The flow of time in the Connecticut valley : $b geological imprintsBain, George W. (George William)
Science
The flow of time in the Connecticut valley : $b geological imprints
Bain, George W. (George William)
Geology -- Connecticut River Valley
Today and Yesterday
From the Coolidge Memorial Bridge the broad lowland seems to reach out
in all directions towards the encircling hills. Far down the river, the
distant bank rises a sheer thirty feet from the water and is high enough
to surmount even the worst of floods. Yet each year this bank recedes as
the unconsolidated sediment at its base is sapped by the stream and is
carried away. Three times the river road has been moved back from the
insatiable Connecticut, and today the main Hockanum highway takes the
long route far from the water’s edge.
_The River Works_
Nearer the bridge the land is lower, and it shows the effects of
frequent inundation, but not of scour. A great sand bar lies in the
curve of the stream, and the low parallel ridges suggest that they, too,
were awash in the Connecticut before its eastern bank encroached so far
upon the town of Hadley. The tongue of land which serves as
Northampton’s airport is a succession of bars and abandoned channels
which record the migration of the river away from its old bank along
Bridge Street. The Connecticut is robbing Hadley to pay Northampton, but
there was a time when Northampton was pilfered, too.
Swales line the landscape as far as Hadley; and each year, at the time
of high water, they must now be content with the meager overflow, where
once they sped the entire stream upon its southward course. But even
now, in flood, their original function may be restored. For the swale
just west of Hadley was a roaring torrent in 1938, 1936, and 1896.
Indeed, it threatened to appropriate the entire stream, and each of the
great curving hollows that furrow the lowland are scour-channels which
were made at other times.
[Illustration: Fig. 1. _The Connecticut River undercuts the Hadley
bank at Hockanum._]
[Illustration: Fig. 2. _Natural levees border the Connecticut River
south of the Sunderland Bridge._]
Public-domain text, read in full here on John Shaqi.
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