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European geological surveys and GEOSS –
observing the Earth beneath our feet:
why does it matter?
Patrice Christmann, Secretary-General, EuroGeoSurveys
W
hile the atmosphere and the Earth’s surface are acces-
sible to direct observation including by remote sensing
techniques, the observation of the Earth’s subsurface,
its related resources and hazards require the use of comple-
mentary observation techniques. Many of these are of an
indirect nature, such as the cartography of the various physical
properties of the subsurface (geophysics).
Geology is all about understanding, mapping and modeling the
Earth’s subsurface nature, structure and dynamics, and its related
resources and hazards. It is also the forensic science needed to
understand our Earth’s long and turbulent past. The resulting spatial
data, information and knowledge are needed to better address soci-
etal issues of today and tomorrow such as climate change,
sustainable use of natural resources, land-use planning, manage-
ment and storage of waste, mitigation of the impacts of natural
hazards of geological origin, identifying public health issues and
many more.
An ever-growing number of Earth observation techniques is avail-
able to geologists to produce the information required by the wide
range of end users of geological information, ranging from the macro
scale, such as the use of remotely sensed data and/or direct in situ
observations and mapping, to the nano scale, such as isotopic
geochemistry needed to determine the age of rock formations, or
electronic microprobe studies of mineral grains to develop the tech-
nologies best suited for the efficient recovery of the valuable metals
content from an ore body. Geological data describing the nature,
structure and ages of superficial formations and bedrock formations
is in most cases a fundamental geographic data layer necessary, in
combination with other data layers, to produce the information
required by end users.
In addition to technologies, considerable human skills are neces-
sary to select the right data sources and to steer/implement the data
acquisition process, which in many cases requires direct observa-
tion in the field, and afterwards to do the combinatorial processing
and modelling of heterogeneous Earth observation datasets.
Processing and modelling by experienced scientists is necessary to
turn raw Earth observation data, which is meaningless to most end
users, into the geographic information required to address end users’
concerns. The whole process is steered by specific end uses, each
requiring the use of different data sources and processing/model-
ling techniques. For instance, the process involved in developing
geographic information necessary to mitigate the potential impacts
of landslides is very different from the process involved
in generating information to guide mineral exploration
or sustainable groundwater management. Therefore,
geological surveys are institutions populated by scien-
tists from a wide range of complementary disciplines,
working together to deliver high-quality geographic
information to end users.
Understanding and mapping the subsurface and
providing the derived geographic information to end
users is essential to the global economy and to social
well-being. The underground is home to many
resources that are essential to life: energy (fossil and the
clean, renewable, dependable geothermal energy),
groundwater (the main source of drinking water supply
in many countries) and minerals (the main material
flow across the world economy).
Subsurface also means space to develop a wide range
of infrastructures, and storage for gas, waste or water.
Geology also has a strong incidence on the nature and
fertility of soils. The chemical elements in rocks deter-
mine the chemical composition of the groundwater they
host, of soils derived from their weathering and, from
this, the chemical elements found in our food and
drinking water. Excess or deficit of certain of these
elements can significantly impact health.
The subsurface and its dynamics are also the source
of many natural hazards. Some, such as earthquakes,
landslides or volcanic eruptions are spectacular and
hence are easily perceived by public authorities. Some
are more subtle and difficult to notice before their
economic and social impacts become visible: among
these are land heave and subsidence, gaseous emana-
tions (radon gas emanations are considered in various
epidemiological studies as an important source of lung
cancer), caving-in of man-made or natural cavities, and
shrinkage and swelling of clay-rich soils (costing
billions of euros to insurance companies compensating
the resulting damage to buildings).
Access to and sustainable use of natural resources of
geological origin, and mitigation of the impacts of
natural disasters of geological origin, will be issues of
growing importance – the Earth’s population is set to
reach nine billion in 2050, and the populations of
GEOSS C
OMPONENTS
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BSERVING
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YSTEMS