Tuckerman Ravine
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 descentDodge's Drop is a steep descent beside Hillman's Highway, entered from the Boott Spur ridge.
Boott Spur 2
Backcountry descentChute Variation South
Backcountry descentThis Chute variation follows a tight gully beside the main line, requiring turns in a confined passage.
The Icefall
Backcountry descentThe Icefall crosses frozen waterfalls immediately left of the Lip when viewed uphill. Snow coverage determines whether those drops remain exposed.
Left Gully
Backcountry descentLeft 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 descentSluice 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 descentUpper Cutler
Backcountry descentCenter Headwall
Backcountry descentBetween the Lip and Chute, the headwall's ski lines weave through rock outcrops and ice flows. Coverage changes which passages connect.
The Chute
Backcountry descentChute 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 descentRight Gully doglegs above Lunch Rocks before its lower runout.
Lobster Claw
Backcountry descentLobster 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 descentThe 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 descentThis Chute variation narrows into a tight slot, leaving less turning room than the main hourglass line.
The Empress
Backcountry descentTuckerman Ravine Trail
Ski tourThis 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 descentRaymond 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 descentHillman's Highway has two steep upper forks that merge into a longer gully below, south of Tuckerman's main bowl.
Hillmans Highway variation
Backcountry descentLion Head Gully
Backcountry descentThe Lip
Backcountry descentThe 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 descentLittle Headwall is the waterfall step in the drainage between Tuckerman's bowl and the ski return toward the Sherburne.