The theory is called plate tectonics, which posits that Earth's outer shell is divided into several large, rigid plates that move and interact with one another. This movement can result in phenomena such as earthquakes, volcanic activity, and the drifting of continents over millions of years.
Continental drift is caused by the movement of tectonic plates, which float on the semi-fluid asthenosphere beneath them. Heat generated by radioactive decay in the Earth's interior causes convection currents in the mantle, which in turn drives the movement of these plates. This movement can result in the continents drifting apart or colliding with each other over millions of years.
A continental shift refers to the movement of continents on the Earth's surface due to plate tectonics. This movement is very slow, occurring over millions of years, and can result in changes to the configuration of the continents and the ocean basins. Examples of continental shifts include the breakup of Pangaea into the continents we see today.
Some Islands are parts of continents (high points in the continental shelf) eg The British Isles. Some Islands are parts of continents that have become detached during continental drift (eg Seychelles or Madagascar) Some Islands are unrelated to continents and result from oceanic plate processes (eg Hawaii). Some Islands are a result of the interaction between continental and oceanic plates (eg some of the Caribbean Islands, Japan and Cyprus).
Scientists now believe that the movement of tectonic plates caused by mantle convection could be a possible cause of continental drift. This phenomenon describes how the Earth's crust is broken into large plates that float on the semi-fluid asthenosphere beneath them, causing them to slowly move and shift over time. This movement can result in the continents drifting apart or coming together.
Convection currents in the Earth's mantle drive the movement of tectonic plates, which can result in continent drifting. As the currents move material within the mantle, they push and pull on the overlying tectonic plates, causing them to shift and move. This movement can lead to the breakup of supercontinents, the formation of new ocean basins, and the drifting of continents over millions of years.
Wegner believed that the force causing continental drift was the movement of the continents through the Earth's crust, driven by the gravitational forces associated with the rotation of the Earth. This movement was theorized to be a result of the continents floating on the denser, underlying mantle layer.
The breakup of Pangaea involved the gradual drifting apart of the tectonic plates carrying the continents. This movement created new ocean basins and shifted landmasses to their current positions over millions of years. Today's configuration of continents is a result of this ongoing process of plate tectonics.
Continental drift is the idea that Wegener created, that all the continents were once a single landmass which he called Pangaea, and they have since drifted apart.
what happened as a result of columbus coming to american continents
yes, mountains are the result of drifting of earths crust towards each other over millions of result... The Himalaya, Andes etc. mountains were made through this drifting process....
They are the result of continental collision, with the mean rate of drift of continents around the globe being only 20 - 30 mm per year.