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Photo taken from balcony of Staubbach bursting over the cliff edge into the Weisse Lütschine
he name Lütschine dervices from the Celtic name leucos or leuca , meaning "white" or "bright, shiny" and so for clarity it became the "Weisse Lütschine". Flowing 8.6 km through from the Stechelberg area through the Lauterbrunnen Valley to Zweilütschinen (two Lütschine). Here it joins the Schwarze Lütschine, or Black Lütschine that has flown 12.3km from Grindelwald. Folk tales say the villagers of Lauterbrunnen never even washed so their could remain white.
Made up of rain, snow melt and ice, each of which has its own footprint in the river water makeup, researchers can determine the origin of the waters from the to the catchment area of the Weisse Lütschine (165 km2). Researchers also consider the influence from soil and geological features over which the waters flow and have found that snowmelt dominates between April and July with an annual total of almost 40% of the runoff at that time. This glacier melt occurs mainly between July and September and reaches a quarter of the annual total outflow of the Weisse Lütschine. The researchers say that the rain component measured and isolated between May and October is striking and contributes a third of the waters for the Weisse Lütschine. (Source: Gabriel Peier, 20.12.2016 Hydrology Group, Bern University http://www.hydrologie.unibe.ch/projekte/poster/Poster_PEIER.pdf)
Where is the Weisse Lütschine’s source? From 72 and more waterfalls and streams flow over the massive magnificent walls surrounding the luminous Lauterbrunnen valley into the rushing, bustling Weisse Lütschine. From the Schilthorn side these include the Sefinenlutchine, Schiltbach and the mighty Murrenbach Falls.
From the south, high up are 5 or 6 contributing streams from the direction of the Mittaghorn, Grosshorn, Tschingelhorn, Gspaltenhron (the pyramid-like shape) and Breithorn (German for "broad horn". Breithorn is the huge concical shining mountain peaked with translucent ice at the southernmost part of the valley. The Breithorn (3,780 m) can often have the mystical pinkish aurora or optical phenomenon at sunset called Alpenglow. This massive straddles the Cantons of Bern and Vallias and is part of the border between Lauterbrunnental and the Lötschental valleys. This Breithorn is not to be mistaken for the other Breithorn near Blatten at 4,164 m and part of the Pennine Alps mountain range.
At Stechelberg, the fervent torrents of the higher up Schmadibrunnen purge into a 60m cascade and force their way from the Breithom Glacier roaring downwards with a noise like thunder to the hydro station. Managing the power of these waters is a constant concern for the valley authorities as they move the rocks around and yet the majesty of these roaring pure waters have their own wilfulness and draw attention, almost demanding to be watched.
At the curved wooden bridge near the power station in Stechelberg one can be lured by several gushing, racy white waters, seemingly always is a hurry to become the impetuous waters of the Lütchine waters that come from the Sefinenlutchine and Schiltbach. Walking upward from Stechelberg towards Gimmelwald is enchanting to watch playful and forceful waters making rock sculptures on their way. The Spiessbach above Gimmelwald pours over a monstrous rocky outcrop under which one can stand and lookout through the curtain of water raging from overhead. A slippery but worthwhile side path from Gimmelwald to Murren.
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