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Continental drift is a highly supported scientific theory, originating in the early 20th century, that Earth's continents move or drift relative to each other over geologic time. [1] The theory of continental drift has since been validated and incorporated into the science of plate tectonics , which studies the movement of the continents as ...
The evolution of tectonophysics is closely linked to the history of the continental drift and plate tectonics hypotheses. The continental drift/ Airy-Heiskanen isostasy hypothesis had many flaws and scarce data. The fixist/ Pratt-Hayford isostasy, the contracting Earth and the expanding Earth concepts had many flaws as well.
Polflucht (from German, flight from the poles) is a geophysical concept invoked in 1922 by Alfred Wegener to explain his ideas of continental drift.. The pole-flight force is that component of the centrifugal force during the rotation of the Earth that acts tangentially to the Earth's surface.
The root of this was Alfred Wegener's 1912 publication of his theory of continental drift, which was a controversy in the field through the 1950s. [2] At that point scientists introduced new evidence in a new way, replacing the idea of continental drift with instead a theory of plate tectonics. [ 2 ]
Preparation for history When NASA began strapping living chimps and launching them into space from Cape Canaveral down the state, my brother, Robert, decided to get in on the action.
The expanding Earth or growing Earth was a hypothesis attempting to explain the position and relative movement of continents by increase in the volume of Earth. With the recognition of plate tectonics in 20th century, the idea has been abandoned.
History doesn’t begin when you want it to or when it’s convenient. Demonstrators that ignore history deserve to be ignored. Harry Bulkeley is a retired Knox County judge and a local historian.
[25] [26] [27] During this time, Earth's crust cooled enough that rocks and continental plates began to form. Some scientists think because Earth was hotter in the past, [ 28 ] [ 29 ] plate tectonic activity was more vigorous than it is today, resulting in a much greater rate of recycling of crustal material.