William Bingley - Travels in North America, From Modern Writers

This division of the great western continent is more than five thousand miles in length; and, in some latitudes, is four thousand miles wide. It was originally discovered by Europeans, about the conclusion of the fifteenth century; and, a few years afterwards, a party of Spanish adventurers obtained possession of some of the southern districts. The inhabitants of these they treated like wild animals, who had no property in the woods through which they roamed. They expelled them from their habitations, established settlements; and, taking possession of the country in the name of their sovereign, they appropriated to themselves the choicest and most valuable provinces. Numerous other settlements have since been established in different parts of the country; and the native tribes have nearly been exterminated, while the European population and the descendants of Europeans, have so much increased that, in the United States only, there are now more than ten millions of white inhabitants.

The surface of the country is extremely varied. A double range of mountains extends through the United States, in a direction, from south-west to north-east; and another range traverses nearly the whole western regions, from north to south. No part of the world is so well watered with rivulets, rivers, and lakes, as this. Some of the lakes resemble inland seas. Lake Superior is nearly 300 miles long, and is more than 150 miles wide; and lakes Huron, Michigan, Erie, Ontario, and Champlain, are all of great size. The principal navigable rivers of America are the Mississippi, the Ohio, the Missouri, and the Illinois. Of these the Mississippi flows from the north, and falls into the Gulf of Mexico. The Ohio flows into the Mississippi: it extends in a north-easterly direction, and receives fifteen large streams, all of which are navigable. The Missouri and the Illinois also flow into the Mississippi: and, by means of these several rivers, a commercial intercourse is effected, from the ocean to vast distances into the interior of the country. Other important rivers are the Delaware and the Hudson , in the United States, and the St. Lawrence , in Canada. The bays and harbours of North America are numerous, and many of them are well adapted for the reception and protection of ships. Hudson's Bay is of greater extent than the whole Baltic sea. Delaware Bay is 60 miles long; and, in some parts, is so wide, that a vessel in the middle of it cannot be seen from either bank. Chesapeak Bay extends 270 miles inland. The Bay of Honduras is on the south-eastern side of New Spain, and is noted for the trade in logwood and mahogany, which is carried on upon its banks.

The natural productions of North America are, in many respects, important. The forests abound in valuable timber-trees; among which are enumerated no fewer than forty-two different species of oaks. Fruit-trees of various kinds are abundant; and, in many places, grapes grow wild: the other vegetable productions are numerous and important. Among the quadrupeds are enumerated some small species of tigers, deer, elks of immense size, bisons, bears, wolves, foxes, beavers, porcupines, and opossums. The American forests abound in birds; and in those of districts that are distant from the settlements of men, wild turkeys, and several species of grouse are very numerous. In some of the forests of Canada, passenger-pigeons breed in myriads; and, during their periodical flight, from one part of the country to another, their numbers darken the air. The coasts, bays, and rivers, abound in fish; and various species of reptiles and serpents are known to inhabit the interior of the southern districts. Among the mountains most of the important metals are found: iron, lead, and copper, are all abundant; and coals are not uncommon.

That part of North America which is under the government of the United States, now constitutes one of the most powerful and most enlightened nations in the world. The inhabitants enjoy the advantage of a vast extent of territory, over which the daily increasing population is able, with facility, to expand itself; and much of this territory, though covered with forests, is capable of being cleared, and many parts of it are every day cleared, for the purposes of cultivation.

The origin of the United States may be dated from the time of the formation of an English colony in Virginia, about the year 1606. Other English colonies were subsequently formed; and, during one hundred and fifty years, these gradually increased in strength and prosperity, till, at length, the inhabitants threw off their dependance upon England, and established an independent republican government. This, after a long and expensive war, was acknowledged by Great Britain, in a treaty signed at Paris on the 30th of November, 1782.

The boundaries of the States were determined by this treaty; but, some important acquisitions of territory have since been made. In April, 1803, Louisiana was ceded to them by France; and this district, in its most limited extent, includes a surface of country, which, with the exception of Russia, is equal to the whole of Europe. Florida , by its local position, is connected with the United States: it belonged to Spain, but, in the year 1820, it was annexed to the territories of the republic.

Geographical writers have divided the United States into three regions: the lowlands or flat country; the highlands, and the mountains. Of these, the first extend from the Atlantic ocean to the falls of the great rivers. The highlands reach from the falls to the foot of the mountains; and the mountains stretch nearly through the whole country, in a direction from south-west to north-east. Their length is about 900 miles, and their breadth from 60 to 200. They may be considered as separated into two distinct chains; of which the eastern chain has the name of Blue Mountains , and the western is known, at its southern extremity, by the name of Cumberland and Gauley Mountains , and afterwards by that of the Alleghany Mountains . The Alleghanies are about 250 miles distant from the shore of the Atlantic. Towards the north there are other eminences, called the Green Mountains and the White Mountains . The loftiest summits of the whole are said to be about 7000 feet in perpendicular height above the level of the sea.

Few countries can boast a greater general fertility of soil than North America. The soil of the higher lands consists, for the most part, of a brown loamy earth, and a yellowish sandy clay. Marine shells, and other substances, in a fossil state, are found at the depth of eighteen or twenty feet below the surface of the ground. Some of these are of very extraordinary description. In the year 1712, several bones and teeth of a vast nondescript quadruped, were dug up at Albany in the state of New York. By the ignorant inhabitants these were considered to be the remains of gigantic human bodies. In 1799 the bones of other individuals of this animal, which has since been denominated the Mastodon or American Mammoth , were discovered beneath the surface of the ground, in the vicinity of Newburgh, on the river Hudson. Induced by the hope of being able to obtain a perfect skeleton, a Mr. Peale, of Philadelphia, purchased these bones, with the right of digging for others. He was indefatigable in his exertions, but was unable, for some time, to procure any more. He made an attempt in a morass about twelve miles distant from Newburgh, where an entire set of ribs was found, but unaccompanied by any other remains. In another morass, in Ulster county, he found several bones; among the rest a complete under jaw, and upper part of the head. From the whole of the fragments that he obtained, he was enabled to form two skeletons. One of these, under the name of mammoth, was exhibited in London, about a year afterwards. Its height at the shoulder was eleven feet; its whole length was fifteen feet; and its weight about one thousand pounds. This skeleton was furnished with large and curved ivory tusks, different in shape from those of an elephant, but similar in quality. In 1817 another skeleton was dug up, from the depth of only four feet, in the town of Goshen , near Chester. The tusks of this were more than nine feet in length.