GT Zirkon
Family overview
- Ultra Light Italic
- Thin Italic
- Light Italic
- Book Italic
- Regular Italic
- Medium Italic
- Bold Italic
- Black Italic
- Ultra LightManly P. Hall and other students of esoteric wisdom have also noted that many ancient crystals were produced by ‘zodiacal formulae’ grown at specific times, when the sun, moon and planets were in special heavenly positions.
- Ultra Light ItalicMinerals are classified by key chemical constituents; the two dominant systems are the Dana classification and the Strunz classification.
- ThinZircons from Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, have yielded U-Pb ages up to 4.404 billion years
- Thin ItalicZircon is a common accessory to trace mineral constituent of most granite and felsic igneous rocks.
- LightCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- Light ItalicResearchers 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.
- BookZircon is mainly consumed as an opacifier, and has been known to be used in the decorative ceramics industry.
- Book ItalicChemical substitution and coordination polyhedra explain this common feature of minerals.
- RegularZirconium is a chemical element with symbol Zr and atomic number 40.
- Regular 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.
- MediumRadioactive dating shows that the zircon crystals were formed more than 4 billion years ago.
- Medium ItalicYellow, orange and red zircon is also known as “hyacinth”, from the flower hyacinthus, whose name is of Ancient Greek origin.
- BoldMinerals are classified by key chemical constituents; the two dominant systems are the Dana classification and the Strunz classification.
- Bold ItalicSilicon and oxygen constitute approximately 75% of the Earth’s crust, which translates directly into the predominance of silicate minerals.
- BlackAn interesting habit occasionally exhibited in Zircon from a few localities is that their color darkens and their luster dulls upon prolonged exposure to sunlight.
- Black ItalicZircon is a common accessory to trace mineral constituent of most granite and felsic igneous rocks.
- 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

