Plattspitzen

Plattspitzen

The Plattspitzen from the northeast (Jubiläumsgrat)
Highest point
Elevation 2,680 m (8,790 ft)
Coordinates 47°23′45″N 10°59′17″E / 47.39583°N 10.98806°E / 47.39583; 10.98806Coordinates: 47°23′45″N 10°59′17″E / 47.39583°N 10.98806°E / 47.39583; 10.98806
Geography
Plattspitzen

12 kilometres southwest of Garmisch-Partenkirchen, Bavaria/Tyrol

Parent range Wetterstein Mountains, Northern Limestone Alps
Climbing
First ascent 1871 by Hermann von Barth
Normal route From the Zugspitzplatt to the northwest

The Plattspitzen is a 2,680 metre high mountain in the Wetterstein Mountains on the border between Germany and Austria. It is a very striking mountain and the southern companion of Germany's highest peak, the Zugspitze, located at the opposite end of the ledge known as the Plattumrahmung. The mountain has three summits: the eastern summit, known as the Gatterlspitz (2,680 m), the middle summit (Mittelgipfel, 2,674 m) and the western summit (Westgipfel, 2,676 m). It was first climbed in 1871 by Hermann von Barth, who conquered all three peaks alone departing from the Zugspitzplatt ledge. At that time the mountain was also known as the Wetterschrofen.[1]

Location

The mountain is made of Wetterstein limestone and lies just under 3 kilometres south of the Zugspitze, forming the southern cornerstone of the Zugspitze massif. One kilometre to the west it meets the higher, but much less prominent Wetterspitzen (2,746 m). To the south, towards the valley of the Gais, the mountain has a very steep and rugged face, about 700 metres high.

Base and climbing

The Plattspitzen can be climbed from the Knorr Hut (2,052 m) to the northeast by crossing the Platt along the northwestern ridge, parts of which are medium difficulty (in places up to Grade III).[2] The duration of this route up to the eastern summit is about five hours.

References

  1. Hermann von Barth: Aus den Nördlichen Kalkalpen (1874)
  2. gps-tracks.com

Sources and maps

This article is issued from Wikipedia - version of the 11/28/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.