The theory of Pangea.
The theory is called "continental drift," and it proposes that the Earth's continents were once connected as one supercontinent called Pangaea.
Alfred Wegener proposed the hypothesis of continental drift in 1912, suggesting that the continents were once joined in a supercontinent he called Pangaea. His idea laid the groundwork for the development of the theory of plate tectonics.
The theory is called continental drift, proposed by Alfred Wegener. It suggests that continents were once part of a supercontinent called Pangaea and have since drifted to their current positions. This theory is supported by evidence such as matching coastlines and similar geological features on different continents.
The hypothesis that states the continents were once joined together in a single supercontinent is called "Pangaea." This theory suggests that due to the movement of tectonic plates, Pangaea eventually broke apart over millions of years to form the continents as we know them today.
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.
Pangaea is the supercontinent that once formed from all the continents.
The theory is called "Pangaea", which suggests that all current continents were once part of a single supercontinent that broke apart over millions of years.
The continents used to all form the supercontinent of Pangea. The theory of continental drift explains how they separated and formed today.
The continents used to all form the supercontinent of Pangea. The theory of continental drift explains how they separated and formed today.
The theory that suggests the Earth once had a supercontinent is called Pangaea. It proposes that all current continents were once connected as one large landmass before breaking apart and moving to their current positions. The evidence for this theory includes the matching shapes of continents, similar geologic formations across different continents, and the distribution of fossils.
The theory is called "continental drift," and it proposes that the Earth's continents were once connected as one supercontinent called Pangaea.
The theory that suggests the Earth was once a single supercontinent that gradually broke up into the continents we know today is called "continental drift" proposed by Alfred Wegener in the early 20th century. This theory later evolved into the theory of plate tectonics.
Alfred Wegener proposed the hypothesis of continental drift in 1912, suggesting that the continents were once joined in a supercontinent he called Pangaea. His idea laid the groundwork for the development of the theory of plate tectonics.
The theory that suggests that the Earth was once a single supercontinent that gradually broke up into the continents we know today is called the theory of plate tectonics. This theory explains how the Earth's lithosphere is divided into large plates that move and interact with each other, leading to the shifting of continents over millions of years.
The theory is called continental drift, proposed by Alfred Wegener. It suggests that continents were once part of a supercontinent called Pangaea and have since drifted to their current positions. This theory is supported by evidence such as matching coastlines and similar geological features on different continents.
Alfred Wegener proposed the theory of continental drift, suggesting that all the continents were once connected in a single supercontinent he named Pangaea.
The theory that all seven continents were once part of a supercontinent called Pangaea is known as plate tectonics. This theory explains how the continents have moved over geological time due to the shifting of tectonic plates.