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12 THE EARTH MOVES
rsuasively explain  o cross tileocean but to find its rilobite found in Europe and t but noe as 1964  ical difficulties.”

    to be sure, egener made mistakes. ed t Greenland is drifting  by about amile a year, o believe in o accept t massive continents some, like a plo motored ts.

    It  ermine ted a possible ist to understand tradioactive ion currents o slide continents around on tial textbook Principles of P publisa continental drift t s fundamentals t prevails today. It ill a radical proposition for time and icized, particularly in ted States,o drift lasted longer tted,  anyevident sense of irony, t ed s so clearly and compellingly tstudents migually come to believe trike&gt;htt<a href="p://&lt;/strike&gt;" target="_blank">p://&lt;/strike&gt;</a>

    Elseious support. In 1950, a vote at ting of tision for t of Science s about noinental drift. (er citedtragically misled Britiss imes inental drift; in mygeological bones, so to speak, I feel tastic one.”

    Continental drift  entirely  support in ted States. Reginald Daly of, but ed t t, and ended to be considered interesting, even a toucoo exuberant for serious consideration. And so most American academicsstuck to t tinents  positions forever and ttures could be attributed to someteral motions.

    Interestingly, oil company geologists  if you ed to find oil youo allo of surface movements t e tectonics.

    But oil geologists didn’t e academic papers; t found oil.

    t no one o resolving. t ion of .
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