Day 6 · Sat 4 Jul Via ferrata

Passo San Pellegrino → Rifugio Mulaz

A grassy ridge above Val Venegia, then the stony grind to the Mulaz shelf — hello, Pale di San Martino.

13.4 kmdistance
+1211 mclimb
−546 mdescent
2601 mhigh point
5.5–6.5 hDemanding
Forecast · Saturday 4 JulyRifugio Mulaz area
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Today's elevation — from the GPS track▲ 2601 m
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Gravel roads climb past Lago di Cavia to Passo Valles, then path 751 takes up one of the most scenic ridgelines of the route — high above Val Venegia while the pale ramparts of the Pale di San Martino grow across the sky: Cimon della Pala, the 'Matterhorn of the Dolomites'.

Past Sasso Arduini the grass runs out: a steep 400 m grind on loose Focobon scree (an occasional cable near the top) reaches Passo del Mulaz (2,619 m), then ten minutes down to the hut on its shelf — front-row seats for sunset on the Focobon walls.

Highlights — tap to expand

1Coffee at Passo San Pellegrino ☕
Coffee stopPasso San Pellegrino (1,918 m)

You begin the day on the broad green saddle of Passo San Pellegrino, at roughly 1,918 metres, a working ski pass that carries the road between Moena in the Val di Fassa and Falcade in the Veneto. It is one of the great frontier passes of the Dolomites: it marks the boundary between the autonomous province of Trentino and the province of Belluno, with the long crest of the Costabella rising to the south and the gentler dome of Col Margherita to the north. The name carries real history. It comes from the Pellegrini, the religious order who, in the second half of the 1300s, established a hospice here to shelter pilgrims and travellers crossing the high col in bad weather; that hospice eventually became a hotel, and the tradition of feeding and sheltering strangers on this windswept saddle has, in a sense, never stopped.

Geologically you are standing in a soft, grassy gap between two very different worlds. Behind and around the pass the slopes are largely volcanic and sedimentary, cloaked in pasture and larch, but ahead lie the pale dolomite walls that give the whole range its name. That pale rock is the fossilised remains of Triassic coral reefs and lagoons that grew in a warm, shallow tropical sea called the Tethys some 250 million years ago, later buried, chemically altered into dolomite, and finally heaved skyward when the African and European plates collided. The Dolomites' nine mountain systems were inscribed as a UNESCO World Heritage Site in 2009 for exactly this geological storytelling, and over the coming hours you will walk straight toward one of the most spectacular chapters of it.

2Lunch at Rifugio Passo Valles 🍴
Rifugio Passo Valles (2,032 m)
LunchRifugio Passo Valles (2,032 m)

After climbing through forest past the little tarn of Lago di Cavia and over the grassy Forcella di Pradazzo, you cross the road at Passo Valles, where Rifugio Passo Valles sits squarely on the saddle at about 2,032 metres. The pass is a true watershed and a true border: it separates the great dolomite bulk of the Pala Group to the south from the dark, porphyritic (volcanic) range of Cima Bocche to the north, and it links the Val di Fassa side with the Biois and Primiero valleys of the Veneto. The contrast underfoot is striking, the reddish volcanic rock and rolling pasture of Cima Bocche on one hand, the pale vertical limestone of the Pale beginning to loom on the other.

This is the recognised lunch stop of the day, and a well-earned one. The hut is a sturdy, friendly, road-accessible refuge, the natural place to refuel and gather yourself before the rougher, longer, and much more committing second half of the stage toward the Mulaz shelf. After Passo Valles there is no further shelter and no easy escape until you reach the high terrace at Rifugio Volpi al Mulaz, so this is the moment to eat properly, top up every water bottle, and check the weather, because the afternoon traverse runs across exposed, high ground where an electrical storm would be no joke.

3First view of the Pale
Forcella di Pradazzo / ridge above Val Venegia
ViewForcella di Pradazzo / ridge above Val Venegia

Beyond Passo Valles the route swings onto the high traverse (trail 751) and onto open ground, and the panorama that will define the rest of your trek finally opens all at once. Across the green trough of Val Venegia rises the entire northern rampart of the Pale di San Martino, and it is worth pausing to grasp the scale of what you are seeing. The Pala Group is the largest mountain group in all of the Dolomites, covering some 240 square kilometres between eastern Trentino and the Belluno Veneto. At its heart, hidden behind these peaks, lies one of the most extraordinary landscapes in the Alps: a high rock plateau of roughly 50 square kilometres, an almost lunar desert of bare, pale dolomite undulating between about 2,500 and 2,800 metres, ringed by the spires you are now looking at.

The wall in front of you is built from the pale dolomite rock that gives the whole range its name and its luminous, ghostly colour at dawn and dusk, hence the old local name for these mountains, the Monti Pallidi, the Pale Mountains. That rock began as a Triassic coral reef and carbonate platform in the warm, shallow Tethys Sea some 240 million years ago; buried, chemically transformed into dolomite through the circulation of magnesium-rich waters (a process geologists call dolomitization), and finally thrust thousands of metres into the sky by the collision of the African and European plates. Its sheer hardness is exactly why it erodes into these vertical walls and jagged towers rather than smooth slopes, and why UNESCO inscribed the Dolomites as a World Heritage Site in 2009.

4Ridge above Val Venegia
Forcella Venegia (2,212 m) to Forcella Venegiotta (2,299 m)
ValleyForcella Venegia (2,212 m) to Forcella Venegiotta (2,299 m)

The high route now traverses the grassy crests on the western flank of Val Venegia, crossing the gentle notches of Forcella Venegia at around 2,212 metres and Forcella Venegiotta (Passo di Venegiòta) at about 2,299 metres. The walking here is still kind, climbing along the slopes beneath the pyramidal Cima Valles on open alpine pasture, with the great dolomite wall as a constant companion to your right. These soft, rolling forcelle are the last easy, pastoral ground of the day before the trail tips into the stonier, steeper approach to the Mulaz shelf.

Below to the right the famous green sweep of Val Venegia falls away, and it is one of the most beloved corners of the Dolomites. This is a glacial valley, carved and smoothed by ancient ice, and its broad meadows and grazing cattle run straight toward the foot of the Pale, giving the head of the valley its picture-perfect contrast of emerald grass against pale vertical rock. Through it threads the infant Travignolo stream, fed by the small Travignolo glacier glinting in its cirque between Cimon della Pala and Vezzana high above. The malghe (working dairy huts) of Venegia and Venegiota below still graze cattle and make cheese here through the short alpine summer.

5Cimon della Pala
Cimon della Pala (3,184 m)
ViewCimon della Pala (3,184 m)

Dominating the traverse is Cimon della Pala, the slender 3,184-metre fang long celebrated as the Matterhorn of the Dolomites, il Cervino delle Dolomiti, a comparison popularised by the pioneering English alpinist and writer John Ball for its sharp, isolated, instantly recognisable profile. It is by far the best-known summit of the Pale di San Martino group, and the postcard symbol of the entire range. Curiously, it is not actually the highest peak of the group; its near neighbour Cima Vezzana edges it out at 3,192 metres. But Vezzana is a broad-shouldered bulk, while Cimon della Pala tapers to a needle, and from almost every angle the slimmer Cimon looks the taller and grander of the two. From the ridge above Val Venegia it stands very nearly alone against the sky, a clean pale spire that the eye returns to again and again.

The peak's first ascent is a classic of Dolomite mountaineering. On 3 June 1870 the Englishman Edward Robson Whitwell, with the guides Santo Siorpaes of Cortina d'Ampezzo and Christian Lauener of Lauterbrunnen in the Swiss Bernese Oberland, reached the summit. Earlier attempts had been turned back by a sheer wall on the southern side; Whitwell's insight was to swing around and attack from the north, climbing the steep ice of the Travignolo glacier, the same cirque of remnant ice you can see tucked between Cimon della Pala and Vezzana. The modern normal route is a serious mountaineering objective for experienced climbers, reached via the Bolver-Lugli via ferrata to the Fiamme Gialle bivouac at around 3,005 metres and then up cabled and laddered rock to the top, well beyond the line of the Alta Via.

6Cabled climb to the Mulaz shelf
Rifugio Volpi al Mulaz (2,571 m)
Via ferrataRifugio Volpi al Mulaz (2,571 m)

The final pull is the genuine work of the day. From the high traverse the trail (signpost 751) climbs toward Passo del Mulàz, and the last stretch onto the Mulaz shelf is a steeper, stonier, sometimes loose scramble protected in places by fixed cables, the short Ferrata del Canalino al Mulaz, threaded up a gully through the more exposed rock just below the pass. This is not a full, sustained via ferrata, the wires are intermittent and a harness is not strictly required, but they are genuinely welcome on tired legs and useful handholds where the ground is steep and the rock can be greasy. Take it steadily, mind loose stone underfoot and any walkers below you, and you will top out at Passo del Mulàz (about 2,619 m) with the hut just a few minutes' descent beyond.

The reward is Rifugio Giuseppe Volpi al Mulaz, perched at about 2,571 metres on a high open terrace at the head of the wild Val Focobon, directly beneath the dark pyramid of Monte Mulaz and ringed by the pale spires of the northern Pale. It is a historic refuge with real pedigree. It was built in 1907 on the initiative of the Venice section of the Italian Alpine Club (CAI Venezia), constructed by the local builder Emanuele Murer with land and timber granted by the municipality of Falcade, and inaugurated on 10 September 1907; for the occasion neighbouring Trentino villagers built the approach path from Passo Rolle. The hut is dedicated to Giuseppe Volpi (1877-1947), Count of Misurata, the Venetian industrialist and statesman who founded the Adriatic electricity company SADE and the great industrial port of Marghera; his family funded the hut's enlargement and renovation in 1959-1960.

Where's the coffee?

Coffee — Passo San Pellegrino (1,918 m), the bars and hotels at the road pass where the day begins
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Lunch — Rifugio Passo Valles (2,032 m), the welcoming hut at Passo Valles and the classic break before the harder second half

Watch out for

The Focobon scree to Passo del Mulaz is steep and loose with a possible short cable near the pass. Fill water at Passo Valles — the climb is dry.

Tonight

Rifugio Volpi al Mulaz

2,571 m

CAI Venezia's 1907 stone hut, helicopter-supplied, no road for miles. Dorms, hot meals — and the best sunrise of the trip from the doorstep.

Hut site →
Journal — Day 6 · Sat 4 Jul
Date

To be filled in once we've seen all the awesome, incredible, amazing, exciting, grandiose, breathtaking, jaw-dropping, soul-stirring, once-in-a-lifetime aspects of the Dolomites.

The northern Pale di San Martino & Rifugio Mulaz

Historical things to know

The Pale di San Martino is the largest mountain group of the Dolomites, a vast massif whose interior is occupied by the Altopiano delle Pale — a high, almost lunar rock plateau of roughly 50 km² lying between about 2,500 and 2,700 m. It was once a carbonate reef and lagoon in the Tethys some 200–250 million years ago, the plateau corresponding to the former inner lagoon, later uplifted and stripped by erosion. Its principal summits include Cima della Vezzana (3,192 m) and the iconic pyramid of Cimon della Pala (3,184 m); the northern sector is crowned by Monte Mulaz (about 2,906 m).

The Pale, together with San Lucano, the Dolomiti Bellunesi and the Vette Feltrine, form one of the nine systems of the Dolomites UNESCO site inscribed in 2009. Covering more than 31,000 hectares, it is among the largest and most pristine — both bare high plateau and deep, forested valleys — a landscape famously associated with the writer Dino Buzzati.

Monte Mulaz gives its name to the Rifugio Giuseppe Volpi al Mulaz, at 2,571 m at the Passo del Mulaz at the head of the Val Focobon. The hut was promoted by CAI Venezia and completed in 1907 by the builder Emanuele Murer; the Municipality of Falcade supplied timber from its forests, and the refuge was inaugurated on 10 September 1907, with an access path opened on the Trentino side linking Passo Rolle to the new hut.

The refuge was named for Giuseppe Volpi, Count of Misurata (1877–1947), the Venetian industrialist who founded the electrical utility SADE and the Venice Film Festival — reflecting both CAI Venezia's patronage networks and the era's habit of naming huts for benefactors. Still operated by CAI Venezia, it remains one of the historic refuges of the Pale, more than a century after its founding.

Strategically placed at the junction of the Val Venegia, Passo Valles and Passo Rolle approaches, the Mulaz hut is a classic base for the northern Pale and a key stage of the Alta Via 2. As with much of the range, its surrounding paths and ridges bear the imprint of the 1915–1917 mountain war, when the Pale stood within the Dolomite front of the "White War."

💡 Fun fact

These pale summits were once a warm, shallow sea. The rock is essentially fossilised coral reef, built up on an ocean floor more than 200 million years ago, in the Triassic period.

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