Chronology of continents
From Wikipedia, the free encyclopedia
A continent is a large geographical region defined by the continental shelves and the cultures on the continent.[1] In the modern day, there are seven continents. However, there have been more continents throughout history. Vaalbara was the first supercontinent.[2] Europe is the newest continent.[3] Geologists have predicted that certain continents will appear, these being Pangaea Proxima, Novopangaea, Aurica, and Amasia.
List of continents
| Name | Era | Time before present | Image | Reference |
|---|---|---|---|---|
| Vaalbara | Eoarchean | 3.6-2.7 Ga | [2] | |
| Ur | Paleoarchean | 3.1 Ga | [4] | |
| Kenorland | Neoarchean | 2.7 Ga | [5] | |
| Arctica | Neoarchean | 2.565 Ga | [6] | |
| Columbia | Paleoproterozoic | 2.1-1.5 Ga | [7] | |
| Atlantica | Paleoproterozoic | 2.0 Ga | [8] | |
| Nena | Paleoproterozoic | 1.9 Ga | [9] | |
| Baltica | Paleoproterozoic | 1.8 Ga | [10] | |
| Rodinia | Neoproterozoic | 1100-633 Ma | [11] | |
| Avalonia | Neoproterozoic | 750 Ma | [12] | |
| Pannotia | Neoproterozoic | 500-600 Ma | [13] | |
| Pampia | Neoproterozoic | 555-515 Ma | [11] | |
| Gondwana | Neoproterozoic | 550 Ma | [14] | |
| Cimmeria | Neoproterozoic | 550 Ma | [15] | |
| Laurasia | Neoproterozoic | 550 Ma | [16] | |
| Cuyania | Paleozoic | ~420-390 Ma | [17] | |
| Chilenia | Paleozoic | ~420-390 Ma | [18] | |
| Pangaea | Paleozoic | 335 Ma | [16] | |
| Africa | Paleozoic | 300 Ma | [19] | |
| South America | Mesozoic | 225 Ma | [20] | |
| North America | Mesozoic | 200 Ma | [21] | |
| Mauritia | Mesozoic | 70-60 Ma | [22] | |
| Asia | Mesozoic | 66 Ma | [23] | |
| Australia | Cenozoic | 10 Ma | [24] | |
| Europe | Cenozoic | 5 Ma | [25] | |
| Pangaea Proxima | ~250 myf | [3] | ||
| Novopangaea | ~250 myf | [26] | ||
| Aurica | ~250 myf | [26] | ||
| Amasia | ~250 myf | [26] |