Deep Siberian
Top Investment Grade
Distinct red/blue flashes. Contains the highest iron density.
You are not merely an owner; you are the steward of a specific spectrum of light against the entropy of the sun.
Amethyst is purple because gamma radiation knocked electrons out of place millions of years ago. The sun puts them back.
The stone is currently in total darkness. The "Color Centers" (excited iron atoms) are stable.
Investment Grade
Not all amethysts react to light the same way. The darker the stone, the more "Color Centers" you have to lose.
Top Investment Grade
Distinct red/blue flashes. Contains the highest iron density.
Rich & Jammy
Deep, saturated purple often found in geodes. Very photosensitive.
Standard Commercial
Lighter violet. Often heat-treated to become Citrine.
Victorian Style
Pale lilac/pink. Iron content is low, so fading is less dramatic but still possible.
Hardness measures resistance to scratching, not breaking.
Status: Pristine
Select an object to test relative hardness.
(Hover to reveal truth)
Indirect UV scatter from nearby windows can fade a stone over 5-10 years. Only total darkness stops the clock.
(Hover to reveal truth)
Heat turns Amethyst into Citrine (Yellow). Thermal shock from hot water can also fracture the stone instantly.
Verify your stewardship protocols. Each choice strengthens or degrades your shield integrity.
The system will present 5 scenarios. Your choices determine the longevity of your stone.
Select an environment to test safety.
Sequence Inactive
Follow the sequence precisely to avoid thermal shock and mechanical damage.
Fill two bowls with lukewarm water. Add a single drop of phosphate-free soap to the first bowl.
Why? Phosphate residue dulls the luster.
The stone's refractive index is restored. Return it to the dark box.
Advanced stewardship requires understanding the fundamental physics, chemistry, and history of the violet quartz. Access the dossiers below for the complete 2026 preservation standards.
To truly protect amethyst, one must understand that its color is not a chemical dye, but a quantum accident. Pure quartz ($SiO_2$) is transparent. Amethyst occurs when trace amounts of iron ($Fe^{3+}$) replace silicon in the crystal lattice. However, $Fe^{3+}$ alone only produces a pale yellow color (Citrine). The deep violet hue is born from gamma irradiation. Millions of years ago, natural radiation from surrounding bedrock (often granite containing Potassium-40) bombarded these iron impurities.
This high-energy event ejected an electron from the iron atom, oxidizing it to an unstable $Fe^{4+}$ state, creating what physicists call a Color Center. This specific electron configuration creates an absorption band at approximately 540nm, absorbing yellow/green light and transmitting the violet spectrum we adore.
The tragedy of amethyst stewardship is that this process is reversible. The "Color Center" is essentially an excited, unstable state held in suspension. It "wants" to return to its neutral, colorless state. Ultraviolet (UV) radiation acts as the catalyst for this return. When a high-energy UV photon (from sunlight) strikes the lattice, it provides just enough energy for a wandering electron to jump back into the hole left in the iron atom. This "neutralizes" the color center. The iron remains in the stone, chemically unchanged, but the geometry that bent the light is gone. The stone turns grey or clear.
This process, known as optical bleaching, is cumulative. A stone that spends 1 hour in the sun every day for 10 years will fade just as surely as one left on a dashboard for a month. The degradation curve is logarithmic; initial fading is slow, but once the lattice destabilizes, color loss accelerates.
In 2026, ultrasonic cleaners have become a common household appliance. For diamonds, they are excellent. For amethyst, they are a death sentence. Ultrasonic cleaners work by "cavitation"โcreating microscopic bubbles in the water that implode with immense force to blast away dirt. Amethyst is a Type II gemstone, meaning it almost always contains inclusions. These can be liquid-filled ("negative crystals") or healed fractures ("feathers"). When the ultrasonic waves hit these liquid inclusions, the vibration can cause the liquid inside the stone to expand rapidly. This internal pressure creates a stress fracture from the inside out. The stone doesn't just crack; it can shatter into cleavage fragments.
The surface of a polished amethyst depends on its vitreous (glass-like) luster to sparkle. However, silicon dioxide ($SiO_2$) is susceptible to etching from strong alkalis. Many "Dip" jewelry cleaners are ammonia-based (high pH). Repeated exposure to ammonia can micro-etch the surface of quartz, dulling the sharp facet junctions that give the stone its "crispness." Over time, an ammonia-cleaned amethyst will look sleepy or oily, not because it is dirty, but because the polish has been chemically abraded. The only approved solvent is surfactant-rich water: mild dish soap breaks the lipid bonds of skin oils without chemical aggression.
Historically, the finest amethysts came from the Ural Mountains in Russia. These stones, known as "Deep Siberian," possessed a unique property: red and blue flashes inside the purple body color. The mines are long exhausted, making true Siberian amethyst a rare investment asset. If you possess a vintage piece (pre-1900) with deep saturation, stewardship transforms from simple care to asset management. The loss of color in a Siberian amethyst deletes 80-90% of its market value.
Today, the market is defined by two major sources with distinct geological profiles. Brazilian Amethyst (Rio Grande do Sul) forms in massive geodes within basalt lava flows. These stones are generally lighter, with color often concentrated at the tips of the crystals. They are abundant and heat-treated commercially. Uruguayan Amethyst (Artigas), specifically from the Catalan region, forms in smaller gas cavities with much higher iron concentrations. This results in a "jammy," midnight purple. While more beautiful, Uruguayan stones are significantly more photosensitive due to the density of their color centers. A Uruguayan geode left on a sunny porch will turn grey within 2-3 years, whereas a paler Brazilian stone might last 10 years before noticeable change.
Prior to the 19th century, Amethyst was considered a "Cardinal Gem," equal in value to Diamond, Ruby, Sapphire, and Emerald. It adorned the fingers of Bishops and the crowns of royalty (including the British Imperial State Crown). Its scarcity was its value; the only major sources were Russia and scattered deposits in Europe.
This changed overnight with the discovery of massive deposits in Brazil in the 1800s. Suddenly, amethyst was abundant. The price crashed, democratizing the purple hue for the Victorian middle class. While this made the stone accessible, it also led to a degradation in care standards. "Semi-precious" implies "semi-disposable." This Codex aims to reverse that mindset. An amethyst, regardless of market price, is a non-renewable geological miracle. The specific conditions required to create a deep purple crystalโiron impurities plus gamma radiation plus hydrothermal growthโare rare in the universe. We preserve it not for its price tag, but for its irreplaceable physics.
There is a persistent myth that heating a faded amethyst will restore its purple. This is chemically false. Heating amethyst ($400^\circ C - 500^\circ C$) irreversibly changes the oxidation state of the iron, turning the stone yellow or orange (Citrine) or green (Prasiolite). Once an amethyst has been "burned" into Citrine, it can never be purple again.
The only theoretical way to restore color is to subject the stone to high levels of gamma radiation (Cobalt-60 source), mimicking the geological process. However, this is not a viable solution for the consumer. Industrial irradiation is prohibitively expensive for single stones. Furthermore, the color produced is often unstable or an ugly brown-grey ("smoky") that requires subsequent heat treatment to fix. Finally, stones treated this way can become slightly radioactive and must be quarantined. Conclusion: Prevention is the only cure. Once the violet is gone, it has returned to the ether.
Unlike diamonds, which are cut to maximize brilliance, amethyst is often cut to maximize color retention. Amethyst crystals often exhibit color zoningโangular bands of color separated by clear quartz. This is due to fluctuating conditions during the crystal's growth over millions of years.
A skilled lapidary (gem cutter) will orient the stone so that the deepest color zone is at the bottom (the culet). When you look through the table (top), the color reflects throughout the entire stone, creating an illusion of uniform purple. If you re-polish a damaged amethyst without understanding this zoning, you might accidentally grind away the only layer of color in the gem, turning a vibrant jewel into a piece of clear glass. This is why "aggressive buffing" to remove scratches is dangerous. Always consult a specialist lapidary who understands quartz zoning before attempting repair.