— — the last snow worth climbing for.
“A glacial cirque scooped from the eastern side of Mount Washington, the headwall standing close to 55 degrees in places. In April and May the snow softens through the afternoon and the ravine fills with skiers who hiked four miles in from Pinkham Notch with their boards on their backs. People sit on the rocks at Lunch Rocks and watch the lines come down. Avalanches still close the bowl on bad days. from the studio
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Tuckerman Ravine is a glacial cirque carved into the southeastern face of Mount Washington, in the Cutler River drainage of the White Mountain National Forest. The bowl bottoms at about 4,400 feet and the headwall climbs to roughly 5,400 feet, with sustained pitches between 40 and 55 degrees. The ravine is named for the 19th-century botanist Edward Tuckerman, who studied the alpine flora here in the 1840s. The Forest Service operates the Hermit Lake shelters at the floor of the bowl, and the Mount Washington Avalanche Center posts a daily bulletin through the spring season.
Spring is the Tuckerman season. From April into late May, deep wind-loaded snow softens through the afternoon and skiers and riders hike up the Tuckerman Ravine Trail from Pinkham Notch, 2.4 miles and 1,800 feet to Hermit Lake, then another 0.8 miles into the bowl. Lunch Rocks, the natural stone amphitheatre on the south side, fills with spectators on warm Saturdays. The pilgrimage runs back at least a century, with the first formal ski descents recorded in the 1920s and the first Inferno race held in 1939.
The trailhead is the AMC's Pinkham Notch Visitor Center on Route 16, north of Jackson. The standard approach to the floor of the ravine is the Tuckerman Ravine Trail, 3.2 miles and roughly 2,400 feet of climb to the base of the headwall. Conditions change quickly: warm afternoons trigger crevasses, undermining and ice fall, and avalanche cycles continue into May. Read the daily Avalanche Center bulletin before leaving the parking lot. The bowl is open and unmaintained terrain, not a ski area.