The Danube Bend gorge trail

Itinerary

• From the bus stop we follow the P sign (heading towards the church) all the way to the Rám Gorge junction.
• The Z sign leads through the Rám Gorge.
• From the junction above the gorge, turn left and follow the Z◼ sign towards Rám Mountain.
• We visit the Rám Rock via the Z▲ sign, then return the same way.
• Turning left on the Z◼ sign, we join the asphalt road.
• Follow the asphalt road to the right, along the yellow cycling sign.
• At the next junction (at the top of the gorge) turn right onto the S sign, which we follow through the Lukács valley.
• Returning to the Mill Valley, turn left and walk along the asphalt all the way back to Dömös (P sign).

Detailed tour description

Up along the creek

Starting from Dömös beside the church, we begin the tour following the neatly painted P signs. The street turns right, leading into the narrow Mill Valley, where neat houses line the base of the slope. Observing the close relationship of built and natural environments, it quickly becomes clear why Dömös became popular with various artists in the 19th century when a small artist colony formed on the village’s edge with newly built or renewed summer houses. Due to the Danube’s gorge and steep hillsides, the village fortunately could not sprawl out much, thus it has retained a pleasant, forested foothill settlement with a quite unique location. Looking forward, the forest draws nearer, but it’s also worth looking back: steeply rising Saint Michael’s Mountain across the Danube looms as if towering at the end of the street.

Suddenly, the sign turns left off the valley asphalt road to cross to the far side of the creek. At this spot, a mill once stood on the watercourse, which could provide continuous energy with reliable year-round output. The grey boulders lying in the bed largely originated from the inclined body of Keserűs Mountain above us. Following the base of this considerable mountain mass, we walk along the outer edge of the collapsed, worn caldera of the former volcanic formation. For geological reasons alone, the Rosa mine, starting to the left, is unlikely to have been drilled into the mountain for coal or lignite mining purposes as some sources suggest. Water stands in the bottom of the narrow corridor, but it’s forbidden to enter because a sizable bat colony inhabits inside. (There is also another mine tunnel nearby.)

The charming trail follows the widely spreading creek, offering plenty of chances to notice enormous stones carried by the water during raging floods. On the opposite side, a winding asphalt road hosts a buffet, but its pleasures are best reserved for the end of our outing on the way back. A diverse old-growth forest covers the valley and its sides, characterized by a mix of tree species and ages—here and there, some ancient root crowns emerge like stiff snakes from the eroded soil.

After a short climb and a bend, a rotunda-like rain shelter appears in a meadow ahead, with the small, friendly building of the Holy Cross Chapel shining to our left in the shade of beech trees. It commemorates an apparition: in 1885, the image of Virgin Mary appeared shining on a beech tree to two girl gooseherds. The miracle tree quickly gained fame, and a flood of pilgrims swarmed the valley and village—who were rudely discouraged by the village: only two years after the first apparition, the deputy bailiff and some policemen simply cut down the tree. Unfortunately, nobody has erected a memorial to the expression of the visiting pilgrim group from Ipolyszakállas at that time, but the Dömös holy tree was replaced by a chapel erected on the site within decades. Beside it, a flood-damaged ditch connects, at whose mouth springs the Kaintz spring (named after a former tourist trail).

We are halfway to Rám Gorge, so let's continue! The trail does not leave the creek, which flows through an increasingly narrow and noticeably descending valley. On the outer curves of its small bends, the hiking path has been dangerously undermined in some places; a major flood could fundamentally change its relationship with the trail. We bypass a ruined building and shortly before, heeding the call of the Z sign, turn right. We cross the asphalt road and, as the nature trail sign draws attention, leaving the resting place, we head for the Rám Gorge.

Towards the gorge!

We wade through the creek and proceed between increasingly narrow hillsides. Steep slopes show fallen trunks, while mainly beeches inhabit the cool, humid valley. Going deeper (passing a spring), we finally reach the gorge entrance, indicated by the appearance of relatively low cliff walls, the rustling of water, and most clearly, the railing provided for gripping. The bed contains timber debris chipped by forestry, and progress is hindered not only by the boulders falling from cliff walls but also by the fact that on the trail we share space with the creek. The first waterfall appears, less than 2 meters high, but we bypass it because the rising water has carved a detour around a hard block.

Further in, the terrain temporarily calms, and we cross the creek numerous times where it tumbles over mossy rocks. Then conditions change again, and suddenly we are squeezed between gigantic, raw cliff walls, revealing the gorge’s structure. During one volcanic phase that formed the Visegrád Mountains, violent eruptions hurled various debris and glowing ash into the air, which fell and cascaded down the slopes covering vast areas. Over millions of years, the creek carved a deep corridor into the consolidated dacite breccia, forming a real gorge with steps. Water (and hikers ascending) cover a 112-meter altitude difference over about 600 meters of length. The path is bordered by walls over 30 meters high in places; massive blocks fallen from them indicate that the gorge’s shaping is unfinished, the creek and rock mass continuously wrestling.

Chain of rock basins

Soon we enter a gloomy rock basin, where initially it seems impossible to go further. A memorial warns of hidden dangers, and a railing and wooden cross close off the gorge’s short, drier branch. To the right leads the compressed path, where the gorge suddenly turns back to the left—here we confront the first bigger waterfall spanned by a ladder. The relatively soft tuff wall is carved in an arch shape over its height by the cutting creek, but it struggles more with the resistant lava rock: you have to slide down its steps. Climbing the slippery ladder wet with spray, you enter the narrowest, most exciting section of the gorge: stepping in the creek within a wild rocky pass squeezed by steep cliffs, movement secured by a railing. The volcanic debris forms knobby walls scarcely covered by vegetation, and the creek’s tough shapes aren’t softened by the view of the next rock slide where a 7-meter-high cascade rushes down.

The supporting ladders (and the pipe) are relatively recent in the gorge; in the early 20th century, hikers had to retreat if they failed to find hold or step on timber debris and stones. Then chains were added for gripping, later larger ladders followed; the current equipment offers undeniable security (and durability) but is somewhat intrusive—a 21st-century innovation.

The trail winds through sharp bends before ascending the last two-part ladder. The gorge widens, then narrows again (perhaps more than any prior section), eventually crossing a larger waterfall by grabbing the railing (steps are carved into the rock here). No more serious obstacles follow: the upper section was heavily filled with flood debris, and the now-unused railing is waist-high. A wooden bridge crosses the bed; the steps ahead promise the tour’s most tiring moments. These small wooden steps are necessary because we walk on slippery mud exposed by the Hármas Forrás and its feeder streams, washed by the creek to the gorge’s last meters. Old beeches’ root curls emerge from the eroded soil layer, and the path is bordered by indentations. A resting place offers a chance to catch breath before turning towards the Rám Rock.

A glance from below the mountains

The name Rám, as shown on the map, appears several times around here, and although various legends generally speak of people who fell between the gorge walls shouting “Rám is breaking!”, or the old Hungarian meaning of the word “rám” as ‘copper’ suggesting a mint in the naming background, the reality is simpler. Its origin may be the German “Ramsberg,” meaning “bear garlic mountain,” or simply the “Rahm” family name. (Several nearby place names also have personal name origins.)

The Z◼ sign heads left, initially crossing young woods, then passing through natural stands featuring big beeches in the Három-forrás area. The Dobogókő massif rises along a fault line here, where a chain of springs feeds from precipitation absorbed by the mountain crest. We proceed along a waving path, the spiritual significance of the site noted by a carved wooden gate, under which the Z▲ sign slips through.

Hikers have built a whole army of stone men from scattered rocks on the ground, behind which stands the worn, sweaty climb to Rám Rock confronting us. The hard but quickly disappearing trial is rewarded with a magnificent mountainous panorama. Deep in the Visegrád Mountains, we look out squeezed between hills, with Dobogókő’s ridge running high to the right and Keserűs Mountain rising opposite (at its end the Predikáló chair lookout is recognizable). On a side ridge, the bare rock ridge of Vadálló-kövek towers over the forest. Our rock is formed from sliding debris (breccia) of the ancient volcano’s mantle, carved by erosion and highlighted by tectonic movements—just like the surrounding heights, thanks to which one can feel in an enclosed mountain amphitheater. (The rock tower rising from the ridge is named Ferenczy Rock after a former captain of the Hungarian Carpathian Association.)

Back to the Danube with the water

A relaxing path follows back to the Danube, which we start again from the foot of the mountain turning left on the Z◼ sign. We only step a few meters on the trail because we turn right onto the asphalt road. We walk about 1 kilometer on it, then again take a right and descend on the S sign. The road arcs on the side of Árpád Castle, inspiring legends, where Bronze Age earthworks have been identified, with copper pieces found at its foot—allegedly a counterfeit workshop operated in the former “Mint Ditch.” We approach the Lukács valley through a windswept forest, which gradually engulfs the serpentine bend. Again, we can admire tangled forests and deeply cut creekbeds exposing rocks before our path joins the Mill Valley.

We find our way back to Dömös on the left. This time, it’s worth choosing the atmospheric valley asphalt rather than the already traveled hiking trail, as a buffet awaits hikers further down. We can reach the village center in about half an hour.