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Originally posted by Phlynx
So your saying this could be a Yellowstone like explosion?
Originally posted by alysha.angel
Originally posted by Phlynx
So your saying this could be a Yellowstone like explosion?
not that big no. but big enough to cause high levels of damge to large parts of iceland .
Originally posted by MoorfNZ
You can monitor Katla's webcam here:
www.ruv.is...
EDIT: Since dawn broke I have been unable to get a pic on Katla webcam.. anyone else?
[edit on 23-3-2010 by MoorfNZ]
Originally posted by berkeleygal
Good morning
Here's a good web cam of Eyjafjallajökull frá Hvolsvelli
I even saw a helicopter fly by about 10 minutes ago.
mila.is...
Here's tremor graphs for all of Iceland
hraun.vedur.is...
Is another Chilean volcano awakening? Melimoyu volcano in the Aysén region of southern Chile, a glaciated stratovolcano with a summit elevation of 2400 m and a distinctive horned profile, has been making some seismic noise over the past few days. Chile’s state geological service SERNAGEOMIN reported on 20 March that three earthquakes, two of magnitude 3.3 and one of magnitude 5.0, were detected on 17 March beneath Melimoyu. The earthquakes, which have been felt by people in towns near the volcano, continued at a lower level on 18 March.
Originally posted by westcoast
reply to post by PuterMan
Okay, this is scary. Just how big would the potential erruption for this one be? Mags that high beneath any volcano is a definate wake-up call!
A stratovolcano, sometimes called a composite volcano,[1] is a tall, conical volcano with many layers (strata) of hardened lava, tephra, and volcanic ash. Stratovolcanoes are characterized by a steep profile and periodic, explosive eruptions. The lava that flows from stratovolcanoes tends to be viscous; it cools and hardens before spreading far. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Stratovolcanoes are sometimes called "composite volcanoes" because of their composite layered structure built up from sequential outpourings of eruptive materials. They are among the most common types of volcanoes, in contrast to the less common shield volcanoes. A famous stratovolcano is Krakatoa, best known for the eruption in 1883.