آرکتیکا
Sign in to saveArctica or Arctida is a hypothetical ancient continent which formed approximately 2.565 billion years ago in the Neoarchean era. It was made of Archaean cratons, including the Siberian Craton, with its Anabar/Aldan shields in Siberia, and the Slave, Wyoming, Superior, and North Atlantic cratons in North America. Arctica was named by because the Arctic Ocean formed by the separation of the North American and Siberian cratons. Russian geologists writing in English call the continent "Arctida" since it was given that name in 1987, alternatively the Hyperborean craton, in reference to the hyp
Key facts
- Historical continent.name
- Arctica
- Historical continent.image
- File:2400_Ma_paleoglobe.png
- Historical continent.caption
- Arctica, 2400 Ma (Siderian)
- Historical continent.formation_year
- 2565 Ma
- Historical continent.type
- Paleocontinent
via Wikipedia infobox
Wikidata facts
- Instance of
- paleocontinent
Show 1 more fact
- Commons category
- Arctica (continent)
Sources (1)
via Wikidata · CC0
Available in 19 languages
- Français
- Deutsch
- 中文
- Русский
- Português
- Italiano
- العربية
- Bahasa Indonesia
- Icelandic
- Kurdish
- Nederlands
- Norwegian Nynorsk
- Svenska
- Tiếng Việt
- Ukrainian
- Western Frisian
- فارسی
- 한국어
via Wikidata sitelinks · CC0