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The volcanic landscape around Fagradalsfjall and the town of Grindavík has become the epicenter of a new geological era for Iceland. After laying dormant for over 800 years, the Reykjanes Peninsula reawakened in March 2021, marking the start of a volcanic cycle that scientists predict could last for decades. The Awakening: Fagradalsfjall (2021–2023) The initial activity centered on Fagradalsfjall, a shield volcano located about 8 km northeast of Grindavík. This phase was characterized by "tourist-friendly" effusive eruptions in valleys like Geldingadalir and Meradalir. These eruptions produced slow-moving basaltic lava and minimal ash, allowing thousands of visitors to hike to the glowing rivers of molten rock. The Shift: Sundhnúkur Crater Row (2023–2026) In late 2023, the volcanic activity shifted west toward the Sundhnúkur crater row, significantly increasing the danger. Unlike the isolated valleys of Fagradalsfjall, these fissures opened dangerously close to Grindavík and critical infrastructure, including the Svartsengi Power Station and the Blue Lagoon. Impact on Grindavík: A massive magma gallery formed directly beneath the town, causing significant ground deformation and large cracks in the streets. This led to a permanent evacuation of the residents in early 2024. Defensive Measures: Iceland constructed massive earthen barriers (lava dams) to redirect flows away from the power plant and the remains of the town—a feat of engineering rarely seen on this scale. Current Status (March 2026) As of early 2026, the region remains highly active. The pattern has settled into a cycle of "recharge and erupt": magma accumulates beneath Svartsengi for several months, causing the ground to lift, followed by short, intense fissure eruptions along the Sundhnúkur row. While the town of Grindavík remains largely a ghost town protected by walls, the area serves as a powerful reminder of the raw, unpredictable nature of the Mid-Atlantic Ridge.