• Chemistry: (Th, U)SiO4, Thorium Uranium Silicate.
  • Class: Silicates
  • Subclass: Nesosilicates
  • Uses: As a minor ore of thorium and uranium and as mineral specimens.
  • Specimens

Thorite is the most common thorium mineral. Thorium is a highly radioactive element and could be used as a replacement for uranium in nuclear power generation. It is estimated to be three times as common as uranium and all the thorium in the Earth's crust could have more potential energy than both uranium and the fossil fuel reserves combined. Uranium and thorium are considered to be the primary sources of the internal heat of the Earth through their radioactive decay.

Although thorite is the most common thorium mineral, it is not the primary ore of thorium. The phosphate mineral monazite has an average of about 6% thorium in its composition that includes several rare earth elements. Enough monazite is mined to supply most of the current thorite demand. If monazite deposits become scarce or the demand for thorium increases, then thorite and to lesser extents other thorium bearing minerals such as thorianite, thorogummite , huttonite and thorutite will gain greatly in importance.

Thorite is currently an important ore of uranium. A variety of thorite often called "uranothorite" is particularly rich in uranium and has been a viable uranium ore at Bancroft, Ontario, Canada. Other varieties of thorite include "orangite", an orange variety; "calciothorite" an impure variety with trace amounts of calcium and "freyalite" actually a discredited variety containing cerium (it turned out to be an altered form of the mineral melanocerite).

There is a closely related mineral to thorite called thorogummite that was once considered a variety of thorite but is now known to be an alteration product of thorite. Thorogummite has some of the SiO4 tetrahedrons replaced by four hydroxides for a formula that looks like:

(Th, U)2(SiO4)(2 - X)(OH)4X

The X represents the conversion of one silicate tetrahedron with a negative four charge (-4) to four hydroxides with a negative one charge (-1) each. So that if half the silicate tetrahedrons are replaced by the four hydroxides, where X = 1, the formula would look like this:

(Th, U)2SiO4(OH)4

Thorite also is related to a mineral called huttonite. Thorite and huttonite are dimorphs (di means two and morph means shape). The two minerals have the same chemistry, they just have different structures. A similar situation occurs with the dimorphism of diamond and graphite, both of whom are composed of carbon, but have very different structures. Huttonite ironically belongs in the Monazite Group and is related structurally to its members.

Because thorite is highly radioactive, specimens are often metamict. This is a condition found in radioactive minerals and results from the destructive effects of its own radiation on its crystal lattice. The effect can destroy a crystal lattice completely while leaving the outward appearance unchanged. Thorogummite is believed to be formed from thorite by hydration which is facilitated by metamictation.

Specimens of thorite generally come from igneous pegmatites and volcanic extrusive rocks, hydrothermal veins, contact metamorphic rocks, and as small grains found in detrital sands. Crystals are rare, but when found can produce nicely shaped short prismatic crystals with pyramidal terminations. Remember, this is a radioactive mineral and should be stored away from other minerals that are subject to damage from radioactivity and of course human exposure should be limited !


  • Color is normally black, but also brownish black, orange, yellowish-orange and dark green.
  • Luster is resinous.
  • Transparency: Crystals are opaque.
  • Crystal System is tetragonal; 4/m 2/m 2/m
  • Crystal Habits include short prismatic crystals with a square cross-section and simple pyramidal terminations. Also massive, embedded irregular grains and reniform.
  • Cleavage is poor, in two directions lengthwise, but is rarely seen.
  • Fracture is conchoidal.
  • Hardness is 4.5 - 5
  • Specific Gravity is 4.1 - near 7.
  • Streak is orange to brown.
  • Other Characteristics: Nearly always metamict and always strongly radioactive.
  • Associated Minerals include quartz, feldspars, biotite and betafite.
  • Notable Occurrences are found at Langesundfjord, Norway; Bancroft, Ontario, Canada; Eifel District, Germany and Arizona, USA.
  • Best Field Indicators are color, luster, crystal habit, fracture and especially radioactivity.
THORITE specimens:
(hover for more info)
THORITE specimen tho-1
$ 25.00
Dims: 1.1 x 0.9 x 0.6" (2.8 x 2.3 x 1.5 cm)
Wt: 10.3 g
Saint Pierre Dome, El Paso County, Colorado, U.S.A.
Several portions of Thorite crystals are partly embedded in the host rock of this thumbnail specimen. All of these crystals are broken and incomplete, so much so that their tetragonal tabular form is impossible to determine (I would imagine that given this mineral's radioactivity, it would not form very definable crystals in the first place). They have a deep red-brown coloration and a dull matte luster, and are, of course, opaque. They rest in a dull, pale brown host rock that looks a lot like shale.
no photo
tho-1 ($ 25.00)
Saint Pierre Dome, El Paso County, Colorado, U.S.A.
THORITE specimen tho-2
$ 35.00
Dims: 0.9 x 0.8 x 0.5" (2.3 x 2.0 x 1.3 cm)
Wt: 6.2 g
Saint Pierre Dome, El Paso County, Colorado, U.S.A.
This thumbnail specimen consists of at least 2 partial tabular Thorite crystals. One of these crystals is heavily damaged and appears to be less than 50% complete, but the more exposed one seems to be at least 75% complete, if not more, and has visible dimensions of 0.5 x 0.4 x 0.1" (1.3 x 1.0 x 0.3 cm). Its tetragonal form is not well-defined, but is detectable. Both crystals have a moderately dark red-brown coloration and a matte luster, and are thoroughly opaque. They are partly embedded in a host rock that appears to be made up of a feldspar, and is rather rust-stained.
no photo
tho-2 ($ 35.00)
Saint Pierre Dome, El Paso County, Colorado, U.S.A.
THORITE specimen tho-3
$ 185.00
Dims: 0.9 x 0.8 x 0.3" (2.3 x 2.0 x 0.8 cm)
Wt: 7.7 g
Kemp property, Tory Hill, Cardiff Township, Haliburton County, Ontario, Canada
This thumbnail specimen consists of a single tetragonal tabular Thorite crystal. It is in good condition, showing little human-induced damage. Though it is heavily worn, it has the best form that I have ever seen in Thorite, as its tetragonal tabular form is definable. All of its edges are rounded and its faces are pitted and uneven, but can still be identified as such. The crystal has a moderately dark, rusty-brown coloration and a matte luster, and is thoroughly opaque. A few other smaller, broken Thorites are partly intergrown with the larger crystal, but there is no host rock present.
no photo
tho-3 ($185.00)
Kemp property, Tory Hill, Cardiff Township, Haliburton County, Ontario, Canada
THORITE specimen tho-4
$ 375.00
Dims: 1.8 x 1.4 x 1.0" (4.6 x 3.6 x 2.4 cm)
Wt: 0.9 oz. (26 g)
Kemp Prospect, Wilberforce, Ontario, Canada
Six intact Thorite crystals rest on the brown base of this hand specimen. These crystals are in excellent condition - the only visible damage is a crack that spans the length of the piece, running through 5 of them. The largest of these has dimensions of 0.7 x 0.4 x 0.3" (1.8 x 1.1 x 0.8 cm) and the smallest is maybe 33% of that size. All have excellent tetragonal tabular form, though their edges are somewhat rounded, and all have a rust-red color and a dull, earthy luster. A small, rounded and incomplete Thorite crystal is embedded in the bottom of the matrix rock. The piece registers substantially on my geiger-muller counter.
no photo
tho-4 ($375.00)
Kemp Prospect, Wilberforce, Ontario, Canada
THORITE specimen tho-5
$ 75.00
Dims: 1.6 x 1.5 x 0.9" (4.0 x 3.9 x 2.2 cm)
Wt: 0.9 oz. (25 g)
Kemp Prospect, Wilberforce, Ontario, Canada
One intact Thorite crystal rests on the base of this hand specimen. This crystal is in excellent condition, showing very light damage in a confined area, and has dimensions of 0.7 x 0.7 x 0.5" (1.8 x 1.8 x 1.3 cm). Its tetragonal tabular form is quite fat, giving it an almost prismatic habit, and its edges are rather rounded and worn. At least 3 other Thorite crystals are present on the piece, but these have a nearly black color, as opposed to the brick-red color of the intact crystal, and all of these are broken and incomplete. All have a dull, earthy luster, but the breakage surfaces of the incomplete crystals show a waxy or greasy luster. The piece registers quite readily on a geiger-muller counter.
no photo
tho-5 ($ 75.00)
Kemp Prospect, Wilberforce, Ontario, Canada


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