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F338 Skjaldbreiðarvegur: Across the Shield Volcano

Methven Forbes

14 March 2026

F338 Skjaldbreiðarvegur: Across the Shield Volcano

F338 Skjaldbreiðarvegur: Across the Shield Volcano

The F338 Skjaldbreiðarvegur cuts a remarkable path across one of Iceland's most distinctive geological features, offering intrepid drivers the rare opportunity to traverse the broad shoulders of Skjaldbreiður, the country's most perfectly formed shield volcano. This 28-kilometre highland track connects the Kaldidalur valley to the Þingvellir region, crossing terrain that exemplifies Iceland's volcanic origins whilst providing access to some of the island's most pristine wilderness.

The Shield Volcano Highway

Skjaldbreiður, meaning "broad shield" in Icelandic, rises to 1,060 metres above sea level and spans roughly 10 kilometres at its base. Unlike the dramatic peaks that dominate much of Iceland's volcanic landscape, this ancient shield volcano presents a gentle, dome-like profile that perfectly illustrates how successive lava flows can build massive geological structures over millennia. The F338 traces a route across its northeastern flanks, offering an unparalleled opportunity to experience this geological wonder up close.

The road itself demands respect and preparation. Classified as a mountain road requiring 4WD vehicles, the F338 presents challenges that range from river crossings to loose volcanic scree. The route typically opens in late June or early July, remaining accessible through September depending on weather conditions. The Icelandic Road and Coastal Administration (Vegagerðin) maintains current status updates, though local conditions can change rapidly.

Geological Significance and Formation

Skjaldbreiður represents one of Iceland's finest examples of shield volcano formation, created during a period of intense volcanic activity approximately 9,000 years ago. The volcano's broad, gently sloping profile results from highly fluid basaltic lava flows that spread widely before cooling, building up the mountain's characteristic shield-like shape over numerous eruptions.

The F338 provides direct access to observe these ancient lava fields, where pillow basalts and ropey pāhoehoe formations create an otherworldly landscape. The road surface itself often runs across solidified lava flows, with the black volcanic rock creating striking contrasts against patches of hardy highland vegetation and seasonal snow fields that persist well into summer.

Geologists particularly value this region for studying Icelandic volcanism's evolutionary patterns. The shield volcano's formation occurred during the early Holocene period, making it relatively young in geological terms yet old enough to show significant weathering and ecosystem development across its surface.

Route Description and Challenges

Eastern Approach via Þingvellir

Most travellers encounter the F338's eastern terminus near Þingvallavatn, Iceland's largest natural lake. The initial 8 kilometres present relatively straightforward driving across fairly level terrain, though the surface alternates between graded gravel and rougher volcanic rock sections. Two small river crossings occur within the first 5 kilometres, typically presenting minimal challenge during normal summer conditions but requiring caution during periods of heavy rainfall or rapid snowmelt.

The Central Traverse

The road's most demanding section begins approximately 12 kilometres from the eastern entrance, where the route climbs steadily across Skjaldbreiður's northeastern slopes. Here, drivers encounter loose scree sections and several stream crossings that can become problematic during adverse weather. The landscape opens dramatically, revealing expansive views across the Langjökull glacier to the north and the Reykjanes Peninsula extending toward the Atlantic.

Navigation requires attention, as the F338 intersects with several smaller tracks used for research access and emergency routes. Proper maps and GPS coordinates prove essential, particularly when visibility deteriorates in the frequent highland weather changes.

Western Descent to Kaldidalur

The road's final 8-kilometre section descends toward the Kaldidalur valley, reconnecting with the F550 Kaldidaluvegur near the historic route between Iceland's southwestern regions and the north. This descent presents spectacular views of Langjökull's southern reaches whilst crossing terrain that transitions from stark volcanic desert to areas supporting dwarf birch and willow communities.

Flora and Fauna

Despite its seemingly barren appearance, the Skjaldbreiður region supports remarkable biodiversity adapted to highland volcanic conditions. Arctic foxes maintain territories across the lava fields, whilst rock ptarmigan thrive in areas where vegetation provides adequate cover. During summer months, wheatears and snow buntings establish breeding territories, their songs providing unexpected soundtrack to the stark landscape.

Plant communities demonstrate remarkable adaptation to volcanic soils and extreme weather conditions. Racomitrium moss creates extensive grey-green carpets across older lava flows, whilst specialised lichen communities colonise the youngest rock surfaces. These pioneer species play crucial roles in soil development, gradually creating conditions that support more complex plant communities.

Practical Considerations

Vehicle Requirements and Preparation

The F338 demands proper 4WD vehicles with adequate ground clearance. Standard rental cars lack sufficient capability for safe passage, whilst many basic 4WD vehicles may struggle with the route's more challenging sections. Recommended equipment includes spare tyres, emergency communication devices, and sufficient fuel for extended highland travel.

Tyre pressure adjustments prove beneficial when crossing loose volcanic surfaces, though drivers must carry proper inflation equipment for subsequent road sections. River crossing techniques become essential knowledge, as several fords require careful assessment of depth and current strength.

Safety and Emergency Preparedness

Weather conditions change rapidly in Iceland's highland regions, with summer snowfall possible even during July and August. Emergency supplies should include warm clothing, food provisions, and emergency shelter capabilities. The Icelandic Association for Search and Rescue (ICE-SAR) maintains emergency shelters throughout highland regions, though their locations require advance research and GPS coordinates.

Mobile phone coverage remains sporadic to non-existent along much of the F338, making satellite communication devices advisable for serious emergencies. The safe travel plan system (safetravel.is) provides essential registration services for highland travel.

Optimal Timing and Conditions

Prime travel conditions typically occur during July and August when daylight extends beyond 18 hours and weather patterns show greatest stability. Early morning departures prove advantageous, allowing completion during optimal light conditions whilst providing safety margins for unexpected delays.

September travel becomes increasingly challenging as weather deteriorates and daylight hours decrease rapidly. However, clear September days offer exceptional photography opportunities with autumn colours contrasting dramatically against the volcanic landscape.

The F338 Skjaldbreiðarvegur represents highland driving at its most rewarding, combining geological education with genuine adventure across one of Iceland's most distinctive volcanic features. Proper preparation transforms this challenging route into an unforgettable journey across the broad shield that helped build Iceland itself.

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Our Verdict

A practical guide worth reading before you go.