Canada -- Description and travel; United States -- Description and travel
great Manitou also employed her to manufacture thunder and clouds for
the valley. Sometimes she wove the clouds out of cobwebs, gossamers
and morning dew, and sent them off, flake by flake, floating in the
air, to give light summer showers. Sometimes she would blow up black
thunder-storms and send down drenching rains to swell the streams and
sweep everything away. All these storms coming from the west appeared
to originate in the mountains. The Indians also told of the imps that
haunted their dells, luring the hunters to places of peril. When the
Dutch colonists came along, they sent expeditions into the mountains,
searching for gold and silver, but chiefly found wildcats, causing
them to be named the Kaatsbergs, and from this their present title has
come to be, in time, the Kaatskills or the Catskills.
These attractive mountains are a group of the Alleghenies, having
spurs extending northwest and west, at right angles to the general
trend of the range, thus giving them quite a different form from that
usual in the Allegheny ridges. They assume also more of the abrupt and
rocky character of the Alpine peaks, and instead of the usual folds or
fragments of arches commonly seen elsewhere, the Catskill crags are
masses of piled-up strata in the original horizontal position. They
have a most precipitous declivity facing the east towards the river
valley. Deep ravines, which the Dutch called "Cloves," are cut into
them by the mountain torrents, descending in places in beautiful
cascades, sometimes for hundreds of feet. This aggregation of rocky
cliffs and rounded peaks, and the intersecting gorges and smiling
verdant valleys, have become a great resort for the summer
pleasure-seeker, with myriads of hotels and boarding-places, where it
is said that eighty to a hundred thousand people will go in the
season. Their eastern verge is drained by the Hudson, while the many
brooks and kills flowing out to the westward are gathered into the two
branches that form the Delaware River.
Public-domain text, read in full here on John Shaqi.
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