Chapter 4: Dating Methods & Chronology Flashcards

1
Q

Relative Dating

A
  • chronological sequence without recourse to a fixed time scale
  • no actual dates are assigned
  • seriation
  • stratification
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2
Q

Seriation

A
  • chronological ordering of a group of artifacts or assemblages where the most similar are placed adjacent to each other in the series
  • involves creating a typology of artifacts and placing them in a relative chronology
  • must be using same kind of object (ex. pots)
  • columns: different types
  • rows: proportion (percent) of each type at a site
  • when organized chronologically they will have a “battleship” shape
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3
Q

Stratigraphy

A
  • in a succession of layers the bottom layer is the earliest and the top layer the latest
  • law of superposition
  • principle of association
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4
Q

Law of Superposition

A

in a series of layers in the earth, the one at the bottom was deposited first and those above were deposited sequentially from oldest to youngest

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5
Q

Principle of Association

A

two objects found in the same deposit/layer were deposited at the same time

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6
Q

Chronometric Dating

A
  • aka absolute dating
  • an estimate of the age
  • always include an error (±) or a range
  • based on natural processes occurring all the time
  • radioactive decay
  • accumulation of trapped electrons

ex. radio carbon, thermoluminescence, argon-argon, uranium series

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7
Q

Methods Based on Radioactive Decay

A
  • elements have multiple forms (isotopes), including some that are unstable (radioactive)
  • half-life
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8
Q

Half-life

A

dating methods based on the principle when a radioactive isotope (R.I.) decays

ex. radiocarbon (R.I. = C-14, half life = 5,730 years)

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9
Q

Radioactive Decay Calculations

A
  • the amount of an isotope that has accumulated or that remains in a material
  • known half life
  • age determined is a statistical estimate

ex. 500 bp ± 50
* means: 68.2% chance that the date is between 550 bp and 450 bp
* double the error: 95.4% chance that the date is between 600 and 400 bp

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10
Q

Luminescence Methods

A
  • electrons from radioactive decay in the environment
  • trapped in flaws in crystal of some minerals (quartz, feldspar, carbonates)
  • accumulate in the traps over time
  • determine the ‘dose rate’ using a dosimeter that is place in the sediment for a known duration
  • measure the amount of electrons and compare with dose rate to determine the amount of time elapsed
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11
Q

Thermoluminescence (TL)

A
  • pottery, burned flint
  • “stopwatch” zeroed by heating (pots, heated rock)
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12
Q

Optically Stimulated Luminescence (OSL)

A
  • wind deposited sediment
  • “stopwatch” is zeroed by light (sediment)
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13
Q

Electron Spin Resonance (ESR)

A
  • teeth
  • “stopwatch” is zeroed by formation of the crystal (teeth)
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14
Q

Absolute Dating

A
  • actual date in solar years previous to the present
  • dendrochronology
  • varves
  • historical chronology
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15
Q

Dendrochronology

A

study of tree-ring patterns

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16
Q

Varves

A

fine layers of washed up sediment deposited in glacial lakes

17
Q

Historical Chronology

A
  • documents with dates (maps, letters, treaties)
  • objects with known dates (coins, nails)