Supercontinents

Vaalbara is considered the oldest known supercontinent, existing during the Archean Eon.

Pangea was formed by the collision of all the major landmasses during the late Paleozoic era.

Rodinia was a supercontinent that existed during the Proterozoic Eon.

Columbia was formed by the collision of several cratons during the late Precambrian era.

Pannotia was a supercontinent that existed during the late Precambrian era.

Gondwana was formed by the collision of several landmasses during the early Paleozoic era.

Laurasia was formed by the collision of several landmasses during the early Mesozoic era.

Gondwanaland was formed by the collision of Gondwana and Laurasia during the late Mesozoic era.

Eurasia was formed by the collision of Europe and Asia during the Cenozoic era.

Amasia is a hypothetical supercontinent that is predicted to form in the future by the collision of Asia and North America.

Nuna was a supercontinent that existed during the Proterozoic Eon.

Kenorland was formed by the collision of several cratons during the early Proterozoic era.

Ur is a hypothetical supercontinent that is believed to have existed during the Archean Eon.

Vaalbara is considered the oldest known supercontinent, existing during the Archean Eon.

Kenorland was a supercontinent that existed during the Archean Eon.