GT Zirkon
Family overview
- Ultra Light Italic
- Thin Italic
- Light Italic
- Book Italic
- Regular Italic
- Medium Italic
- Bold Italic
- Black Italic
- Ultra LightYellow, orange and red zircon is also known as “hyacinth”, from the flower hyacinthus, whose name is of Ancient Greek origin.
- Ultra 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.
- ThinChemical substitution and coordination polyhedra explain this common feature of minerals.
- Thin ItalicThe dark brown to black color observed in most Zircon crystals is caused from iron oxide impurities.
- LightNew York University chemists have created three-dimensional DNA structures, a breakthrough bridging the molecular world to the world where we live.
- Light ItalicMinerals are classified by key chemical constituents; the two dominant systems are the Dana classification and the Strunz classification.
- BookCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- Book ItalicThe name zircon is taken from the name of the mineral zircon, the most important source of zirconium.
- RegularZircon is a common accessory to trace mineral constituent of most granite and felsic igneous rocks.
- Regular ItalicZircon often contains traces of radioactive elements in its structure, which causes it to be metamict.
- MediumAn interesting habit occasionally exhibited in Zircon from a few localities is that their color darkens and their luster dulls upon prolonged exposure to sunlight.
- Medium ItalicSilicon and oxygen constitute approximately 75% of the Earth’s crust, which translates directly into the predominance of silicate minerals.
- BoldMinerals 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.
- Bold ItalicZircons from Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, have yielded U-Pb ages up to 4.404 billion years
- BlackZircon often contains traces of radioactive elements in its structure, which causes it to be metamict.
- Black 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.
- 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