Plate tectonics.
The theory proposing that continents slowly moved into their current locations is called "plate tectonics." This theory suggests that Earth's outer shell is divided into several plates that glide over the mantle, causing the continents to shift over time.
Plate tectonics.
its Continental drift
The hypothesis that the continents have mved slowly to their current locations.
The theory that continents have moved slowly over time to their current locations is called continental drift. This theory was proposed by Alfred Wegener in the early 20th century and later developed into the theory of plate tectonics, which explains the movement of Earth's lithosphere through the interaction of tectonic plates.
plate tectonics
The hypothesis that continents have slowly moved to their current locations is called continental drift. This theory was proposed by Alfred Wegener in the early 20th century and later developed into the theory of plate tectonics, which explains how the Earth's lithosphere is divided into large plates that move and interact with each other. This movement of continents is driven by processes like seafloor spreading and subduction at plate boundaries.
The idea that continents move slowly across Earth's surface is called plate tectonics. This theory explains how the Earth's lithosphere is divided into plates that move and interact with each other, leading to processes such as earthquakes, volcanic activity, and the formation of mountain ranges.
The idea that continents move slowly across the earth's surface is called the continental drift.
Alfred Wegner proposed the theory of 'continental drift'. He suggested that all the continents had originally been joined together as one landmass, after which they had seperated and slowly drifted along the ocean floors to their current locations. Wegener investigated the apparent match of the coastlines of South America and Africa. The evidence was supported by the rocks in the two continents. The mountains running accross south Africa apeared to match those in Argentine, and there were many types of rock found in the two locatinos.
The process in which continents slowly move is called plate tectonics. This movement is caused by the interactions of large sections of the Earth's lithosphere known as tectonic plates. Over time, these plates drift and collide, leading to the formation of mountains, volcanoes, and earthquakes.
Through the passage of time, the continents have gradually moved across the earth's surface into their present positions. This is called the continental drift.