BorisJ Photography
Getting closer
I'm getting closer to the Preikestolen.
Preikestolen or Prekestolen, also known by the English translations of Preacher's Pulpit or Pulpit Rock, is a famous tourist attraction in Forsand, Ryfylke, Norway. It consists of a steep cliff which rises 604 metres (1982 feet) above Lysefjorden, opposite the Kjerag plateau, with an almost flat top of approximately 25 by 25 metres (82 by 82 feet).
The old local name of the site is Hyvlatonnå (English: Planned Tooth). The name Prekestolen (without the i) was coined around the year 1900 when the local tourist organisation, Stavanger Turistforening wanted to promote the site for trekking. The "i" was added later to concord with Nynorsk, the official local form of Norwegian, and the site is now known both locally and officially as "Preikestolen."
The cliff was formed during the ice age, 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. Due to these cracks, the plateau will at some point fall down, but all the geological investigations have revealed that this will not happen in the foreseeable future, and geologists have confirmed the safety of the plateau.
Rogaland,
Norway
Copyright © BorisJ Photography - Boris Jusseit - all rights reserved - please do not use this image on any media without my permission.
Getting closer
I'm getting closer to the Preikestolen.
Preikestolen or Prekestolen, also known by the English translations of Preacher's Pulpit or Pulpit Rock, is a famous tourist attraction in Forsand, Ryfylke, Norway. It consists of a steep cliff which rises 604 metres (1982 feet) above Lysefjorden, opposite the Kjerag plateau, with an almost flat top of approximately 25 by 25 metres (82 by 82 feet).
The old local name of the site is Hyvlatonnå (English: Planned Tooth). The name Prekestolen (without the i) was coined around the year 1900 when the local tourist organisation, Stavanger Turistforening wanted to promote the site for trekking. The "i" was added later to concord with Nynorsk, the official local form of Norwegian, and the site is now known both locally and officially as "Preikestolen."
The cliff was formed during the ice age, 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. Due to these cracks, the plateau will at some point fall down, but all the geological investigations have revealed that this will not happen in the foreseeable future, and geologists have confirmed the safety of the plateau.
Rogaland,
Norway
Copyright © BorisJ Photography - Boris Jusseit - all rights reserved - please do not use this image on any media without my permission.