Vaalbara is a hypothetical supercontinent that is believed to have existed around 2.5 to 3.1 billion years ago during the Paleoproterozoic era. It is thought to have been a joining of several ancient cratons, specifically the West Australian craton and the Kaapvaal craton. The existence of Vaalbara is suggested by geological and paleomagnetic evidence.
Vaalbara
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The first supercontinent is called Rodinia. It existed around 1.3 billion years ago and was formed through the collision of smaller continents.
The first continent is believed to be Pangaea, which existed around 300 million years ago. Pangaea eventually broke apart due to tectonic plate movements, leading to the formation of the continents we know today.
The supercontinent that was formed during the Paleozoic era was called Pangaea. It existed approximately 335 to 175 million years ago and was made up of almost all of Earth's landmasses. Pangaea began to break apart during the Mesozoic era, eventually leading to the continents we recognize today.
Slower again than Plate Tectonics could be the cycle of super-continent accumulation and dispersal. There have been several of these. Vaalbara, 3.1 - 2.8 Ga ago. Ga = Giga years ago. 10^9. Kenorland, 2.7 - 2.5 Ga ago Columba / Nuna, 2.0 - 1.5 Ga ago Rodina, 1100 - 750 Ma ago Pangaea, 300 - 200 Ma.
When the continents were all together, they were called supercontinents. The Earth is thought to be 4.6 billion years old. The oldest theorized supercontinent is Vaalbara, which may have formed 3.3 billion to 3.6 billion years ago. The oldest known supercontinent is Ur, which formed 3 billion years ago. The Kenorland supercontinent formed 2.7 billion years ago. Columbia formed 1.8 billion to 1.5 billion years ago. Rodinia formed 1.1 billion to 750 million years ago. Pannotia, which also is called the Vendian supercontinent, formed 600 million to 540 million years ago. Pangaea formed 500 million to 200 million years ago. Laurasia formed 200 million years ago. And the last supercontinent was Gondwana. But that title may be held only temporarily by Gondwana. For the future may hold possibilities of one or two supercontinents within the next millions of years.