GT Zirkon

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Family overview
  • Ultra Light Italic
  • Thin Italic
  • Light Italic
  • Book Italic
  • Regular Italic
  • Medium Italic
  • Bold Italic
  • Black Italic
  • Ultra Light
    Zircon is an important gemstone, with several color forms used in various forms of jewelry.
  • Ultra Light Italic
    Zircon 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.
  • Thin
    Zircon is a common accessory to trace mineral constituent of most granite and felsic igneous rocks.
  • Thin Italic
    Some 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.
  • Light
    Zirconium is a mineral belonging to the group of nesosilicates.
  • Light Italic
    Minerals 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.
  • Book
    Zircon often contains traces of radioactive elements in its structure, which causes it to be metamict.
  • Book Italic
    In 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.
  • Regular
    The English word “zircon” is derived from “Zirkon”, which is the German adaptation of this word.
  • Regular Italic
    Zirconium is a mineral belonging to the group of nesosilicates.
  • Medium
    Zircons from Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, have yielded U-Pb ages up to 4.404 billion years
  • Medium Italic
    Minerals 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
    Recent 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.
  • Bold Italic
    Radioactive dating shows that the zircon crystals were formed more than 4 billion years ago.
  • Black
    Researchers 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 Italic
    Mineral classification schemes and their definitions are evolving to match recent advances in mineral science.
  • Settings
    Size
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.

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Latin-alphabet languages: Afaan, Afar, Afrikaans, Albanian, Alsatian, Amis, Anuta, Aragonese, Aranese, Aromanian, Arrernte, Asturian, Atayal, Aymara, Azerbaijani, Basque, Belarusian, Bemba, Bikol, Bislama, Bosnian, Breton, Cape Verdean Creole, Catalan, Cebuano, Chamorro, Chavacano, Chichewa, Chickasaw, Cimbrian, Cofán, Cornish, Corsican, Creek, Croatian, Czech, Danish, Dawan, Dholuo, Drehu, Dutch, English, Estonian, Faroese, Fijian, Filipino, Finnish, French, Frisian, Friulian, Galician, Ganda, Genoese, German, Gikuyu, Gooniyandi, Greenlandic (Kalaallisut), Guadeloupean Creole, Gwich’in, Haitian Creole, Hawaiian, Hiligaynon, Hopi, Hungarian, Icelandic, Ido, Igbo, Ilocano, Indonesian , Irish, Istro-Romanian, Italian, Jamaican, Javanese, Jèrriais, Kaingang, Kala Lagaw Ya, Kapampangan, Kaqchikel, Kashubian, Kikongo, Kinyarwanda, Kiribati, Kirundi, Kurdish, Ladin, Latin, Latvian, Lithuanian, Lombard, Low Saxon, Luxembourgish, Maasai, Makhuwa, Malay, Maltese, Manx, Māori, Marquesan, Megleno-Romanian, Meriam Mir, Mirandese, Mohawk, Moldovan, Montagnais, Montenegrin, Murrinh-Patha, Nagamese Creole, Nahuatl, Ndebele, Neapolitan, Niuean, Noongar, Norwegian, Occitan, Old Icelandic, Old Norse, Oshiwambo, Palauan, Papiamento, Piedmontese, Polish, Portuguese, Q’eqchi’, Quechua, Rarotongan, Romanian, Romansh, Rotokas, Inari Sami, Lule Sami, Northern Sami, Southern Sami, Samoan, Sango, Saramaccan, Sardinian, Scottish Gaelic, Seri, Seychellois Creole, Shawnee, Shona, Sicilian, Silesian, Slovak, Slovenian, Somali, Upper and Lower Sorbian, Northern and Southern Sotho, Spanish, Sranan, Sundanese, Swahili, Swazi, Swedish, Tagalog, Tahitian, Tetum, Tok Pisin, Tokelauan, Tongan, Tshiluba, Tsonga, Tswana, Tumbuka, Turkish, Tuvaluan, Tzotzil, Venetian, Vepsian, Võro, Wallisian, Walloon, Waray-Waray, Warlpiri, Wayuu, Welsh, Wik-Mungkan, Wolof, Xavante, Xhosa, Yapese, Yindjibarndi, Zapotec, Zarma, Zazaki, Zulu, Zuni

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