Tourmaline is a favorite of mineral collectors, gemstone collectors, and anyone who loves colorful semiprecious gemstone jewelry. It is often found in transparent crystals that have bright colors and are large enough for display, for faceting into gemstones, and even for carving. Exhibits on the third floor of the Natural History Museum of Utah include a variety of raw tourmaline specimens, jewelry, and carvings, but there are many more tourmaline specimens stored safely away in display drawers in the Museum's Earth Lab as well as the secure collections cabinets. In this article, we're happy to show you some of those colorful Tourmaline specimens from NHMU's collections and teach you more about this beautiful group of minerals.
A Family of Minerals
But before we look at beautiful specimens, let’s learn a little bit about tourmaline. Tourmaline is not a single mineral, but instead is a group or family of minerals that all have the same crystal structure but different atoms that fit into that structure. For example, the mineral dravite has the chemical formula Na(Mg3)Al6(Si6O18)(BO3)3(OH)3(OH). Fluor-dravite has the same formula except the (OH) on the end is replaced by F (fluorine).
Image 1 — A cross section of an elbaite tourmaline crystal from Minas Gerais, Brazil.
Other tourmaline minerals have other atoms such as K, Mn, Fe and Li in the place of some or all of the Na, Mg and Al. This accounts for the wide range of colors of tourmaline minerals, yet all have a hardness of 7.5 on the Moh’s hardness scale, which is hard enough for use as gemstones.
Tourmaline belongs to the trigonal crystal system, so we can usually recognize a tourmaline crystal by its’ slightly rounded 3-sided cross section. This is illustrated in Image 1 by a cross section of an elbaite tourmaline crystal from Minas Gerais, Brazil. This specimen is about 5 cm across and of the deep red color usually referred to as “rubellite”.
Elbaite: The Best-Known Tourmaline
Image 2 — An elbaite crystal that is green at the base and grades to red near the tip of the crystal.
Because elbaite is usually found as transparent and very colorful crystals that are large enough to cut into gemstones, it is the variety of tourmaline most people are familiar with. It is named after Elba, Italy where it was first found and described. Most commonly found in red, pink or green, it can also be blue or gray and in a variety of shades from pale to intense.
But, one of the most special characteristics of elbaite is that it can have multiple colors in the same crystal, often red or pink with green. When this happens, the stone is referred to as “watermelon” tourmaline. Image 2 shows an elbaite crystal that is green at the base and grades to red near the tip of the crystal. This one is also from Minas Gerais, Brazil. This crystal was formed in an open space or cavity in the rock where the crystal had been able to grow freely into the open space in the cavity. That is why the crystal is so perfect.
Image 3 shows a cluster of elbaite crystals from Minas Gerais, Brazil where smaller crystals grew out of the side of a group of larger crystals.
Image 3 — A cluster of elbaite crystals from Minas Gerais, Brazil.
Image 4 — A giant elbaite watermellon tourmaline specimen coated with feldspar crystals.
Elbaite tourmaline crystals are found intergrown with or associated with other minerals, especially quartz, mica and feldspar. Image 4 shows a giant elbaite watermellon tourmaline specimen coated with feldspar crystals. This elbaite is about 30 cm long, red in the interior and green on the outside, and estimated to contain more than 3500 carats of gem quality material.
Gem quality elbaite has been found in several places in the United States. One of the most famous places is San Diego County, California. Image 5 illustrates bicolored elbaite on quartz from the Himalaya Mine, Mesa Grande, California. Image 6 shows a specimen of bicolored elbaite with lepidolite mica and quartz from the other side of the country at Paris, Maine.
Image 5 — Bicolored elbaite on quartz from the Himalaya Mine, Mesa Grande, California.
Image 6 — A specimen of bicolored elbaite with lepidolite mica and quartz from the other side of the country at Paris, Maine.
Sometimes elbaite crystals form in sunbursts frozen in lepidolite mica as shown in Image 7. This specimen was collected in the Stewart Mine near Pala, California.
Image 7 — Elbaite crystals form in sunbursts frozen in lepidolite mica.
Quartz crystals often grow on the surface of elbaite crystals (Image 8) and sometime enclose the end of the tourmaline crystal, almost like a lollypop (Image 9).
Image 8 — Quartz crystals often grow on the surface of elbaite crystals.
Image 9 — Quartz crystals enclose the end of a tourmaline crystal, almost like a lollypop.
Image 10 shows a quite unusual specimen from Minas Gerais, Brazil with green elbaite on a manganese oxide mineral. Another unusual specimen, this one from Keystone, South Dakota, is illustrated in Image 11. Blue-green elbaite crystals are enclosed in muscovite mica.
Image 10 — An unusual specimen from Minas Gerais, Brazil with green elbaite on a manganese oxide mineral.
Image 11 — Blue-green elbaite crystals are enclosed in muscovite mica from Keystone, South Dakota.
Dravite and Schorl
Not all tourmaline minerals are transparent with bright colors. Although it can be green or yellow, dravite and fluor-dravite are typically brown. Image 12 shows a dravite specimen from the famous locality at Gouverneur, New York. Image 13 shows a specimen of schorl from another famous locality at Pierrepont, New York. Schorl is always black and is one of the most common tourmaline minerals, even occurring at a couple localities in Utah.
Image 12 — A dravite specimen from the famous locality at Gouverneur, New York
Image 13 — A specimen of schorl from another famous locality at Pierrepont, New York.