this is easy! I LEARNED IT IN SCIENCE! WERGNER DICOVERED IT. WEGNERS EARLIER THEORY OF CONTINENTAL DRIFT WAS REEXAMMINED AND A NEW THEORY WAS BORN ............................ THE THEORY OF PLATE TECTONICS
Other scientists questioned the theory of plate tectonics initially because there was no known mechanism to explain how continents could move. Additionally, some were skeptical of the idea because it challenged the prevailing belief at the time that the Earth's surface was static and immovable.
Harry Hammond Hess is famous for his contributions to the theory of plate tectonics. He proposed the idea of seafloor spreading, which suggested that new oceanic crust is formed at mid-ocean ridges and then gradually moves away from the ridge. This theory provided key evidence in support of the broader concept of plate tectonics.
No, magma refers to molten rock beneath the Earth's surface. The idea that the Earth's crust is broken into plates that move on top of the mantle is known as plate tectonics. Plate tectonics explains the motion of Earth's lithosphere and how different landforms are shaped.
Alfred Wegener is considered the father of the theory of continental drift. In the early 20th century, he proposed the idea that the continents were once connected and had drifted apart over time, forming the basis for the modern theory of plate tectonics.
this is easy! I LEARNED IT IN SCIENCE! WERGNER DICOVERED IT. WEGNERS EARLIER THEORY OF CONTINENTAL DRIFT WAS REEXAMMINED AND A NEW THEORY WAS BORN ............................ THE THEORY OF PLATE TECTONICS
The idea of seafloor spreading, proposed by Harry Hess in the early 1960s, helped promote the theory of plate tectonics. This idea explained how new oceanic crust is formed at mid-ocean ridges and then spreads out, pushing older crust aside. This process provided a mechanism for how continents move and gave strong evidence for the movement of tectonic plates.
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One idea used to promote the theory of plate tectonics was the discovery of matching coastlines and geological features on opposite sides of the Atlantic Ocean, known as "continental drift." This supported the idea that continents were once connected and had drifted apart over time due to the movement of tectonic plates.
The theory of plate tectonics supports the idea of continental drift. It suggests that the Earth's lithosphere is divided into large plates that move over the asthenosphere, which explains the movement of continents over time.
The existance of land bridges between continents
The theory of plate tectonics was developed by a combination of scientists, including Alfred Wegener, who proposed the idea of continental drift, and Harry Hess, who proposed the idea of seafloor spreading. Their work was later expanded upon by researchers like Fred Vine, Drummond Matthews, and J. Tuzo Wilson, leading to the development of the modern theory of plate tectonics.
plate tectonics
The theory of plate tectonics builds on the idea of continental drift by explaining how the Earth's lithosphere is broken into plates that move over the asthenosphere. Plate tectonics also accounts for the movement of not just continents, but also oceanic crust, creating a more comprehensive understanding of Earth's geological processes. Additionally, plate tectonics provides a mechanism for explaining the formation of mountain ranges, earthquakes, and volcanic activity at plate boundaries.
The theory of plate tectonics explains that the Earth's lithosphere is divided into plates that move due to convection currents in the mantle. Wegener's idea of continental drift proposed that continents were once connected and had drifted apart, but he did not have a mechanism to explain how this occurred. Plate tectonics provides the scientific framework to explain how and why continents move.
The idea that Earth's lithosphere is divided into large moving sections is called the theory of plate tectonics. This theory explains how the Earth's lithosphere is broken into several plates that shift and interact with each other, resulting in various geological phenomena like earthquakes, volcanoes, and mountain formation.
The plate tectonic theory was primarily developed by Alfred Wegener in the early 20th century. He proposed the idea of continental drift, which later laid the foundation for our modern understanding of plate tectonics.