HR: 10:50h
AN: ED31E-03 [PDF]
TI: Geological map of the future: digital, interactive, and 3D
AU: * Thorleifson, H
EM: thorleif@umn.edu
AF: Minnesota Geological Survey, 2642 University Ave W, St Paul, MN 55114-1057 United States
AB:
Geological survey agencies are developing methods for government geological mapping in the post-paper map era. Surficial and
bedrock maps are being digitized and reconciled, while multiple generations of legends are being made accessible in a
categorized format. Regional 3D geological models that integrate soils and geology, surficial and bedrock geology, as well as
onshore and offshore are increasingly in demand as the information, technology, and protocols to build them progress.
Applications such as regional groundwater modelling require digitizing, reconciliation, and assembly of a digital elevation
model, bathymetry, offshore geology, soils, surficial geology, public domain drillhole and geophysical data, bedrock maps,
and existing stratigraphic models typically expressed as structure contours. New stratigraphic modelling, particularly
required for surficial unconsolidated deposits in many regions, requires information from cored holes logged by geologists as
well as geophysical surveys. These high-quality results are extrapolated laterally using drill hole data, commonly large
quantities of water well data of varying resolution and reliability. Much effort is required to adequately georeference the
drillhole data, and to parse large numbers of unique lithological descriptions. Stratigraphic modelling methods ideally use
all data and an approach that permits judgement in the acceptance or rejection of data, while interpolation and extrapolation
are guided by genetic insights. Models are best captured as a grid of predicted stratigraphy profiles that convey expert
opinion on interpolation and extrapolation from the data points. Reconciliation of mapping with that of neighbouring
jurisdictions is a key step, as is balancing subjective definition of strata with more objective geostatistical approaches to
characterizing the heterogeneous physical properties of the strata. Progress is readily achievable in undeformed strata,
while deformed strata present far greater challenges. Increasingly, databases of observations and measurements are being
retained alongside the interpreted model, and models are being assigned varying confidence levels such that the result is
seen not as an end but a means for prioritizing new mapping. Current activity is broadening our reliance not only from paper
maps to digital models, but also from plan view maps, to drillhole databases, to 3D models, to dynamic models such as
groundwater flow models. Pressing user requirements demand that geological survey work rapidly advance along this
progression.
DE: 1829 Groundwater hydrology
DE: 8094 Instruments and techniques
DE: 9820 Techniques applicable in three or more fields
SC: Education and Human Resources [ED]
MN: 2003 Fall Meeting