Plizio Visual Lab

Danube Sinkhole

Plizio editorial teamData Sources
Landmark
—°10
Danube Sinkhole (Germany)

Weather…

The Danube Sinkhole (Donauversickerung) is a globally significant geological phenomenon in the Upper Danube Nature Park in Baden-Württemberg. Between the towns of Immendingen and Möhringen, the water of the young Danube disappears completely for about 150 to 200 days a year into fissures and crevices of the karstified Jurassic limestone. Underground, the water carves its way through a branching cave system over a straight-line distance of about twelve kilometers before resurfacing at the Aachtopf, Germany's most powerful karst spring. From there, it flows via the Radolfzeller Aach into Lake Constance and thus into the Rhine, representing a spectacular hydrological connection between the Danube and Rhine river systems. During full seepage, the riverbed of the Danube lies completely dry for kilometers, allowing hikers to walk on the stony ground. This phenomenon is a striking example of the ongoing 'capture' of the Danube by the Rhine system, which could eventually lead to the upper course of the Danube draining permanently into the Rhine.

Best time to visit & climate

The most pleasant time to visit is Jun–Aug.

JanFebMarAprMayJunJulAugSepOctNovDec
Avg °C-2-138121618171393-1
Rain mm6854666710910810910676806877

📋 Practical info

📍
Address
Donaupark, 78194 Immendingen
🕒
Hours
24/7
💶
Entry
free
🌐
🚌
Transit
Immendingen train station (Ringzug), approx. 15-minute walk to the sinking area
🅿️
Parking
Parking lot at Donauhalle Immendingen, free of charge
Accessibility
Paved gravel paths available, direct access to the riverbed however stony and uneven
📷
Photos
Photography permitted at all times
Best time
Summer months July and August, as the sinking is often completely observable then
🎧
Audio guide
no

Geography

Coordinates
47.93000, 8.76000

Facts

  • The Danube seeps away completely for approximately 150 to 200 days a year.
  • The water resurfaces at the Aachtopf after a 12 km underground journey.
  • The phenomenon was first scientifically documented in 1874.
  • Hydrologically, the water switches here from the Danube to the Rhine system.
  • During dry periods, hikers can walk directly on the stony riverbed.
  • Geologically, this is an example of stream capture through karstification.

Explore nearby

Notable places around

Route planner — Car & Motorhome

Where do you start? We build the route here, with stops and country notes along the way.

Vehicle
Only stops with (optional):

© OpenStreetMap contributors · OpenRouteService

Sights in the town Danube Sinkhole (10)

Donauversinkung

The Danube seeps into the karst here for about half the year. Part of the water resurfaces at the Aachtopf spring.

Unteres Schloss🏰 castle

Building in Immendingen. The Lower Castle now serves as a residential and commercial property.

St. Theopont und Synesius

Church building in Hattingen, part of Immendingen. It is dedicated to Saints Theopont and Synesius.

Burg Hewenegg

Deserted castle site in Baden-Württemberg. Only a few wall remnants of the former castle remain.

ForstBW Arboretum Höwenegg

Arboretum on the Höwenegg hill. Planted with various tree species, it is a place for walks.

Pfarrkirche St. Peter und Paul

Church building in Baden-Württemberg. The parish church is dedicated to Saints Peter and Paul.

Oberes Schloss🏰 castle

Building in Immendingen, Freiburg region. The Upper Castle is a historic structure in the town.

Höwenegg

Nature reserve in Baden-Württemberg. It protects the landscape and habitats of the Höwenegg area.

St. Jakobus und Johannes

Church building in Immendingen, Baden-Württemberg. It is dedicated to Saints James and John.

Burgstall Immendingen

Deserted castle site in Immendingen. The exact location is only traceable through archaeology.

Sights nearby

Frequently asked questions

When is the best time to see the Danube sinkhole?
It is most impressive during dry summer months when the Danube disappears completely into the riverbed on many days.
Where does the water actually go?
The water flows underground through karst rock and resurfaces 12 km to the south at the Aachtopf spring.
Is there an entrance fee?
No, the Danube sinkhole is a freely accessible natural phenomenon and does not cost any admission.
Where can I park for the hike?
Parking is available in Immendingen or Möhringen, where well-marked trails lead directly to the sinkhole sites.
Can you walk in the dry riverbed?
Yes, during total dry-ups, you can carefully walk in the gravelly riverbed and see the sinkholes up close.
Danube Sinkhole: where is it located?
Danube Sinkhole is located in Baden-Württemberg, Germany.
Danube Sinkhole: what is there to see?
Highlights include Donauversinkung, Unteres Schloss, St. Theopont und Synesius.
Danube Sinkhole: when is the best time to visit?
The most pleasant time to visit is Jun, Aug.
Danube Sinkhole: why is it worth visiting?
The Danube Sinkhole (Donauversickerung) is a globally significant geological phenomenon in the Upper Danube Nature Park in Baden-Württemberg.
View on map → The Top 50 Attractions → OpenStreetMap →
Europe
Explore with Plizio Discover more places in Europe
More places in Germany →

Nearby cities