Höllental (Wetterstein)

	Höllental (Wetterstein) The ''Höllental'', English translation "Hell Valley" or "Valley of Hell" is one of the routes on the German side leading up the Zugspitze on the German-Austrian border in the northern Alps. It is located in the district of Garmisch-Partenkirchen. See also Zugspitze The Zugspitze (), at above sea level, is the highest peak of the Wetterstein Mountains as well as the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen, and the Austria–Germany border runs over its western su ... Höllental on the German Wikipedia ZUGSPITZE 360° atop the Zugspitze via the Höllental External links Valleys of the Alps Valleys of Bavaria Canyons and gorges of Germany {{GarmischPartenkirchendistrict-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	Zugspitze The Zugspitze (), at above Normalhöhennull, sea level, is the highest peak of the Wetterstein Mountains as well as the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen, and the Austria–Germany border runs over its western summit. South of the mountain is the ''Zugspitzplatt'', a high karst plateau with numerous caves. On the flanks of the Zugspitze are three glaciers, including the two largest in Germany: the Schneeferner#Northern Schneeferner, Northern Schneeferner with an area of 30.7 hectares and the Höllentalferner with an area of 24.7 hectares. The third is the Schneeferner#Southern Schneeferner, Southern Schneeferner which covers 8.4 hectares. The Zugspitze was first climbed on 27 August 1820 by Josef Naus, his survey assistant, Maier, and mountain guide, Johann Georg Tauschl. Today there are three normal routes to the summit: one from the Höllental (Wetterstein), Höllental valley to the northeast; another out of the Reintal (Wetterste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	Garmisch-Partenkirchen (district) Garmisch-Partenkirchen ( Bavarian: ''Garmasch-Partakurch'') is a ''Landkreis'' (district) in Bavaria, Germany. It is bounded by (from the west and clockwise) the districts of Ostallgäu, Weilheim-Schongau and Bad Tölz-Wolfratshausen, and by the Austrian state of Tyrol. History In medieval times the alpine lands were owned by the bishops of Freising and the abbots of Ettal Abbey. In 1803, when the clerical states of Germany were dissolved, the region was acquired by Bavaria. Geography The district is located in the Bavarian Alps and includes the highest mountain of Germany, the Zugspitze (2962 m). The highest peaks are grouped along the Austrian border, where the mountain ridges of the Wettersteingebirge and the Karwendelgebirge rise. Between them the Isar river runs northwards. North of these ridges there is a valley housing the tourist resort of Garmisch-Partenkirchen. The valley together with the surrounding mountains is called the Werdenfelser Land. Further north the ridges ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	Valleys Of The Alps The main valleys of the Alps, orographically by drainage basin. Rhine basin (North Sea) High Rhine Aare Limmat Linth (Glarus) Lake Walen *Seeztal Klöntal Sernftal Reuss *Lake Lucerne Sarner Aa (Brünig Pass connects to the Aare basin) Muota Schächental, Klausen Pass connects to Glarus Urseren Susten Pass connects to the Gadmertal Furka Pass connects to the Goms Saane/Sarine *Sense Gürbetal Lake Thun, Bernese Oberland * Kander **Simmental *Diemtigental (Chirel, Fildrich (Narebach, Senggibach, Gurbsbach)) Suldtal Kiental Engstligental Kandertal , Habkern Brienzersee, Interlaken Lütschine * Saxettal * Schwarze Lütschine, Lütschental, Grindelwald, Grosse Scheidegg connects to Reichenbachtal * Weisse Lütschine, Lauterbrunnental, Lauterbrunnen **Sefinental Giessbach Haslital, Meiringen *Reichenbachtal (Rychenbach, Seilibach), Grosse Scheidegg connects to ... [...More Info...] [...Related Items...] OR:** [Wikipedia] [Google] [Baidu]
picture info	Valleys Of Bavaria A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]