Hagafell Volcano — Live Webcam from Grindavik

Hagafell Volcano — Live Broadcast from the Blazing Reykjanes

This page features the Hagafell volcano webcam — a live broadcast from the very epicenter of volcanic activity on the Reykjanes Peninsula. The camera is installed at a safe distance and shows the current state of the eruption: fountains of molten lava, flows of incandescent material, and columns of volcanic ash. This is one of the few online cameras that allow you to observe an active Icelandic volcano in real time from anywhere in the world.

Hagafell is a mountain in southwestern Iceland that has become the symbol of a new volcanic era on Reykjanes. After nearly a millennium of dormancy, the peninsula awakened: since 2021, a series of powerful eruptions have occurred here, culminating in 2024 when lava approached Grindavik. The online camera captures all phases of activity — from quiet periods to violent eruptions.

Where Hagafell Is Located — Geography of the Reykjanes Peninsula

Hagafell volcano is located on the Reykjanes Peninsula — a narrow strip of land between the Atlantic Ocean and Reykjavik. It is part of the Eldvörp–Svartsengi volcanic system, which stretches as a chain of fissures from the ocean coast deep into the peninsula. The system is located southeast of Keflavik Airport and north of Grindavik.

The Reykjanes Peninsula is where the Mid-Atlantic Ridge emerges above the surface. Here, the North American and Eurasian tectonic plates diverge at a rate of about 2 cm per year, creating faults and fissures through which magma rises to the surface. The region contains several volcanic systems: Reykjanes, Eldvörp-Svartsengi, Fagradalsfjall, Krýsuvík, Brennisteinsfjöll, and Hengill.

Grindavik — a small fishing town with a population of about 3,500 — is just a few kilometers from Hagafell. This proximity made the 2023–2025 eruptions so dramatic: lava literally approached residential neighborhoods, and evacuation became routine for local residents.

Eruption Chronology: 2023–2025

Modern volcanic activity on Reykjanes began in 2021 with the Fagradalsfjall eruption, which attracted thousands of tourists. But the real crisis unfolded later. In November 2023, a series of earthquakes with magnitudes up to 5.2 triggered the evacuation of Grindavik. And on January 14, 2024, an eruption at the foot of Hagafell breached the anti-lava defenses and destroyed three houses in Grindavik.

The January 2024 eruption was smaller in scale than previous ones, but the fissure opened less than 100 meters from Grindavik. This created an unprecedented situation: incandescent flows moved directly toward the town, and hastily erected protective berms could only divert part of the lava. The 2023–2025 eruption series became the first case in over 50 years where an eruption destroyed homes in an Icelandic settlement.

On May 29, 2024, the eighth eruption in this area in three years occurred. Each new event brings a fresh batch of magma from the depths — fissures open in different locations, altering the landscape and creating new threats to infrastructure. The Hagafell camera captures these changes, allowing you to track the evolution of volcanic activity.

The Eldvörp–Svartsengi Volcanic System

Hagafell is not an independent volcano but part of the extensive Eldvörp–Svartsengi fissure system. Such systems are typical for Iceland: instead of a single central crater, eruptions occur through linear fissures ranging from hundreds of meters to several kilometers in length. Magma rises through these faults, creating chains of lava fountains.

Historically, Reykjanes volcanic systems have erupted in temporary clusters with millennial periods of inactivity (800–1,000 years). The last such cluster occurred in the 10th–12th centuries, and now the region has entered a new phase of activity. This means eruptions could continue for decades with varying intensity.

The Eldvörp–Svartsengi system includes not only Hagafell but also other centers of activity: Sundhnúkur (where the most powerful eruptions of 2023 occurred), Þorbjörn, and sections along the coast. The Svartsengi geothermal power plant, which provides energy for the Blue Lagoon and surrounding areas, is located in close proximity to the fissure zone.

What's Happening Now — Activity Monitoring

The Hagafell online camera operates in real time, allowing you to assess the current state of the volcano. During active periods, the broadcast shows bright orange-red lava fountains rising tens of meters high. Columns of smoke and ash rise upward, shrouding the sky in a gray haze. Flows of incandescent material cascade down the dark volcanic landscape, creating new landforms.

Between eruptions, the camera shows solidified lava flows with a characteristic crust, in places revealing glowing hot spots. Fumaroles — outlets of hot gas — create steam plumes that can be mistaken for smoke from a new eruption. This is why it's important to know how to interpret the image: fumarole steam is white and dissipates, while volcanic ash is gray and drifts with the wind.

The Icelandic Meteorological Office and the University of Iceland maintain constant monitoring of the region. Data from seismographs, GPS stations, and satellite imagery complement the picture provided by the webcam. Warnings are issued when there is a threat to the population, and the camera allows visual confirmation of an eruption's onset.

How to Interpret the Camera Image

Observing a volcano through an online camera requires understanding what you're actually seeing. Here are the key elements of the broadcast:

Lava fountains — vertical jets of molten rock, glowing orange and red. Their height can reach 50–100 meters during powerful eruptions. The color ranges from bright orange (temperature around 1,100°C) to dark red (cooling lava).

Lava flows — horizontal movements of incandescent material down slopes. On camera, they appear as glowing rivers slowly advancing. Flow speed ranges from several meters per hour to fast flows on steep slopes.

Smoke and ash — gray or dark columns rising from the vent. Unlike white fumarole steam, volcanic ash is dense and drifts with the wind. During strong eruptions, ash can rise to heights of several kilometers.

Solidified lava — a dark crust in the foreground, covered with cracks. In places, hot spots glow through it — this is residual heat from recent flows.

Safety and Regional Accessibility

The Hagafell camera is installed at a safe distance from the active zone. This is critically important: proximity to the vent of an active volcano is deadly not only because of lava but also due to toxic gases (sulfur dioxide, hydrogen sulfide), pyroclastic flows, and unpredictable fissure behavior.

Grindavik and its surroundings were evacuated multiple times in 2023–2024. Route 427, connecting the town to Reykjavik, was periodically closed due to lava flows. The Blue Lagoon — the famous geothermal resort — was closed for months during peak activity. Local authorities erected protective berms, but they do not guarantee safety during powerful eruptions.

For tourists who want to see the volcano in person, helicopter excursions and guided hiking tours are organized. However, the safest way to observe is precisely the webcam, which provides a complete picture without risk to life.

Nearby Attractions and Other Regional Cameras

The Reykjanes Peninsula is rich not only in volcanoes but also in geothermal attractions. In the Grindavik and Hagafell area, you'll find:

Blue Lagoon — a geothermal spa resort operating on water from the Svartsengi power plant. Its vivid blue waters contrast with the dark lava fields.

Geldingadalir — a geothermal area with mud pots and fumaroles, located between Grindavik and Reykjavik. Here you can observe volcanic activity in miniature.

Krýsuvík — a geothermal area with colorful hills and solfataras, popular among tourists.

Þorbjörn — a mountain west of Grindavik, also part of the Eldvörp–Svartsengi system and a potential center for future eruptions.

Other webcams are also installed in the region, allowing observation of different sections of the volcanic system. By combining their data, you can build a complete picture of activity across the entire peninsula.

What You Can See on the Camera

The Hagafell webcam broadcast shows a panorama of the active volcano on the Reykjanes Peninsula. Depending on the phase of activity, you can observe on screen:

During an eruption — bright orange-red fountains of molten lava erupting from fissures on the slopes. Several active centers can operate simultaneously, creating a "wall of fire" effect. Columns of smoke and volcanic ash rise upward, shrouding the sky in a gray haze. Flows of incandescent material cascade down the dark landscape, leaving glowing trails behind them.

In the foreground — a volcanic landscape covered by solidified lava flows from previous eruptions. A dark crust with cracks, in places with glimpses of hot spots indicating recent activity. Fumaroles create steam plumes rising from the ground.

During quiet periods, the camera shows solidified lava cover with characteristic topography — pāhoehoe (smooth, ropy structures) and ʻaʻā (rough, jagged surfaces). Fumarole fields continue to emit steam, reminding us that the volcano is merely sleeping. The sky over Reykjanes is often overcast, creating a dramatic contrast with the dark ground.

The camera operates around the clock, allowing you to observe the volcano at any time of day. At night, the glowing lava flows and hot spots on the slopes are especially visible — a spectacle impossible to forget. During the day, landscape details and color variations in volcanic rocks are better distinguished.