Tufa runnels or fissure ridges
Some of the rarest travertine formations are fissure ridges or (unoficcially) tufa runnels. Tufa runnels are defying our understanding about streams: we have used that streams flow where it is lower. In a case of active fissure ridges we see the opposite: there is a ridge or even a wall and… on the top of this ridge (or wall) flows a lucid stream of clean water!
Tufa runnels are formed by lime-rich springs and often are formed along existing fissures which emit spring water. As the lime is deposited on the bed of stream, it rises higher and higher. But, as the travertine is deposited on both sides of the stream (helped by moss), it can not "escape" and continues to rise up together with the wall. Tallest fissure ridges might get more than 15 meters tall and might be more than 500 m long.
In most cases tufa runnels are just elongated ridges of travertine with narrow chanel on the top. Sooner or later the stream by some natural occasion is diverted away – then travertine gets dry, overgrown with grass and bushes and finally degraded beyond recognition.
In some, very rare cases though there forms a true natural wall of travertine with a stream on the top of this wall.
Wonder of Usterling
One of the most impressive tufa runnels – may be the most impressive of them all is located in cozy countryside of Bavaria, near the beautiful historical town of Landau an der Isar.
Here, on a forested slope protrudes a weird wall. It has formed over several millenia and now is 37 m long and up to 5.4 m tall. Its summit is some 40 – 50 cm wide. Most impressive characteristic of this wall is that it is… a wall. Its base is only a little thicker than the summit. Geological process continues – along the upper rim of the wall runs a stream and every year the wall grows per some centimeters. Stream is slightly meandering – also the wall repeats these small meanders. At the end the stream forms a small waterfall and falls down, further turning into a common brook.
Travertine wall is covered with vegetation – with moss (e.g. Cratoneuron commutatum) and algae. It plays an important role in the development of wall – dead parts of plants and algae are quickly covered with lime – thus vegetation facilitates faster growth of the wall.
This is not the only tufa runnel in Bavaria – there are known at least 16 other ones but none of the other ones has formed such outstanding wall as tufa runnel in Usterling.
Human assistance in the name of John the Baptist
People have noticed this unusual natural formation long ago. Very interesting, painted Late Gothic relief is located in the local Usterling church – it shows that Jesus is baptised by John the Baptist right at this peculiar cliff! This relief was made in 1520 and shows the Groving Rock as it looked back then. Thanks to this locals call the cliff Johannisfelsen.
Unusual natural landmarks often have served as cult sites for Pre-Christian religions. It is possible that the Groving Rock also had such importance – up to these days some believe that water of this spring can heal eyes. Thanks to this belief in earlier times this was well known pilgrimage site. Now people come here on St.John’s Day, 24th June. One can speculate that the church has taken over some Pre-Christian midsummer festivities and replaced it with the cult of John the Baptist.
At the wall is standing small chapel – St.Johannes-Kapelle. Local clergy has taken care of the cliff for centuries – it has been cleaned of grass, soil and shrubs. During the winter the water was channeled away to avoid damage by the ice. We can be sure that this amazing landmark now exists only thanks to this care.
Growing Wall is natural monument since 1937 and currently nature conservation authorities have taken over the care of it.
- Wachsender Felsen von Usterling – shield at the site. File accessed on May 1, 2017
|Coordinates:||48.6622 N 12.6486 E|
|Categories:||Spring tufa, travertine and other formations, Springs|
|Address:||Europe, Germany, Bavaria, Dingolfing-Landau district, some 4 km west from Landau an der Isar, in Usterling, on a wooded slope|
|Name in German:||Wachsende Felsen von Usterling, Johannisfelsen|
Germany has picturesque landscape and rather many natural landmarks, but these are overshadowed by the rich and diverse cultural heritage. From time to time immense values have been lost in warfare, but Germans have duly rebuilt their cultural treasures and are constantly creating new values.
This category includes very diverse landmarks which have one thing in common: all of them are created by springs which are depositing chemical sediments – silica, carbonates, salt or other chemical compounds.
Travertine is an excellent contribution, condensing the large literature base on travertine into one book. The book’s strength is the thorough, well-organized, and interdisciplinary survey of travertine, reflecting the author’s extensive experience with the topic. Each chapter in this book provides and excellent starting point and literature review to launch more detailed inquiries about travertine and travertine depositing systems.
Looks at the earth’s crust, sedimentary strata, erosion, geologic mapping, fossil beds, folds and faults, volcanoes, and glaciers.