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A magnitude 4.9 earthquake struck the Granada region of southern Spain on 18th August 2026 at 08:37 UTC, followed by a series of additional tremors including magnitudes 4.6 and 4.7, along with numerous smaller aftershocks. The quake occurred at a shallow depth of 10 km, resulting in strong, widely felt shaking across Granada and surrounding municipalities.
Earthquake magnitude is calculated using scientific methods that measure the total energy released during fault movement. Link to: How Earthquake Magnitudes Are Calculated
Granada lies within a tectonically active zone influenced by compression between the Eurasian Plate and the African Plate. Although Spain is not located on a major subduction boundary, southern Spain experiences moderate seismicity due to crustal faulting associated with this plate interaction.
Shallow earthquakes in this region often produce sharp, intense shaking that can be felt across a wide metropolitan area.
The tectonic plates beneath southern Europe play a major role in how earthquakes form and how strongly they are felt across the region. Link to: What Is a Subduction Zone?
The initial 4.9 quake and subsequent 4.6–4.7 tremors were surface‑level events, meaning the shaking was more intense than deeper earthquakes of similar magnitude. Residents reported:
Several buildings suffered visible structural damage, including cracked facades, dislodged bricks, and damaged walls.
Shallow earthquakes often produce stronger shaking because seismic energy reaches the surface more quickly. Link to: How Earthquake Depth Affects Shaking, Damage, and What People Feel
The 4.9 event was followed quickly by additional tremors:
Emergency services received over 500 calls reporting falling debris, cracks, and damage inside homes.
Authorities confirmed at least three people suffered light injuries, including a minor who was taken to hospital.
Significant disruption occurred across the province:
Residents described intense fear, falling objects, and damage inside homes, with some choosing to leave the city temporarily.
This earthquake occurred inland and at a shallow depth. There is no tsunami risk.
EarthExtremities.com will continue monitoring official updates from USGS, IGN, and regional emergency services. Any revisions to magnitude, depth, or damage assessments will be added as new information becomes available.
For readers who want a clear overview of why earthquakes occur, our guide explains the main causes and processes behind seismic activity. Link to: Why Earthquakes Happen — A Simple Explanation
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