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
โณDiscussions
๐ฌ Home๐ Search๐ 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 HelpHambergite or Some thing Else ?
24th Jan 2012 19:43 UTCSajjad Shakir
{ Attachment 36331 Unavailable! phorum_files/3/363/36331/ }
24th Jan 2012 20:16 UTCRonald John Gyllenhammer Expert
I think you have it right, it looks like Hambergite.
Ron
25th Jan 2012 00:00 UTCJosé Zendrera ๐ Manager
For color and lustre could be also pollucite but shape looks more rhombic than cubic. Finally, as Ron and you, I also bet for hambergite.
Wassalam,
Jose
25th Jan 2012 00:17 UTCCraig Mercer
25th Jan 2012 03:26 UTCSteve Hardinger ๐ Expert
25th Jan 2012 12:44 UTCSajjad Shakir
26th Jan 2012 00:34 UTCJosé Zendrera ๐ Manager
26th Jan 2012 04:13 UTCJim Bean ๐
A picture from each side as Jose suggests, would be helpful.
26th Jan 2012 15:54 UTCSajjad Shakir
26th Jan 2012 15:57 UTCPeter Andresen Expert
After all it's second time you ask about this sample:
http://www.mindat.org/forum.php?read,11,225826,225829#msg-225829
And it created some fuzz when you tried to sell the same sample on mindat auctions based on the opinions from this forum... is this a second try to do the same?
26th Jan 2012 16:20 UTCSajjad Shakir
26th Jan 2012 17:03 UTCPeter Andresen Expert
26th Jan 2012 17:16 UTCJosé Zendrera ๐ Manager
http://attminerals.com/mineral_identification.htm
Peter, is very likely but is not same sample. Anyway, I think is not forbidden to ask two times the same thing. Please relax, nobody has committed a crime!
26th Jan 2012 17:44 UTCSajjad Shakir
26th Jan 2012 18:14 UTCJohannes Swarts
Couldn't some simpler tests be run?
What about looking at hardness, density?
What about chemical tests for Be and B?
Seems a bit simpler than sending something out for XRD. My college profs used to call this the black box approach.
Just a thought,
Best Regards,
Hans
26th Jan 2012 19:37 UTCRonald John Gyllenhammer Expert
There are tests that can be performed in lieu of more accurate up to date and available methods. I will give you one. If it means alot to you, you can attempt it if you wish. It will not be completely definitive but will bring you closer to an id.
The specific gravity range of values (as measured) for Hambergite are 2.347-2.372, since your specimen is one large crystal, this value should be measurable for your sample. You probably neither have a jolly balance nor one large enough for your specimen so you need to improvise. Methods for determining specific gravity have been presented here many times by long time helpful Mindat members such as Donald Peck. I propose a method below from another source. If you find it easy, try it. If not, perhaps someone else can help with an easier method. In addition, you need invest some time of your own to perform other basic tests, just to get closer to an id. You should test and determine hardness, streak, feel (is it greasy, etc.). Here are basic instructions for determining specific gravity, good luck with it.
How to test using specific gravity
"Testing a mineral for a specific gravity value is a complicated procedure. For the layman, it is done by water displacement and requires a beaker and a scale. The weight of the beaker is taken and written down, as well as the weight of the specimen. The beaker is partially filled up with water, and the level of the water is noted. The mineral is put into the beaker with water, and the water level rises. The difference in the amount of water before the specimen was put in and after it was put in is noted. The mineral is taken out, and the water is spilled out. Then the beaker is filled with the amount of water that the specimen displaced and measured. The difference in weight of the beaker when it was empty and the current measurement (the beaker with the displaced water) is the weight of the displaced water. The weight of the displaced water has the same volume as the specimen, but a different mass. The weight of the specimen is divided by the weight of the displaced water, and that number attained is the specific gravity of that specimen. This test cannot be conducted for an embedded mineral, but only for a single crystal or mass, for obvious reasons."
Source: http://www.minerals.net/resource/property/SpecificGravity.aspx
Sajjad, this method is neither precise nor accurate and can be inaccurate but it should give you a fair estimate.
All the best,
Ron
26th Jan 2012 19:55 UTCSajjad Shakir
26th Jan 2012 20:04 UTCRonald John Gyllenhammer Expert
As I have never used this specific gravity testing method, I cannot attest to it's accuracy. So please report back to us if you can with the results of your testing and your thoughts on it. Thanks.
Ron
26th Jan 2012 21:44 UTCJosé Zendrera ๐ Manager
26th Jan 2012 22:22 UTCCraig Mercer
Thanks Ron.
27th Jan 2012 02:03 UTCReiner Mielke Expert
27th Jan 2012 05:59 UTCSajjad Shakir
27th Jan 2012 10:40 UTCSajjad Shakir
27th Jan 2012 12:12 UTCJosé Zendrera ๐ Manager
27th Jan 2012 13:13 UTCFranz Bernhard Expert
Franz Bernhard
27th Jan 2012 16:17 UTCKelly Nash ๐ Expert
27th Jan 2012 21:32 UTCJosé Zendrera ๐ Manager
1- Place the beaker half-full of water on the scale and press the button "tare" to put the score to zero.
2- Introduce the specimen hanging from a string without touching the bottom or sides. The display will indicate the weight of water volume displaced by the specimen. As density of water is 1, the display will indicate the specimen volume in cubic centimetres.
3- You divide the specimen weight in grams for its volume in cubic centimetres and you will have the density.
The result, as you can see, is very accurate, 2,87 to 2,9.
Fast, easy, accurate, cheap and home made. Very thanks Reiner!
27th Jan 2012 22:20 UTCPeter Andresen Expert
I'm happy you didn't feel offended with my post. I have collected several hambergites during the last years, and have no idea how to explain why they are hambergites, so this string do realy tickle my interest too! I would love to have a good wet-chemistry, or some other way to identify the hambergite in an easy way, and I'm sure it's out there... I got plenty of small shards to do tests on if anyone have suggestions!
The way I can identyfy the hambergites I find is only based on paragenesis, and "intuition" about luster and morphology how it occure in the nepheline syenite pegmatites I collect in, which are totaly different from granite pegmatites. And with the new nomenclature for tourmalines based on OH/F, it should be interesting to check all hambergites if there could be a "hambergite-(F)" out there!
I'm looking forward to se more ways how to identify hambergite, and hope those huge crystals you have prove to be hambergites, Sajjad!
Regards
Peter
28th Jan 2012 00:13 UTCCraig Mercer
Any thoughts ?
28th Jan 2012 02:12 UTCRonald John Gyllenhammer Expert
>" I'm looking forward to se more ways how to identify hambergite..."
Have you ever tried any of the old flame or blowpipe type tests for id? I have experimented with them and have had some success. I have an old book; "Identification and Qualitative Chemical Analysis of Minerals" (Orsino Smith, 1953) that details the procedure for id of borates using HSO4 to decompose the borate sample and alcohol for flame test, amongst many other tests. I'll post the details verbatim for determination of a borate if you feel that you would actually try it. Just let me know. Also, this book can be had from Amazon for 10 or 12 bucks.
Ron
EDIT: Here's another proposed method from; "SIMPLE FIELD TEST FOR DISTINGUISHING MINERALS BY ABRASION pH*, Rollin E. Stevens and Maxwell K Carron. Hambergite listed on page 42. I have never tried this but it sounds interesting. http://www.minsocam.org/ammin/AM33/AM33_31.pdf
29th Jan 2012 05:34 UTCSajjad Shakir
29th Jan 2012 08:54 UTCSajjad Shakir
Best Regards
29th Jan 2012 15:08 UTCJosé Zendrera ๐ Manager
If you did like first case, your result (2,32) is very closely to hambergite density (2,36).
29th Jan 2012 15:25 UTCSajjad Shakir
i did following steps..
1.. first got weight of crystal which was 130 grams..
2. . Then i placed Container filled with water on scale and make zero.. like you do in picture ...
3.. i wrap a wire over the crystal and hanged it in water ... it gave me one time 56 and second time 55 grams....
then i devide 130 grams of crystal weight on 56 and then on 55... one time it gives 2.32 and one time it gives me 2.36 ...
best Regards
29th Jan 2012 17:26 UTCJosé Zendrera ๐ Manager
Relating your draw, it looks rhombic system. To be sure, you can check if corner angles in first draw are exactly 90ยบ. If they are, for sure is orthorhombic (as hambergite).
What about hardness? Did you try to scratch a quartz? Hambergite is 7,5, only little bit more hard than Q, is not easy to see the small scratch it can do on Q, but you can try to see with lens.
29th Jan 2012 17:41 UTCSajjad Shakir
29th Jan 2012 18:35 UTCJosé Zendrera ๐ Manager
29th Jan 2012 19:18 UTCSajjad Shakir
1st Feb 2012 13:25 UTCSajjad Shakir
thay are some test they do on a certificate and its shows that its 100 percent hambergite...
1st Feb 2012 14:40 UTCRonald John Gyllenhammer Expert
1st Feb 2012 17:18 UTCSajjad Shakir
You know that i sold these specimen by the name of orthoclase about 25 specimen but now i realized that its very expensive.. thanks ronald once again
1st Feb 2012 17:41 UTCRonald John Gyllenhammer Expert
1st Feb 2012 19:34 UTCPeter Andresen Expert
2nd Feb 2012 06:28 UTCSajjad Shakir
2nd Feb 2012 07:10 UTCCraig Mercer
Goodluck with the sales my friend,
Craig.
2nd Feb 2012 19:25 UTCSajjad Shakir
16th Feb 2012 07:27 UTCRock Currier Expert
If you have the money you might consider buying a contact refractometer and a light source, preferably one that is rich in "sodium". You may be able to find one on the internet for $500 or less. A used instrument will be OK. The heart of this relatively simple instrument is a lead rich glass hemicylinder that in time "oxidizes" and the readings you get from them become hard to read. You can correct this by polishing the surface of the hemicylinder with a little tin oxide on a moist cloth and by rubbing it vigorously with your finger. With this instrument you will be able to check the refractive index of gems and specimens, provided you have a flat polished surface ground somewhere on the specimen or a piece of a specimen. There are a lot of gem cutters in Pakistan and having a small flat polished surface should be easy and cheap. This can yield fairly definitive results and is a powerful but relatively simple identification tool. It will enable you to identify many gemstones and minerals with a fair degree of accuracy. The GIA (Gemological Institute of America sells these and trains all their students on their use. There are other instruments out there besides theirs. The contact refractometer, like all analytical instruments has its limitations and it is not good for minerals/gems with a high refractive indixes but it would certainly identify hamburgite. It is not as powerful an analytical tool as a petrographic microscope but is much easier to learn to use. This is one of the chief tools used in all gemological laboratories. You would have to learn a little bit about mineral optics, but once you do, it would certainly give you a step up on the competition.
21st Feb 2012 09:56 UTCSajjad Shakir
13th Mar 2012 09:59 UTCGWK
I wanted to pass on a refinement of this specific gravity measurement procedure which is more accurate by perhaps a factor of 5 as long as the weight measurement scale is accurate and linear over a large range of weights. The method is based on simple physics principles of buoyancy. The idea is similar; find the weight of a pure specimen or crystal, determine its volume by the buoyancy principle and divide weight by volume to get a very accurate measure of specific gravity or density.
The volume of the specimen is obtained by water displacement, but by weight and not reading the volume from a graduated cylinder. The method starts by tying a fine thread around the specimen , enough to support its weight in air. Fill a beaker 2/3 full of room temperature tap water. Weigh the beaker plus water to the nearest 0.1 grams. Immerse the specimen in the water by suspending it on a fine thread. Make absolutely sure that the specimen is not touching the sides or bottom of the beaker, yet is fully submerged. Weigh the beaker + water + suspended specimen. The weight difference between (beaker + water + specimen) - (beaker + water ) = weight of the volume of displaced water. Since water at room temperature has a density of 1.0 gm/cc, the weight of the displaced water is also equal to the volume of the specimen. This is the fine point that makes this method more accurate. Divide the specimen weight by this better estimate of specimen volume to get a density accurate to better than two decimal places (X . XX) if the specimen volume is about 100ccs or larger.
The other advantage is that you don't need a high accuracy graduated cylinder to get volume, just a good scale.
I hope this sheds some light on this discussion. I would like to see that this hambergite is the real deal. if this still doesn't settle the issue, I have an SEM with XRD and EDS x-ray spectroscopy systems at my place of employment. If you can send me a sample, I can have one of the techs check it for beryllium and boron. We can also check for silicon, aluminum, potassium to rule out the other minerals suggested here. Thanks, GWK
13th Mar 2012 12:14 UTCVandall Thomas King Manager
Kaygeedee minerals in Canada will do an EDS for $10. Because of the composition of hambergite, the scan should show that it is composed of nothing - that is, the specimen contains undetectable elements.
13th Mar 2012 16:00 UTCAlfredo Petrov Manager
A common source of errors is impurities in crystals (including even clouds of microscopic bubbles - If your crystal isn't gemmy, it's probably not pure); and tiny air bubbles attached to the surface of the crystal being tested, so make sure the specimen is completely wetted, without bubbles. I use a tiny drop of strong detergent in the water to improve wettability, although professional mineralogists will probably cringe at the extra errors being introduced. Professionals use disgusting stinky organic solvents instead of water for extremely accurate density determinations, with the attendant mathematical calculations to take care of the difference in fluid density, but water is adequate for ordinary ID tests.
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 ยฉ 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 02:04:07
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are ยฉ 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 02:04:07