The Iceland eruption is a fissure eruption, in which lava issues from a long, narrow vent instead of a simple hole in the ground. Hawaii is another place where fissure eruptions occur. In the geologic past, huge fissure eruptions are associated with large igneous provinces or LIPs. A LIP in India was largely responsible for environmental upsets around the time of the dinosaur extinction 65 million years ago, and the Yellowstone LIP has left a wide trail of lava plains across Idaho leading to the great caldera in Wyoming's northwest corner, our own "supervolcano."
By the way, it was Iceland that gave rise to Benjamin Franklin's most widely cited geological accomplishment, when he supposedly linked the 1783 eruption of Laki to the severe winter that followed. Um, not really. I think you could make a better case that Franklin was actually the father of borehole paleothermometry.
Background:
Volcanoes in a Nutshell
About calderas
An Oregon caldera
A model for supervolcano eruptions
The world's largest supervolcanoes
More volcanic links


Comments
I thought 1816 was the year without a summer http://www.cfa.harvard.edu/~wsoon/GoldbergMay05-d/Summer_of_1816.pdf
I’ve never heard of Laki and 1783; how does that compare?
J a
Thanks for that very interesting link. There is some worry about a another larger eruption that could occur in Iceland which could have similiar consequences as in 1816.
http://throughthesandglass.typepad.com/through_the_sandglass/2010/04/eyjafjallajokulled-stranded-in-the-usa.html