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
    Silicon and oxygen constitute approximately 75% of the Earth’s crust, which translates directly into the predominance of silicate minerals.
  • Ultra Light 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.
  • Thin
    An interesting habit occasionally exhibited in Zircon from a few localities is that their color darkens and their luster dulls upon prolonged exposure to sunlight.
  • Thin Italic
    Zircon is a common accessory to trace mineral constituent of most granite and felsic igneous rocks.
  • Light
    As short and stubby crystals, as well as prismatic which are sometimes elongated.
  • Light Italic
    During 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.
  • Book
    During 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.
  • Book Italic
    Radioactive dating shows that the zircon crystals were formed more than 4 billion years ago.
  • Regular
    Zircon is mainly consumed as an opacifier, and has been known to be used in the decorative ceramics industry.
  • Regular Italic
    Zirconium is a mineral belonging to the group of nesosilicates.
  • Medium
    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.
  • Medium Italic
    An interesting habit occasionally exhibited in Zircon from a few localities is that their color darkens and their luster dulls upon prolonged exposure to sunlight.
  • Bold
    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.
  • Bold Italic
    The dark brown to black color observed in most Zircon crystals is caused from iron oxide impurities.
  • Black
    Silicon and oxygen constitute approximately 75% of the Earth’s crust, which translates directly into the predominance of silicate minerals.
  • Black Italic
    Zircon often contains traces of radioactive elements in its structure, which causes it to be metamict.
  • 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