Alexander Du Toit
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Alexander Du Toit was a South African geologist who significantly contributed to the theory of continental drift. He modified Alfred Wegener's hypothesis by proposing that Earth's ancient supercontinent, Pangaea, had actually been composed of two large landmasses: Laurasia in the north and Gondwana in the south. Du Toit meticulously documented evidence, including matching glacial deposits and similar fossil flora and fauna across the southern continents, to support his ideas. His 1937 book, Our Wandering Continents, presented a comprehensive argument for these concepts, though widespread acceptance by Northern Hemisphere scientists was delayed until the development of plate tectonics theory in the 1960s.1234
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- continental drift
In 1937 Alexander L. Du Toit, a South African geologist, modified Wegener’s hypothesis by suggesting two primordial continents: Laurasia in the north and Gondwana in the south.
Read MoreIn 1937 Alexander L. Du Toit, a South African geologist, modified Wegener’s hypothesis by suggesting two primordial continents: Laurasia in the north and Gondwana in the south.
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plate tectonicsDriving forces…of them, the South African Alexander Du Toit, remained an ardent believer. After Wegener’s death, Du Toit continued to amass further evidence in support of continental drift.
Read More…of them, the South African Alexander Du Toit, remained an ardent believer. After Wegener’s death, Du Toit continued to amass further evidence in support of continental drift.
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