Meerfelder Maar


Share content:

The Maar was created in an explosion about 80,000 years ago. The power of volcanic activity broke the slopes of the Maar basin in clods. However, this uniqueness can hardly be seen with the naked eye. The impressive olivine bombs are visible evidence – they are round rock blocks made from the mineral olivine which were ejected when the volcano erupted.
In the south the pretty village Meerfeld nestles on the steep slopes. Here the flowing Meerbach flooded loose material ejected during the eruption. So the water was pushed into the northern part and the approximately 18 meters deep Maar lake was born. But not only natural circumstances contributed to the downsizing of the Maar lake: During the 19th century parts of the Maar basin have been artificially drained in order to create additional agricultural land. Currently the lake, which lies at an altitude of 335 metres a.s.l., has a water surface of 24.8 hectares and is approximately 18 metres deep.
Visitors can discover these and other unique evidence of the region’s volcanism on one of the numerous tours through the protected area. In addition you can observe the diverse Flora and Fauna of the Maar which enchants with rare species of waders, wet meadows and sedge. In the south a wide reed zone has formed, which is home to all kinds of animals.
Water sports enthusiasts also get their money’s worth in Maar: Besides fishing it is possible to swim in destinated areas on the north shore and to cool off in the refreshing water after a tour. The bathing season in the natural swimming pool Meerfeld Maar lasts from May to September.

Besides a few parking spaces in Meerfeld there is also a designated parking space on the southeastern shore, which can be reached via the K10.




Meerfelder Maar
54531 Meerfeld


Plan your journey

Route on Google Maps

Arrive by train

You might also be interested in

Blick vom Maarkreuz aufs Schalkenmehrener Maar, © Eifel Tourismus GmbH, D. Ketz

Schalkenmehrener Maar

Especially if you visit the GesundLand Vulkaneifel in summer, a detour to the Schalkenmehren Maar is a must. Located directly at the village of the same name and opposite the Weinfelder Maar, the Schalkenmehrener Maar is one of the three Dauner Maars and offers a wonderful backdrop for an extended walk or an extensive hike. If you look closely, you can see that the Schalkenmehren Maar was once a double maar, formed by volcanic activity around 20,000 to 30,000 years ago. But the tuffs of the western maar filled up the eastern maar funnel, so that nothing can be seen of the second maar today, except for the fen vegetation that has spread in this area. Take a little discovery tour and observe numerous animal and plant species along the way!