GT Zirkon

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Family overview
  • Ultra Light Italic
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  • Book Italic
  • Regular Italic
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  • Ultra Light
    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.
  • Ultra Light Italic
    Manly 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.
  • Thin
    Commercially valuable minerals and rocks are referred to as industrial minerals.
  • Thin Italic
    Zircon often contains traces of radioactive elements in its structure, which causes it to be metamict.
  • Light
    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.
  • Light Italic
    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.
  • Book
    Minerals are classified by key chemical constituents; the two dominant systems are the Dana classification and the Strunz classification.
  • Book Italic
    Zirconium is a chemical element with symbol Zr and atomic number 40.
  • Regular
    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.
  • Regular Italic
    The name zircon is taken from the name of the mineral zircon, the most important source of zirconium.
  • Medium
    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.
  • 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
    Radioactive dating shows that the zircon crystals were formed more than 4 billion years ago.
  • Bold 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.
  • Black
    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.
  • Black Italic
    The green coloring in many rounded pebbles usually indicates the Zircon is radioactive variety.
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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