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.
Table lands at the foot of the Rocky Mountains.
In endeavoring to explore these Alpine heights, and the sources of the Red and Arkansaw rivers, Captain Pike and his party were bewildered amidst snows, and torrents, and precipices. The cold was so intense, that several of the party had their limbs frostbitten, and were obliged to be abandoned to their fate, by Pike and his surviving companions. In a lateral ridge, separating the valley of the Arkansaw from that of the Platte river, in north latitude forty-one degrees, is a remarkable peak, called the Great White Mountain; so remarkable, indeed, as to be known to all the savage tribes for hundreds of miles round, and spoken of in terms of admiration by the Spaniards of New Mexico, and which formed the boundary of their knowledge to the north-west. The altitude of this peak was taken on the base of a mile by Pike, and found to be ten thousand five hundred and eighty-one feet above the level of the meadow at its foot; and the height of this latter was estimated at eight thousand feet above the level of the sea; in all, eighteen thousand five hundred and eighty-one feet of absolute elevation; being six thousand feet higher than the peak of Teneriffe, by Humboldt’s measurement; or two thousand eight hundred and ninety-one feet short of that of Chimborazo, admitting the elevation of this last to be twenty-one thousand four hundred and seventy-two feet. Captain Pike and his companions never lost sight of this tremendous peak, unless in a valley, for the space of ten weeks, wandering amongst the mountains. What is the elevation at the sources of the Missouri can only be matter of mere conjecture. The level of the river, where they left their canoes, could not be less than six thousand feet above the sea; but how high the mountains rose above this point the narrative does not inform us, and hardly gives us any data to decide. The central chain, as usual, is marked in the map as highest, and covered with snow during the whole year. The latitude is between forty-five and forty-seven degrees; and between these parallels, in Europe, the lower limit of perpetual congelation is fixed at from nine to ten thousand feet above the level of the sea; and it can hardly be supposed that the summits of this snowy range were less than eight thousand five hundred or nine thousand feet high, making a reasonable