Kerið Crater, formed 6,500 years ago, is a striking volcanic caldera in Iceland’s Western Volcanic Zone. Its red rock slopes, covered in green moss, surround a vivid aquamarine lake. Unlike explosive craters, Kerið collapsed after its magma chamber emptied.
Summary Description
Highlights
Description
Kerið Crater was formed 6,500 years ago and lies at the northern end of a row of craters known as Tjarnarhólar. It is part of the Western Volcanic Zone which also includes the Reykjanes peninsula and Langjökull Glacier. The caldera is approximately 55 m deep, 170 m wide, and 270 m across, and is made up of a unique red volcanic rock.
Visitors to Kerið will be able to hike down one of its sloping walls blanketed with deep green moss, and admire the stunning aquamarine lake at the bottom. The lake is shallow, but its vivid color is due to minerals from the soil.
Kerið was not formed by a volcanic explosion, but rather a cone volcano that erupted and emptied its magma reserve. The weight of the cone then collapsed into the empty magma chamber, creating the current crater. The water in the bottom of the crater is at the same level as the water table and is not caused by rainfall.
Included / Excluded
What's Included
- Parking
- Admission
Important Information
Know Before You Go
- Be prepared for changing weather conditions; sturdy shoes and layered clothing are recommended.
- Plan for around 30–60 minutes to fully enjoy the site.
- The rim trail is an easy walk, and the descent to the lake involves a moderate, gravel path.
Cancellation
Cancellation Policy: standard
Cancellation Cutoff: 24 hours
Cancellation Notes: Up to 24 hours before the beginning of the activity: full refund Less than 24 hours before the beginning of the activity or no-show: no refund
Options
Kerið Crater Admission
| RETAIL PRICE | |
|---|---|
| Adult (13-64 years) | 600 kr. |
Additional Information
Kerið is open during daylight hours
