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Balsam Lake Mountain is one of the Catskill Mountains, located in the Town of Hardenburgh, New York, United States. It is the westernmost of the range's 35 High Peaks. Its exact height has not been determined, but the highest contour line on topographic maps, , is usually given as its elevation. Located within the Balsam Lake Mountain Wild Forest management unit of the Catskill Park Forest Preserve, in the late 19th century its summit became the site of the first fire lookout tower in the state, operated by members of a nearby sportsmen's club. It was later taken over by the state's conservation agencies, which built several improved towers on the site, one of which remains, along with its accessory buildings and has been listed on the National Register of Historic Places, although it has not been used for fire detection since 1988. The summit is also the site of a rare sphagnum bog that has been affected by acid rain since a mid-20th century windstorm blew down many of the trees sheltering it at the time. The tower and the views it commands, as well as its ease of access by the old truck road to the tower, have made it a popular attraction for hikers despite the mountain's remote location. Many are peakbaggers aspiring to membership in the Catskill Mountain 3500 Club, for which Balsam Lake is a required peak. ==Geography== Balsam Lake Mountain is in the middle of a long range beginning at Barkaboom Mountain to the west and extending east to Doubletop Mountain. It rises from a base well over on the north and south, with cols over between it and neighboring peaks. Creeks rise in several narrow valleys on all sides, the largest of which is Clark Hollow on the northwest. The steep valley slopes alternate with gentler ridges in between. The summit plateau above is relatively flat, shaped like a large T pointing north, south, and east. On the west, a steep face drops to a shallow col of between Balsam Lake Mountain and the neighboring easternmost summit of Mill Brook Ridge. South of that summit extends Woodpecker Ridge, which with Balsam Lake Mountain and the connecting ridge forms the narrow valley in which the feeder stream to Balsam Lake, the feature the neighboring mountain is named for, rises. Black Brook flows out of the hollow on the southeast, below a more gradual ridge descending from the summit to a low of , where it connects to the and peaks〔 known unofficially as West and East Schoolhouse mountains between Balsam Lake and Graham Mountain, the High Peak two miles (3.2 km) to its east.〔 Mill Brook, which gives the mountain to the west its name, rises from the hollow on the northeast. It is joined by an unnamed tributary which flows into it from Clark Hollow.〔 All the streams that rise on Balsam Lake Mountain are part of the Delaware River's watershed. Mill Brook on the north slopes feeding that river's East Branch directly at Pepacton Reservoir, making it part of New York City's water supply. Water from the southern streams drains into the Beaver Kill not far below the mountain, which itself reaches the East Branch at East Branch well below the reservoir's dam at Downsville. The southern and northwestern portions of the mountain, down to an elevation of in Clark Hollow, are owned by the state. Its Department of Environmental Conservation (DEC) manages the land as part of the Balsam Lake Mountain Wild Forest, which stretches across Mill Brook Ridge and circles back to Beaverkill Road around private lands along Beecher Lake and brook. The northern slope, up to on the summit's northern spur and along the fire tower road, is privately owned by the descendants of railroad baron Jay Gould, who grew up in nearby Roxbury. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Balsam Lake Mountain」の詳細全文を読む スポンサード リンク
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