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Pilis and Visegrád Mountains

Pilis and Visegrád Mountains

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Pilis and Visegrád Mountains

Page Type: Area/Range

Location: Hungary, Europe

Lat/Lon: 47.71531°N / 18.93494°E

Object Title: Pilis and Visegrád Mountains

Activities: Hiking, Sport Climbing

Season: Spring, Summer, Fall, Winter

Elevation: 2480 ft / 756 m


Page By: peterbud

Created/Edited: Jan 25, 2010 / Feb 23, 2015

Object ID: 591982

Hits: 10281 

Page Score: 91.75%  - 36 Votes 

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View from Pilis
View of the Visegrád Mountains from Pilis-tető

The Pilis and Visegrád Mountains are a small (about 400 km2) but popular mountain group in northern Hungary. The names are of Slavic origin: Pilis (pleš) means "bald" (the mountain tops of Pilis usually have a clearing), while Visegrád means "high castle" (vyše hrad). The latter is the name of a small town - once Hungarian royal seat - located by the Danube River.

For a long time these two mountain groups were treated as one, and referred to as "Pilis". In fact, they form a compact topographic entity, however their geology differs greatly. In the Triassic period, the whole area was covered by a shallow subtropic sea, so the oldest rocks are sedimentary. Later, in the Miocene period, intensive volcanic activity changed the scene in the northern part (which is now the Visegrád Mountains), where the sedimentary fundaments were covered by andesitic rocks (only in several deep gorges the older sedimentary layers are visible). The southern part (now the Pilis) wasn't affected by volcanism, and further sedimentation took place before the range was lifted up.

Panoramic view from Dobogó-kő (700 m) - Visegrád Mountains
Overview map of Pilis and Visegrád Mountains
Overview map


Thus, the key to be used to differentiate between the two mountain groups is the rock type. South of the tectonic fault line defined by the villages of Pomáz, Pilisszentkereszt and Pilisszentlélek lie the sedimentary Pilis, while north of it lie the volcanic Visegrád Mountains. The latter are geologically more akin to the nearby, but topographically clearly separate, Börzsöny Mountains.

In the southwest, the Pilis are separated from the Buda Hills by the Pilisvörösvár Basin. In the east and in the north, the Visegrád Mountains are almost entirely bounded by the Danube River. There is a certain mountain block (the Szent-Mihály-hegy) north of the Danube Bend, which in geological terms belongs to the Visegrád Mountains, however, it is often treated as part of the Börzsöny, for geographical reasons (the Danube is a clear-cut border).

The highest point of the Pilis Mountains is Pilis-tető (756 m), while that of the Visegrád Mountains is Dobogó-kő (700 m). Both are rather flattish mountain-tops. On Pilis-tető, in the late 1970's the area around the former hiker's hut was converted into a military air defense base, which operated until 1996 - today its abandoned buildings are a "ghost-base". Nevertheless, the hikers and paragliders have returned to the place. The story of Dobogó-kő is slightly different. The first hiker's hut was opened in 1898. The place gained popularity rapidly, and has grown into a complete holiday resort by now (with motorized vehicles, and the kind of people who come with them). The natural rocky lookout (after which the mountain is named) offers nice views on the surrounding mountains and the Danube. Also, there are interesting rocks below this "balcony".

Eastern Pilis
Hills of SE Pilis
Winter on Pilis-tető
A splendid winter day on Pilis-tető (756 m) - Pilis Mountains

The Lordly ridge
The Kevély (Lordly) ridge
Tell them apart
Parts of Pilis Mts. (right) and Visegrád Mts. (left)

View from Nagy-Kevély
(Big Lordly)
Southeastern part of Pilis - labeled version
The Southeastern reach of Pilis Mts.

Main sights

Julianus lookout
Lookout tower on Szent-Mihály-hegy

Despite their modest height, the Pilis and Visegrád mountains provide several interesting places worth checking out. As these mountains are within a good reach of the capital, they are rarely short of visitors.

Danube Bend

The Danube Bend (Dunakanyar in Hungarian) is a scenic area, where the Danube River takes a pronounced, sharp turn between the mountains. The bend itself is based on the U-shaped caldera of an old volcano that ceased being active about 15 million years ago. The originally 1300-1500 m high volcano has been degraded and fractioned by landslides and subsequent geological processes to the remains which are now the Visegrád Mountains. Szent-Mihály-hegy (St. Michael's Mountain), situated on the north side of the river bend, is a remnant of a secondary lava dome, just like its counterpart on the southern bank, called Prédikálószék (Pulpit), from where the greatest view on the entire Danube Bend opens up.

The Danube Bend in Hungary
The Danube Bend from Prédikálószék
Visegrád Mountains
View of Visegrád Mountains and the Danube River from Szent-Mihály-hegy
Vadálló-kövek in summer
(Sentinel Rocks)
The Danube Bend
Szent-Mihály-hegy from the Danube's right bank looks like an island
The Duna from Dobogókő
Danube from Dobogókő


Despite being made of limestone, the Pilis do not feature many deep gorges. The most pronounced one (called Szurdok) is located just southeast of Pilisszentkereszt village. Tourist trails lead both inside and along the upper perimeter of the gorge. The route along the bed of the canyon involves several wooden bridges across the stream, so its "wilderness factor" is not so high.

The Visegrád Mountains offer compensation in the form of a couple of well-developed volcanic gorges. The most popular ones are the Rám-szakadék (Rám Gorge) and Holdvilág-árok (Moonlight Ravine) - both receive a lot of visitors every season. The former is (over-)equipped with metal ladders and handrails at the key sections, the latter has remained more natural (a decade ago, a flash flood wiped out most of the man-made bridges). Some claim the Moonlight Ravine was a pre-Christian cultic place, others don't accept this. But without doubt the site was mined for magnesia in the early Middle Ages. Close by there is another ravine, the Salabasina-árok - once a marked trail lead through it, but now it's wild again and rarely visited. Another interesting spot is the Vasas-szakadék (Iron Fissure) - a short but deep tectonic cleft in the middle of the forest.

In summer
Rám Gorge
Moonligt canyon
Moonlight Ravine
In summer
Rám Gorge
My family in the Vasas-szakadék
Iron Fissure

Scenic rock formations

Both the Pilis and the Visegrád Mountains feature several exposed, scattered through the woodland, rock formations - some are well-known, some are less so. Depending on which region they are located in, their rock material is either andesite (Vadálló-kövek - Sentinel Rocks, Zsivány-sziklák - Goon Rocks, Gomba-szikla - Mushroom Rock, also called as Napoleon's hat), limestone (Vaskapu - Iron Gate, Fekete-kő - Black Rock) or another sedimentary rock (i.e.: the dolomitic Teve-szikla - Camel Rock). The limestone walls of Oszoly are a classic climbing crag in the Pilis.

Sundial rock
Sundial Rock, Oszoly
Napoleon s hat
Napoleon's hat
Goon Rocks

Iron Gate

Camel Rock


Given their geology, the Pilis Mountains are rich in caves (in Hungarian: barlang). These range from simple, short, "dwelling-size" halls (which also served as home for the ancient man) to complex cave systems, parts of which haven't been fully explored yet. The caves and sinkholes are to be found all across the hills; the richest area seems to be the Pilis-tető mountain. Here a couple of long caves - previously believed to be separate - have recently been proven to be connected (with gas-tracing method), but not all of the connections have been explored yet. More information can be found on this site (in Hungarian, but with photos).

cave system
Icicle stalagmites
Winter surprise in
"Teddy Bear" cave

Stalactites on the
roof of Pilis cave
Icicle stalagmites
Winter surprise in
"Teddy Bear" cave

Cloister cliffs
The Cloister cliffs and the neighbouring Csévi cliffs are abundant in caves
A far-from-complete, arbitrary selection of caves in the Pilis:

Pilis-barlang (Pilis cave)
Ajándék-barlang (Gift cave)
Leány-Legény-Ariadne-barlangrendszer (cave system of Girl, Lad, and Ariadne caves)
Kis-kevélyi-barlang / Mackó-barlang (Little Lordly / "Teddy Bear" cave)
Pilisszántói-kőfülke (cave dwelling of Pilisszántó)
Szopláki-ördöglyuk ("Devil's hole" of Szoplák Mtn.)
Papp Ferenc-barlang (Ferenc Papp cave)
Gyopáros-barlang / Nagy-Kevélyi-kőfülke (Edelweiss cave / Big Lordly cave)
Zöld-barlang (Green cave)
Kevély-nyergi zsomboly (sinkhole of Kevély-saddle)
Csúcs-hegyi-barlang (cave of Csúcs Mtn.)
Sátorkőpusztai-barlang (cave of Sátorkőpuszta)

The longer and hardly accessible caves feature very nice stalagmites and stalacites. These are closed for protection of both the caves and people (there are dangerous passages). Some, however, can be safely and legally visited under the supervision of professional guides. Other caves (dwellings), or their easily accessible parts, can be visited freely.

Teddy Bear cave
"Teddy Bear" cave (open)
Cave dwelling of Pilisszántó
cave of Pilisszántó (open)

Lad's Cave (partly open)

"Vacska" Cave (closed)

Gift Cave (closed)