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The Lost River is so-named because the brook draining the southern part of Kinsman Notch disappears below the surface in a narrow, steep-walled glacial gorge. The gorge is partially filled with immense blocks of granite, through the spaces of which the brook cascades along its subterranean course until it eventually emerges and joins the Pemigewasset River, which flows southward from Franconia ...
Hemlock Gorge Reservation is a state-owned, public recreation area and urban wild comprising 23 acres (9.3 ha) on the Charles River in Newton and Needham, Massachusetts. The reservation is managed by the Massachusetts Department of Conservation and Recreation .
The Gorge Amphitheatre, originally known as Champs de Brionne Music Theatre and commonly referred to as The Gorge, is an outdoor concert venue in Grant County, Washington, United States. It is situated near the Columbia River in Central Washington, nine miles (14 km) west of George. The venue is managed by Live Nation.
Today, the gorge continues to be shaped by the East Branch of the Westfield River. The walls of the gorge are quite steep, more than 30 feet (9.1 m) in some places. During periods of low water, it is possible to get down to the floor of the gorge, but it is not recommended, and no trails exist from the cliff edge to the bottom.
The John Botume House, which serves as the park's visitor center View of Boston skyline. Middlesex Fells Reservation, often referred to simply as the Fells, is a public recreation area covering more than 2,200 acres (890 ha) in Malden, Medford, Melrose, Stoneham, and Winchester, Massachusetts, United States.
The Lost River begins on the eastern slopes of Mount Moosilauke below the peak of Mount Jim and above Kinsman Notch, one of the major passes through the White Mountains. As it flows through the notch, it passes through Lost River Gorge , an area where enormous boulders falling off the flanking walls of the notch at the close of the last Ice Age ...
Ausable Chasm is the namesake of the Ausable River, which runs through the gorge and empties into Lake Champlain about one mile (1.6 km) away. The gorge started forming about 10,000 years ago through headward erosion caused by Rainbow Falls, a 91 feet (28 m) waterfall at the gorge's southern extreme. [ 3 ]
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