Piedra del Penol, the giant rock above Guatape’s water maze
Published on 08/31/2026 at 20:03 | Editorial responsibility: Rafael Müller, Editor-in-Chief AD HOC NEWS
Piedra del Penol, also known as El Peñón de Guatapé or La Piedra del Peñol, is a massive rock rising above the reservoir landscape near Guatape in Colombia. The monolith’s height and stepped access to a viewing area make it a rare combination of geological landmark and built lookout in the Antioquia region.
A solitary monolith in the Antioquia hills
Piedra del Penol stands in the municipality of Guatape in Colombia’s Antioquia department, between the towns of Guatape and El Peñol. The rock is described as an inselberg, a solitary block of stone that rises from gentler surrounding terrain without forming part of a continuous ridgelandmark inselberg in Colombia. Its local names reflect a shared identity: Guatape and El Peñol each claim the rock in their own way, which is why visitors encounter both Piedra del Peñol and Peñón de Guatapé on signs and mapspeñón de Guatapé, o piedra del Peñol.
The monolith reaches a height in the region of 200 to 220 m (656 to 722 ft) above its base, according to local descriptions from tourism authorities220-meter-high monolithmonolito de 220 metros de altura. It is often described as granite or quartz-rich rock, with a surface that appears dark and blocky when seen from the surrounding roads220-meter-tall granite monolith. From the lower slopes, the rock’s bulk dominates the view, rising above green hills, scattered trees and small buildings.
A staircase through a natural fissure
Piedra del Penol is not only a natural landmark; it is also a place that visitors can climb by stairs built directly against the rock. A zigzagging staircase rises through a fissure on one side of the monolith, using the narrow cleft in the stone as a corridor between the base and the upper viewing areasbrick staircase of 659 steps rises up through a broad fissurestaircase of exactly 740 steps, built into a natural fissure. Different guides give slightly different counts for the steps, but all agree that the staircase runs to several hundred steps and reaches a platform close to the summit.
The climb is laid out in a series of flights connected by small landings, enclosed by concrete and brick balustrades for most of the way. Visitors ascend alongside the rough rock surface, with occasional openings giving views back over the access road and the reservoir. Near the top, further steps and ramps lead to viewing terraces, kiosks and small structures, turning the summit area into a compact, built-up lookout. From there, the height of the monolith above the water and hills becomes clear, and the reservoir’s branching form can be seen sweeping around the lower slopesclimbing its 740 steps carved into the rough stone.
Stone above a flooded valley
One of the striking aspects of Piedra del Penol is the relationship between rock and water. At the foot of the monolith, roads and paths lead towards the Embalse Guatapé, a hydroelectric reservoir whose irregular shoreline almost surrounds the hillrises from near the edge of the Embalse Guatapé. The reservoir dates from the late twentieth century, when a dam flooded parts of the valley to provide power for Medellín and the wider regionreservoir created in the 1970s to generate hydroelectric power. Seen from the summit terraces, the lake forms long, finger-like inlets between peninsulas and islands, creating the “water maze” landscape that visitors associate with Guatape.
Guatape itself lies nearby on the shores of the reservoir, a town known for its colourful facades and decorative panels on houses, while El Peñol stands further along the shore. Boats trace routes between the settlements and the scattered islets, and the rock is visible as a landmark from many parts of the reservoir. The monolith’s elevation above sea level is given in guides at around 2,135 m (7,005 ft), placing it within the Andean highlands and making the panorama from the top a view across layered hills rather than sheer peaks2,135 meters above sea level.
Visiting Piedra del Penol: what travellers from Western Europe should know
- Piedra del Penol stands between Guatape and El Peñol in the Antioquia department of Colombia, and is reached by road from Medellín and from the lakeside town of Guatapebetween the municipalities of Guatapé and El Peñol.
- The climb to the upper viewing terraces runs up a long staircase of several hundred steps built into a fissure in the rock, so visitors need to be comfortable with sustained stair climbing on concrete and brickstaircase of exactly 740 steps.
- The official language is Spanish and the currency is the Colombian peso.
- Piedra del Penol rises above a reservoir landscape, and the approach from Guatape passes lakeside roads and small hills before reaching the parking area at the base of the rocktake the road that curves up past the gas station to reach the parking lot.
- Entry requirements depend on your nationality; UK travellers can check the FCDO travel advice at gov.uk/foreign-travel-advice, Irish travellers the Department of Foreign Affairs at ireland.ie.
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Frequently asked questions about Piedra del Penol
Where is Piedra del Penol located?
Piedra del Penol stands between the municipalities of Guatape and El Peñol in the Antioquia department of Colombia, close to the Embalse Guatapé reservoirlocated between the municipalities of Guatapé and El Peñol.
What can visitors expect during a climb?
Visitors climb several hundred concrete and brick steps built into a fissure in the rock, passing landings and low walls, and reaching viewing terraces near the summit with wide views over the reservoir landscapestaircase of exactly 740 steps, built into a natural fissure.
What makes Piedra del Penol distinctive compared with other viewpoints?
Piedra del Penol combines a high, solitary monolith with a built staircase and summit terraces, rising above a hydroelectric reservoir whose branching inlets and islands create a distinctive water-and-hill panorama beneath the rock220-meter-high monolith located between the municipalitiesreservoir created in the 1970s to generate hydroelectric power.
