# Reintal

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{{Short description|Upper and lower valleys of the River Partnach in Germany}}
thumb|The Upper Reintal from the Zugspitzplatt
The '''Reintal''' ("Rein Valley") is the name given to the upper and lower valleys of the River [Partnach](/source/Partnach) between the  ''[Zugspitzplatt](/source/Zugspitzplatt)'' plateau and the [Partnachklamm](/source/Partnachklamm) gorge. A hiking route to Germany's highest mountain, the [Zugspitze](/source/Zugspitze) runs through the valley.

The valley was formed during the [Würm Ice Age](/source/W%C3%BCrm_Ice_Age) by the Reintal Glacier and then deepened by the Partnach in the post-ice age period after the retreat of the glacier to the periphery of the [Schneefernerkopf](/source/Schneefernerkopf) mountain. The upper Reintal, which was shaped by the glacier and today forms a U-shaped [glacial valley](/source/glacial_valley), ends between the ''Hohe Gaifkopf'' in the west and the [Schachen](/source/Schachen_(Wetterstein)) in the east. The lower Reintal lies in the area of the former glacial lake of the Loisach Glacier, into which the Reintal Glacier flowed from the southwest. It is a [V-shaped valley](/source/V-shaped_valley) and has been predominantly shaped by the Partnach river.

thumb|left|Wetterstein location map
[[File:Luftbild Alpen 04 (RaBoe).jpg|thumb|In the centre of the picture are the Wetterstein Mountains and the Reintal, that runs up to the snow-covered ''[Zugspitzplatt](/source/Zugspitzplatt)'']]
Together with the [Höllental](/source/H%C3%B6llental_(Wetterstein)) valley to the north, the Reintal divides the [Wetterstein Mountains](/source/Wetterstein_Mountains) into several ridges. The northern periphery is formed by the [arête](/source/ar%C3%AAte)s of the [Höllentalspitzen](/source/H%C3%B6llentalspitzen) (2,743 m) and the ''Hohe Gaifkopf'' (1,864 m). The highest points on the southern flank of the valley lie on the [Hochwanner](/source/Hochwanner) (2,744 m), the [Hinterreintalschrofen](/source/Hinterreintalschrofen) (2,670 m) and the [Dreitorspitze](/source/Dreitorspitze) (2,682 m). The valley floor lies at elevations between 1400 m above [NN](/source/Normalnull) at the source of the Partnach river, 1,002 m at the entrance to the gorge of the ''Hinteren Klamm'' and 797 m at the start of the Partnachklamm gorge, in the upper Reintal therefore about 1300 to 850 m above the surrounding mountain peaks. [?] In the upper Reintal the rubble from [rockslide](/source/rockslide)s from the southern faces of the Hochwanner and Hinterreintalschrofen also play a rôle in the shaping of the valley. These have spilled into the old glacial valley, forced back the course of the Partnach to the north and, in places, impounding it.

Around 1800 rockslides created two small lakes, the ''Vordere Blaue Gumpe'' and ''Hintere Blaue [Gumpe](/source/Gumpe)''. On 23 August 2005 the former was completely filled with sediment as a result of heavy rain (200mm in 24h) whereupon high pressure broke the natural dam. The resulting deluge of flood water caused considerable damage further down the valley.<ref name="Leki">Leki.de: ''Wegesanierungsarbeiten im Wettersteingebirge: Sicher wandern zur Reintalanger Hut'' {{cite web |url=http://www.leki.de/23-e_5617,r_429.htm |title=Wegesanierungsarbeiten im Wettersteingebirge: Sicher wandern zur Reintalangerhütte - Trekking - News - - LEKI |accessdate=2009-10-30 |url-status=dead |archiveurl=https://web.archive.org/web/20110719060301/http://www.leki.de/23-e_5617,r_429.htm |archivedate=2011-07-19 }}</ref><ref name="INIST">CAT.INIST: ''The life-span of a small high mountain lake, the Vordere Blaue Gumpe in the Bavarian Alps'' [http://cat.inist.fr/?aModele=afficheN&cpsidt=18806225]</ref>

A moderately steep climbing path to the [Zugspitze](/source/Zugspitze) runs through the Reintal, the section as far as the [Knorr Hut](/source/Knorr_Hut) forming part of the Red Trail of the [Via Alpina](/source/Via_Alpina). The mountain huts in the valley, the Bock Hut and [Reintalanger Hut](/source/Reintalanger_Hut), are used by hikers and climbers as bases for numerous tours.

Due to its great distance from any settlements and because no roads runs up the valley the Reintal is very unspoilt and still very natural, despite being easily accessible on foot. Together with the [Wimbachtal](/source/Wimbachtal) in the [Berchtesgadener Land](/source/Berchtesgadener_Land) it may be considered as one of the most impressive, large, near-natural valley landscapes in the [Bavarian Alps](/source/Bavarian_Alps). The upper Reintal is protected as a [nature reserve](/source/nature_reserve).

== Other photos ==
<gallery>
File:Wettersteinhauptkamm_mit_Reintal_von_S_HQ.jpg|The Blassenkamm and Reintal from the west (from Gatterl)
File:Reintal_vom_Gatterl_HQ.jpg|The Reintal from the west (from Gatterl)
File:Blaue Gumpe vor dem Bergsturz.jpg|The Vordere Blaue Gumpe before its destruction
File:Blaue Gumpe nach dem Bergsturz.jpg|The Vordere Blaue Gumpe after its destruction
</gallery>

{{Commons category|Reintal}}

== References ==
<references/>

== Sources ==
* David Morche: ''Untersuchungen zum fluvialen Sedimenttransport in Einzugsgebieten der nördlichen Kalkalpen (Reintal/Wettersteingebirge und Lahnenwiesgraben/Ammergauer Alpen)'' [http://sundoc.bibliothek.uni-halle.de/diss-online/08/08H202/of_index.htm] [http://sundoc.bibliothek.uni-halle.de/diss-online/08/08H202/prom.pdf]

{{coord missing|Bavaria}}

{{Authority control}}

Category:Valleys of Bavaria
Category:Garmisch-Partenkirchen (district)
Category:Wetterstein

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Adapted from the Wikipedia article [Reintal](https://en.wikipedia.org/wiki/Reintal) by Wikipedia contributors ([contributor history](https://en.wikipedia.org/wiki/Reintal?action=history)). Available under [Creative Commons Attribution-ShareAlike 4.0 International](https://creativecommons.org/licenses/by-sa/4.0/). Changes may have been made.
