to be very little hope that we should live to see another, the coolness,
steady obedience, and untiring exertions of each individual, were every
way worthy of British seamen.
“The storm gained its height at 2 P.M., when the barometer stood at
28·40 inches, and after that time began to rise. Although we had been
forced many miles deeper into the pack, we could not perceive that the
swell had at all subsided, our ships still rolling and groaning amidst
the heavy fragments of crushing bergs, over which the ocean rolled its
mountainous waves, throwing huge masses upon one another, and then again
burying them deep beneath its foaming waters, dashing and grinding them
together with fearful violence.” For three successive years were these
dangers encountered during this bold and hazardous enterprise.
The ocean is one mass of water, which, entering into the interior of the
continents, has formed seas and gulfs of great magnitude, which afford
easy and rapid means of communication, while they temper the climates of
the widely expanding continents.
The inland seas communicating with the Atlantic are larger, and
penetrate more deeply into the continents, than those connected with the
great ocean; a circumstance which gives a coast of 48,000 miles to the
former, while that of the great ocean is only 44,000. Most of these
internal seas have extensive river domains, so that by inland navigation
the Atlantic virtually enters into the deepest recesses of the land,
brings remote regions into contact, and improves the condition of the
less cultivated races of mankind by commercial intercourse with those
that are more civilized.
Public-domain text, read in full here on John Shaqi.
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