They justified their animosity by complaining that he was unable to explain convincingly what might make continents move. On the contrary, the educated classes of both Europe and America joined ranks to spend much of the next half-century attacking Wegener's "delirious ravings" and trying to demolish both his hypothesis and his character. However, these revelations failed to attract an excited welcome: the association's minutes noted dismissively that there was "no discussion due to the advanced hour". Marsupials in South America and Australia were not only similar but hosted similar flatworm parasites. The fossils of tropical plants could be found on Spitsbergen. Wegener showed that the geology of the Appalachians matched that of the Scottish Highlands, and that rock strata occurring in Brazil also appeared in South Africa. However, no one took the proposition seriously until a meteorologist named Alfred Wegener presented the case for "continental displacement" to the Frankfurt Geological Association in 1912. ![]() It was in 1596 that a Flemish cartographer called Abraham Ortelius noticed the apparent fit between the coastlines of Africa and South America, and conjectured the movement of land-masses as a possible explanation.
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