to Haverhill, or else lying at anchor or aground, waiting for wind or tide; until, at last, you glide under the famous Chain Bridge, and are landed at Newburyport. Thus she who at first was “poore of waters, naked of renowne,” having received so many fair tributaries, as was said of the Forth,
“Doth grow the greater still, the further downe;
Till that abounding both in power and fame,
She long doth strive to give the sea her name”;
or if not her name, in this case, at least the impulse of her stream. From the steeples of Newburyport you may review this river stretching far up into the country, with many a white sail glancing over it like an inland sea, and behold, as one wrote who was born on its head-waters, “Down out at its mouth, the dark inky main blending with the blue above. Plum Island, its sand ridges scolloping along the horizon like the sea-serpent, and the distant outline broken by many a tall ship, leaning, still, against the sky.”
Rising at an equal height with the Connecticut, the Merrimack reaches the sea by a course only half as long, and hence has no leisure to form broad and fertile meadows, like the former, but is hurried along rapids, and down numerous falls, without long delay. The banks are generally steep and high, with a narrow interval reaching back to the hills, which is only rarely or partially overflown at present, and is much valued by the farmers. Between Chelmsford and Concord, in New Hampshire, it varies from twenty to seventy-five rods in width. It is probably wider than it was formerly, in many places, owing to the trees having been cut down, and the consequent wasting away of its banks. The influence of the Pawtucket Dam is felt as far up as Cromwell’s Falls, and many think that the banks are being abraded and the river filled up again by this cause. Like all our rivers, it is liable to freshets, and the Pemigewasset has been known to rise twenty-five feet in a few hours. It is navigable for vessels of burden about twenty miles; for canal-boats, by means of locks, as far as Concord in New Hampshire, about seventy-five miles from its mouth; and for smaller boats to Plymouth, one hundred and thirteen miles. A small steamboat once plied between Lowell and Nashua, before the railroad was built, and one now runs from Newburyport to Haverhill.
Unfitted to some extent for the purposes of commerce by the sand-bar at its mouth, see how this river was devoted from the first to the service of manufactures. Issuing from the iron region of Franconia, and flowing through still uncut forests, by inexhaustible ledges of granite, with Squam, and Winnipiseogee, and Newfound, and Massabesic Lakes for its mill-ponds, it falls over a succession of natural dams, where it has been offering its privileges in vain for ages, until at last the Yankee race came to improve them. Standing at its mouth, look up its sparkling stream to its source—a silver cascade which falls all the way from the White Mountains to the sea—and behold a city on each successive plateau, a busy colony of human beaver around every fall. Not to mention Newburyport and Haverhill, see Lawrence, and Lowell, and Nashua, and Manchester, and Concord, gleaming one above the other. When at length it has escaped from under the last of the factories, it has a level and unmolested passage to the sea, a mere waste water, as it were, bearing little with it but its fame; its pleasant course revealed by the morning fog which hangs over it, and the sails of the few small vessels which transact the commerce of Haverhill and Newburyport. But its real vessels are railroad cars, and its true and main stream, flowing by an iron channel farther south, may be traced by a long line of vapor amid the hills, which no morning wind ever disperses, to where it empties into the sea at Boston. This side is the louder murmur now. Instead of the scream of a fish-hawk scaring the fishes, is heard the whistle of the steam-engine, arousing a country to its progress.
This river too was at length discovered by the white man, “trending up into the land,” he knew not how far, possibly an inlet to the South Sea. Its valley, as far as the Winnipiseogee, was first surveyed in 1652. The first settlers of Massachusetts supposed that the Connecticut, in one part of its course, ran northwest, “so near the great lake as the Indians do pass their canoes into it over land.” From which lake and the “hideous swamps” about it, as they supposed, came all the beaver that was traded between Virginia and Canada—and the Potomac was thought to come out of or from very near it. Afterward the Connecticut came so near the course of the Merrimack that, with a little pains, they expected to divert the current of the trade into the latter river, and its profits from their Dutch neighbors into their own pockets.
Unlike the Concord, the Merrimack is not a dead but a living stream, though it has less life within its waters and on its banks. It has a swift current, and, in this part of its course, a clayey bottom, almost no weeds, and comparatively few fishes. We looked down into its yellow water with the more curiosity, who were accustomed to the Nile-like blackness of the former river. Shad and alewives are taken here in their season, but salmon, though at one time more numerous than shad, are now more rare. Bass, also, are taken occasionally; but locks and dams have proved more or less destructive to the fisheries. The shad make their appearance early in May, at the same time with the blossoms of the pyrus, one of the most conspicuous early flowers, which is for this reason called the shad-blossom. An insect called the shad-fly also appears at the same time, covering the houses and fences. We are told that “their greatest run is when the apple-trees are in full blossom. The old shad return in August; the young, three or four inches long, in September. These are very fond of flies.” A rather picturesque and luxurious mode of fishing was formerly practised on the Connecticut, at Bellows Falls, where a large rock divides the stream. “On the steep sides of the island rock,” says Belknap, “hang several arm-chairs, fastened to ladders, and secured by a counterpoise, in which fishermen sit to catch salmon and shad with dipping nets.” The remains of Indian weirs, made of large stones, are still to be seen in the Winnipiseogee, one of the head-waters of this river.
It cannot but affect our philosophy favorably to be reminded of these shoals of migratory fishes, of salmon, shad, alewives, marsh-bankers, and others, which penetrate up the innumerable rivers of our coast in the spring, even to the interior lakes, their scales gleaming in the sun; and again, of the fry which in still greater numbers wend their way downward to the sea. “And is it not pretty sport,” wrote Captain John Smith, who was on this coast as early as 1614, “to pull up twopence, sixpence, and twelvepence, as fast as you can haul and veer a line?”—“And what sport doth yield a more pleasing content, and less hurt or charge, than angling with a hook, and crossing the sweet air from isle to isle, over the silent streams of a calm sea.”
On the sandy shore, opposite the Glass-house village in Chelmsford, at the Great Bend where we landed to rest us and gather a few wild plums, we discovered the Campanula rotundifolia, a new flower to us, the harebell of the poets, which is common to both hemispheres, growing close to the water. Here, in the shady branches of an apple-tree on the sand, we took our nooning, where there was not a zephyr to disturb the repose of this glorious Sabbath day, and we reflected serenely on the long past and successful labors of Latona.
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