In geology
we define geological contacts between units and we place a line in a map when
we have identified this in the field, in most places the contacts are inferred
and are shown as dotted lines. The extrapolation to depth is even more
uncertain and can be improved by geophysical measurements and
validated by drilling.
In general
that is how geology works, mapping of units from satellite images and aerial
photos, validation in the field and presentation in a geological map; which is
now a digital map and is increasingly a 3 dimensional digital geological map. Where resources need to be defined the mapping is followed up by
geophysical images and ultimately by drilling to define the true geological contacts.
This is the
bulk of the geologist's job and we know what the confidence is in our
geological images and geophysical models. The challenge is communicating this
to the public in a world where we will be increasingly using the subsurface
space to build, to store things such as gas and heat, to extract resources and
to secure nuclear waste and avoid emission of waste CO2 from power
stations by underground storage. There is no doubt that public pressure on
defining the environmental consequences of these activities is increasing and
geologists will be required to provide robust models of the subsurface if we
are to convince them about the science that we do.
BGS is
working on creating a 3 dimensional geological map of the UK which will vary in
resolution depending on where you are in the UK. It will be high resolution
below the major cities where the upper 100's of meters are critical for
construction, ultra-high resolution in the proposed UK nuclear waste
repositories, potential CO2
storage reservoirs and in future areas of
resource exploitation. In other areas BGS will
focus on high level landscape models allowing for protection and understanding
of the UK geological heritage, farming development and modelling of flood risk and other natural hazards.
Only where
we have observed a geological contact will the locations be exact otherwise we
will always need to infer contacts and build geological scenarios to the best
of our abilities.