The Fall Line |
November 18th, 2011 |
geography |
In school I learned that major cities are where they are because when
people and goods mostly moved by boat you needed to be on the ocean,
or at least a river. But how do we explain new york being on the
ocean while richmond is well inland? It turns out that there's
a geologic feature called the atlantic
seaboard fall line where the composition changes rapidly from metamorphosed
Paleozoic rocks to post-orogenic, flat-lying late-Mesozoic and
Cenozoic rocks. This makes waterfalls, or at least rapids, and
tends to mark the farthest up the river you can get most shipping:
Referenced in: Free Raisins Summer Tour 2013
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