It should
be pretty clear already.
How Do They
Do it?
The monitoring
activity at Volcán de Colima includes the
recording of volcanic and tectonic seismic
activity, ground deformation, thermometry, and
meteorology; receiving infrared and visible
satellite imagery from AVHRR and GOES; and
performing geological surveys at the volcano and
in the surrounding areas. Prior to the
September 1992 publication of the report from
which this information was gathered, there were
five Telemetric seismic stations, each with
short-period vertical seismometers, located on
and in the vicinity of the volcano, and two
located in the depression between the tectonic
fault systems of Colima. However, there were
plans to add three more stations before the
year’s end, putting one on the volcano, one in
the depression, and one in the subduction zone,
for a total of ten stations in the Red Sísmica
de Colima (RESCO). Other equipment as of 1992
included: 3 portable three-component digital
stations for registration onsite, a Blum
tiltmeter, two Telemetric meteorological
stations, one Telemetric thermometric station, a
deformation network of benchmarks, a VHF/FM
communication system, and the capacity for
receiving infrared and visible images from
meteorological satellite.20
Current
deformation monitoring at Colima includes the
usage of electric distance measurement, which
measures distance from a fixed point to
reflectors on the edifice and GPS networks,
which can measure the changes in a geodetic
network; electronic and dry inclinometers,
which, respectively, record the changes of a
plane and determine angles of tilt and precisely
determine variations of the network that can be
attributed to the movement of the deformation
source; trigonometrical and geometrical
leveling, which detect uplift or depression at
points on the edifice, and gravimetry, which
measures changes in a gravitational field.21
Geochemical
monitoring at Colima is particularly important
at Colima, especially in terms of its usefulness
in predicting eruptions. Where seismic
anomalies often fail to accurately indicate an
eruption, gas emissions, for example, can signal
important changes that may be nearly definitive
hallmarks of impending activity. Therefore, in
addition to the heavily-relied-upon seismic
data, information concerning sulfur dioxide
levels, the gas composition of eruption plumes
and the atmospheric surroundings, the chemical
composition of lava and spring waters, and the
characteristics of the ash produced are also
closely monitored and studied.23
Visual
monitoring, although highly dependent on weather
conditions, has been utilized to observe and
record the activity at the Volcán de Colima
since 1998, capturing dome growth; lava,
block-and-ash, and pyroclastic flows;
explosions; ash fall; ballistics; and even
subsequent forest fires. It also records the
more mundane behaviors, including the eruption
and height of a volcanic plume, a change in
color, and the formation of new fumaroles, for
instance. This method of monitoring operates
twenty-four hours a day at two stations:
Estación Naranjal, located 15 km south of the
volcano at the Volcano Observatory in El
Naranjal, and Estación Nevado, located 5.3 km
north of the volcano on Nevado de Colima, which
both broadcast to the Volcano Observatory of the
University of Colima. According to the site,
eight more cameras are being installed at
various points around the volcano in order to
assist in the monitoring activities.22
It is also helpful
to read scientific articles on current research
being done at Colima in order to see the various
monitoring sources available to and used by
geologists and volcanologists interested in this
volcano.
Suggested reading:
-
"Recent lahars
at Volcan de Colima (Mexico): Drainage
variation and spectral classification"
-
"Modeling of
pyroclastic flows of Colima Volcano, Mexico:
implications for hazard assessment"
-
"Debris
avalanches and debris flows transformed from
collapses in the Trans-Mexican Volcanic
Belt, Mexico - behavior, and implications
for hazard assessment"
Available through
ScienceDirect
and links on the Sources page.