Cimon della Pala

Cimon della Pala

Cimon della Pala is the most famous summit of the Pale di San Martino, rising to approximately 3,185 meters (10,449 feet) in the Italian Dolomites. Its slender pyramidal profile dominates the view from Passo Rolle and has earned it the enduring nickname “Matterhorn of the Dolomites” — Il Cervino delle Dolomiti.

Although nearby Vezzana is slightly higher, Cimon della Pala has become the visual symbol of the entire mountain group. Its steep southwest walls tower above San Martino di Castrozza, while the Travignolo basin separates it from Vezzana on the north.

The mountain also occupies a central place in Dolomite mountaineering history. Edward Robson Whitwell, Santo Siorpaes, and Christian Lauener made the first recorded ascent on June 3, 1870, climbing the dangerous northern side above the Travignolo Glacier. Their success helped trigger an extraordinary period of exploration in the Pale di San Martino.

Today, Cimon della Pala remains a genuine mountaineering summit. The popular Bolver-Lugli via ferrata provides access to the high shoulder and Bivacco Fiamme Gialle, but reaching the actual summit requires additional exposed rock climbing. This is not a mountain that can be reached by an ordinary hiking trail.

⚡ Fast Facts

Feature	Details
Mountain	Cimon della Pala
Also called	Cimone
Nickname	Matterhorn of the Dolomites / Cervino delle Dolomiti
Country	Italy
Province	Trento
Region	Trentino-Alto Adige/Südtirol
Mountain group	Pale di San Martino
Greater range	Dolomites / Eastern Alps
Modern LiDAR elevation	Approx. 3,185 m / 10,449 ft
Traditional elevation	3,184 m / 10,446 ft
Prominence	Approx. 257 m / 843 ft
Isolation	Approx. 0.83 km / 0.51 mi
Key saddle	Approx. 2,928 m / 9,606 ft
Parent peak	Vezzana
Nearest Higher Neighbor (NHN)	Vezzana
Coordinates	Approx. 46.2853° N, 11.8216° E
Pale di San Martino rank	2nd-highest major summit
Rock	Dolomite and related carbonate rock
Geologic age	Primarily Triassic
Protected area	Paneveggio–Pale di San Martino Natural Park
UNESCO status	Part of the Dolomites World Heritage Site
Major neighboring peak	Vezzana
Nearby summit	Cima dei Bureloni
Nearby mountain	Cima di Focobon
Nearby hiking summit	Cima della Rosetta
Nearby major massif	Pala di San Martino
First recorded ascent	June 3, 1870
First ascenders	Edward Robson Whitwell, Santo Siorpaes and Christian Lauener
First-ascent route	North side via Travignolo Glacier
Modern normal route established	July 9, 1889
Normal-route pioneers	Ludwig Darmstädter, Luigi Bernard and Johann Niederwieser “Stabeler”
Normal-route difficulty	Approx. UIAA III / III+
Major via ferrata	Bolver-Lugli
High shelter	Bivacco Fiamme Gialle
Bivouac elevation	3,005 m / 9,859 ft
New bivouac installed	2025
Major historic face	Southwest Face
Famous early route	Leuchs Route, 1905
Known for	Matterhorn-like profile, first major ascent of the Pale, classic Dolomite scenery

Modern LiDAR gives the summit approximately 3,185 meters, one meter above the traditional 3,184-meter figure. Peakbagger also gives 257 meters of prominence and 0.83 kilometer of isolation, with higher terrain reached toward Vezzana.

📍 Where Is Cimon della Pala?

Cimon della Pala rises in the northern portion of the Pale di San Martino, immediately above San Martino di Castrozza and Passo Rolle.

Its location helps explain its extraordinary fame.

From Passo Rolle, the mountain presents a narrow, sharply pointed profile that resembles a much more isolated peak. Vezzana rises immediately behind and north of it, but much of that larger mountain is hidden from the classic western viewpoint.

This perspective creates the illusion that Cimon stands almost alone.

To the northeast lie Cima dei Bureloni and the northern Pale.

To the south, the range continues toward Pala di San Martino, Cima di Fradusta, Sass Màor, and Cima della Madonna.

🏔️ Second-Highest Peak of the Pale di San Martino

Cimon della Pala is the second-highest major summit of the Pale di San Martino.

The highest is Vezzana, which reaches approximately 3,192 meters.

Cimon follows at roughly 3,184–3,185 meters.

Cima dei Bureloni comes next at approximately 3,130 meters.

The difference between Vezzana and Cimon is therefore only about seven or eight meters.

For many years, early maps actually suggested that Cimon della Pala was the higher mountain.

That misunderstanding influenced the earliest mountaineers who came to the Pale.

📏 Modern Elevation

The traditional published elevation of Cimon della Pala is 3,184 meters.

Modern LiDAR-based measurements refine the natural summit to approximately:

3,185.0 meters / 10,449 feet

This slight difference is normal when newer point-cloud measurements replace older surveying methods.

Both figures remain useful.

Regional tourism authorities, historical climbing literature, and many maps continue to use 3,184 meters, while modern topographic databases may use 3,185.

📊 Prominence and Isolation

Cimon della Pala has approximately 257 meters (843 feet) of topographic prominence.

Its key saddle lies at approximately 2,928 meters.

The mountain’s topographic isolation is only around:

0.83 kilometer / 0.51 mile

Higher terrain is reached toward Vezzana.

These figures illustrate an interesting contrast.

Cimon appears extremely independent from Passo Rolle, yet in strict topographic terms it is closely connected to Vezzana.

Its visual dominance comes primarily from steep relief and perspective rather than enormous prominence.

🧭 Vezzana: The Nearest Higher Neighbor

Vezzana rises immediately northeast of Cimon della Pala.

At approximately 3,192 meters, it is the highest summit in the Pale di San Martino.

The two peaks are separated by the high terrain around Passo del Travignolo and the upper Travignolo basin.

From the north, their physical relationship becomes much clearer than from the famous western viewpoint.

Topographically, Vezzana is both Cimon della Pala’s parent peak and its Nearest Higher Neighbor.

Historically, however, Cimon received far more attention.

Its striking silhouette caused early visitors and cartographers to believe that it was the dominant high point of the entire group.

🏔️ The “Matterhorn of the Dolomites”

Cimon della Pala is widely known as the Matterhorn of the Dolomites.

The comparison refers particularly to the view from Passo Rolle.

From that direction, the mountain rises as a narrow rock pyramid with steep faces on both sides, strongly recalling the outline of the Matterhorn in the Pennine Alps.

The British mountaineer and Alpine writer John Ball is traditionally credited with popularizing the comparison.

The nickname endured because it captures something important about the mountain.

Cimon is not the highest peak around it, but from its most famous viewpoint it possesses exactly the sort of isolated, elegant profile associated with iconic mountains.

🏷️ Where the Name Comes From

The name Cimon della Pala can be understood through local geography.

Cimon or Cimone refers to a great or prominent summit.

The second part is associated with the Pala Monda, a steep grassy slope beneath the southwest side of the mountain.

The complete name therefore developed from the mountain’s relationship with this lower feature rather than from the entire Pale di San Martino group.

Local Primiero dialect also uses forms such as el Zimon.

Over time, Cimon della Pala became the internationally recognized name.

🪨 Geology of Cimon della Pala

Cimon della Pala is built largely from thick beds of Triassic dolomite, particularly the massive carbonate rocks that form the characteristic towers and cliffs of the Pale di San Martino.

Its geological story began more than 200 million years ago.

At that time, the region was covered by tropical seas.

Large carbonate platforms developed in shallow water, separated by deeper marine basins.

Sediment accumulated over enormous periods.

Marine organisms, chemical precipitation, and reef-like communities all contributed to the formation of thick carbonate deposits.

Later chemical alteration introduced magnesium, transforming portions of limestone into dolomite.

🌊 A Mountain Born Underwater

Nothing about the modern appearance of Cimon della Pala suggests a tropical sea.

Yet its enormous cliffs are essentially remnants of ancient marine environments.

The rock forming the summit was deposited long before the Alps existed.

During the Triassic, carbonate platforms built upward through shallow seas while deeper basins accumulated different sediments.

The Pale di San Martino preserve these relationships exceptionally well.

Their vertical walls expose enormous sections through what were once submarine environments.

This geological preservation is one reason the Dolomites have such international scientific importance.

🌋 Ancient Volcanic Activity

The Triassic landscape was not purely carbonate.

Volcanic activity also affected the region.

Submarine eruptions and igneous processes produced volcanic deposits between and around the carbonate platforms.

These contrasting rock types influenced later erosion.

Different layers weathered at different rates, helping create the sharp transitions between cliffs, ledges, valleys, and plateaus visible throughout the Pale.

Cimon della Pala therefore belongs to a mountain landscape created by an interaction between marine sedimentation, volcanism, tectonic uplift, and erosion.

🌎 Raising the Dolomites

The rocks remained beneath later sediments for millions of years.

The modern Alps began developing when tectonic collision compressed the region.

Ancient marine strata were uplifted, faulted, fractured, and carried thousands of meters above sea level.

Once exposed, erosion began removing enormous quantities of rock.

Rivers cut valleys.

Rainwater entered cracks.

Freeze-thaw cycles widened fractures.

Gravity pulled loosened blocks from cliffs.

Glaciers later intensified the process during the Ice Age.

The famous pyramid of Cimon della Pala is therefore the eroded remnant of a much larger ancient rock mass.

🧊 Travignolo Glacier

The Travignolo Glacier lies between Cimon della Pala and Vezzana on their northern side.

Historically, the glacier was much more substantial than the remnant ice and snow terrain visible today.

It played a central role in the first ascent.

Whitwell, Siorpaes, and Lauener approached across the Travignolo Glacier before climbing the steep northern rocks of Cimon.

The glacier also feeds the Travignolo stream, which flows north and west from the Pale.

Like most small glaciers in the Dolomites, Travignolo has undergone major retreat during the modern warming period.

The surrounding terrain increasingly consists of exposed rock, moraine, seasonal snow, and shrinking permanent ice.

🧊 Ice Age Glaciation

The present Travignolo ice is only a tiny remnant of the glaciers that once occupied the Pale di San Martino.

During the Pleistocene, large glaciers filled valleys throughout the massif.

Moving ice carved deep troughs, excavated cirques, steepened cliffs, and removed enormous quantities of rock.

Passo Rolle and the surrounding valleys retain strong evidence of this glacial history.

When the ice retreated, it left behind moraine, polished rock, glacial basins, and the dramatic vertical relief that now frames Cimon della Pala.

📜 Early Exploration of the Pale

The Pale di San Martino began attracting foreign travelers during the nineteenth century.

British visitors played a particularly important role.

Josiah Gilbert and George Cheetham Churchill reportedly became fascinated by an image of Cimon della Pala they saw in 1862 and later traveled through the region.

Their writings helped introduce the Dolomites to a wider English-speaking audience.

Douglas Freshfield, Francis Fox Tuckett, Leslie Stephen, John Ball, and other major figures of early Alpine exploration soon followed.

For mountaineers, one question quickly became unavoidable:

Could Cimon della Pala be climbed?

🧗 Paul Grohmann’s Attempt

Austrian mountaineering pioneer Paul Grohmann attempted to find a route toward the summit before the successful first ascent.

He explored the mountain from the side of Val dei Cantoni and the Pale plateau.

A major rock barrier eventually stopped the attempt.

Other climbers investigated similar terrain.

The problem was not merely technical climbing difficulty.

Early mountaineers had no detailed route descriptions and could not see many of the mountain’s hidden ledges and weaknesses from below.

Finding a possible line was itself a major challenge.

🧗 Whitwell’s Failed Attempt

Edward Robson Whitwell also initially tried the Val dei Cantoni side.

On May 27, 1870, Whitwell and Francis Fox Tuckett explored the mountain with guides but failed to find a passage through the cliffs.

Rather than abandon the objective, Whitwell reconsidered the mountain.

He eventually concluded that the less obvious northern side above the Travignolo Glacier might provide a route.

That decision changed the history of the Pale di San Martino.

📜 First Recorded Ascent

On June 3, 1870, Edward Robson Whitwell set out with two outstanding mountain guides:

• Santo Siorpaes, from Cortina d’Ampezzo
• Christian Lauener, from Lauterbrunnen, Switzerland

They climbed the Travignolo Glacier and then attacked the northern face.

The terrain involved steep rock, snow, ice, and significant rockfall danger.

After working through the complex upper mountain, they reached the summit at approximately 11:00 in the morning.

Whitwell left a written record of the ascent.

That contemporary evidence firmly establishes June 3, 1870 as the date of the first summit climb.

🏔️ They Thought It Was the Highest Peak

The first ascenders believed they might have conquered the highest mountain of the Pale di San Martino.

From many viewpoints, that assumption is understandable.

Cimon appears taller and more dominant than Vezzana.

Maps of the era also contained inaccurate elevation information.

The misunderstanding lasted only two more years.

In 1872, Douglas Freshfield and Charles Comyns Tucker climbed Vezzana and helped establish that it was actually the higher summit.

Cimon nevertheless remained the more famous mountain.

🧗 The Original North Route

The first-ascent route crossed the Travignolo Glacier and climbed the north side.

It is rarely used today.

The reasons are significant.

Rock on the northern side can be unstable, and rockfall has long been recognized as a major hazard.

Changes in glacier and snow conditions have also altered the character of the approach.

Modern climbers generally prefer routes from the south and southeast, where the rock and access are more suitable.

The original line remains historically fascinating but is no longer the standard way to climb the mountain.

🧗 The Modern Normal Route

The modern normal route was established on July 9, 1889 by:

• Ludwig Darmstädter
• Luigi Bernard
• Johann Niederwieser, known as Stabeler

Their route found a more practical line on the eastern or southeastern side of the mountain.

The normal route generally reaches around UIAA Grade III, with some descriptions using III+ for the harder passages or variations.

Although modest by modern rock-climbing standards, the route remains exposed and Alpine in character.

It requires genuine climbing ability, route finding, and experience descending technical rock.

🧗 The Summit Is Not a Via Ferrata Hike

One important distinction is often overlooked.

The Bolver-Lugli via ferrata does not by itself reach the summit of Cimon della Pala.

The protected route climbs the mountain’s southwest side and reaches the high shoulder near the Bivacco Fiamme Gialle.

From there, reaching the actual 3,185-meter summit requires additional alpine rock climbing.

This summit section is often called the Variante per la Vetta.

It is only partly equipped and requires climbing experience.

Hikers who are comfortable on via ferratas but lack independent rock-climbing skills should not assume that completing Bolver-Lugli automatically makes the summit appropriate.

🧗 Via Ferrata Bolver-Lugli

The Via Ferrata Bolver-Lugli, also called the Ferrata del Cimone, is one of the classic protected routes of the Pale di San Martino.

It climbs the southwest side of Cimon della Pala toward the high shoulder at approximately 3,000 meters.

The route involves roughly 700 meters of equipped climbing and around 1,000 meters of total ascent depending on the starting point.

Regional tourism information classifies the route as difficult and suitable for experienced via ferrata users.

It was created to celebrate the centenary of the 1870 first ascent and was later extensively renovated.

The combination of altitude, exposure, length, and weather makes the route more serious than a simple technical grade might imply.

🏠 Bivacco Fiamme Gialle

The Bivacco Fiamme Gialle stands at approximately 3,005 meters on the high southern shoulder of Cimon della Pala.

The original bivouac was installed in the late 1960s and became one of the best-known emergency shelters in the Pale.

In October 2025, a completely new structure was installed to replace it.

The modern bivouac continues to provide emergency shelter along the high route toward Cimon and the Travignolo area.

The original historic structure was removed from the mountain and transferred to the MUSE science museum in Trento, where it became part of an exhibition about mountains, science, environmental change, and human experience.

🚨 The Bivouac Is Not an Easy Destination

The presence of a modern shelter should not create the impression that Bivacco Fiamme Gialle is easily accessible.

Reaching it via Bolver-Lugli requires a serious high-altitude via ferrata.

Recent mountain-rescue warnings have emphasized that visitors attracted primarily by photographs of the new bivouac sometimes underestimate the difficulty of reaching it.

The shelter should be regarded as part of a demanding Alpine route, not as an ordinary hiking attraction.

Weather, snow, ice, altitude, and exposure can all transform the journey quickly.

🏠 Rifugio Rosetta Approach

Another approach to the high Cimon area begins from Rifugio Rosetta – Giovanni Pedrotti, at approximately 2,578–2,581 meters.

The refuge sits near the western edge of the Pale plateau.

From there, experienced mountaineers can travel toward Passo Bettega and Val dei Cantoni, eventually reaching Passo del Travignolo and the Bivacco Fiamme Gialle area.

The SAT lists Cimon della Pala as approximately 3½ hours from Rifugio Rosetta, noting that the final portion is difficult.

This approach avoids the Bolver-Lugli ferrata but still enters serious Alpine terrain.

🏜️ The Pale Plateau

South and east of Cimon della Pala spreads the extraordinary Altopiano delle Pale di San Martino.

The plateau covers roughly 50 square kilometers.

Its barren landscape contrasts dramatically with the green valleys below.

Pale carbonate rock dominates the terrain.

Vegetation is sparse.

Karst depressions, scree, snow patches, and rocky basins create a landscape often compared with the surface of another planet.

Cima della Rosetta provides relatively easy access to this high landscape, while Cimon della Pala rises as one of its most dramatic western boundary peaks.

🧗 Northwest Ridge

The northwest ridge became another classic early route.

Gilberto Melzi and Giuseppe Zecchini climbed it in 1893.

The route follows the long ridge descending toward the Passo Rolle side of the mountain.

Its profile is one of the most obvious features visible from below.

Although once more frequently climbed, it now receives relatively limited traffic compared with the normal route.

The climb nonetheless represents another important stage in the development of Cimon della Pala as a mountaineering mountain.

🧗 Georg Leuchs and the Southwest Face

In 1905, German climber Georg Leuchs completed a remarkable solo ascent of the great southwest face.

The route represented an extraordinary achievement for the period.

Modern descriptions give approximately 1,000 meters of climbing, with difficulty reaching around UIAA Grade V on some sections.

Leuchs had to identify a path through the enormous wall without modern protection, detailed guidebooks, or reliable communication.

The route remains a historic achievement in Dolomite climbing.

🧗 The Andrich Route

The southwest wall attracted increasingly strong climbers during the twentieth century.

In 1934, Alvise Andrich and Furio Bianchet established another major route on the face.

The climb pushed difficulty substantially beyond the early classical routes.

Andrich belonged to the generation that transformed Dolomite climbing during the interwar years.

Routes became more direct, steeper, and technically demanding.

The immense southwest face of Cimon provided an ideal arena for this new style.

🧗 Direttissima Fiamme Gialle

Another major line is the Direttissima Fiamme Gialle, established during the 1960s.

The route takes a direct path through steep sections of the southwest wall.

Early ascents relied more heavily on aid climbing, while later climbers have repeated much of the terrain free.

The route’s name reflects the long association between Cimon della Pala and the Fiamme Gialle, Italy’s Guardia di Finanza mountain organization.

The relationship is also represented by the high bivouac and the nearby Alpine training school.

🛡️ Cimon della Pala and the Guardia di Finanza

Cimon della Pala has an unusual institutional connection with the Guardia di Finanza.

The mountain appears in the organization’s heraldic imagery and has long been associated with its Alpine training and rescue traditions.

The Fiamme Gialle section of the Club Alpino Italiano maintains the high bivouac on the mountain.

This connection adds a distinctive human-history element to Cimon.

Few Dolomite peaks are as strongly associated with a modern public institution.

🌄 Passo Rolle

The classic view of Cimon della Pala comes from Passo Rolle, at approximately 1,980 meters.

From the pass and nearby Baita Segantini, the mountain rises as an elegant rock pyramid.

Vezzana is largely hidden behind it, enhancing Cimon’s apparent independence.

This view has appeared in countless photographs, guidebooks, paintings, tourism campaigns, and calendars.

It is one of the defining visual images of the Italian Dolomites.

Even visitors with no interest in climbing can experience Cimon della Pala at its most dramatic from the Passo Rolle region.

🌄 Enrosadira

Cimon della Pala also participates spectacularly in the Dolomite phenomenon known as enrosadira.

At sunrise and sunset, low-angle light can turn the pale mountain walls shades of yellow, orange, pink, and red.

The effect is especially impressive from Passo Rolle.

The pointed summit can remain illuminated after the lower landscape has fallen into shadow.

Cloud and atmospheric conditions change the colors from day to day.

This interaction between carbonate rock and evening light contributes strongly to Cimon’s iconic status.

🌍 UNESCO World Heritage Site

Cimon della Pala forms part of The Dolomites UNESCO World Heritage Site, inscribed in 2009.

It lies within the large component containing the Pale di San Martino, San Lucano, Dolomiti Bellunesi, and Vette Feltrine.

The protected component covers more than 31,000 hectares.

UNESCO recognizes the Dolomites for exceptional scenic beauty and geological significance.

Cimon perfectly expresses both qualities.

Its steep walls and pointed profile create extraordinary scenery, while the rocks preserve evidence of ancient Triassic carbonate platforms and the geological processes that built the Dolomites.

🏞️ Paneveggio–Pale di San Martino Natural Park

Cimon della Pala lies within Paneveggio–Pale di San Martino Natural Park.

The park protects a landscape stretching from forested valleys to high rock summits.

Lower elevations contain conifer forests and Alpine meadows.

Higher slopes support increasingly sparse vegetation.

Near the summit, almost everything becomes bare rock.

The protected area also encompasses much of the Travignolo watershed and the western Pale plateau.

Preserving such a broad elevation range protects not just individual mountain landmarks but entire connected ecosystems.

🌿 Flora and Fauna

The upper mountain supports little vegetation because of the combination of altitude, cold, wind, steep rock, and unstable debris.

Lower terrain is much richer.

The Pale plateau supports specialized high-elevation plants including saxifrages, gentians, potentillas, rampions, yellow Alpine poppies, and edelweiss where suitable soil exists.

Forests lower on the mountain include spruce, larch, fir, and stone pine.

The broader natural park supports chamois, Alpine ibex, red deer, roe deer, marmots, golden eagles, ptarmigan, Alpine choughs, and numerous smaller species.

🐐 Chamois and Ibex

Chamois are particularly well adapted to the cliffs and broken slopes of the Pale.

Their specialized hooves provide excellent grip on steep rock.

Alpine ibex have also been reintroduced to the broader protected landscape.

Both species can move through mountain terrain far more confidently than humans.

Wildlife should never be approached closely or forced away from preferred routes, particularly where cliffs limit escape options.

🦅 Golden Eagles

Golden eagles use the high cliffs and valleys of the Pale di San Martino.

The enormous walls around Cimon provide ideal soaring conditions.

Air heated by the sun rises along the rock, allowing eagles to gain height with relatively little effort.

From Passo Rolle, the Pale plateau, and neighboring trails, patient observers may occasionally see these large raptors circling above the mountains.

🌩️ Weather and Mountain Conditions

Weather can change rapidly around Cimon della Pala.

Thunderstorms are an important summer hazard.

Lightning is particularly dangerous on via ferrata cables, summit ridges, and exposed rock faces.

Fog creates serious navigation problems in Val dei Cantoni and around Passo del Travignolo.

Snow can remain well into summer at high elevations.

Even during apparently warm periods, fresh snow, hail, or freezing conditions are possible above 3,000 meters.

Anyone climbing Cimon should treat the forecast as a major part of route planning.

⚠️ Mountaineering Safety

Cimon della Pala is not an ordinary hiking summit.

Major hazards include:

• Exposed rock climbing
• Difficult via ferrata terrain
• Long approaches
• Rockfall
• Loose Dolomite rock
• Snow and ice
• Thunderstorms
• Lightning
• Fog
• High winds
• Route-finding difficulties
• Complicated descent
• Altitude
• Limited water
• Remote rescue conditions

The Bolver-Lugli via ferrata requires proper equipment and experience.

Continuing from the bivouac to the summit requires additional climbing skills.

Less experienced visitors should consider climbing with a qualified mountain guide.

🏔️ Cimon della Pala and Vezzana

Cimon della Pala and Vezzana form one of the most interesting pairs in the Dolomites.

Vezzana is higher.

Cimon is more famous.

Vezzana has a comparatively broad profile.

Cimon appears as a dramatic pyramid.

Topographically, Vezzana is Cimon’s parent and nearest higher neighbor.

Historically, Cimon was climbed first because early mountaineers mistakenly believed it was the highest mountain of the group.

Together, they dominate the northern Pale.

🏔️ Cimon della Pala and Cima dei Bureloni

Cima dei Bureloni rises northeast of Cimon to approximately 3,130 meters.

Bureloni is the third-highest major summit of the Pale.

Its huge northwest wall gives it a much broader and heavier appearance.

Cimon, by contrast, is defined by its pointed silhouette.

The two mountains are especially impressive when seen from Val Venegia and the Passo Rolle region.

🏔️ Cimon della Pala and Cima di Focobon

Cima di Focobon stands farther northeast at approximately 3,054 meters.

Focobon forms a complicated fortress of towers and pinnacles.

Its architecture is very different from Cimon’s cleaner pyramid.

Both mountains require genuine mountaineering.

Together with Bureloni and Vezzana, they create one of the most spectacular high chains in the Dolomites.

🏔️ Cimon della Pala and Monte Mulaz

Monte Mulaz rises farther north to approximately 2,906 meters.

Mulaz is substantially lower and easier to reach.

Experienced hikers can climb its normal route without sustained technical rock climbing in favorable conditions.

That makes Mulaz a useful alternative for visitors who want a summit experience and outstanding views of Cimon della Pala without undertaking technical mountaineering.

🏔️ Cimon della Pala and Pala di San Martino

Pala di San Martino rises south of Cimon to approximately 2,982 meters.

Although lower, it has greater topographic prominence and enormous western walls.

Both mountains played important roles in the earliest exploration of the Pale.

Cimon was first climbed in 1870.

Pala di San Martino followed in 1878 after years of attempts.

Together they helped establish San Martino di Castrozza as one of the great historical centers of Dolomite mountaineering.

🏔️ Cimon della Pala and Cima della Rosetta

Cima della Rosetta lies southeast of Cimon and reaches approximately 2,743 meters.

Rosetta is dramatically easier to access because the cable-car system climbs close to the high plateau.

From Rosetta and Rifugio Pedrotti, hikers receive excellent views toward Cimon, Vezzana, and the northern Pale.

The contrast is striking.

Rosetta provides an accessible introduction to the high Dolomites.

Cimon remains a serious mountaineering summit requiring technical skill.

🌄 Why Cimon della Pala Stands Out

Cimon della Pala is not the highest mountain of the Pale di San Martino, yet it became the mountain that represents them.

Its 3,185-meter summit, approximately 257 meters of prominence, and modest 0.83-kilometer isolation cannot fully explain its fame.

The answer lies in shape and position.

From Passo Rolle, Cimon rises as an almost perfect rock pyramid. Vezzana disappears largely behind it, making the mountain look dramatically independent. The resulting silhouette inspired the nickname Matterhorn of the Dolomites and became one of the defining images of northern Italy.

Its geological story stretches back more than 200 million years to Triassic tropical seas.

Its mountaineering story is equally remarkable.

Whitwell, Siorpaes, and Lauener climbed the dangerous northern side on June 3, 1870, launching a new era of exploration in the Pale. Darmstädter, Bernard, and Stabeler found the modern normal route in 1889. Later climbers explored the northwest ridge, southwest wall, and increasingly difficult direct lines.

That tradition continues today.

The Bolver-Lugli via ferrata brings experienced climbers to the spectacular high shoulder and the modern Bivacco Fiamme Gialle, replaced with a new structure in 2025. Beyond it, the final summit still demands real alpine climbing.

For anyone exploring the mountains of Italy, Cimon della Pala represents the Dolomites at their most characteristic: pale rock, enormous vertical relief, pioneering mountaineering history, changing glaciers, dramatic light, and a summit profile that is almost impossible to forget.

🔗 Related Articles

• Vezzana
• Cima dei Bureloni
• Cima di Focobon
• Monte Mulaz
• Pala di San Martino
• Cima di Fradusta
• Cima della Rosetta
• Sass Màor
• Cima della Madonna
• Mountains in Italy

📚 Sources

• Peakbagger — Cimon della Pala
• Club Alpino Italiano / Lo Scarpone — 1870: The First Ascent of Cimon della Pala
• Società degli Alpinisti Tridentini — 150 Years Since the First Ascent of Cimon della Pala
• Palaronda Trek — Mountaineering History of the Pale di San Martino
• San Martino di Castrozza — Pale di San Martino
• San Martino di Castrozza — Bolver-Lugli Via Ferrata
• PlanetMountain — Via Ferrata Bolver-Lugli
• San Martino di Castrozza — Pale di San Martino Climbing Guide
• Società degli Alpinisti Tridentini — Rifugio Rosetta Giovanni Pedrotti
• Club Alpino Italiano — Bivacco Fiamme Gialle
• Club Alpino Italiano / Lo Scarpone — New Bivacco Fiamme Gialle Installed on Cimon della Pala
• MUSE — Historic Bivacco Fiamme Gialle
• Dolomites UNESCO — Pale di San Martino, San Lucano, Dolomiti Bellunesi and Vette Feltrine
• UNESCO World Heritage Centre — The Dolomites