Brazil -- Description and travel; Geology -- Amazon River Valley
Tout à vous,
L. AGASSIZ.[63]
Although no longer on board an independent steamer, we are still the
guests of the company, having government passages. Nothing can be more
comfortable than the travelling on these Amazonian boats. They are clean
and well kept, with good-sized state-rooms, which most persons use,
however, only as dressing-rooms, since it is always more agreeable to
sleep on the open deck in one’s hammock. The table is very well kept,
the fare good, though not varied. Bread is the greatest deficiency, but
hard biscuit makes a tolerable substitute. Our life is after this
fashion. We turn out of our hammocks at dawn, go down stairs to make our
toilets, and have a cup of hot coffee below. By this time the decks are
generally washed and dried, the hammocks removed, and we can go above
again. Between then and the breakfast hour, at half past ten o’clock, I
generally study Portuguese, though my lessons are somewhat interrupted
by watching the shore and the trees, a constant temptation when we are
coasting along near the banks. At half past ten or eleven o’clock
breakfast is served, and after that the glare of the sun becomes trying,
and I usually descend to the cabin, where we make up our journals, and
write during the middle of the day. At three o’clock I consider that the
working hours are over, and then I take a book and sit in my
lounging-chair on deck, and watch the scenery, and the birds and the
turtles, and the alligators if there are any, and am lazy in a general
way. At five o’clock dinner is served, (the meals being always on deck,)
and after that begins the delight of the day. At that hour it grows
deliciously cool, the sunsets are always beautiful, and we go to the
forward deck and sit there till nine o’clock in the evening. Then comes
tea, and then to our hammocks; I sleep in mine most profoundly till
morning.
To-day we stopped at a small station on the north side of the river
called Barreira das Cudajas. The few houses stand on a bank of red
drift, slightly stratified in some parts, and affording a support for
the river-mud, shored up against it. Since then, in our progress, we
have seen the same formation in several localities.
Public-domain text, read in full here on John Shaqi.
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