Laacher See: The Caldera in the Middle of Europe Is Bubbling Intensively – Is the Volcano Awakening Again?

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The Laacher See is a caldera in the Rhine Valley of Germany.

And a new video of the crater filled with water shows the lake is bubbling. Is the caldera awakening?

The Laacher See caldera in Germany is bubbling suggesting magma intrusion and degassing, Laacher See caldera Germany Europe bubbling video
The Laacher See caldera in Germany is bubbling suggesting magma intrusion and degassing.

Above, a pristine blue lake filled with boaters and swimmers. Below, magma bubbles and swells.

The Laacher See is a caldera lake situated only ~30 km south of Bonn and ~60 km south of Köln (Cologne), just to the west of the Rhine River.

It is part of the East Eiffel Volcanic Field and the 8-km wide caldera is currently filled with a lake.

Now, most people don’t think of volcanic activity occurring in central Europe, but it is believed that a mantle plume lies below this part of the continent, creating rifting and the volcanism in the Eifel Volcanoes.

And now a recent video of the Laacher See caldera shows the lake bubbling, suggesting that there is still magma degassing under the lake:

The formation of the Laacher See caldera

Laacher See last erupted ~12,900 years ago and that covered a significant area of Europe with ash and tephra. With an estimated Volcanic Explosivity Index value of 6, this eruption was 250 times larger than the eruption of Mount St. Helens in 1980.

Remains of this eruption can be found all over Europe and is often used for dating of sediments. The ash from the eruption can be found in the North Sea and throughout central Europe.

There is some suggestion that the Laacher See eruption could have had a strong effect on the climate of Europe after the eruption and the human populations living there at the time.

Although it has been quiet since the climactic eruption ~12,900 years ago, the caldera should still be considered potentially active as CO2 seeps exist in some parts of the lake, suggesting that there is still magma degassing under the lake.

In fact, the CO2 can be a hazard, supposedly killing some Medieval monks in their sleep. There is no hazard map for Laacher See. If you want to learn more about such explosive lakes read the following post:

The Laacher is still considered to be an active volcano, proven by seismic activities and heavy thermal anomalies under the lake.

Carbon dioxide (CO2) gas from magma still bubbles up at the southeastern shore (mofettes), and scientists believe that a new eruption can happen at any time, which, today, would be a disaster beyond all description.

Below, you will find a recent interview by DW about the ongoing magmatic recharge beneath Laacher See Volcano:

DW: Lake Laach, which is very close to where I’m sitting right now [40 kilometers, or 25 miles from Bonn, Germany] — there are deep earthquakes showing that magma is rising beneath this lake. That sounds… scary. What’s happening?

Dr. Torsten Dahm: We concluded in our work that it is possible that magma is rising. But actually, we cannot say for sure that a large amount is rising.

DW: So I’m going to jump to the big question that I think most people in the Rhineland area of western Germany will wonder when they read this kind of headline, which is — is an eruption imminent?

Dr. Torsten Dahm: No, we don’t think that can be concluded. And we don’t actually expect an immediate eruption very soon, or in the near future.

But it shows us that there is activity going on, and also magmatic activity. And it’s the first time that we have direct evidence, meaning direct in the sense of observing seismic signals. So we know it’s really occurring now.

DW: This volcano is so destructive. 13,000 years ago it erupted with such violence that its ash STOPPED THE RHINE. I still can’t get over that. It makes me wonder, how are we monitoring Lake Laach right now, and what should we improve?

Dr. Torsten Dahm: The ash dam created a temporary Rhine ‘reservoir’ behind it, which ultimately broke as a destructive tsunami

The observations we have now — we’ve only been able to resolve these kinds of signals because we improved a seismic network. But it’s actually not optimal. There are other important signals that should be measured continuously and in real time — for instance, the gas flows, or the chemical analysis of gases, in the places where we know that gas from the deep mantle source is coming to the surface. And also, the little uplift, or deformation, or movement of the surface could be measured today with geodetic data, so with continued GPS [monitoring], for instance. That is not in place at the moment.

DW: This is a lake that has sailboat and rowboat rentals, and you have a lot of Germans heading to this lake in the summertime for a swim. Are you saying that the gases bubbling out of Lake Laach aren’t being actively monitored? Is that typical, to not do that?

Dr. Torsten Dahm: There have been occasional investigations of the gases. So they are monitored. But not in a continuous manner. So we have no real-time monitoring of these gases.

DW: For a report last year I went swimming in a part of Lake Laach where CO2 gases were bubbling up, it was like champagne. So now I’m kind of thinking that maybe wasn’t the best idea.

Dr. Torsten Dahm: So yeah, there is a danger in this region. And everywhere where you have CO2. As you know, [CO2] can be dangerous. I always thought it was forbidden to swim in some areas of Lake Laach, or at least it was not recommended to swim there.

DW: I can tell you that the path I took was well traveled. There was an empty wine bottle, or beer bottle, there. So yeah, it’d be good to monitor those gases!

Dr. Torsten Dahm: I mean with volcanoes, as with anywhere in the world, something could change. The flux of gas, or the amount of gas coming out, might change. And it would be important to know this. 

DW: What’s the next step for your research at Lake Laach?

Dr. Torsten Dahm: We think there are several really open questions which need to be answered and investigated better. And one key question is really whether there are already magmatic reservoirs of larger volumes existing in the shallow crust, or maybe even in the intermediate depths or deeper crust. So this would be very important to know and to understand in order to better understand the real volcanic hazard.

Torsten Dahm is the co-author of a new report published in the Geophysical Journal International entitled, “Deep low-frequency earthquakes reveal ongoing magmatic recharge beneath Laacher See Volcano (Eifel, Germany).”

If you are interested by unknown caldera around the world, I am sure you will love this article about the Chalupas Supervolcano that may erase Ecuador from world’s map during its next mega-eruption:

So do you think this bubbling water is a sign the Laacher See caldera is waking up? More volcanic news on Strange Sounds and Steve Quayle. [Facebook, DW]

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