1844. Proceeding along the northern side of the Karywah of Islamabad, we arrive at the place where the higher ranges begin to descend upon it; and at this spot alone, near the highest end of the valley, the most ungeological would be convinced of its having once contained a lake, as the remains of beaches formed of shingly conglomerate, are to be seen there deposited in horizontal layers, and resting upon distorted lime- stone strata.' But I have before noticed this place, in my general remarks
...made upon entering the valley.
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