Mount Hekla: Saturday quake was clearly visible in webcam (shaking) monitoring Mount Hekla. (Photo: Míla webcam).
A webcam which monitors the volcano Hekla in South Iceland, caught the shaking of the ground during Saturday’s powerful 4.5 magnitude earthquake West of Hekla.
The initial quake was followed by a powerful earthquake swarm which lasted 10-15 seconds, and were felt all over South Iceland.
See Iceland Magazine Article: Footage from Mt. Hekla volcano monitoring webcam shows earth tremble during Saturday’s quake
The 4.5 magnitude earthquake west of volcano Hekla on Saturday was followed up by a 3.2 magnitude quake in the Bárðarbunga caldera later the same evening.
The quake, which had its epicenter at a depth of 4.3 km (2.7 miles) in the N.E. part of the caldera, was followed by a swarm of smaller quakes, including two 2.1 and 2.5 magnitude quakes in the N.E. and S.E parts of the caldera.
It is uncertain whether these episodes are connected, but may be associated with tectonic plate movement and separation.
Bárðarbunga Future Eruption?
The earthquakes in Bárðarbunga are caused by magma thrusting its way from the mantle to the magma chambers of the volcano, refilling it after the 2014-15 Holuhraun eruption. Bárðarbunga is preparing for continued volcanic activity – probably in the near future.
Volcanic Zones & Seismic Rift Zones
SISZ= South Iceland Seismic Zone, between the East and West Volcanic Zones (EVZ and WVZ),
extending from Reykjanes Volcanic Belt (RVB). (Photo: Wikipedia, Creative Commons)
Saturdays quake west of Hekla took place in the South Iceland Seismic Zone (SISZ), a transform fault between offset sections of the Mid-Atlantic Ridge which runs through Iceland.
The zone is made up of a series of fracture faults, which run from SW to NE.
The zone extends from the volcano Hengill, the easternmost part of the Reykjanes volcanic zone, to Hekla, which is the westernmost volcano in the East Volcanic Zone (EVZ).
The Massive “South Iceland Quake”
There are no active volcanoes in the South Iceland Seismic Zone (SISZ), but it is extremely active.
The area sits between the two volcanic zones, and is constantly being pulled in two different directions, causing tension to build up in the crust, which is then periodically released in earthquakes.
The zone has been the source of the most powerful earthquakes in Iceland, as the most powerful earthquake which has taken place in Iceland since the country was settled took place in the Southern Seismic Zone.
Vatnajökull Glacier: Weekend’s activity in Bárðarbunga (Green Star: identifies 3.2 magnitude quake on Saturday). (Photo: IMO)
During 1784 a massive earthquake, which is believed to have been 7.1 magnitude, shook all of southern Iceland, causing widespread damage to farmhouses.
The second largest earthquake, and the largest to be measured with modern equipment, was detected in 1912.
This quake was 7.0 on the Richter scale.
Both quakes took place close to Saturday’s tremor.
Quakes of this magnitude are believed to hit once every 100-150 years, and could cause significant damage.
Locals in South Iceland are still waiting for the “big one”.
ICE2017 Team continues to keep a close eye on developments of these recent activity, as it may influence our planning / execution for this years adventure.
Maybe we will have the opportunity to experience an earthquake and /or a live volcanic eruption.