0
What else can I help you with?
Why was wegener's hypothesis not widely accepted at the time it was prospered?
Wegener was ignored for so long because no scientists believed him about his theory of continental drift. No scientists believed him because he couldn't explain how the continents had moved until the time of Harry Hess or J. Tuzo Wilson.
What is the opposite of geologist?
That's a hard question to answer, since a Geologist is someone who researches rocks, minerals, and the composition of the earth, what would you consider the opposite of a geologist. Possibly someone who studies the stars such as an astronomer.
What was Frederick J vine hypothesis?
The theory is actually called the Vine-Matthews-Morley hypothesis, It is also known as the Morley-Vine-Matthews hypothesis. Independent of each other, geophysicist Frederick John Vine and Canadian geologist Lawrence W. Morley introduced the first scientific test of the seafloor spreading theory of continental drift and plate tectonics. The hypothesis stated that if the seafloor spreading theory was correct, rocks surrounding mid-oceanic ridges would show symmetric patterns of magnetization reversals captured in cooling volcanic rocks. Morley attempted to get his findings published in February and April of 1963, but was rejected. Vine and his advisor, Drummond Hoyle Matthews, published in 1963. Verification of the theory was found in later geomagnetic surveys.
Why did most scientists originally reject the theory of continental drift?
Most scientists originally reject the theory of continental drift since it did clearly explain continents would move. This is a theory that has been established by Wegener and did not get good support initially.
Who was the geologist that first proposed the theory of continental drift?
The geologist who first proposed the theory of continental drift was Alfred Wegener. He introduced the concept in 1912, suggesting that continents were once connected and have since drifted apart over geological time. Wegener's ideas were initially met with skepticism, but they laid the groundwork for the later development of plate tectonics. His evidence included the fit of continental margins, fossil similarities, and geological formations across continents.
How did other geologist's feel about Alfred wegener's hypothesis?
i am not sure
Why was the continental drift rejected by scientists?
yes becouse wenger is not geologist and he could not explain the how continental drift theory
What proposal did the british geologist arthur Holmes make in 1929?
In 1929, British geologist Arthur Holmes proposed the theory of radioactivity as a significant factor in Earth's internal heat production, which could drive convection currents in the mantle. This idea contributed to the understanding of plate tectonics by suggesting that these currents could influence continental drift. Holmes' work helped shift the geological community's perspective on Earth's dynamics and provided a scientific basis for the movement of tectonic plates.
Why did geologist rejects Alfred idea of continental drift?
He didn't have proof of a force causing the movement
What careers did Alfred Wegener have?
Alfred Wegener was trained as an astronomer and earned a PhD in that field in 1904. He moved into meteorology and climatology, became a record-holding balloonist and pioneered the use of weather balloons. He was also a geologist and proposed the theory of Continental Drift, but died more than 20 years before that theory received general acceptance in the scientific community.
What scientist who first proposed that thermal convection in the mantle causes continental drift?
Arthur Holmes who is a geologist.
Why was wegener's hypothesis not widely accepted at the time it was prospered?
Wegener was ignored for so long because no scientists believed him about his theory of continental drift. No scientists believed him because he couldn't explain how the continents had moved until the time of Harry Hess or J. Tuzo Wilson.
What is the opposite of geologist?
That's a hard question to answer, since a Geologist is someone who researches rocks, minerals, and the composition of the earth, what would you consider the opposite of a geologist. Possibly someone who studies the stars such as an astronomer.
What was Frederick J vine hypothesis?
The theory is actually called the Vine-Matthews-Morley hypothesis, It is also known as the Morley-Vine-Matthews hypothesis. Independent of each other, geophysicist Frederick John Vine and Canadian geologist Lawrence W. Morley introduced the first scientific test of the seafloor spreading theory of continental drift and plate tectonics. The hypothesis stated that if the seafloor spreading theory was correct, rocks surrounding mid-oceanic ridges would show symmetric patterns of magnetization reversals captured in cooling volcanic rocks. Morley attempted to get his findings published in February and April of 1963, but was rejected. Vine and his advisor, Drummond Hoyle Matthews, published in 1963. Verification of the theory was found in later geomagnetic surveys.
Why did most scientists originally reject the theory of continental drift?
Most scientists originally reject the theory of continental drift since it did clearly explain continents would move. This is a theory that has been established by Wegener and did not get good support initially.
Who convinced Charles Darwin to publish his first book?
Charles Lyell, a geologist and friend of Darwin, encouraged him to publish his first book "On the Origin of Species." Lyell believed in the theory of evolution and saw the potential impact of Darwin's work on the scientific community.
Who was the geologist that first proposed the theory of continental drift?
The geologist who first proposed the theory of continental drift was Alfred Wegener. He introduced the concept in 1912, suggesting that continents were once connected and have since drifted apart over geological time. Wegener's ideas were initially met with skepticism, but they laid the groundwork for the later development of plate tectonics. His evidence included the fit of continental margins, fossil similarities, and geological formations across continents.
