteven garza
YOU GOT IT! THOSE are probably the only COMPLETELY turquoise turquoise there is. During the xlization process, it would likely have a fairly stabile composition, apart from other turquoise group members, which would settle at differing rates; the nodules & veins, being amorphous, probably came out of solution SO fast, they never got a chance to properly separate & form individual xls - I guess you could say they became "turquoise group member soup".
Your friend, Steve
3rd Mar 2015 01:23 UTCAlfredo Petrov Manager
The RRUFF page for Lynch Station turquoise crystals shows it being pretty close to the Cu end-member.
3rd Mar 2015 01:50 UTCWayne Corwin
3rd Mar 2015 03:02 UTCDoug Daniels
3rd Mar 2015 03:35 UTCPaul Brandes 🌟 Manager
3rd Mar 2015 04:55 UTCDoug Daniels
3rd Mar 2015 14:05 UTCJamison K. Brizendine 🌟 Expert
When I was briefly at Western Kentucky University, we received quite a number of specimens from the Dos Pobres Mine in Arizona. The specimens we received contained veins of an unknown mineral we thought were turquoise.
We ran a bunch of samples in our XRD and to our surprise all of them registered as aheylite. We had our doubts, that this was aheylite, so some of the poorer samples we “spiked” with quartz, just to make sure our machine wasn’t taking a faulty reading. The XRD again read the quartz without a problem, but with the unknown mineral, it was still reading aheylite.
Just to confirm our findings, we sent the samples to a laboratory at the University of Kentucky. UK’s laboratory had deduced that these samples were a positive reading for turquoise, but the peaks it showed also had a very close match to both planerite and aheylite as well.
3rd Mar 2015 14:33 UTCOwen Melfyn Lewis
You talk of a 'real turquoise' and as 'true turquoise which is very rare' but decline to specify what you mean by this. You also say that 'recent work' (whose?) on hundreds of pieces' that 'has shown NO American turquoise, mineralogically, in any jewelry.'
Without explanation, that comes across just as a load of old cobblers ;-)
I have a cabochon piece of turquoise (with some quite attractively included matrix) from Kingman County, Arizona. I'll guess that there are a million+ other pieces of jewellery where the turquoise is of US origin. Or do you mean that turquoise is not found in the US (though most of us think it is). Again, to make sense of this you really do need to share with us what you think is the 'real/true/very rare turquoise' and where it is found,
If you mean that triclinic translucent monocrystals of turquoise that are large enough to be visible to the naked eye are rare, I could agree with you but, though pretty under the microscope, these are of little gem (commercial) interest. But even these are to be found in the US (Lynch Station, Virginia, I believe). The gem interest is in the aggregated form of such minute micro crystals that has an opaque/near opaque character. Like some other materials (e.g. lapis lazuli) the mineral composition is not fixed but varies within certain limits. The variable composition leads to some specimen being more attractive than others and, hence, also more valuable.
The USA is a leading source of turquoise for the gem trade, though little of it is considered to be of the finest grade. Historically, top grade Iranian turquoise is considered to be the best. Most of the turquoise deposits around the world (including those in the UK) are not considered to be of gem quality.
The standard trade reference book for the jewellery trade is 'Gems, their Sources, Description and Identification' (now called just 'Gems' from the current 6th edition). As said already this gives the US (esp. the south-western states) as a prime source of gem grade turquoise.
3rd Mar 2015 18:22 UTCD Mike Reinke
Also, I passed on a chance to get a Lynch station Va. turquoise last year, and now that I have a microscope, I regret that...
Thanks for everyone's input.
Mike
3rd Mar 2015 18:45 UTCOwen Melfyn Lewis
Yes, pity about that Lynch Station turquoise monocrystal that escaped you. I'd very much like to capture one of those myself - from any location.
3rd Mar 2015 20:42 UTCsteven garza
You seem to be having trouble separating "-ologies", which, in the very quote you used, DOES explain what I mean; what you need, is a sit-down", with someone you trust, who can make better sense of what I'm saying. Apparently, I'm not capable of expressing this in a way you'll absorb; my bad.
Your friend, Steve
3rd Mar 2015 21:31 UTCOwen Melfyn Lewis
And it's nothing to do with 'ologies'; just spit it out.
3rd Mar 2015 21:45 UTCDon Saathoff Expert
Don S.
3rd Mar 2015 23:04 UTCRock Currier Expert
However in the greater reality of the world, any blue stone set in jewelry made by Indians (even Asian Indians) will be called turquoise and no matter how much we may rant and rave about it, this greater reality will almost certainly never change in our lifetimes.
When talking about turquoise with someone we only need to ask enough questions to understand which reality they are coming from in order for polite communication to flow. Its very much like trying to settle on the definition for jade.
4th Mar 2015 00:01 UTCOwen Melfyn Lewis
The mineralogical view is that turquoise is either of two binary solid solution series that form triclinic crystals, right?
Rarely, such crystals are large enough (say 100 micron+) to see with the naked eye, right? But most times the crystals are smaller, requiring a microscope to identify them individually, right? These minute steep triclinic crystals form massive aggregations that are widely cut up and polished into pieces some cm+ across, to be used for ornamentation or set in jewellery.
How can does crystal size or crystal aggregation determine whether or not the mineral is turquoise? I don't think it does. Are calcite or aragonite any other species just because their crystals are minute and aggregated? I think not. What then is particular to turquoise for some to suggest that an aggregated crystalline form is in some way not 'real' and must be something else? A (say) 5mm monocrystal of turquoise may indeed be a rare form of turquoise but, methinks, that is all it is.
4th Mar 2015 01:26 UTCReiner Mielke Expert
4th Mar 2015 06:21 UTCAlfredo Petrov Manager
The first step in reaching an understanding or consensus is to admit differences in usage do exist, and that that is not necessarily a bad thing or an "error". Without that recognition, all discussion is hopeless and we might as well devote our time to more profitable issues.
Reiner, photos end up placed under "Turquoise" because either: a) they look like turquoise; or b) they've traditionally been called "turquoise" in the past. Are they really all turquoise, correctly identified? .....Without reliable detailed analyses, we'll never know. (Which is pretty much what one could say of most photos of most minerals ;-) )
4th Mar 2015 11:54 UTCDavid Von Bargen Manager
" Light blue or blue-green 'turquoise' from
many world-wide localities is actually planerite
rather than turquoise. Pure or nearly pure
turquoise is quite rare as well, and the mineral
from the Bishop mine, Lynch Station, Campbell
Co., VA, is the best high-purity, well-crystallized,
highly Cu-substituted turquoise (e.g. Schaller,
1912) that we examined. A re-determination of
the density of the turquoise that was analysed by
Schaller (1912) was made using methylene iodide
diluted with acetone: Dobs = 2.86(1); Dc~lo = 2.91.
Some material from Lynch Station is intermediate
between turquoise and chalcosiderite, and a few
samples of chalcosiderite were found as well in a
batch of assorted samples from the mine (J. Nelen
microprobe data, 1984, pers. comm.)."
http://www.minersoc.org/pages/Archive-MM/Volume_62/62-1-93.pdf
4th Mar 2015 18:35 UTCReiner Mielke Expert
I understand that similar issues exist for other minerals, however, unless I am misunderstanding this the chances are very good that most of the photos of massive turquoise in Mindat are planerite. Therefore to me it would be logical to place them under planerite and not turquoise (unless proven otherwise). Another better option would be to move them all to turquoise group. This also raises the more important issue of the localities for turquoise, is turquoise even actually found at all these localities or is it mostly planerite? Maybe turquoise should be deleted and replace by turquoise group ( unless proven to be turquoise). Leaving things as they are only compounds the error.
4th Mar 2015 20:32 UTCAlfredo Petrov Manager
5th Mar 2015 03:49 UTCRock Currier Expert
5th Mar 2015 05:45 UTCDon Saathoff Expert
5th Mar 2015 14:42 UTCWayne Corwin
5th Mar 2015 16:07 UTCElise Skalwold
Alfredo Petrov Wrote:
> The first step in reaching an understanding or
> consensus is to admit differences in usage do
> exist, and that that is not necessarily a bad
> thing or an "error".
Just to expand on that – in pursuit of mineralogy, along the way I've been surprised how much variation there is in the geological sciences regarding definitions and different understandings of some concepts depending on one's specialty. As for “gem people” – that’s really, really broad. Our friend Dick Hughes whom I've brought over to your Tucson booth (to his delight) published a great article co-authored with his mentor Dr. John L. Emmett entitled “Betwixt Two Worlds : A search for gemology in the 21st Century” archived here: http://www.ruby-sapphire.com/21st-century-gemology.htm Though I've never hesitated to argue with either of them over dinner, it may shed light for some on at least part of the “gem people” concept. My own direction goes down a path which is more narrowly defined; see a review of the first-ever Gemological Session of the GSA (2013) “Gemology bears triumphant tidings. A review of the historic 125th Anniversary Annual Meeting of the Geological Society of America” archived here: http://www.nordskip.com/GSA_Gemology_Session.pdf
Cheers!
Elise
5th Mar 2015 18:12 UTCOwen Melfyn Lewis
Many thanks for the link to the Minsocam paper, which was helpful to read and of which I have added a copy to my personal collection. For any interested, the chemical analysis by wt% of a sample from Greece makes an interesting read when put alongside the similar data from fifteen analyses of turquoise from three different localities in China shown here http://www.gemsdat.be/turquoise.htm (scroll right to the bottom of the page).
I was interested too in the determination of SG by the 'mixed liquid flotation' method. Having spent many days (running to weeks), years ago, trying to squeeze the last ounce out of that method, I finally gave it up for all but very specific needs. Learned a lot in the process though :-) I found the intractable problems to be:
- Difficulty in determining accurately the density of the final liquid mix at some fixed temperature.
- The need for strict temperature control of the liquid.
- The need for tables of temperature correction for each mix of liquids.
- The amount of time in preparation required to obtain as a one-off the SG of some unknown crystal.
That said, the value the authors derived is nicely within the uncomfortably loose range of SG values for turquoise that gemmologists have to content themselves with (see the above linked page for this also).
@ Alfredo, Reiner,
Re. moving the 'unwashed' photos to a Turquoise Group gallery: sounds like a plan to me that might help clear thought though, I suspect, that even this could not remove all dubiety from the winnowed turquoise species gallery. A most thought-provoking paper in my little collection is a doctoral thesis on how emerald may be identified and whether a given sample can be be tied to its locality of origin with reasonable certainty. For the purposes of this discussion, there were two of the conclusions that bear pondering on:
- Detection by wt% of a given element (Cr in the case of the paper) can vary by a greater margin between different specimens even from the same mine then may be the margin of variation between specimens from widely separated localities.
- That (given the laboratory resources of the materials science faculty of a major university) it is possible to identify the source locality of a mineral where there are extensive records for the same mineral from that locality. However, it requires an matrix of analytical methods, no single analysis being sufficient for this purpose,
I'll try and dig out and post a link to Dr Huong's paper as other may find it as thought-provoking as do I.
5th Mar 2015 23:21 UTCThomas Lühr Expert
I can't understand your commotion and agree with Alfredo: it's a question of terminology.
Please correct me if i did not understand the point and let me give an other example, without gemmological reference:
The mineral 'wolframite' is known and called so since generations of miners. However it is not a mineral (in mineralogical sense) but a name for each member of the ferberite-hübnerite-series.
The mineralogist calls it (per definition) as ferberite if it contains more Fe than Mn, in opposite case hübnerite. If he means one of the the end members, he should add a word like "pure". Only a not analyzed specimen is called wolframite by the mineralogist.
However, for the miner is the exact composition not of interest (but the physical properties and the content of W) and the historical name wolframite is for him a "good" name, doesn't care about ferberite or hübnerite.
Now you can replace:
miner by gemmologist
wolframite by turquoise
hübnerite by planerite
ferberite by turquoise too !!
The last line may be cause the confusion: In this case one of the end members has the same name like the historical name of the mixtures.
In consequence the gemmologist calls all mixtures (depending of physical properties) as turquoise (analogue wolframite), the mineralogist (depending of composition) only 50% (analogue ferberite). The rest has to be called planerite.
Thomas
6th Mar 2015 01:22 UTCReiner Mielke Expert
6th Mar 2015 01:39 UTCOwen Melfyn Lewis
6th Mar 2015 02:47 UTCJason Evans
6th Mar 2015 03:59 UTCAlfredo Petrov Manager
I will buy a whip as a gift for the organization entrusted with preventing confusion in mineral nomenclature, and ask them to please use it liberally on any subcommittee that yet again proposes a group name that duplicates a species name. :-D
6th Mar 2015 04:49 UTCD Mike Reinke
You got some, that quickly?!
There will be 3 small shows around me this month. I can only hope the dealers aren't reading this, or know where I live, or I'll never be able afford some now! lol
Great verse, Owen. May I supplement it with 2 Tim. 2:14, it isn't good to fight over words, it overturns people. even mineral people, and they are a devoted bunch!
You have to be devoted, to wade into these waters of mixed definitions. Ours is not a lightweight hobby, I found out very quickly...
Mike
6th Mar 2015 13:25 UTCOwen Melfyn Lewis
-------------------------------------------------------
> Great verse, Owen. May I supplement it with 2
> Tim. 2:14...
Aahh Mike, you certainly may...
Well, if nought else, this meandering thread has stimulated me to buy a facsimile copy of Joseph Pogue's work of 1915, 'The turquoise : a study of its history, mineralogy, geology, ethnology, archaeology, mythology, folkore, and technology' which, I understand, is still regarded as the bench-mark comprehensive study of the subject in the English language.
I agree with Alfredo (and Steve G, I think) that there can be no good end served by using the same word to name both a mineral species and the mineral group of which that species is a member. That said, it is not immediately clear to me which - the group or the species - should in every case keep the historic name. For example, in the case of 'turquoise', it seems to me that all interests would be best served by renaming the species and leaving the historic name to describe the group. But, taking the Beryl group/species, my feeling is that the reverse would be true and that the common good would be better served by reserving the historic name for the species and renaming the mineral group. What do others think?
6th Mar 2015 13:53 UTCAlfredo Petrov Manager
In this case I agree with Owen entirely. Unfortunately these decisions on reorganization of Groups are made by small subcommittees composed of a handful of mineralogists specializing in that group, with no mechanism that I'm aware of for any comments by the public (ie. anyone outside mineralogical academia, including gemmologists, curators...) until after the decisions are published, which is of course too late for anyone to say "Perhaps this group ought to have a different name?".
6th Mar 2015 14:21 UTCElise Skalwold
6th Mar 2015 16:28 UTCOwen Melfyn Lewis
This thread originated as a gentle discussion of turquoise jewellery, treatments and imitants, so your Gilson enquiry is really not out of place. O'Donoghue (after Webster) reports that the Gilson method might be a tweak on the Hofman method published in 1927 However his description of the Hofman method is too vague to serve as more than a pointer. MO'D points to 'Synthetic analogs and imitations of natural precious stones', a monograph available in Russian only, as a source of information on the Gilson method. Gilson worked with Russian colleagues on the method.
My understanding is that the Gilson business and its excellent products closed over 20 years ago and that he sold much/most of his know-how to Kyocera, Japan. That business, mainly through its ceramics division, continues experimental work on a range of synthetic gems and holds several Japanese patents. According to the CIBJO white book (2013) as at that date there was no synthetic turquoise in the market. I'm inclined to take that with a pinch of salt, it seeming more likely that it is there but rare as hen's teeth in comparison to the truckloads of imitant material and treated mined turquoise. It seems possible that a small amount of synthetic turquoise may be in circulation and passes cursory examination, when cut and polished, as being geologically formed.
8th Mar 2015 03:11 UTCRock Currier Expert
8th Mar 2015 03:25 UTCTony Albini
Tony Albini
8th Mar 2015 10:56 UTCDavid Von Bargen Manager
8th Mar 2015 15:46 UTCOwen Melfyn Lewis
-------------------------------------------------------
> http://www.minersoc.org/pages/Archive-MM/Volume_62
> /62-1-93.pdf
Another for the archive. Many thanks, David.
8th Mar 2015 16:39 UTCChris Krietsch
Some Lynch Station Virginia material that I have had for over 35 years. Sorry for the photography, free hand with a cannon camera. These are in my collection unmarked, I guess I should put a label on them so when I am gone someone will know what it is.
10th May 2015 19:07 UTCJosé Zendrera 🌟 Manager
Piece at right was bought personally in 1972 in Mashhad, Iran, which is close to Nishâpûr deposit so I would say that it has many probabilities to be real turquoise. Accurately measured density is 2.49 (little low for turquoise, probably due to embedded matrix), hardness is about 5 and streak is light-bluish white. Size is 5 x 4 x 1 cm
Specimen at left was bought in Kathmandu, Nepal, in 2012, allegedly coming from Iran across China following the Silk Road. Density is 2.66 and hardness also about 5, both can be hardly scratched with a knife. Don't looks dyed, I sanded 2 mm deep for checking and found no changes. Powder (= streak) is also light-bluish white. Size: 6 x 4 x 3 cm
Until here, no much difference between them aside from color hue and inter-nodular matrix. But fluorescence is very different. I know that many "turquoise" are in fact other species (howilite, planerite, other turquoise group minerals or even magnesite, aragonite and others) but I don't know the UV response of these minerals (except aragonite, which use to be fluorescent but not in these colors).
Maybe someone can give a clue...
1 - Halogen light
2 - Long wave UV (385 nm, filtered)
3 - Short wave UV (250 nm, filtered) (overexposed pic)
11th May 2015 03:02 UTCAlfredo Petrov Manager
11th May 2015 20:57 UTCJosé Zendrera 🌟 Manager
I did another fluorescence comparative, this time with all available turquoise at home, including cabochons and even pendants and a ring. Except the big nodule at left, all pieces were bought long ago in Mashhad, not far from the most classic turquoise deposit ( http://www.mindat.org/loc-25357.html ).
Note that under long wave (at center) cabochons at left fluoresce in same color than the big nodule. Also they have similar black embedded material. Green stuff, so-called "green turquoise" in origin, should be a mix of different minerals absolutely inert under UV.
Under short wave (below) the fluorescence of big nodule is still suspiciously strong and uniform. Draws attention the green small fluorescences in small pieces at right, which correspond to clear stuff that scratches glass, then should be quartz. No idea of what could be the yellow shine on the ring.
26th Jun 2016 11:11 UTCAbdullah Paracha
hello
I just bought this ring and was confused whether this is original turquoise or not so, i put a lighter against the stone which turned the stone blackish it did not melt and did not smell although there was a cracking type of sound and very small bubbles appeared on the stone which I cleared by the tissue the surface of the stone is kind of rough can anyone please tell me what type of turquoise is this and whether this is original or not please do reply
26th Jun 2016 12:37 UTCBob Harman
26th Jun 2016 16:43 UTCJosé Zendrera 🌟 Manager
It looks like the teardrop piece above at right in my last photo. Maybe a sub-product of the turquoise mines, not exactly turquoise but a mix of secondary copper and mafic minerals.
I personally bought this pendant time ago in a workshop in Mashad (Iran), near the turquoise mines so that I have no doubts about his authenticy.
The small bubbles that appeared when it was burned could be a varnish used to give polished appearance but I can not confirm this because I did not subjected my piece to so destructive burning test, you were very bold.
Cheers.
27th Jun 2016 04:00 UTCDoug Daniels
27th Jun 2016 04:52 UTCWayne Corwin
12th Aug 2016 15:15 UTCMirva L
- Mirva
13th Aug 2016 03:11 UTCDoug Daniels
13th Aug 2016 09:28 UTCMirva L
- Mirva
15th Sep 2016 22:00 UTCOowho
16th Sep 2016 00:06 UTCOwen Melfyn Lewis
- Spectroscope. Not all turquoise specimen will show a clear spectrum but those for those that do the absorption spectrum is diagnostic.Cut -off in the yellow as about 570nm and all longer wavelengths absorbed is diagnostic if present. Also look for an absorption line in the violet at about 430nm and maybe also at 420 nm - or else there may be a cut-off absorption of all wavelengths above anout 425nm. . A very powerful incandescent light source is needed.
- Refractive index (using spot method). 1.61
- Mohs hardness. 5-6.
- SG. 2.76 +0.34/-0.14.
If you can find a rock and gem club anywhere near you they should be happy to help you by trying these doing these tests for you.
Best guess off the photos? For me, it'd be reconstructed turquoise waste. That would figure at the price too.But certain proof of that would require destructive testing :-/
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 25, 2024 15:43:32
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 25, 2024 15:43:32