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.
The theory of plate tectonics was developed through the contributions of several scientists, including Alfred Wegener, who proposed the theory of continental drift in the early 20th century. Later research by Harry Hess and Robert Dietz provided evidence for seafloor spreading, leading to the development of the modern plate tectonics theory in the 1960s.
Alfred wegener was also accomplished in meteorology, however this eventually led to his death, for Alfred froze to death bringing supplies to a team of metorologists working hard somewhere in the north.
The discovery of seafloor spreading and the mapping of plate tectonics boundaries in the mid-20th century caused scientists to re-evaluate and eventually accept Alfred Wegener's hypothesis of continental drift, leading to the development of the theory of plate tectonics. These discoveries provided a mechanism for how continents could move and interact with each other.
Alfred Wegener, a German meteorologist, proposed the theory of continental drift in the early 20th century. He suggested that the continents were once part of a single supercontinent called Pangaea that broke apart and drifted to their current positions. Although his ideas were initially met with skepticism, they formed the foundation for the modern theory of plate tectonics.
Other evidence to support Alfred Wegener's theory of continental drift includes matching geological formations and rock types on different continents, similar fossil collections on continents that are now separated by oceans, and the fit of the continents' coastlines like pieces of a jigsaw puzzle. Additionally, the discovery of mid-ocean ridges and the study of paleomagnetism has further bolstered the theory.
It was Alfred Wegener but other scientists did not believe him but he found evidence
Other scientists rejected Alfred Wegener's hypothesis of a supercontinent that broke apart, known as "continental drift," because Wegener did not provide a plausible mechanism for how the continents could move. Additionally, his hypothesis was seen as radical and went against the prevailing scientific beliefs of the time. It was not until the discovery of plate tectonics in the 1960s that Wegener's ideas gained more widespread acceptance.
The theory of plate tectonics was developed through the contributions of several scientists, including Alfred Wegener, who proposed the theory of continental drift in the early 20th century. Later research by Harry Hess and Robert Dietz provided evidence for seafloor spreading, leading to the development of the modern plate tectonics theory in the 1960s.
i am not sure
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.
Scientists now know about plate tectonics, which explains how the Earth's lithosphere is divided into plates that move and interact with each other. This knowledge would have answered the scientists who rejected Wegener's theory of continental drift because it provides a mechanism for how continents can drift and shift positions over time. Plate tectonics also explains various geological phenomena, such as earthquakes, volcanic activity, and the formation of mountain ranges.
Alfred wegener was also accomplished in meteorology, however this eventually led to his death, for Alfred froze to death bringing supplies to a team of metorologists working hard somewhere in the north.
why did other scientist not accpet Alfred Wegeners theory
Other scientists did not believe Alfred Wegener's hypothesis of continental drift in the early 20th century because he did not provide a plausible mechanism for how continents could move through the oceanic crust. Additionally, Wegener's evidence supporting his idea was largely based on geological and fossil similarities between continents, which were not considered strong enough to support such a revolutionary idea at the time. It wasn't until the mid-20th century, with the development of the theory of plate tectonics, that Wegener's hypothesis gained widespread acceptance.
Alfred Wegener was the first to publish his theory although other people thought it
Alfred Wegener proposed his theory of continental drift through publications, such as his book "The Origin of Continents and Oceans" in 1915. He presented his ideas at scientific conferences and engaged in discussions with other geologists to promote his theory, despite facing initial skepticism from the scientific community. Wegener's theory gained more widespread acceptance after his death.
Alfred Wegener postulated the theory of continental drift, which later contributed to the development of the theory of plate tectonics.