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- A 3-Step Process for
- Evaluating the Authenticity of Siliceous Artifacts – Flint / Chert
- Presented by Jim Fisher B.A. M.Ed.
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- Inspect surface for evidence of alteration due to natural chemical
weathering
- Utilize microscopic review of weathering phenomena as a
- potential dating method
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- Chert forms through chemical precipitation
- Nodular and bedded forms often occur in carbonates
- Chert can be microscopically fibrous or microcrystalline
(cryptocrystalline)
- Chalcedony– chalcedonic
- (fibrous) microstructure
- Members of the silica family
- silicates – siliceous – SiO2
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- Visible and invisible chemical differences exist between surfaces of
“fresh” source samples of chert and archaeological artifacts made from
the same material.
- Weathering can oxidize or reduce minerals on the surface of an artifact.
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- Groundwater may dissolve some elements and then deposit others in
resulting pores (mineral dissolution and replacement).
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- Some are unstable at surface conditions
- Surface implies exposure to elements exterior to the parent material
resulting in post-depositional modification
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- Clay minerals
- Carbonate minerals (i.e. cavities where calcareous crinoid fossils
dissolve)
- Iron minerals (evident as FeO - post depositional iron oxide) i.e.
pyrite, hematite, limonite
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- pH scale: range from 0 to
14, <7=acidic >7=basic (alkaline)
- Silica solubility not effected by pH<9 and >2
- Ocean = 8.1-8.3 (mildly alkaline)
- Streams in arid areas = 7-8 (nearly neutral to mildly alkaline)
- Streams in humid areas = 5-6.5 (moderately to mildly acidic)
- Presence of impurities effects silica solubility profoundly
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- Low pH water (acidic) encourages carbonates to dissolve, silica can then
be mobilized and deposited over time in spaces left by the dissolved
carbonates
- Water pitting
- Un-replaced patches of carbonate minerals and elements (calcium - Ca,
magnesium- Mg) can also be seen in cherts– should appear chemically
weathered.
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- Consistent with that seen on naturally weathered hand samples collected
in similar environment?
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- Look for evidence of oils, stains, waxes, suspicious residues
- Uniform coating? High spots show
wear through the coating?
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- Hard or soft billet percussion?
- Evidence of recent use of copper or other metal tools?
- Presence/absence of pressure flaking (hard or soft tool flaking?)
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- Crushing in notches
- Step fractures (“hanging flakes”) with no patina beneath and/or
exceedingly loose or prevalent
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- Presence of saw marks, flat areas on face of artifact?
- Unusual uniformity in thickness?
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- Presence of polish (i.e. phytolithic sheen on hafted microliths)?
- Evaluate sharpness of lateral blade edges and flake scar ridges
- Evidence of mechanical grinding, tumbling or sandblasting?
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- Due to agricultural implement?
Iron oxide (FeO) staining?
- Ancient impact fracture?
- Preform failure & re-chipping – ancient or modern?
- Use of ultraviolet light can detect evidence of modern re-chipping
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- Though not technically a mechanically induced property, the effect can
be the result of man’s intentional interaction with the material.
- Intentional or unintentional heating?
“Pot lidding” present?
- Consistent with heat treating cultures/typologies in archaeological
record?
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- Morphometric analysis: Do the artifact’s attributes fall within
acceptable morphometric ranges for the type?
- Flaking style consistent with type?
- Cross-section consistent with type?
- W/T ratio within acceptable range for type?
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- Finishing attributes (i.e. basal grinding) consistent with type?
- Account for resharpening: Hafting
area free of use-wear?
- Plausible material given reported provenance and considering cultural
use as indicated in archaeological record?
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