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Hverfjall (Hverfell) - Tuff Cone
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Hverfjall (Hverfell)

description Hverfjall (Hverfell) Overview

Hverfjall, also known as Hverfell, is a prominent tuff ring volcano located in northeastern Iceland, situated near the geothermal area of Lake Mývatn. The crater was formed approximately 2,500 years ago during a short but explosive volcanic eruption. It features a massive, circular crater measuring roughly one kilometer in diameter, with steep walls composed of dark volcanic ash and tuff. The site is a popular hiking destination for tourists, with designated trails leading to the rim for views of the volcanic terrain.

help Hverfjall (Hverfell) FAQ

Where is Hverfjall located?

Hverfjall, also called Hverfell, is in northeastern Iceland near Lake Mývatn. It lies close to the region's geothermal landscapes and is one of the area's most prominent volcanic features.

What type of volcano is Hverfjall?

Hverfjall is a tuff ring volcano formed by a short, explosive eruption. Its broad circular crater is made largely from fragmented volcanic material rather than a typical lava-built cone.

How old is Hverfjall?

Hverfjall formed approximately 2,500 years ago. Its age places it among the volcanic features created during the relatively recent geological history of the Lake Mývatn region.

What does Hverfjall's crater look like?

The volcano has a massive, nearly circular crater surrounded by a dark tuff rim. The name Hverfell is also used for the same feature, so visitors may see both names on maps and travel guides.

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