Canada -- Description and travel; United States -- Description and travel
The great curiosity of St. John is the "reversible cataract" in the
river, caused in the gorge just west of the city by the enormous tides
of the Bay of Fundy. The great river above the city is a wide estuary,
but before entering the harbor it is compressed into a short, deep and
narrow gorge, barely one hundred and fifty yards wide in some places,
and obstructed by several rocky islets. As this is the best
crossing-place, two bridges are thrown side by side over the chasm,
one for a railway and the other for a street, resting upon the
limestone cliffs a hundred feet above the water. As the tide ebbs and
flows, the rushing river currents make the reversible cataract, almost
under the bridges, with the water pouring down both ways at different
tidal stages. Through this contracted pass the entire current of the
vast St. John valley finds its outlet to the sea. When the ebb tide
quickly empties the harbor below, the accumulated river waters cannot
get into the gorge fast enough to reduce as rapidly the level of the
broad basin above, and they consequently rush down, a cataract,
swelling sometimes to ten or twelve feet at the upper entrance to the
gorge, and make whirling, seething rapids below. When the tide turns,
this outflow is gradually checked by the rise in the harbor, but soon
the tremendous incoming flood from the Bay of Fundy overpowers the
river current, fills up the gorge, and rapidly rising in the gorge
rushes inward to the broad basin, thus making the cataract fall the
other way. Twice every day this ever-changing contest is fought, and
were it not for the obstruction made by this narrow, rocky gateway,
these enormous tides would rush along in full force and overflow a
large surface of the very low-lying interior of New Brunswick. The
river makes a sharp bend just at the outlet of the gorge, turning from
south to northeast around a rocky cape protruding far into the stream;
then it broadens out into a rounded bay, and a short distance beyond
sharply bends again into the harbor of St. John. Vessels are taken
through the gorge at proper tidal stages, guided by tugs and floating
at high speed with the rushing current. This is one of the most
remarkable exhibitions made of the curious influence of these enormous
Bay of Fundy tides.
Public-domain text, read in full here on John Shaqi.
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