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john and sebastian cabot - Cristo Raul

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JOHN AND SEBASTIAN CABOT 159<br />

In apology for him it<br />

may<br />

be said that he was<br />

possibly influenced by the Verrazano map,<br />

or rather<br />

by a copy of a portion of the same, which not only<br />

showed a Ocean great (Mar de Verrazano) to the<br />

West of that strip of Eastern seaboard which was the<br />

whole of North America then known, but depicted this<br />

Western Ocean as<br />

communicating<br />

with the Atlantic<br />

by a narrow channel a little to the north of Florida.<br />

True the Verrazano map itself, in an inscription at<br />

this point, carefully<br />

stated that an isthmus of l<strong>and</strong> six<br />

miles across separated the two seas, <strong>and</strong> thus left no<br />

doubt as to the c continental<br />

<strong>and</strong> unbroken character<br />

of the North American Atlantic seaboard ;<br />

but this in<br />

scription was omitted in the earliest copy we possess, 1<br />

which also substituted a connecting strait for a dividing<br />

tongue of l<strong>and</strong>. In many respects the Harleian map<br />

here referred to bears a striking resemblance to the<br />

Cabotian planisphere of 1<br />

544<br />

quite as close a likeness,<br />

in fact, as is borne to that same planisphere by the<br />

Desliens map of 1541 ;<br />

<strong>and</strong> the probability is strong<br />

that Cabot was acquainted with both. But in any<br />

case, it may be said, the story of Sebastian s actual<br />

coasting of that seaboard as far as Florida would be<br />

disproved by this Apology, for then Sebastian would<br />

have known enough to contradict, from personal<br />

knowledge, the mistake suggested by his interrogator,<br />

1<br />

See the portrayal of this feature (the isthmus) in the Harleian<br />

map of circa 1536 to 1540, which is the oldest existing known<br />

specimen of Dieppese cartography.

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