GT Zirkon
Family overview
- Ultra Light Italic
- Thin Italic
- Light Italic
- Book Italic
- Regular Italic
- Medium Italic
- Bold Italic
- Black Italic
- Ultra LightZircon 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.
- Ultra Light 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.
- ThinZircon is an important gemstone, with several color forms used in various forms of jewelry.
- Thin ItalicZirconium is a mineral belonging to the group of nesosilicates.
- 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.
- BookMineral classification schemes and their definitions are evolving to match recent advances in mineral science.
- Book 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.
- RegularZircon is an important gemstone, with several color forms used in various forms of jewelry.
- Regular ItalicCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- MediumZirconium is a chemical element with symbol Zr and atomic number 40.
- Medium ItalicSilicon and oxygen constitute approximately 75% of the Earth’s crust, which translates directly into the predominance of silicate minerals.
- BoldZircon is a common accessory to trace mineral constituent of most granite and felsic igneous rocks.
- Bold ItalicThe dark brown to black color observed in most Zircon crystals is caused from iron oxide impurities.
- BlackResearchers 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.
- Black ItalicAs short and stubby crystals, as well as prismatic which are sometimes elongated.
- 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

