Trapiche Gems: An Introduction
Satisfying the human desire for symmetry, trapiche gems have a special allure. A trapiche (pronounced tra·PEE·che) is a type of milling wheel used to process sugar cane. Its spokes made it the namesake of trapiche gems, with their “spokes” or “arms” of inclusions between gemmy mineral growth. Since the geological conditions necessary to create these gems are uncommon, trapiche gems are some of the rarest specimens on Earth.
Due to their fairly recent discovery and extreme rarity, relatively little information on these gems is available. In this introduction to trapiche gems, you’ll learn some of the basic facts about these stones and their formation.
What is a Trapiche Gem?
Not to be confused with star stones, trapiche gems are minerals that form with a radiating star of inclusions between growth sectors. Some form with a core or hub with spokes radiating outward from the core, while others form spokes from the center of the gem. Only minerals with a highly symmetric crystal habit are known to form the “spokes” or “arms” that define a trapiche gem. Additionally, all true trapiche gems contain inclusions of organic matter.
Which Minerals Can Form Trapiche Gems?
In 1995, over a century after the first description of trapiche emeralds, Mong Hsu, Myanmar reported finding trapiche rubies. The next year, trapiche sapphires entered the market. Gemological laboratories have also confirmed specimens of trapiche tourmaline, garnet, quartz, spinel, and aquamarine.
Trapiche Gem Formation
True trapiches form where geothermal waters meet a carbonaceous host rock. These fluids are full of the chemicals that lead to gem formation, so seed crystals can form. Then, a type of zoning occurs during mineral growth. The gem ceases to grow along the rough edges of the crystal. Instead, it grows only on the smooth faces. This leads to the equivalent growth faces that trapiche gems display.
Type A and Type B
When the gem material grows on the mineral faces, with arms of carbonaceous inclusions, the trapiche gem is “type A” or “standard.” Exceptionally rare specimens of “type B” or “reverse” trapiches can also occur. In these specimens, the gem material itself forms the arms.
True trapiche gems have inclusions between growth sections. However, simple color zoning or inclusion growth within a crystal can create “trapiche-like” patterns in some gems. This means that the crystal of these trapiche-like gems is continuous, whereas in true trapiches the mineral is broken up into sectors which grow individually.
Still, these gems have the stunning symmetry associated with trapiche gems and are also immensely rare. The same minerals that form true trapiches may form trapiche-like color zoning or, in the case of rutilated quartz, spectacular patterned inclusions. In addition, diamond and pezzottaite (a part of the beryl family) can grow into trapiche-like gems.
Minerals with less symmetric crystal habits may also form trapiche-like gems. For example, trapiche-like rhodochrosite occurs in Argentina.