description Tuckerman Ravine Overview
Tuckerman Ravine is a prominent glacial cirque located on the eastern slopes of Mount Washington in the White Mountains of New Hampshire. The geographic formation is characterized by a steep, bowl-shaped headwall carved by glacial activity, which frequently accumulates deep snowpack. It is historically recognized as a significant location for extreme backcountry skiing and mountaineering, particularly during the spring when skiers hike into the bowl to descend its steep terrain. The area is managed by the US Forest Service and contains several smaller sub-bowls and technical ice climbing routes.
help Tuckerman Ravine FAQ
Where is Tuckerman Ravine located?
Tuckerman Ravine is a prominent glacial cirque located on the eastern face of Mount Washington in New Hampshire, USA. Mount Washington is notoriously famous for having some of the most severe and extreme weather conditions on Earth.
Why is Tuckerman Ravine famous for backcountry skiing?
The ravine is famous for its extreme spring backcountry skiing, drawing thousands of thrill-seekers every year. Skiers literally hike up the steep, snow-filled bowl to carve turns down incredibly steep pitches like the infamous Headwall.
What are the dangers of visiting Tuckerman Ravine?
The area is notorious for severe avalanche danger, sudden weather changes, and deep crevasses known as bergschrunds that open up in the snowpack. Rescues in the steep, icy terrain are highly complex and require specialized mountaineering teams.
What is the annual spring tradition at Tuckerman Ravine?
Every spring, the ravine hosts an infamous adventure race called the Tuckerman Inferno. Furthermore, thousands of spectators gather at the 'Lunch Rocks' in April simply to watch extreme skiers tackle the towering, near-vertical headwall.
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