Forensic Geology
(tutor - Mike Horne FGS, Hull University)
for the University of Hull
Departments of Chemistry and Lifelong Learning
Forensic Geology Techniques
1 - Materials
All geological materials have an original source and geological age.
1A - Hard
Minerals
Crystallography, Mineralogy, Optical mineralogy thin sections, polished thin sections, polished sections, XRD, chemical tests, electron microprobe.
Rocks
Igneous, Metamorphic and Sedimentary.
Mineralogy, Textures, particle shape and size, Optical mineralogy thin sections, polished thin sections, XRF, chemical tests, electron microprobe, absolute dating.
Man-made materials of a geological origin
Bricks, tiles, ceramics, glass, metals and alloys,
Crystallography, Mineralogy, Optical mineralogy thin sections, polished thin sections, polished sections, XRD, chemical tests, electron microprobe.
Fossils
Identification and relative dating, absolute dating.
Water
From rivers or groundwater.
Isotopes
1B- Soft
Poorly consolidated sediments - may be true geological deposits of great age, or recently deposited sediment or weathering products such as soils.
Particle sizing
Sieving, laser particle sizing,
Particle identification, shape analysis, particle statistics.
Sand and silts
Particle analysis as above, heavy mineral analysis, geochemistry, microfossils, environmental analysis.
Gravels
Particle analysis as above, clast types and origin, geochemistry, microfossils, environmental analysis.
Clays
Particle sizing by decanting, clay mineral identification by XRD, geochemistry by XRF, microfossils, nanofossils, palynology.
Air-bourn particles
Palynolology, geochemistry.
2 - Site investgation
"Trace Fossils" - e.g. footprints
As well as the size and make of the footwear (and therefore possible source) - we can gather information about height, speed, direction, changes of direction, water content of the substrate and perhaps even the surrounding environment and season of the year.
Stratigraphy - establishing the order of events.
In stratigraphy we work on the principle that the oldest sediment is at the bottom, unless it has been turned upside down and we consider ‘cross cutting’ relationships. Remember that the sediment on a suspects footwear has been turned upside down!
Geophysics - non-invasive ground surveys (as seen on Time Team)
To find changes in the soil, subsoil or rockhead - such as grave cuts and ditches.
Resistivity, magnetic, ground penetrating radar, seismic, metal detactor.
copyright Mike Horne - 2019
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