Alfred Wegener.
The theory of Pangaea was proposed by Alfred Wegener in 1912. Wegener suggested that the continents were once connected in a supercontinent known as Pangaea and have since drifted apart.
Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of Pangaea in 1912. He suggested that the continents were once joined together as a single landmass, which he called Pangaea, and that they have since drifted apart to their current positions.
Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of Pangaea and Panthalassa in the early 20th century. He suggested that the continents were once joined together in a supercontinent called Pangaea, surrounded by a single large ocean known as Panthalassa.
James Hutton did not propose the theory of Pangaea; it was actually proposed by Alfred Wegener in the early 20th century. Wegener's theory suggested that the Earth's continents were once joined together in a single supercontinent called Pangaea, which later broke apart and drifted to their current positions.
Alfred Wegener was the scientist who first proposed the theory of continental drift, which later developed into the theory of plate tectonics. He suggested that the continents were once joined together in a single supercontinent called Pangaea and have since drifted apart.
The theory of Pangaea was proposed by Alfred Wegener in 1912. Wegener suggested that the continents were once connected in a supercontinent known as Pangaea and have since drifted apart.
Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of Pangaea in 1912. He suggested that the continents were once joined together as a single landmass, which he called Pangaea, and that they have since drifted apart to their current positions.
Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of Pangaea and Panthalassa in the early 20th century. He suggested that the continents were once joined together in a supercontinent called Pangaea, surrounded by a single large ocean known as Panthalassa.
James Hutton did not propose the theory of Pangaea; it was actually proposed by Alfred Wegener in the early 20th century. Wegener's theory suggested that the Earth's continents were once joined together in a single supercontinent called Pangaea, which later broke apart and drifted to their current positions.
The theory of Pangaea was proposed by Alfred Wegener in 1912. He suggested that the continents were once joined together before breaking apart and drifting to their current positions.
Alfred Wegener was the scientist who first proposed the theory of continental drift, which later developed into the theory of plate tectonics. He suggested that the continents were once joined together in a single supercontinent called Pangaea and have since drifted apart.
Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of Pangaea in 1912. Wegener suggested that the continents were once connected in a supercontinent that later drifted apart to form the continents we see today.
The plate tectonic theory was first proposed by Alfred Wegener in 1912. He suggested that the continents were once joined together in a single landmass called Pangaea and have since drifted to their current positions.
The concept of Pangaea, a supercontinent that existed during the late Paleozoic and early Mesozoic eras, was first suggested by the German meteorologist Alfred Wegener in 1912. Wegener proposed the idea as part of his theory of continental drift, arguing that continents were once joined together and have since drifted apart. His ideas were initially met with skepticism, but they laid the groundwork for modern plate tectonics.
The existence of the supercontinent Pangaea was first proposed by Alfred Wegener, a German meteorologist and geophysicist, in 1912. Wegener's theory of continental drift suggested that the continents were once joined together in a single landmass before drifting apart over millions of years.
Alfred Wegener, a German meteorologist, proposed the first formal theory of continental drift in 1912. He suggested that the continents were once joined together in a single landmass called Pangaea, which later broke apart and drifted to their current positions.
the world was first known as a pangaea. pangaea is also called "all land"