Stapafell

Natural landmarks of Iceland

TypeHyaloclastite mountain

RegionWest Iceland

DifficultyModerate

Stapafell is about 526 m high ridge shaped fresh momentum and won volcanic mountain on the south slopes of the Snæfellsjökull, about 3 km north of the cave and above Arnarstapa. No road leads up the mountain to the north east of Kýrskarð and Jokulhals to Ólafsvíkur. Norðasutan the famous cave's Bottom Mount which is Rauðfeldsgjá and you can hike along the canyon towards the bottom. Top of the Rock Stapafell Cross Fell, an ancient icon of the cast is considered to be the residence of dulvætta.

Source: See here
photo: Anton Stefánsson

More details

Rock typeHyaloclastite / palagonite

Formation typeSubglacial volcanic mountain

Best seasonSummer

Hiking routeHikeable

Glacier coverNot glacier covered

VolcanismVolcano

Volcanic activityNot an active volcano

Overview

Stapafell is an Icelandic mountain whose character reflects the interaction of volcanic bedrock, glacial erosion and a harsh maritime climate.

History

Stapafell has primarily served as a regional landmark and part of the traditional landscape of its surrounding area. Cultural context: Stapafell contributes to the visual and cultural identity of its region and is part of the long relationship between Icelandic communities and mountain landscapes.

Geology

The geology of Stapafell is best understood within the wider volcanic history of Iceland. Glaciers, frost weathering and running water later modified the original volcanic landform.

Hiking

Hiking possibilities around Stapafell vary by route, season and access point. Exact distance and duration should be taken from a dedicated route record where available.

Safety

Conditions on Stapafell can change quickly. Wind, low cloud, rain, snow, ice and loose ground can all increase difficulty. Visitors should check current conditions and choose routes appropriate to their experience. Practical visitor information: Visitors should choose an experience that matches current conditions and their own experience

Views & surroundings

From higher ground, views generally open across neighbouring valleys, ridges and lowlands, depending on weather and access. Surroundings: Stapafell should be understood as part of its wider Icelandic landscape, including neighbouring valleys, ridges, lowlands and volcanic or glacial features. Nearby highlights: Natural attractions and mountains near Stapafell

Interesting facts

Stapafell is part of the broader story of how Icelandic mountains are built by volcanism and reshaped by ice and erosion. Understand Stapafell by noticing not just the summit, but also its rock, slopes, neighbouring landforms and position within the wider landscape. Notable features: The importance of Stapafell lies in the way its shape, geology and regional setting combine to create a distinct local landscape feature. Summary: Stapafell is a regional Icelandic mountain whose form reflects volcanic bedrock, glacial erosion and ongoing weathering. Themes: Stapafell; mountains; nature; hiking; geology

Frequently asked questions

What is special about Stapafell?: Stapafell is part of Iceland's mountain landscape, shaped by the combined effects of volcanism, glaciers, erosion and a harsh maritime climate.
How was Stapafell formed?: The geology of Stapafell is linked to Iceland's volcanic bedrock, while glaciers, frost, running water and weathering later reshaped the landform.
What should visitors know before visiting Stapafell?: Conditions around Stapafell can change quickly. Check access and weather before travelling, stay on established routes where possible and avoid damaging fragile natural surfaces.