New England -- History -- Colonial period, ca. 1600-1775
This formation of upland and valley extends to the shore-line of Sound
and ocean, the broad coastal plain, which is so marked a feature from
New Jersey southward, being almost wholly absent in New England. This is
probably due to a subsidence of the shore, which allowed the ocean to
flow back over part of the land, and which also explains the many
hundred islands off the coast of Maine, and the drowned river valleys
along the Sound. So numerous are the islands, bays, and headlands of the
rugged coast north of the Isles of Shoals, that they expand the two
hundred and thirty miles of shore to nearly three thousand, if all are
included in the measurement. In this section, also, there are many good
harbors, particularly that of Portland, but the coast is so greatly
dissected as to make land communication along it very difficult; while
the small boats, which partially served the needs of commerce and travel
in early days, were seriously interfered with by the great rise and fall
of the tides. Both these conditions tended to isolate the colonial
settlements and hinder their development. The upland country, with its
poorer soil and more difficult conditions of life, also approaches
nearer to the sea in Maine and New Hampshire than farther south, so
that, although Portsmouth, too, has a fine harbor, those states have
always been more thinly settled than the others.
The coast of Massachusetts is less rugged, but more varied. South of the
granite headland of Cape Ann, the shores of Boston Bay are still rocky
and irregular; but both shores of the great sandy curve of the Cape Cod
peninsula, which, with Cape Ann, encloses the waters of Massachusetts
Bay, are smooth and moulded by wind and wave. The coast again becomes
rough around Buzzard's Bay, while the almost land-locked waters of Rhode
Island have drowned the old river-system of that state. Opposite
Connecticut lies Long Island, the only island of any considerable size
along the entire Atlantic coast; so that the Sound, or inland sea, thus
formed between it and the mainland, gives to Connecticut the advantage
of a quiet, protected waterway for all its ports.
Public-domain text, read in full here on John Shaqi.
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