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마지막 업데이트: 4월 28, 2026
하이라이트 • 동굴
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Unfortunately, the path there is completely overgrown and impassable. As of June 25, the descent isn't worth it.
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The Nerother Kopf is an extinct volcano of recent date. It was formed about 15,000 years ago when the earth broke up here and glowing magma welled up from the depths of the earth. At that time, a fracture zone formed in the earth rock, which formed the origin of the volcanic chain "West Eifel". https://www.neroth.de/tourismus/nerother-kopf
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The Millstone Cave is located at the summit of the Neroth Head, a wooded hill of volcanic origin east of Neroth. The entrance is just below the Freudenkoppe castle ruins at an altitude of about 640 m and can be reached via a hiking trail. The cave is 18 meters deep and its vault up to 10 meters high. It is walkable, but unlit (torch required). Wikipedia
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Millstones were mined in the 18 meter deep cave at the top of the Nerother Kopf until the 18th century. The lava stone was not only mined for the production of millstones, but was also used to build the immediately adjacent Freudenkoppe Castle.
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When you enter the Birresborn Ice Caves, the cold comes first. For centuries the so-called "ice caves" were used as ice storage facilities, even in hot summers the temperature does not rise above 7 degrees. Just one of many possible uses over time. The history of the caves as a mining site for coveted millstones is still recognizable today. The millstones were used nationwide to grind oak bark, which was then used as a tannin in leather processing. From quarry to refuge, the caves became a haven during World War II and other times of need. Today bats use the caves as winter quarters, so for nature conservation reasons the ice caves in Birresborn are only open from April to October. Tip: sturdy shoes and a flashlight are recommended for visiting the caves. https://www.gerolsteiner-land.de/a-birresborner-eishoehlen-1
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