The most voluminous and among the earliest existing records connected with the River St. Lawrence, and the great lakes which it drains, are the well-known "Relations of the Jesuits," so called, comprising a yearly account of the labors of the Missionary Fathers sent out by the College at Paris to Christianize the Indians. In 1615, they established their mission at Quebec, and from thence extended their operations westward. In 1626, they reached the large and powerful tribe of Indians which occupied the splendid domain which may be described with proximate accuracy as bounded by a line commencing at a point on the southerly shore of Lake Ontario, about thirty miles west of the mouth of the Genesee River, and running thence parallel to that river to a point due west from Avon; thence nearly due west to Buffalo; thence along the north shore of Lake Erie to the Detroit River; thence up that river to a point directly west from the west end of Lake Ontario; thence east to that lake, and finally along the southern shore of it to the place of beginning.
The oldest and most notable name in all this territory is Niagara, as would naturally be inferred, when we consider the varied and wonderful features of the mighty river which flows across this country. Taking leave of Lake Erie, its clear waters gradually spread themselves out in a broad, bright channel, over a plain, open country, having a slight declivity, just sufficient to make a gentle current, thereby adding the living beauty and force of motion to the broad expanse of a lake-like surface, that surface itself diversified and relieved by the pleasant islands, large and small, which are scattered over it. Eddying into every quiet bay, coquetting with every salient angle, moving to the melody of its own murmurs, it flows on serenely and musically.
But after a time this holiday journey is interrupted. A fearful change takes place. The careless waters are hurried down a long and sharp descent, over the rough, denuded, bowlder-studded bed-rock of the stream. Breaking and bounding, surging and resurging, flashing and foaming, rushing fiercely upon some huge bowlder, recoiling an instant, then madly leaping entirely over it, rushing on to others huger still, then breaking wildly around them, the troubled waters hurry on until, culminating in their sublimest aspect, they plunge sheer downward in the grandest of cataracts.
And now the scene and the effect it produces on the beholder both change. The rapids are beautiful; the falls are grand; those are exhilarating, these are inspiring; those are noisy, turbulent, fickle; these are calm, resistless, inexorable.
After the water has made the final plunge over the precipice the cataract acquires its most impressive characteristics; the majestic monotone, the bow, the cloud, which is its veil by night, its crowning glory and beauty by day. The combinations of grandeur and beauty have reached their climax in the fall, the foam, the voice, the spray, the bow.
The Rapids above the Falls
The chasm of the river from the Falls to Lewiston will be sufficiently described in treating of the geology of the district. From Lewiston to Lake Ontario, seven miles, the waters of the river flow on through an elevated and fertile plain, in a strong, calm, majestic current, smiling with dimples and reversed in occasional eddies, but neither broken by rapids nor impeded by islands. Finally it is lost in the lake, after passing an immense bar formed by the enormous mass of sedimentary matter carried down by its own current. The landscape, as seen from the top of the terrace above Lewiston, is one of the finest and most extensive of its peculiar character which can be found on the continent, all its features being such as appertain to a broad, open country.