glssopteris and other fossels were found on different contenents and could not swim across. also all of the contenents fit together like a. jiggsaw puzzle
Europe.
Asia
5
none
Two forms of evidence used to support continental drift are fossil evidence, where similar plant and animal fossils are found on different continents that were once connected, and geological evidence, such as matching rock formations and mountain ranges across separate continents. These pieces of evidence provide support for the idea that continents were once joined together and have since drifted apart.
The five contenents are : Australia Africa Europe Asia America
Asia and north America
Australia
Antarctica.
Egypt is in Africa, which is a contenent.
The mantle.