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oceans； which was published in german in 1912 and鈥攄espite the outbreak of the firstworld war in the meantime鈥攊n english three years later。
because of the war； wegener鈥檚 theory didn鈥檛 attract much notice at first； but by 1920； whenhe produced a revised and expanded edition； it quickly became a subject of discussion。
everyone agreed that continents moved鈥攂ut up and down； not sideways。 the process ofvertical movement； known as isostasy； was a foundation of geological beliefs for generations；though no one had any good theories as to how or why it happened。 one idea； which remainedin textbooks well into my own school days； was the baked apple theory propounded by theaustrian eduard suess just before the turn of the century。 this suggested that as the moltenearth had cooled； it had bee wrinkled in the manner of a baked apple； creating oceanbasins and mountain ranges。 never mind that james hutton had shown long before that anysuch static arrangement would eventually result in a featureless spheroid as erosion leveledthe bumps and filled in the divots。 there was also the problem； demonstrated by rutherfordand soddy early in the century； that earthly elements hold huge reserves of heat鈥攎uch toomuch to allow for the sort of cooling and shrinking suess suggested。 and anyway； if suess鈥檚theory was correct then mountains should be evenly distributed across the face of the earth；which patently they were not； and of more or less the same ages； yet by the early 1900s it wasalready evident that some ranges； like the urals and appalachians； were hundreds of millionsof years older than others； like the alps and rockies。 clearly the time was ripe for a newtheory。 unfortunately； alfred wegener was not the man that geologists wished to provide it。
for a start； his radical notions questioned the foundations of their discipline； seldom aneffective way to generate warmth in an audience。 such a challenge would have been painfulenough ing from a geologist； but wegener had no background in geology。 he was ameteorologist； for goodness sake。 a weatherman鈥攁 german weatherman。 these were notremediable deficiencies。
and so geologists took every pain they could think of to dismiss his evidence and belittlehis suggestions。 to get around the problems of fossil distributions； they posited ancient 鈥渓andbridges鈥潯herever they were needed。 when an ancient horse named hipparion was found tohave lived in france and florida at the same time； a land bridge was drawn across theatlantic。 when it was realized that ancient tapirs had existed simultaneously in southamerica and southeast asia a land bridge was drawn there； too。 soon maps of prehistoricseas were almost solid with hypothesized land bridges鈥攆rom north america to europe； frombrazil to africa； from southeast asia to australia； from australia to antarctica。 theseconnective tendrils had not only conveniently appeared whenever it was necessary to move aliving organism from one landmass to another； but then obligingly vanished without leaving atrace of their former existence。 none of this； of course； was supported by so much as a grainof actual evidence鈥攏othing so wrong could be鈥攜et it was geological orthodoxy for the nexthalf century。
even land bridges couldn鈥檛 explain some things。 one species of trilobite that was wellknown in europe was also found to have lived on newfoundland鈥攂ut only on one side。 noone could persuasively explain how it had managed to cross two thousand miles of hostileocean but then failed to find its way around the corner of a 200…mile…wide island。 even moreawkwardly anomalous was another species of trilobite found in europe and the pacificnorthwest but nowhere in between； which would have required not so much a land bridge as aflyover。 yet as late as 1964 when the encyclopaedia britannica discussed the rival theories； itwas wegener鈥檚 that was held to be full of 鈥渘umerous grave theoretical difficulties。鈥�
to be sure； wegener made mistakes。 he asserted that greenland is drifting west by about amile a year； which is clearly nonsense。 （it鈥檚 more like half an inch。） above all； he could offerno convincing explanation for how the landmasses moved about。 to believe in his theory youhad to accept that massive continents somehow pushed through solid crust； like a plowthrough soil； without leaving any furrow in their wake。 nothing then known could plausiblyexplain what motored these massive movements。
it was arthur holmes； the english geologist who did so much to determine the age of theearth； who suggested a possible way。 holmes was the first scientist to understand thatradioactive warming could produce convection currents within the earth。 in theory thesecould be powerful enough to slide continents around on the surface。 in his popular andinfluential textbook principles of physical geology ； first published in 1944； holmes laid outa continental drift theory that was in its fundamentals the theory that prevails today。 it wasstill a radical proposition for the time and widely criticized； particularly in the united states；where resistance to drift lasted longer than elsewhere。 one reviewer there fretted； without anyevident sense of irony； that holmes presented his arguments so clearly and pellingly thatstudents might actually e to believe them。
elsewhere； however； the new theory drew steady if cautious support。 in 1950； a vote at theannual meeting of the british association for the advancement of science showed that abouthalf of those present now embraced the idea of continental drift。 （hapgood soon after citedthis figure as proof of how tragically misled british geologists had bee。） curiously；holmes himself sometimes wavered in his conviction。 in 1953 he confessed： 鈥渋 have neversucceeded in freeing myself from a nagging prejudice against continental drift； in mygeological bones； so to speak； i feel the hypothesis is a fantastic one。鈥�
continental drift was not entirely without support in the united states。 reginald daly ofharvard spoke for it； but he； you may recall； was the man who suggested that the moon hadbeen formed by a cosmic impact； and his ideas tended to be considered interesting； evenworthy； but a touch too exuberant for serious consideration。 and so most american academicsstuck to the belief that the continents had occupied their present positions forever and thattheir surface features could be attributed to something other than lateral motions。
interestingly； oil pany geologists had known for years that if you wanted to find oil youhad to allow for precisely the sort of surface movements that were implied by plate tectonics。
but oil geologists didn鈥檛 write academic papers； they just found oil。
there was one other major problem with earth theories that no one had resolved； or evene close to resolving。 that was the question of where all the sediments went。 every yearearth鈥檚 rivers carried massive volumes of eroded material鈥�500 million tons of calcium； forinstance鈥攖o the seas。 if you multiplied the rate of deposition by the number of years it hadbeen going on； it produced a disturbing figure： there should be about twelve miles ofsediments on the ocean bottoms鈥攐r； put another way； the ocean bottoms should by now bewell above the ocean tops。 scientists dealt with this paradox in the handiest possible way。
they ignored it。 but eventually there came a point when they could ignore it no longer。
in the second world war； a princeton university mineralogist named harry hess was putin charge of an attack transport ship； the uss cape johnson。 aboard this vessel was a fancynew depth sounder called a fathometer； which was designed to facilitate inshore maneuvers during beach landings； but hess realized that it could equally well be used for scientificpurposes and never switched it off； even when far out at sea； even in the heat of battle。 whathe found was entirely unexpected。 if the ocean floors were ancient； as everyone assumed； theyshould be thickly blanketed with sediments； like the mud on the bottom of a river or lake。 buthess鈥檚 readings showed that the ocean floor offered anything but the gooey smoothness ofancient silts。 it was scored everywhere with canyons； trenches； and crevasses and dotted withvolcanic seamounts t