Olympos
The mountain of the gods
The mountain of the gods
It is the highest mountain in Greece, renowned worldwide primarily for its mythological significance, as the twelve "Olympian" gods—according to ancient Greek religion—dwelt at its summit (Mytikas, 2,918 m). It is also the second-highest mountain in the Balkans, surpassed only by Rila in Bulgaria.
Various theories have been proposed regarding the etymology of the name "Olympus" (sky, radiant, high, rock, etc.).
According to one theory, "Olympus" is a pre-Greek place name of unknown etymology, the original meaning of which was likely simply "mountain."
It rises imposingly on the border between Macedonia and Thessaly, featuring a series of high peaks and deep ravines, surrounded by an area of exceptional biodiversity. To protect this unique heritage, it was designated as Greece's first National Park as early as 1938.
The first person to ascend the summit of the mythical mountain—Mytikas—was Christos Kakkalos, a hunter and *laouto* player from Litochoro; on August 2, 1913, he guided two Swiss men—the renowned photographer Frédéric Boissonnas and his companion, Daniel Baud-Bovy—to the top. "Olympus had been calling to us for so long," notes the Swiss Boissonnas in his account. "Its beauty lies not merely in nature; its beauty is spiritual. It expresses the divine." The path to the summits was now open.
Every year, thousands of nature lovers visit Mount Olympus to admire the allure of its natural landscape up close and enjoy exploring its slopes. Even greater numbers of mountaineers and climbers flock there from every corner of the globe to conquer its peaks—most notably Mytikas, the abode of the twelve Olympian gods.
The massive mountain range of Olympus looms imposingly on the border between Macedonia and Thessaly, featuring a series of high peaks and deep ravines, surrounded by an area of exceptional biodiversity. To protect this unique heritage, it was designated as Greece's first National Park as early as 1938.
Every year, thousands of nature lovers visit Mount Olympus to admire the allure of its natural landscape up close and enjoy exploring its slopes. Even greater numbers of mountaineers and climbers flock from every corner of the globe to conquer its peaks—above all, Mytikas, the abode of the twelve Olympian gods.
The Mountain
The massive mountain range of Olympus rises imposingly on the border between Macedonia and Thessaly, featuring a series of high peaks and deep ravines, surrounded by an area of exceptional biodiversity. To protect this unique heritage, it was designated as Greece’s first National Park as early as 1938.
Every year, thousands of nature lovers visit Mount Olympus to admire the allure of its natural landscape up close and enjoy exploring its slopes. Even greater numbers of mountaineers and climbers flock from every corner of the globe to conquer its peaks—above all, Mytikas, the abode of the twelve Olympian gods.
Well-equipped mountain refuges, along with a variety of mountaineering and climbing routes, are available to visitors wishing to explore the mountain's beauty. Litochoro, situated at the mountain's eastern foothills—100 km from Thessaloniki—serves as a classic starting point; it is also the finish line for the world-renowned Olympus Marathon, held every summer.
Mount Olympus, the highest mountain in Greece, is located on the border between Macedonia and Thessaly, marking the boundary between the prefectures of Pieria and Larissa (coordinates 40°05’N 22°21’E).
The impact of rain and wind, combined with the often violent forces of nature, sculpted the current form of Mount Olympus; it rises proudly like a giant tower to an altitude of nearly 3,000 meters, with no surrounding mountain challenging its dominance. Situated just 18 km from the beach at Litochoro, it allows many adventurous visitors to combine a visit to its snow-capped peaks with a swim along the coast of Olympus—all in a single day.
The mountain’s boundaries extend in a roughly circular shape with a circumference of 150 km and an average diameter of 26 km, as follows:
To the northwest, starting from the Vlach village of Kokkinoplos, the Makryrema stream separates Olympus from the Voulgara massif, while the villages of Petra, Vrontou, and Dion are situated on the northeastern foothills. On the eastern side lies the town of Litochoro, where the Enipeas (Vythos) Gorge—which cuts through the mountain massif—terminates. To the southeast, the Ziliana Ravine forms a natural boundary separating the area from Kato Olympus, while the villages of Sykaminea and Karya are located on the southwestern foothills. To the west, the boundaries are defined by the Holy Trinity Monastery of Sparmos and the village of PXirokampi—an area characterized by low-growing vegetation and small fauna—extends along the foothills of Mount Olympus; further east lies the fertile plain of Dion, traversed by streams flowing from Olympus before they empty into the Thermaic Gulf. UNESCO: Inclusion of Mount Olympus in the World Heritage List
By a unanimous decision of the UNESCO World Heritage Committee, Mount Olympus and the broader region surrounding it have been inscribed on the UNESCO World Heritage List as a Mixed Site.
By a unanimous decision of the UNESCO World Heritage Committee, Mount Olympus and the wider area surrounding it have been inscribed on the UNESCO World Heritage List as a "Mixed Property."
The decision was reached during the proceedings of the Committee’s 48th Session on Sunday, July 26, 2026, in Busan, South Korea, where the nomination dossier submitted by the Ministries of Culture and of Environment & Energy was deliberated.
It is worth noting that Olympus was designated Greece’s first National Park in 1938, was included in UNESCO’s "Man and the Biosphere" programme as a protected area (Biosphere Reserve) in 1981, was declared a national park by Presidential Decree in 2021, and is now listed among UNESCO’s World Cultural and Natural Heritage sites.
Commenting on this highly significant development for the iconic mountain, the Mayor of Dion-Olympus, Vangelis Geroliolios, emphasized: "The inscription of Olympus on the UNESCO World Heritage List as a 'Mixed Site' reflects to the world the unique coexistence of natural and cultural wealth that characterizes the mountain of the gods."
For the Municipality of Dion-Olympus, this development represents an opportunity for sustainable growth, the strengthening of the local economy, the promotion of our cultural identity (culture, gastronomy, alternative forms of tourism), and the showcasing of our natural wealth on an international level. At the same time, it entails a significant responsibility; as the wider region acquires this new honorary designation, there arises a need for enhanced protection of the natural environment and adherence to the principles of sustainability.
Managing this significant success presents a challenge in itself. The increased volume of visitors must under no circumstances lead to the degradation of the natural environment. Olympus requires a well-organized plan for visitor reception and management.
For this reason, critical interventions are needed to strengthen mechanisms for protecting both visitors and the environment, create modern visitor facilities, improve the organization of parking and access, and raise environmental awareness among visitors.
At the same time, continuous cooperation among all stakeholders is required to ensure that every decision is guided by the need to preserve the outstanding universal value of Mount Olympus. The Municipality of Dion-Olympus is already collaborating closely with the Ministries of Environment and Culture, OFYPEKA, the Region of Central Macedonia, the scientific community, archaeological and forestry authorities, mountaineering clubs, and all relevant stakeholders to implement an effective management system for the monument.
Geology – Morphology
Geology
Mount Olympus is a compact, rocky mountain with multiple peaks and a nearly circular shape; it covers a relatively small area (600 square kilometers). It is one of our relatively younger mountains, as the age of its principal rock formations is estimated not to exceed 200 million years—a time when the greater part of Greece (and the Mediterranean) lay at the bottom of a shallow sea, where the materials that would later form the current rocks were deposited.
Subsequent geological events caused the uplift of the entire area and the former seabed. One million years ago, glaciers covered Mount Olympus, carving out the mountain's plateaus and hollows. As temperatures subsequently rose, the ice melted, and the resulting torrents swept large quantities of fragmented rock to lower elevations, forming alluvial fans that spread across the entire region, from the mountain's foothills to the sea.
You can find more details about the geology of Mount Olympus at the Museum of the Geological History of Olympus.
Morphology
The region's complex geological history is evident in the morphology of the National Park and Mount Olympus as a whole. Its landscape is characterized by deep ravines and dozens of smooth-contoured peaks—many exceeding an altitude of 2,000 meters, such as Agios Antonios (2,815 m), Kalogeros (2,700 m), Toumba (2,801 m), and Profitis Ilias (2,803 m). However, it is the central, near-vertical rocky peaks that truly impress the visitor; viewed from the direction of Litochoro, the mountain's profile traces a distinct "V" shape against the horizon between two peaks of nearly equal height.
On the left branch lies Greece’s highest peak, Mytikas ("Pantheon" – 2,918m), while on the right, Stefani ("Throne of Zeus" – 2,909m) stands as Olympus’s most impressive and precipitous peak; its final 200 meters rise vertically, presenting the most demanding section of the ascent.
Further south, Skolio (the second-highest peak at 2,912m) completes an arc of approximately 200 degrees; its sheer rock faces form a wall-like structure on the western side, enclosing an impressive, precipitous, amphitheater-like hollow—"Megala Kazania"—that is 700 meters deep and has a circumference of 1,000 meters.
On the eastern side of the high peaks, their steep slopes form parallel, band-like ledges known as "Zonaria." From there, even narrower and steeper gullies—the "Loukia"—lead to the summit.
On the northern side, between Stefani and Profitis Ilias, lies the "Plateau of the Muses" at an elevation of 2,550 meters, while further south—near the center of the mountain massif—one finds the extensive alpine meadow of Bara at an altitude of 2,350 meters.
The numerous ravines and gullies lend Olympus an appearance of rare beauty. The most distinctive ravines are those of Mavrolongos-Enipeas (14 km) and Mavratzas-Sparmos (13 km); these converge near the location known as Bara, effectively slicing the mountain mass into two elliptical sections. At the southern foothills, the large Ziliana ravine—spanning 13 km—forms a natural boundary separating the mountain from Kato Olympus.
There are also numerous chasms and a series of caves, many of which remain unexplored. The nature and arrangement of the rock formations, combined with the climate, favor the presence of many springs—primarily below an altitude of 2,000 meters—as well as small seasonal lakes, torrents, and a small river, the Enipeas, which originates at Prionia and flows into the Aegean Sea.