S America and N America - the Panama Canal, Europe, Asia, and Africa - the Suez.
The matching coastlines or jigsaw puzzle-like fit of the continents, as well as the fossil and rock formations that span across continents, suggested to early cartographers the concept of continental drift or the idea that the continents were once joined together in a single supercontinent. This idea eventually led to the development of the theory of plate tectonics.
Scientists use evidence such as matching geological formations, fossils, and remnants of ancient climates found on separate continents to support the theory of plate tectonics. By analyzing these pieces of evidence, scientists can infer that the continents were once part of a single supercontinent called Pangaea.
Wegener's background as a climatologist helped him notice similar fossil and rock formations, as well as ancient climates, on continents that are now separated by oceans. This led him to propose the theory of continental drift, suggesting that the continents were once joined together and have since drifted apart.
North America and Europe had matching rocks and minerals found, indicating that these continents were once joined together as part of the supercontinent Pangaea.
Around 200 million years ago, all the continents were joined together in a supercontinent called Pangaea. This event is known as Pangea's formation during the late Paleozoic and early Mesozoic eras. Over time, Pangaea began to break apart, eventually leading to the continents we see today.
Evidence of continental drift includes the matching shapes of continents, similar fossils found on different continents, and geological features that align across separate continents. These clues suggest that the continents were once joined together in a single landmass called Pangea.
Africa
Africa
Australia is not joined to another continent.
When all the continents were joined together as one supercontinent, it was called Pangaea.
The shape of the continents and the way they could fit together best suggests the formation of supercontinents in the past. Also, the distribution of biodiversity gives us information on which continents were joined and at what point they diverged.
If specific fossils are found in two separated continents, it means that both continents were once joined.
The two continents that are joined together are Asia and Europe.
Europe and Asia
The supercontinent that all continents were once joined to is called Pangaea. It existed during the late Paleozoic and early Mesozoic eras before breaking apart into the continents we know today.
Wegener believed all continents had once been joined because of the similar shapes of coastlines, matching geological formations across continents, and evidence of past glaciation extending from multiple continents, suggesting they were once connected.
The continents were once joined together as a supercontinent called Pangaea due to the movement of tectonic plates on the Earth's surface. Over millions of years, these plates have shifted and broken apart, moving the continents to their current positions.