er developed t tinents ogeto mingle, before tinents  apart and floated off to t positions. All t togetsteinente und Ozeane, or tinents andOceans, break of torld ar in time—in Engliser.

    Because of t attract mucice at first, but by 1920,  quickly became a subject of discussion.

    Everyone agreed t continents moved—but up and do sideical movement, knoasy, ion of geological beliefs for generations,to  extbooks o my o before turn of tury. ted t as tenEart ing oceanbasins and mountain ranges. Never mind t James ton  anysucatic arrangement ually result in a featureless sps. trated by Rutury, t Earts —mucoomuco allo of cooling and sed. And any tains sributed across tently t, and of more or less t by t  t some ranges, like time unately, Alfred egener  t geologists .

    For a start, ions questioned tions of tive o generate , but egener eorologist, for goodness sake. A remediable deficiencies.

    And so geologists took every pain to dismiss tleions. to get around tributions, ted ancient “landbridges” ime, a land bridge lantic.   ancient tapirs ed simultaneously in Sout Asia a land bridge oo. Soon maps of preoricseas  solid o Europe, fromBrazil to Africa, from Sout Asia to Australia, from Australia to Antarctica. tive tendrils  only conveniently appeared o move aliving organism from one landmass to anot t leaving atrace of tence. None of ted by so mucual evidence—not it ury.

    Even land bridges couldn’t explain some trilobite t o  only on one side. Noone could pe