GT Zirkon
Family overview
- Ultra Light Italic
- Thin Italic
- Light Italic
- Book Italic
- Regular Italic
- Medium Italic
- Bold Italic
- Black Italic
- Ultra LightCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- Ultra Light ItalicThe abundance and diversity of minerals is controlled directly by their chemistry, in turn dependent on elemental abundances in the Earth.
- ThinZirconium is a chemical element with symbol Zr and atomic number 40.
- 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 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.
- BookSilicon and oxygen constitute approximately 75% of the Earth’s crust, which translates directly into the predominance of silicate minerals.
- 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 mainly consumed as an opacifier, and has been known to be used in the decorative ceramics industry.
- Regular ItalicSome 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.
- MediumZirconium is a chemical element with symbol Zr and atomic number 40.
- Medium ItalicThe name derives from the Persian zargun meaning gold-hued; this word is corrupted into “jargoon”, a term applied to light-colored zircons.
- BoldZirconium is a chemical element with symbol Zr and atomic number 40.
- Bold 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.
- BlackZircon 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.
- Black ItalicThe English word “zircon” is derived from “Zirkon”, which is the German adaptation of this word.
- 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