The Pangaea theory or the Expanding Earth theory posits that the Earth originally had one supercontinent that slowly divided. Pangaea is the name of the supercontinent.
Alfred Wegener proposed the theory of continental drift in 1912, suggesting that the Earth's continents were once joined together in a single supercontinent called Pangaea and have since drifted apart to their current positions. He argued that the continents move slowly over time due to tectonic plate movement.
The hypothesis that states that continents slowly moved to their present-day positions on Earth is called continental drift. This theory was proposed by Alfred Wegener in the early 20th century, suggesting that continents were once part of a single supercontinent called Pangaea and have since drifted apart.
Pangaea was a supercontinent that existed about 335 million years ago and eventually broke apart to form the continents we have today due to the movement of tectonic plates. Over millions of years, the continents have drifted apart, leading to the formation of new oceans and mountain ranges as a result of plate tectonics.
Wegener's idea is known as continental drift. He proposed that the Earth's continents were once connected as a single landmass called Pangea and have since drifted apart over time.
The hypothesis is called continental drift. It suggests that the Earth's continents were once part of a single supercontinent called Pangaea and have since moved slowly over time to their current positions. This movement is driven by the process of plate tectonics.
Alfred Wegener proposed the theory of continental drift, suggesting that the continents were once joined together in a single landmass called Pangea and have since drifted apart to their current positions on Earth's surface. He believed that the continents moved slowly over time due to the process of plate tectonics.
Alfred Wegener proposed the theory of continental drift in 1912, suggesting that the continents had once been part of a single supercontinent called Pangaea. He suggested that the continents slowly drifted apart over millions of years due to the movement of the Earth's tectonic plates.
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.
Through the passage of time, the continents have gradually moved across the earth's surface into their present positions. This is called the continental drift.
The theory is called plate tectonics, which posits that Earth's outer shell is divided into several large, rigid plates that move and interact with one another. This movement can result in phenomena such as earthquakes, volcanic activity, and the drifting of continents over millions of years.
Alfred Wegener proposed the theory of continental drift in 1912, suggesting that the Earth's continents were once joined together in a single supercontinent called Pangaea and have since drifted apart to their current positions. He argued that the continents move slowly over time due to tectonic plate movement.
The hypothesis that states that continents slowly moved to their present-day positions on Earth is called continental drift. This theory was proposed by Alfred Wegener in the early 20th century, suggesting that continents were once part of a single supercontinent called Pangaea and have since drifted apart.
Pangaea was a supercontinent that existed about 335 million years ago and eventually broke apart to form the continents we have today due to the movement of tectonic plates. Over millions of years, the continents have drifted apart, leading to the formation of new oceans and mountain ranges as a result of plate tectonics.
Wegener's idea is known as continental drift. He proposed that the Earth's continents were once connected as a single landmass called Pangea and have since drifted apart over time.
plate tectonics
The theory of plate tectonics suggests that the Earth's continents were once connected as a single landmass called Pangea. Over millions of years, the landmass broke apart and drifted to their current positions. This process continues today, with continents still slowly moving.
The hypothesis is called continental drift. It suggests that the Earth's continents were once part of a single supercontinent called Pangaea and have since moved slowly over time to their current positions. This movement is driven by the process of plate tectonics.