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The Auberg above Gerolstein is a rocky plateau formed from dolomite and part of the impressive "Gerolstein Dolomites" nature reserve, which has been protected since 1990 and covers approximately 102 hectares. Geologically, it is a reef formed around 380 million years ago in a warm, shallow sea, exposed by karstification and folding – typical features of this Devonian limestone reef. At an elevation of approximately 360 meters above sea level, the Auberg offers spectacular views over Gerolstein, the Kyll Valley, and the entire Volcanic Eifel region – a real highlight on tours along the Eifelsteig or local circular trails such as the "Gerolsteiner Dolomiten Acht" (Gerolstein Dolomites Eight). The trail leads through narrow crevices and past bizarre rock formations, providing a true sense of discovery while hiking. Botanically, the Auberg is a valuable habitat: rare orchids, nutrient-poor grasslands, juniper, and species-rich mosses can be found on the sparse Dolomite rocks – as well as bats in protected crevices. Smaller populations also use the area as a resting, breeding, and hunting ground. For Komoot users, there are several tour options: for example, Eifelsteig stage 9 (Hillesheim–Gerolstein) or the local "Gerolsteiner Dolomiten Acht" (approx. 8 km), where the Auberg is a sublime intermediate destination. There's also a Reservoir–Auberg–Lissingen loop, an easy, family-friendly walk (approx. 4 km, 1 hour) with panoramic views and rocky outcrops.

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From here you have a beautiful view of the Auberg, from where you can enjoy a wonderful view of Gerolstein.

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The steep climb to the castle is quite difficult. A real calf biter! But once at the top you forget it all. Beautiful ruin and the cave is more than worth it.

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"With an area of approx. 102 hectares, the area around the Gerolsteiner Dolomites has been a nature reserve since 1990. + occurring animal species: bat + occurring plant species: juniper, orchids, character plants calcareous grassland, grove rush-beech forest, woodruff-beech forest, orchid-limestone-beech forest Around 380 million years ago there was a warm, subtropical shallow sea here, in which mighty reefs of stromatopores - relatives of sponges - and corals formed. After the dolomitization, sinking and folding of the rocks, the Devonian deposits were lifted out again. Today's Gerolsteiner Dolomites were formed, which rise steeply above the Kylltal north of the center of Gerolstein. The rocks "Hustley", "Munterley", "Drohende Ley", "Große Kanzel" and "Auberg" characterize the cityscape from afar and form the landmark of Gerolstein. The most famous summit of the Gerolsteiner Dolomites is the "Munterley" - with a height of 482 meters - and offers a breathtaking view over Gerolstein, the Kylltal and far into the Vulkaneifel. Stone Age people, who settled here 30,000 years ago, obviously enjoyed this view, as evidenced by stone tools and bones found at the nearby Buchenloch Cave. Visiting the Gerolsteiner Dolomites can be perfectly combined with hiking the Felsenpfad - the northern part of the "Gerolsteiner Dolomiten Acht". The almost eight-kilometer round tour offers many magical places and geological traces." https://www.eifel.info/a-gerolsteiner-dolomites

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Very well preserved ruin. Exploring them with children is a very special experience. Especially nice in late spring when the trees all around are fresh green.

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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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