Cycle de Wilson
Quasi-periodic aggregation and dispersal of Earth's continental crust
The supercontinent cycle is the quasi-periodic aggregation and dispersal of Earth's continental crust. There are varying opinions as to whether the amount of continental crust is increasing, decreasing, or staying about the same, but it is agreed that the Earth's crust is constantly being reconfigured.
Nº Q955317 ★★
Peu commune · Histoire
Cycle de Wilson
Quasi-periodic aggregation and dispersal of Earth's continental crust
The supercontinent cycle is the quasi-periodic aggregation and dispersal of Earth's continental crust. There are varying opinions as to whether the amount of continental crust is increasing, decreasing, or staying about the same, but it is agreed that the Earth's crust is constantly being reconfigured.
Dernier prix
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Prix plancher
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Médiane 7 j
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Ventes 30 j
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Fourchette 30 j
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En circulation
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médiane
min – max
ventes
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| Date | médiane | Min | Max | ventes |
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Historique des ventes
- Dernière vente
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- Moyenne 30 j
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- Plus bas 30 j
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- Plus haut 30 j
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- Ventes 7 j
- 0
- Ventes 30 j
- 0
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Sur Wikipédia
Texte en anglais Pas encore d'article dans ta langue : extrait en anglais.
The supercontinent cycle is the quasi-periodic aggregation and dispersal of Earth's continental crust. There are varying opinions as to whether the amount of continental crust is increasing, decreasing, or staying about the same, but it is agreed that the Earth's crust is constantly being reconfigured. One complete supercontinent cycle is said to take 300 to 500 million years. Continental collision makes fewer and larger continents while rifting makes more and smaller continents.
Texte : Wikipédia en anglais, CC BY-SA 4.0. · Image : User:Kieff (CC BY-SA 3.0) ·
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