Through the mid-20th century, the major objection to Alfred Wegener's continental drift hypothesis was based on: O Apparent polar wander paths are different for each of the major continents in their present locations O Poor fit of the continents for reconstructed Pangaea in the Atlantic Earthquakes and volcanoes are randomly distributed around the Earth O No fossil evidence could support the suggested supercontinental configurations O Lack of a mechanism for moving continents through the oceanic crust Climatic zones had been the same (relative to poles and equator in their present locations) for more than 000 "I'

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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Through the mid-20th century, the major objection to Alfred Wegener's continental drift
hypothesis was based on:
Apparent polar wander paths are different for each of the major continents in their present locations
Poor fit of the continents for reconstructed Pangaea in the Atlantic
Earthquakes and volcanoes are randomly distributed around the Earth
No fossil evidence could support the suggested supercontinental configurations
Lack of a mechanism for moving continents through the oceanic crust
Climatic zones had been the same (relative to poles and equator in their present locations) for more than
300 million years
Transcribed Image Text:Through the mid-20th century, the major objection to Alfred Wegener's continental drift hypothesis was based on: Apparent polar wander paths are different for each of the major continents in their present locations Poor fit of the continents for reconstructed Pangaea in the Atlantic Earthquakes and volcanoes are randomly distributed around the Earth No fossil evidence could support the suggested supercontinental configurations Lack of a mechanism for moving continents through the oceanic crust Climatic zones had been the same (relative to poles and equator in their present locations) for more than 300 million years
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