What does not support the theory of continental drift?
Although the evidence for continental drift was extremely strong, scientists rejected the idea because no mechanism for how solid continents could move around on the solid earth was developed.
Which of the following is not evidence supporting the continental drift hypothesis?
The ancient climate did not have any effect on the continental drift hypothesis. Continental Drift is known to be a theory in which the Continents of the Earth have moved over a geologic time that is relative to each other and that is the reason why they appear to have “Drifted” across the ocean bed.
What evidence of Earth’s climate in the past supports the theory of continental drift?
Lesson Summary. Alfred Wegener gathered evidence that the continents had moved around on Earth’s surface. The evidence for continental drift included the fit of the continents; the distribution of ancient fossils, rocks, and mountain ranges; and the locations of ancient climate zones.
Do continents touch the ocean floor?
So continents float on magma. The magma comes from the mantel. Oceanic plates do the same; however, they can go underneath continental plates. If the continents went underneath the oceanic plates, overtime, coastal cities would be submerged underwater, and eventually, under the ocean floor.
Can you swim under a continent?
There’s only one place in the world where you can swim in the tectonic plates between 2 continents. The Silfra fissure in Iceland is the crack between North America and Europe. It is the only place in the world where you can swim between two tectonic plates.
Can you swim under countries?
No, the land doesn’t go all the way down under an island. You can swim right underneath islands.
Do any islands float?
Surely chunks of solid earth on which we stand cannot drift easily about the surface of a water body. But floating islands do indeed exist on six of the seven continents and sometimes in the oceans between them. This may be clearly observed from all sides: the islands lie half above and half below the water’s surface.