Continental drift is the theory that the planet's continents have shifted over geologic time relative to each other, and they appear to have drifted across the ocean bed. Abraham Ortelius first put forward the notion that continents might have drifted in 1596.
It was then further developed in the initial part of the 20th century, mostly by Alfred Wegener. Wegener said that the continents move around us, and they were joined together as a single supercontinent. During the time Wegner was alive, scientists did not believe this. Wegener collected irrefutable evidence that the continental drift theory was real.
Individual rocks of the same type and age were discovered on both sides of the Atlantic. The eastern US and Canada applications are just like mountain ranges in Greenland, Ireland, Great Britain, and Norway. There were also extinct plants and animals found in the rocks.
The correct answer is Continental Drift.
Continental drift is the geology theory that states that continents are slowly moving over the earth's surface. This was first described by Alfred Wegener, who is a geophysicist and meteorologist, in 1912. In the 2oth century, he published a paper where he stated that the continental mass was drifting along the earth's surface. He believed that all the continents were once part of a single large mass known as “Pangaea.”
Pangaea refers to a supercontinent that included all the landmass of the earth before the Triassic period, and that broke up into Laurasia and Gondwana.
Continental drift is explained by the plate tonic theory, which refers to the large scale movement of the tectonic plates.
The correct answer to this question is continental drift. Alfred Wegener is the father of this theory, and he was a scientist. This is one of the earliest ideas about how geologists believed continents moved over time.
The theory of continental drift was published in the 20th century, and it was published in a paper. In this paper, Wegener explained that the continental landmasses were drifting along with the Earth. Sometimes, this drift would be going through oceans and into one another, which is called continental drift. The idea of continental drift has now been replaced with the theory of plate tectonics.