The Columbian Class book : Consisting of Geographical, Historical And Biographical Extracts

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5. The objects rent asunder are too great, the ruin is too vast, and too coaiplete, to have been accomplished bj these agents. The change appears to have been etfectuat- ed. v;hen the suiface of the earth extensive! j subsided ; vhen countries, and continents, assumed a new fL\ce ; and a general commotion of the elements produced t'ne disruption of some mountains, and merged others be- neath the common level of desolation. Nothing less than this, will account for the sundering of a long range o
...f great rocks ; or rather, ol vast mountains ; or for the existing evidences of the immense force, by Vvhich the rupture wasefiected.
6. The entrance of the chasm is formed bj two rocks, standing perpendicularly at the distance of twenty-two fe^t from each other : one about twentj feet in heio;ht, the other ab;>ut twelve. Half of the space is occupied by th ' brook, mentioned as the head stream of the Saco; the other half by the road. The stream is lost, and invisi- ble, beneath a mass of fragments, partly blown out of the- road, and partly thrown down by some great convulsion.


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