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Growing waterfall Dreimühlen
Üxheim
The Dreimühlen waterfall is probably the most interesting waterfall in the Eifel. It was formed from limestone deposits of three spring tributaries of the Ahbach. Due to the constant deposition, the sinter bank is constantly "growing", which is where the name "growing waterfall" comes from…
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Ortsgemeinde Bermel
Bermel
The landscape of the municipality of Bermel is characterized by the idyllic Elztal and the Hochbermel (570 m above sea level). This former basal stone mining site, a landmark of the region, as well as the Kleinbermel together form the nature reserve "Hochbermel" above the 350-soul community…
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Trasshöhlen
Burgbrohl
The sky in the Brohl valley darkened when the Laacher See volcano erupted just five kilometers away. The once loose materials from the glowing avalanche have caked over time to form a rock that is called “trass” in our region.
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May 11, 2025 - Jun 29, 2025 Führung über das Klostergelände von Maria Laach
Maria Laach
The impressive abbey church forms the heart of the Maria Laach monastery complex and is considered one of the most beautiful and best-preserved Romanesque monuments in the country - in the tradition of the great Romanesque cathedrals in Speyer, Mainz and Worms in the Rhineland…
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The growing waterfall Dreimühlen
The Dreimühlen waterfall is probably the most interesting waterfall in the Eifel. It was formed from limestone deposits of three spring tributaries of the Ahbach. Due to the constant deposition, the sinter bank is constantly growing, which is where the name growing waterfall comes from…
More information
Growing waterfall Dreimühlen
The Dreimühlen waterfall is probably the most interesting waterfall in the Eifel. It was formed from limestone deposits from three spring tributaries of the Ahbach. Due to the constant deposition, the sinter bank is constantly growing, which is where the name growing waterfall comes from…
More information
Vulkan Goldberg
Ormont
The quaternary volcano Goldberg, northeast of the municipality Ormont, is the northwesternmost foothill of the quaternary volcanic field in the Westeifel. The volcano is 649. 1 meters above normal zero. The Goldberg was formed about 10 to 11,000 years ago in two eruptions…
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Ettringer Lay - Vulkanparkstation
Ettringen
About 150 years ago in the " Ettringer Lay " ( Lay= stone quarry ) the deepest stone beeches around the Bellerberg volcano were formed. Not without danger the mighty stone columns of its western lava flow were broken here in order to extract building material or paving stones from it…
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Kaiserhalle Burgbrohl
Burgbrohl
The special reason for building the Kaiserhalle in this form as a self-supporting domed hall was the need for the builder Wilhelm Bell to provide evidence that local building materials such as lime, lava sand and trass can also be used for extreme loads…
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