Alfred Wegener was unable to prove his theory about Pangaea because he lacked a mechanism to explain how continents could move across the Earth's surface. Additionally, Wegener's theory was met with skepticism from the scientific community at the time due to the lack of supporting evidence and alternative explanations being more widely accepted. It wasn't until the development of the theory of plate tectonics in the 1960s that Wegener's ideas were finally validated.
Alfred Wegener proposed the theory of Pangaea based on the fit of the continents, similarities in rock formations, and fossil evidence across continents. He also noted similarities in geological structures and climate data that suggested the continents were once connected before drifting apart. However, Wegener's theory was not widely accepted until much later when additional evidence and advancements in plate tectonics supported his ideas.
Alfred Wegener proposed the theory of continental drift, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart. His theory was rejected because he could not provide a plausible mechanism for how the continents could move across the ocean floor. It was not until the discovery of plate tectonics that Wegener's ideas were accepted and incorporated into the scientific understanding of Earth's geology.
Alfred Wegener, a German scientist, was one of the first to propose the theory of continental drift in the early 20th century. He suggested that all continents were once part of a single supercontinent called Pangaea and had drifted to their current positions over time.
Alfred Wegener's theory of continental drift was not accepted in his lifetime because he lacked a mechanism to explain how continents could move. Additionally, his evidence was not widely considered sufficient or conclusive at the time, and he faced significant opposition from the scientific community, particularly geologists entrenched in the established theory of stationary continents.
The ascertations that Alfred Wegener posed with his Continental Drift theory pre-dated the technology necessary to prove his vision. In 1968 the new science of plate tectonics supported Wegener's theory.
The ascertations that Alfred Wegener posed with his Continental Drift theory pre-dated the technology necessary to prove his vision. In 1968 the new science of plate tectonics supported Wegener's theory.
Alfred Wegener was unable to prove his theory about Pangaea because he lacked a mechanism to explain how continents could move across the Earth's surface. Additionally, Wegener's theory was met with skepticism from the scientific community at the time due to the lack of supporting evidence and alternative explanations being more widely accepted. It wasn't until the development of the theory of plate tectonics in the 1960s that Wegener's ideas were finally validated.
Alfred Wegener's theories of continental drift were dismissed initially because he lacked a valid mechanism to explain how continents could move. Additionally, Wegener faced resistance from the scientific community because his ideas contradicted the prevailing belief in stationary continents. It was not until the development of plate tectonics in the 1960s that Wegener's ideas gained widespread acceptance.
A young german scientist named Alfred Wegener came up with it.Alfred Wegener of Germany.Wegener pronounced Veg-ner.He died in Iceland trying to prove his theory and is now frozen in a glacier
J. Tuzo Wilson did not directly prove Alfred Wegener's theory of continental drift. Instead, Wilson proposed the theory of plate tectonics, which provided a comprehensive explanation for the movement of Earth's lithosphere. This theory incorporated and expanded upon Wegener's ideas, leading to a better understanding of the mechanisms driving the movement of Earth's crustal plates.
Alfred Wegener.
Alfred Wegener proposed the theory of Pangaea based on the fit of the continents, similarities in rock formations, and fossil evidence across continents. He also noted similarities in geological structures and climate data that suggested the continents were once connected before drifting apart. However, Wegener's theory was not widely accepted until much later when additional evidence and advancements in plate tectonics supported his ideas.
Alfred Wegener's theory was rejected because he could not prove how the continents actually moved. He showed evidence of fossils from Africa and South America, but still coul not prove the convection surrents going on underground. Other geologists did not believe in his theory just because he was a meteorologist, not a geologist like themselves.
♥ pendejo u look it up joto ♥
Alfred Wegener proposed the theory of continental drift, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart. His theory was rejected because he could not provide a plausible mechanism for how the continents could move across the ocean floor. It was not until the discovery of plate tectonics that Wegener's ideas were accepted and incorporated into the scientific understanding of Earth's geology.
Alfred Wegener's theory was rejected because he could not prove how the continents actually moved. He showed evidence of fossils from Africa and South America, but still coul not prove the convection surrents going on underground. Other geologists did not believe in his theory just because he was a meteorologist, not a geologist like themselves.