GT Zirkon
Family overview
- Ultra Light Italic
- Thin Italic
- Light Italic
- Book Italic
- Regular Italic
- Medium Italic
- Bold Italic
- Black Italic
- Ultra LightSome rocks, such as limestone or quartzite, are composed primarily of one mineral—calcite or aragonite in the case of limestone, and quartz in the latter case.
- Ultra Light ItalicThe dark brown to black color observed in most Zircon crystals is caused from iron oxide impurities.
- ThinCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- Thin ItalicZircons from Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, have yielded U-Pb ages up to 4.404 billion years
- LightCommercially valuable minerals and rocks are referred to as industrial minerals.
- Light ItalicThe name zircon is taken from the name of the mineral zircon, the most important source of zirconium.
- BookConnected to internal radiation damage, these processes partially disrupt the crystal structure and partly explain the highly variable properties of zircon.
- Book ItalicZircons from Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, have yielded U-Pb ages up to 4.404 billion years
- RegularRecent experiments, for example, have shown that crystals grow five times faster when their supersaturated solution is subjected to frequencies of 10 to 100 cycles a second.
- Regular ItalicIn crystal growth, combinations of light intensity, light color, electric current, sound, the direction of these, plus the shape and size (frequency pattern) of the container or room, will all affect the final characteristics and energy potentials of a desired stone.
- MediumRadioactive dating shows that the zircon crystals were formed more than 4 billion years ago.
- Medium ItalicZirconium is a chemical element with symbol Zr and atomic number 40.
- BoldCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- Bold ItalicRadioactive dating shows that the zircon crystals were formed more than 4 billion years ago.
- BlackThe green coloring in many rounded pebbles usually indicates the Zircon is radioactive variety.
- Black ItalicThe abundance and diversity of minerals is controlled directly by their chemistry, in turn dependent on elemental abundances in the Earth.
- 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

