Alfred Wegener proposed the theory of continental drift, suggesting that the continents were once part of a supercontinent called Pangaea that broke apart and drifted to their current positions due to the movement of the Earth's tectonic plates. He suggested that the continents "plowed" through the oceanic crust as they moved.
Alfred Wegener, a German meteorologist, first proposed the theory of continental drift in 1912. He suggested that the continents were once joined together in a single landmass called Pangaea and had since drifted apart to their current positions.
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 called the supercontinent in his theory "Pangaea," which means "all lands" in Greek. He proposed that Pangaea existed about 300 million years ago and gradually broke apart to form the continents we have today.
The theory of Pangea was first proposed by Alfred Wegener in 1912. He suggested that Earth's continents were once joined together in a single landmass and later drifted apart to their current positions.
Alfred Wegener found several lines of evidence to support the theory of Pangaea, including the fit of the continents, similar rock formations and mountain ranges across continents, matching fossil remains on different continents, and similar climates and glacial deposits in areas that are now far apart.
Alfred Wegener theorize that all the continents were once joined together in a single landmass and have since drifted apart.
An earthquake.
They were joined together, then drifted apart to their current positions
Alfred Wegener, a German meteorologist and geophysicist, proposed the theory of continental drift in the early 20th century. He suggested that continents were once part of a single supercontinent called Pangaea and gradually drifted apart over time.
Alfred Wegener, a German meteorologist, first proposed the theory of continental drift in 1912. He suggested that the continents were once joined together in a single landmass called Pangaea and had since drifted apart to their current positions.
The concept of Pangaea, the ancient supercontinent, was proposed by Alfred Wegener in 1912 based on evidence from the fit of continents, fossil similarities, and rock formations. He suggested that the continents were once connected and have since drifted apart.
Alfred Wegener proposed the theory of continental drift in the early 20th century because he observed similar plant and animal fossils on continents that are now far apart, as well as matching geological formations and evidence of ancient climates that suggest the continents were once joined together 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.
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 believed that all of the continents were originally part of a single supercontinent called Pangaea, which existed about 300 million years ago. He suggested that over time, the continents drifted apart to their current positions through a process he called continental drift.
Alfred Wegener called his theory of moving continents "continental drift." He proposed that Earth's continents were once joined together in a single supercontinent called Pangea, which later broke apart and drifted to their current positions.
The idea of continents moving is known as the theory of plate tectonics, and it was proposed by Alfred Wegener in the early 20th century. Wegener suggested that continents were once joined together in a supercontinent called Pangaea and have since drifted apart.