Supercontinents are landmasses formed when continents collide and merge together. Some of the earliest proposed supercontinents include Vaalbara 3.5 billion years ago, Ur 3 billion years ago, and Kenorland 2.7 billion years ago. Later supercontinents included Columbia/Nuna/Hudsonland 1.8 billion years ago, Rodinia between 1.1-0.75 billion years ago, and Pannotia 750 million years ago. The most well known supercontinent, Pangaea, formed 300 million years ago before breaking apart. Scientists predict that in around 100 million years, a new supercontinent called Amasia will form when Asia collides with North America and other continents.