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Various

"The Bay State Monthly, Volume 3, No. 5"

"It would not be surprising," he says, "if this
archipelago covered as much area as New Hampshire and Vermont combined."
If these hoary old mountains could tell us their history since creation,
how short-lived and insignificant our own little lives would appear!
Professor Hitchcock has also traced the course of glacial drift among
the mountains in a most interesting manner. Glacial action, and marks of
scarification are numerous on the north and west sides of them while
they are entirely wanting on the southeastern slopes. In some instances
the general course of the drift from the northwest was changed by the
position of the mountains. For instance, Ragged Mountain and Kearsarge,
South, rise abruptly from comparatively level regions and from their
proximity to each other gave rise to a different motion of the ice, the
marks of which still show its course.
The view from this, the oldest of the mountains is scarcely surpassed by
any in the state. To the north, Moosilauke, Chocorua, Lafayette, Mount
Washington and the main peaks of the principal White Mountain group lie
sharply outlined.


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