The mountains rise within a mile of the town. They extend westward for twelve miles, lying in two groups, separated by a fine salt-water fiord known as Somes Sound. The park's boundary is exceedingly irregular, with deep indentations of private property. It is enclosed, along the shore, by an excellent automobile road; roads also cross it on both sides of Somes Sound.
There are ten mountains in the eastern group; the three fronting Bar Harbor have been renamed, for historic reasons, Cadillac Mountain, the Flying Squadron, and Champlain Mountain. For the same reason mountains upon Somes Sound have been renamed Acadia Mountain, St. Sauveur Mountain, and Norumbega Mountain, the last an Indian name; similar changes commemorating the early English occupation also have been made in the nomenclature of the western group. Tablets and memorials are also projected in emphasis of the historical associations of the place.
Both mountain groups are dotted with lakes; those of the western group are the largest of the island.
The pleasures, then, of the Lafayette National Park cover a wide range of human desire. Sea bathing, boating, yachting, salt-water and fresh-water fishing, tramping, exploring the wilderness, hunting the view spots—these are the summer occupations of many visitors, the diversions of many others. The more thoughtful will find its historical associations fascinating, its geological record one of the richest in the continent, its forests well equipped schools for tree study, their branches a museum of bird life.
To climb these low mountains, wandering by the hour in their hollows and upon their sea-horizoned shoulders, is, for one interested in nature, to get very close indeed to the secrets of her wonderful east. One may stand upon Cadillac's rounded summit and let imagination realize for him the day when this was a glaciered peak in a mighty range which forged southward from the far north, shoulder upon shoulder, peak upon peak, pushing ever higher as it approached the sea, and extending far beyond the present ocean horizon; for these mountains of Mount Desert are by no means the terminal of the original mighty range; the slow subsidence of the coast has wholly submerged several, perhaps many, that once rose south of them. The valley which now carries the St. Croix River drained this once towering range's eastern slopes; the valley of the Penobscot drained its western slopes.
The rocks beneath his feet disclose not only this vision of the geologic past; besides that, in their slow decay, in the chiselling of the trickling waters, in the cleavage of masses by winter's ice, in the peeling of the surface by alternate freezing and melting, in the dissolution and disintegration everywhere by the chemicals imprisoned in air and water, all of which he sees beneath his feet, they disclose to him the processes by which Nature has wrought this splendid ruin. And if, captivated by this vision, he studies intimately the page of history written in these rocks, he will find it full of fascinating detail.
The region also offers an absorbing introduction to the study of our eastern flora. The exposed bogs and headlands support several hundred species of plants typical of the arctic, sub-arctic, and Hudsonian zones, together with practically all of the common plants of the Canadian zone, and many of the southern coasts. So with the trees. Essentially coastal, it is the land of conifers, the southern limit of some which are common in the great regions of the north, yet exhibiting in nearly full variety the species for many miles south; yet it is also, in its sheltered valleys, remarkably representative of the deciduous growths of the entire Appalachian region.
FRENCHMAN'S BAY FROM THE EAST CLIFF OF CHAMPLAIN MOUNTAIN
Lafayette National Park