January 17, 1997
A weekly feature provided by scientists at the Hawaiian Volcano
Observatory.
New Seismology Projects for 1997
1997 is off to a promising start at the Hawaiian Volcano Observatory
(HVO). Already in the works for the New Year are two projects
aimed at improving our views into the volcano and into the island
with new seismic monitoring tools.
First, we are preparing for the return, next month, of 30 visiting
seismologists from Japan, Italy, Alaska, and from the U S Geological
Survey's Western regional office in Menlo Park, California. We
will continue our cooperative study of volcanic processes beneath
Kilauea's summit caldera under the auspices of the Japan-US
Science and Technology (JUST) agreement.
Some readers will recall that, last January, scientists from the
same group of universities and agencies joined HVO staff in the
first JUST seismic project. In that project, we deployed a large
number of portable seismic recorders at Kilauea's summit
to record the different earthquake signals generated by the volcano.
Results from last year's study include a better understanding
of how the seismic signals propagate through Kilauea's
summit region. We also recorded the earthquake swarm on February
1, 1996, that caused considerable concern about a possible eruption
in the summit crater.
This year the JUST study will again focus on Kilauea's
summit region. We will deploy approximately 100 portable seismic
recorders and sensors in semicircular, diamond, and linear arrays
or antennas. The array configurations will allow us to tune our
recordings and determine directional propagation characteristics
of the seismic signals. Seismic waves travel at different speeds
in different directions. To last year's types of sensors,
we are also adding a number of ÏbroadbandÓ seismometers
to record a more complete spectrum of seismic signals. The JUST
project will be in operation at HVO in early February for a period
of about 10 days.
In addition to the JUST study, HVO is working with a university
and Federal consortium on the installation of a new, permanent
seismographic station in the Humu'ula Saddle region. This new
station will feature both a broadband, digital seismograph and
a strong-motion accelerometer. The broadband sensor will be installed
at the bottom of a 100 meter-deep well. This will increase the
sensitivity of the station by avoiding the noise generated at
the Earth's surface. The accelerometer can record large
local earthquakes, up to magnitude 8, without going off scale.
The data from these sensors will be transmitted to HVO and be
incorporated into our existing data streams. The site will also
be linked to O'ahu and to the mainland.
The new borehole station is sponsored by the Incorporated Research
Institutions for Seismology (IRIS) consortium. IRIS has about
100 member institutions whose goal is to improve our understanding
of the Earth with a number of different projects. Because of our
unusual location in the middle of the Pacific Ocean, the IRIS
working group for global, digital seismographic networks has been
interested in stations in Hawaii for quite some time. HVO will
benefit from the greater quality and cleaner signals from the
broadband system.
Through HVO partnerships and cooperative studies like IRIS and
JUST we are able to upgrade our operational capabilities and conduct
research that will allow us to improve our understanding of how
volcanoes work.
Eruption Update
The eruption of Kilauea Volcano continues. Lava continues to flow
into the ocean via a single main feeder tube to the coastal bench.
There were substantial rockfalls within Pu'u O'o vent. No new
breakouts were seen on the flowfield. There were no felt earthquakes
on the Island last week.
        

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