May 12th. 2012.
We woke up to a rainy ugly, really cold day like Dr. Anna's weather prediction called for. We were really glad that we went up to Krippenstein the day before.
We cooked breakfast, because we had appartmants in this hotel with full kitchen. We left for Werfen and the ice cave around 11 a.m.
This is the google map showing the rout from Hallstatt to Werfen.
It took us about 90 minutes to drive to Werfen and from there we took the narrow mountain road to the cable railway station. This road had a dirt surface, with steep inclines and hairpin bends scratching up the side of the mountain. We parked at the top of the road and supposedly had an about a 10 minute walk to reach the cable railway station. However Whitney felt sick so it took us just a little over an hour. We could see the valley and the river far below, and the castle which sits on a small hill outside Werfen. The weather was pretty bad, however the view with the fog and clouds were incredible.
The cable car was a small one, holding only six people standing. There were two cars on a continuous loop of cable which kept the load fairly well balanced at all times. There were tremendous concrete counterweights which moved in some fashion when the cars moved up and down.
From the upper station we had about a 20 minute walk to the entrance of the ice cave.
"The Eisriesenwelt
(Austrian word
for "World of the ice giants") is a natural limestone ice cave located in
Werfen. The cave is located in the Hochkogel mountain which is part of the
Tennengebirge section of the Alps.
It is the largest ice cave in the world,
extending more than 42km.
The Tennengebirge
mountains were
formed during the late Tertiary period, during the Würm glaciation period of the
Pleistocene. The mountain range, one of the massifs in the Austrian Alps, is the
largest karst plateau
in the Salzburger Alps, and the Eisriesenwelt is located at the rim of this
plateau. Although the cave has a length of 42 km, only the first kilometer, the
area that tourists are allowed to visit, is covered in ice. Eisriesenwelt was
formed by the Salzach river, which eroded passageways into the mountain. The ice
formations in the cave were formed by thawing snow which drained into the cave
and froze during winter.
Since the entrance to the
caves is open year-round, chilly winter winds blow into the cave and freeze the
snow inside. In summer, a cold wind from inside the cave blows toward the
entrance and prevents the formations from melting.
This is an official picture of the cave.
These are the pictures we were not suppose to take.
From Allison Major's Journal
The cave was gorgeous! There were walls and
columns of stalagmites and stalactites all around us. There were so many stairs
to climb up and down throughout the cave. The guide would light up the
caves with a long strip of Mg that made the cave glow with the most beautiful
shades of blue imaginable. Some of the ice walls were 45 feet thick! The only
lights in the cave were our small ancient looking carbide burning lanterns and
the occasional periods when the guide would light the cave with his long strips
of Mg. The cave consisted of limestone, like the rest of all the Alps, that
glittered with frost. It’s another one of those things that the beauty of it
couldn’t be captured in any other way than with the eyes. However unprepared and
hard this day was on everyone due to the cold, high altitude sickness and
hellacious winds on top of the mountain this day held its own kind of magic and
I’m happy we went.
After the cave we drove back to Werfen cold and hungry, soon we found a cool restaurant and had a really good dinner before driving back to Obertraum to our hotel.