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Hyeopjaegul - Lava Tube
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Hyeopjaegul

description Hyeopjaegul Overview

Hyeopjaegul is a lava tube located within Hallim Park on Jeju Island, South Korea. Formed by ancient basaltic lava flows, the cave is notable for its secondary carbonate speleothems, which developed from the dissolution of overlying shell-rich sands. The tube maintains a consistent internal temperature and features unique geological formations. It is part of a network of volcanic caves on the island and is accessible to the public as a show cave.

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Where is Hyeopjaegul located?

Hyeopjaegul is a notable lava tube located within Hallim Park on the southern coast of Jeju Island, South Korea. Jeju Island itself is a massive volcanic shield volcano. The lava tube is part of the Geomunoreum Lava Tube System, which is recognized as a UNESCO World Heritage site.

What makes Hyeopjaegul lava tube unique?

Hyeopjaegul is highly unique because, unlike most dry lava tubes, it contains secondary carbonate speleothems like stalactites and stalagmites. These limestone formations were created by water percolating through overlying shell-rich sands. This combination of volcanic formation and limestone deposits makes it extremely rare in geology.

Can you visit Hyeopjaegul cave?

Yes, Hyeopjaegul cave is fully accessible to tourists visiting Hallim Park on Jeju Island. Visitors can walk along constructed paths to view the fascinating rock formations, the carbonate deposits, and the various lava formations like lava toes. It is a must-see geological attraction for anyone visiting South Korea.

How was the Hyeopjaegul lava tube formed?

The Hyeopjaegul lava tube was formed thousands of years ago when highly fluid, basaltic lava flowed from a volcanic eruption. As the outer edges of the lava flow cooled and hardened, the hotter interior continued to flow, eventually leaving a hollow, cylindrical cave behind. The unique shell-sands covering the area later washed into the cave, creating its rare limestone features.

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