Wegener called the whole land mass of land "Pangaea".not too sure but i think it means entire Earth . They were all at the Southern Hemisphere and then drifted away and finally came to the place hwere they currently are , this is Wegener's continental drift theory .
Alfred wegener came up with the theory of continental drift, when all of the continents were together as one the landmass was called Pangea
Alfred Wegener proposed the theory of continental drift, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart. This theory laid the foundation for the modern theory of plate tectonics.
Alfred Wegener did not develop the theory of climatic regions. He is, however, known for proposing the theory of continental drift, suggesting that Earth's continents were once joined together as a single landmass called Pangaea. This idea laid the foundation for the modern theory of plate tectonics.
Alfred Wegener is credited with being the founder of the theory of continental drift. In the early 20th century, he proposed the concept that Earth's continents were once joined together in a single landmass called Pangaea and have since drifted apart.
Alfred Wegener, a German meteorologist, is credited with developing the Theory of Continental Drift in the early 20th century. He proposed that Earth's continents were once joined together in a single landmass called Pangaea, and over time they drifted apart to their current positions.
Alfred wegener came up with the theory of continental drift, when all of the continents were together as one the landmass was called Pangea
Alfred Wegener proposed the theory of Continental Drift in 1912. He suggested that the continents were once joined together in a single landmass called Pangaea and then slowly drifted apart over millions of years.
The idea of continental drift was first proposed by Alfred Wegener in 1912. Wegener's theory suggested that the continents were once joined together in a single landmass called Pangaea and had drifted apart over time.
Alfred Wegener proposed the theory of continental drift, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart. This theory laid the foundation for the modern theory of plate tectonics.
The man who pioneered the continental drift hypothesis was Alfred Wegener. He proposed the theory in 1912, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart.
Alfred Wegener was a German meteorologist and geophysicist. He is known for developing the theory of continental drift, which proposed that the Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart. Wegener's work was highly influential in the development of the theory of plate tectonics.
Wegener's theory - Continental drift
Alfred Wegener did not develop the theory of climatic regions. He is, however, known for proposing the theory of continental drift, suggesting that Earth's continents were once joined together as a single landmass called Pangaea. This idea laid the foundation for the modern theory of plate tectonics.
Alfred Wegener is credited with being the founder of the theory of continental drift. In the early 20th century, he proposed the concept that Earth's continents were once joined together in a single landmass called Pangaea and have since drifted apart.
Alfred Wegener is credited with proposing the theory of continental drift in 1912. Wegener suggested that continents were once joined together in a single landmass called Pangaea and have since drifted apart over millions of years.
The theory that all continents were once joined together in a supercontinent called Pangaea and have since drifted apart is known as the theory of continental drift. This theory was proposed by Alfred Wegener in the early 20th century and later developed into the theory of plate tectonics.
Alfred Wegener, a German meteorologist, is credited with developing the Theory of Continental Drift in the early 20th century. He proposed that Earth's continents were once joined together in a single landmass called Pangaea, and over time they drifted apart to their current positions.