When the Allen brothers decided that
the high, wooded bank of Buffalo
Bayou opposite the mouth of White Oak Bayou was the place to establish
a
new town, they advertised the location as the head of tidewater.

This was an important point. As land speculators, the Allens knew that
a
town rooted in commerce had the best chance for fast growth. The faster
the
growth of the town, the sooner they could cash in on their $5,000
investment
by selling lots.
Harrisburg, some six miles or so downstream, was the major port during
the
pre-republican period. By establishing a port farther upstream and
closer
to the interior of Texas, John and Augustus Allen sought to capitalize
on
the setback that Harrisburg suffered when it was burned to the ground
by
Santa Anna on his march to San Jacinto.
The race to create to the shipping center of the new republic began in
the
late summer of 1836 as Gail Borden surveyed the townsite of Houston and
the
Allens declared it as the place where steamers from New Orleans would
unload
the fine goods of the world for Texas. Houston was the head of
tidewater
and a port accessible by ocean-going steam ships.
The head of tidewater was significant because the tidal flow meant that
there
would be a reliable depth of water in the bayou for shipping.
Whether the junction of White Oak Bayou and Buffalo Bayou was actually
the
head of tidewater was a subject of debate during the intense
competition
of the mid-1800's. When dredging of the bayou became the common
practice,
the point was moot.
Today, the point at which the tidal influence occurs is a few hundred
yards
upstream of the Shepherd Drive bridge. Early in the twentieth century,
the
gauge at Waugh Drive measured the tidewater, but the subsidence that
has
occurred in the last fifty years has caused the U. S. Geological Survey
to
abandon the gauge at Waugh Drive in favor of the one at Shepherd Drive.
The tidal influence on the bayou is easily seen in a comparison of the
readings
of the Shepherd Drive gauge with the Piney Point gauge which is several
miles
upstream.
The graph of the gauge height at Piney Point shows a fairly level
pattern
of stream flow (except where there is a spike due to a rain storm). At
the
Shepherd Drive gauge (called, somewhat ironically, Buffalo Bayou at
Houston),
the gauge height undulates in a wave-like pattern, clearly showing the
effect
of the tide.
Yet, without looking at the graph of the gauges, one would not even be
aware
of this tidal effect. The tidal influence on Buffalo Bayou, which was
such
a critical factor in the establishment of the city of Houston, is today
just
an interesting curiosity
All material printed on this
page
and this web site is copyrighted. All rights reserved.
Copyright by Louis F. Aulbach,
2003