Alfred Wegner's theory of continental drift stated that the continents were all once together but over time have drifted apart.
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The theory of continental drift, proposed by Alfred Wegener in 1912, suggests that continents were once joined together in a single supercontinent called Pangaea and have since drifted apart. This theory laid the foundation for the modern theory of plate tectonics, which explains the movement of Earth's lithosphere. Wegener's theory was initially met with skepticism but has since been supported by overwhelming geological and paleontological evidence.
Continental drift was first proposed by a scientist named Alfred
Wegener. He theorized that the continents were once one large landmass that drifted apart very slowly over a long time.
Alfred Wegener introduced the theory of continental drift, which proposed that Earth's continents were once joined together as a single supercontinent called Pangea and have since moved to their current positions. This theory laid the foundation for the development of the modern theory of plate tectonics.
Pangaea is the name of the supercontinent proposed by Alfred Wegener as part of his theory of continental drift.
Alfred Wegener's support of continental drift was known as the theory of "continental drift," which proposed that the continents were once joined together as a single supercontinent called Pangaea and have since drifted apart.
Alfred Wegener, a German scientist, proposed the theory of continental drift which led to the concept of a supercontinent called Pangaea.
Alfred Wegener developed the theory of Continental Drift in the early 1900s, but it was not widely accepted until much later. He presented his ideas in 1912 and published his theory in a book titled "The Origin of Continents and Oceans" in 1915. Wegener's work laid the foundation for the modern theory of plate tectonics.