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if each of the rocks sampled had pointed to the pole in the same position as today,
posite.
Creer then got the brilliant idea of adding to his map the pole position that John
shown by the point labeled “S-USA,” it lay well off the position of the Silurian
pole as determined by the polar wandering curve from British rocks. Rocks from
Europe and North America showed the pole in different places at the same time.
rocks. The other lines are pole positions estimated from past climates. “S-USA” is the pole posi-
tion as determined by Graham for Silurian rocks from Pennsylvania. From Creer's 1955 Ph.D.
dissertation.
Source
: K. M. Creer and E. Irving, “Testing Continental Drift: Constructing the
First Palaeomagnetic Path of Polar Wander (1954),”
Earth Sciences History
31, no. 1(2012):
111-145.
Sometimes inscience wecanidentify asymbolic instant, acritical turningpoint,
after which nothing was ever the same. One occurred the first time Rutherford had
enough information to calculate a mineral's age from radioactivity and found it
to far exceed Kelvin's upper limit. Surely another arrived the instant Creer lifted
his pen from plotting the American Silurian pole on his map. The continents had
moved.
Runcorn Converts