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<strong>Document</strong><br />
2<br />
Geography Lost and Found<br />
Page 31<br />
Anyone who owns an atlas has noticed at some point that the Brazilian bulge of South America seems<br />
to fit almost exactly into the facing indentation on the coast of Africa. At least a few people have long<br />
been aware that if you make cutouts of the outlines of the continents and treat the assemblage as a kind<br />
of jigsaw puzzle, the pieces fit together passably well into a single giant land mass and the fit is<br />
considerably improved if you include the continental shelves as well as the dry land. But until the<br />
middle of the 1960s this observation was pretty much ignored by geologists. A heretic like Alfred<br />
Wegener might claim that the fit was too good to be coincidence, that it demonstrated that continents<br />
were somehow drifting pieces of a primordial supercontinent. But mainstream geology could conceive<br />
of no mechanism for such drift, and thus ignored his ideas.<br />
So how did mainstream geology account for the shapes of the continents? Indeed, how did it account<br />
for the existence of the continents, or for that matter of all of the aspects of the earth's surface that we<br />
now believe to be the result of plate tectonics such as fault lines, rings of volcanoes, and for that matter<br />
mountain ranges? The answer, by<br />
<strong>file</strong>:///<strong>D|</strong>/Export2/<strong>www</strong>.<strong>netlibrary</strong>.<strong>com</strong>/<strong>nlreader</strong>/<strong>nlreader</strong>.<strong>dll</strong>@bookid=409&<strong>file</strong>name=page_31.html [4/18/2007 10:30:06 AM]