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originally posted by: Darkblade71
M5.7 - 116km SSE of Akureyri, Iceland 2014-08-26 01:26:08 UTC
earthquake.usgs.gov...
Another big one.
There have been no signs of harmonic tremor.
Harmonic tremor describes continuous rhythmic earthquakes that can be detected by seismographs. Harmonic tremors often precede or accompany volcanic eruptions.
There are no indications that the intensity of the activity declining.
The following three scenarios are still considered most likely:
The migration of magma could stop, accompanied by a gradual reduction in seismic activity.
The dike could reach the surface of the crust, starting an eruption.
In this scenario, it is most likely that the eruption would be near the northern tip of the dyke. This would most likely produce an effusive lava eruption with limited explosive, ash-producing activity.
An alternate scenario would be the dyke reaching the surface where a significant part, or all, of the fissure is beneath the glacier. This would most likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity.
Other scenarios cannot be excluded. For example, an eruption inside the Bárðarbunga caldera is possible but presently considered to be less likely.
The dyke beneath Dyngjujökull is now thought to be close to 40 km long. Modeling of GPS data indicates that about 50 million cubic meters of magma have added to the volume in the last 24 hours.
There are no indications that the intensity of the activity declining. Currently, three scenarios are considered most likely:
1) The migration of magma could stop, attended by a gradual reduction in seismic activity.
2) The dike could reach the surface of the crust, starting an eruption. In this scenario, it is most likely that the eruption would be near the northern tip of the dike. This would most likely produce an effusive lava eruption with limited explosive, ash-producing activity.
3) An alternate scenario would be the dike reaching the surface where a significant part, or all, of the fissure is beneath the glacier. This would most likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity. Other scenarios cannot be excluded. For example, an eruption inside the Bárdarbunga caldera is possible but at present considered to be less likely.
Just under 900 earthquakes have been detected by the network since midnight, somewhat fewer than at the same time yesterday. The intrusive dike is now about 40 km long. Most of the activity has been near the edge of the glacier. An earthquake M4.6 (EMSC M4.4) occurred at 11:56. Reports were received from Akureyri (a town in northern Iceland) that the earthquake was found there. The earthquakes are mostly on similar depth as before, i.e. 8-12 km. A few were larger than M3. Few earthquakes were located in the Bárðarbunga caldera today.