The Tide Had Been
A High One When We Beached Our Boat At The Foot
Of A Bluff.
Two hours later the receding tide
left us a quarter of a mile from the current.
The river was
Fully two miles wide at this point,
and so powerful was its current that steamers
anchored in it were obliged to keep their wheels
slowly revolving to ease the strain on their
anchors. Early on Monday morning we beheld
with consternation that the tide did not reach
our boat, and by dint of hard labor we
constructed a railroad from a neighboring fence,
and moved the Mayeta on rollers upon it over
the mud and the projecting reef of rocks some
five hundred feet to the water, then embarking,
rowed close along the shore to avoid the current.
A deep fog settled down upon us, and we were
driven to camp again on the left bank, where a
cataract tumbled over the rocks fifty or more
feet. Tuesday was a sunny day, but the usual
head wind greeted us. The water would rise
along-shore on the flood three hours before the
downward current was checked in the channel
of the river. We could not place any
dependence in the regularity of the tides, as strong
winds and freshets in the tributaries influence
them. Earlier in the season, as a writer
remarks, "until the upland waters have all run
down, and the great rivers have discharged the
freshets caused by thawing of the snows in the
spring of the year, this current, in spite of tides,
will always run down." To the uninitiated the
spectacle is a curious one, of the flood tide rising
and swelling the waters of a great river some
eight to ten feet, while the current at the surface
is rapidly descending the course of the stream.
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