Earthquake
hits waters off Japan
26
October, 2013
An
earthquake with a magnitude of 7.3 on the Richter scale hit the
waters 231 miles (371 kilometers) east of Japan on October 25,
2013, reports rt.com,
adding that the quake prompted an evacuation at the devastated
Fukushima Daiichi plant and that strong tremors could be felt on
Japan’s main Honshu Island, as well as on the northern island of
Hokkaido.
USGS.gov
reported the quake as having a magnitude of 7.1 followed up by
several smaller quakes, as indicated on the image below, which also
indicates the location of Fukushima.
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The
image below shows that methane readings of 1950+ were recorded on and
around the location where the earthquake hit. The image merely shows
methane that did enter the atmosphere. More methane will have escaped
from the seabed, but much of it will have oxidized in the water.
The
occurence of this earthquake is very worrying, due to the situation
at the Fukushima Daiichi nuclear plant. It is also relevant to the
situation in the Laptev Sea, north of Siberia, for a number of
reasons, including:
As
the above image clearly shows, earthquakes can trigger methane
releases from the seabed, as previously discussed in the post Methane
Release caused by Earthquakes.
Global
warming is contributing to the occurance of earthquakes. For years,
geophysical hazard specialist Bill
McGuire has studied this
impact of global warming, in particular the Earth's crust bouncing
and bending in response to the melting of the great ice sheets and
the filling of the ocean basins—dramatic geophysical events that
triggered earthquakes, spawned tsunamis, and provoked a series of
eruptions from the world's volcanoes. Bill
McGuire warns that
staggering volumes of melt water poured into the ocean basins,
warping and bending the crust around their margins. The resulting
tossing and turning provoked a huge resurgence in volcanic activity,
seismic shocks, and monstrous landslides—the last both above the
waves and below.
According to calculations posted
by Doyle Doss in January 2012,
the increase in weight of the Pacific Ocean over the last 50 years
due to freshly introduced water from land ice melt is 10 Trillion 331
Billion 125 Million 200 Thousand TONS. In conclusion, global warming
is making methane releases triggered by seismic activity worse.
The
fault lines around Japan are interconnected with other fault lines,
as illustrated by the image below, from the post High
Methane Levels over Laptev Sea,
showing methane readings on October 20, 2013 pm. Earthquakes can
trigger further earthquakes, especially along the same or
interconnected fault lines.
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The image below shows methane readings on October 25, 2013 pm, indicates that high methane readings continue to be recorded over the Laptev Sea.
The
above image also shows that the Laptev Sea was hit by an
earthquake with a magnitude of 4.6 on the Richter scale on
September 28, 2013. Earlier, on August 7 and on September 9,
earthquakes with similar magnitudes had hit the Laptev Sea closer to
land, as described in the post Earthquake
hits Laptev Sea.
For
more than a month, large amounts of methane have been present over
the Arctic Ocean, in particular over the Gakkel Ridge and, more
recently, also over the Laptev Rift.
Sediments
under the Arctic Ocean contain huge amounts of methane in the form of
hydrates and free gas. Some areas, such as the Gakkel Ridge and the
Laptev Rift are prone to earthquakes, volcanoes and landslides, as
they are part of a tectonic fault line that crosses the Arctic Ocean.
The
danger is that, as the permafrost retreats and the snow and ice cover
declines rapidly, methane in the Arctic is on the brink of being
released abruptly and in large quantities from the seabed. A single
earthquake, perhaps even outside of the Arctic Ocean could set this
off. There are many more factors that influence seismic activity,
such as the position of sun, moon and stars, and the depth at which
seismic activity occurs, as tremors can be felt far away from
earthquakes that occur at greater depth. Anyway, the danger is that
earthquakes will trigger abrupt release of methane from the seabed of
the Arctic Ocean, and since methane is a powerful greenhouse gas,
such a release could further accelerate local warming, triggering
further destabilization of methane in the seabed, escalating into
abrupt climate change across the globe.
The
depth of the seabed is also important in this regard, since shallow
seas can warm up rapidly, while methane that escapes from the seabed
has less chance to get oxidized in shallow seas. Large parts of the
Arctic Ocean are very shallow, in particular the Laptev Sea, as
further descibed in the post methane
hydrates.
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