Kjeragbolten is a 5 m³ boulder wedged in a mountain crevasse by the edge of the Kjerag mountain. It is possible to walk onto the rock without any equipment, but there is a direct 241 m drop below and then another 735m gradient down to Lysefjorden. The name means "Kjerag Boulder" or "Kjerag Bolt".
it was snowing and the flakes came upwards, it was bizarre. in the morning i was pretty sure of myself to go on this rock and make a dance. ha, but that was in the morning.
first step was to get around a edge to climb on the actually stone. that was not a problem even when a lot of people say that is the hardest bit. i was standing there and i think i just standing to long and it was a too long thinking. man i can tell you my heart was on 200 beats a second and my pans filled up ;-) than i did the step. one foot on it and than.....that was it. i just could not do it my second leg was like concrete. couldn't get on it.
still stand retreat
angered about myself
this was on the way down again. skurill(german) is the word i just can describe this decent. we have been a group of approx 10 and still it was hard to find the way back. the track is marked with red painted dots on stones every 50 to 100 meters. it just doesn\t help when the snow comes side wards and covering these bloody dots. so we sprayed out in a line just in few side and did make our way down. slowly but surely. alone it could have been hours and hours to find the down. it was cloudy, stormy and up there in this kind of condition everything looks the same. IT WAS SO COOL.
Preikestolen tour
Preikestolen or Prekestolen, also known by the English translations of Preacher's Pulpit or Pulpit Rock, and by the old local name Hyvlatonnå (“the carpenter-plane’s blade”), is a massive cliff 604 metres (1982 feet) above Lysefjorden, opposite the Kjerag plateau, in Forsand, Ryfylke, Norway. The top of the cliff is approximately 25 by 25 metres (82 by 82 feet), almost flat. The cliff was formed during the Ice age, about approximately 10,000 years ago, when the edges of the glacier reached the cliff. The water from the glacier froze in the crevices of the mountain and eventually broke off large, angular blocks, which were later carried away with the glacier. This is the cause of the angular shape of the plateau. Along the plateau itself there continues to be a deep crack. The cracks show that the plateau will at some point fall down, but all the geological investigations have revealed that this event will not happen in the foreseeable future, and the geologists have thus confirmed the safety of the plateau
it was a beautiful walk and the few is stunning, but there is for sure a down on this spot. tourist and tourists and tourists. i should not say anything because i have been there as well but there are just too many of us. the track is a bit like a autobahn and not really a challenge. still you if you are in this area you should do it, its a pretty cool plateau.
mystic
on the way down. that was the first time that i could get rid off my raincoat ;-)
the few down towards the sea
after all the hikes and not much people around we decided to visit bergen the most rainy town in norway. the world is just funny. we have been on tour since almost 3 weeks and in bergen we did have the most beautifully weather on the whole trip. you have to love things like that.
on the way to bergen with the ferry
see food. that was so yummy could be mine ;-) old, worn out but cool
Bergen is a city and municipality in Hordaland on the west coast of Norway. As of 10 November 2012, the municipality had a population of 267,200 and Greater Bergen had a population of 392,900, making Bergen the second-largest city in Norway. The municipality covers an area of 465 square kilometers (180 sq mi) and is located on the peninsula of Bergenshalvøyen. The city center and northern neighborhoods are located on Byfjorden and the city is built around the Seven Mountains. Many of the extra-municipal suburbs are located on islands. Bergen is the administrative center of Hordaland and consists of eight boroughs—Arna, Årstad, Åsane, Bergenhus, Fana, Fyllingsdalen, Laksevåg and Ytrebygda.
Trading in Bergen may have started as early as the 1020s, but the city was not incorporated until 1070. It served as Norway's capital from 1217 to 1299, and from the end of the 13th century became a bureau city of the Hanseatic League. Until 1789, Bergen enjoyed exclusive rights to mediate trade between Northern Norway and abroad. The remains of the quays, Bryggen, is a World Heritage Site.
Bryggen (Norwegian for the Wharf), also known as Tyskebryggen (the German Wharf) is a series of Hanseatic commercial buildings lining the eastern side of the fjord coming into Bergen, Norway. Bryggen has since 1979 been on the UNESCO list for World Cultural Heritage sites. The name has the same origin as the Flemish city of Brugge.
the back parts of the bryggen. small alleys with little bridges from one house to the next. on the roof of the houses you can see the opening where they haled up the fish to dry it in the roof spaces.
Jostedalsbreen (English: Jostedal Glacier) is the largest glacier in continental Europe. It is situated in Sogn og Fjordane county in Western Norway Jostedalsbreen lies in the municipalities of Luster, Sogndal, Jølster, and Stryn. The highest peak in the area is Lodalskåpa at a height of 2,083 metres (6,834 ft).
Jostedalsbreen has a total area of 487 square kilometres (188 sq mi). The highest point is Høgste Breakulen at 1,957 metres (6,421 ft) above mean sea level. Branches of the glacier reach down into the valleys, for instance Bøyabreen in Fjærland and Nigardsbreen, both at 300 metres (980 ft) above sea level. The thickest part of the glacier is 600 metres (2,000 ft). Jostedalsbreen has a length of a little more than 60 kilometres (37 mi) and covers over half of the national park which was established in 1991 and covers 1,310 square kilometres.
i wanna go there to do a bit of ice climbing. to late in the season and there have been just other tours available. so we decided to take the kayak and make a little hike on the glacier. ice cold water and kayak just seemed to be the right thing to do. cool bananas. it was awesome even i still have the opinion that you should not book tours.
it was an 1.5 hours paddle over the glacier lake
until we hit the bottom of this massive ice.
it was very impressive
short brake
and than preparing for the walk
first i took a quick flight over the glacier just to make sure we will be safe ;-)
a couple of the crevasses are big enough to hover with an helicopter in it. at least that was one of the stories the guide told us. yeah sure. what ever.
looks cool but is just a little hole at the side of the glacier where probably every tourist gets in to take one of these pictures where it looks like you are mr ice ;-)
direction lom we drove over the sognefjell pass. it was already dark when we hit the highest point of the pass and actually i did want to camp on the other site a little bit more less an altitude. just cruising along the way up on a very small pass road the wheels start spinning. ice, ice, ice. it was one icy mirror. not a chance to go further. the worst thing was i could not just stay there. so did have to back up all in reverse. half an hour driving, it was more a bit gliding, down the hill. and once more on this trip my heart beat went up. 20 cm at the time. break, sliding. stop. 20 cm, break, sliding. by the time we have been on a spot where i could actually turn the car i was exhausted and ready for cigarette ;-) no more further. our campsite probably 1500 m above sea, cold windy and the worry we could get stuck here for a couple of days. mike with his blue eyed thinking didn't have even snow change with him. one more lesson learned. don't go without a winter equipment on tour in norway even when its summer ;-)
nice and icy
Lom Stave Church (Norwegian: Lom stavkyrkje) is a stave church situated in Lom municipality in the Gudbrandsdal district of Norway. The church is a triple nave stave church that uses free standing inner columns to support a raised section in the ceiling of the main nave. This type of church is amongst the oldest Stave Churches. The church was first situated in a sub valley to the valley Gudbrandsdal in Oppland County, some 60 kilometers (37 mi) west of Otta.
The church dates to approximately second part of 12th century, but was rebuilt into a cruciform church during the 17th century. The chancel was decorated in 1608, and the nave was enlarged towards west in 1634. The cross section was added in 1663, but this was made in stave like frame work. A complete restoration took also place in 1933, and a smaller one in 1973. This stave church is actually one of just a very few stave churches of which the original medieval crest with a dragon head still survives
last stop was the Arctic circle. where i could build another memorial for one of the sponsors for my donation idea. thanks HELGA. i will spend your money well further down the track.
it was a cool trip with shit loads of cool things we have done. thanks again to my visitor jasmin ;-)
happy days