アルプスの峡谷・トップ20

Force of nature and man becomes very small

The waterfalls are very impressive

You can discover a lot on the way to the gorge.

Magnificent waterfalls, especially after heavy rainfall. The sounds are very impressive.

From 1910 to 1912, the Partnach Gorge, which is up to 80 meters deep, was opened up for tourism under the most difficult conditions and at great financial expense.

The sign above the entrance to the gorge, a popular photo motif, shows the time it was opened up in the years 1910-1920.

Lower entrance to the gorge. here you can buy the tickets

The Partnach Gorge is a 700-meter-long gorge in the Reintal near Garmisch-Partenkirchen, cut by the Partnach torrent to a depth of more than 80 meters in places. The valley floor is at about 800 m above sea level in the middle of the gorge. In 1912, the Partnach Gorge was declared a natural monument. The path always runs on the right side of the stream. In the Middle Triassic, around 240 million years ago, dark gray, relatively hard layers of alpine shell limestone, known as Wurstel limestone or Knollenkalk, were deposited on the bottom of a shallow sea in the area of today's Partnach Gorge. On the bulging layers of this rock, you can still often see traces of burrowing and feeding by the sea creatures of that time. Around five million years later, significantly softer marls were deposited in the same sea basin, which are now known as the Partnach layers. During the later Alpine folding, the so-called Wamberger Saddle was formed from these rock layers. The erosion power of the Partnach, fed by the Schneeferner on the Zugspitzplatt, was great enough to quickly erode the softer layers, keep pace with the ongoing uplift of the terrain and thus also cut into the hard alpine Muschelkalk. Today, the river forms the typical narrow valley shape of a gorge in the Muschelkalk area, while to the north and south of it, in the areas of the softer Partnach layers, wider valley shapes predominate. Source: https://de.wikipedia.org/wiki/Partnachklamm