Each face is as unique as the one on your skull.

We forged the form, you find your features.

Build your Face from the finest diamonds and gemstones this planet has to offer.

We’ll do the hard work for you, trust us on that. But how your Face looks is up to you!

Just something to consider upon your selection — different metals can help or hinder the natural colours of certain gemstones.

There’s no right or wrong — don’t let anyone tell you what you like!

Choose between a platinum or a gold frame.

Diamonds are in a class of their own, made of pure super-compressed carbon, arranged in a crystal lattice. Diamonds form when pure carbon is subjected to both extreme heat and pressure, roughly 150 to 200 kilometres deep in the Earth’s mantle.

The earliest recorded usage of diamonds was in India, during the 4th century BC. They are referenced in ancient Sanskrit texts such as the Arthashastra.

The word diamond comes from Greek ‘adamas’, meaning unconquerable.

Rubies are members of the corundum mineral family. They are composed of crystalline aluminium oxide (Al₂O₃), the same as sapphires!

Rubies are formed under intense heat and pressure deep within the Earth’s crust. Their formation is a particularly rare geological event as it requires an environment rich in aluminium, but low in silica and iron.

The earliest recorded usage of rubies was in ancient India, 200 BC. They’re referred to in ancient Sanskrit texts under the name ‘Ratnaraj’, or King of Gems. Rubies were believed to protect warriors in battle, guaranteeing rebirth as an emperor.

This makes ruby one of the earliest documented gemstones in human history.

Sapphires belong to the corundum mineral family, the same as rubies. They are formed of aluminium oxide (Al2O3).

Sapphires contain trace amounts of iron and titanium to give them their blue colour. Sapphires form 6 to 18 miles underground when intense heat (800°C–2,000°C) and pressure force aluminium and oxygen to crystallise. This requires a rare, silica-poor environment. Over millions of years, these crystals are pushed to the surface by tectonic shifts, or volcanic activity, where they are usually found in riverbeds.

The earliest recorded usage of sapphires was in Ancient Persia 500–300 BC. Persians even believed that the sky was blue because it reflected a giant sapphire beneath the Earth.

Sapphires are also extensively referenced in Greek and Roman texts, and even the Bible, associated with divine favour and truth.

Ultimately sapphire has been associated with wisdom and heaven for well over 2,000 years.

Emeralds belong to the beryl family of minerals (Be3Al2(SiO3)6). They get their green colour from trace amounts of chromium and sometimes vanadium. Other famous members of the beryl family include aquamarine, morganite, and red beryl.

Emerald formation is often referred to as a ‘geological miracle’, requiring superheated fluids to collide rare beryllium with deep-earth minerals chromium (and sometimes vanadium), which normally never meet.

Commonly recognised rankings in value by country: 1) Columbia  2) Zambia  3) Brazil  4) Afghanistan and Pakistan  5) Others, like Ethiopia and Russia

Emeralds’ usage traces back to Ancient Egypt, a staggering 1500 BC, mined at Mons Smaragdus (Cleopatra’s Mines). They were used by Egyptians, Greeks, and Romans as symbols of fertility, rebirth and eternal youth.

White diamonds are made of pure super-compressed, crystalline carbon. To make them yellow, the additional presence of nitrogen is needed. They have the same immense hardness as white diamonds (10 on the Mohs scale).

Just like white diamonds, they require extreme conditions to form. Yellow diamonds crystallise approximately 100 miles (160 km) beneath the Earth’s surface, in the mantle. They require temperatures exceeding 1,000°C and intense pressure to form. During crystallisation, nitrogen atoms substitute for some of the carbon atoms in the diamond’s crystal lattice.

They also remain trapped at these immense depths until rare, volcanic eruptions blast them closer to the surface, where they can be mined, or even found.

The earliest recorded use of yellow diamonds was in India, 4th–3rd century BC. Yellow diamonds were documented alongside colourless stones in early Sanskrit texts.

They were historically worn as symbols of divine favour, representing wealth and authority. In Europe, yellow diamonds were once considered less desirable, until modern fancy-colour grading reframed them as luxury objects. Yellow diamonds are a modern re-interpretation of ancient material.

Natural carbonado (the ‘space’ diamonds) are one of the rarest and certainly the most mysterious members of the family. Unlike other diamonds, they are polycrystalline, meaning they are made of millions of tiny carbon diamond crystals fused together.

Many scientists believe carbonados formed in supernova explosions billions of years ago, likely arriving on Earth inside a massive meteorite that crashed into the supercontinent Pangea before Africa and South America split apart.

Unlike traditional diamonds, they are highly porous, containing traces of nitrogen and hydrogen (common in space). They have also never been found in traditional diamond-bearing volcanic pipes (which is how diamonds usually come to the surface).

Carbonados are truly a unique, and fascinating stone — but beware of treated, or synthetics. These are increasingly prevalent.

Brazilians in the early 1700s were the first to find carbonado diamonds, discovered during gold-mining expeditions. Interestingly they were initially dismissed as low-value because they could not be faceted traditionally.

For years the were adopted for industrial use. It was only much later, in the late 20th century, when testing methods became more advanced, that we realised the true unique formation and structure of these stones, sky-rocketing their value.