theory of continental drift造句
例句與造句
- If current theories of continental drift are correct, this land was Antarctica.
- Later in 1967, after a minor geological history and theories of continental drift.
- Simpson was influentially, and incorrectly, opposed to Alfred Wegener's theory of continental drift.
- Wegener s theory of Continental Drift was later replaced by the theory of tectonic plates.
- Wegener's theory of continental drift was later vindicated, with significant modifications, in the theory of plate tectonics.
- It's difficult to find theory of continental drift in a sentence. 用theory of continental drift造句挺難的
- _All the earth's landmasses, according to the theory of continental drift, were once part of what supercontinent?
- The Morley Vine Matthews hypothesis was the first key scientific test of the seafloor spreading theory of continental drift.
- He was an early advocate of the then discredited Wegener theory of continental drift, which subsequently gained acceptabtability as plate tectonics.
- This confirmation of Alfred Wegener's theory of continental drift strengthened the proposal of a single, ancient land mass, which is called Pangaea.
- A widely known example is Alfred Wegener's theory of continental drift, which eventually served as the basis for the accepted model of plate tectonics.
- Additionally, the theory of continental drift offered a possible explanation as to the formation of mountains; Plate Tectonics built on the theory of continental drift.
- Additionally, the theory of continental drift offered a possible explanation as to the formation of mountains; Plate Tectonics built on the theory of continental drift.
- Moving on to the 20th century, Alfred Wegener introduced the Theory of Continental Drift in 1912, though it was not widely accepted until the 1960s.
- There is often resistance to radical views, witness the 70 years that it took for Wegener's theory of continental drift ( plate tectonics ) to gain acceptance.
- Plate tectonics also provided a mechanism for Alfred Wegener's theory of continental drift, in which the continents move across the surface of the Earth over geologic time.
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