The continents are constantly shifting. There was never a time or location that it has happened more or less. Scientists estimate that they drift 2 cm (0.8 inch) per year on average.
Drift is a word that generally means to move slowly away from the origin... It has many uses, such as continental drift wherein the continental plates move relative to one another through various geological processes such as convection, subduction, and diversion.
Cynognathus is a good candidate for providing evidence for the continental drift theory because its fossil has been found in both South America and Africa, which were once connected in the supercontinent Gondwana. This distribution pattern supports the idea of continental drift, as it suggests that these continents were once joined together and later drifted apart.
Wegener's theory of continental drift assumed the existence of one original supercontinent called Pangaea.
Most scientists originally reject the theory of continental drift since it did clearly explain continents would move. This is a theory that has been established by Wegener and did not get good support initially.
Wegener's hypothesis of continental drift was not widely accepted during his time because he could not provide a convincing mechanism for how continents could move across the Earth's surface. His ideas contradicted the prevailing geological theories, and many scientists were skeptical of his lack of evidence for a force driving the drift. Today, scientists understand that continental drift is driven by plate tectonics, where the movement of tectonic plates is caused by convection currents in the Earth's mantle. This mechanism provides a clear explanation for the movement of continents over geological time.
Continental drift is one of the many affects of the earth and it can harm the earth because it could crash into other countries
once but in the distant future the continents will thus drift together hence creating another supercontinent.
I think about 2 years
Drift is a word that generally means to move slowly away from the origin... It has many uses, such as continental drift wherein the continental plates move relative to one another through various geological processes such as convection, subduction, and diversion.
Continental Drift is an obsolete name for the theory of Plate Tectonics and yes, it is true. It has been proved in many ways, by comparing the composition of oceanic crust and its ages with that of the continental crust, by plotting the reversals of magnetism in the oceanic crust and many other ways.
Cynognathus is a good candidate for providing evidence for the continental drift theory because its fossil has been found in both South America and Africa, which were once connected in the supercontinent Gondwana. This distribution pattern supports the idea of continental drift, as it suggests that these continents were once joined together and later drifted apart.
One, it was named Pangaea
Wegener's theory of continental drift assumed the existence of one original supercontinent called Pangaea.
continental drift can change there earth in many different ways like land forms and climates for example the Hawaiian islands were originally and under water volcano but over the years it has traveled under the crust making new land.
Most scientists originally reject the theory of continental drift since it did clearly explain continents would move. This is a theory that has been established by Wegener and did not get good support initially.
Wegener's hypothesis of continental drift was not widely accepted during his time because he could not provide a convincing mechanism for how continents could move across the Earth's surface. His ideas contradicted the prevailing geological theories, and many scientists were skeptical of his lack of evidence for a force driving the drift. Today, scientists understand that continental drift is driven by plate tectonics, where the movement of tectonic plates is caused by convection currents in the Earth's mantle. This mechanism provides a clear explanation for the movement of continents over geological time.
Many scientists initially rejected the hypothesis of continental drift because there was a lack of a plausible mechanism to explain how continents could move. Additionally, the idea went against established scientific beliefs at the time and was considered too radical. It was not until the development of the theory of plate tectonics that continental drift was more widely accepted in the scientific community.