MIT OpenCourseWarehttp://ocw.mit.edu 12.002 Physics and Chemistry of the Earth and Terrestrial Planets Fall 2008 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms.Polar Wander and Continental Drift 1620 - Francis Bacon, pointed out similarities of coastlines of Brazil and Africa 1912 - Alfred Wegner (German meteorologist and geologist) All continents assembled 250 million years ago as one supercontinent called Pangaea Based on similar geology and fossils. They since drifted to their current position. 1956 - Keith Runcorn demonstrated that Apparent Polar Wander (APW) paths of North America and Europe from late Paleozoic to early Mesozoic rocks in North America and Europe matched better if Atlantic closed. 1957 - Ted Irving showed that the APW paths of some continents also matched if Atlantic were closed before the Earth Mesozoic. 1960s - Vine and Matthews: argued that stripes of rocks with alternating polarity of magnetization reflected creation of new crust at seafloor ridges followed by symmetrical spreading: convection Same time - paleomagnetists like Allen Cox (Stanford) started studying continental lavas. Eventually found that 105 to 106 years the field reversed. Magnetostatigraphic timescale of periods of alternating magnetic fields. Record of last reversal in seafloor rocks same as in continents (780,000 thousand years ago) 1960's Magnetic reversals Seafloor spreading Rigid plates These three elements together really brought plate tectonics hypothesis to foreground. Lithosphere is part of convective process; on all other terrestrial planets today, the uppermost part (lithosphere) is not part of convection. Arthur Holmes - radiometric dating - relating continental drift (1929) with
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