Technical gemstone minerals (beryl, opal, turquoise, feldspar, olivine) Be3Al2Si6O18 / SiO2 / CuAl6(PO4)4(OH)8 / KAlSi3O8 / (Mg,Fe)2SiO4

Be3Al2Si6O18 (beryl) · beryl hexagonal; turquoise triclinic; orthoclase monoclinic; olivine orthorhombic; opal amorphous

Five gem minerals, grouped because they are sold and studied as crystal or mineral material rather than as single compounds: beryl (emerald is its green chromium-bearing form), opal (amorphous hydrated silica), turquoise (a hydrated copper aluminium phosphate), orthoclase feldspar (the family that includes moonstone) and olivine (peridot is its magnesium-rich form).

9 sources · Updated 2026-10-26 · CC BY 4.0

Evidence level

2 of 5

Lab-measured

Hardness

7.5 to 8

Density

2.63 to 2.97 g/cm3

Refractive index

1.567 to 1.610

Beryllium supply

430 t

Recipe, share of the weight

  • Be not statedBeryllium
  • Al not statedAluminium
  • Si not statedSilicon
  • O not statedOxygen
  • Cu not statedCopper
  • Mg and Fe not statedMagnesium and iron

Best for

Hard, transparent mineral material where hardness and density matter (beryl and forsterite are the hardest, at Mohs 7 to 8)

Weakest at

Brittleness and cleavage: the Handbook lists beryl, orthoclase and forsterite as brittle, and orthoclase cleaves perfectly on two planes. Opal and turquoise are softer, at Mohs 5 to 6

Risk at a glance

  • People Low. Beryl carries beryllium toxicity risk
  • If it fails Moderate. Brittle fracture
  • Corrosion No data. No corrosion data recorded

Quick facts: Be3Al2Si6O18 / SiO2 / CuAl6(PO4)4(OH)8 / KAlSi3O8 / (Mg,Fe)2SiO4

Key properties of Be3Al2Si6O18 / SiO2 / CuAl6(PO4)4(OH)8 / KAlSi3O8 / (Mg,Fe)2SiO4
PropertyValueBasis
Density1.9 to 3.27 g/cm³5 sourced values across conditions

What is the density of Technical gemstone minerals?

Technical gemstone minerals has a density of 1.9 to 3.27 g/cm³. The range covers 5 sourced values across the tempers, forms and test conditions the sources report; room-temperature values are used where a source states a temperature.

What is Technical gemstone minerals used for?

Uses recorded in the sources include Beryllium metal, oxide and beryllium-copper master alloy made from beryllium hydroxide (Utah plant); Plate glass, ceramic tiles and sanitaryware, made with feldspar as a flux and raw material.

Why it exists

These five minerals are the gem minerals that a technical buyer would weigh for hardness, density and optical index. Beryl is the hardest at Mohs 7.5 to 8. Opal is the lightest, with a density of 1.9 to 2.3 g/cm3. Turquoise and opal are the softest, at Mohs 5 to 6. The Handbook and webmineral pages give the index for each mineral, and the USGS covers beryllium and feldspar supply.

Where it's used

Beryllium from beryl

USGS: beryllium products went mainly to consumer electronics (about 29%) and aerospace and defense (about 24%). Imported beryl was one feedstock for the beryllium hydroxide used to make metal and oxide.

Feldspar for glass and ceramics

USGS: feldspar is a flux for plate glass, ceramic tiles and sanitaryware. Ceramics and pottery took 53% of domestic feldspar end use.

Recipe

Be3Al2Si6O18 (beryl); CuAl6(PO4)4(OH)8 4H2O (turquoise); SiO2 with water (opal); KAlSi3O8 (orthoclase); (Mg,Fe)2SiO4 (olivine); Mg2SiO4 (forsterite)

The five minerals are not one compound. Beryl is a beryllium aluminium silicate, turquoise a hydrated copper aluminium phosphate, opal a hydrated silica, orthoclase a potassium aluminium silicate, and olivine a magnesium iron silicate. Each is a natural mineral, so the formula varies with the locality.

What Be3Al2Si6O18 / SiO2 / CuAl6(PO4)4(OH)8 / KAlSi3O8 / (Mg,Fe)2SiO4 is made of
IngredientShare of the weightWhat it does
Beryllium Be not stated The light metal in beryl and the source of beryllium metal and oxide.
Aluminium Al not stated Present in beryl, turquoise and orthoclase.
Silicon Si not stated The main framework element of beryl, opal, orthoclase and olivine.
Oxygen O not stated Present in every silicate and phosphate.
Copper Cu not stated The colour-giving metal in turquoise.
Magnesium and iron Mg and Fe not stated The two cations that form the olivine series; peridot is the magnesium-rich end.

Weight shares are as printed in the sources.

What it can do

Hardness

7.5 to 8

Beryl is at Mohs 7.5 to 8 in the Handbook of Mineralogy, the hardest of the five. Orthoclase is 6 to 6.5, and turquoise is 5 to 6.

Density

2.63 to 2.97 g/cm3

Measured beryl density is 2.63 to 2.97 g/cm3. Opal is 1.9 to 2.3 g/cm3, and forsterite is 3.275 g/cm3.

Refractive index

1.567 to 1.610

The ordinary refractive index of beryl is 1.567 to 1.610, and opal is isotropic at 1.43.

Beryllium supply

430 t

World beryllium mine production was about 430 metric tons of beryllium content in 2025, with the United States at 230 tons.

How it compares

On the printed values, beryl is the hardest of the five minerals at Mohs 7.5 to 8, and forsterite (the magnesium end of the olivine series) is next at Mohs 7. Opal is the lightest, at 1.9 to 2.3 g/cm3. Beryl (2.63 to 2.97 g/cm3) is lighter than the olivine group (3.3) and forsterite (3.275), and turquoise (2.86) falls inside its range. Turquoise and opal are the softest. The sources read give no cost, availability or purity comparison between the minerals as crystal material, and none of them is sold by Goodfellow in the pages read.

The same measurements for each material, so you can compare them. Each row names the key condition under the value; the full conditions and methods are in the numbered notes under Technical details. Other materials are shown beside it; each was measured under its own conditions, so open its page before comparing closely. Compare every grade in the family.

Benchmarks
MeasurementBe3Al2Si6O18 / SiO2 / CuAl6(PO4)4(OH)8 / KAlSi3O8 / (Mg,Fe)2SiO4Al2O3Cr:Al2O3CaF2LiFZnSeZnSCsICdSe
Physical and electrical
Density of beryl, measured range2.63 to 2.97 g/cm³13.97 g/cm³3.98 g/cm³3.18 g/cc2.639 g/cc5.27 g/cm³4.09 g/cm³4.51 g/cc5.81 g/cm³
Density of beryl, calculated2.64 g/cm³23.97 g/cm³3.98 g/cm³3.18 g/cc2.639 g/cc5.27 g/cm³4.09 g/cm³4.51 g/cc5.81 g/cm³
Hardness of beryl7.5 to 8 -39 -9 -no datano datano datano datano data3.25 -
Density of turquoise, measured2.86 g/cm³63.97 g/cm³3.98 g/cm³3.18 g/cc2.639 g/cc5.27 g/cm³4.09 g/cm³4.51 g/cc5.81 g/cm³
Hardness of turquoise5 to 6 -79 -9 -no datano datano datano datano data3.25 -
Density of opal, range1.9 to 2.3 g/cm³113.97 g/cm³3.98 g/cm³3.18 g/cc2.639 g/cc5.27 g/cm³4.09 g/cm³4.51 g/cc5.81 g/cm³
Hardness of opalRange printed on the webmineral opal page5.5 to 6 -9 -9 -no datano datano datano datano data3.25 -
Density of orthoclase, measured range2.55 to 2.63 g/cm³123.97 g/cm³3.98 g/cm³3.18 g/cc2.639 g/cc5.27 g/cm³4.09 g/cm³4.51 g/cc5.81 g/cm³
Hardness of orthoclase6 to 6.5 -139 -9 -no datano datano datano datano data3.25 -
Specific gravity of olivine, calculated3.3 g/cm³173.97 g/cm³3.98 g/cm³3.18 g/cc2.639 g/cc5.27 g/cm³4.09 g/cm³4.51 g/cc5.81 g/cm³
Hardness of olivineRange printed on the webmineral olivine page6.5 to 7 -9 -9 -no datano datano datano datano data3.25 -
Density of forsterite, measured3.275 g/cm³183.97 g/cm³3.98 g/cm³3.18 g/cc2.639 g/cc5.27 g/cm³4.09 g/cm³4.51 g/cc5.81 g/cm³
Hardness of forsterite7 -199 -9 -no datano datano datano datano data3.25 -
Other measurements
Refractive index of beryl, ordinary ray (omega)1.567 to 1.61 -41.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of beryl, extraordinary ray (epsilon)1.565 to 1.599 -51.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of turquoise, alpha1.61 -81.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of turquoise, beta1.62 -91.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of turquoise, gamma1.65 -101.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of opalValue printed on the webmineral opal page1.43 -1.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of orthoclase, alpha1.518 to 1.52 -141.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of orthoclase, beta1.522 to 1.524 -151.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of orthoclase, gamma1.522 to 1.525 -161.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of olivine, alphaRange printed on the webmineral olivine page1.63 to 1.65 -1.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of olivine, gammaRange printed on the webmineral olivine page1.67 to 1.69 -1.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -
Refractive index of forsterite, gamma1.67 -201.768 -1.759 -1.399 -1.392 -2.403 -2.201 -1.739 -2.431 -

Why choose it, and why not

Good for

  • Hard, transparent mineral material where hardness matters: beryl at Mohs 7.5 to 8, and forsterite at Mohs 7.
  • Beryllium feedstock: imported beryl converted to beryllium hydroxide, as the USGS describes.
  • Glass and ceramic raw material: feldspar as a flux for plate glass and ceramic tiles.

Watch out for

  • Brittleness: beryl, orthoclase and forsterite are brittle, and orthoclase has perfect cleavage.
  • Softness: turquoise and opal are at Mohs 5 to 6, below beryl and orthoclase.
  • Beryllium toxicity: beryl dust must be controlled.
  • Source limits: no corrosion, ageing, fracture toughness or thermal data was read for these minerals.

Beryl is the hardest and most useful for technical crystal work, with a clear beryllium-toxicity limit. Opal, turquoise and the feldspar and olivine minerals are useful as data points but have few technical uses in the sources read. Goodfellow does not list these minerals on the pages read in this run, so this file is a mineral data record, not a supplier listing. For the alumina crystals used as optics and substrates, see the sapphire and ruby profiles (sapphire.yaml and ruby.yaml).

Technical details

For scientists and researchers. Everything above comes from the record below: every number with its method, its conditions and its source.

Notes

The method, full conditions and any caveat for the numbered rows above.

Notes for the numbered rows
#MeasurementMethodConditionsCaveat
1Density of beryl, measured rangeRange printed in the Handbook of Mineralogy beryl entrymineral beryl (Be3Al2Si6O18), including emeraldnote Handbook says density increases with alkali content; average 2.7—
2Density of beryl, calculatedCalculated value printed in the Handbook of Mineralogy beryl entrymineral beryl (Be3Al2Si6O18)—
3Hardness of berylRange printed in the Handbook of Mineralogy beryl entrymineral beryl (Be3Al2Si6O18)scale Mohs (the Handbook prints the hardness without naming the scale)—
4Refractive index of beryl, ordinary ray (omega)Range printed in the Handbook of Mineralogy beryl entrymineral beryl (Be3Al2Si6O18)wavelength not stated in the entrynote Handbook says the index increases with alkali content—
5Refractive index of beryl, extraordinary ray (epsilon)Range printed in the Handbook of Mineralogy beryl entrymineral beryl (Be3Al2Si6O18)wavelength not stated in the entry—
6Density of turquoise, measuredValue printed in the Handbook of Mineralogy turquoise entrymineral turquoise (CuAl6(PO4)4(OH)8 4H2O)note Handbook says less when massive—
7Hardness of turquoiseRange printed in the Handbook of Mineralogy turquoise entrymineral turquoisescale Mohs (the Handbook prints the hardness without naming the scale)—
8Refractive index of turquoise, alphaValue printed in the Handbook of Mineralogy turquoise entrymineral turquoisewavelength not stated in the entry—
9Refractive index of turquoise, betaValue printed in the Handbook of Mineralogy turquoise entrymineral turquoisewavelength not stated in the entry—
10Refractive index of turquoise, gammaValue printed in the Handbook of Mineralogy turquoise entrymineral turquoisewavelength not stated in the entry—
11Density of opal, rangeRange printed on the webmineral opal page (Physical Properties)mineral opal (SiO2 with water)note the page gives an average of 2.09 g/cm3—
12Density of orthoclase, measured rangeRange printed in the Handbook of Mineralogy orthoclase entrymineral orthoclase (KAlSi3O8), the feldspar family that includes moonstonenote moonstone is an adularia variety; the Handbook orthoclase entry does not name moonstone—
13Hardness of orthoclaseRange printed in the Handbook of Mineralogy orthoclase entrymineral orthoclasescale Mohs (the Handbook prints the hardness without naming the scale)—
14Refractive index of orthoclase, alphaRange printed in the Handbook of Mineralogy orthoclase entrymineral orthoclasewavelength not stated in the entry—
15Refractive index of orthoclase, betaRange printed in the Handbook of Mineralogy orthoclase entrymineral orthoclasewavelength not stated in the entry—
16Refractive index of orthoclase, gammaRange printed in the Handbook of Mineralogy orthoclase entrymineral orthoclasewavelength not stated in the entry—
17Specific gravity of olivine, calculatedCalculated value printed on the webmineral olivine pagemineral olivine group, (Mg,Fe)2SiO4—
18Density of forsterite, measuredValue printed in the Handbook of Mineralogy forsterite entrymineral forsterite (Mg2SiO4), the magnesium end member of the olivine series—
19Hardness of forsteriteValue printed in the Handbook of Mineralogy forsterite entrymineral forsteritescale Mohs (the Handbook prints the hardness without naming the scale)—
20Refractive index of forsterite, gammaValue printed in the Handbook of Mineralogy forsterite entrymineral forsteritewavelength not stated in the entry—

Risks and side effects

Hazards to people, what happens when a cell overheats, and how the material is handled and stored.

For people

USGS says beryllium is toxic and that industry must control its dust, fumes and mists. Beryl is a beryllium feedstock, so the same concern applies to beryl dust.

Beryllium
USGS: beryllium is toxic, so workplace dust, fumes and mists must be controlled.
Silica
Opal is a hydrated silica. No silica hazard was read in a source, so none is stated here.

If it fails

The failure facts come from the Handbook of Mineralogy entries, not from field incidents.

Breaking
The Handbook lists beryl, orthoclase and forsterite as brittle, so they break rather than bend.
Cleavage
Orthoclase cleaves perfectly on two planes, so a stressed crystal can split along flat faces.

Handling and storage

Dust
Keep beryl dust out of the air in the workplace, as the USGS says for beryllium.
Not covered
No storage temperature or humidity limit was read for any of the five minerals.

Test details
The original wording and numbers from the sources, for readers who want them.

Failure risks

Failure risks
FailureTrigger and consequence
Brittle fracturemoderate severityImpact or bending of a faceted or thin pieceThe Handbook lists beryl, orthoclase and forsterite as brittle, so these crystals break rather than bend.
Perfect cleavage in orthoclasemoderate severityStress along the cleavage planesThe Handbook gives perfect cleavage on the 001 and 010 planes, so the crystal splits along flat faces.

Handling and storage

  • Keep beryl dust, fumes and mists out of the workplace air, as the USGS notes that industry must control beryllium dust.

Supply and geography

How common the raw materials are and where they come from.

Beryllium, world mine production 2025 estimate (metric tons of beryllium content)

Top producers (2025)
United States 53.5%, Brazil 18.6%, China 17.9%, Nigeria 9.3%
Recycling
USGS: recovered from new and old scrap, which may be 20% to 25% of total beryllium consumption.
Substitutes
USGS: aluminum, silicon carbide, steel or titanium may replace beryllium metal in some uses, but the substitutes reduce performance.; USGS: aluminum nitride or boron nitride may be substituted for beryllium oxide.

Feldspar, world mine production 2025 (thousand metric tons)

Top producers (2025)
India 19.4%, Turkey 17.1%, Iran 12.6%, China 11.9%
Recycling
USGS: feldspar is not recycled by producers; container cullet reduces consumption of feldspar in glass.
Substitutes
USGS: imported nepheline syenite was the major alternative material for feldspar.