Barrier beaches of the Atlantic coastMerrill, Frederick J. H. (Frederick James Hamilton)
Science
Barrier beaches of the Atlantic coast
Merrill, Frederick J. H. (Frederick James Hamilton)
Barrier islands; Beaches -- New Jersey
Property-owners along the ocean front of the beaches have generally
made the mistake of supposing that the domain of the Atlantic was
bounded by the high-water mark of the spring tides. Any one who
should build a dwelling on the strand below ordinary high-water mark
would be considered lacking in common sense, yet it is scarcely less
foolish to build within reach of the storm-waves. It is, of course,
true that many cottages are now much nearer the water’s edge than
they were a few years ago. This is due to the wear of the shore by
currents already described as flowing parallel to it and removing the
sand which the waves have loosened. If the action of these currents
should be stopped--and there is good evidence to show that a system
of jetties would intercept them and cause them to drop their stolen
load of sand--the wear of the shore would be arrested and the yearly
encroachments of the ocean would cease.
With regard to the inundation of Atlantic City by the sea in the
great September storm of 1889 it should be said that this catastrophe
ought not to be considered very wonderful, since the greater portion
of the city is less than ten feet above mean tide, and the highest
point recorded by the New Jersey State Survey is only thirteen feet
above that level. As ordinary tides rise a foot above this plane, and
spring tides nearly two feet, it is evident that a prolonged easterly
storm would soon cause a considerable area to be overflowed. Since the
bays and channels which lie between the beach and the mainland are
almost completely landlocked and the inlets are relatively narrow, the
water-level is soon raised to a height of two or three feet above the
meadows, and this is sufficient to cover most of the railroad tracks.
To be sure, no such inundation as the recent one has occurred since
Atlantic City became a place of importance, nor do the old residents
on the coast remember such a storm in former years; but it is evident
that, while the beaches were uninhabited, such a storm as the one in
question would attract less attention, since it would cause little if
any loss of property.
Public-domain text, read in full here on John Shaqi.
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