Discover Strotzbüsch: Spring, Üßbach Valley and Mill History

Strotzbüsch brings together a wooded stream valley, a warm mineral spring and traces of mill and Roman history. Different aspects can shape your travel plans: nature and geology sit alongside local history and opportunities for hiking or cycling. The local accommodation options also help you get a sense of the destination.

Mineral Spring and Geology

In the Üßbach Valley, about 150 metres north of Strotzbüscher Mill, there is a thermal mineral spring. Its water is approximately 20°C and is among the warm spring waters of the West Eifel-Moselle mineral water province. The temperature is one characteristic of the water; its mineral and carbon dioxide levels provide further information about its composition.

Each litre of water contains 4,030 mg of dissolved minerals and 614 mg/l of carbon dioxide; it is classified as sodium bicarbonate chloride water. The formation of the Eifel mineral springs is associated with volcanic activity during the Quaternary period. Volcanic rocks are also found around Strotzbüsch. The specific water measurements and the region-wide volcanic connection can therefore be viewed as two aspects of the spring’s geology.

Üßbach Valley, Hiking Trail and Activities

The Üßbach Valley is wooded and is also known as Siebenbachtal. A signposted hiking trail leads from Strotzbüsch into the valley, passing the thermal spring and the mill with its campsite. The name Siebenbachtal, or “Seven Streams Valley,” comes from a viewpoint on the opposite slope, from which the stream can be seen seven times.

Possible activities in Strotzbüsch include longer hikes, cycling on the Maare-Mosel Cycle Route and Nordic walking. It is worth checking trail conditions before setting out on a hike or bike ride. The signposted trail through the valley connects the wooded landscape with the spring and mill sites.

Mill and Local History

The first miller at Strotzbüscher Mill is recorded in 1701; construction of the present mill building began in 1838. It was the last mill in the Vulkaneifel district whose waterwheel was powered by the Üßbach. The start of construction on the present building and the mill’s earlier use of water power are distinct aspects of its history.

Strotzbüsch lies directly on the B421. The Roman tomb is about 150 metres beyond the Strotzbüsch turnoff on the B421 towards Oberscheidweiler. Its protective structure and current presentation date from 2003. The village’s history also includes Strotzbüsch becoming an independent parish; the church is dedicated to Saint Vincentius.

Accommodation

Accommodation in Strotzbüsch includes an inn with rooms, a nature campsite and several holiday apartments. Strotzbüscher Mill is inhabited and offers guest accommodation. Confirm the current operating status and availability of your preferred accommodation before travelling. This allows you to take the different types of accommodation into account when planning your trip, without treating the inn, campsite, holiday apartment and guest accommodation as interchangeable.

Geological Setting: Vulkaneifel

Across the wider Vulkaneifel destination, 77 maars have been identified to date; 350 eruption centres have also been counted there, around 270 of them from the more recent phase. The Eifel Volcano Museum in Daun offers a broader geological perspective: it presents three-dimensional landscape models of cinder cones, maars and mineral springs, as well as exhibits on West Eifel volcanism. These regional facts place the spring and geology of Strotzbüsch in the wider context of the Vulkaneifel.

Discover more destinations: Strohn, Brockscheid, Steiningen, Meisburg, Mückeln, Darscheid, Demerath, Winkel.

For the wider travel overview: Daun.