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Fakes & FraudsIrridescent pyrite suns
2nd May 2008 22:51 UTCgeminerals
I am a part-time mineral dealer/collector. At my recent show, I had some
irredescent pyrite sun's from Sparta, Illinois. They are brassy with lovely
blue/green/red hues. Another dealer had a flat of the more common less brassy and duller sun's that he was selling. He mentioned to me that mine had been treated with bleach to give them that appearance of irredescence. Is this true?
If so, I would like to be able to tell potential customers of this before they commit to buy.
Thanks,
Greg
3rd May 2008 04:32 UTCsteven garza
Not only is that true, besides making them prettier, it also makes them MUCH more susceptable to breakdown from moisture in the air. They have a considerable amount of marcasite intermixed (typical for shale pyrites) & the treatment seems to "turn on" the decomposition process. Except for those kept in "dry boxes", most that others have bought have deteriorated in 5 to 7 yrs, leaving a shelf/box full of crumbly gray-white powder & giving off LOTS of sulfuric acid fumes. I bought one from two wholesale brothers who told me, right up front, they were treated; within 1 yr, I started smelling the fumes being generated & after 4, I had nothing left. I bought the piece STRICTLY to have something to show people what happens to these specimens.
My suggestion: get rid of them & consider the loss the cost of education that's worth a LOT more!
Hope this helps.
Your friend, Steve
3rd May 2008 06:11 UTCgeminerals
Thanks so much for the information; too bad as they sure are pretty. I will have to cull the one in my collection; I don't like the sound of sulfuric acid fumes floating around my cabinet full of specimens. Thanks for the fast response.
Best regards,
Greg
5th May 2008 18:16 UTCgeminerals
Thanks,
Greg
15th Jun 2008 12:14 UTCKevin Farrell
Marcasite content? I've heard of "pyrite disease" relating to marcasite. How common is this?
I have both pyrite suns and marcasite specimens that I've had more than 20 years with no sign of deterioration...
16th Jun 2008 03:59 UTCJustin Zzyzx Expert
that one already looks like it will go. Depending on your location and storage measures, you'll start to notice that the least shiney areas will get darker and darker, eventually turning into a powder, which will then turn white as it ages. Yum.
16th Jun 2008 12:37 UTCsteven garza
Justin is right; it's JUST starting to go & you just have to wait a little longer & you'll REALLY notice the "sulfuric" smell. Once the process has started, it's pretty much a forgone conclusion that you are looking at the best it'll ever be, for the next few months.
As far as the other marcasites, it depends on what type rock it came from & location, as Justin also mentioned; to be honest, ALL marcasite specimens are a crap shot & need to be handled sparingly & watched carefully. You just never know WHICH will sit in your collection for 50 yrs & which will start to alter the day you get them!
I've found that most that come from a shale environment, as the Illinois suns do, will disintergrate anywhere from a few months to 10 yrs (though, THAT'S rare!); those that come from from a limestone that has SOME copper mineralization or metamorphic environment tend to be stable. Don't know the reason for the copper making them stable, but, as copper IS a botanical poison & sulphide-eating bacteria ARE plants, that might be a good reason, even if the Cu is in PPM.
Hope this helps.
Your friend, Steve
16th Jun 2008 13:36 UTCPaul L. Boyer
16th Jun 2008 13:37 UTCKevin Farrell
That one's from Zigler Mine, Sparta, Illinois.
Shameless Plug: I think I'll do some education at the first meeting of the newly formed Hunstville Texas Area Gem & Mineral Society - see http://www.mindat.org/msgboard-15.html
Thanks again, Kevin
16th Jun 2008 14:21 UTCDan Weinrich Expert
Regarding the Sweetwater chalcopyrites. Some are treated with an acid solution to bring out the color. Others though are completely natural. I have seen them freshly collected, in miners lunchboxes, that are beautifully iridescent.
Dan Weinrich
16th Jun 2008 21:20 UTCsteven garza
Read the following: "Once considered a part of the plant kingdom, bacteria were eventually placed in a separate... more"; I'm sorry that I didn't keep up on the reclassification, I grew up when they had JUST decided that was where they belonged. One of the points for putting them there, as I remember, was their sensitivity to CU, the same as algae, fungi, & most other plant species; one of the reasons they DIDN'T want them in plants is they also had some animal characteristics, such as mobility. I guess they finally decide a proper place for them.
Your friend, Steve
2nd Jul 2008 01:55 UTCMark Heintzelman 🌟 Expert
In the breakdown, Pyrite accounted for 23% of mineralization in these deposits, Kaolin, Quartz and "Carbonates" accounts for the other 76%. Observations of Marcasite made up only a portion of the last 1% of mineralization, along with Sphalerite, Galena, et al.
Steven has pointed to an observation I've made myself, in this case concerning those large cubic Pyrites which occur throughout Pennsylvania. Anecdotal as it may be, the ones which occurred within the coal field regions proved to be unstable. All but one I've owned eventually exhibited some degree of decay, however not a single one from outside the coal regions ever have.
I only have four of these Illinois "suns" in my personal collection, two golden in color (one is "iridescent") and two silver colored. I too have had them for many, many years now, and thankfully none of them have so far shown any evidence of decay (lucky me I guess).
MRH
2nd Jul 2008 04:31 UTCAlfredo Petrov Manager
A dry atmosphere helps, but even that is only a delaying tactic; the air is never dry enough to stop the decomposition completely.
With regard to iridescence, note that ANY mineral becomes iridescent when coated with an extremely thin layer of another substance (like a tiny drop of oil spread out over a rain puddle). If Nature hasn't already created this layer for you, you can do it yourself by any number of different chemical reactions, but it is the thickness of the layer, not the type of reaction, that will determine whether you get iridescence or not.
2nd Jul 2008 04:41 UTCsteven garza
Your report said, "In the breakdown, Pyrite accounted for 23% of mineralization in these deposits, Kaolin, Quartz and "Carbonates" accounts for the other 76%. Observations of Marcasite made up only a portion of the last 1% of mineralization, along with Sphalerite, Galena, et al"; it DOESN'T say where they took those samples, which layers or at what point in those layers the samples were taken, or, how many samples were evaluated. Here's what I found: mild HCl DOES attack marcasite, like crazy, while pyrite seems to hold up quite well. I've used samples from one deposit to prove this point to beginners, bcs the marcasite & MOST of the pyrite grow separately into each other. A sample of marcasite will be GONE in about 1 day, while the pyrite (bcs it DOES have some marcasite in it, too) will have subtantially dulled faces, but, little else (if you want a piece of this to try, let me know). When I tried this on a pyrite dollar, I was left with a MASSIVE display of slightly pyritey "swiss cheese", which means there MUST be some marcasite in them. Something else to consider: what if the supposed (you won't convince ME there's only 1%; would someone sacrifice a piece & do a probing?) 1% breaking down CATALYZES the pyrite breakdown, in a slower reaction environment? Much like calcite/aragonite specimens tend to do, quicker than calcite or aragonite specimens, alone, do?
I, too, have "suns" that have lasted a LONG time (over 50 yrs), BUT, under the same conditions (they were kept together), I've had MANY that have "died" within 4 yrs. BTW, after my FIRST result of that experiment, I trashed ALL specimens that smelled the slightest breakdown. Wish I had done it on specimens from other locations.
Your friend, Steve
2nd Jul 2008 16:07 UTCMark Heintzelman 🌟 Expert
It always bugged me that I've heard so many contradictory "facts" about these Pyrite "dollars", so last year I decided to try and find some research papers which addressed them. This was the only descriptive report I could find with particulars on the subject, and not for lack of trying! :) It is perhaps more generalized than I would like, and it covers/describes a rather wide region, noting little variation. Perhaps this is a troubling oversimplification, but not having conducted the research in this report myself, I cannot say. The breakdown of mineralization noted is a region wide assessment, the low accounting of Marcasite does not indicate it was not concentrated (i.e. in these concretions), but only indicates it's presence in the region is uncommon. I would think however, that a scholarly approach to describing these concretions was made, which included a reasonably large subset of specimens taken from various sites and at various levels, etc. I personally prefer that these details be remarked upon in the report, describing the subset used for any study, but sadly this report does not. So it is only an assumption on my part that some diligence was taken in developing this description. Considering the source I would think it a reasonable assumption though.
As Alfredo confers, there are any number of occurrences where the local Pyrites are particularly unstable, without being caused by inter-development with Marcasite. I don't want to argue with your own observation, just noting what has been reported to have been observed concerning the regions mineralization and these concretions in particular.
Luckily, I learned early on to separate pieces showing signs of Pyrite disease from the rest of my collection, and I still have a separate "ward" for those pieces, some still worth retaining even after 20 odd years. It is always sad though to have to commit a decent specimen to the trash, but I've had to do it (kicking and scratching all the way to the bin)!
MRH
8th Jul 2008 03:04 UTCWes Gannaway
23rd Jul 2008 01:26 UTCTed Kepling
23rd Aug 2008 15:31 UTCAlysson Rowan Expert
You may be able to stabilise the specimen as follows:
Wash thoroughly in a solution of baking soda (to neutralise any acid), possibly soaking for a few days. Then a long soak in clean water, and a soak in distilled water.
Dry thoroughly in a warm place and then either soak in oil (not recommended) or varnish with something like crystal mount (a clear, toluene-soluble varnish).
Of course, there are no guarantees, and in one of my specimens, the decay was kicked off by the soak.
I have lost a couple of rarities from a very unusual site to this. In the case of a rather fine micro fan cluster, the whole process of decomposition took about 5 days - before I could even take decent photographs.
12th Sep 2008 23:53 UTCPaolo Malesci
We have observed differences in the behaviour of pyrites of Rio Marina Mine, Elba Island, Italy, related to the matrix: on lamellar hematite matrix are more stable that on granular pyrite matrx.
Despite of care they are not eternal: at the University of Florence Mineralogical Museum all the specimen of the ancient collection (late 18th century) had been lost and so also the greatest share of the hystorical (Foresi & Roster) Elban collection.
26th Nov 2008 22:03 UTCJason Evans
27th Nov 2008 11:41 UTCKevin Farrell
2nd Dec 2008 19:18 UTCPeter Hargis
"Dont worry about my clients or inventory it WILL NEVER CRUMBLE now I must get back to my three e-bay stores and 20-50 packages daily made.Good luck with buying on E-bay bye bye now"
It seems a little condescending to me (maybe it's just me), and I was wondering if I could post the name of his eBay store to let people know he is selling treated minerals without acknowleding it to his customers. Or is this something that is not allowed/recommended. Thank you.
2nd Dec 2008 20:08 UTCAlfredo Petrov Manager
The iridescence on some minerals is caused by an extremely thin coating of another substance on the surface, like the rainbow effects created by a drop of oil on a puddle of rainwater. Nature can do this at certain early stages of weathering, an effect that is lost at later stages when the alteration film gets too thick.
If I saw a whole flat of pieces that were all equally iridescent, I'd be highly suspicious that they were treated; the naturally iridescent pieces tend to be quite non-uniform in degree of iridescence.
2nd Dec 2008 20:13 UTCPeter Hargis
5th Dec 2008 16:52 UTCAlbert Mura
5th Dec 2008 17:01 UTCAlbert Mura
5th Dec 2008 18:26 UTCMaggie Wilson Expert
First, the flippant and dismissive tone diminishes your concerns. Yelling at you via USING CAPS is also bad form. Finally, the seller goes on to elevate his position by claiming to have so much Ebay business, that he must of course be legit.
Sure, the product may be bona fide. But it is my not so humble opinion that the seller could use some lessons in PR. Remarks like those do not help his case.
Maggie
27th Nov 2011 08:58 UTCjake
27th Nov 2011 11:55 UTCRock Currier Expert
What mines are currently producing the suns? What is the largest pyrite "sun" you have seen.
Rock
27th Nov 2011 15:15 UTCAlbert Mura
27th Nov 2011 22:17 UTCJake
27th Nov 2011 23:14 UTCAlbert Mura
8th Dec 2014 18:40 UTCpnjfm
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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 15:53:59