Eisriesenwelt
One of the world's largest ice caves, located in the Austrian Alps.
The Eisriesenwelt, which translates from German as “World of the Ice Giants,” is a natural cave of limestone and ice in Werfen, Austria, roughly 40 kilometers south of Salzburg. It sits inside the Hochkogel mountain, part of the Tennengebirge range in the Alps, and holds the title of the world’s largest ice cave, stretching over 42 kilometers. Each year, around 200,000 tourists visit.
The Tennengebirge mountains formed during the late Tertiary period, specifically the Würm glaciation of the Pleistocene. This range, one of the massifs in the Austrian Alps, is the largest karst plateau in the Salzburger Alps, and the Eisriesenwelt lies at the edge of this plateau. Although the cave measures 42 kilometers in length, only the first kilometer—the section open to tourists—is covered in ice; the rest is limestone. The Salzach river carved the passageways, and the ice formations came from thawing snow that drained into the cave and froze in winter. Because the entrance stays open year-round, cold winter winds blow in and freeze the snow inside. In summer, a cold wind from the cave blows outward, keeping the formations from melting.
The cave was first officially discovered in 1879 by Anton Posselt, a natural scientist from Salzburg, who explored only the first 200 meters. Before that, locals knew of it but believed it was an entrance to Hell and refused to enter. Posselt published his findings in a mountaineering magazine in 1880, but the report was soon forgotten. Alexander von Mörk, a speleologist from Salzburg, remembered Posselt’s discovery and led several expeditions starting in 1912, followed by other explorers. Von Mörk died in World War I in 1914, and an urn with his ashes rests in a niche inside the cave. In 1920, a cabin called Forscherhütte was built for explorers, and the first routes up the mountain were established, drawing tourists. Later, another cabin, the Dr. Oedl House, and paths from Werfen and Tenneck were added. A cable car was built in 1955, cutting the 90-minute climb to three minutes. Today, the National Austrian Forest Commission owns the cave and has leased it to the Salzburg Association of Cave Exploration since 1928, still receiving a share of entrance fees.
The cave is open from May 1 to October 26, with hours from 9:00 a.m. to 4:30 p.m. in July and August, and 9:00 a.m. to 3:30 p.m. in May/June and September/October. Temperatures inside are usually below freezing, so warm clothing is advised. Photography is not allowed once inside. The tour starts at the entrance and goes inward to Posselt Hall, a large room with a stalagmite called Posselt Tower at its center. Past the tower, an ashen cross on the wall marks the farthest point Anton Posselt reached. From there, visitors see the Great Ice Embankment, a massive formation 25 meters high that shows the area of greatest ice growth. Next is Hymir’s Castle, named after a Norse giant, where stalactites form Frigga’s Veil, also called the Ice Organ. The tour then reaches the Alexander von Mörk Cathedral, one of the largest rooms in the cave and the resting place of von Mörk’s ashes. The final stop is the Ice Palace, one kilometer into the cave and 400 meters underground. From there, visitors must turn back and walk through the caves to the entrance. The round trip takes about one hour and 15 minutes.
- length
- About 42 km
Lore & Background
The Eisriesenwelt was formed by water from the Salzach river system, which eroded passageways into the mountain. The ice formations were created by thawing snow that drained into the cave and froze during winter. Since the entrance is open year-round, chilly winter winds blow into the cave and freeze the snow inside; in summer, a cold wind from inside blows toward the entrance and prevents the formations from melting. The cave is inside the Hochkogel mountain in the Tennengebirge section of the Alps, a karst plateau formed during the late Tertiary period and the Würm glaciation of the Pleistocene. Before his discovery, locals believed it was an entrance to Hell and refused to explore it.
Reader's Guide
Its geological formation, shaped by the Salzach river and glacial processes, offers a unique natural spectacle. The cave's history reflects a shift from local superstition—where it was feared as an entrance to Hell—to scientific exploration and tourism. The tourist-accessible area covers only the first kilometer, which is ice-covered, while the remaining 41 km are limestone. The tour includes notable features such as Posselt Hall, Hymir's Castle, and the Alexander von Mörk Cathedral, where von Mörk's ashes rest. The cave's legacy lies in its blend of natural wonder, historical exploration, and ongoing public fascination, preserved through careful management and seasonal operation from May to October.
Did You Know?
- The cave extends about 42 km, but only the first kilometer is covered in ice.
- An urn containing the ashes of explorer Alexander von Mörk is inside a niche in the cave.
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