GT Zirkon
Family overview
- Ultra Light Italic
- Thin Italic
- Light Italic
- Book Italic
- Regular Italic
- Medium Italic
- Bold Italic
- Black Italic
- Ultra LightAustralia leads the world in zircon mining, producing 37% of the world total and accounting for 40% of world EDR for the mineral.
- Ultra Light ItalicAn interesting habit occasionally exhibited in Zircon from a few localities is that their color darkens and their luster dulls upon prolonged exposure to sunlight.
- ThinThe name derives from the Persian zargun meaning gold-hued; this word is corrupted into “jargoon”, a term applied to light-colored zircons.
- Thin ItalicMinerals are distinguished by various chemical and physical properties. Differences in chemical composition and crystal structure distinguish the various species, which were determined by the mineral’s geological environment when formed.
- LightMinerals are distinguished by various chemical and physical properties. Differences in chemical composition and crystal structure distinguish the various species, which were determined by the mineral’s geological environment when formed.
- Light ItalicDuring the growth process, crystals are also highly susceptible to consciousness imprinting, whereby the meditations, through-patterns, healing energy or bioelectric field identity of the grower may be enjoined within the crystalline structure and memory.
- BookZirconium is a chemical element with symbol Zr and atomic number 40.
- Book ItalicThe dark brown to black color observed in most Zircon crystals is caused from iron oxide impurities.
- RegularCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- Regular ItalicCurrently, zircons are typically dated by uranium-lead (U-Pb), fission-track, cathodoluminescence, and U+Th/He techniques.
- MediumThe dark brown to black color observed in most Zircon crystals is caused from iron oxide impurities.
- Medium ItalicZircons from Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, have yielded U-Pb ages up to 4.404 billion years
- BoldResearchers found that same carbon 12 isotope in the diamond specks, indicating that they may have been formed from ancient microbes that were buried deep underground and subjected to enormous pressure.
- Bold ItalicChemical substitution and coordination polyhedra explain this common feature of minerals.
- BlackCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- Black ItalicZircons from Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, have yielded U-Pb ages up to 4.404 billion years
- 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

