Painite was once considered one of the rarest minerals on earth. The first painite to be recognized as new mineral (painite #1) was a sample discovered in Burma in the early 1950's. For many years only two crystals of this hexagonal mineral were known to exist. Its chemical formula is ideally: CaZrBAl9O18. However, it also contains minor amounts of chromium and vanadium that contribute to the orange-red to brownish-red color of the mineral plus traces of iron. In addition to zirconium, minor amounts of titanium and hafnium also are part of its composition. While it often appeared in lists of gemstones, only two faceted gemstones had been reported prior to mid-2005. The discovery of a new locality in northern Myanmar in 2002, and the discovery of major new localities in the Mogok area led to the recovery of several thousand crystals and fragments. Nearly complete crystals remain few in number and high quality facet material remains rare, although several hundred crystals and pieces have been faceted to date.
More About the History of Painite
is a 1.7 gram
crystal that resides in the British Museum of Natural History,
London (BM 1954,192). It was obtained in 1952 through a donation by
Pain, and originally
described in an article by Claringbull et al in
1957. The slice of this crystal (painite #1b) that was used
the X-ray structure determination (Moore & Araki, 1976) and
the optical (Shigley et al., 1986) and Raman spectra is now at
the California Institute of Technology.
|The dichroism of a 0.606 mm thick slice of painite #1b embedded in beads of a colorless plastic shows that the crystal is orange-red for light polarized parallel to the c-axis and pale purple when polarized perpendicular to the c-axis.||
Painite BM 1914,1118. An earlier painite sample was in the British Museum of Natural History, but was originally misidentified as a brown tourmaine with rubies from Mogok, Burma. In late 2007, this sample was proven to be painite by an electron microprobe analysis. In the photo, painites #1 and #2 are also shown. (Photo provided by Alan Hart, British Museum of Natural History)
Painite #2 is a dark, 2.118 gram crystal on public display in the British Museum of Natural History, London. There are no reported detailed studies of this crystal.
Painite #3 is a 0.27 gram crystal now in the collection of the Gemological Institute of America. It was discovered in 1979 at the Gemological Institute of America (GIA) in a parcel of gemstone rough and has been extensively studied at the GIA, at the Los Angeles County Museum of Natural History, and at Caltech (Shigley et al., 1986). It is a dichroic, deeply colored, brownish-orange red crystal with a density of 4.03.
|Chemical Analysis Painite #3 (Shigley et al, 1984)
Painite #4 [updated May 2006] was originally ~11 grams (55 cts) when discovered in late summer, 2001, in Burma. The identity of painite #4 was first suspected by Burmese investigators based on its density, refractive indices and hardness. A 0.188 gram slice (painite 4b) was removed from it and was sent to Caltech for confirmation of the original tentative identification where its identity was confirmed in September, 2001. The XRF analysis showed major Al, Ca, and Zr, and minor Ti, Fe, Hf, and Cr. The Raman spectrum matched the standard painite spectrum that we acquired from the sample of painite #1b that was originally used to determine the crystal structure (Moore & Araki, 1976). Even though the orientation of crystal #4b is different, its infrared reflectance spectrum is similar to that of painite #1b [in the (0001) orientation]. Slice 4b is now privately owned in the USA. A small aliquot of 4b also resides at Caltech. A second slab that was also removed (painite 4c) is in the US National Museum of Natural History, Smithsonian Institution. The main mass (painite 4a, now 54 cts) of the dark, nearly opaque crystal was originally privately owned in Burma.
|Chemical Analysis Painite
|Painite 4a was subsequently acquired by the GRS Gemresearch Swisslab AG, Switzerland. It has been the object of detailed study at the AIGS laboratory in Bangkok, the GRS Swiss lab, and university labs in Switzerland. A 0.030 gram fragment (painite 4d) was removed from the main crystal and appears at the website of the GRS Gem Research Swiss Lab. Detailed chemical analyses and a redetermination of the crystal structure are reported by Armbruster et al. (2004). Unaware that their crystal was identical with crystal #4, Armbruster et al. stated that the 54 ct crystal came from a new crystal which they labeled painite #6.|
Painite #5 is a 0.508 gram faceted gemstone that was first identified by GRS (Thailand) Co. Ltd. in Bangkok. It was studied by the GRS Gem Research Swiss Lab and pictured on their website. It currently resides with its owner in Burma. (updated 26-May-2006)
Painite #6 was in a bag of lower-quality, gem rough purchased by the author of this web site in Namya (Nanyarseik), northern Myanmar, in March, 2002. After it was brought back to the author's laboratory, it identified from its chemical composition and Raman spectrum. This locality is a ruby mine far removed from the original discovery locality at Ongaing and represents the second known locality where this phase occurs. The crystal has undergone detailed study at Caltech.
|It was originally identified from its X-ray fluorescence spectrum while embedded in plastic with corundums in a mount prepared for analysis in a scanning electron microscope (image to the right). It is currently embedded in a plastic mount that was used for electron microprobe analysis. This allows the internal detail to be seen. When the mount is tilted so the line of sight is down the long axis, the symmetrical pattern of the internal features can be seen.||
Painite #7 was also purchased by the author of this web site in Namya, northern Myanmar, in March, 2002, and positively identified based on its chemical composition and Raman spectrum. This 0.0467 gram, dichroic pale pink crystal is in the author's collection at Caltech and has been subjected to detailed study of its composition and optical spectrum. This crystal, and all other others discovered to date from the Namya localilty, are much paler than painite crystals found at Ongaing and other localities in the vicinity of Mogok.
Analysis Painite #7
Painite #8 is a brownish-orange uniaxial crystal that was found in May, 2004, near Ohngaing village, Mogok region, Myanmar. It was identified as painite in Mogok by a gemologist on the basis of standard gemological testing. The strongly dichroic crystal has a specific gravity of 4.00. The 0.522 gram stone currently resides in Burma. Many of the numerous small, secondary crystals have been removed from the edge of the master crystal and are the object of study in Burma and at Caltech. The Raman spectrum confirms that they are painite.The optical spectrum of 0.809 mm thick, 2.9 mm long crystal '8b' shows the same features as those of crystal #1. Like the main crystal, they are dichroic in transmitted light with the most intense red color when light is polarized parallel to the long c-axis of the crystal. The outline of the crystal shape of fragment 8b is apparent looking down the long axis of the crystal. The main mass of this crystal now resides with the GRS in Switzerland. (updated 26-May-2006)
Painite #9 was offered for sale in 2004 in Yangon, after which it went into private ownership in Japan. It reportedly weighs about 340 mg and is an orange-red color similar to painite #8. It is now in the collection of the GRS in Switzerland. (updated 26-May-2006).
Painite #10, a dark, brownish-orange uniaxial crystal was found in December, 2004, near Ohngaing village, Mogok region, Myanmar. It was identified as painite in Mogok on the basis of standard gemological testing. It is strongly dichroic from brown to red. The 0.93 gram stone was orginally studied by a Burmese gemologist and is now in the collection of the GRS in Switzerland. (updated 26-May-2006).
Painite #11 is a dark brown-orange crystal that was announced on 31-December, 2004. It was identified as painite in Mogok on the basis of standard gemological testing. It is nearly 2 cm long and about 1 cm wide. The 2.58 gram stone currently now resides in the collection of the GRS in Switzerland. This crystal is of particular interest because one side of the crystal has numerous small rubies attached. These rubies are abundant on the crystal. (updated 26-May-2006)
Painite #12 is an orange-brown, 0.156 gram, transparent, uniaxial, gemmy crystal with one perfect termination was obtained in Burma in 1992. It is currently under private ownership in Burma but its existance was only recently made public. As such, it may be the fourth painite crystal actually discovered.
Painite #13 is an orange-brown, 0.264 gram, transparent, dichroic, gemmy crystal identified January 4, 2005, by a gemologist in Mogok. It was found near Mogok, Burma, and is currently under private ownership. It was offered for sale (April, 2005) partly through advertisements on the web.
News about our discovery and identification of painites #6 and #7 was relayed to geologists in Myanmar in 2004. Efforts were soon underway to find more in the northern province. Those efforts were successful.
Painites #14 and #15 - Press Releases from Asia
The Associated Press/Rangoon reported on March 15, 2005 that two crystals were found near Phakant, Kachin State, Myanmar, by geology student Kyaw Khaing Win. Phakant is near Namya where painites #6 and #7 were obtained.
The Myanmar Times reports the discovery of the same two stones in the Namyar region but puts the data of discovery as November, 2004. A picture from the Yagon City website, repeating the Myanmar Times article, shows the painite #15 crystal.
Painite #14 is a pale pink, 0.0727 gram, transparent, dichroic gemmy crystal identified in late 2004. The outline of the crystal shape of crystal 14 is apparent looking down the long axis of the crystal. Its identity was positively confirmed at Caltech in early 2005 and it is currently under private ownership in the United States.
Painite #15 is a 0.0662 gram, medium red-brown, dichroic crystal, transparent crystal identified in late 2004 or early 2005. The outline of the crystal shape of crystal 15 is apparent looking down the long axis of the crystal. Its identity was positively confirmed at Caltech in early 2005 and it is currently under private ownership in the United States.
These crystals are believed to have been discovered in late 2004 to early 2005.
Painite #16 is a crystal that was found in the Mogok region. (November 2005 - recent information indicates that this is actually painite #9)
Painite #17 is a crystal that was found the Mogok region.
Painite #18 is a small gemstone faceted from a painite found in Northern Myanmar. This is the second reported faceted painite. (See painite #5, also a faceted stone).
Painite #19 is a small stone found in Northern Myanmar
Three more painites were discovered in early 2005 in Burma.
The properties of these there
stones are characteristic of the
crystals that come from the Namya locality.
Painite #20 is a 0.0280 gram (0.0140 ct) pale purplish pink, dichroic crystal fragment devoid of a termination. Looking down the c-axis, the hexagonal shape of the crystal can be seen. There are also inclusions in the crystal that contain brown and red phases within and around the longer, tubular inclusions. This crystal is under private ownership and has been studied at Caltech.
Painite #21 is a 0.0335 gram (0.1675 ct) grayish purplish pink, dichroic crystal fragment with comparatively fresh prism faces, but devoid of terminations. Looking down the c-axis, the hexagonal shape of the crystal can be seen. There are also inclusions in the crystal that contain brown and yellow phases within and around the longer, tubular inclusions. This crystal is currently under private ownership and has been studied at Caltech.
Painite #22 is a 0.0321 gram (0.1605 ct) pale purplish pink, dichroic, clear crystal fragment that is devoid of terminations. Looking down the c-axis, the hexagonal shape of the crystal can be seen. The surface of this crystal has a tree-bark texture that some of the other crystals from northern Burma have. This crystal is privately owned and has been studied at Caltech.
Much additional information about the first 22 painites was reported in May 2005 at the Goldschmidt 2005 Conference in a session (Page A278) on the gem minerals (Rossman et al., 2005). The authors concluded that the mineral forms in a skarn deposit. After submission of the abstract, but before it was presented at the meeting, the skarn deposit where painite formed was located in Myanmar as reported below.
The Painite Mine near Ongaing
December, 2004: The initial source of painite has been claimed by local residents to be alluvial pebbles obtained near Ohngaing Village in Myanmar. These painites showed only modest water rounding indicating that the primary source was nearby. The actual source of painite near Ongaing Village has finally been located. Ohngaing Village is slightly more than a mile NNW of Mogok. From Ohngaing Village one can see Mogok in the distant valley in this picture. Painite was reported to found at a small mine just at the edge of Ohngaing known as the Sinhalite Mine. The mine produces mostly spinels of assorted colors, tourmaline and sinhalite. The mine doesn't produce any gem-quality corundum. Painite is said to be found in the upper portion of the mine near the contact of leucogranite and marble in weathered soil.
Subsequent exploration of the
geological formation has greatly
expanded the region where painite is found as indicated in the
Painite #23 is a 4.8 mm long, 0.9 mm wide intergrowth of two crystals (estimated weight, 0.03 grams) in a matrix of rubies, rutile, and fine-grained clay minerals including anatase and iron oxide. It is weakly dichroic from reddish-brown to yellow-brown but the dichroism is hard to see because of darker inclusions in cracks in the specimen. It was reported in late May, 2005. It's identity was confirmed from its Raman spectrum. It is currently under private ownership and has been at Caltech for confirmation of the identification, but was not removed from the host matrix. Its color and properties indicate that it originated in the deposits in the Mogok district.
Painite #24 is also a crystal on matrix that was shown in Yangon in May, 2005. No further details are available at this time.
Painite 25 is an approximately 2 cm long crystal in a matrix of a skarn rock containing ruby and biotite. The crystal has a dark color typical of crystals discovered so far in the Mogok region. The locality is west of Mogok, near Kyaukpyatthat (Kyauk Pyar Thart). They are found at the Wetloo quarter near the base of Hinthar Hill where they form at the contact zone of leocogranite and marble. Once the actual source was known, an extensive effort was made to find more painites from the Mogok deposits. These efforts were comparatively successful resulting in a plentiful supply, at least compared to early 2005.
The Wetloo Mine on Hinthar Hill; painite occurs at the contact zone near the base of the hill.
Mid July, 2005.
Within one week of the
discovery of painite at Wetloo, Painite
was found east of Mogok
very close to Thurein-taung
(painite locality = number 1 in photo; village = number 2) at Ah
Sein Taw Quarter. Many fragments and crystals of painite
have been found there.
Nearly every home there had painite for sale. Most are mineral specimen
can be cut to a cabochon and only a few are suitable for
faceting. This locality is also known as Thu-Rein-Thaung
and as Sun Mountain. The painite occurs in a skarn deposit in contact
Late July, 2005
Numerous painites were available in the local gem and mineral markets.
a) 0.08 ct transparent crystal
b) 53 ct nearly opaque crystal
c) 0.226 ct terminated crystal
d) 0.2 to 0.5 ct crystals and fragments
Smaller, secondary deposits have also been located in the area that further increase the supply of painite.
Larger quantitites available in late August, 2005
Numerous fragments of painite crystals have been discovered as a result of extensive efforts to sluice the entire area where painite occurs. Most of these were sent to Thailand for processing and sale. Most of them were purchased by the company, Pala International. Most of them came from the Wetloo Mine and others came from the Thurein-taung locality.
a) 36.5 grams of crystal
b) 120 grams of fragments
A few incomplete, dark crystals exceeding several hundred carats have been found.
c) 107 gram crystal
d) A 96 gram specimen of a crystal with smaller crystals attached.
Fine specimens exist, but are rare.
e) An 8.2 ct crystal from the Wetloo Mine
f) three nice crystals all less than 1 cm long
Also, crystals both large and small, have been found with ruby attached
g) 40 gram crystal partially covered with small rubies
h) painite and ruby in matrix
While many pieces have been cut into dark red cabochons, facet quality material is said to remain almost unattainable.
i) 10 cts, Thurein Taung locality, small, crystals
j) 5 cts, nodules of facet quality
Matrix specimens with abundant painite fragments have also been obtained.
Further information (early October 2005)
A number of small faceted stones have been prepared from the recently discovered highest quality stones. A picture of the three largest new faceted stones, and more history about the recent stones is available on the website of Palagems. As of the second week of October, 2005, specimens of painite and faceted stones have been available for sale on the internet at several sites.
Museum Painites (late October 2005)
number of crystals and faceted
stones have been obtained by major museums and are expected to
soon be on public display. The Los Angeles County Museum of
Natural History has a 4.9 mm (0.47 ct) faceted stone.
Both the National Museum of Natural History - Smithsonian Institution, and the American Museum of Natural History have also obtained examples of painite.
More crystals (mid November 2005)
About 700 crystals and two faceted stones were brought to the Asian Institute of Geomological Sciences in Bangkok by a Burmese dealer. Details were posted on the AIGS website.
A New Locality for Painite - Bawlonegyi Painite Mines (early December 2005)
Painite is now found in the Bawlonegyi area due west of Mogok. The crystals are small in size and have a color similar to the painites from the Wetloo mine with six sided crystals. They have been found only in secondary deposits, to date. Here are pictures taken in mid December 2005 of Bawlonegyi Palaung Village and a miner panning for painite.
Thurein Taung Painite Mine (Mid December, 2005)
Wetloo Painite Mines (Mid December, 2005)
Here are pictures of painite from the Wetloo painite Mines, a different view of the workings, and the local area. Here is the mine in spring 2006.
New Localities for Painite (December, 2005)
Painite has been reported from both Kin and Kabaing, two villages west of the other Mogok region localities.
Tucson Mineral Show (Early February, 2006)
Painites were for sale at the Tucson Mineral show.
From the GemResearch Swiss Lab (May 2006)
The GemResearch Swiss Lab reports the discovery of the largest painite specimen to date weighing 633 grams (3,165 cts). Found in mine tailings, it is a large, lusterous painite crystal overgrown with numerous rubies.
Painite in Matrix (May 2006)
A 5 mm crystal in matrix. Another crystal in matrix with spinels. A 1 cm crystal in matrix with excellent crystal faces. A 4.5 cm crystal of painite mostly replaced by ruby; a closeup of a painite region. Additional pictures: a lusterous 26.3 gram painite with prominent red spinel. A 4.5 cm crystal and a 4.4 cm crystal pair. A painite crystal with hexagonal shape.Painite crystal from Namya (Sep 2006)
Painite was found mainly at two localities, Wet Loo
and Thurein Taung.
Lesser amounts were found in Baw Lone Gyi, in the northwest part of Hin Thar Taung.
Some miners who searched for painite in a contact zone of marble and leucogranite in Hin Thar Taung, located at the upper side of Wet Loo mine, found small samples of painite with ruby in marble matrix in past year.
Some people thought that may be primary but it is only in the trend of the contact zone.
Samples were of mineral specimen quality but not suitable for gems.
b) In Myanmar, few gem quality painites were available in the gem markets, but a few older stones from the mid 2000's were available. They brought high prices in the past five years.
c) New samples of Namya painites have not been available as the large mines are closed and only informal mining occurs.
d) Likewise, in Mogok, only informal mining was occuring and that was directed at high value stones such as ruby, sapphire and spinel.
Armbruster T, Döbelin N, Peretti A, Günther D, Reusser E, Grobéty B (2004) The crystal structure of painite CaZrB[Al9O18] revisited. American Mineralogist 89, 610-613.
Claringbull GF, Hey MH, Payne CJ (1957) Painite, a new mineral from Mogok, Burma. Mineralogical Magazine 31, 420-5.
Harlow GE, Bender W (2013) A study of ruby (corundum) compositions from the Mogok Belt, Myanmar: Searching for chemical fingerprints. American Mineralogist 98, 1120-1132.
Hart A, Rumsey M (2014) A wonderfully 'painful'
discovery. The Journal of Gemmology 34, 10-11.
Makovicky E, Olsen LA (2008) High-pressure Al-rich hexagonal phases—What are their kin? American Mineralogist 93, 1585-1587.
Moore PB, Araki T (1976) Painite, CaZrB[Al9O18]: Its crystal structure and relation to jeremejevite, B5[3Al6(OH)3O15], and fluoborite, B3[Mg9(F,OH)9O9]. American Mineralogist 61, 88-94.
Nissinboim A, Harlow GE (2011) A study of ruby on painite from the Mogok Stone Tract: Gems and Gemology, Research Track, Gem Localitiesand Formation, 47, 140–141.
PalaGems.com (2014) Painite Comes to Pala. https://www.palagems.com/painite.htm pdf file
Peretti A (2003) Rare gemstone: painite. Contributions to Gemology. Gem Research Swiss Lab. 2, 19-20.
Povarennykh AS, Clark AM, Jones GC (1978) The infrared spectrum of painite. Mineralogical Magazine 42, 518-19.
Rossman GR, Naung S, Harlow GE, Hunt J (2005) Painite (CaZrBAl9O18): A second source in Myanmar and metasomatic origins. Abstract. Goldschmidt Conference 2005, Moscow, ID. Geochimica et Cosmochimica Acta 69, A278.
Rossman GR (2006) New discoveries of painite in Myanmar (Burma). Gems & Gemology 41, 356.
Shigley JE, Kampf AR, Rossman GR (1986) New data on painite. Mineralogical Magazine 50, 267-70.Thu, K. (2007) The igneous rocks of the Mogok Stone Tract: Their distributions, petrography, petrochemistry, sequence, geochronology and economic geology, 139 p. Ph.D. thesis, Yangon University, Yangon, Myanmar. (p 125–126)
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