What is the Supercontinent Cycle?

Supercontinent is generally defined as a continent with more than one continental core or craton.

Since 300 million to 200 million years ago,

Transcontinental

Continent of Armenia: Relative to the doctrine of the other Pangu, this group believes that the Pacific Ocean will disappear

The ultimate Pangu continent: after 250 million to 400 million years, the Atlantic Ocean will disappear

Australia-Antarctica-Eurasia, Africa: 130 million years later. Antarctica collides with southern Australia-Eurasia and Africa

Australia-Eurasia, Africa: 60 million years later. Australian mainland collides with East Asia to create orogenic movement equivalent to the Himalayas

Sur-continent

Eurasia and Africa: 5 million years ago to today

American continent: 15 million years ago to today

Eurasia: 60 million years to this day

Supercontinental prehistoric

Gondwana: 600 million to 30 million years ago

Laurasia: 300 million to 60 million years ago

Pangu continent: 300 million to 180 million years ago

Europe and America: 300 million years ago

Continent of Pannosia: 600 million to 540 million years ago

Rodinia: 1.1 billion to 750 million years ago

Continental Colombia: 1.8 billion to 1.5 billion years ago

Nina Continent: 1.8 billion years ago

Kenoland: 2.7 billion years ago

Ur continent: three billion years ago.

Komati Strata: 3.475 million years ago

Wabara: 3.6 billion years ago

Irgan Craton: 4.4 billion to 4.3 billion years ago ^[2]