A Book of the United States. VariousЧитать онлайн книгу.
Kennebec also rises in the highlands, near the sources of the Androscoggin, and flows nearly south to the sea; falls and rapids render the navigation difficult above the tide at Augusta, from which place it is navigable for vessels of one hundred tons, and from Hallowell and Gardiner for ships to the sea. The country watered by the Kennebec generally consists of excellent land; it is one of the best grazing districts in New England; and there are upon the banks of the river a number of flourishing and handsome towns.
The Merrimack rises in New Hampshire, and has two principal branches: one of them being the outlet of lake Winnipiseogee. The north or longer branch is called the Pemigewasset, and has its source near the Notch of the White Mountains. At its junction with the outlet of the lake this stream takes the name of Merrimack, and flows south seventy-eight miles to Chelmsford, where it enters Massachusetts, through which it runs east to the sea. Its whole course is about two hundred miles. There are numerous falls in the New Hampshire portion. Though not equal to the Connecticut for fine scenery, the Merrimack is a noble and beautiful stream. Its waters are pure and salubrious, and on its borders are many flourishing towns. Its name in the Indian language signifies a sturgeon. Its width varies from fifty to one hundred and twenty rods; it receives many minor streams and rivers, which form the outlet of several small lakes. Its obstructions have been partly remedied by locks at different places, and there is a good navigation for vessels of two hundred tons to Haverhill. Two chain bridges cross the river at Newburyport, and Salisbury.
The Piscataqua has its rise and its whole course in New Hampshire. It is formed by the junction of several small streams in a wide and deep bed; the longest of these streams is Salmon Fall river, which forms part of the boundary between New Hampshire and Maine.
The Connecticut is the largest river of the New England States. It rises beyond the high-lands which separate the states of Vermont and New Hampshire from Lower Canada. It has been surveyed to the head spring of its northern branch, about twenty-five miles beyond the forty-fifth degree of latitude, from which to its mouth it flows upwards of three hundred miles through a well inhabited country. Its navigation is much interrupted by falls. It receives several rivers, as the Chicapee, Deerfield, Miller’s, and Farmington. At Hartford it meets the tide, whence it passes on in a winding course, till it falls into Long Island sound, between Saybrook and Lyme. This river is navigable for sloops, as far as Hartford, fifty miles distant from its mouth; and the produce of the country, for two hundred miles above it, is brought thither in flat-bottomed boats, which are so light us to be portable in carts.
The Hudson, or the North River, is formed by the confluence of the Hudson proper and the Mohawk, which unite below Waterford, ten miles above Albany. The Hudson takes its rise in the forty-fourth degree of north latitude, from the foot of the mountains which separate the waters of the St. Lawrence from those of Lake Champlain, and the Mohawk in the table-land surrounding Oneida lake. The Mohawk river rises to the north-east of Oneida lake, about eight miles from Sable Water, a stream of Lake Ontario. It runs first twenty miles south to Rome; then south-east one hundred and thirty-four miles; and, after receiving many tributary streams in its course, falls into the Hudson by three mouths. It is a large stream of water; and is now navigable for boats from Schenectady to Rome, one hundred and four miles distant. From Albany to Schenectady is a portage of sixteen miles, on account of the falls and rapids, which render the river unnavigable. These falls and rapids, denominated the Cohoes, are three miles from the junction of the Mohawk with the Hudson. The river is one thousand feet wide at these falls; the rock over which the stream descends is forty feet perpendicular height; and the whole height of the cataract, including the descent above, is seventy feet. Properly speaking, the North river is no other than a narrow gulf of the sea, entering inland at New York, and penetrating across the double chain of the Alleghany Mountains, as far as the confluence of the above mentioned streams, one hundred and seventy miles from the sea. This is what distinguishes the Hudson from all other rivers in the United States. In no other does the tide ascend beyond the first range; but in the North river, it crosses the first chain at West Point, sixty miles north of New York; and the second at Catskill, after having burst the beds of granite which opposed its passage, and cut them into a thousand different shapes. Hence the deep valley of the Hudson has derived a most singular and magnificent aspect; the western bank being, in some places, five hundred feet of perpendicular height above the level of the river.12
Along the shore of the Hudson, a mural precipice extends twenty miles. It commences at Weehawken, four miles north of the city of Jersey, gradually rising towards the north, and mostly occupied by forests. It is known by the name of the Palisadoes.
Palisadoe Rocks.
Raritan River, in the northern part of New Jersey, is formed by two branches which unite about twenty miles above New Brunswick. It becomes navigable two miles above that city, at a place called Brunswick Landing. Flowing by New Brunswick, and gradually becoming broader and deeper, it passes Amboy and then widens into Raritan bay, which is immediately connected with the ocean. It is navigable for sloops of eighty tons as far as New Brunswick, seventeen miles.
The Delaware issues by two streams, called the Coquago and the Rappadon, the union of which, forty miles in a direct line from their sources, form the Delaware, from the Katskill Mountains, in the county of Delaware, state of New York. Running first south, it next turns to the south-east, forming, for the space of sixty miles, the boundary between Pennsylvania and New York; and thence, forms again the line of separation between the former state and that of New Jersey, for upwards of one hundred miles more to Trenton, where there are falls, but of no great height. Thence, with increased breadth, it pursues a course of thirty-six miles farther, to Philadelphia, where it is a mile broad. Thence it proceeds to Newcastle, forty miles below Philadelphia, where it is two miles broad. Thence it spreads out into a spacious bay, and falls into the Atlantic seventy miles below Newcastle, by an outlet of twenty-five miles. The whole course of the river, from the Atlantic to its source, is three hundred and fifty miles; and two hundred and eighty from the head of Delaware bay, including the windings. Its two chief tributary streams are the Lehigh and Schuylkill. The navigation betwixt the Delaware and Chesapeak is now improved by means of a canal.
The River Susquehannah, of all those of the eastern states, most resembles the Mississippi and the St. Lawrence, on account of its numerous and distant branches. The north-east branch, which is the remotest source, is formed by the junction of two small streams that issue from the lakes of Camadebago, Ustavantho, and Otsego, in the state of New York. It runs south and south-west in such a winding course, (receiving in its progress the Unadilla and Chenango rivers from the north,) that it crosses the boundary line between New York and Pennsylvania no less than three times. It forms a junction with the Tioga, in forty-one degrees and fifty-seven minutes north latitude; and thence pursues a south-east course of seventy miles to Wyoming; whence, making a sudden bend at a right angle, it runs a south-west course of eighty miles, and unites with the west branch at Northumberland. The river, now increased to the breadth of half a mile, flows south through the mountains, a course of forty miles, to its junction with the Juniata, when, turning to the east for ten miles, it emerges from the mountains above Harrisburg, and after a south-east course of eighty miles, falls into Chesapeak bay. The western branch of the Susquehannah is formed by many streams, beyond the Alleghany Mountains; and its most southern source is within a very few miles of the Conemaugh, or Kiskeminitas, which falls into the Alleghany a little above Pittsburg. After running a very winding course of two hundred miles, principally among the mountains, it joins with the east branch at Northumberland. The Juniata rises in the Alleghany Mountains, and, pursuing an eastern and very serpentine and mountainous course, falls into the Susquehannah, after running two hundred miles. The whole course of the Susquehannah, from Chesapeak bay to the head of the north-east branch, is four hundred and fifty miles; and, including all its branches, it waters a tract of forty thousand square miles. Where it falls into the sea it is fully a mile broad; at Harrisburg it is nearly of the same breadth, and from three to five feet deep. There are seven falls in this river, which, with the numerous islands and rocks, render it navigable only for a few miles by large vessels.
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