Alfred Wegener's fully developed theory of continental drift attempted to point out evidences that the continents were once joined into a single continent he called Pangea. Wegener's theory hypothesized that the continents were able to push through the rock of the seafloor to their present positions.
As evidence, he noted, as had others before him, of the geographic correlation in coastline perimeters of South America and Africa. This was the feature that led Wegener to investigate for other evidences. His investigations revealed that mountain ranges in South America and Africa, and strata and composition of coal fields in Europe and North America matched or lined up. Additionally, matching reptilian fossils were found on either side of the ocean, indicating that the continents were once joined together. Although he was unable to find a mechanism for his proposed continental drift theory, he also observed that the more shallow an ocean, the younger its geologic age. It wasn't until the 1950's and 1960's, with the discovery of the Mid-Atlantic Ridge, and other sea floor mapping discoveries that Wegener's hypothesis started to become more accepted. The newer science of plate tectonics owes much to Wegener's scientific groundwork.
Read more: What_evidence_did_Alfred_Wegener_use_to_support_his_theory_of_continental_drift
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one clue that support wegener's theory is the fact that similar rock _______ line up accross today's continents.
Did you mean Plate Tectonics Theory? - Plate Tectonics Theory is the combination of Continental Drift and Ocean/Sea Floor Spreading. BTW. The scientist who started it is Howard Baker continued by Alfred Wegener.
Alfred Wegener proposed the theory of continental drift at the beginning of the 20th century. His idea was that the Earth's continents were once joined together, but gradually moved apart over millions of years. The idea was rejected at first as he was a Meteorologist and not regarded as a proper scientist.
me and your mom
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.
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'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.
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
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.
Alfred Wegener
It is the Continental Drift theory, whereby the landmasses of the world today were together and are slowly drifting apart The theory was proposed by Alfred Wegener.
It is the Continental Drift theory, whereby the landmasses of the world today were together and are slowly drifting apart The theory was proposed by Alfred Wegener.
Alfred Wegener
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