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How Kjeragbolten Got There

Kjeragbolten is a glacial deposit: a boulder of about five cubic metres left behind during the last glaciation, around 50,000 BC, and wedged into the crevice as the land rebounded after the ice melted faster than the sea rose. It has been sitting there ever since, 984 metres above the Lysefjord.
VolumeAbout 5 cubic metres
Above the fjord984 m / 3,228 ft
OriginGlacial deposit
Left behindAround 50,000 BC
How it is heldWedged in a crevice
How you get onA stride from the side

The mechanism, in plain words

Ice carried the rock, the ice melted, and the rock ended up in a gap. The part people find harder to picture is why it is stuck rather than sitting loosely: as the ice went, the land underneath rebounded upward, and it rose faster than the sea did. The crevice closed on the boulder. The valley below was formed and re-formed by meltwater through many glaciation cycles, so what you are looking at is not one event but a long sequence of them, with a five-cubic-metre souvenir left at the end.

That is also the answer to the question people really mean, which is whether it is going to fall out. It is wedged. It is not balanced.

What it looks like from a couple of metres away

Smaller and more solid than the photographs. The famous images are shot from the side or from below, which flattens the crevice walls out of the frame and makes the rock look like it is floating. Standing on the plateau you can see the two walls of the crevice quite clearly, and the boulder sitting between them, and the effect changes entirely. You step onto it from the side, onto a flat top, with rock on both sides of you. No climbing equipment is needed and none is provided.

Whether that step feels frightening is a separate question, and an honest one: the scary page deals with it. What is not in doubt is the record. There is no recorded death from falling off Kjeragbolten in Norwegian history, which is covered on has anyone fallen.

The queue

On an August afternoon there is a line for the photograph, and it moves at the speed of whoever is currently on the rock. Most people take a minute. Some take five, with the whole family being directed. It is good-natured and it is also the reason to be out there early, which is the argument made on the crowds page.

Local tip

Hand your camera to the person behind you in the queue rather than to somebody in your own group. They are standing in exactly the right place, they have just watched five people get photographed, and you will be doing the same for them ninety seconds later.

What there is to book

Not the trail. Nobody sells a ticket to Kjerag and nobody could, because there is no gate and nobody standing at one. What you pay for is the ride out of Stavanger and the guide who walks it with you, and the road up is open for about five months a year. The options are laid out on the bookings page and compared on the decision page.

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Frequently asked questions

How big is Kjeragbolten?

About five cubic metres of rock, wedged in a crevice roughly 984 metres above the Lysefjord.

Is the boulder going to fall?

It is wedged in the crevice rather than balanced on anything, and it has been there since the last glaciation.

Do you need equipment to stand on it?

No. You step on from the side onto a flat top. No climbing equipment is needed and none is provided.

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