Quelle im Nettepark „Hetzebue“

Plaidt

In the original cadastre of Plaidt from 1826, the Prussian surveyors from outside the town called this small spring and the surrounding land "Im Hützeborn". In dialect it is called "Hetzebue", whereby the "ue" is not pronounced like "ü" but "u". In High German it is called "Hitzeborn", which refers to a warm spring. The water temperature is clearly in the positive range all year round. When the sewage pipes were laid from the old sewage treatment plant behind the school to the sewage treatment plant in Andernach in the late 1990s, which runs right under the path in this part of the park, the "Hetzebue" was completely buried. A few years later, it fought its way back to the surface. The Plaidter Geschichtsverein (Plaidter History Society) had the spring restored in 2014 so that a short rest can be taken at this point and the spring bed can be walked on.

mehr lesen

Share content:

At a glance

Opening hours

  • From December 1st to December 31st
    Monday
    00:00 - 23:59

    Tuesday
    00:00 - 23:59

    Wednesday
    00:00 - 23:59

    Thursday
    00:00 - 23:59

    Friday
    00:00 - 23:59

    Saturday
    00:00 - 23:59

    Sunday
    00:00 - 23:59

Place

Plaidt

Contact

Quelle im Nettepark "Hetzebue"
Zugang zum Park am Ende der Mühlenstraße
56637 Plaidt

Bitte akzeptieren Sie den Einsatz aller Cookies, um den Inhalt dieser Seite sehen zu können.

Alle Cookies Freigeben

Plan your journey

per Google Maps

You might also be interested in

Gleitfalte, © Baumann Fotografie

Gleitfalte am Dachsbusch

The mining of volcanic material on the Dachsbusch ate deeper and deeper into the old cinder cone. It gives us an insight into the volcanic and climatic history. The volcanic layers show how they slipped during a cold period about 150,000 years ago due to the alternation of thawing and freezing. The badger bush does not need to fear further depletion, as the area is now a nature reserve. Follow the signposted path to the right up to the gliding fold, where you will find more information.

Aschestrom, © Vulkanregion Laacher See

Aschestrom in Bad Tönisstein

Almost 13,000 years ago, glowing clouds from the Laacher See volcano raced down the Brohltal and filled it with loose volcanic masses. This impressive spectacle can still be seen here today. Follow the road on the right behind the building complex and go uphill for a few meters. On the slope to the right, the layers of ash (trass) that have settled on the rocks of the older basement can be clearly seen. And where volcanoes were active, mineral springs are usually not far away.