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 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 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.
Sea floor spreading Subduction Plate tectonics Continental sift theory
Alfred Wegener proposed the theory of continental drift in the early 20th century, which suggested that continents were once connected in a supercontinent called Pangaea. This theory laid the foundation for our understanding of plate tectonics and the movement of the Earth's continents.
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 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.
Sea floor spreading Subduction Plate tectonics Continental sift theory
Sea floor spreading Subduction Plate tectonics Continental sift theory
Sea floor spreading Subduction Plate tectonics Continental sift theory
Sea floor spreading Subduction Plate tectonics Continental sift theory
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 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.
Sea floor spreading Subduction Plate tectonics Continental sift theory
that the continents were once all connected as one supercontinent, called Pangaea, which broke apart and drifted to their current positions over millions of years. This theory eventually led to the development of the theory of plate tectonics to explain the movement of Earth's large landmasses.
Alfred Wegener proposed the theory of continental drift in the early 20th century, which suggested that continents were once connected in a supercontinent called Pangaea. This theory laid the foundation for our understanding of plate tectonics and the movement of the Earth's continents.
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.