side with hemlock, pine, spruce, and other evergreens. These mountains are from ten to fifteen miles wide, much intersected with valleys, and abounding in springs and streams. Vegetation decreases on approaching their summits; the trees diminish in size, and frequently terminate in a shrubbery of spruce and hemlock, two or three feet high, with branches so interwoven as to prevent all passage through them. The sides of the mountains are generally rugged and irregular; some of them have large apertures and caves. Their tops are coated with a compact and firm moss, which lies in extensive beds, and is sometimes of a consistency to bear the weight of a man without being broken through. These mosses absorb a great deal of moisture, and afford wet and marshy places, which in the warm season are the constant resort of water fowl. The loftiest summits are Killington Peak, near Rutland; Camel’s Rump, between Montpelier and Burlington, and Mansfield Mountain, a few miles farther north, all which are more than three thousand five hundred feet above the level of the sea. Ascutney, a single mountain near Windsor, is three thousand three hundred and twenty feet in height.
The range called Green Mountains in Vermont, enters the west part of Massachusetts from the north, and forms the Hoosac and Tagkannuc Ridges, which run nearly parallel to each other south, into Connecticut. The most elevated peaks of the Tagkannuc Ridge are Saddle Mountain in the north, four thousand feet high, and Tagkannuc Mountain in the south, three thousand feet. No summits of the Hoosac Ridge much exceed half these elevations. Mount Holyoke, in the neighborhood of Northampton, commands a prospect of the highest beauty; the waters of the Connecticut wind about its base, giving fertility and wealth of vegetation to the surrounding country. On its top a shanty is erected, in which refreshments are kept for the visitors who at favorable seasons make this excursion in great numbers.
There are two distinct chains belonging to the Alleghany range in the state of New York, the Catskill and the Wallkill. The Catskill, which is the most northern, is the continuation of the proper Alleghany or western chain; the eastern is called, by some geographers, Wallkill.
A visit to the Catskill is a favorite excursion of northern travellers, and several days may be spent very agreeably in examining the grand and romantic scenery of the neighborhood. Pine Orchard is a small plain, two thousand two hundred and fourteen feet above the Hudson, scattered with forest trees, and furnished with an elegant house of great size. Immediately below is seen a wild and mountainous region, finely contrasting with the cultivated country beyond, which presents every variety of hill and valley, interspersed with town, hamlet, and cottage.
The hills of Weehawken are on the west side of the Hudson, nearly opposite the city of New York.
Weehawken.
The Highlands of the Hudson, or Fishkill Mountains, which first appear about forty miles from New York, are marked for their sublimity and grandeur, and interesting from their connection with many great events of the revolution. This chain is sixteen miles in width, and extends twenty miles along both sides of the Hudson. The height of the principal has been estimated at one thousand five hundred and sixty-five feet. The Peruvian Mountains consist of a lofty tract in the northern part of New York, being round the sources of the Hudson, and separating the waters of Lake Champlain from those of the St. Lawrence. They received their name from the supposition that they contained mineral treasures. Their loftiest summit, called Whiteface, is about three thousand feet above the level of Lake Champlain.
Highlands.
The Apalachian chain in Pennsylvania spreads to its widest limits, and covers with its various ranges more than one half of the state. The greatest width of the chain equals two hundred miles. It consists of parallel ridges sometimes little distant from each other, and at other times with valleys twenty or thirty miles broad lying between them. The range nearest the coast is called the South Mountain, and is a continuation of the Blue Ridge of Virginia. This, however, is hardly a distinct ridge, but only an irregular series of rocky, broken eminences, sometimes disappearing altogether, and at others spreading out several miles in breadth. These eminences lie one hundred and fifty or two hundred miles from the sea, and their height does not exceed one thousand two hundred feet above the surrounding country. Beyond these are the Kittatinny or Blue Mountains, which extend from Maryland to New Jersey across the Susquehanna and Delaware. Farther westward are the ridges bearing the names of the Sideling Hills, Ragged Mountains, Great Warrior Mountain, East Will’s Mountain, till we come to the Alleghany Ridge, the highest range, and from which this whole chain has in common language received the name of the Alleghany Mountains. The highest summits are between three and four thousand feet above the level of the sea. West of the Alleghany are the Laurel and Chesnut Ridges.
These mountains are in general covered with thick forests. The Laurel Mountains are overgrown on their eastern front with the tree from which they are named. The wide valleys between the great ridges are filled with a multitude of hills, confusedly scattered up and down. The tops of the ridges sometimes exhibit long ranges of table land, two or three miles broad; some of them are steep on one side, and extend with a long slope on the other. These mountains are traversed by the great streams of the Susquehanna chain, and the head-waters of the Ohio.
The Wallkill, which crosses the Hudson at West Point, forty miles below the Catskill, is the continuation of the Blue Ridge, or Eastern Chain, which is the most general appellation for the extensive ridge which fronts the Atlantic. The eastern and western ranges run parallel to each other, south-west, till on the frontiers of North Carolina and Virginia they unite in a knot which has been called the Alleghany Arch, because the principal chain embraces there in a curve all its collaterals from the east. A little farther to the south, but still in North Carolina, a second knot unites all the collateral ridges from the west, and forms a culminating point of heads of rivers. The second bifurcation stretches south-west and then west, and the name of the 2Cumberland Mountains through the whole state of Tennessee, while the proper Alleghany Chain, left almost alone, continues its course to the south-west, and completes the boundary of Georgia and the two Carolinas. From the Alleghany Arch, there are three principal ridges or ramifications of the Alleghany, running north-east and nearly parallel to each other, namely, the Alleghany Proper, the North Mountain, and the Blue Ridge. Of the last ridge the highest summits are the Otter Peaks. The elevated district of South Carolina presents seven or eight mountains running in regular directions, the most distinguished of which is the 3Table Mountain. Mr. Jefferson, with peculiar felicity of illustration, called the range of the Alleghanies the spine of the United States separating the eastern from the western waters, and the whole of the territory from the Mississippi to the Atlantic into three natural divisions, materially differing from each other in climate, configuration, soil, and produce; namely, the coast, the mountains, and the western territory.
In extent, in elevation, and in breadth, the Rocky Mountains far exceed the Alleghanies of the Eastern States. Their mean breadth is two hundred miles, and where broadest, three hundred. Their height must be very great, since, when first seen by Captain Lewis, they were at least one hundred and fifty miles distant. On a nearer approach, the sublimity of the prospect is increased, by the appearance of range rising behind range, each yielding in height to its successor, till the most distant is mingled with the clouds. In this lofty region the ranges are covered with snow in the middle of June. From this last circumstance, these ranges have been sometimes denominated the Shining Mountains—an appellation much more appropriate than that of the Rocky or Stony Mountains, a property possessed by all mountains, but peculiar to none. The longitudinal extent of this great chain is immense, running as far north-west as sixty degrees north latitude, and perhaps to the Frozen Ocean itself. The snows and fountains of this enormous range, from the thirty-eighth to the forty-eighth degree of northern latitude, feed, with never-failing supplies, the Missouri and its powerful auxiliary streams.
