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years ago solidified into what is now Mt. Stuart did so somewhere off what is
now Southern California or Mexico. This discovery shook the geological es-
tablishment to its core.
Soon afterward, other paleomagnetic findings suggested that not just
Mt. Stuart, but also other pieces of northwestern Washington and southern
British Columbia, journied from lower latitudes. Each of these rock bodies
had to have traveled between 2,000 and 3000 kilometers from the south. But
here was more than simple transport. The rock bodies were also rotated as
A) Morphogeological belts of Western Canada.
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