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nt succession, until the peaks vanish in the distant horizon. It is indeed a sublime sight, and may well inspire feelings of deepest reverence for the Power that controls those mighty forces that produced these everlasting hills. Though loth to leave this grand pinnacle, we must not tarry longer upon Greylock. Let us now take a trip down the Housatonic valley, close beside the Taconic range. This forms an almost continuous ridge across the State, and its summit is nearly upon the line between our State and New York. There are no peaks of consequence until we get south of Pittsfield. The range is bold and precipitous on its western side, and fine views may be obtained from almost any part of the ridge. The highest point of the old stage road between Pittsfield and Albany affords a good prospect, though a view from an old road between Hancock and Lanesboro is perhaps more striking. On either side are the valleys of the Hudson and Housatonic, the cities of Albany and Pittsfield, the distant Catskills and the Hoosac range. A little south of Pittsfield is a spur from the Taconic range, parting from it at Egremont. The various portions have received different names--the northern being called Lenox Mountain, the middle Stockbridge Mountain, and the southern Tom Ball. The last named is the highest part of the spur, and is located in the township of Alford. The view from Tom Ball is very fine. A perfect panorama of hills, with handsome towns and villages nestling in the valleys, is spread out before the eyes, while the southern horizon is filled by the giant piles in the township of Mount Washington. Going still further south we find just north-east of Great Barrington a vast mass to which the ugly name of Beartown Mountain was applied by our forefathers. Its altitude is nearly equal to that of the other great hills of Berkshire, but being quite gradual in ascent, and much rounded, does not impress the traveller as much as it might, and there are no peaks from which a good view is obtainable. Just west of this is a hill that deserves mention. It is called Monument Mountain, and was so named because of a great pile of stones found at its southern extremity, and supposed to have been placed there by the aborigines to commemorate some important event. This hill rises only about five hundred feet above the plain, but its eastern side presents an imposing appearance, being an almost perpendicular wall of quartz. From the top there
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