Travels in the Interior of Brazil: Principally through the northern provinces, and the gold and diamond districts, during the years 1836-1841Gardner, George
History
Travels in the Interior of Brazil: Principally through the northern provinces, and the gold and diamond districts, during the years 1836-1841
Gardner, George
Brazil -- Description and travel; Mines and mineral resources -- Brazil
of those annoying insects. As I slept in my clothes without any covering,
I was obliged to shield my face with my pocket-handkerchief, and thrust
my hands into my pockets. Although I was thus in some measure protected
from their bites, it was long before I could again fall asleep, from the
continued humming noise, almost as loud as that of bees, which they were
making around me. When I got up at daybreak, after a restless night, I
found that besides the mosquitos, I was surrounded by thousands of a
small black sand-fly (_Merohy_), not much larger than a grain of fine
gunpowder, but whose bites are no less irritating than those of their
larger congeners. The morning tide, we found, did not rise so high as it
did on the previous evening, and it was with some difficulty that the
jangada was floated into deep water, which was not effected till nearly
nine o’clock, A.M. In crossing the bar at the mouth of the river, we had
to pass through a line of small breakers, three of which swept over the
elevated platform on which I was sitting, and drenched me to the skin,
thereby rendering the remainder of the voyage very uncomfortable. It was
one o’clock, P.M., when we reached a little village called Peba, which
is situated on the coast, about five leagues to the north of the mouth
of the Rio San Francisco: this was the termination of my sea-voyage, as
the heavy surf which breaks over the shallow bar of that river will not
allow jangadas to enter it. The village is situated a little way inland,
and is hidden from the sea by a high embankment of sand, which at this
place is very much drifted by the wind; it is, however, recognised at
a considerable distance, from the number of tall cocoa-nut trees which
grow near the shore. I was here particularly struck with a fact which
goes a great way to explain the phenomenon of the stem of a fossil tree
being found passing through several strata of sandstone rock. Many of the
cocoa-nut trees have their stems embedded to the depth of fifty feet and
upwards in the embankment of sand which stretches along the shore, and
in many places is several hundred feet broad; some of them, indeed, are
so deeply embedded, that the nuts can be gathered without climbing the
tree. Now as this sand has accumulated at different periods, particularly
during the prevalence of the north-east trade-wind, it must present, if
ever it becomes hardened, a vast number of irregularly horizontal beds,
through which the stems of the palms will be found to pass.
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