By ZACHARY KEYSER
4-5 minutes
According to the Guardian, beginning on January 21, the
peninsula region has suffered over 8,000 earthquakes due to magma
shifting under the ground beneath the volcanic system.
The Northern Lights are seen above the ash plume of a volcano in Eyjafjallajokull, Iceland, April 22, 2010
(photo credit: REUTERS)
A volcanic region in the Reykjanes peninsula, south-west of
Iceland’s
capital, that has been dormant for over 800 years has been showing
activity over the past two months, according to scientists. The last
time the volcanoes in the region erupted in the 10th century, fountains
of lava sporadically spewed out of the crater vents over the course of
300 years.
According to
the Guardian,
beginning on January 21, the peninsula region has suffered over 8,000
earthquakes due to magma shifting under the ground beneath the volcanic
system.
“It seems that after being relatively inactive for many
centuries, this region is waking up,” said Lancaster University
volcanologist Dave McGarvie.
The extended eruption period is
powered by five volcanic systems interconnected within the Icelandic
region. Scientists claim that these five systems interact with one
another every 1,000 years or so, creating the abnormally long eruption
episodes - whereas normally volcanoes in the region are only active for a
few years and then become dormant shortly after.
With the volcano
being nine miles from Iceland's Keflavik international airport, the
Iceland GeoSurvey estimates that if the volcanic system begins to erupt
then eventually the entire complex will be coated with 2cm of ash -
halting all travel to and from the area.
“The worst-case scenario
is if lava flows towards the town of Grindavík,” said Kristín Jónsdóttir
from the Icelandic Meteorological Office, according to
the Guardian.
“There is also other important infrastructure in the vicinity including
a geothermal power plant. Hot and cold water supply may be at risk,
along with roads, including the road between Reykjavík and Keflavík
airport.”
While the region typically remains active for centuries
once it gets going, the eruptions are sporadic and small in comparison
to larger volcanic events such Skaftáreldar (fires of Skaftá) within the
crater row of Lakagígar, which lasted for about a year and became the
most fatal volcanic event in Iceland's history.
The Skaftáreldar
eruption produced around 14-cubic-kilometers of basalt lava - most of
the lava was produced within the first five months. Researchers claim
that Skaftáreldar occurred in ten "pulses" consisting of short-lived
explosions followed by longer periods of "fire-fountaining."
Not only did the immediate effects have a significant impact on the
Icelandic
population, the eruptions also produced millions of tons of hydrogen
flouride and sulfur dioxide, which polluted nearly the entirety of the
region and still has an effect on the climate today.
According to
Wired,
sixty percent of all livestock died from pollution and 10,000
Icelanders died from the famine that followed. The smog that has built
up around most of Eastern Europe today is known as the "Laki haze" named
after the crater row.
So, while the recent volcanic activity in
the Reykjanes peninsula will more than likely be minor in comparison to
Lakagígar, it will still be an inconvenience to say the least for
hundreds of years to come if the volcanic system turns on the jets.
“People
on the Reykjanes peninsula, and their descendants for several
generations, may have to be on their guard and ready to evacuate every
so often,” said McGarvie.
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