Magnetism in Gemstones
An Effective Tool for Gem Identification
© Kirk Feral
Purple: Purple and lavender color in Tourmaline is rare, and it is likely due to a combination of pink color from manganese (Mn3+) and blue color from iron (Fe2+). Pink plus blue = purple. Pale purple Tourmalines are sometimes referred to as "Siberite" (a term associated with Siberia where purple Tourmaline has been found). In copper-bearing Paraiba Tourmalines, purple and violet colors are due to pink from manganese (Mn3+) plus blue from copper (Cu2+). The purple "Siberite" gem below (left) shows a Moderate magnetic response. The "Siberite" on the right is strongly magnetic and shows a near-drag response. The stronger magnetism is due to a higher concentration of cryptic (colorless) manganese (Mn2+) in addition to the small amounts of Mn3+ and Fe2+ that create purple color in both gems.
Tourmalines: Pink, Red and Other Colors
Pink and Red: Pink Tourmalines and red Tourmalines ("Rubellite") are colored by manganese in the valence state of Mn3+, which generally produces lower magnetic susceptibility than what is found in gems colored by Mn2+. This is because only tiny amounts of Mn3+ are sufficient to produce bright pink and red colors. Consequently, pink and red Tourmalines are among the least magnetic Tourmalines, with responses ranging from Inert to Weak to Moderate.
Pink Tourmaline (1.99ct., Moderate, SI 78)
Pink Tourmaline (2.1ct.,Strong, SI 156)
"Rubellite" (6.45ct., Inert, SI <0)
Bi-Color: A single Tourmaline crystal can have 2 colors that exist separately rather than blended. Crystals can either grow with a central core of one color and outer rim of another color (as in the slice pictured below left), or with bands of different color along the crystal shaft (represented center and right). Any combination of colors is possible. The most frequently seen bi-color gem is “watermelon” Tourmaline, in which pink or red color meets green color. Bi-color Tourmalines can show different magnetic responses within the same gem, with pink/red sections tending to be the most weakly magnetic, or diamagnetic.
The bi-color gem shown on the right is gray on the left side and pinkish red on the right side. The gray portion (Fe3+) might be the result of natural irradiation of pale green color (Fe2+). Originally, this gem may have been pale green (Fe2+) on the left side, and pale yellow (Mn2+) on the right side. The gray side is strongly magnetic, and the pink side is inert (diamagnetic).
The orangey red Tourmaline pictured below has an unusual color. Do we call it "Rubellite"? Unlike "Rubellite" Tourmalines with purer red color, this orangey red gem is strongly magnetic. Perhaps the reason for the strong magnetism is similar to that proposed for the pink gem above: the rough crystal may have begun as a yellowish gem with high Mn2+ content, and the gem retains a significant concentration of magnetic Mn2+.
"Rubellite"? (8.15ct., Strong, SI 326)
The pink Tourmaline trillion shown below is one of the palest pink Tourmalines in this study, yet it shows the strongest magnetic response: it drags. How is this possible? In addition to pink, there is yellow color in this gem. Yellow color in Tourmalines is associated with manganese in the valence state of Mn2+, and as we shall see, it can also be colorless or cryptic. Perhaps this pink Tourmaline began with an unusually high concentration of Mn2+. After natural radiation exposure, it may have retained more Mn2+ (yellow) than most other pink Tourmalines. Perhaps the pink color is very pale because radiation exposure time was short and the alteration to Mn3+ (pink ) was minimal.
Pale Pink Tourmaline (2.40ct., Drag, SI 391)
For reasons unknown, pink Tourmaline appears then to be associated with a higher total concentration of manganese than less magnetic red Tourmaline. Research is needed to determine why this might be the case, but it is likely related to the proportion of cryptic manganese (Mn2+) to pink/red manganese (Mn3+).
A study titled "The Role of Natural Radiation in Tourmaline Coloration" (Reinitz & Rossman,1988) suggests that when pink and red Tourmaline crystals first form geologically, they probably contain low concentrations of Mn2+ with little or no Mn3+, and are probably colorless or pale in color. Natural gamma radiation from radioactive decay changes the Mn2+ to Mn3+ over geologic time and changes the body color from colorless or pale color to pink color, and eventually to red color due to Mn3+. But Mn3+ oxide in Tourmaline actually has a slightly higher magnetic susceptibility than Mn2+ oxide.
"Rubellite" (3.18ct., Moderate, SI 78)
However, one pinkish brown Tourmaline in our study showed a Drag response (see photo below). Spectrometer analysis suggests that the high magnetic susceptibility of this gem may be due to an abundance of cryptic Fe3+ iron in addition to the Fe2+-Ti4+ charge transfer that produces brown color. However, it is difficult to determine with a spectrometer whether it is cryptic iron (Fe3+) or cryptic manganese (Mn2+) that is responsible for the high magnetic susceptibility.
Pinkish Brown: Most pinkish brown Tourmalines such as the 2 gems pictured below do not show strong magnetism. It is likely that the color of these gems is due to iron-titanium charge transfer (brown color) in addition to low concentrations of manganese (Mn3+, pink color). The cushion on the left shows an Inert (Diamagnetic) response, and the square on the right shows a Weak response.
Pinkish Brown Tourmalines
(1 ct., Inert, SI <0 & 2ct., Weak SI 48)
Colorless and Near-colorless: Colorless Tourmalines such as the cabochon shown below (left) have the trade name "Achroite". Like most colorless allochromatic gems of any kind, it is diamagnetic because it lacks sufficient metallic chromophores to be attracted to a magnet. The near colorless yellow and pink gems shown below (right) are also diamagnetic. The manganese ions (Mn2+ and Mn3+) responsible for the faint colors are in concentrations too low to be detectable with a magnet.
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2.59ct., Inert & Moderate
1.99ct., Moderate & Weak
.64ct., Strong & Inert
Artificial irradiation in a laboratory will also create or enhance pink and red colors in Tourmaline gems, and this is a common treatment process. Subsequent treatment with heat will reduce or eliminate the pink and red colors and change the Mn3+ back to Mn2+. No experiments have been done to compare the magnetic susceptibilities of Tourmaline before and after irradiation or heat treatment, but we can speculate that irradiation might increase magnetic susceptibility slightly, and heat treatment might lower it slightly.
Pure yellow Tourmalines such as the 2 gems above are rare. Brownish yellow gems such as the 3 shown in the photo below are more common. Iron (Fe2+-Ti4+ charge transfer) is likely responsible for the brown component. The magnetic responses of these gems range from Inert to Drag.
The greenish yellow gem from Brazil and yellow pear from Tanzania pictured below have high manganese content and the highest magnetic susceptibilities of all yellow Tourmaline tested (SI 512 and SI 477). These are some of the highest magnetic susceptibilities for transparent Tourmalines of any color. Elbaite is known to mix in solid solution with Tsilaisite, a greenish yellow species with very high manganese (Mn2+) content. The Brazilian gem below (left) is likely an Elbaite whose composition is approaching Tsilaisite along the Elbaite-Tsilaisite solid solution continuum. The same may be true of other yellow Tourmalines that have very strong magnetism, such as the Tourmaline pear from Tanzania shown below (right).
A study that compares magnetic susceptibility to levels of manganese within Tsilaiste gems of known chemical compositions might show that Tsilaisite gems can be identified by susceptibility measurements alone. Determining the relative compositions of pure yellow Tourmalines that are intermediate between Tsialaisite and Elbaite end-members might also be possible using magnetic measurements if the theoretical susceptibility value of the pure Tsilaisite end member can be calculated.
Another interesting study might be to determine the changes in magnetic susceptibility of yellow gems induced by treatments. It has been shown that when yellow Tourmalines are treated with high temperature or irradiation, the Mn2+ changes to Mn3+ and the gems become red in color (Laurs, B. et. al, 2007). We might speculate that when strongly magnetic yellow gems are altered to red through these treatment processes, the magnetic susceptibilities of these gems will be slightly increased as a result of the change in the valence state of the manganese ions.
Gray: Gray color is sometimes seen in transparent Tourmalines. The Tourmaline cushion pictured below left shows a combination of blue and gray colors. It is highly magnetic and shows a Drag response due to high iron content. The blue color in this gem is likely due to the presence of iron (Fe2+). Is irradiation involved in the gray color, or does the blue-gray color and strong magnetism simply indicate an intermediary between blue Elbaite and black Schorl? The high measured magnetic susceptibility of this gem is intermediate between transparent blue Tourmaline and opaque black Tourmaline (Schorl).
The rectangular gem pictured below right is lavender-gray. Like the blue-gray gem on the left, it shows a Drag response and has a measured magnetic susceptibility that is at the high end for Elbaite Tourmaline. Iron accounts for the strong magnetism, and perhaps a small amount of Mn3+ (pink) is associated with the lavender color.
Unlike green and blue Tourmalines colored by iron, there is no clear correlation between color saturation and magnetic susceptibility when we compare light pink gems to bright pink gems, or light red gems to dark red gems. However, pink gems on average have higher magnetic susceptibilities than red gems, which is the reverse of what we would expect.
Rough Crystal (6mm), Burma
Pinkish Brown Tourmaline
(1.23 ct., Drag, SI 436)
Mozambique Yellow Tourmaline
(2.5ct.. Weak, SI <20)
Zambian Yellow Tourmaline
(.34ct., Drag, SI 309)
Brownish Yellow Tourmalines
(2.2ct., Inert, SI <0 & 1.16ct., Moderate, SI 104 & 1.5ct., Drag, SI 443)
Yellow Tourmaline, Brazil
(2.7ct., Drag, SI 512)
Bluish Gray Tourmaline
(7.50ct., Drags, SI 529)
Lavender Gray Tourmaline
(4.35ct., Drags. SI 469)
(1.84ct., Moderate SI 87)
(3.13ct., Inert, SI <0)
(38.54ct., San Diego, CA)
(1.09ct. & 3.64ct., Inert, SI <0)
As a side note, if we have a yellow gem of any kind that we are trying to identify, a Drag response to a magnetic wand narrows the possibilities to just 2 gem species: yellow Tourmaline or yellow Mali Garnet. These are the only 2 primary or common gemstones that will exhibit a Drag response.
As illustrated by the 2 gems shown below, there is no correlation between color intensity and magnetic susceptibility in yellow Tourmalines. The gem on the left from Mozambique shows a very Weak magnetic response. It is at least 15 times less magnetic than the gem on the right from Zambia, which has similar color and shows a Drag response. Spectrometer analysis indicates that the gem on the right is more magnetic because it has higher manganese (Mn2+) content.
Yellow: Yellow is an uncommon body color for Tourmaline gems. Sometimes referred to as Canary Tourmalines, yellow Tourmalines are mined in Zambia, Malawi, Mozambique, Nigeria, Madagascar and Brazil. The color is due to manganese-titanium (Mn2+-Ti4+) charge transfer as well as to ions of manganese in the bivalent state (Mn2+). As we have already seen, this valence state of manganese in high concentrations can result in high magnetic susceptibility. In this study, yellow Tourmalines had the widest range of magnetic response and susceptibility of any transparent color variety, ranging from Inert (< 0 SI) to Drag response (SI 512).
Yellow Tourmalines from Nigeria
(.92ct., Inert, SI <0, & 1.35ct., Moderate, SI 78)
As we have already shown, iron ions (Fe3+) and manganese ions (Mn2+) can be present in some colorless and near-colorless Tourmalines in levels that are sufficient to induce magnetic attraction without contributing color. Refer to the example of the bi-color (Indicolite blue and colorless) bar presented on the previous page in which the colorless portion shows moderate to strong magnetic susceptibility.
Pictured below is a near-colorless Tourmaline from Madagascar with only a hint of blue and yellow colors due to iron and manganese ions. Surprisingly, this gem is strongly magnetic. Examples such as these are further evidence that cryptic or "invisible” iron and/or manganese ions may at times account for large differences in magnetic susceptibility between two Tourmalines of similar color.
(4.68ct., Strong, SI 278)
Cryptic Manganese: Manganese (Mn2+) is a weak chromophore in Tourmalines, and increasing concentrations of Mn2+ may not necessarily correspond to brighter yellow color. The Mn2+ ions can be cryptic when in lower concentrations: i.e. these Mn2+ ions may not by themselves create color. The intensity of yellow color may be primarily controlled by Mn2+-Ti4+ charge transfer, which might be related to the concentration of titanium ions present in any particular gem. Cryptic ions of manganese (Mn2+) do not absorb enough light to be visible as absorption bands under a spectroscope, but they can be detected with a spectrometer and with a magnetic wand.
(1.18ct., Strong, SI 213)
Rossmanite is a rarely-seen lithium Tourmaline species with a chemical composition that is only slightly different than that of Elbaite (sodium Tourmaline). Like Elbaite, it derives it’s color and magnetism from idiochromatic Tourmalines that are mixed within it. Transparent crystals are generally pale pink due to manganese (Mn3+). Shown below is an example of an opaque pinkish purple Rossmanite cab from Manitoba, Canada. Purple color in this Rossmanite specimen may be related to inter-grown crystals of purple Lepidolite, another lithium mineral.
(9.5ct., Weak, SI <20)
High Manganese (Mn2+) Content
Causes This Gem to Drag
Yellow Tourmaline, Tanzania
(3.23ct, Drag, 477)
We encountered one highly anomalous red "Rubellite" with very high magnetic susceptibility. A 4.56ct gem from Madagascar shows a Drag response, and has a magnetic susceptibility measurement (SI 382) that is more than 5 times higher than the next most magnetic "Rubellite" in our study. Spectrometer analysis indicates a significant amount of cryptic manganese (Mn2+) may be responsible for the high magnetism.
"Rubellite" (4.56ct., Drag, SI 382)