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Here is the Berkshire Athenæum, with its excellent public library, where we must stay long enough to glance through the town history, compiled by Mr. J.E.A. Smith. A century and a half ago an unbroken wilderness stretched between the Hoosac and Taconic ranges. The mountains rose by steady degrees from the hills of Connecticut to Mount Mansfield, in Vermont, 4,400 feet above the level of the sea.

Some fifteen miles farther away, in the same direction, appeared the loftier Dome of Taconic, looking blue and indistinct, and hardly so substantial as the vapory sea that almost rolled over it. The nearer hills, which bordered the valley, were half submerged, and were specked with little cloud-wreaths all the way to their tops.

Our southern view at that time, with the clouds and atmospherical hues, is quite indescribable and unimaginable; and the various distances of the hills which lie between us and the remote dome of Taconic are brought out with an accuracy unattainable in summer.

Agassiz says that fishes existed contemporaneously with species of all the invertebrate sub-kingdoms in the Taconic, or sub-Cambrian strata. This is the extreme limit of known geological strata in which life is found to have existed.

On one side the eye follows for the space of an eagle's flight, the serpentine mountain chains, southwards from the great purple dome of Taconic the St.

The epicontinental sea was shoaled and narrowed, and muds were washed in from the adjacent lands. THE TACONIC DEFORMATION. The Ordovician was closed by a deformation whose extent and severity are not yet known. From the St.

Twenty miles of it might have been visible at once, between the windows of Tanglewood and the dome of Taconic, had it been possible to see so far, among the eddying drifts that whitened all the atmosphere. It seemed as if the hills were giants, and were flinging monstrous handfuls of snow at one another, in their enormous sport.

Louis; Ingleside School, Taconic School and the Catherine Aiken School, in Connecticut; Science Hill, at Shelbyville, Kentucky; Ferry Hall, at Lake Forest, Illinois; the El Paso School for Girls; the Lincoln School, in Providence, Rhode Island; Wyoming Seminary, another coeducational school; as well as schools for American girls in Germany, France, and Italy.

The dome of Taconic looks dark, and seems to have no snow on it, though I don't understand how that can be. I saw, a moment ago, on the lake, a very singular spectacle.

As a result of these movements, perhaps several times repeated, a great mountain range was upridged, which has been long since leveled by erosion, but whose roots are now visible in the Taconic Mountains of western New England.