가장 멋진 동굴 11곳

This was created as part of a Stations of the Cross at St. Bartholomew's Church, but the Stations of the Cross were never completed. The rock niche was chosen at the time to recreate the tomb of Jesus. Anyone looking through the bars into the tiny grotto will see a stone tomb surrounded by flower baskets.

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The tomb was created as part of a Stations of the Cross, but the Stations of the Cross were never completed. The rock niche was chosen at the time to recreate the tomb of Jesus. Anyone looking through the bars into the tiny grotto will see a stone tomb surrounded by flower baskets.

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The somewhat overgrown path to the cave suggests that either a lot of hikers are taking photos here, or that something is living there. I didn't look closely and just took a photo.😏

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Another cave

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Not easy to find in summer (sign fallen and heavily overgrown), easier to find in spring

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The rock grotto is the last and only station on the Way of the Cross at St. Bartholomew's Church in Balduinstein.

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If I had read the sign, I would also know who was lying here...oh yes, Jeses. It's just fake. But scary.

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At this point there is a half meter wide gap through the limestone rock in the Landgraben valley.

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The information sign gives information about the rock festival and the Nepumuk figure that stands nearby.

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a wooden plaque with an inscription below an imposing rock formation “In many legends, the wild woman is the good fairy who usually helps poor people during the night. Your apartment is the lonely forest and in it a narrow crevice. "

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A rock grave awaits you at the end of the Way of the Cross

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On the sign there is information about the rock festival and the Nepumuk figure that stands nearby.

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Nature has always been interesting and here it shows what it can do!

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Nice shortcut, if you do not want to Schaumburg.

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Impressive stone formation you will not find everywhere

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Unique rock formations - a look into the history of the earth:

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Unique rock formations. Unique view of the history of the earth.

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The folds of the wild women ________________________________________ We all certainly heard that the Alps, or even the Himalayas, arose from the collapse of two continents. As a reminder, if two continental plates collide, parts of the plates are unfolded, similar to a carpet that is pushed together from two sides. Now someone may say, "Bending stones, that's just not possible." - but it is important to remember that these processes are extremely slow and / or take place at great depth, where there is high pressure and much heat, so that the rock material becomes soft and flexible. This patterning of rocks happens not only on a large scale, in whole mountains and continents, but also on a small scale. The result can be wonderfully examined by the example of the Wildweiberhöhle. To be able to record which rocks fold or bend in which way, the different types of folds are named (e.g., folds, creases, and creases) and their geometry determined (e.g., convolution angle, radius at inflection points, or symmetry). On the basis of the following overview (excerpt), the rock fold of the Wildweiberhöhle is to be determined.   The geometric properties of a fold: • The point with the smallest curvature radius is called a hinge. • The "straight" section is the thigh. • Legs of equal length form a symmetrical fold, unequal legs an asymmetrical fold. • The highest point of a fold is the vertex, the lowest of the trough. • The point where the direction of curvature changes is the turning point. • The distance between the trough hinges or the crown hinges is the wavelength, the perpendicular to the intervening hinge the amplitude. • The opening angle is determined by the tangents on the legs through the turning points. • At opening angles of 120 ° -180 °, this is called an open, obtuse fold. 120 ° -70 ° form an open, acute-angled fold. At 30 ° -70 ° the fold is closed, Below 30 ° it is called "narrow". Sources: Websites: mineralienatlas.de, wikipedia.de (in each case the article about wrinkles) Book: Treatises of the Royal Prussian Geological Institute, Issue 76, 1913 Additional information (No information available!)

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