It was extremely obvious to those who possess any shred of intelligence.
lol
Alfred Wegener was the proponent of the Continental Drift Theory. The scientific community accepted this theory due to the phenomena of paleomagnetism, sea floor spreading and plate tectonics.
The continental drift theory gained widespread acceptance in the 1960s, primarily due to the development of the theory of plate tectonics. This new understanding provided a comprehensive framework explaining the movement of continents and the mechanisms driving it, such as seafloor spreading and subduction. The integration of geological, paleontological, and geophysical evidence during this decade solidified the scientific community's acceptance of the concept.
Continental drift is the theory that the Earth's continents have moved over time due to the movement of tectonic plates. Plate tectonics is the scientific theory that describes the large-scale movements and interactions of Earth's lithosphere. Continental drift was one of the key pieces of evidence that led to the development of the theory of plate tectonics.
Some scientists initially doubted the theory of continental drift due to a lack of plausible mechanism to explain how continents could move. Additionally, the scientific community was initially resistant to the idea proposed by Alfred Wegener, as it challenged existing geological paradigms. It wasn't until the development of plate tectonics in the 1960s that continental drift gained widespread acceptance in the scientific community.
No. The vast majority of geologists rejected Wegener's hypothesis of continental drift. it was not until more than 25 years after Wegener's death that the scientific community began to accept plate tectonics.
continental drift is caused by plate tectonics
Research on the sea floor, such as magnetic striping and age dating of rocks, provided strong evidence for plate tectonics and continental drift in the second half of the 1900s. These findings helped to change scientific thought, as they demonstrated the movement of lithospheric plates and provided a mechanism for how continents move and interact on Earth's surface. This research revolutionized our understanding of Earth's geology and led to the acceptance of the theory of plate tectonics in the scientific community.
Marie Tharp's new discovery of the Mid-Atlantic Ridge was initially met with skepticism by the scientific community, as her findings challenged existing theories of plate tectonics. However, as more evidence emerged supporting her mapping of the ocean floor, her work was eventually accepted and revolutionized the field of geology. Tharp's discovery provided crucial evidence for the theory of continental drift and plate tectonics.
Continental drift is the theory that continents have moved over time, while plate tectonics is the broader theory that explains how the Earth's lithosphere is divided into plates that move and interact with each other. Continental drift was an early idea that eventually led to the development of plate tectonics as a more comprehensive explanation for the movement of Earth's crust.
Plate tectonics is the scientific theory that explains how the Earth's outer shell is divided into several large, rigid plates that move and interact with each other. Continental drift is the idea that continents have moved and shifted positions over time. The relationship between plate tectonics and continental drift is that plate tectonics provides the mechanism for how continents drift and move around the Earth's surface. The movement of the plates causes the continents to shift and change positions, supporting the concept of continental drift.
Alfred Wegener is a famous scientist involved with the theory of plate tectonics. He proposed the theory of continental drift in the early 20th century, which eventually led to the development of the modern theory of plate tectonics.