Frederick J. Vine supported Alfred Wegener's theory of continental drift by providing a mechanism for it through the concept of seafloor spreading in the 1960s. Vine, along with Dr. Drummond Matthews, discovered that the patterns of magnetic striping on the ocean floor corresponded to periods of magnetic reversals, which suggested that new oceanic crust was continuously formed and pushed outward from mid-ocean ridges. This evidence lent significant support to Wegener's ideas by demonstrating how continents could drift apart over geological time. Thus, Vine's work helped validate and expand upon Wegener's foundational concepts in plate tectonics.
Alfred Wegener, a German meteorologist, was the scientist who first proposed the theory of continental drift in 1912. He suggested that the continents were once connected in a single landmass called Pangaea that later broke apart and moved to their current positions.
Fossils found on different continents that were once part of a single landmass supported Alfred Wegener's theory of continental drift. These fossils, along with matching rock formations, ancient climate evidence, and geological features, helped to provide evidence to support the idea of a supercontinent that broke apart over time.
Seafloor spreading provided a mechanism for the movement of continents, supporting Alfred Wegener's hypothesis of continental drift. As magma rises at mid-ocean ridges and solidifies, it creates new oceanic crust, pushing older crust away from the ridge and causing continents to drift apart. This process offered a tangible way to understand how continents could move over geological time, reinforcing the idea that they were once part of a supercontinent, Pangaea. Thus, seafloor spreading helped validate and expand upon Wegener's original theories.
Yes, Wegener did use evidence of glacial striations to support his theory of continental drift. He observed that matching glacial striations on continents separated by oceans suggested they were once connected and had moved apart. This was one of the pieces of evidence Wegener used to develop his theory of plate tectonics.
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Frederick J. Vine helped Alfred Wegener by providing important evidence to support the theory of continental drift. Vine's research on magnetic anomalies in the ocean floor provided crucial support for Wegener's idea of plate tectonics. This collaboration helped to further validate Wegener's revolutionary theory in the field of geology.
Frederick J. Vine contributed to Alfred Wegener's theory of continental drift by providing crucial evidence through the concept of seafloor spreading. In the early 1960s, Vine, along with Dr. Drummond Matthews, discovered that magnetic patterns on the ocean floor aligned with the theory of plate tectonics, supporting Wegener's ideas about continental movement. Their research demonstrated how new oceanic crust was formed at mid-ocean ridges and pushed continents apart, thus reinforcing Wegener's hypotheses with empirical data. This work was pivotal in the eventual acceptance of plate tectonics as a fundamental geological theory.
Alfred Wegener, a German meteorologist, was the scientist who first proposed the theory of continental drift in 1912. He suggested that the continents were once connected in a single landmass called Pangaea that later broke apart and moved to their current positions.
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Fossils found on different continents that were once part of a single landmass supported Alfred Wegener's theory of continental drift. These fossils, along with matching rock formations, ancient climate evidence, and geological features, helped to provide evidence to support the idea of a supercontinent that broke apart over time.
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Look up Alfred Wengener, he was the first to descover this!!!!!!!!!!!!!!To prove the idea of Alfred L. Wegener HERE:Wegener used to fit of the continents, the distribution of fossils, the similar sequence of rocks at numerous locations, ancient climates, and the movement of the polar regions.I'm sure with my answer! obejerojamjam@yahoo.com :))
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Alfred Wegener proposed the theory of continental drift in the early 20th century based on evidence of the movement of continents. At that time, the concept of divergent plate boundaries, where plates move apart, was not well understood. Only in the 1960s, with advancements in technology and the discovery of seafloor spreading, did the theory of plate tectonics, which includes divergent boundaries, become widely accepted. Wegener's work laid the foundation for our current understanding of the Earth's dynamic crustal movements.