Uncommon Elements Make Uncommon Gemstones


Step 1: Introduction to Gemology

Lesson 5

Why are some gems more common in nature than others? Gemology teaches us that crystalline gemstones need five things to develop: ingredients, temperature, pressure, time, and space. Let’s take a closer look at that first requirement. Since the principal source of ingredients for gems is the rocky Earth itself, knowing the abundance of the elements that make up the minerals in the Earth’s crust will help us understand why there are common and uncommon gemstones.

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“Quartz” by Franco is licensed under CC By 2.0

The Abundance of Elements In The Earth’s Crust

The following figures are estimated percentages of the Earth’s crust by weight.

The eight most common elements in the crust are:

  • Oxygen (O) 46.4%
  • Silicon (Si) 28.15%
  • Aluminum (Al) 8.23%
  • Iron (Fe) 5.63%
  • Calcium (Ca) 4.15%
  • Sodium (Na) 2.36%
  • Magnesium (Mg) 2.33%
  • Potassium (K) 2.09%

All other elements represent a mere 0.66% of the crust.

From a gemological perspective, the following uncommon elements in the Earth’s crust are of particular interest:

  • Manganese (Mn) .095%
  • Carbon (C) .02%
  • Zirconium (Zr) .0165%
  • Vanadium (V) .0135%
  • Chromium (Cr) .01%
  • Nickel (Ni) .0075%
  • Copper (Cu) .0055%
  • Cobalt (Co) .0025%
  • Lithium (Li) .002%
  • Beryllium (Be) .00028%

A World of Oxygen and Silicon

Oxygen and silicon make up more than 74% of the Earth’s crust. It’s not surprising that quartz (SiO2) is one of the most common gemstone minerals. However, oxygen and silicon are also found in some uncommon gemstones. Spodumene is a gemstone mineral composed of oxygen, silicon, aluminum, and lithium (LiAlSi2O6). Lithium makes up just two thousandths of 1% of the Earth’s crust.

Spudomene_sfaccettato,_da_minas_geiras,_brasile
“Spudomene sfaccettato, da minas geiras, brasile” (Faceted Spodumene) by Sailko is licensed under CC by 3.0

Kunzite, a pinkish variety of spodumene, gets its color from the addition of another uncommon element, manganese.

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“Crystals of spodumene var. kunzite” by Géry Parent is licensed under CC By-ND 2.0

From Emery Boards to Prized Jewels

Corundum (Al2O3) is a common mineral composed of aluminum and oxygen. You’ll frequently find it on sandpaper and nail files as emery. Gem-grade corundum, however, is considerably more rare, even rarer than diamonds. Corundum gems that include a rare trace of chromium are red in color. This red variety of corundum is more commonly known as ruby. Chromium is just one hundredth of 1% of the Earth’s crust.

Beryllium is less than three ten-thousandths of 1% of the Earth’s crust but it’s a primary ingredient of beryl gemstones (Be3Al2Si6O18). With the addition of chromium, beryl becomes emerald. Likewise, with the addition of cobalt, another rare element, spinel takes on a very rare cobalt blue color.

Spinel-199585
“Spinel” by Rob Lavinsky is licensed under CC By-SA 3.0

About the author
Donald Clark, CSM IMG
Donald Clark, CSM founded the International Gem Society in 1998. Donald started in the gem and jewelry industry in 1976. He received his formal gemology training from the Gemological Institute of America (GIA) and the American Society of Gemcutters (ASG). The letters "CSM" after his name stood for Certified Supreme Master Gemcutter, a designation of Wykoff's ASG which has often been referred to as the doctorate of gem cutting. The American Society of Gemcutters only had 54 people reach this level. Along with dozens of articles for leading trade magazines, Donald authored the book "Modern Faceting, the Easy Way."
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