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
The beaches which are now in their highest state of development are
Sandy Hook, Seven-Mile Beach, and Holly Beach near Cape May. These
typical examples of the sea-born barriers are much alike in structure,
and consist of four principal divisions. The first division, or
interior, is an undulating area covered with heavy timber, of which
the size suggests its age. Immense hollies, oaks, pines, and red
cedars abound, many of the first measuring two feet in diameter, and
some of the latter attaining a circumference of four or five yards.
The sassafras grows in remarkable luxuriance and immense grape-vines
are everywhere to be seen, overhanging a dense undergrowth. In spring
and summer the ground is covered with fragrant blossoms; columbines,
violets, pinks, orchids, and a host of other flowers lend their blight
colors to enhance the varied greens of the foliage. This is the beach
primeval. Skirting it seaward is the second division, which bears
smaller timber. Low cedars, hollies, and pines are here the chief forms
of arboreal vegetation, and fewer flowering plants are seen. This zone
is of later formation, and its trees are younger than those of the
first. Adjoining it is the third division, which consists of a belt of
undulating dunes a few hundred feet or yards in width, and bearing
the mossy Hudsonia or scrubby bushes of beach plum and wax-myrtle, or
in some places, especially on the outer row of dunes, only supporting
a meager growth of beach grass. Frequently, between two rows of dunes,
an expanse of salt meadow occurs, or a sand flat bearing stunted forms
of plant life. With this third division ends the domain of vegetation,
succeeded by the sloping strand upon which the tide rises and falls.
The sand-bar, exposed at low water at the extremity of the beach,
is constantly increased in length and height by the action of the
currents, and the process of beach formation is here continually in
progress.
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