GT Zirkon
Family overview
- Ultra Light Italic
- Thin Italic
- Light Italic
- Book Italic
- Regular Italic
- Medium Italic
- Bold Italic
- Black Italic
- Ultra LightZircons from Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, have yielded U-Pb ages up to 4.404 billion years
- Ultra Light ItalicYellow, orange and red zircon is also known as “hyacinth”, from the flower hyacinthus, whose name is of Ancient Greek origin.
- ThinCurrently, zircons are typically dated by uranium-lead (U-Pb), fission-track, cathodoluminescence, and U+Th/He techniques.
- Thin ItalicScientists then studied the diamonds’ composition, looking specifically at their carbon isotopes.
- LightNew York University chemists have created three-dimensional DNA structures, a breakthrough bridging the molecular world to the world where we live.
- Light ItalicZircon is ubiquitous in the crust of Earth and it occurs as a common accessory mineral in igneous rocks, in metamorphic rocks and as detrital grains in sedimentary rocks.
- BookSilicon and oxygen constitute approximately 75% of the Earth’s crust, which translates directly into the predominance of silicate minerals.
- Book ItalicAs short and stubby crystals, as well as prismatic which are sometimes elongated.
- RegularMinerals are classified by key chemical constituents; the two dominant systems are the Dana classification and the Strunz classification.
- Regular ItalicThe green coloring in many rounded pebbles usually indicates the Zircon is radioactive variety.
- MediumMineral classification schemes and their definitions are evolving to match recent advances in mineral science.
- Medium ItalicThe abundance and diversity of minerals is controlled directly by their chemistry, in turn dependent on elemental abundances in the Earth.
- BoldScientists then studied the diamonds’ composition, looking specifically at their carbon isotopes.
- Bold ItalicScientists then studied the diamonds’ composition, looking specifically at their carbon isotopes.
- BlackThe abundance and diversity of minerals is controlled directly by their chemistry, in turn dependent on elemental abundances in the Earth.
- Black ItalicMinerals are classified by key chemical constituents; the two dominant systems are the Dana classification and the Strunz classification.
- Settings
Typeface information
GT Zirkon is an extravagant sans serif workhorse. It blends the worlds of rational tool and ornamentation by applying techniques used to optimize type for small sizes in a refined way.
Typeface features
OpenType features enable smart typography. You can use these features in most Desktop applications, on the web, and in your mobile apps. Each typeface contains different features. Below are the most important features included in GT Zirkon’s fonts:
- SS01
- Alternate Arrows
Volume ↗
- SS02
- Alternate f
Refraction
- ONUM
- Oldstyle Figures
0123456789
- SMCP
- Small Caps
Ore Deposit
Typeface Minisite


- Visit the GT Zirkon minisite to discover more about the typeface family’s history and design concept.
GT Zirkon in use

