The idea that first described the movement of continents is called continental drift. Proposed by Alfred Wegener in the early 20th century, it suggested that Earth's continents were once connected in a supercontinent called Pangaea and have since drifted apart.
Wagner proposed the theory of continental drift, suggesting that the continents were once joined together in a single supercontinent called Pangaea. He observed that identical rock sequences and geological structures appeared on different continents, supporting the idea of continental movement over time.
Wegener's theory of continental drift proposed that the continents were once joined together in a single supercontinent called Pangaea. Over time, the continents drifted apart to their current positions. This idea eventually led to the development of the theory of plate tectonics, which explains the movement of Earth's lithosphere on the underlying asthenosphere.
Fossil symbols and mountain belts were helpful in deciding the theory of plate tectonics because they provided evidence of past connections between continents and the movement of tectonic plates. Fossil similarities between continents suggested that they were once connected, and asymmetric mountain belts indicated the direction of plate movement. These pieces of evidence supported the idea that continents move and drift on the Earth's surface.
plate tectonics, which explains the movement of Earth's outer shell. Fossil remains on separate continents that were once part of the same landmass suggest that continents were once connected and have since drifted apart. The shape of continents also fits together like a puzzle, supporting the idea of continental drift and plate tectonics.
The distribution of mountain ranges across different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe, supports Wegener's idea of continental drift. These mountain ranges were once connected when the continents were part of a supercontinent, and their alignment provides evidence for the movement of land masses over time. Additionally, the presence of similar geological features and rock formations on separate continents suggests a shared history of mountain building.
shapes of the continents fit together. fossils of same dinosaur are found in different continents. same plant fossils in different continents.
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Continental drift is the idea that Wegener created, that all the continents were once a single landmass which he called Pangaea, and they have since drifted apart.
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The idea of that the continents were shifting was first observed by Abraham Ortelius in 1596 and further examined in the early 1900's and in the 1960's when the theory of plate tectonics were developed, scientists were able to understand it more clearly.
Wagner proposed the theory of continental drift, suggesting that the continents were once joined together in a single supercontinent called Pangaea. He observed that identical rock sequences and geological structures appeared on different continents, supporting the idea of continental movement over time.
The idea that continents move slowly across the earth's surface is called the continental drift.
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Wegener's theory of continental drift proposed that the continents were once joined together in a single supercontinent called Pangaea. Over time, the continents drifted apart to their current positions. This idea eventually led to the development of the theory of plate tectonics, which explains the movement of Earth's lithosphere on the underlying asthenosphere.
Fossil symbols and mountain belts were helpful in deciding the theory of plate tectonics because they provided evidence of past connections between continents and the movement of tectonic plates. Fossil similarities between continents suggested that they were once connected, and asymmetric mountain belts indicated the direction of plate movement. These pieces of evidence supported the idea that continents move and drift on the Earth's surface.
It is called "reference frame"; and yes, that's the basic idea - related to what will you measure movement.