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∙ 12y agocontinental drift theory
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∙ 12y agoThe theory that all continents were once joined together in a supercontinent called Pangaea and have since drifted apart is known as the theory of continental drift. This theory was proposed by Alfred Wegener in the early 20th century and later developed into the theory of plate tectonics.
This idea is called the theory of continental drift, which suggests that all continents were once part of a single landmass called Pangaea that later split and drifted apart over millions of years.
The hypothesis that Earth's continents were once joined in a single landmass and then gradually moved apart is known as the theory of continental drift, proposed by Alfred Wegener in 1912. This theory laid the foundation for the development of the theory of plate tectonics.
The hypothesis that states the continents once formed a single landmass, broke up, and drifted to their present locations is known as the theory of plate tectonics. This theory explains the movement of Earth's lithosphere plates and the distribution of continents and oceans on the planet's surface. It is supported by evidence from fossil records, rock formations, and the matching coastlines of continents like South America and Africa.
a continental theory
pangea
The distribution of mountains on different continents provided evidence for Wegener's theory of continental drift. He observed that mountain ranges on separate continents, such as the Appalachians in North America and the Caledonian mountains in Scotland, lined up when the continents were reconstructed into a single landmass (Pangaea). This alignment suggested that the continents were once connected and had drifted apart over time.
The theory is called the theory of continental drift, proposed by Alfred Wegener in the early 20th century. It suggests that the continents were once joined together as a single large landmass called Pangaea and have since drifted apart to their current positions.
The theory of continental drift did originate in the 1930s. Continental drift asserts that the continents were once a single landmass called Pangaea that drifted apart over time.
One theory is plate tectonics, which suggests that Earth's continents drifted apart from a single landmass called Pangaea. Another theory is continental drift, proposed by Alfred Wegener, which suggests that continents move due to the movement of the Earth's tectonic plates. Both theories provide insights into the geologic history and formation of Earth's continents.
The theory that explains the existence of a supercontinent called Pangaea is known as continental drift. According to this theory, proposed by Alfred Wegener in the early 20th century, the continents were once joined together in a single landmass and have since drifted apart over millions of years. Geological and fossil evidence, such as matching coastlines and similar plant and animal species on separate continents, support this theory.
Wegener proposed the theory of continental drift, suggesting that the continents were once connected in a single landmass called Pangaea. He proposed that the continents drifted apart over time due to the movement of the Earth's crustal plates.