GT Zirkon
Family overview
- Ultra Light Italic
- Thin Italic
- Light Italic
- Book Italic
- Regular Italic
- Medium Italic
- Bold Italic
- Black Italic
- Ultra LightMinerals 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.
- Ultra 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.
- 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 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.
- LightScientists then studied the diamonds’ composition, looking specifically at their carbon isotopes.
- Light ItalicManly 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.
- BookMineral classification schemes and their definitions are evolving to match recent advances in mineral science.
- Book ItalicMinerals are classified by key chemical constituents; the two dominant systems are the Dana classification and the Strunz classification.
- RegularSome 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.
- Regular ItalicZircon is a common accessory to trace mineral constituent of most granite and felsic igneous rocks.
- MediumSilicon and oxygen constitute approximately 75% of the Earth’s crust, which translates directly into the predominance of silicate minerals.
- Medium ItalicCrystals are almost always terminated with a pyramidal termination, and may be doubly terminated, and occasionally entirely pyramidal resembling an octahedron.
- BoldThe English word “zircon” is derived from “Zirkon”, which is the German adaptation of this word.
- 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
- 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 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.
- 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.
- Designed by Tobias Rechsteiner
- Released in 2018
- Available in 16 styles
- GT Zirkon is available for customization and language extensions
- Download the free trial fonts
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
