Inside the Volcano - Thrihnukagigur Magma Chamber

The Thrihnukagigur volcano is dormant. It last erupted over 4,000 years ago. There are no indications of it erupting again in the near future. The volcano’s name, quite unpronounceable for anyone other than locals, would be directly translated as "Three Peaks Crater".

The three craters (one of which you will be descending into) are prominent landmarks, standing against the sky on the highland edge, about 20 km (13 miles) southeast of the capital area, and within the protected area of Blafjoll Country Park.

The most north-easterly of the three peaks is a small cinder cone, standing about 35 m/100 ft higher than its surroundings. At the top of this cone is a funnel-shaped opening, about 4×4 m (12×12 ft) wide, this is the entrance of a huge 120 m (400 ft) deep, bottle-shaped volcanic vault, measuring 50×70 m (160×220 ft) at the bottom. Volcanic passages continue down to the southwest, to a total depth of about 200 m (700 ft).

The beauty of the crater mostly consists of the various coloration found inside and its enormous and to some extent intimidating size. To put it in context, the ground space is equivalent to almost three full-sized basketball courts sited next to each other and the height is such that the full sized Statue of Liberty would easily fit into the chamber. So make no mistake – this chamber is colossal!

You will spend up to an hour inside the volcano (or less if you prefer), and there is plenty of time to take as many photos as you wish. However, you are not allowed to take away rocks and stones from the crater. Expert guides will be with you at all times, in the cable lift and on the ground in the magma chamber.

While waiting for everyone in the group to complete the volcano visit, you will have the opportunity to enjoy a traditional Icelandic meat soup, hot coffee / tea / chocolate and perhaps some sweets. Don´t be surprised when we ask for your email – we would like to send you a quick survey to complete after the tour.

Finally, accompanied by a guide who is with you at all times, you walk back over the lava field. The coach will be waiting for you in the parking lot, ready to drive you back to Reykjavik.

Pickup in Reykjavik: Pick-up starts 30 min before departure. See the booking system for available departure times. Please be ready at your selected pickup location when pickup begins.

* Important note regarding pick-up: The best option to join the tour is simply to take advantage of our complimentary hotel pick-up service by selecting your hotel or guest house from the drop-down list when booking your tour. We urge you to be ready outside the lobby 30 minutes before the tour departure time.

Alternatively, you can make your own way to the Gray Line Bus Terminal in Holtagarðar, 104 Reykjavik. Please arrive at least 30 minutes prior to the tour departure time stated on the voucher and introduce yourself at the Sales Desk for check-in.

Where is the meeting point?

The meeting point is at a ski cabin, located in Bláfjöll (the Blue Mountains). It takes about 30 minutes to drive there from Reykjavík. The name of the cabin is Breiðabliksskáli.

When to be there?

When choosing the "Meet on location" option, please make sure that you arrive at the meeting point 5-10 minutes before the start time.

Fitness level: Moderate (the difficulty is 2–3 out of 5). No knowledge of hiking or climbing is required. The hike is on slightly hilly and uneven ground. This is NOT a tour for those in limited physical shape.

Distance walked: 3 km (2 miles) each way for some 45–50 minutes, with a guide

Don’t worry, expert guides will be with you at all times and you can rest assured extreme safety precautions are taken every step of the way.

We ask all visitors to behave responsibly during the tour. This environment is extremely sensitive and we expect all visitors to leave no footprint behind. Whatever you carry in with you, you must also carry out.

Simply put, Iceland is one giant geological hotspot. The country is one of the most active volcanic regions in the world, with eruptions occurring every 3–4 years on average. But why is Iceland so active? It is mostly due to its location on the Mid-Atlantic Ridge, where the Eurasian and North American plates are moving apart – and therefore literally opening the earth’s crust. The Thrihnukagigur volcano sits in the center of this ridge.