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Guidebooks/Mount Washington/Tuckerman Ravine
Waypoint44.2605° N, 71.2924° W

Tuckerman Ravine

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Tuckerman Ravine is the glacier-carved bowl on Mount Washington’s southeast face. Its broad headwall and flanking gullies form the setting for the mountain’s best-known spring skiing. The curved walls and basin are the lasting imprint of glacial erosion.

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22 items

Dodge’s Drop

Backcountry descent

Dodge's Drop is a steep descent beside Hillman's Highway, entered from the Boott Spur ridge.

Boott Spur 2

Backcountry descent

Chute Variation South

Backcountry descent

This Chute variation follows a tight gully beside the main line, requiring turns in a confined passage.

The Icefall

Backcountry descent

The Icefall crosses frozen waterfalls immediately left of the Lip when viewed uphill. Snow coverage determines whether those drops remain exposed.

Left Gully

Backcountry descent

Left Gully is a long, rock-walled couloir in Tuckerman Ravine. The walls constrict the middle of the route, then end at a wider upper opening. A rock buttress separates its mouth from Chute.

The Sluice

Backcountry descent

Sluice is a southeast-facing, convex ski line in Tuckerman Ravine, with an icefall partway down and a runout above Lunch Rocks. Wind-slab fractures can propagate uphill and laterally toward the Lip and the mouth of Right Gully, beyond the skier's immediate position.

Stovepipe

Backcountry descent

Upper Cutler

Backcountry descent

Center Headwall

Backcountry descent

Between the Lip and Chute, the headwall's ski lines weave through rock outcrops and ice flows. Coverage changes which passages connect.

The Chute

Backcountry descent

Chute is a steep, east-facing, funnel-shaped couloir in Tuckerman Ravine. Its shape collects substantial snow above a narrow choke. MWAC identifies the ascent as having no meaningful protected stopping places or escape from an avalanche inside the gully.

Right Gully

Backcountry descent

Right Gully doglegs above Lunch Rocks before its lower runout.

Lobster Claw

Backcountry descent

Lobster Claw is a forked snow gully beneath Lion Head ridge, on the right side of Tuckerman Ravine when viewed uphill.

John Sherburne Ski Trail

Backcountry descent

The Sherburne is the downhill ski return toward Pinkham Notch from the Hermit Lake area. Granite Backcountry Alliance lists 2.4 miles and 1,918 feet of vertical drop, with repeated fall-line turns. Use the Tuckerman Ravine Trail for uphill travel and the Sherburne for downhill travel; GBA specifies no skiing on the Tuckerman Ravine Trail.

Chute North Variation

Backcountry descent

This Chute variation narrows into a tight slot, leaving less turning room than the main hourglass line.

The Empress

Backcountry descent

Tuckerman Ravine Trail

Ski tour

This mapped approach runs from Pinkham Notch through Hermit Lake to the floor of Tuckerman Ravine. Use it for uphill travel, with the John Sherburne Ski Trail as the designated downhill ski return.

Raymond Cataract

Backcountry descent

Raymond Cataract lies north of Lion Head ridge. Its upper bowl funnels into a narrow streambed and cascading waterfall, creating a terrain trap below the skiing. A deep snowpack is needed to cover the waterfall terrain; apparent coverage higher in the bowl does not establish a usable lower exit.

Hillmans Highway

Backcountry descent

Hillman's Highway has two steep upper forks that merge into a longer gully below, south of Tuckerman's main bowl.

Hillmans Highway variation

Backcountry descent

Lion Head Gully

Backcountry descent

The Lip

Backcountry descent

The Tuckerman Ravine Trail passes through the Lip, where the slope steepens over a convex rollover toward the ravine floor. Seeing Hermit Lake below does not make this a straightforward descent: snow-covered trail terrain here can require mountaineering equipment and skills.

Little Headwall

Backcountry descent

Little Headwall is the waterfall step in the drainage between Tuckerman's bowl and the ski return toward the Sherburne.